Impact of freshwater runoff from the southwest Greenland Ice Sheet on fjord productivity since the late 19th century
Climate warming and the resulting acceleration of freshwater discharge from the Greenland Ice Sheet are impacting Arctic marine coastal ecosystems, with implications for their biological productivity. To accurately project the future of coastal ecosystems and place recent trends into perspective, pa...
Published in: | The Cryosphere |
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Online Access: | https://doi.org/10.5194/tc-16-2471-2022 https://tc.copernicus.org/articles/16/2471/2022/ |
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ftcopernicus:oai:publications.copernicus.org:tc99790 2023-05-15T15:00:54+02:00 Impact of freshwater runoff from the southwest Greenland Ice Sheet on fjord productivity since the late 19th century Oksman, Mimmi Kvorning, Anna Bang Larsen, Signe Hillerup Kjeldsen, Kristian Kjellerup Mankoff, Kenneth David Colgan, William Andersen, Thorbjørn Joest Nørgaard-Pedersen, Niels Seidenkrantz, Marit-Solveig Mikkelsen, Naja Ribeiro, Sofia 2022-06-24 application/pdf https://doi.org/10.5194/tc-16-2471-2022 https://tc.copernicus.org/articles/16/2471/2022/ eng eng doi:10.5194/tc-16-2471-2022 https://tc.copernicus.org/articles/16/2471/2022/ eISSN: 1994-0424 Text 2022 ftcopernicus https://doi.org/10.5194/tc-16-2471-2022 2022-06-27T16:22:42Z Climate warming and the resulting acceleration of freshwater discharge from the Greenland Ice Sheet are impacting Arctic marine coastal ecosystems, with implications for their biological productivity. To accurately project the future of coastal ecosystems and place recent trends into perspective, palaeo-records are essential. Here, we show runoff estimates from the late 19th century to the present day for a large sub-Arctic fjord system (Nuup Kangerlua, southwest Greenland) influenced by both marine- and land-terminating glaciers. We followed a multiproxy approach to reconstruct spatial and temporal trends in primary production from four sediment core records, including diatom fluxes and assemblage composition changes and biogeochemical and sedimentological proxies (total organic carbon, nitrogen, <math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><mi mathvariant="normal">C</mi><mo>/</mo><mi mathvariant="normal">N</mi></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="24pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="f135772273124e8de131c1d3d27c70de"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-2471-2022-ie00001.svg" width="24pt" height="14pt" src="tc-16-2471-2022-ie00001.png"/></svg:svg> ratio, biogenic silica, δ 13 C, δ 15 N, and grain-size distribution). We show that an abrupt increase in freshwater runoff in the mid-1990s was reflected by a 3-fold increase in biogenic silica fluxes in the glacier-proximal area of the fjord. In addition to increased productivity, freshwater runoff modulates the diatom assemblages and drives the dynamics and magnitude of the diatom spring bloom. Our records indicate that marine productivity is higher today than it has been at any point since the late 19th century and suggest that increased mass loss of the Greenland Ice Sheet may continue promoting high ... Text Arctic glacier Greenland Ice Sheet Copernicus Publications: E-Journals Arctic Greenland The Cryosphere 16 6 2471 2491 |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
Climate warming and the resulting acceleration of freshwater discharge from the Greenland Ice Sheet are impacting Arctic marine coastal ecosystems, with implications for their biological productivity. To accurately project the future of coastal ecosystems and place recent trends into perspective, palaeo-records are essential. Here, we show runoff estimates from the late 19th century to the present day for a large sub-Arctic fjord system (Nuup Kangerlua, southwest Greenland) influenced by both marine- and land-terminating glaciers. We followed a multiproxy approach to reconstruct spatial and temporal trends in primary production from four sediment core records, including diatom fluxes and assemblage composition changes and biogeochemical and sedimentological proxies (total organic carbon, nitrogen, <math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><mi mathvariant="normal">C</mi><mo>/</mo><mi mathvariant="normal">N</mi></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="24pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="f135772273124e8de131c1d3d27c70de"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-2471-2022-ie00001.svg" width="24pt" height="14pt" src="tc-16-2471-2022-ie00001.png"/></svg:svg> ratio, biogenic silica, δ 13 C, δ 15 N, and grain-size distribution). We show that an abrupt increase in freshwater runoff in the mid-1990s was reflected by a 3-fold increase in biogenic silica fluxes in the glacier-proximal area of the fjord. In addition to increased productivity, freshwater runoff modulates the diatom assemblages and drives the dynamics and magnitude of the diatom spring bloom. Our records indicate that marine productivity is higher today than it has been at any point since the late 19th century and suggest that increased mass loss of the Greenland Ice Sheet may continue promoting high ... |
format |
Text |
author |
Oksman, Mimmi Kvorning, Anna Bang Larsen, Signe Hillerup Kjeldsen, Kristian Kjellerup Mankoff, Kenneth David Colgan, William Andersen, Thorbjørn Joest Nørgaard-Pedersen, Niels Seidenkrantz, Marit-Solveig Mikkelsen, Naja Ribeiro, Sofia |
spellingShingle |
Oksman, Mimmi Kvorning, Anna Bang Larsen, Signe Hillerup Kjeldsen, Kristian Kjellerup Mankoff, Kenneth David Colgan, William Andersen, Thorbjørn Joest Nørgaard-Pedersen, Niels Seidenkrantz, Marit-Solveig Mikkelsen, Naja Ribeiro, Sofia Impact of freshwater runoff from the southwest Greenland Ice Sheet on fjord productivity since the late 19th century |
author_facet |
Oksman, Mimmi Kvorning, Anna Bang Larsen, Signe Hillerup Kjeldsen, Kristian Kjellerup Mankoff, Kenneth David Colgan, William Andersen, Thorbjørn Joest Nørgaard-Pedersen, Niels Seidenkrantz, Marit-Solveig Mikkelsen, Naja Ribeiro, Sofia |
author_sort |
Oksman, Mimmi |
title |
Impact of freshwater runoff from the southwest Greenland Ice Sheet on fjord productivity since the late 19th century |
title_short |
Impact of freshwater runoff from the southwest Greenland Ice Sheet on fjord productivity since the late 19th century |
title_full |
Impact of freshwater runoff from the southwest Greenland Ice Sheet on fjord productivity since the late 19th century |
title_fullStr |
Impact of freshwater runoff from the southwest Greenland Ice Sheet on fjord productivity since the late 19th century |
title_full_unstemmed |
Impact of freshwater runoff from the southwest Greenland Ice Sheet on fjord productivity since the late 19th century |
title_sort |
impact of freshwater runoff from the southwest greenland ice sheet on fjord productivity since the late 19th century |
publishDate |
2022 |
url |
https://doi.org/10.5194/tc-16-2471-2022 https://tc.copernicus.org/articles/16/2471/2022/ |
geographic |
Arctic Greenland |
geographic_facet |
Arctic Greenland |
genre |
Arctic glacier Greenland Ice Sheet |
genre_facet |
Arctic glacier Greenland Ice Sheet |
op_source |
eISSN: 1994-0424 |
op_relation |
doi:10.5194/tc-16-2471-2022 https://tc.copernicus.org/articles/16/2471/2022/ |
op_doi |
https://doi.org/10.5194/tc-16-2471-2022 |
container_title |
The Cryosphere |
container_volume |
16 |
container_issue |
6 |
container_start_page |
2471 |
op_container_end_page |
2491 |
_version_ |
1766332956008251392 |