Factors controlling the burial of organic carbon in laminated and bioturbated sediments off NW Mexico: implications for hydrocarbon preservation
- 30 June 1999
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 63 (11-12) , 1723-1734
- https://doi.org/10.1016/s0016-7037(99)00073-3
Abstract
No abstract availableThis publication has 43 references indexed in Scilit:
- Glacial‐interglacial variability in upwelling and bioproductivity off NW Mexico: Implications for Quaternary paleoclimatePaleoceanography and Paleoclimatology, 1998
- Production and dissolution of biogenic silica in the ocean: Revised global estimates, comparison with regional data and relationship to biogenic sedimentationGlobal Biogeochemical Cycles, 1995
- Large changes in oceanic nutrient inventories from glacial to interglacial periodsNature, 1995
- On the organic carbon maximum on the continental slope of the eastern Arabian SeaJournal of Marine Research, 1995
- Carbon budget for the mid-slope depocenter of the Middle Atlantic BightDeep Sea Research Part II: Topical Studies in Oceanography, 1994
- Gulf of California biogeographic regions based on coastal zone color scanner imageryJournal of Geophysical Research: Oceans, 1994
- Geochemical evidence for enhanced preservation of organic matter in the oxygen minimum zone of the continental margin of northern California during the Late PleistocenePaleoceanography and Paleoclimatology, 1994
- Timing of Late Quaternary productivity pulses in the Panama Basin and implications for atmospheric CO2Paleoceanography and Paleoclimatology, 1991
- Processes controlling the organic carbon content of open ocean sedimentsPaleoceanography and Paleoclimatology, 1988
- The inorganic geochemistry of Cretaceous black shales (DSDP Leg 41) in comparison to modern upwelling sediments from the Gulf of CaliforniaGeological Society, London, Special Publications, 1986