Influence of export rain ratio changes on atmospheric CO2 and sedimentary calcite preservation
- 7 March 2009
- journal article
- research article
- Published by Springer Nature in Journal of Oceanography
- Vol. 65 (2) , 209-221
Abstract
No abstract availableKeywords
This publication has 60 references indexed in Scilit:
- Reconciling surface ocean productivity, export fluxes and sediment composition in a global biogeochemical ocean modelBiogeosciences, 2006
- Anthropogenic ocean acidification over the twenty-first century and its impact on calcifying organismsNature, 2005
- The biological pump in the northwestern North Pacific based on fluxes and major components of particulate matter obtained by sediment-trap experiments (1997–2000)Deep Sea Research Part II: Topical Studies in Oceanography, 2002
- Role of increased marine silica input on paleo‐pCO2 levelsPaleoceanography and Paleoclimatology, 2000
- What caused the glacial/interglacial atmospheric pCO2 cycles?Reviews of Geophysics, 2000
- A global oceanic sediment model for long‐term climate studiesGlobal Biogeochemical Cycles, 1999
- Annual biogenic particle fluxes to the interior of the North Atlantic Ocean; studied at 34°N 21°W and 48°N 21°WDeep Sea Research Part II: Topical Studies in Oceanography, 1993
- A universal solver for hyperbolic equations by cubic-polynomial interpolation I. One-dimensional solverComputer Physics Communications, 1991
- Climatic change and CaCO3 preservation: An 800,000 year bathymetric Reconstruction from the central equatorial Pacific OceanPaleoceanography and Paleoclimatology, 1989
- On the Late Pleistocene ocean geochemistry and circulationPaleoceanography and Paleoclimatology, 1988