Group 2i Isochrysidales produce characteristic alkenones reflecting sea ice distribution
Abstract Alkenones are biomarkers produced solely by algae in the order Isochrysidales that have been used to reconstruct sea surface temperature (SST) since the 1980s. However, alkenone-based SST reconstructions in the northern high latitude oceans show significant bias towards warmer temperatures...
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2021
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Online Access: | http://dx.doi.org/10.1038/s41467-020-20187-z http://www.nature.com/articles/s41467-020-20187-z.pdf http://www.nature.com/articles/s41467-020-20187-z |
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crspringernat:10.1038/s41467-020-20187-z 2023-05-15T16:29:55+02:00 Group 2i Isochrysidales produce characteristic alkenones reflecting sea ice distribution Wang, Karen Jiaxi Huang, Yongsong Majaneva, Markus Belt, Simon T. Liao, Sian Novak, Joseph Kartzinel, Tyler R. Herbert, Timothy D. Richter, Nora Cabedo-Sanz, Patricia Institute at Brown for Environment and Society National Science Foundation 2021 http://dx.doi.org/10.1038/s41467-020-20187-z http://www.nature.com/articles/s41467-020-20187-z.pdf http://www.nature.com/articles/s41467-020-20187-z en eng Springer Science and Business Media LLC https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 CC-BY Nature Communications volume 12, issue 1 ISSN 2041-1723 General Physics and Astronomy General Biochemistry, Genetics and Molecular Biology General Chemistry journal-article 2021 crspringernat https://doi.org/10.1038/s41467-020-20187-z 2022-01-14T15:36:47Z Abstract Alkenones are biomarkers produced solely by algae in the order Isochrysidales that have been used to reconstruct sea surface temperature (SST) since the 1980s. However, alkenone-based SST reconstructions in the northern high latitude oceans show significant bias towards warmer temperatures in core-tops, diverge from other SST proxies in down core records, and are often accompanied by anomalously high relative abundance of the C 37 tetra-unsaturated methyl alkenone (%C 37:4 ). Elevated %C 37:4 is widely interpreted as an indicator of low sea surface salinity from polar water masses, but its biological source has thus far remained elusive. Here we identify a lineage of Isochrysidales that is responsible for elevated C 37:4 methyl alkenone in the northern high latitude oceans through next-generation sequencing and lab-culture experiments. This Isochrysidales lineage co-occurs widely with sea ice in marine environments and is distinct from other known marine alkenone-producers, namely Emiliania huxleyi and Gephyrocapsa oceanica . More importantly, the %C 37:4 in seawater filtered particulate organic matter and surface sediments is significantly correlated with annual mean sea ice concentrations. In sediment cores from the Svalbard region, the %C 37:4 concentration aligns with the Greenland temperature record and other qualitative regional sea ice records spanning the past 14 kyrs, reflecting sea ice concentrations quantitatively. Our findings imply that %C 37:4 is a powerful proxy for reconstructing sea ice conditions in the high latitude oceans on thousand- and, potentially, on million-year timescales. Article in Journal/Newspaper Greenland Sea ice Svalbard Springer Nature (via Crossref) Greenland Svalbard Nature Communications 12 1 |
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Open Polar |
collection |
Springer Nature (via Crossref) |
op_collection_id |
crspringernat |
language |
English |
topic |
General Physics and Astronomy General Biochemistry, Genetics and Molecular Biology General Chemistry |
spellingShingle |
General Physics and Astronomy General Biochemistry, Genetics and Molecular Biology General Chemistry Wang, Karen Jiaxi Huang, Yongsong Majaneva, Markus Belt, Simon T. Liao, Sian Novak, Joseph Kartzinel, Tyler R. Herbert, Timothy D. Richter, Nora Cabedo-Sanz, Patricia Group 2i Isochrysidales produce characteristic alkenones reflecting sea ice distribution |
topic_facet |
General Physics and Astronomy General Biochemistry, Genetics and Molecular Biology General Chemistry |
description |
Abstract Alkenones are biomarkers produced solely by algae in the order Isochrysidales that have been used to reconstruct sea surface temperature (SST) since the 1980s. However, alkenone-based SST reconstructions in the northern high latitude oceans show significant bias towards warmer temperatures in core-tops, diverge from other SST proxies in down core records, and are often accompanied by anomalously high relative abundance of the C 37 tetra-unsaturated methyl alkenone (%C 37:4 ). Elevated %C 37:4 is widely interpreted as an indicator of low sea surface salinity from polar water masses, but its biological source has thus far remained elusive. Here we identify a lineage of Isochrysidales that is responsible for elevated C 37:4 methyl alkenone in the northern high latitude oceans through next-generation sequencing and lab-culture experiments. This Isochrysidales lineage co-occurs widely with sea ice in marine environments and is distinct from other known marine alkenone-producers, namely Emiliania huxleyi and Gephyrocapsa oceanica . More importantly, the %C 37:4 in seawater filtered particulate organic matter and surface sediments is significantly correlated with annual mean sea ice concentrations. In sediment cores from the Svalbard region, the %C 37:4 concentration aligns with the Greenland temperature record and other qualitative regional sea ice records spanning the past 14 kyrs, reflecting sea ice concentrations quantitatively. Our findings imply that %C 37:4 is a powerful proxy for reconstructing sea ice conditions in the high latitude oceans on thousand- and, potentially, on million-year timescales. |
author2 |
Institute at Brown for Environment and Society National Science Foundation |
format |
Article in Journal/Newspaper |
author |
Wang, Karen Jiaxi Huang, Yongsong Majaneva, Markus Belt, Simon T. Liao, Sian Novak, Joseph Kartzinel, Tyler R. Herbert, Timothy D. Richter, Nora Cabedo-Sanz, Patricia |
author_facet |
Wang, Karen Jiaxi Huang, Yongsong Majaneva, Markus Belt, Simon T. Liao, Sian Novak, Joseph Kartzinel, Tyler R. Herbert, Timothy D. Richter, Nora Cabedo-Sanz, Patricia |
author_sort |
Wang, Karen Jiaxi |
title |
Group 2i Isochrysidales produce characteristic alkenones reflecting sea ice distribution |
title_short |
Group 2i Isochrysidales produce characteristic alkenones reflecting sea ice distribution |
title_full |
Group 2i Isochrysidales produce characteristic alkenones reflecting sea ice distribution |
title_fullStr |
Group 2i Isochrysidales produce characteristic alkenones reflecting sea ice distribution |
title_full_unstemmed |
Group 2i Isochrysidales produce characteristic alkenones reflecting sea ice distribution |
title_sort |
group 2i isochrysidales produce characteristic alkenones reflecting sea ice distribution |
publisher |
Springer Science and Business Media LLC |
publishDate |
2021 |
url |
http://dx.doi.org/10.1038/s41467-020-20187-z http://www.nature.com/articles/s41467-020-20187-z.pdf http://www.nature.com/articles/s41467-020-20187-z |
geographic |
Greenland Svalbard |
geographic_facet |
Greenland Svalbard |
genre |
Greenland Sea ice Svalbard |
genre_facet |
Greenland Sea ice Svalbard |
op_source |
Nature Communications volume 12, issue 1 ISSN 2041-1723 |
op_rights |
https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1038/s41467-020-20187-z |
container_title |
Nature Communications |
container_volume |
12 |
container_issue |
1 |
_version_ |
1766019629030834176 |