Cupped Fringe Lichen (Heterodermia hypoleuca): COSEWIC assessment and status report 2025
Official title: COSEWIC Assessment and Status Report on the Cupped Fringe Lichen (Heterodermia hypoleuca) in Canada
Committee on the status of Endangered Wildlife in Canada (COSEWIC)
Endangered 2025
Third party material
Further to the Terms and conditions for this website, some of the photos, drawings, and graphical elements found in material produced by COSEWIC are subject to copyrights held by other organizations and by individuals. In such cases, some restrictions on the use, reproduction or communication of such copyrighted work may apply and it may be necessary to seek permission from rights holders prior to use, reproduction or communication of these works.
Document information
COSEWIC status reports are working documents used in assigning the status of wildlife species suspected of being at risk. This report may be cited as follows:
COSEWIC. 2025. COSEWIC assessment and status report on the Cupped Fringe Lichen Heterodermia hypoleuca in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. xii + 61 pp. (Species at risk public registry).
Production note:
COSEWIC would like to acknowledge Samuel Brinker for writing the status report on the Cupped Fringe Lichen (Heterodermia hypoleuca) in Canada, prepared under contract with Environment and Climate Change Canada. This report was overseen by André Arsenault, Co-chair of the COSEWIC Mosses and Lichens Specialist Subcommittee.
For additional copies contact:
COSEWIC Secretariat
c/o Canadian Wildlife Service
Environment and Climate Change Canada
Ottawa, ON K1A 0H3
E-mail: Cosewic-cosepac@ec.gc.ca
Committee on the Status of Endangered Wildlife in Canada (COSEWIC)
Également disponible en français sous le titre :
Évaluation et Rapport de situation du COSEPAC sur l’Hétérodermie à dessous blanchâtre (Heterodermia hypoleuca) au Canada.
Cover illustration/photo:
Cupped Fringe Lichen; photo by Samuel Brinker.
© His Majesty the King in Right of Canada, 2025.
Catalogue No. CW69-14/849-2025E-PDF
ISBN 978-0-660-78434-2
COSEWIC assessment summary
Assessment summary – May 2025
Common name: Cupped Fringe Lichen
Scientific name: Heterodermia hypoleuca
Status: Endangered
Reason for designation: This rare arboreal lichen occurs in southern Canada in the provinces of Ontario, Quebec, and New Brunswick, and is closely associated with the alkaline bark of several broadleaf tree species, including ashes, elms, maples, and oaks. Ash trees in humid forests, its preferred habitat, are suffering from severe mortality associated with a non-native insect, the Emerald Ash Borer. As a result, there is a past and future decline of this lichen reducing the size of the population by more than 70% over the next three generations.
Occurrence: Ontario, Quebec, New Brunswick
Status history: Designated Endangered in May 2025.
COSEWIC executive summary
Cupped Fringe Lichen
Heterodermia hypoleuca
Wildlife species description and significance
The Cupped Fringe Lichen, Heterodermia hypoleuca, is a leafy lichen that grows in grey to blue-grey rosettes, usually to 10 cm in size, though it can occasionally reach up to 25 cm across. It typically grows on the trunks of mature hardwood trees. The rosettes are made up of 1 to 3 mm wide-branching lobes that are loosely attached to tree bark by a network of pale to dark root-like structures (rhizines) that cover the white undersides of the lichen. The fruit bodies (apothecia) on the upper surface are typically cup-shaped, with abundant marginal lobules.
Aboriginal (Indigenous) knowledge
All species are significant, interconnected, and interrelated. There is no species-specific Aboriginal Traditional Knowledge (ATK) in the report.
Distribution
The Cupped Fringe Lichen is a temperate to subtropical species with a widely disjunct global distribution. It is found throughout portions of eastern and western North America, as well as low-lying and montane regions of Central and South America, Africa, and eastern Asia. In the United States, it ranges mainly from the Appalachian Mountains west to the Ozark Ecoregion and north to the Great Lakes Basin. In Canada, the species occurs at its northern limit in portions of Ontario, Quebec, and New Brunswick.
Habitat
The Cupped Fringe Lichen is entirely dependent on the host trees on which it grows. In Canada, these are usually large, long-lived hardwood species in areas with productive, mature hardwood forests that overlay circum-neutral to alkaline substrates. Individuals occur on the trunks (and rarely the thick branches) of living trees, from a few centimetres above the ground up to at least 10 metres, though they most commonly occur between 1 and about 5 metres. Ash trees are the primary host substrate, supporting 74% of the population, followed by oak trees, which host 21%. Habitat includes humid, mature to old calcareous swamps, hardwood forests with vernal ponds or areas with persistent standing water, and rarely, Bur Oak alvar savannah near the Great Lakes coasts.
Biology
The Cupped Fringe Lichen can reproduce in two ways: sexually, through ascospores, or asexually, by breaking apart and growing from fragments. The ascospores, which contain only fungal DNA, are released from the fruiting bodies (apothecia) and are carried by wind, water, and animals. If the conditions are right, the ascospores grow fungal strands (hyphae). For a new lichen to form, these fungal strands must encounter a compatible green alga on a suitable bark surface. If the habitat and conditions are suitable, the fungal strands surround the alga and, along with other microorganisms such as bacteria and other fungi, grow together to create a new lichen.
Population sizes and trends
The enumerated Canadian population identified by field sampling is 476 thalli on 144 trees. For the assessment, we use the number of host trees as individual equivalents. A total of 46 subpopulations have been documented, 36 of which are considered extant. Of these, 34 are in Ontario, 1 is in Quebec, and 1 is in New Brunswick. About 98% of mature individuals occur in Ontario, 2% in Quebec, and less than 1% in New Brunswick. A 21% decline in mature individuals and a 35% decline in host trees is expected within five years, where thalli and dead host trees will be lost as bark substrates deteriorate. Over the next three generations (30 to 90 years), a 78% decline in mature thalli and a 74% decline of host trees (individual equivalents) is projected due to host tree mortality. The estimated Canadian population is likely higher than current counts suggest. Estimates suggest there could be an additional 580 to 900 thalli on 190 to 270 ash trees (individual equivalents) on private land between Peterborough and the Ottawa River, extending north to Pembroke. However, mortality rates for these individuals would likely near 100% within three generations.
Threats and limiting factors
The overall threat impact to the survival of the Cupped Fringe Lichen was assessed as Very high – High. The species is completely dependent on its host trees for continued survival. A total of 107 ash trees sustaining 351 mature individuals will be lost due to the impacts of Emerald Ash Borer (EAB), representing a 72% loss of all occupied host trees and a 74% decline in the number of mature individuals. Only five extant subpopulations occur exclusively on non-ash substrates and are not threatened by EAB. Logging and wood harvesting, road construction, and drought and severe storms caused by climate change are other significant threats.
Protection, status, and ranks
The Cupped Fringe Lichen has a global rank of G5 (Secure). It has a national rank and General Status rank of N3 (Vulnerable) in Canada, which will likely change to N2 following a current revision in Quebec. The Natural Heritage Information Centre (Ontario) has assigned the species a rank of S2 (Imperiled), and the Quebec Conservation Data Centre has assigned it a rank of S3 (Vulnerable); however, it is being revised to S1–S2. It is not yet ranked in New Brunswick. It is not explicitly protected by any federal or provincial laws, nor by any international agreements or conventions. Thirteen extant subpopulations occur in provincial parks and conservation reserves, or in privately owned/managed protected areas.
Technical summary
Heterodermia hypoleuca
Cupped Fringe Lichen
Hétérodermie à dessous blanchâtre
Range of occurrence in Canada (province/territory/ocean): Ontario, Quebec, New Brunswick
Demographic information
Generation time (usually average age of parents in the population; indicate if another method of estimating generation time indicated in the IUCN guidelines (2011) is being used)
Unknown, but estimated to be between 10 and 30 years based on other well-characterized lichen species found on stable bark substratum of mature/long-lived hardwood trees.
Is there an [observed, inferred, or projected] continuing decline in number of mature individuals?
Yes, observed and inferred. Observed declines from Emerald Ash Borer (EAB) and storm events causing windthrow killing occupied trees. Inferred due to continuing host tree mortality from EAB.
Estimated percent of continuing decline in total number of mature individuals within [5 years or 2 generations, whichever is longer up to a maximum of 100 years].
No. Not estimated over two generations.
[Observed, estimated, inferred, or suspected] percent [reduction or increase] in total number of mature individuals over the last [10 years, or 3 generations, whichever is longer up to a maximum of 100 years].
A 4% observed reduction in the number of mature individuals based on declines at three subpopulations totalling at least 20 thalli (on dead, downed trees at three confirmed subpopulations, possibly at a fourth based on dead trees observed from roadside). The reductions are recent, over the last five years, not three generations.
[Projected or suspected] percent [reduction or increase] in total number of mature individuals over the next [10 years, or 3 generations, whichever is longer up to a maximum of 100 years].
Yes. A 74% decline (projected) over the next three generations based on the number of occupied trees (individual equivalents) (107) lost to EAB (101) or other causes (storm events or natural decay) (6).
[Observed, estimated, inferred, or suspected] percent [reduction or increase] in total number of mature individuals over any period [10 years, or 3 generations, whichever is longer up to a maximum of 100 years], including both the past and the future.
Yes. A 74% decline (inferred) based on the number of occupied trees (individual equivalents) lost to EAB (107) or other causes (storm events or natural decay) (6) over the next three generations at extant subpopulations and a 4% past (recent) decline.
Are the causes of the decline a. clearly reversible and b. understood and c. ceased?
- No, decline not clearly reversible if EAB persists and continues to spread
- Yes, cause of decline understood
- No, decline not ceased
Are there extreme fluctuations in number of mature individuals?
No
Extent and occupancy information
Estimated extent of occurrence (EOO)
127,452 km2
Index of area of occupancy (IAO)
(Always report 2 × 2 grid value).
180 km2
Is the population “severely fragmented” that is, is >50% of its total area of occupancy in habitat patches that are (a) smaller than would be required to support a viable population, and (b) separated from other habitat patches by a distance larger than the species can be expected to disperse?
Likely no, but unknown because the size of habitat patches needed to support a viable population of this species has not been determined.
Unknown
Number of “locations” (use plausible range to reflect uncertainty if appropriate)
There are six locations: one location represents 31 extant subpopulations with the most plausible threat from EAB; the remaining 5 extant subpopulations face impacts from climate change, but are treated separately since those effects are likely to be site-specific.
Is there an [observed, inferred, or projected] decline in extent of occurrence?
Yes, projected loss of 25 subpopulations where individuals occur exclusively on ash trees that will be lost due to indirect mortality via EAB (EAB was observed already at 14 of these).
Is there an [observed, inferred, or projected] decline in index of area of occupancy?
Yes, projected loss of 25 subpopulations and 107 occupied trees where individuals occur exclusively on ash trees expected to die due to indirect mortality via EAB (EAB was observed already at 14 of these).
Is there an [observed, inferred, or projected] decline in number of subpopulations?
Yes, projected loss of 25 of 36 extant subpopulations where all individuals occur exclusively on ash trees that will succumb to EAB (EAB was observed already at 14 of these 25).
Is there an [observed, inferred, or projected] decline in number of “locations”?
No
Is there an [observed, inferred, or projected] decline in [area, extent and/or quality] of habitat?
Yes, observed decline in area and quality of habitat at 14 subpopulations where the quality and extent of swamp forest with mature ash is declining due to EAB as large diameter/mature ashes (preferred substrate) aren’t being replaced. Projected for another 15 subpopulations where ash is an important canopy component, and these habitats will continue to decline in quality with the loss of key host trees. Also, potentially suitable unoccupied habitat with ashes is declining, limiting dispersal potential.
Are there extreme fluctuations in number of subpopulations?
No
Are there extreme fluctuations in number of “locations”?
No
Are there extreme fluctuations in extent of occurrence?
No
Are there extreme fluctuations in index of area of occupancy?
No
| Subpopulations (give plausible ranges) | N mature individuals |
|---|---|
| Ontario (34 extant subpopulations) |
|
| Quebec (1 extant subpopulation) |
|
| New Brunswick (1 extant subpopulation) |
|
Known population Additional individuals possible on private land in Ontario Total estimated population |
|
Quantitative analysis
Is the probability of extinction in the wild at least [20% within 20 years or 5 generations whichever is longer up to a maximum of 100 years, or 10% within 100 years]?
Not assessed
Threats (direct, from highest impact to least, as per IUCN Threats Calculator)
Was a threats calculator completed for this species?
Yes (Appendix 3).
Overall assigned threat impact: Very high – High
- Natural system modifications (7.3 Other ecosystem modifications) Very high – High Impact
- Climate change and severe weather (11.1 Habitat shifting and alteration) Unknown Impact (11.2 Droughts) Unknown Impact (11.4 Storms and flooding) High – Low Impact
- Biological resource use (5.3 Logging and wood harvesting) Medium – Low Impact
- Transportation and service corridors (4.1 Roads and railroads) Low Impact
- Pollution (9.5 Air-borne pollutants) Unknown Impact
Rescue effect (immigration from outside Canada)
Status of outside population(s) most likely to provide immigrants to Canada.
Not ranked (that is, SNR or no rank) in any adjacent U.S. jurisdictions. However, Maine, Michigan, New York, Pennsylvania, and Vermont have only historical collections (none from the last 20 years). Minnesota has four recent collections from three sites. Ohio has one recent collection from 2017.
Is immigration known or possible?
Possibly, but unlikely because of distance. The closest extant site is in Ohio, over 600 km from the nearest Canadian site.
Would immigrants be adapted to survive in Canada?
Presumably.
Is there sufficient habitat for immigrants in Canada?
Unknown. It is unclear whether habitat is limiting in most of its range. However, it is highly unlikely to mitigate the ongoing impact of EAB.
Are conditions deteriorating in Canada?
Yes. Both the availability of its most important host trees (ashes) and the amount of swamp forest with mature ash is declining due to EAB, which is reducing substrate availability, and ashes are not reaching a suitable size rapidly enough to compensate for losses.
Are conditions for the source (that is, outside) population deteriorating?
Unknown. However, ashes face the same threat posed by EAB in adjacent jurisdictions in Maine, Michigan, Minnesota, New York, Ohio, Pennsylvania, and Vermont.
Is the Canadian population considered to be a sink?
No
Is rescue from outside populations likely?
No. Rescue is unlikely to change status because mature ash trees are dying due to EAB.
Data sensitive species
Is this a data sensitive species?
No
Status:
COSEWIC status history: Designated Endangered in May 2025.
Status and reasons for designation
Status: Endangered
Alpha-numeric codes: A3bce+4abce; C2a(i)
Reason for designation: This rare arboreal lichen occurs in southern Canada in the provinces of Ontario, Quebec, and New Brunswick, and is closely associated with the alkaline bark of several broadleaf tree species, including ashes, elms, maples, and oaks. Ash trees in humid forests, its preferred habitat, are suffering from severe mortality associated with a non-native insect, the Emerald Ash Borer. As a result, there is a past and future decline of this lichen reducing the size of the population by more than 70% over the next three generations.
Applicability of criteria
Criterion A (Decline in total number of mature individuals):
Meets Endangered, A3bce. Observed decline in number of mature individual equivalents that is projected to continue over the next three generations at a rate of 74%. Meets Endangered, A4abce, observed past decline of 4%, and future inferred and projected decline of mature individual equivalents at a rate of 74%. Most of the decline is due to the effects of an introduced insect species causing mortality of the preferred host trees.
Criterion B (Small range and decline or fluctuation):
Not applicable for Endangered. Meets Threatened, B2ab(i,ii,iii,iv,v). IAO is 180 km2. The population is (a) known to occur from fewer than 10 locations, and (b) has a projected continuing decline in (i) EOO, (ii) IAO, (iv) number of sub-populations; an observed and projected continuing decline in (iii) quality of habitat; and observed and inferred continuing decline in (v) number of mature individual equivalents.
Criterion C (Small and declining number of mature individuals):
Meets Endangered, C2a(i). Number of mature individual equivalents is 334 to 414, with fewer than 250 in any one subpopulation, and there is an inferred continuing decline.
Criterion D (Very Small or restricted population):
Not applicable for Endangered. Meets Threatened, D1. Number of mature individual equivalents (334 to 414) is fewer than the threshold of 1,000.
Criterion E (Quantitative analysis):
Not applicable. Analysis not conducted.
COSEWIC history
The Committee on the Status of Endangered Wildlife in Canada (COSEWIC) was created in 1977 as a result of a recommendation at the Federal-Provincial Wildlife Conference held in 1976. It arose from the need for a single, official, scientifically sound, national listing of wildlife species at risk. In 1978, COSEWIC designated its first species and produced its first list of Canadian species at risk. Species designated at meetings of the full committee are added to the list. On June 5, 2003, the Species at Risk Act (SARA) was proclaimed. SARA establishes COSEWIC as an advisory body ensuring that species will continue to be assessed under a rigorous and independent scientific process.
COSEWIC mandate
The Committee on the Status of Endangered Wildlife in Canada (COSEWIC) assesses the national status of wild species, subspecies, varieties, or other designatable units that are considered to be at risk in Canada. Designations are made on native species for the following taxonomic groups: mammals, birds, reptiles, amphibians, fishes, arthropods, molluscs, vascular plants, mosses, and lichens.
COSEWIC membership
COSEWIC comprises members from each provincial and territorial government wildlife agency, four federal entities (Canadian Wildlife Service, Parks Canada Agency, Department of Fisheries and Oceans, and the Federal Biodiversity Information Partnership, chaired by the Canadian Museum of Nature), three non-government science members and the co-chairs of the species specialist subcommittees and the Aboriginal Traditional Knowledge subcommittee. The Committee meets to consider status reports on candidate species.
Definitions
(2025)
- Wildlife Species
- A species, subspecies, variety, or geographically or genetically distinct population of animal, plant or other organism, other than a bacterium or virus, that is wild by nature and is either native to Canada or has extended its range into Canada without human intervention and has been present in Canada for at least 50 years
- Extinct (X)
- A wildlife species that no longer exists
- Extirpated (XT)
- A wildlife species no longer existing in the wild in Canada but occurring elsewhere
- Endangered (E)
- A wildlife species facing imminent extirpation or extinction
- Threatened (T)
- A wildlife species is likely to become endangered if limiting factors are not reversed
- Special Concern (SC)*
- A wildlife species that may become a threatened or an endangered species because of a combination of biological characteristics and identified threats
- Not at Risk (NAR)**
- A wildlife species that has been evaluated and found to be not at risk of extinction given the current circumstances
- Data Deficient (DD)***
- A category that applies when the available information is insufficient (a) to resolve a species’ eligibility for assessment or (b) to permit an assessment of the species’ risk of extinction
- *
- Formerly described as “Vulnerable” from 1990 to 1999, or “Rare” prior to 1990
- **
- Formerly described as “Not In Any Category”, or “No Designation Required.”
- ***
- Formerly described as “Indeterminate” from 1994 to 1999 or “ISIBD” (insufficient scientific information on which to base a designation) prior to 1994. Definition of the (DD) category revised in 2006
The Canadian Wildlife Service, Environment and Climate Change Canada, provides full administrative and financial support to the COSEWIC Secretariat.
Wildlife species description and significance
Name and classification
Scientific name: Heterodermia hypoleuca (Ach.) Trevis.
Pertinent synonyms: Anaptychia hypoleuca (Ach.) A. Massal., Parmelia speciosa var. hypoleuca Ach., Physcia hypoleuca Muhl. Tuckerm., Polyblastidium hypoleucum (Ach.) Kalb
Common names: Cupped Fringe Lichen, Hétérodermie à dessous blanchâtre
Family: Physciaceae
Major Group: Lichens (lichenized Ascomycetes)
Bibliographic citation: Atti Soc. Ital. Sci. Nat. Milano 11: 615. 1868 (1869)
Type: U.S. Pennsylvania, 29 November 1805, Muhlenberg (lectotype, selected by Moberg and Nash 1999: 5, H)
Heterodermia Trevis. is a genus of lichenized fungi in the family Physciaceae (Brodo et al. 2001) with approximately 175 species worldwide (Lücking et al. 2017). The species are most common in tropical montane regions, occurring mostly on tree bark.
The term hypoleuca comes from two Greek roots, hupo, “below,” and leukos, “white,” referring to the white undersides of the thallus lobes.
Mongkolsuk et al. (2015) attempted to split the monophyletic genus Heterodermia into several groups based on collections examined from Thailand, in which they formally described the genera Leucodermia Kalb and Polyblastidium Kalb based on terpenoid chemistry, overall thallus appearance, and anatomy, as well as two informally named species groups, but the phylogenetic position of the named or unnamed groups was not presented. The authors placed H. hypoleuca in Polyblastidium based on its non-ascending, foliose thallus, which attaches to the substrate, and on its ecorticate lower surface. Since a complete phylogeny of the genus is still lacking, the generic divisions proposed by those authors have not been widely accepted (for example, Fernanda de Souza et al. 2022) and North American species are, for now at least, retained within the genus Heterodermia sensu lato (Esslinger 2021).
Morphological description
Heterodermia hypoleuca is a spreading, loosely appressed foliose (leafy) lichen forming roundish patches (Figure 1), typically up to 10 cm wide. In the Canadian population, it has occasionally been observed to reach 25 cm, with linear lobes up to 3 mm wide, that are irregularly or dichotomously branched. Lobules resembling small versions of the primary lobes can develop in older central or damaged portions of the thallus, and these individuals often lack apothecia. The upper surface is mineral grey to blue-grey, smooth and epruinose, often with pycnidia, and the medulla is white. The lower surface is pale, white to tan (often darker towards the centre), and ecorticate (lacking a cortex), with dark, simple to squarrose rhizines coalescing into a mat and projecting marginally. Round apothecia (fruit bodies) <1 to 10 mm in diameter are produced on the lobe surface, and are strongly concave, with brown, non-pruinose discs and thick, in-rolled, lobulate thalline margins. Ascospores are brown, 2-celled, ellipsoid, Pachysporaria-type, measuring on average 23.5 to 30.5 µm × 12.5 to 16.0 µm (Moberg and Nash 1999).
Figure 1. Photographs of Heterodermia hypoleuca from Ontario. A) Overall habit, showing several thalli with apothecia growing on Green Ash bark. B) Closeup of apothecia showing distinctive lobed or “fringed” margins. C) A densely lobulate, merged thallus with many overlapping lobules and no apothecia on Green Ash bark (photos: S. Brinker).
Heterodermia hypoleuca is the only apotheciate species in the genus with non–ascending lobes known to occur in eastern North America (Lendemer 2009).
The photosynthetic partner in H. hypoleuca is a green unicellular coccoid alga in the genus Trebouxia, a very common lichen photobiont partner genus.
Chemistry
The chemical substances present in H. hypoleuca are atranorin, zeorin, and leucotylin.
Population spatial structure and variability
Little is known about the population structure and its variability in H. hypoleuca, but dispersal is likely limited. Individuals in the Canadian population typically occur along meandering river corridors or edges of forested vernal ponds or large wetlands surrounded by rich lowland forest. These environs likely have had less disturbance and logging pressure, being too wet/hazardous or inaccessible, and often contain larger and/or older trees relative to most surrounding forest stands. These sites also appear to be limited in extent and spatially restricted within the larger landscape matrix. The landscape surrounding occupied habitat is most often characterized by younger, even-aged forests; forests without appropriate tree hosts; forests occurring on noncalcareous parent or till material; or forests in drier, less humid upland habitats.
For the purposes of the report, occupied sites separated by at least 1 km, and up to 3 km in areas of continuous forest cover with persistently suitable habitat, have been treated as discrete subpopulations following the guidelines in NatureServe (2020).
Designatable units
There is no evidence for discreteness within the species’ Canadian range. No recognized infraspecific taxa or varieties of H. hypoleuca exist. Genetic diversity in H. hypoleuca has not been sufficiently studied to suggest or refute distinctiveness in any one region. The Canadian population of H. hypoleuca occurs in three COSEWIC National Ecological Areas (Great Lakes Plain, Boreal, Atlantic) (Figure 2), although natural disjunction between these is not sufficient to warrant separate designatable units.
Figure 2. Map of extant Heterodermia hypoleuca subpopulations (white circles ◯) in Canada (excluding extirpated subpopulations and historical collections with vague or questionable localities) used to determine the extent of occurrence (grey polygon) in relation to National Ecological Areas (EAs; Atlantic, Boreal, and Great Lakes Plains).
Long description
The map of southern Ontario, Quebec and New Brunswick indicates the range of three National Ecological Areas (EAs). These are the Atlantic EA in New Brunswick and part of southeastern Quebec, the Boreal EA in northern and central Ontario and Quebec, and the Great Lakes Plains EA in southwestern Ontario and along the land bordering both shores of the St. Lawrence River. The extant subpopulations of Cupped Fringe Lichen, Heterodermia hypoleuca, marked on the map are largely in southern Ontario in both the Great Lakes Plains and Boreal EAs. There is also one subpopulation in Quebec in the Great Lakes Plains EA, one on Manitoulin Island in the Great Lakes Plains EA and one in New Brunswick in the Atlantic EA. The extent of occurrence (EOO) is drawn on the map and covers an area of 127,472 square kilometers.
Special significance
Heterodermia hypoleuca appears to be a good indicator of mature, productive, “high quality” hardwood forests within its Canadian range. Most recent observations tend to occur in habitat that contains older and larger trees than the surrounding environs, and typically show fewer signs of human disturbance. This is a declining ecosystem in the northeast (for example, Hagan and Whitman 2004).
Aboriginal (Indigenous) knowledge
Aboriginal Traditional Knowledge (ATK) is relationship-based. It involves information on ecological relationships between humans and their environment, including characteristics of species, habitats, and locations. Laws and protocols for human relationships with the environment are passed on through teachings and stories, and Indigenous languages, and can be based on long-term observations. Place names provide information about harvesting areas, ecological processes, spiritual significance or the products of harvest. ATK can identify life history characteristics of a species or distinct differences between similar species.
Cultural significance to Indigenous peoples
There is no species-specific ATK in the report. However, H. hypoleuca is important to Indigenous Peoples who recognize the interrelationships of all species within ecosystems.
Distribution
Global range
Heterodermia hypoleuca occurs in temperate to subtropical humid forests and woodlands. It has a disjunct global distribution and is found in montane regions of Central and South America, eastern and southern Africa, Australia, and eastern Asia (Enkhtuya and Javkhlan 2019; Moberg 2011; Swinscow and Krog 1976).
In the United States, its range includes temperate areas of the Appalachian Mountains, extending west locally through the Ohio Valley to Minnesota and the Ozarks (Brodo et al. 2001) (Figure 3). In the northeast, records from New England are mostly historical with only two more recent collections from Maine (Hinds and Hinds 2007). It occurred historically on the eastern seaboard as far south as the Delmarva Peninsula but is considered extirpated in that region (Lendemer and Noell 2018). In the west, it occurs locally along the eastern border of the Sonoran Desert area and in the subtropical part of Baja California (Moberg and Nash 1999).
Figure 3. Distribution of Heterodermia hypoleuca in North America north of Mexico based on collections. Collections made prior to 2003 (>20 years old and considered historical) are indicated with a black circle (●). Early literature reports from Canada that are unverifiable are indicated with a black asterisk (✱). Collections made between 2003 and 2024 are indicated with a white circle (◯).
Long description
The map of central and eastern North America shows the areas covered by deciduous, coniferous and mixed forests. Overlaid on the forest cover are sites where Cupped Fringe Lichen has been collected, and they are all in areas with deciduous or mixed forest. Pre-2003 lichen collections occur from southern Quebec and Ontario through the New England states and along the Appalachian Mountains. There are also pre-2003 collection sites to the west and south of Lake Superior and a few sites near the Texas and Arizona borders with Mexico. The lichen collection sites from 2000 to 2024 occur in three main clusters, one in southern Ontario, one in the southern Appalachians and one in Missouri and Arkansas. A few other collection sites for the 2000 to 2024 period are in Quebec, New Brunswick, Minnesota, Wisconsin and Ohio. Two unverified sites from literature reports are in Ontario, one east of Georgian Bay and the other north of Lake Superior.
Canadian range
Heterodermia hypoleuca occurs in the provinces of Ontario, Quebec, and New Brunswick. It occupies portions of three of Canada’s terrestrial ecozones including the northern part of the Mixedwood Plains, the southern part of the Boreal Shield and a small area of the Atlantic Maritime (Wiken et al. 1996; Figure 2). It reaches its northern distributional limit in this region at 48.4° N. Its Canadian range likely accounts for less than 1% of its global range.
Ontario
In Ontario, there are 34 extant subpopulations representing 98% of the Canadian population, ranging from Peterborough County east to the Ottawa River. A single small outlying subpopulation occurs west of this area on Manitoulin Island. Five subpopulations here are considered extirpated (virtually no likelihood of rediscovery due to significant alteration from urbanization or intensive agriculture, and recent search efforts failed to locate individuals or suitable habitat), and one is possibly extirpated (has not been observed in >20 and the single individual was recorded on a downed tree, suggesting it is likely gone). Two other subpopulations are excluded because they are based on early literature reports and are of questionable validity (see Search effort).
Quebec
In Quebec, there is one extant subpopulation from the St. Armand area near the Vermont border representing 2% of the Canadian population. Another five historical collections are known from Gatineau east to Île Bonaventure. Their status has not been assessed in recent years, but their localities are vague and their continued presence is unknown. However, at least two thalli were recorded on elm trees which have suffered extensive declines due to Dutch Elm Disease and are likely extirpated.
New Brunswick
A small subpopulation in New Brunswick was recently discovered along the St. John River in 2022 (Clayden pers. comm. 2023), representing less than 1% of the Canadian population. There are no other confirmed records from other parts of Canada.
Extent of occurrence and area of occupancy
The extent of occurrence (EOO) is 127,452 km2 calculated using a minimum convex polygon that encompasses records from 2012 to 2024 (Figure 2).
The index area of occupancy (IAO) is 180 km2 calculated using a 2 × 2 km grid drawn over known records from 2012 to 2024.
Records that have vague locational information were only reported historically on dead trees, or are considered extirpated were excluded from these calculations.
Search effort
Ontario
Prior to 1998, H. hypoleuca was considered possibly extirpated in southern Ontario (Wong and Brodo 1992) and in Canada (Goward et al. 1998). Based on verified collections at the Canadian Museum of Nature (CANL), it was formerly present in several locations: Ottawa (Macoun, 1891), near Hull (Macoun, 1907), Brighton (Macoun, s.n.), Prescott (Billings, s.n.), and near Wooler (Macoun 1902). Lichenologists familiar with this lichen (Sam Brinker [SB], Irwin Brodo, Rob Lee [RL], James Lendemer, Chris Lewis [CL], Troy McMullin, and numerous others) have searched many lichen-rich sites in southern Ontario over the past 50 years, covering the range of these historical localities and expected habitat for the species. Dedicated searches of suitable swamp forest habitat were also completed during the preparation of the COSEWIC status report on Flooded Jellyskin (Leptogium rivulare) in Canada (COSEWIC 2015) by SB and CL. Other targeted searches for H. hypoleuca were carried out independently by SB and CL between 2012 and 2019. While no rediscoveries were made at historical locations, this work resulted in the discovery of ten new subpopulations from Peterborough, Hastings, Frontenac, and Renfrew counties (Brinker 2020; Lewis 2019; Lewis and Brinker 2017). Several detailed lichen-focused inventories have also been completed in southern and central Ontario without documenting additional records of H. hypoleuca (for example, Brodo et al. 2013, McMullin and Lendemer 2016, Maloles et al. 2018, Brodo et al. 2021). Between 2022 and 2024, Jon Ruddy (JR) independently searched for H. hypoleuca in eastern Ontario and discovered it in four new subpopulations (See Tables 1 and 2).
Macoun (1902) mentioned H. hypoleuca (as Physcia hypoleuca) from Algonquin Park (July 19, 1900, Red Pine Lake) and Lake Nipigon (July 17, 1884); however, there are no supporting specimens at CANL, where most of Macoun’s collections are housed. Additionally, there have been no subsequent reports from either region, though both areas have been surveyed by experienced lichenologists.
Areas of potential occurrence in the general vicinity of Lake Nipigon, where the lichen was reported by Macoun (1902), have been explored over many years by lichenologists. Ahti’s (1964) pioneering assessment of macrolichens in boreal and arctic portions of Ontario included numerous collection sites along the northern coastal strip of Lake Superior and areas of the Lake Nipigon basin (corresponding to his strongly humid southern boreal forest zone). However, he did not document H. hypoleuca. The area surrounding the city of Thunder Bay which is known for several disjunct stands of Acer saccharum has been well covered by Claude Garton and Paul Barclay-Estrup with respect to foliose and fruticose lichens, and neither documented any records of H. hypoleuca (Barclay-Estrup and Sims 1979, Crowe 1994). Crowe (1994) produced a list of lichens for the Thunder Bay District and did not make mention of H. hypoleuca. Sam Brinker explored numerous islands on Lake Nipigon in 2016 that contained mature cedar forests, and did not successfully locate any individuals. Sam Brinker also searched over 30 mature cedar and ash swamp forests in the Rainy River and Thunder Bay District in 2016 to 2017 during targeted surveys for Rimmed Shingle Lichen (Fuscopannaria leucosticta) (COSEWIC 2019). Numerous islands on the north shore of Lake Superior have been surveyed by SB with Parks Canada in the newly established Lake Superior National Marine Conservation Area, which included visits to numerous offshore islands in 2018 and 2019. The Tuckerman Group of lichenologists (over 40 attendees) visited Sleeping Giant Provincial Park in 2019 and conducted detailed lichen surveys throughout the park, including representative old-growth coastal forest stands and ash and cedar swamp forest, but did not record the species.
Areas of potential occurrence in and surrounding Algonquin Park have also been explored without documenting H. hypoleuca. Several lichen checklists for the park have been compiled from collecting activities of former park staff and CANL research associate staff spanning 50 years. The most recent lichen checklist produced in 2023 (Lewis et al. 2023) included focused surveys of unique habitats including old-growth dependent lichens in mature forest stands, and produced no records of H. hypoleuca. The lack of any substantiating observations casts some doubt about its historical presence here and at Lake Nipigon. These early reports may represent transcription or labelling errors, as both Wong and Brodo (1992) and others who have examined Macoun’s collections (for example, Godfrey 1977), have noted inconsistencies with his label data in his series of Canadian lichens. The overall scarcity of calcareous hardwood stands in Algonquin Park casts further doubt about its presence there.
Heterodermia hypoleuca occurs in Minnesota, but is very rare. There is a possibility that it could occur in adjacent areas of NW Ontario, particularly in the southern Rainy River District. In 2013, SB and CL conducted unsuccessful searches of its potential range in this region, including areas around Lake of the Woods, Rainy Lake, and Rainy River bordering Minnesota, while conducting targeted rare lichen surveys.
Quebec
Prior to recent search efforts, seven specimens representing six subpopulations from Quebec were housed in collections at the CANL, Louis-Marie Herbarium (QFA), and New York Botanical Gardens (NY). All but one were made before approximately 1970. The label data associated with these specimens are mostly vague, with only the nearest town or place name referenced, making relocation difficult. In 1905, John Macoun made three collections, including one from Montmorency Falls and two from “Cap-à-l’Aigle.” While multiple locations in Quebec share the name Cap-à-l’Aigle, Macoun made a collecting trip to the St. Lawrence River Valley in 1905 where he visited Cap-à-l’Aigle on July 25 (Lamb 1968), located on Rivière-Malbaie near its mouth on the St. Lawrence River, just north of Point-au-Pic.
There is a 1958 Fabius LeBlanc collection of H. hypoleuca from Mont Johnson (also known as Mont Saint-Grégoire), southeast of Montreal. There is also a specimen collected by Eric Thorn in 1961 from Île Bonaventure near Gaspé, and an undated Anne Hanes specimen from Gatineau Park. Hanes’ specimen was likely collected sometime between 1967 and 1973, based on a 2023 search of the Consortium of Lichen Herbaria (CLH), which produced 91 of her specimens from Gatineau Park, all made between these years. Despite considerable lichen exploration in the Ottawa and Hull regions by CANL staff and their students, from the 1970s to the present day (which included Gatineau Park), no recent observations of H. hypoleuca have been made in the region (Brodo 1981, 1988; Freebury 2011; Brodo et al. 2021). There was a study of the epiphytic lichens and bryophytes of hardwood forests in the Eastern Townships, but H. hypoleuca was not recorded (LeBlanc 1963). Other notable early lichen studies include surveys of areas between Quebec City and the Gaspé Peninsula (Lepage 1947 to 1949). More recently, researchers such as McMullin et al. (2017), Paquette (2019), and Paquette and McMullin (2020), have contributed to documenting lichen diversity in the Gaspé Peninsula and Côte-Nord, but did not report the presence of H. hypoleuca. Other targeted lichen surveys of southern Quebec in mixed and deciduous forests between the 45th and 50th parallels were recently summarized by Lavoie et al. (2024), which include the discovery of numerous rare lichens, though no new H. hypoleuca locations were documented (See Tables 1 and 2).
The only extant subpopulation that is known in Quebec was discovered by Richard Harris at Sanctuaire George H. Montgomery in 2016 during the 40th annual Andrews Foray (traditionally a bryophyte foray with lichenologists attending as well).
Two specimens collected by Frère Marie-Anselme in 1936 and 1938 from Shefford and Lac Sept-Îles, housed at QFA and originally identified as H. hypoleuca, represent misidentifications. These specimens are Heterodermia speciosa, powdered fringe lichen, and Anaptychia palmulata, shaggy-fringed lichen.
New Brunswick
In New Brunswick, H. hypoleuca was recently discovered by Stephen Clayden in April 2022 on a single multi-stemmed Green Ash (Fraxinus pennsylvanica) near the Saint John River at Lower Lincoln, about 15 km downriver from Fredericton. Its presence on the same tree was reconfirmed in April 2024, and approximately two hours of searching in the same area yielded no additional observations. No other targeted surveys for this lichen have been conducted in the province. However, Green Ash stands along or near the Saint John River between Mactaquac and Saint John have been examined sporadically during general lichen surveys over the past few decades and have not produced any other records of H. hypoleuca (Clayden pers. comm. 2024).
Manitoba
Reference to H. hypoleuca from Manitoba exists in an unpublished list of macrolichens prepared by Michele Piercey-Normore and reported by the Canadian Endangered Species Conservation Council (CESCC) (2010); however, its presence has proven to be incorrect. It was reported in error and the collection believed to be the basis of the report was revised to Heterodermia speciosa (Michele Piercey-Normore and Diana Sawatzky pers. comm. 2022).
Habitat
Habitat requirements
Heterodermia hypoleuca is entirely dependent on the host trees on which it grows. Its preferred substrate is the bark of long-lived hardwood trees that typically occur in mature, productive forests with high humidity and canopy gaps, and frequently with old and leaning trees that often have patchy bryophyte cover (Figure 5). Two subpopulations occur in unusual Bur Oak (Quercus macrocarpa) alvar savannah and another extends into open oak woods along the Ottawa River. At these locations there are numerous old oak trees that occur near large bodies of water, where high levels of constant humidity mimic conditions of humid swamp forests. Thalli colonize the vertical trunks (or rarely thick branches) of living trees from a few centimetres above ground up to at least 10 metres, though recent surveys found individuals to occur mostly at roughly breast height to about 5 metres. Thalli may persist on dead trees for a time, but eventually die as the bark decays or falls off. In a phytosociology study of corticolous cryptograms in Wisconsin, Hale (1955) found it to occur most frequently at 1.3 metres from the base of trees rather than on the base. Host tree trunks are typically clear of dense undergrowth, allowing for good air circulation and light penetration. During surveys between 2019 and 2024, it was observed that suitable host tree trunks that were shaded by dense shrubby undergrowth or were in stands that lacked canopy gaps were not colonized.
Heterodermia hypoleuca’s preferred substrata are trunks of medium- to large-sized hardwood trees with relatively thick, corky, and often fissured bark (Figure 6). These bark characteristics are likely important in retaining moisture and may also provide suitable microhabitat for the establishment of dispersing propagules. Bark chemistry plays an important role in controlling epiphytic lichen communities (Hauck 2011). Roughly 95% of all individuals in the Canadian population occur on ashes (Fraxinus spp.) and oaks (Quercus spp.); 90% of the host trees are ashes and oaks, species which tend to have a slightly basic bark pH, especially as they attain older ages (Farmer et al. 1991). Trees commonly encountered in occupied habitat with smooth or slightly acidic bark, such as Silver Maple (Acer saccharinum) or the hybrid Freeman’s Maple (Acer x freemanii), did not host H. hypoleuca thalli. While the connection between soil and bark chemistry is not proven, significant correlations between bark and soil chemistry suggest higher amounts of total bark calcium is positively correlated with soil pH (Gustafsson and Eriksson 1995). Calcium has also been considered to account for a large part of the buffering capacity and regulation of bark pH (Farmer et al. 1991). In its Canadian range, both tree species selection and underlying soil chemistry support this lichen’s affinity for base-rich substrates.
Occasionally, smaller trees are colonized, but normally within stands that contain larger trees surrounded by continuous forest cover. This suggests forest continuity (temporally unbroken continuity of forest stand habitat), rather than just tree age or size is likely important in determining habitat suitability (for example, Boch et al. 2013). It is unclear if bryophyte cover plays any positive role in the establishment or growth of H. hypoleuca. Thalli were occasionally observed adjacent or partially over bryophytes on tree trunks. More often; however, thalli were growing on bare bark. In some cases, occupied trees had luxuriant bryophyte growth elsewhere on the tree trunks, particularly in humid sites with mature, open canopies.
Table 3 presents the number of mature individuals on each host tree species. Of 476 individuals recorded, 351 (74%) occur on ash trees, including Green Ash (Fraxinus pennsylvanica), Black Ash (F. nigra), and unidentified ash species. Ninety-nine individuals (21%) occur on Bur Oak (Quercus macrocarpa) and Red Oak (Q. rubra), followed by 12 (3%) on American Basswood (Tilia americana), 10 (2%) on Sugar Maple (Acer saccharum), 3 (1%) on Eastern White Cedar (Thuja occidentalis), and one (<1%) on Bitternut Hickory (Carya cordiformis). Figure 7 provides a detailed breakdown of all living and dead host trees occupied by H. hypoleuca at extant subpopulations. Ashes are the most important host substrate, representing 70% of occupied trees. Bur Oak and Red Oak represent 19% of occupied trees, followed by American Basswood (4%), Sugar Maple (3%), Eastern White Cedar (2%) and Bitternut Hickory (<1%). Early collections suggest that additional substrates, such as American Elm (Ulmus americana), spruce (Picea sp.) and birch (Betula sp.) may have been historically occupied.
In adjacent jurisdictions to Canada, such as Wisconsin, habitat descriptions include coastal hardwood forests of southern Lake Superior with varying compositions of oak, maple, and birch, and maple, birch, and balsam fir (Wetmore 1990). In Minnesota, Wetmore (1981) mentioned it from “an old, dry ash bog that probably escaped logging.” In Ohio, only one recent collection has been made where H. hypoleuca occurred on the base of large oaks in mature forest (Curtis 2022 pers. comm.). Elsewhere in the U.S., recent observations, which primarily include areas of high-elevation forest in the Appalachian and Ozark Mountains, are usually associated with higher quality mature forest stands where the lichen mostly occurs on white oaks and other soft-barked trees like ashes (Lendemer pers. comm. 2021).
Habitat trends
A substantial portion of mature forest habitat in eastern North America, including the Canadian range of H. hypoleuca, has been lost since the arrival of Europeans (Fuller et al. 1998; Laflamme et al. 2016). Logging, forest fires, and settlement between the mid-1700s and the early 1900s resulted in the destruction of much of the original forests coinciding with the species range. The Great Lakes Plains National Ecological Area (Figure 2), where 20 of the 36 extant subpopulations representing 56% of the Canadian population of H. hypoleuca occurs, is the most anthropogenically modified region in Canada, having undergone dramatic change over the past 200 years. Forest was originally the dominant ecosystem type in most of the ecozone (Taylor et al. 2014). By 1920, about 90% of the original forests south and east of the Canadian Shield in Ontario were converted to non-forest uses (Larson et al.1999). While forest cover has rebounded since that time to roughly 22% to 25% today, the current landscape is heavily fragmented, and most forest remnants are even-aged second or third growth stands occurring in isolated patches (Taylor et al. 2014). It is estimated that less than 0.07% of the remaining woodlands in the mixedwood plains can be characterized as old-growth (based on a definition of greater than 120 years), which would have been dominant in the period prior to European settlement (Taylor et al. 2014).
Fifteen H. hypoleuca subpopulations representing 42% of the Canadian population fall within extreme southern portions of the Boreal Ecological Area, although these are all within 30 km or less of the Great Lakes Plains boundary to the south, where forests have generally been subject to the same pressures and changes.
One extant subpopulation occurs in the Atlantic Ecological Area. Historical accounts by early travellers in the Atlantic Maritime Ecozone of Quebec and New Brunswick described a different forest from what is encountered in much of the region today, with larger trees and higher proportions of late-successional species (Loo et al. 2010). The early 1800s saw the onset of major changes to forest cover with the start of commercial logging and the availability of an extensive network of rivers and tributaries to transport logs. Sequential waves of selective harvesting and clearcutting of more desirable shade-tolerant hardwoods through to the present day have caused large decreases in cedar, maple, beech, ash, and other tolerant hardwoods in these regions (Bouchard et al. 1989), thereby reducing the quality and extent of suitable habitat for H. hypoleuca. In their description of major forest types and their human influences, Loo et al. (2010) reported that wet calcareous mixedwood and rich tolerant bottomland forests in the region have been greatly reduced and highly fragmented due to clearing and draining for agriculture and urban development, flooding for power production, and removal of trees for timber extraction.
Biology
Life cycle and reproduction
Heterodermia hypoleuca produces apothecia and ascospores derived from meiosis that are expelled from the apothecia, representing propagation through fungal-only propagules. Conidia-bearing structures (pycnidia) are commonly observed on thalli and produce asexual spores that likely function primarily as sexual gametes involved in apothecia formation. However, conidia of a few lichen fungi have been successfully germinated in culture (for example, Vobis 1977), and it is possible that they might function in some cases as vegetative dispersal of the mycobiont. However, there are no records of H. hypoleuca conidia germinating. Because compatible photobiont cells are not dispersed together with ascospores, to germinate and give rise to a new individual, an ascospore must land on a suitable substratum hosting a compatible photosynthetic partner, an alga in the genus Trebouxia. If the photobiont strain and mycobiont partners are compatible, the alga will become enveloped by fungal hyphae and a lichen will begin to form and differentiate into a visible thallus. It is not known how long it takes H. hypoleuca to develop from a germinating ascospore to a reproductively mature thallus, nor is the lifespan known. Soredia, isidia, or other specialized vegetative propagules are lacking in H. hypoleuca. It likely therefore reproduces vegetatively through occasional fragmentation of the thallus, although it is not known how often this occurs or under what circumstances.
Generation time
Like other mature forest-dwelling macrolichens that do not produce specialized asexual reproductive structures containing both the mycobiont and photobiont (for example, Anzia colpodes), the generation time of H. hypoleuca has been estimated to be between 10 and 30 years (COSEWIC 2015). While the generation time of H. hypoleuca is unknown, this may be a reasonable estimate for this species based on other well-characterized lichen species found on stable bark substratum of mature/long-lived trees (for example, Larsson and Gauslaa 2011; Lättman et al. 2009). It may be possible for small fragments or lobules that break off the main thallus to reattach down and perhaps up occupied tree trunks transported by gravity, water flow or animal activity. In some sites little within-stand recruitment seems to occur, even where well-developed thalli are present. This could reflect low rates of successful thallus fragmentation and recolonization, successful re-establishment via ascospores, or both.
Physiology and adaptability
Little is known about the physiology of H. hypoleuca in experimental or quantitative studies. Its requirements can be inferred to some degree from its geographic range and within-site distribution. It is completely dependent on other taxa (host tree substratum) for its survival. Its restriction to certain host tree species suggests a preference for bark with a good moisture-holding capacity, and with a relatively high pH and calcium content. These conditions seem best developed in areas on the landscape where trees occur over base-rich soils or parent material. Areas dominated by acidic bedrock or other non-calcareous soils, or trees with acidic bark do not seem to provide habitat for H. hypoleuca in Canada.
Its preference for wet forests that are flooded for a portion of the year or occur near open water in Canada suggests a need for high relative humidity. Its tendency to grow on tree trunks near water features that produce canopy gaps also indicates a preference for higher light levels than those in closed-canopy forests.
Lobules sometimes present on the thallus surface have a possible role in reproduction and dispersal (synonymous with thallus fragmentation), although this has not been proven. Rather, in lichens that form them, it may serve to increase the surface area and boundary layer for gas exchange and water relations (Ott et al. 1993; Tretiach et al. 2005).
Dispersal and migration
Under suitable conditions, H. hypoleuca thalli produce apothecia which contain ascospores. Once mature, the asci eject the ascospores where they disperse passively by wind providing opportunity to colonize new habitat. It is not known how far spores of H. hypoleuca travel (particularly through fragmented habitats), or how long they survive aloft given the difficulties of direct observation. Studies of deposition in other taxa suggest spore deposition drops off to near zero over several metres (for example, Lönnell et al. 2012), although Ronnås et al. (2017) provide evidence to the contrary for lichen-forming fungi. They show that effective ascospore dispersal can be several hundred to thousands of metres from paternal individuals. Ascospores are much more likely to travel longer distances than larger thallus fragments, but that does not guarantee their successful establishment and development. There are many establishment limitations of ascospores that prevent successful colonization of new trees. Suitable substrates, environmental conditions (light, temperature, humidity), and the presence of compatible photobionts are necessary once they come to rest following a dispersal event. Its absence from many areas of apparently suitable habitat is suggestive of rare instances of successful long-distance dispersal.
Because H. hypoleuca does not produce specialized asexual symbiotic propagules (for example, isidia, soredia, phyllidia, schizidia) its primary reproductive mode to colonize new unoccupied habitat is likely sexual reproduction via only the fungal partner. Larger propagules, such as thalli fragments (containing both fungal and algal cells), may detach and reattach elsewhere on the same tree trunk. While they are unlikely to disperse any measurable distance within suitable habitat beyond occupied trees, they have a higher potential for successful establishment than fungal-only ascospores (Tripp et al. 2016). Although not easily observable, the role of avian, arthropod, and mammalian vectors of ascospores, thallus fragments, or living cells of lichen-forming fungi and their photobionts is widely acknowledged and may play a role in the occasional movement propagules.
Interspecific interactions
No obligate associations are known for this species. Heterodermia hypoleuca is one of several hosts for the lichenicolous fungus Sphaerellothecium gallowayi (Diederich 2007). It produces black perithecia that develop over a superficial, dark mycelium obligatorily confined to species of Heterodermia. It has not been reported on North American material of H. hypoleuca (one record from Papua New Guinea).
Population sizes and trends
Sampling effort and methods
During the preparation of this status report, 30 subpopulations with H. hypoleuca records were assessed by Sam Brinker between 2019 and 2024. More than 60 additional sites (defined as a discrete sampling area separated by at least 1 kilometre) were also searched without locating any individuals. A summary of survey dates, sampling locations, and search result are provided in Table 1. Extirpated and excluded subpopulations (Table 2), those on private land, or with vague geographic details were not assessed. In all, search effort totalled over 275 person hours in southern, central, and northwestern Ontario, from Sarnia north to Lake Superior Provincial Park and Timiskaming, west to Rainy River District and Lake of the Woods (Figure 4). SB also visited two sites in Quebec in the vicinity of the only recently documented subpopulation near St. Armand, and a nearby site at Reserve Ecologique Marcel-Raymond. This survey effort resulted in the discovery of 20 new H. hypoleuca subpopulations. Surveys involved searching the following habitat types:
- deciduous and mixed swamps, particularly along lakeshores or rivers
- deciduous or mixed hardwood forests adjacent to large wetlands, bodies of water, or that contained vernal ponds with seasonally flooded treed areas in geographic regions with calcareous parent or till material
- Oak savannah or woodland remnants near bodies of water
Figure 4. Search effort and locations of Heterodermia hypoleuca observations in Canada. White circles (◯) indicate recent records (made between the years 2003 to 2024). Black circles (●) represent historical records with focused search effort (pre-2003). Black triangles (▲) represent historical records lacking specific search effort. White circles with an x (⊗) represent unsuccessful searches completed during fieldwork for this report between the years 2019 to 2024. Half circles (◑) represent pre-2019 general search and collecting activity with respect to the lichen genus Heterodermia within the Canadian range of H. hypoleuca.
Long description
The map of Ontario, Quebec and the Maritime Provinces shows the areas covered by deciduous, coniferous and mixed forests. Overlaid on the forest cover are sites where Cupped Fringe Lichen, Heterodermia hypoleuca, has been recorded and searched for. Recent records from 2003 to 2024 are mainly in southeastern Ontario and southern Quebec, with one record in New Brunswick. Historical records with focused search effort pre-2023 are hard to see because of symbol overlap; however, there appear to be a few records to the north of Lake Superior. Historical records lacking specific search effort are also few, and they occur in southern Ontario and eastern Quebec. Unsuccessful searches from 2019 to 2024 occurred throughout southern Ontario and along the southwestern Ontario border with the United States. Last, locations with pre-2019 general search and collecting activity are located throughout the map area, with the majority in southwestern Ontario near and north of the Lake Superior shore in Ontario and in eastern Quebec and throughout much of New Brunswick. All locations with records are in areas with deciduous or mixed forest. Some searches occurred in areas with coniferous forest.
Figure 5. Photographs of various hardwood stands supporting habitat for Heterodermia hypoleuca in Canada. A) Mature deciduous hardwood forest with vernal pond in eastern Ontario. B) Deciduous swamp forest with occasional leaning trees in central Ontario. C) Rich lowland floodplain forest along the Ottawa River. D) Bur Oak alvar savannah along Lake Ontario (photos S. Brinker).
Figure 6. Photographs illustrating tree size and bark characteristics of occupied ash trees which host 74% of the Canadian population. A) Old, large-diameter Green Ash tree trunk occupied by Heterodermia hypoleuca at the edge of calcareous deciduous swamp surrounded by younger forest. B–C) Closeups of varying bark texture of large diameter occupied ash trees showing deeply furrowed, corky bark with patchy bryophyte cover (photos S. Brinker).
Surveys consisted of visually examining the trunks and large branches of suitable hardwood trees (at ground level, and aided with binoculars or DSLR camera with a 200 mm zoom lens) believed to have appropriate bark properties (see Habitat requirements), including ashes (Fraxinus nigra, F. pennsylvanica, F. americana), maples (specifically Acer saccharum, A. nigrum), oaks (Quercus macrocarpa, Q. rubra), American Elm (Ulmus americana), American Basswood (Tilia americana), Bitternut Hickory (Carya cordiformis), and Eastern White Cedar (Thuja occidentalis). Once found, counts of mature individuals included all thalli over 1 cm wide (large enough to confidently detect with distinct lobes) and were tallied along with the number of trees and tree species occupied, the number of thalli on dead standing and downed trees, and the presence of Emerald Ash Borer, (Table 4). Identifying individuals was sometimes difficult because thalli in this species can split or merge together, complicating efforts to accurately tally them. A voucher specimen was collected at most subpopulations if one did not exist, except where too few individuals were present. Those details and the presence/absence of apothecia by subpopulation is provided in Appendix 1.
| Date | Sampling location | Ecol. areaa | County/Municipality | Result |
|---|---|---|---|---|
| Ontario | ||||
| 05-Apr-19 | Cavan Swamp | GLP | Peterborough | Negative |
| 06-Jun-19 | Yorkshire Island | GLP | Prince Edward | Negative |
| 18-Jun-19 | Pottawatomi Wetlands | GLP | GREY | Negative |
| 16-Jul-19 | Crown Land | Boreal | Algoma | Negative |
| 28-Jul-19 | Lake Superior Provincial Park | Boreal | Algoma | Negative |
| 04-Sep-19 | Lake Superior Provincial Park | Boreal | Algoma | Negative |
| 12-Mar-20 | Otonabee Gravel Pit Conservation Area | GLP | Peterborough | Negative |
| 28-Jul-20 | Otonabee Region Agreement Forest | GLP | Peterborough | Negative |
| 26-Aug-20 | Ostrander Crown Land Block | GLP | Prince Edward | Negative |
| 28-Aug-20 | Morris Island Conservation Area | GLP | Ottawa | Negative |
| 11-Sep-20 | Tory Hill | Boreal | Haliburton | Negative |
| 12-Sep-20 | Crown Land | Boreal | Frontenac | Negative |
| 08-Oct-20 | Deseronto Rd. | GLP | Hastings | Negative |
| 20-Oct-20 | Presqu’ile Provincial Park | GLP | Northumberland | Negative |
| 05-Nov-20 | Miller Reserve | GLP | Prince Edward | Negative |
| 10-Nov-20 | Sandbanks Provincial Park | GLP | Prince Edward | Negative |
| 03-Mar-21 | Mark S. Burnham Provincial Park | GLP | Peterborough | Negative |
| 16-Jun-21 | Cultus Forest | GLP | Norfolk | Negative |
| 19-Jun-21 | Brittania Conservation Area | GLP | Ottawa | Negative |
| 27-Jun-21 | Crown Land | Boreal | Parry Sound | Negative |
| 28-Jun-21 | Crown Land | Boreal | Parry Sound | Negative |
| 16-Aug-21 | Beaver Creek A | Boreal | Hastings | Positive |
| 20-Aug-21 | Cassidy Block | GLP | Hastings | Positive |
| 27-Aug-21 | Crown Land | Boreal | Lennox and Addington | Negative |
| 13-Sep-21 | Greenock Swamp | GLP | Bruce | Negative |
| 16-Sep-21 | MacGregor Point Provincial Park | GLP | Bruce | Negative |
| 28-Oct-21 | Petroglyphs Provincial Park | Boreal | Peterborough | Negative |
| 19-Oct-21 | Beaver Creek B | Boreal | Hastings | Positive |
| 05-Nov-21 | Pinery Provincial Park | GLP | Lambton | Negative |
| 14-Jun-22 | Massassauga Point | GLP | Prince Edward | Positive |
| 15-Jun-22 | NCC Rose-Hudgins Property | GLP | Prince Edward | Negative |
| 29-Jun-22 | Belmont Lake | Boreal | Peterborough | Positive |
| 12-Aug-22 | Salmon River | GLP | Frontenac | Negative |
| 15-Aug-22 | Salmon River | GLP | Lennox and Addington | Negative |
| 22-Aug-22 | Ottawa River N | GLP | Renfrew | Positive |
| 22-Aug-22 | Ottawa River S | GLP | Renfrew | Positive |
| 23-Aug-22 | Westmeath Provincial Park | GLP | Renfrew | Positive |
| 01-Sep-22 | Frontenac Provincial Park | Boreal | Frontenac | Negative |
| 01-Sep-22 | Frontenac Provincial Park | Boreal | Frontenac | Negative |
| 07-Sep-22 | Frontenac Provincial Park | Boreal | Frontenac | Negative |
| 08-Sep-22 | Crowe River Conservation Reserve | GLP | Peterborough | Positive |
| 15-Sep-22 | Frontenac Provincial Park | Boreal | Frontenac | Positive |
| 23-Sep-22 | Sydenham River Nature Reserve | GLP | Middlesex | Negative |
| 28-Sep-22 | Crowe River Conservation Reserve | Boreal | Peterborough | Positive |
| 27-Oct-22 | H.R. Frink Conservation Area | GLP | Hastings | Positive |
| 03-Nov-22 | Silver Lake Provincial Park | Boreal | Lanark | Positive |
| 03-Nov-22 | Sharbot Lake Provincial Park | Boreal | Frontenac | Positive |
| 04-Nov-22 | Peterborough County Forest | GLP | Peterborough | Negative |
| 09-Nov-22 | Skunks Misery | GLP | Middlesex | Negative |
| 10-Nov-22 | Reid Conservation Area | GLP | Lambton | Negative |
| 02-Dec-22 | Oatbox | GLP | Peterborough | Positive |
| 02-Dec-22 | Otonabee Region Agreement Forest | GLP | Peterborough | Positive |
| 08-Dec-22 | Darling Wildlife Area | GLP | Peterborough | Negative |
| 08-Dec-22 | Squirrel Creek Conservation Area | GLP | Peterborough | Positive |
| 09-Dec-22 | County Forest East | GLP | Peterborough | Positive |
| 09-Jan-23 | Oxtongue River-Ragged Falls Provincial Park | Boreal | Haliburton | Negative |
| 19-Apr-23 | Crow Lake | Boreal | Frontenac | Positive |
| 28-Apr-23 | Murphy’s Point Provincial Park | Boreal | Lanark | Positive |
| 16-Jun-23 | W of Flanders | Boreal | Rainy River | Negative |
| 16-Jun-23 | N of Emo | Boreal | Rainy River | Negative |
| 17-Jun-23 | Bigsby Island, Lake of the Woods | Boreal | Rainy River | Negative |
| 17-Jun-23 | Snake Island, Lake of the Woods | Boreal | Rainy River | Negative |
| 18-Jun-23 | Budreau’s Beach | Boreal | Rainy River | Negative |
| 21-Jun-23 | Elmo Point, Shoal Lake | Boreal | Kenora | Negative |
| 25-Jun-23 | Pigeon River Provincial Park | Boreal | Thunder Bay | Negative |
| 28-Jul-23 | Beckwith | GLP | Lanark | Positive |
| 28-Jul-23 | Ferguson Forest | GLP | Lanark | Negative |
| 17-Aug-23 | Charleston Lake Provincial Park | Boreal | Leeds and Grenville | Positive |
| 24-Aug-23 | Constant Creek Conservation Reserve | Boreal | Renfrew | Positive |
| 28-Sep-23 | Montreal River | Boreal | Timiskaming | Negative |
| 16-Nov-23 | Westmeath Provincial Park | GLP | Renfrew | Positive |
| 17-Nov-23 | Block 509 | Boreal | Lanark | Positive |
| 01-Dec-23 | Rawdon Block | GLP | Hastings | Positive |
| 05-Dec-23 | Moira River | GLP | Hastings | Positive |
| 31-Mar-24 | White Lake | GLP | Peterborough | Negative |
| 18-Apr-24 | Stone Road Alvar | GLP | Essex | Negative |
| 19-Apr-24 | Bickford Oak Woods | GLP | Essex | Negative |
| 28-Apr-24 | Devils 4 Mile Rd | Boreal | Peterborough | Negative |
| 03-May-24 | Wollaston Lake | Boreal | Hastings | Negative |
| 03-May-24 | St. Ola | Boreal | Hastings | Negative |
| 06-May24 | Glanmire | Boreal | Hastings | Positive |
| 09-May-24 | N of Lingham Lake | Boreal | Hastings | Negative |
| 19-Jun-24 | Devon Rd. Mesa | Boreal | Thunder Bay | Negative |
| 23-Jul-24 | Hammer Property | GLP | Peterborough | Negative |
| 24-Jul-24 | Quinte Conservation property | GLP | Hastings | Negative |
| 31-Jul-24 | Hammer Property | GLP | Peterborough | Negative |
| 31-Jul-24 | Indian Point Provincial Park | GLP | Kawartha Lakes | Negative |
| 08-Aug-24 | Moira River | GLP | Hastings | Negative |
| 13-Aug-24 | Vanderwater Conservation Area | GLP | Hastings | Positive |
| 21-Sep-24 | Taquanyah Conservation Area | GLP | Haldimand | Negative |
| 26-Sep-24 | Gore Bay | GLP | Manitoulin | Positive |
| 02-Oct-24 | Lavant | Boreal | Lanark | Positive |
| 07-Nov-24 | Mathison Conservation Area | GLP | Peterborough | Negative |
| Quebec | ||||
| 06-Oct-22 | Philipsburg Migratory Bird Sanctuary | GLP | Saint-armand | Positive |
| 06-Oct-22 | Réserve écologique Marcel-Raymond | GLP | Saint-armand | Negative |
a Ecological Areas: GLP (Great Lakes Plain)
| Subpopulation | Year Found | Last Obs. | Total thalli | Total occupied trees | No. of thalli on dead trees | No. of occupied alive trees | No. of occupied dead trees | Substrate(s) | No. of occupied ash trees | No. ind. on ash trees | Status | Ecol. Area |
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Ontario | ||||||||||||
| Algonquin Park | 1900 | 1900 | ? | ? | ? | ? | ? | ? | ? | ? | Excluded | Boreal |
| Brighton | 1891 | 1891 | ? | ? | ? | ? | ? | ? | ? | ? | Extirpated | GLP |
| Darling Long Lake | 2001 | 2001 | 1 | 1 | 1 | 0 | 1 | Sugar Maple | 0 | 0 | ? Extirpated | Boreal |
| Lake Nipigon | 1884 | 1884 | ? | ? | ? | ? | ? | ? | ? | ? | Excluded | Boreal |
| Near Hull, Ontario | 1907 | 1907 | ? | ? | ? | ? | ? | “Large oak” | 0 | ? | Extirpated | GLP |
| Near Wooler | 1893 | 1893 | ? | ? | ? | ? | ? | ? | ? | ? | Extirpated | GLP |
| Ottawa | 1891 | 1891 | ? | ? | ? | ? | ? | “Tree trunks” | ? | ? | Extirpated | GLP |
| Prescott | 1861 | 1861 | ? | ? | ? | ? | ? | ? | ? | ? | Extirpated | GLP |
| Quebec |
||||||||||||
| “Cap-à-l’Aigle” | 1905 | 1905 | ? | ? | ? | ? | ? | “Old log” and birch bark | 0 | 0 | Historical | Boreal |
| Gatineau Park | n.d. | n.d. | ? | ? | ? | ? | ? | “Elm bark” | 0 | 0 | Historical | Boreal |
| Île Bonaventure | 1961 | 1961 | ? | ? | ? | ? | ? | “Dead spruce” | 0 | 0 | Historical | Atlantic |
| Mont Johnson | 1958 | 1958 | ? | ? | ? | ? | ? | Elm | 0 | 0 | Historical | GLP |
| Montmorency Falls | 1905 | 1905 | ? | ? | ? | ? | ? | “Spruce trees” | 0 | 0 | Historical | Boreal |
? Indicates an unknown value.
Abundance
For this assessment, we use the number of host trees as individual equivalents. The main reason for this approach is that arboreal lichens that live on the bark of trees will not survive when the trees die. This brings better consistency with our assessments for the Mosses and Lichens Specialist Subcommittee (M&L SSC) and is also better aligned with published recommendations made to the International Union for Conservation of Nature (IUCN) (Bergamini et al. 2019; Yarh et al. 2024). For transparency and ease of comparison with previous COSEWIC reports as well as the scientific literature, we still report on the number of lichen thalli.
Based on survey data collected between 2012 and 2024, the Canadian population consists of 476 mature thalli distributed among 144 trees at 36 extant subpopulations. Since H. hypoleuca can reproduce by fragmentation, all thalli that were encountered are included in this estimate. Thirty-four extant subpopulations occur in Ontario, one in Quebec, and one in New Brunswick (Table 4). Ontario contains most individuals, with 465 thalli (98%) on 138 trees (96%), followed by Quebec with 10 thalli (2%) on 5 trees (4%), and New Brunswick with one thallus on one tree (<1%).
The distribution of mature individuals among the three occupied Ecological Areas (EA) is as follows: 331 (70%) individuals on 93 (65%) trees representing 20 subpopulations in the Great Lakes Plain EA, 144 (30%) individuals on 50 (35%) trees representing 15 subpopulations in the Boreal EA, and 1 individual representing a single subpopulation (1%) in the Atlantic EA. The distribution of individuals among substrate types is presented in Figure 7 (see Habitat requirements).
Figure 7. Number and type of alive and dead trees occupied by Heterodermia hypoleuca at extant subpopulations in Canada.
Long description
The pie chart shows that of a total of 144 trees, one-quarter (37) of them are dead. The dead trees are primarily ash (15 Green Ash and 16 Black Ash) along with four American Basswood, one Red Oak and one Sugar Maple. Of the 107 living trees, most are ash (45 Green Ash, 23 Black Ash and two unidentified ash species). Next most populous among the living trees are oak (21 Bur Oak and six Red Oak), and the remainder of the living trees are four Sugar maple, three Eastern White Cedar, two American Basswood and one Butternut Hickory.
An estimated subpopulation size was completed for Ontario to account for additional individuals possibly present on inaccessible private land in eight eastern Ontario counties including Ottawa, Hastings, Lanark, Leeds and Grenville, Lennox and Addington, Peterborough, Prince Edward, and Renfrew. It was projected that an additional 580 to 900 mature individuals on 190 to 270 ash trees (refer to Appendix 2 for an explanation of these values) could occur within approximately 250 km2 of unsurveyed suitable habitat identified by examining digital geospatial datasets including forest cover, landownership, and surficial geology. However, mortality rates for these individuals would likely approach 100% within three generations (30 to 90 years) as they are assumed to occur on ash, which is vulnerable to the threat of EAB. When combined with the 2012 to 2024 survey data, the total Canadian population is estimated to be between 1,056 and 1,376 individuals on 334 to 414 host trees.
Fluctuations and trends
There has been no long-term monitoring of H. hypoleuca in Canada. As a result, there are no data to estimate trends over time. However, since much of the original productive, mature forest cover in the Great Lakes Plains region home to almost two thirds of the Canadian population has been lost, it is likely that H. hypoleuca has experienced a decline here. Review of both historical literature (for example, Billings 1860) and supporting vouchered specimens made mostly prior to the 20th century, suggests H. hypoleuca was previously more widespread since it was found in areas where suitable habitat no longer exists. Early records from southern Ontario where it was recorded at Wooler, Brighton, Ottawa, near Hull, and Prescott lack suitable habitat at present, and are considered extirpated (Table 2). Early literature reports from Algonquin Park and Lake Nipigon (Macoun 1902) cannot be verified.
In Ontario, recent documented losses over the last five years of at least 20 thalli at three subpopulations have been observed (12 at Frontenac Provincial Park, 7 at Belmont Lake, and 1 at Darling Long Lake) and another 4 are suspected (Deseronto Rd.). Prior to 2019, there were 15 individuals reported from Frontenac Provincial Park on four trees (Lewis 2019). Two of the four occupied trees were dead and on the ground hosting 12 of the 15 individuals. A targeted search during this status report by SB failed to relocate any individuals on downed ash trees in the same areas. Thus, the 12 individuals on those two trees have presumably been lost. Six thalli on a recently downed ash at Belmont Lake found by SB in 2022 was revisited in 2024, and all thalli were gone and the bark had fallen off the trunk, and another thallus was no longer present on a nearby Bur Oak. A single thallus was found by RL at Darling Long Lake in 2001 on a downed Sugar Maple. It is presumed to have been lost. Four individuals found by CL at the Deseronto Rd. subpopulation occur on private land in a deciduous swamp adjacent to a road. SB viewed this area in 2020 from the ditch and noted all the Green Ash trees in the deciduous swamp were near dead or dead standing due to EAB infestation. The number of individuals at this subpopulation has presumably declined and may be extirpated now because the host trees appeared to no longer provide suitable habitat.
Between 2019 and 2024, 102 thalli were recorded on 38 dead standing or fallen dead host trees (Figure 7). Bark on these tree hosts was in various stages of deterioration but will soon fall off or decompose, and therefore these individuals will be lost. Over the next five years, there will be an estimated 21% decline in number of mature individuals (unit of count is the total number of observed thalli). This increases to a 35% decline when considering the number of occupied trees that will be lost.
The status of the five historical subpopulations in Quebec is unknown, but their scattered distribution suggests a previously more widespread distribution there. At least two historical collections were made from elm, and it is likely these are no longer extant, as mature elms have been decimated range-wide by Dutch Elm Disease (see Threats and limiting factors).
A total of 253 individuals were recorded on living ash trees between 2019 and 2024, and all of these will presumably die as ash trees succumb to Emerald Ash Borer, which is a threat throughout the entire Canadian range of H. hypoleuca (CFIA 2021). Currently, EAB has been found already at 15 extant subpopulations and is projected to impact an additional 16 over the next three generations (30 to 90 years). When accounting for losses of all individuals on ash trees and on dead trees, the Canadian population is projected to decline by 78% over the next three generations. The decline is 74% if relying on the number of occupied host trees that will be lost (due to EAB or other causes).
Rescue effect
Recruitment via long-distance transport of ascospores from sites outside Canada is conceivable, though given the distances involved, it is impossible to determine how likely this is. The nearest extant site to the Canadian border is in north-central Minnesota (Thayer and Henderson pers. comm. 2019). This site is several 100 kilometres south of the Rainy River District of Ontario, where no records of H. hypoleuca exist. While potentially suitable habitat exists based on recent surveys, targeted searches have not been successful in this region (refer to Table 1 and Figure 4 for a summary of search effort).
The nearest extant site to the Canadian population lies over 600 km to the south in central Ohio (Curtis pers. comm. 2022). Other records from adjacent U.S. jurisdictions found in CLH (2023) are historical (>20 years) and their status is unknown. Given the distances involved and the lack of recent collections in most adjacent states, rescue from these populations seems unlikely.
Threats and limiting factors
Historical, long-term, and continuing habitat trends
The extent and quality of productive mature forest stands in Eastern North America, and particularly their unique interior microclimates constituting the range of H. hypoleuca in Canada, has undoubtedly diminished significantly since European settlement, which has resulted in the loss of a large portion of suitable habitat (see Habitat trends). Early accounts of lichens in southern Ontario including those of Billings (1860) and Macoun (1902) indicate numerous pollution-sensitive and disturbance-sensitive taxa such as Anzia colpodes, Lobarina scrobiculata, Nephroma resupinatum, and Usnea angulata were present in southern Ontario in the 19th or early 20th centuries. However, later-twentieth-century studies (for example, Brodo 1981; Wong and Brodo 1992) and extensive lichen surveys carried out since then by numerous lichenologists in the same region, have failed to document any individuals of these species, a trend that has been observed elsewhere in the northeast (Allen et al. 2019).
Current and projected future threats
The overall threat impact based on the Threats Calculator assessment for H. hypoleuca is Very high – High (Appendix 3). The overall threat impact is calculated by considering the separate impacts of all threat categories. The various threats, in order of importance, include natural system modifications, climate change and severe weather, biological resource use, and transportation and service corridors. Each threat is discussed below.
Natural system modifications (IUCN threat 7.3 other ecosystem modifications); overall threat impact: very high – high
Emerald Ash Borer (EAB) is a wood-boring beetle native to East Asia that is dramatically altering temperate forests in North America where ashes are an important forest canopy component. For most ash species, infestation by EAB causes over 90% mortality of trees with a diameter greater than 2.5 cm (at breast height) within a few years (Klooster et al. 2014). EAB was first detected in southwestern Ontario in 1992 and has since spread to Canadian sites up to 1,100 km northwest and 1,300 km northeast (COSEWIC 2018). EAB larvae feed on the inner bark and sapwood, eventually girdling and killing trees (Herms and McCullough 2014). Mortality of mature ash trees (all species) reached 99% within six years in parts of Michigan and Ohio (Klooster et al. 2014), and similar rates of ash mortality has been noted in affected areas of southern Ontario (COSEWIC 2018). Widespread ash tree mortality caused by EAB is the most serious threat currently facing H. hypoleuca in Canada (Figure 8). Heterodermia hypoleuca is completely dependent on its host trees for its continued survival. As ash trees succumb, the availability of mature, ash-dominated swamp forest habitat in southern Ontario will decline as is expected in other Northeastern regions (Youngquist et al. 2017; Palik et al. 2021).
Figure 8. Photographs depicting mature Green Ash mortality in Heterodermia hypoleuca habitat caused by Emerald Ash Borer (EAB) in Ontario. A) Large diameter, dead-standing Green Ash tree with most of its bark descaled after EAB infestation. B) Closeup of Heterodermia hypoleuca on tree infected with EAB with portion of thallus lost from descaling bark. C) Looking upwards at a Green Ash infected with EAB with approximately 50% of bark descaled (photos S. Brinker).
In Canada, ash trees are the most important host substrate (Table 3 and Figure 7). EAB already occurs at a minimum of 15 of the 31 subpopulations with ash as a host substrate. While EAB was not detected at all sites, the entire Canadian range of H. hypoleuca is within EAB regulated areas where it is well established and spreading (CFIA 2021). This means that over the next three generations (30 to 90 years), it is projected that all occupied ash trees will likely succumb to EAB. This will result in a loss of 74% of the Canadian population (351 thalli or 107 host trees).
| Host tree species | Total mature thalli | Percent of Canadian population | Total occupied trees | Percent of Canadian population |
|---|---|---|---|---|
| Green Ash (Fraxinus pennsylvanica) | 227 | 48% | 60 | 42% |
| Black Ash (Fraxinus nigra) | 122 | 26% | 39 | 27% |
| Bur Oak (Quercus macrocarpa) | 76 | 16% | 22 | 15% |
| Red Oak (Quercus rubra) | 23 | 5% | 6 | 4% |
| American Basswood (Tilia americana) | 12 | 3% | 6 | 4% |
| Sugar Maple (Acer saccharum) | 10 | 2% | 5 | 3% |
| Eastern White Cedar (Thuja occidentalis) | 3 | 1% | 3 | 2% |
| Ash sp. (Fraxinus sp.) | 2 | <1% | 2 | 1% |
| Bitternut Hickory (Carya cordiformis) | 1 | <1% | 1 | 1% |
| Subpopulation | Year Found | Last Obs. | Total thalli | Total occupied trees | No. of thalli on dead trees | No. of occupied alive trees | No. of occupied dead trees | Substratea | No. of occupied ash trees | No. ind. on ash trees | EABb present | Status | Ecol. area |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Ontario | |||||||||||||
| Beaver Creek A | 2021 | 2021 | 18 | 6 | 0 | 6 | 0 | FP, QM | 5 | 17 | No | Extant | Boreal |
| Beaver Creek B | 2021 | 2021 | 12 | 1 | 0 | 1 | 0 | FP | 1 | 12 | No | Extant | Boreal |
| Beckwith | 2023 | 2023 | ~ 40 | ~ 10 | ~ 4 | ~ 8 | ~ 2 | FN, TO | ~ 9 | ~ 39 | No | Extant | GLP |
| Belmont Lake | 2020 | 2022 | 19 | 12 | 3 | 10 | 2 | AS, FP, QM, TO | 2 | 3 | Yes | Extant | GLP |
| Block 509 | 2023 | 2023 | 1 | 1 | 0 | 1 | 0 | FN | 1 | 1 | No | Extant | Boreal |
| Bolingbroke Rd. | 2023 | 2023 | 1 | 1 | 0 | 1 | 0 | FN | 1 | 1 | ? | Extant | Boreal |
| Cassidy Block | 2012 | 2022 | 6 | 2 | 0 | 2 | 0 | FP | 2 | 6 | No | Extant | GLP |
| Charleston Lake PP | 2023 | 2023 | 2 | 2 | 2 | 0 | 2 | FP | 2 | 2 | No | Extant | Boreal |
| Constant Creek CR | 2023 | 2023 | 53 | 16 | 39 | 4 | 12 | FN | 16 | 53 | Yes | Extant | Boreal |
| County Forest East | 2022 | 2022 | 5 | 1 | 5 | 0 | 1 | FP | 1 | 5 | Yes | Extant | GLP |
| Crow Lake | 2023 | 2023 | 2 | 2 | 1 | 1 | 1 | FN | 2 | 2 | No | Extant | Boreal |
| Crowe River | 2017 | 2022 | 28 | 10 | 10 | 6 | 4 | FP | 10 | 28 | No | Extant | GLP |
| Deseronto Rd. | 2014 | 2014 | 1? | 1? | ? | ? | ? | FP | 1? | 1? | Yes | ?Extant | GLP |
| Frontenac PP | 2016 | 2021 | ~ 3 | ~ 2 | 0 | ~ 2 | 0 | AS, FN | 1 | 1 | Yes | Extant | Boreal |
| Glanmire | 2024 | 2024 | 1 | 1 | 0 | 1 | 0 | FP | 1 | 1 | N | Extant | Boreal |
| H.R. Frink CA | 2022 | 2022 | 4 | 2 | 0 | 2 | 0 | FP | 2 | 4 | Yes | Extant | GLP |
| Kip Fleming Tract | 2024 | 2024 | 1 | 1 | 0 | 1 | 0 | QM | 0 | 0 | N | Extant | GLP |
| Massassauga Point | 2022 | 2022 | 18 | 1 | 0 | 1 | 0 | QM | 0 | 0 | N/A | Extant | GLP |
| Moira River | 2023 | 2023 | 5 | 4 | 0 | 4 | 0 | FN, FP | 4 | 0 | Yes | Extant | GLP |
| Mosque Lake Rd. | 2024 | 2024 | 1 | 1 | 0 | 1 | 0 | FN | 1 | 1 | ? | Extant | Boreal |
| Murphy’s Point PP | 2023 | 2023 | 27 | 5 | 0 | 5 | 0 | FP, FN | 5 | 27 | Yes | Extant | Boreal |
| Oatbox | 2011 | 2022 | 14 | 5 | 1 | 4 | 1 | FP | 5 | 14 | Yes | Extant | GLP |
| OR Agreement Forest | 2022 | 2022 | 2 | 1 | 2 | 0 | 1 | FP | 1 | 2 | Yes | Extant | GLP |
| Ottawa River | 2016 | 2023 | 29 | 6 | 0 | 6 | 0 | QM, FP | 2 | 18 | No | Extant | GLP |
| Lavant | 2024 | 2024 | 8 | 4 | 2 | 3 | 1 | FN | 4 | 8 | N | Extant | Boreal |
| Rawdon Block | 2023 | 2023 | 18 | 5 | 3 | 4 | 1 | FP | 5 | 18 | Yes | Extant | GLP |
| S of Marmora | 2012 | 2012 | ~ 1 | ~ 1 | ? | ~ 1 | 0 | ash sp. | ~ 1 | ~ 1 | ? | ?Extant | GLP |
| S. of Quackenbush | 2012 | 2012 | ~ 1 | ~ 1 | ? | ~ 1 | 0 | ash sp. | ~ 1 | ~ 1 | ? | ?Extant | GLP |
| Sharbot Lake PP | 2022 | 2022 | 2 | 1 | 2 | 0 | 1 | FN | 1 | 2 | Yes | Extant | Boreal |
| Shaw Woods | 2023 | 2023 | 1 | 1 | 0 | 1 | 0 | TO | 0 | 0 | N/A | Extant | Boreal |
| Silver Lake PP | 2022 | 2023 | 12 | 6 | 10 | 2 | 4 | TA | 0 | 0 | N/A | Extant | Boreal |
| Squirrel Creek | 2022 | 2022 | 4 | 2 | 3 | 1 | 1 | FP | 2 | 4 | Yes | Extant | GLP |
| Vanderwater CA | 2024 | 2024 | 3 | 1 | 0 | 1 | 0 | FP | 1 | 3 | Yes | Extant | GLP |
| Westmeath PP | 2015 | 2023 | 122 | 22 | 13 | 19 | 3 | FP, QM, QR | 10 | 70 | No | Extant | GLP |
| Quebec | |||||||||||||
| Philipsburg | 2016 | 2022 | 10 | 5 | 2 | 4 | 1 | AS, QM, CC | 0 | 0 | N/A | Extant | GLP |
| New Brunswick | |||||||||||||
| Saint John River | 2022 | 2022 | 1 | 1 | 0 | 1 | 0 | FP | 1 | 1 | Yes | Extant | Atlantic |
a Substrate codes: AS = Acer saccharum; CC = Carya cordiformis; FN = Fraxinus nigra; FP = Fraxinus pennsylvanica; QM = Quercus macrocarpa; QR = Quercus rubra; TA = Tilia americana; TO = Thuja occidentalis. – Dashes indicated missing information which is often the case for older collections and observations.
b EAB = Emerald Ash Borer (Agrilus planipennis) observed in occupied habitat.
? Indicates an unknown value or a degree of uncertainty about status and should be a priority for future assessments.
~ Indicates an estimate derived from the interpretation of available information (rather than an explicit count).
Two historical H. hypoleuca records were collected on elm bark in Quebec. Dutch Elm Disease (DED) impacting native elms (Ulmus spp.) in North America was first detected in the U.S. in the 1930s and rapidly caused widespread and devastating losses to mature elm trees. Its detection in Canada soon followed, first in 1944 in Quebec, and then in Ontario by 1948 (Reed 1950). Its impact was swift as its rate of spread was over 1,900 km a year (Pomerleau 1961). The drastic loss of mature elm trees across the range of H. hypoleuca in Canada has likely resulted in the loss of subpopulations occurring on elm trees, as well as a suitable host substrate. Dutch Elm Disease’s continued impact on elms is apparent since the last recorded thallus from elm bark was from sometime between the late 1960s and early 1970s. At present, while emerging elm seedlings or root suckers from infected trees can reach sexual maturity, trees no longer attain suitably large trunk diameters and bark characteristics prior to the onset of DED attacks (Brasier 1986, 1996), which likely accounts for the absence of recent observations of H. hypoleuca on elm bark.
Climate change and severe weather (IUCN threats 11.4 storms and flooding); overall threat impact: high – low
The full impacts to lichens resulting from anthropogenic climate change are still unclear, partially due to a lack of sufficient study. While a growing body of research suggests that the consequences of climate change could be severe for lichens (Allen and Lendemer 2016; Ellis 2013, 2015), more studies are needed to properly characterize the threat level. In a study of threats to at-risk species in Canada, lichens as a group were found to be the most highly affected taxon of the 12 taxonomic groups assessed (Woo-Durand et al. 2020).
In Canada, nine of the 10 warmest years have occurred during the last 25 years, with 2010 being the warmest on record (3.0°C above the 1961 to 1990 reference value) (ECCC 2023). The effects of widespread warming are evident in many parts of Canada and are projected to intensify in the future. In southern Ontario and Quebec, warmer temperatures are predicted to give drier conditions, especially during the summer months, leading to lower water levels in the Great Lakes region (Feltmate and Thistlethwaite 2013). Projected changes to mean annual temperature would lead to net warming and drying, likely reducing available moisture and humidity, important habitat characteristics for H. hypoleuca (see Habitat). Alteration of hydrological regimes (that is, changes in the amount of precipitation, increased frequency of drought) may also impact the distribution and abundance of suitable host trees in most H. hypoleuca habitat. In a climate change vulnerability assessment of species in the Ontario Great Lakes Basin, Black Ash was found to be moderately vulnerable to climate change in part due to its physiological hydrological niche (its degree of dependence on specific swamp/vernal pool wetland habitat) that is modelled to experience net drying with increasing temperatures (Brinker et al. 2018).
Radical shifts in regional climate envelopes (areas with similar climate regimes) are expected and have been predicted for Ontario based on climate modelling completed by McKenney et al. (2010). Under these scenarios, species with narrow habitat requirements and limited dispersal success, such as H. hypoleuca, may be more vulnerable than habitat generalists, or those with more effective dispersal abilities.
An increase in the frequency and severity in weather events, including blow-down of host trees or physical damage from ice storm activity, is expected with a warming climate (ECCC 2017). A derecho (a widespread, long-lived windstorm associated with a band of rapidly moving showers or thunderstorms) event that occurred in May of 2022 and a tornado later in July along nearly the same path across eastern Ontario (Figure 9) caused widespread and severe damage to the fragmented forest cover in the region, affecting both suitable unsurveyed habitat (Figure 10) and occupied habitat. Recently downed mature trees with H. hypoleuca, which were observed at six subpopulations (totalling at least 22 thalli), were likely—based on the condition of individuals and trees with leaves still attached—toppled during these storm events.
Figure 9. Path of the May 2022 Ontario-Quebec derecho causing extensive damage to forest cover leading to loss of mature trees hosting Heterodermia hypoleuca (modified from Northern Tornadoes Project 2023). The yellow area indicates the general continuous path of the derecho roughly 1,000 km in length, and 100 km in width. The blue areas indicate intensified areas of severe damage. White circles represent extant H. hypoleuca subpopulations.
Long description
The map shows the region from Detroit in the southwest to Quebec City. The path of the derecho begins to the southwest of Detroit and flows in an east-northeast direction, expanding in width along its path. The intensified areas with severe damage occur in the Sarnia region and then from London to Hamilton and Toronto, along the northwestern shore of Lake Ontario, through Ottawa and Trois-Rivières and as far east as Quebec City. Another intensified area occurs in northern Vermont, New Hampshire and Maine with a sliver of the area lying in southern Quebec. Locations within the derecho path but outside of the intensified areas include the northern shores of Lakes Ontario and Erie, the farthest southern shore of Lake Huron and the cities and surrounding regions of Barrie, Kingston, Brockville and Montreal. The extant subpopulations of Cupped Fringed Lichen, Heterodermia hypoleuca, are in and around Kingston, to the northwest of Kingston, to the northwest of Brockville and to the west and northwest of Ottawa. Most of these sites are in the intensified area and most others are in the main path of the derecho. Three subpopulations are outside the derecho flow on the Ontario-Quebec border northwest of Ottawa and one is on the northern shore of Lake Huron. Last, one subpopulation is on the edge of the intensified area along the Quebec-Vermont border.
Figure 10. Severe damage to swamp forest caused by 2022 derecho event (corresponding to area of blue in Figure 9) in eastern Ontario (photo S. Brinker).
Biological resource use (IUCN threats 5.3 logging and wood harvesting, and 5.2 gathering terrestrial plants); overall threat impact: medium – low
Lichens are directly impacted by timber harvesting because logging means that individuals are removed from the forest together with their substratum. While Eastern White Cedar, Green Ash, Red Oak, and Sugar Maple are merchantable timber, other host trees, namely Black Ash and Bur Oak, are not often target species in forestry operations. Species of ash are generally regarded as high-quality firewood (Alden 1994) and may be targeted for harvest in private woodlots throughout the species’ range. At least seven extant subpopulations occur on private land not managed for conservation, though this threat extends to eight on conservation authority-owned land, two municipally owned subpopulations and eight subpopulations on unprotected Crown land, where commercial timber harvesting, or salvage operations may occur. Individuals in these subpopulations make up about 39% of the total Canadian population and could be impacted during logging or salvage activities.
Ash mortality due to Emerald Ash Borer has increased the selective logging of ash trees. In several Northeast U.S. jurisdictions, foresters and loggers have responded to EAB infestations by increasing harvests of ash trees including small-diameter and low-grade trees to promote regeneration of other more merchantable timber (Markowski-Lindsay et al. 2023). While no data are available from Canada, SB has observed increases in selective ash harvesting in forests of southern Ontario where EAB infestations exist.
The removal of hazard trees from managed areas including provincial parks, particularly trees adjacent to roads, day-use areas, trails or campsites, may result in the removal of occupied trees. At Silver Lake Provincial Park, two downed basswood trees were observed around campsites with felled portions of the trunks left on the ground, hosting several H. hypoleuca thalli. Similarly, municipalities may prioritize removal of ash trees from public lands before they became hazardous.
Increased visitation and incidences of collecting thalli could result in mortality because rare and at-risk species tend to spike public interest. Increased collecting pressure or inadvertent damage to individuals from general lichen collecting could come with increased awareness of this rare species, a phenomenon observed elsewhere for listed plant species (for example, Sutter 1987). However, this threat is difficult to document and likely negligible.
Transportation and service corridors (IUCN threat 4.1 roads and railroads); overall threat impact: low
Road construction associated with forestry activities can damage H. hypoleuca habitat if routed through or too close to areas of occupancy. Routing logging roads too close to swamp forest habitat or vernal ponds can alter their hydrological processes, reduce local humidity levels, and decrease host tree availability, if removal of trees along the edge of habitat occurs. In Ontario, if sites are identified on Crown land, protection can be provided via a 30 m buffer to woodland pools through Ontario’s Forest Management Guide for Conserving Biodiversity at the Stand and Site Scales (OMNR 2010). This relies on the correct delineation of pools, which can be misinterpreted if conducted outside the appropriate season, and assumes that staff are trained to identify H. hypoleuca; it would not apply to private land.
Several threats were considered unknown including: the effect of airborne pollutants, climate change resulting in habitat shifts, and alteration and droughts. Details are provided in the Threats Calculator.
Limiting factors
Mode of reproduction and dispersal, as well as the availability of suitable host substrates for lichen colonization, are key limiting factors that have been found to impact lichen rarity. In the predominantly managed landscape where H. hypoleuca occurs, long distances between habitat patches and a limited dispersal range may limit colonization of potentially suitable habitat. Apothecia were absent from thalli at 12 of the 36 extant subpopulations (Appendix 1). Lichens that reproduce sexually, dispersing only the mycobiont, and that are restricted to trees as a substrate are overrepresented among rare species in temperate eastern North American forests (Manzitto-Tripp et al. 2022). Heterodermia hypoleuca joins a growing list of declining macrolichens of temperate northeastern North American mature broad-leaved forests, reproducing primarily via ascospores produced in apothecia that are restricted to growing on tree trunks. Other examples include Anzia colpodes and Myelochroa galbina (COSEWIC 2015; Tripp and Lendemer 2020).
Number of locations
Six locations based on the most plausible threat are identified for H. hypoleuca in Canada. All 36 extant subpopulations fall within the Canadian Food Inspection Agency’s Regulated Zone for Emerald Ash Borer (CFIA 2021), though not all individuals occur on ash. Thalli at 31 subpopulations occur on ash trees and are considered a single location. At these sites, individuals are either already being impacted by EAB or are at a very high risk of being impacted within the next decade (one generation, 10 to 30 years), based on natural expansion rates of 20 km per year (Prasad et al. 2010) or potentially much greater rates owing to human-assisted expansions (such as deliberately moving ash wood) (DeSantis et al. 2013). The impact of climate change on H. hypoleuca is uncertain, but could become a more serious threat in the next three generations (30 to 90 years) and would likely affect each subpopulation separately. The remaining five subpopulations are treated as separate locations.
Protection, status, and ranks
Legal protection and status
There is currently no legal status or protection for H. hypoleuca. It is not covered under the Convention on International Trade in Endangered Species (CITES) or the United States’ Endangered Species Act.
Non-legal status and ranks
Global status
Heterodermia hypoleuca has been assigned a global rank of G5 (Secure), although this rank was last reviewed in 1992 (NatureServe 2023) and should be re-evaluated. It has not been assessed by the International Union for the Conservation of Nature (IUCN).
Status in Canada
In Canada, H. hypoleuca is ranked N3 (Vulnerable), but will likely change to N2 due to a revision in Quebec (Tremblay pers. comm. April 2025). In Ontario, it has a subnational rank of S2 (Imperiled). In Quebec, it is currently ranked S3 (Vulnerable) (NatureServe 2023), although this status may overestimate its security since there is only one extant subpopulation. It is being revised to S1S2 (Tremblay pers. comm. April 2025). Its status has not yet been assessed in New Brunswick.
Status in the U.S.
In the United States, H. hypoleuca has a national rank of NNR (unranked), and it has a rank of S5 (secure) in Kentucky and SNR in Georgia, North Carolina, Pennsylvania, and Wisconsin (NatureServe 2023). Other states where it occurs do not currently assign a rank to the species.
Habitat protection and ownership
In Ontario, 11 extant subpopulations occur in protected areas (Appendix 1). Of these, 8 fall within regulated provincial parks and conservation reserves and 3 are within lands owned and managed for conservation purposes by the Nature Conservancy of Canada. Two occur on private lands managed for conservation. Another 18 occur on lands owned and managed by conservation authorities, municipalities or on Crown land, where logging operations may still occur, and it is uncertain whether some of these are managed for biodiversity conservation. At least 6 subpopulations occur entirely on privately owned land not managed for conservation purposes.
In Quebec, the only extant subpopulation occurs on private land managed for conservation purposes (a migratory bird sanctuary). The remaining historical records do not provide sufficient spatial information to determine land ownership. However, a specimen labelled “Gatineau Park” might correspond with federal lands now managed by the National Capital Commission, and a specimen collected from Île Bonaventure may correspond with lands currently owned by Sépac (Société des établissements de plein air du Québec), which manages parks and wildlife reserves.
Land tenure of the newly discovered subpopulation in New Brunswick is under private ownership.
Acknowledgements
Assistance with documenting the presence and distribution of H. hypoleuca in Canada has been provided by many colleagues. The following are graciously thanked for their generous assistance with fieldwork: Graham Cameron, Cassandra Robillard, Christine Terwissen, and Alison Smith with the Ontario Ministry of Natural Resources and Forestry; Colin Chapman-Lam, consulting lichenologist and botanist based in Ottawa, Canada; Josh Van Wieren and Mary Beth Lynch with Parks Canada; and Tim Trustham and Robert Ormston with Quinte Conservation. Jon Ruddy is thanked for sharing his recent discoveries of H. hypoleuca in eastern Ontario.
The Ontario Ministry of Natural Resources and Forestry provided in-kind support for the Ontario fieldwork component. Arold Lavoie provided insight on the status of the species in Quebec. Stephen Clayden provided valuable information on his recent discovery of the species in New Brunswick. Tomas Curtis provided helpful insight on the status and habitat in Ohio. John Thayer, Otto Gockman and Bobby Henderson provided helpful insight on the status and habitat in Minnesota. Chris Lewis, Chris Deduke, Troy McMullin, Gregory Rand, Gina Schalk, Marie Archambault, Jenna Siu, Mary Sabine, Leah de Forest, and Richard Caners kindly provided useful comments on a previous draft. Thanks to Dwayne Lepitzki for facilitating the threats call and to Jennifer Doubt, Chris Deduke, Toby Spribille, Marc Favreau, Cassandra Robillard, Tegan Padget, and Julie McKnight for participating in it.
Authorities contacted
- Frances Anderson, Lichenologist, Nova Scotia Museum, Nova Scotia
- Dr. Stephen Clayden, Curator (retired), New Brunswick Museum (NMB), New Brunswick
- Dr. Chris Deduke, Canadian Museum of Nature (CANL), Gatineau, Quebec
- Dr. Ted Esslinger, Professor Emeritus, North Dakota State University, North Dakota
- Bobby Henderson, Botanist, U.S. Forest Service, Minnesota
- Dr. Robert Klips, Associate Professor Emeritus, Ohio State University, Ohio
- Jacques Labrecque, Botanist (retired), Ministère de l'Environnement, de la Lutte contre les changements climatiques, Quebec
- Arold Lavoie, Independent Lichenologist, Quebec
- Rob Lee, Independent Lichenologist, Ontario
- Chris Lewis, Species at Risk Biologist, Government of British Columbia
- Dr. Troy McMullin, Lichenologist, Canadian Museum of Nature
- Dr. James Lendemer, Lichenologist and Curator of Botany, New York State Museum
- Dr. Michele Piercey-Normore, Special Advisor to the President, Algoma University, Thunder Bay
- Mr. Jon Ruddy, Research Associate, Canadian Museum of Nature
Information sources
Ahti, T. 1964. Macrolichens and their zonal distribution in boreal and arctic Ontario, Canada. Annales Botanici Fennici 1: 1-35.
Alden, H.A. 1994. Wood Technology Transfer Fact Sheet: Fraxinus spp. Centre for Wood Anatomy Research. United States Department of Agriculture, Forest Service, Forest Products Laboratory, Madison, Wisconsin. 3 pp.
Allen, J.L. and J.C. Lendemer. 2016. Climate change impacts on endemic, high-elevation lichens in a biodiversity hotspot. Biodiversity Conservation 25: 555-568.
Allen, J.L., R.T. McMullin, E.A. Tripp and J.C. Lendemer. 2019. Lichen conservation in North America: a review of current practices and research in Canada and the United States. Biodiversity and Conservation 28: 3103-3148.
Barclay-Estrup, P. and R.A. Sims. 1979. Epiphytes on White Elm Ulmus americana, near Thunder Bay, Ontario. Canadian Field-Naturalist 93: 139-143.
Bates, J.W., P. J. McNee and A.R. McLeod. 1996. Effects of sulphur dioxide and ozone on lichen colonization of conifers in the Liphook Forest Fumigation Project. New Phytologist 132: 653-660.
Bergamini, A., I. Bisang, N. Hodgetts, N. Lockhart, J. van Rooy, and T. Hallingbäck.
2019. Recommendations for the use of critical terms when applying IUCN red-listing criteria to bryophytes. Lindbergia 2019:1-6.
Billings, W.E. 1860. List of plants found growing as indigenous in the neighbourhood of Prescott, C.W. The Canadian Naturalist and Geologist. 5: 14-24.
Boch, S., D. Prati, D. Hessenmöller, E-D. Schulze, and M. Fischer. 2013. Richness of lichen species, especially of threatened ones, is promoted by management methods furthering stand continuity. PLoS One 8. doi:10.1371/journal.pone.0055461.
Bouchard, A., S. Dyrda, Y. Bergeron and A. Meilleur. 1989. The use of notary deeds to estimate the changes in the composition of 19th century forests in Haut-Saint-Laurent, Québec. Canadian Journal of Forest Research 19: 1146-1150.
Brasier C.M. 1986. The population biology of Dutch elm disease: its principal features and some implications for other host-pathogen systems. Pp. 55-118 in: D.S. Ingram and P.H. Williams (eds). Advances in Plant Pathology Vol 5. Academic Press, London/New York.
Brinker, S. 2020. Contributions to the Ontario flora of lichens and allied fungi, with emphasis on the Great Lakes Basin. Opuscula Philolichenum 19: 58-157.
Brinker, S.R., M. Garvey, and C.D. Jones. 2018. Climate change vulnerability assessment of species in the Ontario Great Lakes Basin. Ontario Ministry of Natural Resources and Forestry, Science and Research Branch, Peterborough, ON. Climate Change Research Report CCRR-48. 85 p. + appendices.
Brodo, I.M. 1981. Lichens of the Ottawa Region. Syllogeus 29, National Museum of Natural Sciences, Ottawa, Ontario. 137 pp.
Brodo, I.M. 1988. Lichens of the Ottawa Region. Second Edition. Ottawa Field-Naturalists’ Club, Ottawa, Ontario, Canada.
Brodo, I.M., S.D. Sharnoff, and S. Sharnoff. 2001. Lichens of North America. Yale University Press, New Haven, CT. 795 pp.
Brodo, I.M., R.C. Harris, W. Buck, J.C. Lendemer, and C.J. Lewis. 2013. The Lichens of Bruce Peninsula, Ontario: Results from the 17th Tuckerman Workshop, 18-22 Sept. 2008. Opuscula Philolichenum 12: 198-232.
Brodo, I.M., R.E. Lee, C. Freebury, P.Y. Wong, C.J. Lewis, and R.T. McMullin. 2021. Additions to the lichens, allied fungi, and lichenicolous fungi of the Ottawa region in Ontario and Québec, with reflections on a changing biota. Canadian Field-Naturalist 135: 1-27.
CCME. 2008. A national picture of acid deposition critical loads for forest soils in Canada. Canadian Council of Ministers of the Environment.
CCME. 2013. Progress report on the Canada-wide acid rain strategy for post 2000. Canadian Council of Ministers of the Environment.
CESCC (Canadian Endangered Species Conservation Council). 2011. Wild Species 2010: The General Status of Species in Canada. National General Status Working Group: 302 pp.
CFIA (Canadian Food Inspection Agency). 2021. Areas regulated for the emerald ash borer.
Clayden, S. 2023. Personal Communication to Sam Brinker.
Clayden, S. 2024. Personal communication to André Arsenault by email August 8, 2024.
Consortium of Lichen Herbaria (CLH). 2022. https://lichenportal.org/clh/index.php. (Accessed May–December 2022).
COSEWIC. 2015. COSEWIC assessment and status report on the Black-foam Lichen Anzia colpodes in Canada. Committee on the Status of Endangered Wildlife in Canada. X + 47 pp.
COSEWIC. 2018. COSEWIC assessment and status report on the Black Ash Fraxinus nigra in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. xii + 95 pp.
COSEWIC 2019. COSEWIC assessment and status report on the White-rimmed Shingle Lichen Fuscopannaria leucosticta in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. xi + 85 pp.
Crowe, J. 1994. The lichens of Thunder Bay District, Ontario. Evansia 11: 62-75.
Curtis, Tomas. 2022. pers. comm. to Sam Brinker
DeSantis, R.D., W.K. Moser, D.D. Gormanson, M.G. Bartlett, and B. Vermunt. 2013. Effects of climate on emerald ash borer mortality and the potential for ash survival in North America. Agricultural and Forest Meteorology. 178: 120-128.
Diederich, P. 2007. Sphaerellothecium gallowayi sp. nov., a new lichenicolous ascomycete on Heterodermia from Australia and Papua New Guinea. Bibliotheca Lichenologica 95: 165-169.
ECCC (Environment and Climate Change Canada). 2023. Canadian Environmental Sustainability Indicators: Temperature change in Canada.
Ellis, C.J. 2013. A risk-based model of climate change threat: hazard, exposure, and vulnerability in the ecology of lichen epiphytes. Botany 91: 1-11.
Ellis, C.J. 2015. Ancient woodland indicators signal the climate change risk for dispersal-limited species. Ecological Indicators 53: 106-114.
Enkhtuya, O. and S. Javkhlan. 2019. Three species of Heterodermia recorded in Mongolia. Proceedings of the Mongolian Academy of Sciences 59: 57-64.
Esslinger, T.L. 2021. A cumulative checklist for the lichen-forming, lichenicolous and allied fungi of the Continental United States and Canada, version 24. Opuscula Philolichenum 20: 100-394.
Farmer, A.M., J.W. Bates and J.N.B. Bell. 1991. Comparisons of three woodland sites in NW Britain differing in richness of the epiphytic Lobarion pulmonariae community and levels of wet acidic deposition. Holarctic Ecography 14: 85-91.
Fedrowitz, K., M. Kuusinen, and T. Snäll. 2012. Metapopulation dynamics and future persistence of epiphytic cyanolichens in a European boreal forest ecosystem. Journal of Applied Ecology 49:493-502.
Feltmate, B., and J. Thistlethwaite. 2013. Climate Change Adaptation: A Priorities Action Plan for Canada. University of Waterloo. 122 pp.
Fernanda de Souza, M., A. Aptroot and A. Spielmann. 2022. Key to Heterodermia (Physciaceae, Teloschistales) in Brazil, with 15 new species. Lichenologist 54: 25-44.
Ferry, B.W., M.S. Baddeley, and D.L.H. Hawksworth. 1973. Air Pollution and Lichens. University of Toronto Press, 389 pp.
Freebury, C.E. 2011. The lichens of Gatineau Park, Québec. Unpublished report by the author. 68 pp.
Fuller, J.L., D.R. Foster, J.S. McLachlan and N. Drake. 1998. Impact of human activity on regional forest composition and dynamics in central New England. Ecosystems 1: 76-95.
Godfrey, D. 1977. Notes on Hepaticae collected by John Macoun in southwestern British Columbia. Canadian Journal of Botany 10: 2600-2604.
Gustafsson L. and I. Eriksson. 1995. Factors of importance for the epiphytic vegetation of aspen Populus tremula with special emphasis on bark chemistry and soil chemistry. Journal of Applied Ecology 32: 412-424.
Hagan, J.M. and A.A. Whitman. 2004. Late-successional forest: a disappearing age class and implications for biodiversity. Forest Mosaic Science Notes 2004-2: 1-4.
Hale, M.E. Jr. 1955. Phytosociology of corticolous cryptograms in the upland forests of southern Wisconsin. Ecology 36: 45-63.
Hauck, M. 2011. Site factors controlling epiphytic lichen abundance in northern coniferous forests. Flora - Morphology, Distribution, Functional Ecology of Plants 206: 81-90.
Hawksworth, D.L. and F. Rose. 1970. Qualitative scale for estimating sulphur dioxide air pollution in England and Wales using epiphytic lichens. Nature 227: 145-148.
Hawksworth, D.L. and F. Rose. 1976. Lichens as pollution monitors. Institution of Biology, Studies in Biology,. 66. E. Arnold, London.
Hedenås, H. and L. Ericson. 2008. Species occurrences at stand level cannot be understood without considering the landscape context: Cyanolichens on aspen in boreal Sweden. Biological Conservation 141: 710-718.
Hedrick, J. and J.L. Lowe. 1936. Lichens of Isle Royale, Lake Superior. Bryologist 39: 73-91.
Herms, D.A. and D.G. McCullough. 2014. Emerald Ash Borer invasion of North America: History, biology, ecology, impacts and management. Annual Review of Entomology 59: 13-30.
Hinds, J.W. and P.L. Hinds. 2007. The Macrolichens of New England. Memoirs of the New York Botanical Garden 96: 1-584.
Howe N.M. and J.C. Lendemer. 2011. The recovery of a simplified lichen community near the Palmerton Zinc Smelter after 34 years. Bibliotheca Lichenologica 106: 127-142.
IUCN. 2012. IUCN Red List categories and criteria, version 3.1, second edition. Gland and Cambridge (UK): IUCN Species Survival Commission. 32 pp.
Klooster, W.S., D.A. Herms, K.S. Knight, C.P. Herms, D.G. McCullough, A. Smith, K.J.K. Gandhi and J. Cardina. 2014. Ash (Fraxinus spp.) mortality, regeneration, and seed bank dynamics in mixed hardwood forests following invasion by emerald ash borer (Agrilus planipennis). Biological Invasions 16: 859-873.
Laflamme, J., A.D. Munson, P. Grondin and D. Arseneault. 2016. Anthropogenic disturbances create a new vegetation toposequence in the Gatineau River valley, Québec. Forests 7: 254; doi:10.3390/f7110254
Lamb, M. 1968. Itineraries of John Macoun, with places visited, compiled in the first place from his autobiography (1922). Unpublished document.
Larrson, P. and Y. Gauslaa. 2011. Rapid juvenile development in old forest lichens. Botany: 65-72.
Larson, B.M., J.L. Riley, E.A. Snell and H.G. Godschalk. 1999. The Woodland Heritage of Southern Ontario: A Study of Ecological Change, Distribution and Significance. Federation of Ontario Naturalists, Don Mills, Ontario. 262 pp.
Lättman H., A. Brand, J. Hedlund, M. Krikorev, N. Olsson, A. Robeck, F. Rönnmark and J.E. Mattsson. 2009. Generation time estimated to be 25-30 years in Cliostomum corrugatum (Ach.) Fr. Lichenologist 41: 557-559.
Lavoie, A., J. Collin, J. Gagnon, S.R. Brinker, I.M. Brodo, C. Roy, F. Anderson, R.T. McMullin and A. Huereca. 2024. Additions to the lichens, allied fungi and lichenicolous fungi of Québec, Canada, with emphasis on the area below the 50th parallel. Opuscula Philolichenum 23: 82-112.
LeBlanc, F. 1963. Quelques sociétés ou unions d’épiphytes du sud du Québec. Canadian Journal of Botany 41: 591-638.
Lendemer, J.C. 2009. A synopsis of the lichen genus Heterodermia (Physciaceae, lichenized Ascomycota) in eastern North America. Opuscula Philolichenum 6: 1-36.
Lendemer, J.C. and N. Noell. 2018. Delmarva Lichens: An illustrated manual. Memoirs of the Torrey Botanical Society 28: 1-386.
Lendemer, James. 2021 pers. comm. to Sam Brinker.
Lepage, E. 1947-1949. Les lichens, les mousses et les hépatiques du Québec, et leur rôle dans la formation du sol arable dans la région du bas de Québec, de Lévis à Gaspé. Inventaire des espèces du Québec: Les Lichens. Le Naturaliste Canadien 74: 8-16, 93-101, 225-240, 280-292; 75: 31-48, 90-96, 174-184, 228-256; 76: 45-88.
Lewis, C.J. and S.R. Brinker. 2017. Notes on new and interesting lichens from Ontario, Canada – III. Opuscula Philolichenum 16: 153-187.
Lewis, C.J., 2020. Checklist of the lichens and allied fungi of Frontenac Provincial Park, Ontario. Rhodora 121: 248-296.
Lewis, C.J., I. Brodo and T. McMullin. 2023. Checklist of lichens of Algonquin Provincial Park. The Friends of Algonquin Park, Whitney, Ontario.
Lönnell, N., K. Hylander, B.G. Jonsson and S. Sundberg. 2012. The fate of the missing spores – patterns of realized dispersal beyond the closest vicinity of a sporulating moss. PLoS One. 7. doi.org/10.1371/journal.pone.0041987.
Loo, J., L. Cwynar, B. Freedman and N. Ives. 2010. Changing forest landscapes in the Atlantic Maritime Ecozone. Pp. 35-42 in: D.F. McAlpine and I.M. Smith. Assessment of Species Diversity in the Atlantic Maritime Ecozone. NRC Research Press, Ottawa. 785 pp.
Lücking, R., B.P. Hodkinson and S.D. Leavitt. 2017. The 2016 classification of lichenized fungi in the Ascomycota and Basidiomycota – approaching one thousand genera. Bryologist 119: 361-416.
Macoun, J. 1902. Catalogue of Canadian Plants Part VII.-Lichens and Hepaticae. Geological Survey of Canada, Ottawa: Government Printing Bureau. 180 pp.
Maloles, J.R., R.T. McMullin, J.A. Consiglio, C.J. Chapman, L.L. Riederer and D.E. Renfrew. 2018. The lichens and allied fungi of the Credit River Watershed, Ontario Canada. Rhodora 120: 229-253.
Manzitto-Tripp, E.A, J.C. Lendemer and C.M. McCain. 2022. Most lichens are rare, and degree of rarity is mediated by lichen traits and biotic partners. Diversity and Distributions 28: 1810-1819.
Markowski-Lindsay, M., P. Catanzaro, A. Robillard, B.J. Butler, D.A. Orwig, A.W. D’Amato, J.R. Thompson, D.M. Laflower, M. Graham MacLean and M. Itter. 2023. Forester and logger response to Emerald Ash Borer in Massachusetts and Vermont: A secondary disturbance. Journal of Forestry 121: 319-332.
McKenney, D.W., J.H. Pedlar, K. Lawrence, P.A. Gray, S.J. Colombo and W.J. Crins. 2010. Current and Projected Future Climatic Conditions for Ecoregions and Selected Natural Heritage Areas in Ontario. Ontario Ministry of Natural Resources. Applied Research and Development Branch. III. Series: Climate change research report; CCRR-16. 42 pp.
McMullin, R.T. and J.C. Lendemer. 2016. Lichens and allied fungi of Awenda Provincial Park, Ontario: diversity and conservation status. American Midland Naturalist 176: 1-19
McMullin, R.T., J. Gagnon, F. Anderson, W.R. Buck, S.R. Clayden, B.C. Dorin, A. Fryday, J.G. Guccion, R.C. Harris, J. Hinds, C. Isabel, D. Ladd, E. Lay, J.C. Lendemer, J.R. Maloles, C. Roy and D.P. Waters. 2017. One hundred new provincial, national, and continental lichen and allied fungi records from Parc national de la Gaspésie, Québec, Canada. Northeastern Naturalist 24: 446-466.
Moberg, R. 2011. The lichen genus Heterodermia (Physciaceae) in South America – a contribution including five new species. Nordic Journal of Botany 29: 129-147.
Moberg, R. and T.H. Nash III. 1999. The genus Heterodermia in the Sonoran Desert Area. Bryologist 102: 1-14.
Mongkolsuk, P., S. Meesim, V. Poengsungnoen, K. Buaruang, F. Schumm and K. Kalb. 2015. The lichen family Physciaceae in Thailand II. Contributions to the genus Heterodermia sensu lato. Phytotaxa 235: 1-66.
NatureServe. 2020. Habitat-based Plant Element Occurrence Delimitation Guidance. NatureServe, Arlington, Virginia.
NatureServe. 2023. NatureServe Network Biodiversity Location Data accessed through NatureServe Explorer [NatureServe Explorer]. NatureServe, Arlington, Virginia.
Nieboer, E., J.D. McFarlane and D.H.S. Richardson. 1984. Modification of plant cell buffering capacities by gaseous air pollutants. pp. 314-333, In Koziol, M., and F.R. Whatley (eds.), Gaseous Air Pollutants and Plant Metabolites, Butterworths, London.
Northern Tornadoes Project. 2023. Maps for May 21st derecho and all 2022 ground surveys.
OMNR (Ontario Ministry of Natural Resources) 2010. Forest Management Guide for Conserving Biodiversity at the Stand and Site Scales.
Ott, S., K. Treiber and H.M. Jahns. 1993. The development of regenerative thallus structures in lichens. Botanical Journal of the Linnean Society 113: 61-76.
Palik, B.J., A.W. D’Amato and R.A. Slesak. 2021. Wide-spread vulnerability of black ash (Fraxinus nigra Marsh.) wetlands in Minnesota USA to loss of tree dominance from invasive emerald ash borer. Forestry 94: 455-463.
Paquette, H.A. 2019. Macrolichen and calicioid flora of Forillon National Park, Québec, Canada: the big and little lichens and their associates. M.Sc. thesis. Carleton University. Ottawa, Ontario. 126 pp.
Paquette, H.A. and R.T. McMullin. 2020. Macrolichens of Forillon National Park, Québec, Canada. Northeastern Naturalist 27: 1-35.
Piercey-Normore, Michele and Diana Sawatzky 2022. pers. comm. to Sam Brinker.
Pomerleau, R. 1961. History of the Dutch Elm Disease in the province of Québec, Canada. Forestry Chronicle 37: 356-367.
Prasad, A.M., L.R. Iverson, M.P. Peters, J.M. Bossenbroek, S.N. Matthews, T.D. Sydnor, and M.W. Schwartz. 2010. Modeling the invasive emerald ash borer risk of spread using a spatially explicit cellular model. Landscape Ecology 25: 353-369.
Reed, L.L. 1950. The 1950 status of the Dutch Elm Disease in Canada. The 81 Annual Report of the Entomological Society of Ontario 81: 103-104.
Richardson, D.H.S. 1992. Pollution Monitoring with Lichens. Naturalists’ Handbooks 19. Richmond Publishing, Slough, UK.
Ronnås, C., S. Werth, O. Ovaskainen, G. Várkonyi, C. Scheidegger and T. Snäll. 2017. Discovery of long-distance gamete dispersal in a lichen-forming ascomycete. New Phytologist 216: 216-226.
Showman, R.E. 1997. Continuing lichen recolonization in the Upper Ohio River Valley. Bryologist 100: 478-481.
Sutter, D. 1987. Concerning the protection of rare plant sites. Castanea 52: 147-149.
Swinscow, T.D.V. and H. Krog. 1976. The genera Anaptychia and Heterodermia in east Africa. Lichenologist 8: 103-138.
Taylor, K., W.I. Dunlop, A. Handyside, S. Hounsell, B. Pond, D. MacCorkindale, J. Thompson, M. McMurtry and D. Krahn (lead authors). 2014. Mixedwood Plains Ecozone Status and Trends Assessment—with an emphasis on Ontario. Canadian Biodiversity: Ecosystem Status and Trends 2010, Technical Ecozone+ Status and Trends Report. Canadian Council of Resource Ministers, Ottawa, ON. 344+ XLVIII pgs.
Thayer, J. and B. Henderson 2019. Personal communication to Sam Brinker.
Tremblay, Benoît. 2025. Personal communication by email with André Arsenault in April 2025.
Tretiach, M., P. Crisafulli, E. Pittao, S. Rinino, E. Roccotiello, and P. Modenesi. 2005. Isidia ontogeny and its effects on the CO2 gas exchanges of the epiphytic lichen Psuedevernia furfuracea (L.) Zopf. Lichenologist 37: 445-462.
Tripp, E. A. 2016. Is asexual reproduction an evolutionary dead end in lichens? Lichenologist 48: 559-580.
Tripp, E.A. and J.C. Lendemer. 2020. Field Guide to the Lichens of Great Smoky Mountains National Park. University of Tennessee Press, Knoxville. 569 pp.
Vobis, G. 1977. Studies on the germination of lichen conidia. Lichenologist 9: 131-136.
Wetmore, C.M. 1981. Lichens of Voyageurs National Park, Minnesota. Bryologist 84: 482-491.
Wetmore, C.M. 1990. Lichens of Apostle Islands National Lakeshore, Wisconsin. 1990. Michigan Botanist 29: 65-73.
White, D.J. 1996. Survey and evaluation of the stand structure and life science resources of old growth forest at Billa Lake and Raycroft Lake. Information report No. 21. Eastern Ontario Model Forest, Kemptville, Ontario. 52 pp.
Wiken, B., D. Gautier, I. Marshall, K. Lawton and H. Hirvonen. 1996. A Perspective on Canada’s Ecosystems: An Overview of the terrestrial and Marine Ecozones. Ottawa, CA: Canadian Council on Ecological Areas. NO.14. 88 pp.
Wong, P.Y. and I.M. Brodo. 1992. The lichens of southern Ontario. Syllogeus 69: 1-79.
Woo-Durand, C., J.M. Matte, G. Cuddihy, C.L. McGourdji, O. Venter and J.W.A. Grant. 2020. Increasing importance of climate change and other threats to at-risk species in Canada. Environmental Reviews 28: 449-456.
Yahr, Rebecca, Jessica L. Allen, Violeta Atienza, Frank Burgartz, Nathan Chrismas, Manuela Dal Forno, Polina Degtjarenko et al. “Red Listing lichenized fungi: best practices and future prospects.” The Lichenologist 56, no. 6 (2024): 345-362.
Youngquist, M.B., S.L. Eggert, A.W. D’Amato, B.J. Palik, and R.A. Slesak. 2017. Potential effects of foundation species loss on wetland communities: A case study of Black Ash wetlands threatened by Emerald Ash Borer. Wetlands 37: 787-799.
Biographical summary of report writer
Samuel Brinker (SB) is the provincial botanist and lichenologist with the Natural Heritage Information Centre (NHIC) in the Science and Research Branch of the Ontario Ministry of Natural Resources. In this role, he conducts lichen surveys and biodiversity assessments across the province to monitor their distribution and status. He is a NatureServe member botanist and is responsible for maintaining provincial conservation status ranks for vascular plants and lichens, as well as plant and lichen occurrence data for the province. Since beginning with NHIC in 2009, he has discovered dozens of lichens new to North America, Canada, and Ontario as well as new species to science. Sam is a member of the COSEWIC Vascular Plant Species Specialist Committee and has written or co-written numerous COSEWIC and provincial status reports on lichens and vascular plants.
Collections examined
Specimens housed at the following herbaria/websites were consulted with respect to records of Heterodermia hypoleuca in Canada:
- Canadian Museum of Nature, Lichen Herbarium, Gatineau (CANL)
- Louis-Marie Herbarium, Université Laval, Quebec City (QFA)
- Consortium of Lichen Herbaria (CLH)
- New York Botanical Garden, Bronx, New York (NYBG)
Appendix 1. Collection details and land tenure for all Canadian subpopulations
| Subpopulation | Year Found | Last Obs. | Ownership | 2019 to 2024 SB search effort | Sourcea,b | Apothecia present |
|---|---|---|---|---|---|---|
| Ontario | ||||||
| Algonquin Park | 1900 | 1900 | Unknown | No | Literature report | - |
| Beaver Creek A | 2021 | 2021 | Nature Conservancy | Yes | SB 8961 | Yes |
| Beaver Creek B | 2021 | 2021 | Nature Conservancy | Yes | SB 9169 | Yes |
| Beckwith | 2023 | 2023 | Private | Yes | SB 10091; JR sight record | Yes |
| Belmont Lake | 2020 | 2022 | Crown | Yes | SB 8369 | Yes |
| Block 509 | 2023 | 2023 | Crown | Yes | SB10363 | No |
| Bolingbroke Rd. | 2023 | 2023 | Private | No | JR sight record | No |
| Brighton | 1891 | 1891 | Unknown | No | JM 178 (CANL) | - |
| Cassidy Block | 2012 | 2022 | Conservation Authority | Yes | SB 2790 | Yes |
| Charleston Lake PP | 2023 | 2023 | Ontario Parks | Yes | SB sight record | No |
| Constant Creek CR | 2023 | 2023 | Ontario Parks | Yes | SB 10175 | Yes |
| County Forest East | 2022 | 2022 | Municipal | Yes | SB sight record | Yes |
| Crow Lake | 2023 | 2023 | Crown | Yes | SB 9743 | Yes |
| Crowe River CR | 2017 | 2022 | Ontario Parks | Yes | SB 6319 | Yes |
| Darling Long Lake | 2001 | 2001 | Crown | No | RL 933 (REL) | ? |
| Deseronto Rd. | 2014 | 2014 | Private | Yes | CL 2142 | Yes |
| Frontenac PP | 2016 | 2021 | Ontario Parks | Yes | CL 2620, 2667,3156, 3158 | No |
| Glanmire | 2024 | 2024 | Crown | Yes | SB sight record | No |
| H.R. Frink CA | 2022 | 2022 | Conservation Authority | Yes | SB 9637 | No |
| Kip Fleming Tract | 2024 | 2024 | Nature Conservancy | Yes | SB sight record | No |
| Lake Nipigon | 1884 | 1884 | Unknown | No | Literature report | - |
| Massassauga Point | 2022 | 2022 | Conservation Authority | Yes | SB 9342 | Yes |
| Moira River | 2023 | 2023 | Conservation Authority | Yes | SB sight record | No |
| Mosque Lake Rd. | 2024 | 2024 | Crown | No | JR sight record | Yes |
| Murphy’s Point PP | 2023 | 2023 | Ontario Parks | Yes | SB 9758 | Yes |
| Near Hull, Ontario | 1907 | 1907 | Unknown | No | JM 204-07 (FH) | - |
| Near Wooler | 1893 | 1893 | Unknown | No | Literature report | - |
| Oatbox | 2011 | 2022 | Conservation Authority | Yes | CL 610 | Yes |
| OR Agreement Forest | 2022 | 2022 | Municipal | Yes | SB 9706 | No |
| Ottawa | 1891 | 1891 | Unknown | No | JM s.n. (NEB) | - |
| Ottawa River | 2016 | 2023 | Crown | Yes | SB 4867 and 9533 | Yes |
| Prescott | 1861 | 1861 | Unknown | No | BB s.n. (CANL) | - |
| Lavant | 2024 | 2024 | Crown | Yes | SB sight record | Yes |
| Rawdon Block | 2023 | 2023 | Conservation Authority | Yes | SB 10366 | Yes |
| S of Marmora | 2012 | 2012 | Private | No | CL 1075 | ? |
| S of Quackenbush | 2012 | 2012 | Private | No | CL 1413 | ? |
| Sharbot Lake PP | 2022 | 2022 | Ontario Parks | Yes | SB sight record | No |
| Shaw Woods | 2023 | 2023 | Private | No | JR sight record | No |
| Silver Lake PP | 2022 | 2023 | Ontario Parks/Private | Yes | JR sight record; SB 9658 | No |
| Squirrel Creek CA | 2022 | 2022 | Conservation Authority | Yes | SB 7397 | Yes |
| Vanderwater CA | 2024 | 2024 | Conservation Authority | Yes | SB 10752 | Yes |
| Westmeath PP | 2015 | 2023 | Ontario Parks | Yes | SB 4776 (NY) | Yes |
| Quebec | ||||||
| “Cap-à-l’Aigle” | 1905 | 1905 | Unknown | No | JM s.n. and 4094 (CANL) | Yes |
| Gatineau Park | n.d. | n.d. | Federal | No | AH s.n. (CANL) | Yes |
| Île Bonaventure | 1961 | 1961 | La Sépac | No | ET s.n. (CANL) | No |
| Mont Johnson | 1958 | 1958 | Unknown | No | FL 8725 (QFA) | - |
| Montmorency Falls | 1905 | 1905 | Unknown | No | JM IV-85 (FH) | - |
| Philipsburg | 2016 | 2022 | Private | Yes | RH 61528 (NY), SB 9621 | Yes |
| New Brunswick | ||||||
| Saint John River | 2022 | 2024 | Private | No | SC 28663 | ? |
a Source codes for collectors: BB = Braddish Billings; SB = Samuel Brinker; SC = Stephen Clayden; AH = Ann Hanes; RH = Richard Harris; FL = Fabius LeBlanc; RL = Rob Lee; CL = Chris Lewis; JM = John Macoun; JR = John Ruddy; ET = Eric Thorn.
b Herbarium codes: CANL = Canadian Museum of Nature (Lichens); FH = Harvard University; NEB = University of Nebraska State Museum; NY = New York Botanical Gardens; QFA = Louis-Marie Herbarium; REL = private herbarium of Rob Lee.
Appendix 2. Method for estimating number of individuals and occupied host trees on unsurveyed private land in Ontario
This analysis includes 2019 to 2024 data collected by Sam Brinker (SB) from 45 distinct sites (at least 1 km apart) with suitable habitat on public land between Peterborough and the Ottawa River, where ash trees are the primary host substrate, in locations that had no previous records. This search effort yielded 16 new subpopulations, or a 35% search success rate.
Data used in this assessment incorporates low and high counts to provide a range estimate to reflect some uncertainty. Scenario 1 incorporates 15 subpopulations consisting of 101 individuals on 34 ash trees (the low estimate excluding unusually large Constant Creek subpopulation that may skew the typical habitat based on its extent). Scenario 2 incorporates 16 sites consisting of 154 on 50 trees (the high estimate including Constant Creek subpopulation).
Calculations to determine amount of suitable private land habitat
Approximately 36,871 km2 total area in eight counties in eastern Ontario where Heterodermia hypoleuca ranges: City of Ottawa†, Hastings, Lanark, Leeds and Grenville, Lennox and Addington†, Peterborough, Prince Edward, and Renfrew († denotes counties with no records but likely present).
Approximately 27,431 km2 of this is private land, or about 74% (in private ownership).
Of that private land, approximately 21,890 km2 is underlain by suitable calcareous substrata (the remainder is acidic bedrock and not considered suitable).
Of this remaining area, approximately 250 km2 contains stands with Black Ash based on Forest Resource Inventory values (Black Ash used as a proxy since Green Ash is not differentiated).
For estimation purposes, each subpopulation is assumed to exist within a unique 1 km2 area.
| Average | = | Total number of individuals | = | 101 | ≈ 6.7 individuals/km2 |
|---|---|---|---|---|---|
| Number of sites | 15 | ||||
| Average | = | Total number of individuals | = | 154 | ≈ 10.2 individuals/km2 |
| Number of sites | 16 |
| Average | = | Total number of individuals | = | 34 | ≈ 2.2 host trees/km2 |
|---|---|---|---|---|---|
| Number of sites | 15 | ||||
| Average | = | Total number of individuals | = | 50 | ≈ 3.1 host trees/km2 |
| Number of sites | 16 |
With 250 km2 of unsearched suitable habitat on private land, the potential number of individuals and host ash trees in these areas can be estimated as follows:
- Low = 6.7 individuals per km2 × 250 km2 = 1,675 individuals
- High = 10.2 individuals per km2 × 250 km2 = 2,550 individuals
- Low = 2.2 trees per km2 × 250 km2 = 550 host trees
- High = 3.1 trees per km2 × 250 km2 = 775 host trees
Given the 35% search success rate obtained on public land in similar habitat:
- Low = 35% of 1,675 individuals = 586 individuals (approximately 580)
- High = 35% of 2,550 individuals = 892 individuals (approximately 900)
- Low = 35% of 550 host trees = 192 (approximately 190)
- High = 35% of 775 host trees = 271 (approximately 270)
Assumptions made
- Heterodermia hypoleuca occurs at roughly 5 to 8 thalli per square kilometre where preferred habitat consists of forest units with a Black/Green Ash component
- Heterodermia hypoleuca occurs on roughly 2 to 3 host ash trees per square kilometre where preferred habitat consists of forest units with a Black/Green Ash component
- Forest Resource Inventory data used was accurate (which we understand is not always true)
- Forest Resource Inventory data indicating the presence of Black Ash does not distinguish Green Ash from Black Ash, but its presence indicates saturated. mineral soil (for at least a portion of the year) and excludes upland areas of White Ash
- Land tenure data used was accurate (which may not always be true)
- Surficial geology mapping data was accurate (which we understand is not always true)
Limitations
- Forest Resource Inventory stand description (tree species composition) data covers only 61% (22,600 km2) of the total area for calculations
Appendix 3. Threats calculator assessment for the Cupped Fringe Lichen (Heterodermia hypoleuca)
Species scientific name: Cupped Fringe Lichen (Heterodermia hypoleuca)
Date: 3/4/2024
Assessor(s):
Dwayne Leptizki (Facilitator)
SR writer: Sam Brinker
M&L SSC: Jennifer Doubt, Chris Deduke, Toby Spribille, Marc Favreau, Cassandra Robillard, Tegan Padgett
External participant: Julie McKnight (ECCC)
References: Draft calculator provided by writer S. Brinker. Draft COSEWIC report, teleconference from March 7, 2024.
| Threat impact | Level 1 threat impact counts - high range | Level 1 threat impact counts - low range |
| A (Very high) | 1 | 0 |
| B (High) | 1 | 1 |
| C (Medium) | 1 | 0 |
| D (Low) | 1 | 3 |
| Calculated overall threat impact: | Very high | High |
Assigned overall threat impact:
AB = Very high – High
Overall threat comments:
Estimated generation time: 10 to 30 yrs (for an ascospore to land and grow into a lichen producing fruit bodies that release spores). Therefore, the severity and temporal range is 30 to 90 years into the future. Southern ON, QC, and recent (from 2022) NB (fig 2, pdf), but assessed as single DU because of its continuous distribution and no obvious disjunctions. It is an indicator of high-quality, rich, humid, mature hardwood forest stands, sites close to water, most likely due to humidity; primarily (74%) ash trees; approximately 98% of 476 thalli (in 34 subpopulations) in ON, 2% in QC (1 subpopulation), <1% NB (1 subpopulation). Of the total, 24% (102 individuals) on dead/downed trees and are not expected to survive. Known subpopulations have been lost. There is a 78% loss of entire Canadian population projected due to EAB and recent storm events. There are 13 subpopulations in provincial parks or privately managed lands for conservation; 18 subpopulations occur on “unprotected” lands. Scores for scope below are based on individuals, not subpopulations.
| Number | Threat | Impact (calculated) | Impact | Scope (next 10 years) | Severity (10 years) | Timing | Comments |
|---|---|---|---|---|---|---|---|
| 1 | Residential and commercial development | Not applicable | Negligible | Negligible (<1%) | Extreme (71 to 100%) | Moderate (Possibly in the short term, <10 yrs/3 gen) | Not applicable |
| 1.1 | Housing and urban areas | Not applicable | Negligible | Negligible (<1%) | Extreme (71 to 100%) | Moderate (Possibly in the short term, <10 yrs/3 gen) | Scope restricted and small because most individuals occur in protected areas or lands with almost no likelihood of development. Limited to sites on private land and near settlements that could be impacted, which include Beckwith, Marmora, and possibly two Ottawa River sites (where waterfront cottages are popular). Threat category includes cottages |
| 1.2 | Commercial and industrial areas | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 1.3 | Tourism and recreation areas | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Considered but not scored. Currently only one thallus could be affected by expansion of campgrounds/picnic sites |
| 2 | Agriculture and aquaculture | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 2.1 | Annual and perennial non-timber crops | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 2.2 | Wood and pulp plantations | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 2.3 | Livestock farming and ranching | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Considered but not scored. Past history of grazing and land conversion would have impacted the species, but this is not currently affecting any locations |
| 2.4 | Marine and freshwater aquaculture | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 3 | Energy production and mining | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 3.1 | Oil and gas drilling | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 3.2 | Mining and quarrying | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 3.3 | Renewable energy | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | not applicable |
| 4 | Transportation and service corridors | D | Low | Restricted –Small (1 to 30%) | Moderate – Slight (1 to 30%) | High (Continuing) | Not applicable |
| 4.1 | Roads and railroads | D | Low | Restricted – Small (1 to 30%) | Moderate – Slight (1 to 30%) | High (Continuing) | Associated with subpopulations on Crown land (provincial), private land, municipally owned land, and possibly some Conservation Authority owned lands where active logging is occurring or could occur. Also includes road activities in provincial parks or forestry activities (routing roads through habitat, removal of trees for road construction or widening, altering drainage etc.). (approximately 50+) |
| 4.2 | Utility and service lines | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | not applicable |
| 4.3 | Shipping lanes | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 4.4 | Flight paths | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 5 | Biological resource use | CD | Medium – Low | Restricted – Small (1 to 30%) | Extreme – Serious (31 to 100%) | High (Continuing) | Not applicable |
| 5.1 | Hunting and collecting terrestrial animals | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 5.2 | Gathering terrestrial plants | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Considered but not scored. Increased incidences of collecting could result from listing the species, because rare/threatened species tend to spike public interest and targeted searches by interested individuals. Threat would likely be negligible (in addition to being hard to document). Only lethal collecting, including scientific, scored here |
| 5.3 | Logging and wood harvesting | CD | Medium – Low | Restricted – Small (1 to 30%) | Extreme – Serious (31 to 100%) | High (Continuing) | Associated with subpopulations on Crown land (provincial), private land, municipally owned land, and possibly some Conservation Authority owned lands where active logging is occurring or could occur. Includes direct removal of host trees as merchantable timber, as well as associated indirect and edge effects from that activity (changes in local humidity, stand structure). Ashes are also being targeted for salvage removal due to Emerald Ash Borer infestations. All host trees are hardwoods and are important target species for firewood. Removal of hazard trees in provincial parks and conservation areas around trails, roads and campgrounds was observed in one provincial park, and could occur at three others. (approximately 50+) |
| 5.4 | Fishing and harvesting aquatic resources | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 6 | Human intrusions and disturbance | Not applicable | Negligible | Pervasive (71 to 100%) | Negligible (<1%) | High (Continuing) | Not applicable |
| 6.1 | Recreational activities | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Considered but not scored. A few sites occur near or along trails (particularly St. John River, Philipsburg Wildlife Sanctuary, Bekwith, Massassauga Point, and Silver Lake Provincial Park), which could be impacted by recreational activities, although none were observed, and the impact would most likely be negligible because most individuals are in seasonally flooded areas (not generally used by recreationalists) |
| 6.2 | War, civil unrest and military exercises | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 6.3 | Work and other activities | Not applicable | Negligible | Pervasive (71 to 100%) | Negligible (<1%) | High (Continuing) | Non-lethal collecting and related in situ effects from ongoing information gathering and research (for example, monitoring and conservation actions) expected to continue at many sites. Hazard trees scored under 5.3 |
| 7 | Natural system modifications | AB | Very high – High | Pervasive – Large (31 to 100%) | Extreme (71 to 100%) | High (Continuing) | Not applicable |
| 7.1 | Fire and fire suppression | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Considered but not scored. Vast majority of individuals restricted to rich, mature lowland and swamp forest habitat that is not particularly fire-prone |
| 7.2 | Dams and water management/use | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Considered but not scored. Dams occur on several rivers associated with seasonally flooded swamp forest where the species occurs, but those impacts have likely mostly occurred in the past when the dams were constructed (no new impacts likely). Unaware of any new proposed dams |
| 7.3 | Other ecosystem modifications | AB | Very high – High | Pervasive – Large (31 to 100%) | Extreme (71 to 100%) | High (Continuing) | Emerald Ash Borer* is indirectly affecting individuals by killing their host ash trees forecasted to impact 74% of the Canadian population (that occurs on ash trees and given rates in ranges of EAB spread which is still unclear in heavily forested areas). The scope is not expected to reach 100% (since the species occurs on several other host tree species). Dutch Elm Disease impacts have occurred in the past by killing most large, mature trees which were historically occupied by the species. The disease is still prevalent and elms no longer regularly attain suitably large trunk diameters and bark characteristics prior to the onset of DED attacks which likely accounts for the absence of recent observations of H. hypoleuca on elm. Invasive woody species, particularly common and alder buckthorns (Rhamnus cathartica and Frangula alnus) are invading calcareous areas within range of many subpopulations and could result in changes in understory composition and reduced access to light (although this was only observed directly at one subpopulation). |
| 8 | Invasive and other problematic species and genes | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 8.1 | Invasive non-native/alien species/diseases | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Considered but not scored. Herbivory by invasive slugs (Arion spp.) has been recorded as a threat to several lichens in other parts of Canada and could turn out to be a threat to Heterodermia hypoleuca, though no direct evidence currently exists (and would require additional assessment) |
| 8.2 | Problematic native species/diseases | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Considered but not scored. Beavers cut down trees and thalli associated with trees downed by this activity would be killed. Beaver activity was observed at several locations, though no thalli were observed on trees that were cut down by beaver |
| 8.3 | Introduced genetic material | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 8.4 | Problematic species/diseases of unknown origin | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 8.5 | Viral/prion-induced diseases | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 8.6 | Diseases of unknown cause | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 9 | Pollution | Not applicable | Unknown | Pervasive (71 to 100%) | Unknown | High (Continuing) | Not applicable |
| 9.1 | Domestic and urban waste water | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 9.2 | Industrial and military effluents | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 9.3 | Agricultural and forestry effluents | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 9.4 | Garbage and solid waste | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 9.5 | Airborne pollutants | Not applicable | Unknown | Pervasive (71 to 100%) | Unknown | High (Continuing) | Roughly 95% of all individuals in the Canadian population occur on ashes (Fraxinus spp.) and oaks (Quercus spp.), host trees which are long-lived, and tend to have a slightly basic bark chemistry. Previous as well as ongoing exposure to acid moisture/deposition or sulphur dioxide emissions can eventually overcome the buffering capacity of bark with a neutral or slightly basic pH, making it too acidic. Impact data or quantification of acidification of hardwood tree bark is seemingly lacking/uncertain (reflected in the scores). More southern sites away from continuous forest cover likely more at risk (airborne agricultural and non-point pollutants). Dust from roads/industry considered here, though no individuals appeared to be impacted by dust |
| 9.6 | Excess energy | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 10 | Geological events | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 10.1 | Volcanoes | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 10.2 | Earthquakes/tsunamis | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 10.3 | Avalanches/landslides | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 11 | Climate change and severe weather | BD | High – Low | Pervasive (71 to 100%) | Serious – Slight (1 to 70%) | High (Continuing) | Not applicable |
| 11.1 | Habitat shifting and alteration | Not applicable | Unknown | Unknown | Unknown | Unknown | Range shifts (to areas of unoccupied suitable habitat) associated with changing climatic envelopes possible (because it is at its northern range limit in Canada), but unknown currently |
| 11.2 | Droughts | Not applicable | Unknown | Pervasive (71 to 100%) | Unknown | High (Continuing) | Increased droughts could stress host trees, as well as reduce local humidity levels if swamp forest habitat flood regimes are altered via climate change (increased evapotranspiration, reduced duration, extent, frequency of flooding) |
| 11.3 | Temperature extremes | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
| 11.4 | Storms and flooding | BD | High – Low | Pervasive (71 to 100%) | Serious – Slight (1 to 70%) | High (Continuing) | An increase in the frequency and severity in weather events, including blow-down of host trees or physical damage from ice storm activity, is expected with a warming climate. Two unusual storm events in 2022 (derecho and a tornado) caused damage to habitat at 5 subpopulations where pproximately28 thalli were on recently downed trees. Host trees in wetland soils tend to be shallow-rooted and susceptible to blowdown |
| 11.5 | Other impacts | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable | Not applicable |
Classification of Threats adopted from IUCN-CMP, Salafsky et al. (2008).