Articles | Volume 9, issue 6
https://doi.org/10.5194/cp-9-2595-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-9-2595-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Peak glacial 14C ventilation ages suggest major draw-down of carbon into the abyssal ocean
M. Sarnthein
Institut für Geowissenschaften, University of Kiel, Olshausenstr. 40, 24098 Kiel, Germany
Institut für Geologie und Paläontologie, University of Innsbruck, 6020 Innsbruck, Austria
B. Schneider
Institut für Geowissenschaften, University of Kiel, Olshausenstr. 40, 24098 Kiel, Germany
P. M. Grootes
Institute of Ecosystem Research, University of Kiel, Olshausenstr. 40, 24098 Kiel, Germany
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Cited
81 citations as recorded by crossref.
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- 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
- The Biological Pump During the Last Glacial Maximum E. Galbraith & L. Skinner 10.1146/annurev-marine-010419-010906
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- Enhanced δ13C and δ18O Differences Between the South Atlantic and South Pacific During the Last Glaciation: The Deep Gateway Hypothesis E. Sikes et al. 10.1002/2017PA003118
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- Deep water exchanges between the South China Sea and the Pacific since the last glacial period S. Wan & Z. Jian 10.1002/2013PA002578
- Complementary constraints from carbon (13C) and nitrogen (15N) isotopes on the glacial ocean's soft‐tissue biological pump A. Schmittner & C. Somes 10.1002/2015PA002905
- Modeling the contribution of dissolved organic carbon to carbon sequestration during the last glacial maximum W. Ma & J. Tian 10.1007/s00367-014-0378-y
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- Coupled climate–carbon cycle simulation of the Last Glacial Maximum atmospheric CO<sub>2</sub> decrease using a large ensemble of modern plausible parameter sets K. Kemppinen et al. 10.5194/cp-15-1039-2019
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- Deep-water carbonate dissolution in the northern South China Sea during Marine Isotope Stage 3 N. Wang et al. 10.1016/j.jop.2015.11.004
- Biological and physical controls in the Southern Ocean on past millennial-scale atmospheric CO2 changes J. Gottschalk et al. 10.1038/ncomms11539
- Magnetic Fingerprints of Modern Sediments in the South China Sea Resulting From Source‐to‐Sink Processes C. Kissel et al. 10.1029/2018GC007571
- Rapid Loss of CO2 From the South Pacific Ocean During the Last Glacial Termination K. Allen et al. 10.1029/2019PA003766
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5 citations as recorded by crossref.
- Selection and Treatment of Data for Radiocarbon Calibration: An Update to the International Calibration (IntCal) Criteria P. Reimer et al. 10.2458/azu_js_rc.55.16955
- Response of a comprehensive climate model to a broad range of external forcings: relevance for deep ocean ventilation and the development of late Cenozoic ice ages E. Galbraith & C. de Lavergne 10.1007/s00382-018-4157-8
- Stratigraphic gaps at northern South China Sea margin reflect changes in Pacific deepwater inflow at glacial Termination II M. Sarnthein et al. 10.1007/s11430-013-4678-2
- IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP P. Reimer et al. 10.2458/azu_js_rc.55.16947
- Reduced ventilation and enhanced magnitude of the deep Pacific carbon pool during the last glacial period L. Skinner et al. 10.1016/j.epsl.2014.11.024
Saved (final revised paper)
Latest update: 13 Dec 2024