Articles | Volume 14, issue 11
https://doi.org/10.5194/cp-14-1819-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-14-1819-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
28 Nov 2018
Research article | Highlight paper |
| 28 Nov 2018
| 28 Nov 2018
Carbon burial in deep-sea sediment and implications for oceanic inventories of carbon and alkalinity over the last glacial cycle
Olivier Cartapanis
CORRESPONDING AUTHOR
Earth and Planetary Sciences McGill University, Montreal H3A 2A7, Canada
Institute of Geological Sciences and Oeschger Centre for Climate Change
Research, University of Bern, 3012 Bern, Switzerland
Eric D. Galbraith
Earth and Planetary Sciences McGill University, Montreal H3A 2A7, Canada
Institució Catalana de Recerca i Estudis Avançats (ICREA), Pg.
Lluís Companys 23, 08010 Barcelona, Spain
Institut de Ciència i Tecnologia Ambientals (ICTA) and Department of
Mathematics, Universitat Autònoma de Barcelona, 08193 Barcelona, Spain
Daniele Bianchi
Department of Atmospheric and Oceanic Sciences, University of California
Los Angeles, Los Angeles, CA 90095-1565, USA
Samuel L. Jaccard
Institute of Geological Sciences and Oeschger Centre for Climate Change
Research, University of Bern, 3012 Bern, Switzerland
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36 citations as recorded by crossref.
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- Fates of Terrigenous Dissolved Organic Carbon in the Gulf of Maine X. Wei et al. 10.1021/acs.est.3c08218
- Phanerozoic biological reworking of the continental carbonate rock reservoir C. Walton & O. Shorttle 10.1016/j.epsl.2024.118640
- Intrusion of Arabian Sea high salinity water and monsoon-associated processes modulate planktic foraminiferal abundance and carbon burial in the southwestern Bay of Bengal M. Salman & R. Saraswat 10.1007/s11356-024-32685-4
- The Earth system model CLIMBER-X v1.0 – Part 2: The global carbon cycle M. Willeit et al. 10.5194/gmd-16-3501-2023
- The Ocean Carbon Cycle T. DeVries 10.1146/annurev-environ-120920-111307
- Planktic Foraminiferal Test Size and Weight Response to the Late Pliocene Environment C. Todd et al. 10.1029/2019PA003738
- Stable Carbon Isotopes Suggest Large Terrestrial Carbon Inputs to the Global Ocean E. Kwon et al. 10.1029/2020GB006684
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- Glacial terminations or glacial interruptions? L. Stott 10.1016/j.earscirev.2024.104756
- Low terrestrial carbon storage at the Last Glacial Maximum: constraints from multi-proxy data A. Jeltsch-Thömmes et al. 10.5194/cp-15-849-2019
- The Biological Pump During the Last Glacial Maximum E. Galbraith & L. Skinner 10.1146/annurev-marine-010419-010906
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- The representation of alkalinity and the carbonate pump from CMIP5 to CMIP6 Earth system models and implications for the carbon cycle A. Planchat et al. 10.5194/bg-20-1195-2023
- Glacial state of the global carbon cycle: time-slice simulations for the last glacial maximum with an Earth-system model T. Kurahashi-Nakamura et al. 10.5194/cp-18-1997-2022
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- Orbital CO2 reconstruction using boron isotopes during the late Pleistocene, an assessment of accuracy E. de la Vega et al. 10.5194/cp-19-2493-2023
- Microfossil fragmentation across the Paleocene-Eocene transition at ODP Site 1209 (North Pacific): Implication for reconstructing nannofossil fluxes. N. Pige et al. 10.1016/j.marmicro.2023.102213
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Latest update: 24 Apr 2024
Short summary
A data-based reconstruction of carbon-bearing deep-sea sediment shows significant changes in the global burial rate over the last glacial cycle. We calculate the impact of these deep-sea changes, as well as hypothetical changes in continental shelf burial and volcanic outgassing. Our results imply that these geological fluxes had a significant impact on ocean chemistry and the global carbon isotopic ratio, and that the natural carbon cycle was not in steady state during the Holocene.
A data-based reconstruction of carbon-bearing deep-sea sediment shows significant changes in the...
