Role of deep sea temperature in the carbon cycle during the last glacial
- 18 June 2005
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 20 (2)
- https://doi.org/10.1029/2003pa000914
Abstract
No abstract availableKeywords
This publication has 51 references indexed in Scilit:
- Model sensitivity in the effect of Antarctic sea ice and stratification on atmospheric pCO2Paleoceanography and Paleoclimatology, 2003
- A simple evaluation of cleaning procedures on fossil benthic foraminiferal Mg/CaGeochemistry, Geophysics, Geosystems, 2002
- Tropical cooling at the last glacial maximum and extratropical ocean ventilation1Geophysical Research Letters, 2002
- Phase relationships between millennial‐scale events 64,000–24,000 years agoPaleoceanography and Paleoclimatology, 2000
- On the origin and timing of rapid changes in atmospheric methane during the Last Glacial PeriodGlobal Biogeochemical Cycles, 2000
- What caused the glacial/interglacial atmospheric pCO2 cycles?Reviews of Geophysics, 2000
- Atmospheric CO2 concentration from 60 to 20 kyr BP from the Taylor Dome Ice Core, AntarcticaGeophysical Research Letters, 2000
- Incorporation and preservation of Mg in Globigerinoides sacculifer: implications for reconstructing the temperature and 18O/16O of seawaterPaleoceanography and Paleoclimatology, 2000
- Variations in Mg/Ca and Sr/Ca ratios of planktonic foraminifera caused by postdepositional dissolution: Evidence of shallow Mg‐dependent dissolutionPaleoceanography and Paleoclimatology, 1996
- Primary production at 47°N and 20°W in the North Atlantic Ocean: a comparison between the 14C incubation method and the mixed layer carbon budgetDeep Sea Research Part II: Topical Studies in Oceanography, 1993