Influence of water column anoxia and sediment supply on the burial and preservation of organic carbon in marine shales
- 30 November 1999
- journal article
- Published by Elsevier
- Vol. 60 (9) , 1577-1593
- https://doi.org/10.1016/0016-7037(96)00041-5
Abstract
No abstract availableKeywords
This publication has 49 references indexed in Scilit:
- Glacialá¤-interglacial changes in nutrient utilization in the equatorial Pacific OceanNature, 1995
- Sedimentary nitrogen isotopic ratio as a recorder for surface ocean nitrate utilizationGlobal Biogeochemical Cycles, 1994
- Relationship between inferred redox potential of the depositional environment and geochemistry of the Upper Pennsylvanian (Missourian) Stark Shale Member of the Dennis Limestone, Wabaunsee County, Kansas, U.S.A.Chemical Geology, 1992
- Evidence from nitrogen isotope ratios for enhanced productivity during formation of eastern Mediterranean sapropelsNature, 1992
- Does Sedimentary Organic δ13C Record Variations in Quaternary Ocean [CO2(aq)]?Paleoceanography and Paleoclimatology, 1991
- Geochemistry of recent TOC-rich sediments from the Gulf of California and the Black SeaInternational Journal of Earth Sciences, 1989
- Variable marine productivity and high eolian input recorded by rhythmic black shales in Mid‐Cretaceous pelagic deposits from central ItalyPaleoceanography and Paleoclimatology, 1986
- Anomalous 13C enrichment in modern marine organic carbonNature, 1985
- Carbon isotopes as indicators of dispersal patterns in Devonian-Mississippian shales of the Appalachian BasinGeology, 1981
- Cretaceous anoxic events: from continents to oceansJournal of the Geological Society, 1980