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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Bibliographic Details
Main Author: CORNUAULT, Pauline
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: Universität Bremen 2023
Subjects:
550
Online Access:https://dx.doi.org/10.26092/elib/2651
https://media.suub.uni-bremen.de/handle/elib/7427
id ftdatacite:10.26092/elib/2651
record_format openpolar
spelling 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)
institution 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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