Benthic foraminifera and ostracods suggest a paleobathymetry of about 500 m and slightly under-oxygenated bottom conditions for the deposition of the sediments. Some bio-events, characterized by oligotypical assemblages (Bulimina elongata group high percentage values) indicating stressed bottom conditions and very low oxygen content, seem related to suboxic episodes.
Evolution of the Mediterranean basin during the late Langhian early Serravallian: An integrated paleoceanographic approach
Sprovieri M;
2002
Abstract
Benthic foraminifera and ostracods suggest a paleobathymetry of about 500 m and slightly under-oxygenated bottom conditions for the deposition of the sediments. Some bio-events, characterized by oligotypical assemblages (Bulimina elongata group high percentage values) indicating stressed bottom conditions and very low oxygen content, seem related to suboxic episodes.File in questo prodotto:
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