Evidence for the evolution of an oxygen minimum layer at the beginning of S-1 sapropel deposition in the eastern Mediterranean
- 1 August 1997
- journal article
- Published by Elsevier in Marine Geology
- Vol. 140 (3-4) , 231-236
- https://doi.org/10.1016/s0025-3227(97)00058-3
Abstract
No abstract availableThis publication has 24 references indexed in Scilit:
- IntroductionPublished by Cambridge University Press (CUP) ,2012
- Stable isotope and alkenone temperature records of sapropels from Sites 964 and 967: constraining the physical environment of sapropel formation in the Eastern Mediterranean SeaPublished by International Ocean Discovery Program (IODP) ,1998
- Radiocarbon chronology of Black Sea sedimentsDeep Sea Research Part I: Oceanographic Research Papers, 1994
- Modification and complete removal of eastern Mediterranean sapropels by postdepositional oxidationGeology, 1994
- Evidence from nitrogen isotope ratios for enhanced productivity during formation of eastern Mediterranean sapropelsNature, 1992
- Nutrient dynamics and new production in a warm-core eddy from the Eastern Mediterranean SeaDeep Sea Research Part A. Oceanographic Research Papers, 1992
- Organic carbon accumulation in Bannock Basin: Evaluating the role of productivity in the formation of eastern Mediterranean sapropelsMarine Geology, 1992
- Carbon accumulation rates and the origin of the Holocene sapropel in the Black SeaGeology, 1987
- Sedimentary and geochemical indicators of productivity and oxygen contents in modern and ancient basins: The Holocene Black Sea as the “type” anoxic basinChemical Geology, 1985
- Paleoclimatic Record of a Long Deep Sea Core from the Eastern MediterraneanQuaternary Research, 1977