Late Quaternary productivity changes in the western equatorial Atlantic: Evidence from 230 Th-normalized carbonate and organic carbon accumulation rates
- 1 November 1996
- journal article
- Published by Elsevier in Marine Geology
- Vol. 135 (1-4), 127-152
- https://doi.org/10.1016/s0025-3227(96)00048-5
Abstract
No abstract availableKeywords
This publication has 55 references indexed in Scilit:
- Glacial/interglacial changes in sediment rain rate in the SW Indian Sector of subantarctic Waters as recorded by 230Th, 231Pa, U, and δ15NPaleoceanography and Paleoclimatology, 1993
- “Blue-ocean” paleoproductivity estimates from pelagic carbonate mass accumulation ratesMarine Micropaleontology, 1992
- Geochemical Processes Occurring in the Waters at the Amazon River/Ocean BoundaryOceanography, 1991
- Reconstructing past particle fluxes in the tropical Atlantic OceanPaleoceanography and Paleoclimatology, 1990
- Reconstructing the ocean carbon system variation during the last 150,000 years according to the Antarctic nutrient hypothesisPaleoceanography and Paleoclimatology, 1990
- Surface water response of the equatorial Atlantic Ocean to orbital forcingPaleoceanography and Paleoclimatology, 1989
- On the Late Pleistocene ocean geochemistry and circulationPaleoceanography and Paleoclimatology, 1988
- Global variations of surface ocean productivity in low and mid latitudes: Influence on CO2 reservoirs of the deep ocean and atmosphere during the last 21,000 yearsPaleoceanography and Paleoclimatology, 1988
- The record of Late Pleistocene biogenic sedimentation in the eastern tropical Pacific OceanPaleoceanography and Paleoclimatology, 1988
- Calcite dissolution and the modification of planktonic foraminiferal assemblagesMarine Micropaleontology, 1981