Banff Springs snail (Physella johnsoni) COSEWIC assessment and status report: chapter 13
Technical Summary
Physella johnsoni
Range of Occurrence in Canada: Alberta
Demographic Information
Observed percentage of increase in total number of mature individuals over the last 10 years.
Results based on linear regression estimates of yearly population minima, maxima, and mean for 1996 through 2005 (Figure 12).
Original 5: 1996 max.=10 608; 2005 max.=16 965
All 7: 1996 min.=2 536; 2005 min.=9 358
1996 max.=6 246; 2005 max.=29 908
1996 mean=3 746; 2005 mean=19 058
Original 5 subpopulations combined, minima: no discernible trend in linear regression of yearly minima (P=0.143), maxima: significant increase in linear regression of yearly maxima (P=0.037) and a 60% increase in yearly linear regression estimates of maxima between 1996 and 2005.
Original 5 + re-introduced subpopulations, minima: 269% increase, maxima: 379% increase, mean: 409% increase
Decline projected if drying trend of springs continues/increases
Detailed populations counts occurred once every three weeks from January 1996 through August 2000, and then once every four weeks since then.
Number of mature individuals in each population
Extent and Area Information
In 2006; Historical: 0.345 km2; 1996: 0.0326 km2.
See p.13 on how this was derived.
Historical 1926 excluding the Banff Springs Hotel & Vermilion Cool sites; 1996 includes 5 extant subpopulations; 2006 includes the 5 extant and 2 re-introduced subpopulations.
From 1996–2006, 443%; 91% decline historical - 1996.
Increase over last 10 years due to re-introducing 2 subpopulations.
Extreme fluctuations possible due to extirpation and anthropogenic re-introductions from extant subpopulations.
AO calculated by Alain Filion, COSEWIC Secretariat, April 2008
Biological area of occupancy, based on the two-dimensional surface area of all microsites (see Table 1): 0.0006 km2
Extreme fluctuations possible due to extirpation and anthropogenic re-introduced from extant subpopulations.
Drying trend of springs removes and affects quality of habitat.
Additional protection in the form of Park Superintendent closures, fencing, electronic surveillance, and communication with visitors has improved the overall quality of habitat since 1996.
Quantitative Analysis
Lower Middle: 27%
Cave: 21%
Basin: 4%
Upper C&B: 3%
Lower C&B: 29%
All 5 combined: 0%
Threats (actual or imminent, to populations or habitats)
In order of certainty and severity (highest to lowest) the following threats have been identified (Table 2 and Limiting Factors and Threats) and occur naturally (N) or by humans through facility operations (FO) or other actions (Hu):
- Thermal water flow stoppages (N)
- Thermal water flow reductions / fluctuations (N and FO)
- Thermal water flow redirections (N, FO)
- Limited or low quality habitat (N, FO)
- Soaking and swimming (Hu)
- Population lows and genetic inbreeding (N)
- Trampling and other local disturbances (Hu)
- Limb-dipping (Hu)
- Stochastic events (N)
- Others (predation, competition, collecting, twitch-ups) (Hu, N)
Rescue Effect (immigration from an outside source): No
Current Status
COSEWIC: Threatened (April 1997)
COSEWIC: Endangered (May 2000)
COSEWIC: Endangered (April 2008)
Global Status: G1
Alberta Status: S1
Status and Reasons for Designation
Reasons for Designation: This is a Canadian endemic species with its distribution entirely within the upper reaches of fewer than 5 separate thermal springs locations in Banff National Park, Alberta. These springs comprise a single population, which makes it very susceptible to a catastrophic event. These short-lived animals undergo natural annual fluctuations of over two orders of magnitude. All thermal springs historically or currently occupied by this species have been impacted by human development. These snails are habitat specialists requiring a steady supply of warm thermal spring water containing a high concentration of dissolved minerals and a complex microbial community that provides food and habitat. The species and its habitat are currently protected from disturbance and destruction under Species at Risk Act and the Canada National Parks Act, but illegal activities such as soaking in thermal waters, which can crush snails and eggs and disturb habitat, are ongoing. The increase in frequency of springs drying due to climate change, which has been observed in the past decade, is believed to be an important threat to this species’ survival. However, the species is closely monitored by Parks Canada.
Applicability of Criteria
Criterion A (Decline in Total Number of Mature Individuals):
Does not apply. There is no current evidence that the population is declining or will decline over the next 10 years.
Criterion B (Small Distribution Range and Decline or Fluctuation):
Meets B1ac(iv)+2ac(iv) 1: EO = 0.177 km2 (< 5000 km2) – Endangered 2: AO = 0.0006 km2 (< 500 km2) – Endangered a: Population severely fragmented and found in 3 locations (< or = 5, Endangered), c(iv): Extreme fluctuations of numbers of individuals.
Criterion C (Small and Declining Number of Mature Individuals):
Does not apply. The number of individuals, most mature, varies annually (1 561–33 915) but the population overall has not declined.
Criterion D (Very Small Population or Restricted Distribution):
Meets D2 for Threatened. The species has a very restricted AO (5 km2), with 3 locations forming 1 population; it is a habitat specialist requiring geothermally regulated water, a high concentration of dissolved minerals and a complex microbial community. The population is of limited extent and prone to the effects of human activities or stochastic events within a very short time period.
Criterion E (Quantitative Analysis):
A quantitative analysis was done and the probability of extinction in the wild over the next 40 years (based on the 5 original locations) was zero. The probability of extirpation of individual sub-populations was higher: Lower Middle springs 27%, Cave 21%, Basin 4%, Upper Cave and Basin 3%, Lower Cave and Basin 29%.
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