What caused the atmosphere's CO2 content to rise during the last 8000 years?
- 2 October 2001
- journal article
- Published by American Geophysical Union (AGU) in Geochemistry, Geophysics, Geosystems
- Vol. 2 (10)
- https://doi.org/10.1029/2001gc000177
Abstract
No abstract availableKeywords
This publication has 14 references indexed in Scilit:
- An evaluation of Lohmann's foraminifera weight dissolution indexPaleoceanography and Paleoclimatology, 2001
- Evidence for a reduction in the carbonate ion content of the deep sea during the course of the HolocenePaleoceanography and Paleoclimatology, 1999
- Holocene carbon-cycle dynamics based on CO2 trapped in ice at Taylor Dome, AntarcticaNature, 1999
- Biogenic budgets of particle rain, benthic remineralization and sediment accumulation in the equatorial PacificDeep Sea Research Part II: Topical Studies in Oceanography, 1997
- A model for variation in the chemistry of planktonic foraminifera due to secondary calcification and selective dissolutionPaleoceanography and Paleoclimatology, 1995
- Effect of deep-sea sedimentary calcite preservation on atmospheric CO2 concentrationNature, 1994
- Changes in the distribution of δ13C of deep water ΣCO2 between the Last Glaciation and the HolocenePaleoceanography and Paleoclimatology, 1988
- The role of CaCO3 compensation in the glacial to interglacial atmospheric CO2 changeGlobal Biogeochemical Cycles, 1987
- Recent increase in Pacific CaCo3 dissolution: A mechanism for generating old 14C agesMarine Geology, 1984
- Neutralization of Fossil Fuel CO2 by Marine Calcium CarbonatePublished by Springer Science and Business Media LLC ,1977