The Arctic Ocean fixed nitrogen cycle in past climates: Insights from foraminifer-bound nitrogen isotopes
The dramatic loss of summer sea-ice impacts Arctic Ocean biological productivity through poorly understood pathways. While sea-ice loss alleviates light limitation, productivity within the future seasonally ice-free Arctic Ocean will likely be limited by the supply of biologically available (“fixed”...
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ftunivbruxelles:oai:dipot.ulb.ac.be:2013/299533 2023-05-15T14:32:25+02:00 The Arctic Ocean fixed nitrogen cycle in past climates: Insights from foraminifer-bound nitrogen isotopes Farmer, Jesse Sigman, Daniel M Granger, Julie Fripiat, François AGU Fall meeting (2019: San Francisco) 2019-12-11 No full-text files http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/299533 fr fre http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/299533 Sciences de la terre et du cosmos info:eu-repo/semantics/conferenceContribution info:ulb-repo/semantics/conferenceContribution info:ulb-repo/semantics/openurl/document 2019 ftunivbruxelles 2022-06-12T21:55:22Z The dramatic loss of summer sea-ice impacts Arctic Ocean biological productivity through poorly understood pathways. While sea-ice loss alleviates light limitation, productivity within the future seasonally ice-free Arctic Ocean will likely be limited by the supply of biologically available (“fixed”) nitrogen. Although the Arctic Ocean has experienced past intervals of reduced sea-ice extent and warmer-than-present conditions, little is known about Arctic Ocean nutrient cycling outside of recent conditions. Here we investigate changes in nitrate supply and utilization in the surface Arctic Ocean over the last 40 kyr using measurements of nitrogen isotopes within the organic matrix of planktic foraminifera (FB-δ15N). Preliminary results show a dramatic, 4‰ FB-δ15N increase in the western Arctic Ocean (Mendeleev Ridge) between 12 and 10 ka, synchronous with postglacial opening of the Bering Strait. We interpret this FB-δ15N increase to reflect the rapid resumption of Pacific water nitrate inflow, with associated influences on shelf denitrification and surface ocean nutrient consumption following Bering Strait opening. A corresponding record from the central Arctic Ocean (Lomonosov Ridge) shows minor FB-δ15N variations since 14 ka, indicating that central Arctic productivity was sustained by Atlantic-sourced nitrate throughout this time. These results suggest that shelf denitrification and surface ocean nitrate consumption in the western Arctic is tightly linked to Pacific water inflow. We will discuss opportunities to apply FB-δ15N to Arctic sediments from past warm climates as potential constraints for the future Arctic Ocean fixed nitrogen cycle. info:eu-repo/semantics/nonPublished Conference Object Arctic Arctic Ocean Bering Strait Foraminifera* Lomonosov Ridge Sea ice DI-fusion : dépôt institutionnel de l'Université libre de Bruxelles (ULB) Arctic Arctic Ocean Bering Strait Pacific |
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Open Polar |
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DI-fusion : dépôt institutionnel de l'Université libre de Bruxelles (ULB) |
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ftunivbruxelles |
language |
French |
topic |
Sciences de la terre et du cosmos |
spellingShingle |
Sciences de la terre et du cosmos Farmer, Jesse Sigman, Daniel M Granger, Julie Fripiat, François The Arctic Ocean fixed nitrogen cycle in past climates: Insights from foraminifer-bound nitrogen isotopes |
topic_facet |
Sciences de la terre et du cosmos |
description |
The dramatic loss of summer sea-ice impacts Arctic Ocean biological productivity through poorly understood pathways. While sea-ice loss alleviates light limitation, productivity within the future seasonally ice-free Arctic Ocean will likely be limited by the supply of biologically available (“fixed”) nitrogen. Although the Arctic Ocean has experienced past intervals of reduced sea-ice extent and warmer-than-present conditions, little is known about Arctic Ocean nutrient cycling outside of recent conditions. Here we investigate changes in nitrate supply and utilization in the surface Arctic Ocean over the last 40 kyr using measurements of nitrogen isotopes within the organic matrix of planktic foraminifera (FB-δ15N). Preliminary results show a dramatic, 4‰ FB-δ15N increase in the western Arctic Ocean (Mendeleev Ridge) between 12 and 10 ka, synchronous with postglacial opening of the Bering Strait. We interpret this FB-δ15N increase to reflect the rapid resumption of Pacific water nitrate inflow, with associated influences on shelf denitrification and surface ocean nutrient consumption following Bering Strait opening. A corresponding record from the central Arctic Ocean (Lomonosov Ridge) shows minor FB-δ15N variations since 14 ka, indicating that central Arctic productivity was sustained by Atlantic-sourced nitrate throughout this time. These results suggest that shelf denitrification and surface ocean nitrate consumption in the western Arctic is tightly linked to Pacific water inflow. We will discuss opportunities to apply FB-δ15N to Arctic sediments from past warm climates as potential constraints for the future Arctic Ocean fixed nitrogen cycle. info:eu-repo/semantics/nonPublished |
author2 |
AGU Fall meeting (2019: San Francisco) |
format |
Conference Object |
author |
Farmer, Jesse Sigman, Daniel M Granger, Julie Fripiat, François |
author_facet |
Farmer, Jesse Sigman, Daniel M Granger, Julie Fripiat, François |
author_sort |
Farmer, Jesse |
title |
The Arctic Ocean fixed nitrogen cycle in past climates: Insights from foraminifer-bound nitrogen isotopes |
title_short |
The Arctic Ocean fixed nitrogen cycle in past climates: Insights from foraminifer-bound nitrogen isotopes |
title_full |
The Arctic Ocean fixed nitrogen cycle in past climates: Insights from foraminifer-bound nitrogen isotopes |
title_fullStr |
The Arctic Ocean fixed nitrogen cycle in past climates: Insights from foraminifer-bound nitrogen isotopes |
title_full_unstemmed |
The Arctic Ocean fixed nitrogen cycle in past climates: Insights from foraminifer-bound nitrogen isotopes |
title_sort |
arctic ocean fixed nitrogen cycle in past climates: insights from foraminifer-bound nitrogen isotopes |
publishDate |
2019 |
url |
http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/299533 |
geographic |
Arctic Arctic Ocean Bering Strait Pacific |
geographic_facet |
Arctic Arctic Ocean Bering Strait Pacific |
genre |
Arctic Arctic Ocean Bering Strait Foraminifera* Lomonosov Ridge Sea ice |
genre_facet |
Arctic Arctic Ocean Bering Strait Foraminifera* Lomonosov Ridge Sea ice |
op_relation |
http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/299533 |
_version_ |
1766305827698769920 |