Changes in the distribution of δ13C of deep water ΣCO2 between the Last Glaciation and the Holocene
- 1 June 1988
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 3 (3), 317-341
- https://doi.org/10.1029/pa003i003p00317
Abstract
No abstract availableThis publication has 33 references indexed in Scilit:
- Variations in mode of formation and temperature of oceanic deep waters over the past 125,000 yearsNature, 1987
- Melting history of Antarctica during the past 60,000 yearsNature, 1986
- Benthic foraminiferal δ13C and accumulation rates of organic carbon: Uvigerina Peregrina group and Cibicidoides WuellerstorfiPaleoceanography and Paleoclimatology, 1986
- North Atlantic surface-ocean control of Pleistocene deep-ocean circulationEarth and Planetary Science Letters, 1985
- Reduced advection into Atlantic Ocean deep eastern basins during last glaciation maximumNature, 1983
- Oxygen and carbon isotope record of East Pacific core V19-30: implications for the formation of deep water in the late Pleistocene North AtlanticEarth and Planetary Science Letters, 1983
- Carbon and oxygen isotopic disequilibria of recent deep-sea benthic foraminiferaMarine Micropaleontology, 1981
- Deep water formation in the North Atlantic Ocean during the last ice ageNature, 1980
- Biological fractionation of oxygen and carbon isotopes by recent benthic foraminiferaMarine Micropaleontology, 1980
- The dissolved O2-CO2-13C system in the eastern equatorial pacificDeep Sea Research and Oceanographic Abstracts, 1974