Modes of sapropel formation in the eastern Mediterranean: some constraints based on pyrite properties

Pyrite formation within and directly below sapropels in the eastern Mediterranean was governed by the relative rates of sulphide production and Fe liberation and supply to the organic-rich layers. At times of relatively high SO 2− 4 reduction, sulphide could diffuse downward from the sapropel and fo...

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Veröffentlicht in:	Marine geology 1999, Vol.153 (1), p.199-219
Hauptverfasser:	Passier, Hilde F., Middelburg, Jack J., de Lange, Gert J., Böttcher, Michael E.
Format:	Artikel
Sprache:	eng
Schlagworte:	eastern Mediterranean framboidal microtexture Marine organic carbon pyrite S-34/S-32 sapropel
Online-Zugang:	Volltext
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