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

Viewed

Total article views: 3,600 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,038 1,293 269 3,600 510 130 139
  • HTML: 2,038
  • PDF: 1,293
  • XML: 269
  • Total: 3,600
  • Supplement: 510
  • BibTeX: 130
  • EndNote: 139
Views and downloads (calculated since 12 Sep 2014)
Cumulative views and downloads (calculated since 12 Sep 2014)

Cited

Saved (final revised paper)

Latest update: 28 Mar 2024
Download
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.