Water column dynamics during the last interglacial anoxic event in the Mediterranean (sapropel S5)

Author:

Rohling E. J.1,Hopmans E. C.2,Sinninghe Damsté J. S.2

Affiliation:

1. National Oceanography Centre; Southampton UK

2. Royal Netherlands Institute for Sea Research; Den Burg, Texel Netherlands

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference46 articles.

1. Particulate organic matter in the subsurface chlorophyll maximum layer of the southeastern Mediterranean;Abdel-Moati;Oceanol. Acta,1990

2. Phycobiliprotein distribution across the western Mediterranean divergence;Algarra;Deep Sea Res., Part A,1988

3. Optical transparency, chlorophyll and primary productivity in the eastern Mediterranean near the Israeli coast;Berman;Oceanol. Acta,1984

4. High-resolution stratigraphic framework for Mediterranean sapropel S5: Defining temporal relationships between records of Eemian climate variability;Cane;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2002

5. Circulation changes and nutrient concentrations in the late Quaternary Aegean Sea: A nonsteady state concept for sapropel formation;Casford;Paleoceanography,2002

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