Abstract
In recent Black Sea sediments peculiar sediment layers occur which in sedimentological and geochemical composition differ from over- and underlying sediments. Originally described as turbidites they lack typical turbidite features. An alternative formation mechanism is proposed here and a conceptual model developed. This explains the occurrence of the so-called ‘Degens’-layers by density inversion eventually supported by exsolution of biogenic gas.
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Kempe, S., Liebezeit, G., Duman, M. et al. Extrusion: the formation mechanism for the presumed ‘turbidites’ of the deep Black Sea?. Senckenbergiana maritima 31, 11–16 (2001). https://doi.org/10.1007/BF03042832
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DOI: https://doi.org/10.1007/BF03042832