Abstract
A strong terrestrial contribution of organic matter was found, and significant autochthonous inputs were also present. Both strongly reduced and highly oxidized sediments have been found in the Cenozoic and Jurassic samples. All the Cretaceous sections are anoxic.-from Authors
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CITATION STYLE
APA
Simoneit, B. R. T., Vuchev, V. T., & Grimalt, J. O. (1984). Organic matter along the sedimentary sequences of the Moroccan continental margin, Leg 79, Sites 545 and 547. Initial Reports DSDP, Leg 79, Las Palmas to Brest, 807–824. https://doi.org/10.2973/dsdp.proc.79.133.1984
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