Biological responses to permafrost thaw slumping in Canadian Arctic lakes

2012 ◽  
Vol 58 (2) ◽  
pp. 337-353 ◽  
Author(s):  
JOSHUA R. THIENPONT ◽  
KATHLEEN M. RÜHLAND ◽  
MICHAEL F. J. PISARIC ◽  
STEVEN V. KOKELJ ◽  
LINDA E. KIMPE ◽  
...  
2006 ◽  
Vol 63 (8) ◽  
pp. 1830-1839 ◽  
Author(s):  
David C Hardie ◽  
Roxanne M Gillett ◽  
Jeffrey A Hutchings

The genetic consequences of extended periods at low population size are fundamental to the conservation of depleted species such as the Atlantic cod (Gadus morhua). We compared microsatellite genetic variability among cod populations in Canadian Arctic lakes with that of Gilbert Bay resident and inshore cod from eastern Canada. The Arctic populations had the lowest genetic diversity and were the most strongly genetically structured and distinct. By contrast, eastern Canadian samples expressed high allelic diversity and were not significantly genetically structured or distinct relative to each other, whereas Gilbert Bay resident cod were intermediate to the Arctic and eastern Canadian groups. Our results are consistent with the hypothesis that the Arctic populations were colonized between 8000 and 5000 years ago and have experienced little or no gene flow since that time. Despite isolation at the extreme of the species' range, the Arctic populations have retained relatively high heterozygosities and high genetic effective population sizes relative to census sizes (Ne–Nc ratios). Potential explanations for this include the absence of fishing pressure, allowing for the persistence of large, highly fecund individuals, as well as biotic (e.g., absence of planktivores) and abiotic (e.g., low environmental stochasticity) factors in the Arctic lakes that minimize individual variance in reproductive success.


ARCTIC ◽  
2011 ◽  
Vol 64 (2) ◽  
Author(s):  
David C. Hardie ◽  
Jeffrey A. Hutchings

2015 ◽  
Vol 42 (8) ◽  
pp. 1553-1565 ◽  
Author(s):  
Joshua R. Thienpont ◽  
Jennifer B. Korosi ◽  
Elisa S. Cheng ◽  
Kayla Deasley ◽  
Michael F. J. Pisaric ◽  
...  

Hydrobiologia ◽  
2005 ◽  
Vol 549 (1) ◽  
pp. 131-143 ◽  
Author(s):  
K. Gajewski ◽  
G. Bouchard ◽  
S.E. Wilson ◽  
J. Kurek ◽  
L.C. Cwynar

2011 ◽  
Vol 68 (9) ◽  
pp. 1511-1527 ◽  
Author(s):  
Andrew S. Medeiros ◽  
Roberto Quinlan

An examination of the Chironomidae, the dominant aquatic invertebrate taxa found in Arctic lakes and ponds, was conducted to determine the environmental gradients that may limit their geographical distribution in the eastern Canadian Arctic. Subfossil chironomid head capsules, comprising 86 taxa, were sampled from surficial sediments of 63 lakes that spanned from tree line (northern Manitoba) across multiple regions within the eastern Canadian Arctic. Water chemistry and environmental data were then compared with chironomid assemblages using multivariate analysis. The distribution of chironomids was found to primarily follow a temperature gradient, but additional significant relationships were also found along a nutrient–productivity gradient. Several species of the Tribe Chironomini, which generally represent warm-water adapted taxa, were also found far beyond tree line in the southern Kivalliq region of Nunavut, indicating a more northerly range than previously known. While temperature and trophic status were found to strongly influence the distribution of some taxa, partially constrained gradient analysis indicates that specific chironomid taxa could be used to indicate a primary response to climate regardless of trophic status. This may allow for more holistic inferences of how aquatic communities may respond to climate change as the range of temperature dependant species expand into Arctic systems.


2020 ◽  
Vol 30 (8) ◽  
Author(s):  
Jasmina M. Vucic ◽  
Derek K. Gray ◽  
Rachel S. Cohen ◽  
Maariyah Syed ◽  
Alyssa D. Murdoch ◽  
...  

1988 ◽  
Vol 30 (1) ◽  
pp. 53-66 ◽  
Author(s):  
Richard B. Brugam ◽  
Eric C. Grimm ◽  
Nancy M. Eyster-Smith

A postglacial core was taken from Lily Lake, a soft-water lake, located on carbonate-poor till in eastern Minnesota. Pollen analysis allowed the reconstruction of watershed vegetation change. Diatom assemblages from the core were compared with 255 surface sediment assemblages from Minnesota, Maine, Labrador, and the Canadian arctic. Late-glacial assemblages were similar to Canadian arctic lakes. During the mid-postglacial period of warmer and drier climate, fossil diatom assemblages at Lily Lake were similar to those in the surface sediment of modern eutrophic hardwater lakes in Central Minnesota. The shift to hardwater diatom assemblages coincided with a shift to prairie species in fossil pollen assemblages at about 8000 yr B.P. At about 3400 year B.P. the fossil diatom assemblage that characterized presettlement times was established.


Author(s):  
Rachel S. Cohen ◽  
Derek K. Gray ◽  
Jasmina M. Vucic ◽  
Alyssa D. Murdoch ◽  
Sapna Sharma

The relationship between littoral macroinvertebrate communities and environmental gradients in Arctic lakes is poorly understood, making it difficult to predict whether these important components of lake ecosystems will be affected by emerging stressors such as permafrost thaw and road development. To better understand how littoral macroinvertebrates are related to environmental gradients, we characterized macroinvertebrate communities and environmental variables for 32 Arctic lakes across the boreal–tundra transition in the Northwest Territories. Our analysis showed that a small selection of variables had strong relationships with community structure: calcium, conductivity, latitude, surface area, catchment area, percent fine sediment, chlorophyll a, and whitefish (Coregonus clupeaformis or Coregonus nasus) presence. Many of these variables, including calcium, conductivity, and chlorophyll a levels, are affected by permafrost thaw and road dust contamination. Based on the direction and magnitude of these relationships, we hypothesize that macroinvertebrate abundance might decline in response to permafrost thaw and road dust contamination, while taxon diversity may rise. While correlative in nature, our results and hypotheses may be valuable as future studies evaluate ongoing changes in Canada’s Arctic lakes.


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