Twentieth century δ 13 C variability in surface water dissolved inorganic carbon recorded by coralline algae in the northern North Pacific Ocean and the Bering Sea
The oxygen isotopic composition and Mg/Ca ratios in the skeletons of long-lived coralline algae record ambient seawater temperature over time. Similarly, the carbon isotopic composition in the skeletons record δ 13 C values of ambient seawater dissolved inorganic carbon. Here, we measured δ 13 C in...
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ftdoajarticles:oai:doaj.org/article:a39afcdff8f04221892c3c109ac970eb 2023-05-15T13:14:54+02:00 Twentieth century δ 13 C variability in surface water dissolved inorganic carbon recorded by coralline algae in the northern North Pacific Ocean and the Bering Sea W. Adey P. Lebednik S. Hetzinger R. S. Steneck U. G. Wortmann J. Halfar B. Williams M. Joachimski 2011-01-01T00:00:00Z https://doi.org/10.5194/bg-8-165-2011 https://doaj.org/article/a39afcdff8f04221892c3c109ac970eb EN eng Copernicus Publications http://www.biogeosciences.net/8/165/2011/bg-8-165-2011.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-8-165-2011 1726-4170 1726-4189 https://doaj.org/article/a39afcdff8f04221892c3c109ac970eb Biogeosciences, Vol 8, Iss 1, Pp 165-174 (2011) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2011 ftdoajarticles https://doi.org/10.5194/bg-8-165-2011 2022-12-31T03:18:59Z The oxygen isotopic composition and Mg/Ca ratios in the skeletons of long-lived coralline algae record ambient seawater temperature over time. Similarly, the carbon isotopic composition in the skeletons record δ 13 C values of ambient seawater dissolved inorganic carbon. Here, we measured δ 13 C in the coralline alga Clathromorphum nereostratum to test the feasibility of reconstructing the intrusion of anthropogenic CO 2 into the northern North Pacific Ocean and Bering Sea. The δ 13 C was measured in the high Mg-calcite skeleton of three C. nereostratum specimens from two islands 500 km apart in the Aleutian archipelago. In the records spanning 1887 to 2003, the average decadal rate of decline in δ 13 C values increased from 0.03‰ yr −1 in the 1960s to 0.095‰ yr −1 in the 1990s, which was higher than expected due to solely the δ 13 C-Suess effect. Deeper water in this region exhibits higher concentrations of CO 2 and low δ 13 C values. Transport of deeper water into surface water (i.e., upwelling) increases when the Aleutian Low is intensified. We hypothesized that the acceleration of the δ 13 C decline may result from increased upwelling from the 1960s to 1990s, which in turn was driven by increased intensity of the Aleutian Low. Detrended δ 13 C records also varied on 4–7 year and bidecadal timescales supporting an atmospheric teleconnection of tropical climate patterns to the northern North Pacific Ocean and Bering Sea manifested as changes in upwelling. Article in Journal/Newspaper aleutian low Bering Sea Directory of Open Access Journals: DOAJ Articles Bering Sea Pacific Biogeosciences 8 1 165 174 |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
spellingShingle |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 W. Adey P. Lebednik S. Hetzinger R. S. Steneck U. G. Wortmann J. Halfar B. Williams M. Joachimski Twentieth century δ 13 C variability in surface water dissolved inorganic carbon recorded by coralline algae in the northern North Pacific Ocean and the Bering Sea |
topic_facet |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
description |
The oxygen isotopic composition and Mg/Ca ratios in the skeletons of long-lived coralline algae record ambient seawater temperature over time. Similarly, the carbon isotopic composition in the skeletons record δ 13 C values of ambient seawater dissolved inorganic carbon. Here, we measured δ 13 C in the coralline alga Clathromorphum nereostratum to test the feasibility of reconstructing the intrusion of anthropogenic CO 2 into the northern North Pacific Ocean and Bering Sea. The δ 13 C was measured in the high Mg-calcite skeleton of three C. nereostratum specimens from two islands 500 km apart in the Aleutian archipelago. In the records spanning 1887 to 2003, the average decadal rate of decline in δ 13 C values increased from 0.03‰ yr −1 in the 1960s to 0.095‰ yr −1 in the 1990s, which was higher than expected due to solely the δ 13 C-Suess effect. Deeper water in this region exhibits higher concentrations of CO 2 and low δ 13 C values. Transport of deeper water into surface water (i.e., upwelling) increases when the Aleutian Low is intensified. We hypothesized that the acceleration of the δ 13 C decline may result from increased upwelling from the 1960s to 1990s, which in turn was driven by increased intensity of the Aleutian Low. Detrended δ 13 C records also varied on 4–7 year and bidecadal timescales supporting an atmospheric teleconnection of tropical climate patterns to the northern North Pacific Ocean and Bering Sea manifested as changes in upwelling. |
format |
Article in Journal/Newspaper |
author |
W. Adey P. Lebednik S. Hetzinger R. S. Steneck U. G. Wortmann J. Halfar B. Williams M. Joachimski |
author_facet |
W. Adey P. Lebednik S. Hetzinger R. S. Steneck U. G. Wortmann J. Halfar B. Williams M. Joachimski |
author_sort |
W. Adey |
title |
Twentieth century δ 13 C variability in surface water dissolved inorganic carbon recorded by coralline algae in the northern North Pacific Ocean and the Bering Sea |
title_short |
Twentieth century δ 13 C variability in surface water dissolved inorganic carbon recorded by coralline algae in the northern North Pacific Ocean and the Bering Sea |
title_full |
Twentieth century δ 13 C variability in surface water dissolved inorganic carbon recorded by coralline algae in the northern North Pacific Ocean and the Bering Sea |
title_fullStr |
Twentieth century δ 13 C variability in surface water dissolved inorganic carbon recorded by coralline algae in the northern North Pacific Ocean and the Bering Sea |
title_full_unstemmed |
Twentieth century δ 13 C variability in surface water dissolved inorganic carbon recorded by coralline algae in the northern North Pacific Ocean and the Bering Sea |
title_sort |
twentieth century δ 13 c variability in surface water dissolved inorganic carbon recorded by coralline algae in the northern north pacific ocean and the bering sea |
publisher |
Copernicus Publications |
publishDate |
2011 |
url |
https://doi.org/10.5194/bg-8-165-2011 https://doaj.org/article/a39afcdff8f04221892c3c109ac970eb |
geographic |
Bering Sea Pacific |
geographic_facet |
Bering Sea Pacific |
genre |
aleutian low Bering Sea |
genre_facet |
aleutian low Bering Sea |
op_source |
Biogeosciences, Vol 8, Iss 1, Pp 165-174 (2011) |
op_relation |
http://www.biogeosciences.net/8/165/2011/bg-8-165-2011.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-8-165-2011 1726-4170 1726-4189 https://doaj.org/article/a39afcdff8f04221892c3c109ac970eb |
op_doi |
https://doi.org/10.5194/bg-8-165-2011 |
container_title |
Biogeosciences |
container_volume |
8 |
container_issue |
1 |
container_start_page |
165 |
op_container_end_page |
174 |
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1766266031753396224 |