Quantitative interpretation of atmospheric carbon records over the last glacial termination
- 13 December 2005
- journal article
- Published by American Geophysical Union (AGU) in Global Biogeochemical Cycles
- Vol. 19 (4)
- https://doi.org/10.1029/2004gb002345
Abstract
No abstract availableKeywords
This publication has 102 references indexed in Scilit:
- Glacial North Atlantic: Sea‐surface conditions reconstructed by GLAMAP 2000Paleoceanography and Paleoclimatology, 2003
- Accumulation of biogenic and lithogenic material in the Pacific sector of the Southern Ocean during the past 40,000 yearsDeep Sea Research Part II: Topical Studies in Oceanography, 2003
- Pleistocene vertical carbon isotope and carbonate gradients in the South Atlantic sector of the Southern OceanGeochemistry, Geophysics, Geosystems, 2003
- The Southern Ocean's biological pump during the Last Glacial MaximumDeep Sea Research Part II: Topical Studies in Oceanography, 2002
- A switch from Si(OH)4 to NO3− depletion in the glacial Southern OceanGeophysical Research Letters, 2002
- Global sea–air CO2 flux based on climatological surface ocean pCO2, and seasonal biological and temperature effectsDeep Sea Research Part II: Topical Studies in Oceanography, 2002
- Carbon export fluxes in the Southern Ocean: results from inverse modeling and comparison with satellite-based estimatesDeep Sea Research Part II: Topical Studies in Oceanography, 2002
- Oceanic vertical exchange and new production: a comparison between models and observationsDeep Sea Research Part II: Topical Studies in Oceanography, 2001
- What caused the glacial/interglacial atmospheric pCO2 cycles?Reviews of Geophysics, 2000
- Paleo‐sea surface temperature calculations in the equatorial east Atlantic from Mg/Ca ratios in planktic foraminifera: A comparison to sea surface temperature estimates from U37K′, oxygen isotopes, and foraminiferal transfer functionPaleoceanography and Paleoclimatology, 2000