Alkenone isotopes show evidence of active carbon concentrating mechanisms in coccolithophores as aqueous carbon dioxide concentrations fall below 7 µmol L−1
Coccolithophores and other haptophyte algae acquire the carbon required for metabolic processes from the water in which they live. Whether carbon is actively moved across the cell membrane via a carbon concentrating mechanism, or passively through diffusion, is important for haptophyte biochemistry....
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ftcopernicus:oai:publications.copernicus.org:bg89929 2023-05-15T16:38:48+02:00 Alkenone isotopes show evidence of active carbon concentrating mechanisms in coccolithophores as aqueous carbon dioxide concentrations fall below 7 µmol L−1 Badger, Marcus P. S. 2021-02-15 application/pdf https://doi.org/10.5194/bg-18-1149-2021 https://bg.copernicus.org/articles/18/1149/2021/ eng eng doi:10.5194/bg-18-1149-2021 https://bg.copernicus.org/articles/18/1149/2021/ eISSN: 1726-4189 Text 2021 ftcopernicus https://doi.org/10.5194/bg-18-1149-2021 2021-02-22T17:22:15Z Coccolithophores and other haptophyte algae acquire the carbon required for metabolic processes from the water in which they live. Whether carbon is actively moved across the cell membrane via a carbon concentrating mechanism, or passively through diffusion, is important for haptophyte biochemistry. The possible utilization of carbon concentrating mechanisms also has the potential to over-print one proxy method by which ancient atmospheric CO 2 concentration is reconstructed using alkenone isotopes. Here I show that carbon concentrating mechanisms are likely used when aqueous carbon dioxide concentrations are below 7 µ mol L −1 . I compile published alkenone-based CO 2 reconstructions from multiple sites over the Pleistocene and recalculate them using a common methodology, which allows comparison to be made with ice core CO 2 records. Interrogating these records reveals that the relationship between proxy CO 2 and ice core CO 2 breaks down when local aqueous CO 2 concentration falls below 7 µ mol L −1 . The recognition of this threshold explains why many alkenone-based CO 2 records fail to accurately replicate ice core CO 2 records, and it suggests the alkenone proxy is likely robust for much of the Cenozoic when this threshold was unlikely to be reached in much of the global ocean. Text ice core Copernicus Publications: E-Journals Biogeosciences 18 3 1149 1160 |
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Copernicus Publications: E-Journals |
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ftcopernicus |
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English |
description |
Coccolithophores and other haptophyte algae acquire the carbon required for metabolic processes from the water in which they live. Whether carbon is actively moved across the cell membrane via a carbon concentrating mechanism, or passively through diffusion, is important for haptophyte biochemistry. The possible utilization of carbon concentrating mechanisms also has the potential to over-print one proxy method by which ancient atmospheric CO 2 concentration is reconstructed using alkenone isotopes. Here I show that carbon concentrating mechanisms are likely used when aqueous carbon dioxide concentrations are below 7 µ mol L −1 . I compile published alkenone-based CO 2 reconstructions from multiple sites over the Pleistocene and recalculate them using a common methodology, which allows comparison to be made with ice core CO 2 records. Interrogating these records reveals that the relationship between proxy CO 2 and ice core CO 2 breaks down when local aqueous CO 2 concentration falls below 7 µ mol L −1 . The recognition of this threshold explains why many alkenone-based CO 2 records fail to accurately replicate ice core CO 2 records, and it suggests the alkenone proxy is likely robust for much of the Cenozoic when this threshold was unlikely to be reached in much of the global ocean. |
format |
Text |
author |
Badger, Marcus P. S. |
spellingShingle |
Badger, Marcus P. S. Alkenone isotopes show evidence of active carbon concentrating mechanisms in coccolithophores as aqueous carbon dioxide concentrations fall below 7 µmol L−1 |
author_facet |
Badger, Marcus P. S. |
author_sort |
Badger, Marcus P. S. |
title |
Alkenone isotopes show evidence of active carbon concentrating mechanisms in coccolithophores as aqueous carbon dioxide concentrations fall below 7 µmol L−1 |
title_short |
Alkenone isotopes show evidence of active carbon concentrating mechanisms in coccolithophores as aqueous carbon dioxide concentrations fall below 7 µmol L−1 |
title_full |
Alkenone isotopes show evidence of active carbon concentrating mechanisms in coccolithophores as aqueous carbon dioxide concentrations fall below 7 µmol L−1 |
title_fullStr |
Alkenone isotopes show evidence of active carbon concentrating mechanisms in coccolithophores as aqueous carbon dioxide concentrations fall below 7 µmol L−1 |
title_full_unstemmed |
Alkenone isotopes show evidence of active carbon concentrating mechanisms in coccolithophores as aqueous carbon dioxide concentrations fall below 7 µmol L−1 |
title_sort |
alkenone isotopes show evidence of active carbon concentrating mechanisms in coccolithophores as aqueous carbon dioxide concentrations fall below 7 µmol l−1 |
publishDate |
2021 |
url |
https://doi.org/10.5194/bg-18-1149-2021 https://bg.copernicus.org/articles/18/1149/2021/ |
genre |
ice core |
genre_facet |
ice core |
op_source |
eISSN: 1726-4189 |
op_relation |
doi:10.5194/bg-18-1149-2021 https://bg.copernicus.org/articles/18/1149/2021/ |
op_doi |
https://doi.org/10.5194/bg-18-1149-2021 |
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Biogeosciences |
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1160 |
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