Ice-cover is the principal driver of ecological change in High Arctic lakes and ponds
Recent climate change has been especially pronounced in the High Arctic, however, the responses of aquatic biota, such as diatoms, can be modified by site-specific environmental characteristics. To assess if climate-mediated ice cover changes affect the diatom response to climate, we used paleolimno...
Published in: | PLOS ONE |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
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Public Library of Science (PLoS)
2017
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Online Access: | https://doi.org/10.1371/journal.pone.0172989 https://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0172989&type=printable https://www.ncbi.nlm.nih.gov/pubmed/28296897 http://europepmc.org/abstract/MED/28296897 https://core.ac.uk/display/149581772 https://academic.microsoft.com/#/detail/2687567072 http://europepmc.org/articles/PMC5351862?pdf=render http://europepmc.org/articles/PMC5351862 https://figshare.com/articles/Ice-cover_is_the_principal_driver_of_ecological_change_in_High_Arctic_lakes_and_ponds/4755484 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
fttriple |
language |
unknown |
topic |
Research Article Earth Sciences Marine and Aquatic Sciences Bodies of Water Ponds Lakes Ecology and Environmental Sciences Aquatic Environments Freshwater Environments Biology and Life Sciences Organisms Plants Algae Phytoplankton Diatoms Animals Invertebrates Plankton Geology Petrology Sedimentary Geology Atmospheric Science Climatology Social Sciences Archaeology Archaeological Dating Radioactive Carbon Dating Research and Analysis Methods Chemical Characterization Isotope Analysis Paleoclimatology Paleontology Nonvascular Plants Mosses Evolutionary Biology Marine Biology Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified epiphytic species High Arctic diatom assemblage responses Condition 2 assemblages oasis climate shift novel growth forms epilithic diatom assemblage Condition 1 Condition 2 High Arctic lakes |
spellingShingle |
Research Article Earth Sciences Marine and Aquatic Sciences Bodies of Water Ponds Lakes Ecology and Environmental Sciences Aquatic Environments Freshwater Environments Biology and Life Sciences Organisms Plants Algae Phytoplankton Diatoms Animals Invertebrates Plankton Geology Petrology Sedimentary Geology Atmospheric Science Climatology Social Sciences Archaeology Archaeological Dating Radioactive Carbon Dating Research and Analysis Methods Chemical Characterization Isotope Analysis Paleoclimatology Paleontology Nonvascular Plants Mosses Evolutionary Biology Marine Biology Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified epiphytic species High Arctic diatom assemblage responses Condition 2 assemblages oasis climate shift novel growth forms epilithic diatom assemblage Condition 1 Condition 2 High Arctic lakes John P. Smol Madeline Sugar Katherine Griffiths Neal Michelutti Marianne S. V. Douglas Ice-cover is the principal driver of ecological change in High Arctic lakes and ponds |
topic_facet |
Research Article Earth Sciences Marine and Aquatic Sciences Bodies of Water Ponds Lakes Ecology and Environmental Sciences Aquatic Environments Freshwater Environments Biology and Life Sciences Organisms Plants Algae Phytoplankton Diatoms Animals Invertebrates Plankton Geology Petrology Sedimentary Geology Atmospheric Science Climatology Social Sciences Archaeology Archaeological Dating Radioactive Carbon Dating Research and Analysis Methods Chemical Characterization Isotope Analysis Paleoclimatology Paleontology Nonvascular Plants Mosses Evolutionary Biology Marine Biology Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified epiphytic species High Arctic diatom assemblage responses Condition 2 assemblages oasis climate shift novel growth forms epilithic diatom assemblage Condition 1 Condition 2 High Arctic lakes |
description |
Recent climate change has been especially pronounced in the High Arctic, however, the responses of aquatic biota, such as diatoms, can be modified by site-specific environmental characteristics. To assess if climate-mediated ice cover changes affect the diatom response to climate, we used paleolimnological techniques to examine shifts in diatom assemblages from ten High Arctic lakes and ponds from Ellesmere Island and nearby Pim Island (Nunavut, Canada). The sites were divided a priori into four groups (“warm”, “cool”, “cold”, and “oasis”) based on local elevation and microclimatic differences that result in differing lengths of the ice-free season, as well as about three decades of personal observations. We characterized the species changes as a shift from Condition 1 (i.e. a generally low diversity, predominantly epipelic and epilithic diatom assemblage) to Condition 2 (i.e. a typically more diverse and ecologically complex assemblage with an increasing proportion of epiphytic species). This shift from Condition 1 to Condition 2 was a consistent pattern recorded across the sites that experienced a change in ice cover with warming. The “warm” sites are amongst the first to lose their ice covers in summer and recorded the earliest and highest magnitude changes. The “cool” sites also exhibited a shift from Condition 1 to Condition 2, but, as predicted, the timing of the response lagged the “warm” sites. Meanwhile some of the “cold” sites, which until recently still retained an ice raft in summer, only exhibited this shift in the upper-most sediments. The warmer “oasis” ponds likely supported aquatic vegetation throughout their records. Consequently, the diatoms of the “oasis” sites were characterized as high-diversity, Condition 2 assemblages throughout the record. Our results support the hypothesis that the length of the ice-free season is the principal driver of diatom assemblage responses to climate in the High Arctic, largely driven by the establishment of new aquatic habitats, resulting in increased ... |
format |
Article in Journal/Newspaper |
author |
John P. Smol Madeline Sugar Katherine Griffiths Neal Michelutti Marianne S. V. Douglas |
author_facet |
John P. Smol Madeline Sugar Katherine Griffiths Neal Michelutti Marianne S. V. Douglas |
author_sort |
John P. Smol |
title |
Ice-cover is the principal driver of ecological change in High Arctic lakes and ponds |
title_short |
Ice-cover is the principal driver of ecological change in High Arctic lakes and ponds |
title_full |
Ice-cover is the principal driver of ecological change in High Arctic lakes and ponds |
title_fullStr |
Ice-cover is the principal driver of ecological change in High Arctic lakes and ponds |
title_full_unstemmed |
Ice-cover is the principal driver of ecological change in High Arctic lakes and ponds |
title_sort |
ice-cover is the principal driver of ecological change in high arctic lakes and ponds |
publisher |
Public Library of Science (PLoS) |
publishDate |
2017 |
url |
https://doi.org/10.1371/journal.pone.0172989 https://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0172989&type=printable https://www.ncbi.nlm.nih.gov/pubmed/28296897 http://europepmc.org/abstract/MED/28296897 https://core.ac.uk/display/149581772 https://academic.microsoft.com/#/detail/2687567072 http://europepmc.org/articles/PMC5351862?pdf=render http://europepmc.org/articles/PMC5351862 https://figshare.com/articles/Ice-cover_is_the_principal_driver_of_ecological_change_in_High_Arctic_lakes_and_ponds/4755484 |
long_lat |
ENVELOPE(-74.430,-74.430,78.725,78.725) |
geographic |
Arctic Nunavut Ellesmere Island Canada Pim Island |
geographic_facet |
Arctic Nunavut Ellesmere Island Canada Pim Island |
genre |
Arctic Climate change Ellesmere Island Nunavut Phytoplankton |
genre_facet |
Arctic Climate change Ellesmere Island Nunavut Phytoplankton |
op_source |
10.1371/journal.pone.0172989 2687567072 oai:doaj.org/article:26034e13d4ec460e804dc62783ead5ff 28296897 oai:pubmedcentral.nih.gov:5351862 oai:figshare.com:article/4755484 10|openaire____::081b82f96300b6a6e3d282bad31cb6e2 10|doajarticles::830e55b42c4aaa815c19cfa4f2e5855e 10|openaire____::8ac8380272269217cb09a928c8caa993 10|openaire____::5f532a3fc4f1ea403f37070f59a7a53a 10|driver______::bee53aa31dc2cbb538c10c2b65fa5824 10|openaire____::9e3be59865b2c1c335d32dae2fe7b254 openaire____::1256f046-bf1f-4afc-8b47-d0b147148b18 10|opendoar____::eda80a3d5b344bc40f3bc04f65b7a357 10|opendoar____::8b6dd7db9af49e67306feb59a8bdc52c 10|re3data_____::7980778c78fb4cf0fab13ce2159030dc 10|openaire____::55045bd2a65019fd8e6741a755395c8c 10|openaire____::806360c771262b4d6770e7cdf04b5c5a |
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op_doi |
https://doi.org/10.1371/journal.pone.0172989 |
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PLOS ONE |
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12 |
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fttriple:oai:gotriple.eu:50|dedup_wf_001::4c2c4921cdcf1989136b0c53b1760408 2023-05-15T14:50:59+02:00 Ice-cover is the principal driver of ecological change in High Arctic lakes and ponds John P. Smol Madeline Sugar Katherine Griffiths Neal Michelutti Marianne S. V. Douglas 2017-03-15 https://doi.org/10.1371/journal.pone.0172989 https://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0172989&type=printable https://www.ncbi.nlm.nih.gov/pubmed/28296897 http://europepmc.org/abstract/MED/28296897 https://core.ac.uk/display/149581772 https://academic.microsoft.com/#/detail/2687567072 http://europepmc.org/articles/PMC5351862?pdf=render http://europepmc.org/articles/PMC5351862 https://figshare.com/articles/Ice-cover_is_the_principal_driver_of_ecological_change_in_High_Arctic_lakes_and_ponds/4755484 undefined unknown Public Library of Science (PLoS) http://dx.plos.org/10.1371/journal.pone.0172989 http://dx.doi.org/10.1371/journal.pone.0172989 https://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0172989&type=printable https://dx.plos.org/10.1371/journal.pone.0172989 https://www.ncbi.nlm.nih.gov/pubmed/28296897 http://europepmc.org/abstract/MED/28296897 https://core.ac.uk/display/149581772 https://academic.microsoft.com/#/detail/2687567072 http://europepmc.org/articles/PMC5351862?pdf=render https://dx.doi.org/10.1371/journal.pone.0172989 http://europepmc.org/articles/PMC5351862 https://figshare.com/articles/Ice-cover_is_the_principal_driver_of_ecological_change_in_High_Arctic_lakes_and_ponds/4755484 lic_creative-commons 10.1371/journal.pone.0172989 2687567072 oai:doaj.org/article:26034e13d4ec460e804dc62783ead5ff 28296897 oai:pubmedcentral.nih.gov:5351862 oai:figshare.com:article/4755484 10|openaire____::081b82f96300b6a6e3d282bad31cb6e2 10|doajarticles::830e55b42c4aaa815c19cfa4f2e5855e 10|openaire____::8ac8380272269217cb09a928c8caa993 10|openaire____::5f532a3fc4f1ea403f37070f59a7a53a 10|driver______::bee53aa31dc2cbb538c10c2b65fa5824 10|openaire____::9e3be59865b2c1c335d32dae2fe7b254 openaire____::1256f046-bf1f-4afc-8b47-d0b147148b18 10|opendoar____::eda80a3d5b344bc40f3bc04f65b7a357 10|opendoar____::8b6dd7db9af49e67306feb59a8bdc52c 10|re3data_____::7980778c78fb4cf0fab13ce2159030dc 10|openaire____::55045bd2a65019fd8e6741a755395c8c 10|openaire____::806360c771262b4d6770e7cdf04b5c5a Research Article Earth Sciences Marine and Aquatic Sciences Bodies of Water Ponds Lakes Ecology and Environmental Sciences Aquatic Environments Freshwater Environments Biology and Life Sciences Organisms Plants Algae Phytoplankton Diatoms Animals Invertebrates Plankton Geology Petrology Sedimentary Geology Atmospheric Science Climatology Social Sciences Archaeology Archaeological Dating Radioactive Carbon Dating Research and Analysis Methods Chemical Characterization Isotope Analysis Paleoclimatology Paleontology Nonvascular Plants Mosses Evolutionary Biology Marine Biology Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified epiphytic species High Arctic diatom assemblage responses Condition 2 assemblages oasis climate shift novel growth forms epilithic diatom assemblage Condition 1 Condition 2 High Arctic lakes Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2017 fttriple https://doi.org/10.1371/journal.pone.0172989 2023-01-22T16:41:12Z Recent climate change has been especially pronounced in the High Arctic, however, the responses of aquatic biota, such as diatoms, can be modified by site-specific environmental characteristics. To assess if climate-mediated ice cover changes affect the diatom response to climate, we used paleolimnological techniques to examine shifts in diatom assemblages from ten High Arctic lakes and ponds from Ellesmere Island and nearby Pim Island (Nunavut, Canada). The sites were divided a priori into four groups (“warm”, “cool”, “cold”, and “oasis”) based on local elevation and microclimatic differences that result in differing lengths of the ice-free season, as well as about three decades of personal observations. We characterized the species changes as a shift from Condition 1 (i.e. a generally low diversity, predominantly epipelic and epilithic diatom assemblage) to Condition 2 (i.e. a typically more diverse and ecologically complex assemblage with an increasing proportion of epiphytic species). This shift from Condition 1 to Condition 2 was a consistent pattern recorded across the sites that experienced a change in ice cover with warming. The “warm” sites are amongst the first to lose their ice covers in summer and recorded the earliest and highest magnitude changes. The “cool” sites also exhibited a shift from Condition 1 to Condition 2, but, as predicted, the timing of the response lagged the “warm” sites. Meanwhile some of the “cold” sites, which until recently still retained an ice raft in summer, only exhibited this shift in the upper-most sediments. The warmer “oasis” ponds likely supported aquatic vegetation throughout their records. Consequently, the diatoms of the “oasis” sites were characterized as high-diversity, Condition 2 assemblages throughout the record. Our results support the hypothesis that the length of the ice-free season is the principal driver of diatom assemblage responses to climate in the High Arctic, largely driven by the establishment of new aquatic habitats, resulting in increased ... Article in Journal/Newspaper Arctic Climate change Ellesmere Island Nunavut Phytoplankton Unknown Arctic Nunavut Ellesmere Island Canada Pim Island ENVELOPE(-74.430,-74.430,78.725,78.725) PLOS ONE 12 3 e0172989 |