Articles | Volume 11, issue 3
https://doi.org/10.5194/cp-11-495-2015
https://doi.org/10.5194/cp-11-495-2015
Research article
 | 
18 Mar 2015
Research article |  | 18 Mar 2015

Freshwater discharge controlled deposition of Cenomanian–Turonian black shales on the NW European epicontinental shelf (Wunstorf, northern Germany)

N. A. G. M. van Helmond, A. Sluijs, J. S. Sinninghe Damsté, G.-J. Reichart, S. Voigt, J. Erbacher, J. Pross, and H. Brinkhuis

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Niels van Helmond on behalf of the Authors (05 Feb 2015)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by Editor) (06 Feb 2015) by Alan Haywood
AR by Niels van Helmond on behalf of the Authors (09 Feb 2015)  Author's response   Manuscript 
ED: Publish as is (23 Feb 2015) by Alan Haywood
AR by Niels van Helmond on behalf of the Authors (24 Feb 2015)  Author's response   Manuscript 
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Short summary
Based on the chemistry and microfossils preserved in sediments deposited in a shallow sea, in the current Lower Saxony region (NW Germany), we conclude that changes in Earth’s orbit around the Sun led to enhanced rainfall and organic matter production. The additional supply of organic matter, depleting oxygen upon degradation, and freshwater, inhibiting the mixing of oxygen-rich surface waters with deeper waters, caused the development of oxygen-poor waters about 94 million years ago.