Articles | Volume 6, issue 5
https://doi.org/10.5194/cp-6-645-2010
© Author(s) 2010. 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-6-645-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
08 Oct 2010
A synthesis of marine sediment core δ13C data over the last 150 000 years
K. I. C. Oliver
Department of Earth and Environmental Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK
School of Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, European Way, Southampton SO14 3ZH, UK
B. A. A. Hoogakker
Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 2EQ, UK
S. Crowhurst
Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 2EQ, UK
G. M. Henderson
Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3PR, UK
R. E. M. Rickaby
Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3PR, UK
N. R. Edwards
Department of Earth and Environmental Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK
H. Elderfield
Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 2EQ, UK
Related subject area
Subject: Carbon Cycle | Archive: Marine Archives | Timescale: Milankovitch
Glacial state of the global carbon cycle: time-slice simulations for the last glacial maximum with an Earth-system model
Astronomical tunings of the Oligocene–Miocene transition from Pacific Ocean Site U1334 and implications for the carbon cycle
Orbital control on the timing of oceanic anoxia in the Late Cretaceous
Deep ocean ventilation, carbon isotopes, marine sedimentation and the deglacial CO2 rise
Takasumi Kurahashi-Nakamura, André Paul, Ute Merkel, and Michael Schulz
Clim. Past, 18, 1997–2019, https://doi.org/10.5194/cp-18-1997-2022, https://doi.org/10.5194/cp-18-1997-2022, 2022
Short summary
Short summary
With a comprehensive Earth-system model including the global carbon cycle, we simulated the climate state during the last glacial maximum. We demonstrated that the CO2 concentration in the atmosphere both in the modern (pre-industrial) age (~280 ppm) and in the glacial age (~190 ppm) can be reproduced by the model with a common configuration by giving reasonable model forcing and total ocean inventories of carbon and other biogeochemical matter for the respective ages.
Helen M. Beddow, Diederik Liebrand, Douglas S. Wilson, Frits J. Hilgen, Appy Sluijs, Bridget S. Wade, and Lucas J. Lourens
Clim. Past, 14, 255–270, https://doi.org/10.5194/cp-14-255-2018, https://doi.org/10.5194/cp-14-255-2018, 2018
Short summary
Short summary
We present two astronomy-based timescales for climate records from the Pacific Ocean. These records range from 24 to 22 million years ago, a time period when Earth was warmer than today and the only land ice was located on Antarctica. We use tectonic plate-pair spreading rates to test the two timescales, which shows that the carbonate record yields the best timescale. In turn, this implies that Earth’s climate system and carbon cycle responded slowly to changes in incoming solar radiation.
Sietske J. Batenburg, David De Vleeschouwer, Mario Sprovieri, Frederik J. Hilgen, Andrew S. Gale, Brad S. Singer, Christian Koeberl, Rodolfo Coccioni, Philippe Claeys, and Alessandro Montanari
Clim. Past, 12, 1995–2009, https://doi.org/10.5194/cp-12-1995-2016, https://doi.org/10.5194/cp-12-1995-2016, 2016
Short summary
Short summary
The relative contributions of astronomical forcing and tectonics to ocean anoxia in the Cretaceous are unclear. This study establishes the pacing of Late Cretaceous black cherts and shales. We present a 6-million-year astrochronology from the Furlo and Bottaccione sections in Italy that spans the Cenomanian–Turonian transition and OAE2. Together with a new radioisotopic age for the mid-Cenomanian event, we show that astronomical forcing determined the timing of these carbon cycle perturbations.
T. Tschumi, F. Joos, M. Gehlen, and C. Heinze
Clim. Past, 7, 771–800, https://doi.org/10.5194/cp-7-771-2011, https://doi.org/10.5194/cp-7-771-2011, 2011
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