Past carbonate preservation events in the deep Southeast Atlantic Ocean (Cape Basin) and their implications for Atlantic overturning dynamics and marine carbon cycling ...

Micropaleontological and geochemical analyses reveal distinct millennial-scale increases in carbonate preservation in the deep Southeast Atlantic (Cape Basin) during strong and prolonged Greenland interstadials that are superimposed on long-term (orbital-scale) changes in carbonate burial. These dat...

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Main Authors: Gottschalk, Julia, Hodell, David, Skinner, LC, Crowhurst, Simon, Jaccard, Samuel, Charles, Christopher
Format: Article in Journal/Newspaper
Language:English
Published: Wiley-Blackwell 2018
Subjects:
XRF
Online Access:https://dx.doi.org/10.17863/cam.30877
https://www.repository.cam.ac.uk/handle/1810/283514
id ftdatacite:10.17863/cam.30877
record_format openpolar
spelling ftdatacite:10.17863/cam.30877 2024-02-04T10:00:43+01:00 Past carbonate preservation events in the deep Southeast Atlantic Ocean (Cape Basin) and their implications for Atlantic overturning dynamics and marine carbon cycling ... Gottschalk, Julia Hodell, David Skinner, LC Crowhurst, Simon Jaccard, Samuel Charles, Christopher 2018 https://dx.doi.org/10.17863/cam.30877 https://www.repository.cam.ac.uk/handle/1810/283514 en eng Wiley-Blackwell Southern Ocean carbonate preservation carbonate compensation glacial cycles AMOC XRF Article ScholarlyArticle JournalArticle article-journal 2018 ftdatacite https://doi.org/10.17863/cam.30877 2024-01-05T09:28:50Z Micropaleontological and geochemical analyses reveal distinct millennial-scale increases in carbonate preservation in the deep Southeast Atlantic (Cape Basin) during strong and prolonged Greenland interstadials that are superimposed on long-term (orbital-scale) changes in carbonate burial. These data suggest carbonate oversaturation of the deep Atlantic and a strengthened Atlantic Meridional Overturning Circulation (AMOC) during the most intense Greenland interstadials. However, proxy evidence from outside the Cape Basin indicate that AMOC changes also occurred during weaker and shorter Greenland interstadials. Here we revisit the link between AMOC dynamics and carbonate saturation in the deep Cape Basin over the last 400 kyr (sediment cores TN057-21, TN057-10 and ODP Site 1089) by reconstructing centennial changes in carbonate preservation using mm-scale X-ray fluorescence (XRF) scanning data. We observe close agreement between variations in XRF Ca/Ti, sedimentary carbonate content and foraminiferal shell ... Article in Journal/Newspaper Greenland Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) Greenland Southern Ocean
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Southern Ocean
carbonate preservation
carbonate compensation
glacial cycles
AMOC
XRF
spellingShingle Southern Ocean
carbonate preservation
carbonate compensation
glacial cycles
AMOC
XRF
Gottschalk, Julia
Hodell, David
Skinner, LC
Crowhurst, Simon
Jaccard, Samuel
Charles, Christopher
Past carbonate preservation events in the deep Southeast Atlantic Ocean (Cape Basin) and their implications for Atlantic overturning dynamics and marine carbon cycling ...
topic_facet Southern Ocean
carbonate preservation
carbonate compensation
glacial cycles
AMOC
XRF
description Micropaleontological and geochemical analyses reveal distinct millennial-scale increases in carbonate preservation in the deep Southeast Atlantic (Cape Basin) during strong and prolonged Greenland interstadials that are superimposed on long-term (orbital-scale) changes in carbonate burial. These data suggest carbonate oversaturation of the deep Atlantic and a strengthened Atlantic Meridional Overturning Circulation (AMOC) during the most intense Greenland interstadials. However, proxy evidence from outside the Cape Basin indicate that AMOC changes also occurred during weaker and shorter Greenland interstadials. Here we revisit the link between AMOC dynamics and carbonate saturation in the deep Cape Basin over the last 400 kyr (sediment cores TN057-21, TN057-10 and ODP Site 1089) by reconstructing centennial changes in carbonate preservation using mm-scale X-ray fluorescence (XRF) scanning data. We observe close agreement between variations in XRF Ca/Ti, sedimentary carbonate content and foraminiferal shell ...
format Article in Journal/Newspaper
author Gottschalk, Julia
Hodell, David
Skinner, LC
Crowhurst, Simon
Jaccard, Samuel
Charles, Christopher
author_facet Gottschalk, Julia
Hodell, David
Skinner, LC
Crowhurst, Simon
Jaccard, Samuel
Charles, Christopher
author_sort Gottschalk, Julia
title Past carbonate preservation events in the deep Southeast Atlantic Ocean (Cape Basin) and their implications for Atlantic overturning dynamics and marine carbon cycling ...
title_short Past carbonate preservation events in the deep Southeast Atlantic Ocean (Cape Basin) and their implications for Atlantic overturning dynamics and marine carbon cycling ...
title_full Past carbonate preservation events in the deep Southeast Atlantic Ocean (Cape Basin) and their implications for Atlantic overturning dynamics and marine carbon cycling ...
title_fullStr Past carbonate preservation events in the deep Southeast Atlantic Ocean (Cape Basin) and their implications for Atlantic overturning dynamics and marine carbon cycling ...
title_full_unstemmed Past carbonate preservation events in the deep Southeast Atlantic Ocean (Cape Basin) and their implications for Atlantic overturning dynamics and marine carbon cycling ...
title_sort past carbonate preservation events in the deep southeast atlantic ocean (cape basin) and their implications for atlantic overturning dynamics and marine carbon cycling ...
publisher Wiley-Blackwell
publishDate 2018
url https://dx.doi.org/10.17863/cam.30877
https://www.repository.cam.ac.uk/handle/1810/283514
geographic Greenland
Southern Ocean
geographic_facet Greenland
Southern Ocean
genre Greenland
Southern Ocean
genre_facet Greenland
Southern Ocean
op_doi https://doi.org/10.17863/cam.30877
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