Natural variation of pelagic carbonate production during Cenozoic warm periods ...
The biological carbon uptake, called biological compensation, have been shown to have a huge potential to affect the capacity of the ocean to absorb (anthropogenic) carbon dioxide, and so equilibrate the global carbon budget and hence climate. Since the pelagic calcite flux is made of two fundamenta...
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Online Access: | https://dx.doi.org/10.26092/elib/2651 https://media.suub.uni-bremen.de/handle/elib/7427 |
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ftdatacite:10.26092/elib/2651 2023-12-31T10:22:11+01:00 Natural variation of pelagic carbonate production during Cenozoic warm periods ... CORNUAULT, Pauline 2023 https://dx.doi.org/10.26092/elib/2651 https://media.suub.uni-bremen.de/handle/elib/7427 en eng Universität Bremen https://dx.doi.org/10.1594/pangaea.945848 https://dx.doi.org/10.1594/pangaea.945773 https://dx.doi.org/10.1594/pangaea.945812 https://dx.doi.org/10.1594/pangaea.945789 https://dx.doi.org/10.1594/pangaea.945707 Creative Commons Attribution 4.0 International CC BY 4.0 (Attribution) https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 climate variability carbonate production paleoceanography warm climates microfossils Cenozoic 550 thesis Dissertation Other Thesis 2023 ftdatacite https://doi.org/10.26092/elib/265110.1594/pangaea.94584810.1594/pangaea.94577310.1594/pangaea.94581210.1594/pangaea.94578910.1594/pangaea.945707 2023-12-01T11:28:54Z The biological carbon uptake, called biological compensation, have been shown to have a huge potential to affect the capacity of the ocean to absorb (anthropogenic) carbon dioxide, and so equilibrate the global carbon budget and hence climate. Since the pelagic calcite flux is made of two fundamentally different components, coccolithophore algae and planktonic foraminifera, understanding of the process of biological compensation requires knowledge of variability of their relative contribution to the total pelagic calcite flux. The aspects of the pelagic carbonate production that have changed through time and the mechanisms explaining the observed carbonate flux variability remain, despite their importance, largely unconstrained. In order to evaluate the orbital and long geological time scale variability of the pelagic carbonate production, I generated new high-resolution records of carbonate accumulation rate, using marine sediments deposited in the equatorial Atlantic Ocean (Ceará Rise) at ODP Site 927, ... Doctoral or Postdoctoral Thesis Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
climate variability carbonate production paleoceanography warm climates microfossils Cenozoic 550 |
spellingShingle |
climate variability carbonate production paleoceanography warm climates microfossils Cenozoic 550 CORNUAULT, Pauline Natural variation of pelagic carbonate production during Cenozoic warm periods ... |
topic_facet |
climate variability carbonate production paleoceanography warm climates microfossils Cenozoic 550 |
description |
The biological carbon uptake, called biological compensation, have been shown to have a huge potential to affect the capacity of the ocean to absorb (anthropogenic) carbon dioxide, and so equilibrate the global carbon budget and hence climate. Since the pelagic calcite flux is made of two fundamentally different components, coccolithophore algae and planktonic foraminifera, understanding of the process of biological compensation requires knowledge of variability of their relative contribution to the total pelagic calcite flux. The aspects of the pelagic carbonate production that have changed through time and the mechanisms explaining the observed carbonate flux variability remain, despite their importance, largely unconstrained. In order to evaluate the orbital and long geological time scale variability of the pelagic carbonate production, I generated new high-resolution records of carbonate accumulation rate, using marine sediments deposited in the equatorial Atlantic Ocean (Ceará Rise) at ODP Site 927, ... |
format |
Doctoral or Postdoctoral Thesis |
author |
CORNUAULT, Pauline |
author_facet |
CORNUAULT, Pauline |
author_sort |
CORNUAULT, Pauline |
title |
Natural variation of pelagic carbonate production during Cenozoic warm periods ... |
title_short |
Natural variation of pelagic carbonate production during Cenozoic warm periods ... |
title_full |
Natural variation of pelagic carbonate production during Cenozoic warm periods ... |
title_fullStr |
Natural variation of pelagic carbonate production during Cenozoic warm periods ... |
title_full_unstemmed |
Natural variation of pelagic carbonate production during Cenozoic warm periods ... |
title_sort |
natural variation of pelagic carbonate production during cenozoic warm periods ... |
publisher |
Universität Bremen |
publishDate |
2023 |
url |
https://dx.doi.org/10.26092/elib/2651 https://media.suub.uni-bremen.de/handle/elib/7427 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
https://dx.doi.org/10.1594/pangaea.945848 https://dx.doi.org/10.1594/pangaea.945773 https://dx.doi.org/10.1594/pangaea.945812 https://dx.doi.org/10.1594/pangaea.945789 https://dx.doi.org/10.1594/pangaea.945707 |
op_rights |
Creative Commons Attribution 4.0 International CC BY 4.0 (Attribution) https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.26092/elib/265110.1594/pangaea.94584810.1594/pangaea.94577310.1594/pangaea.94581210.1594/pangaea.94578910.1594/pangaea.945707 |
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1786833241872793600 |