Geochemical evidence for enhanced preservation of organic matter in the oxygen minimum zone of the continental margin of northern California during the Late Pleistocene
- 1 February 1994
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 9 (1) , 47-61
- https://doi.org/10.1029/93pa02829
Abstract
No abstract availableThis publication has 48 references indexed in Scilit:
- Variability of the Late Pleistocene-Early Holocene Oxygen-Minimum Zone off Northern CaliforniaPublished by Wiley ,2013
- Lack of evidence for enhanced preservation of sedimentary organic matter in the oxygen minimum of the Gulf of CaliforniaGeology, 1992
- Persistent Late Pleistocene-Holocene Seasonal Upwelling and Varves Off the Coast of CaliforniaQuaternary Research, 1987
- Depletion of 13C in Cretaceous marine organic matter: Source, diagenetic, or environmental sigal?Marine Geology, 1986
- Determination of carbonate carbon in geological materials by coulometric titrationChemical Geology, 1985
- Geochemistry of Namibian Shelf SedimentsPublished by Springer Nature ,1983
- Variation of upwelling/oceanic conditions during the latest Pleistocene through Holocene off the central Peruvian coast: A diatom recordMarine Micropaleontology, 1981
- Short term sedimentation response in lakes in western United States as measured by automated sampling1Limnology and Oceanography, 1977
- Méthode rapide de caractérisation des roches mètres, de leur potentiel pétrolier et de leur degré d'évolutionRevue de l'Institut Français du Pétrole, 1977
- Origin of Diatom-Rich, Varved Sediments from the Gulf of CaliforniaThe Journal of Geology, 1966