Articles | Volume 17, issue 3
Clim. Past, 17, 1025–1050, 2021
https://doi.org/10.5194/cp-17-1025-2021
Clim. Past, 17, 1025–1050, 2021
https://doi.org/10.5194/cp-17-1025-2021
Research article
 | Highlight paper
12 May 2021
Research article  | Highlight paper | 12 May 2021

Deoxygenation dynamics on the western Nile deep-sea fan during sapropel S1 from seasonal to millennial timescales

Cécile L. Blanchet et al.

Viewed

Total article views: 2,474 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,807 648 19 2,474 129 13 26
  • HTML: 1,807
  • PDF: 648
  • XML: 19
  • Total: 2,474
  • Supplement: 129
  • BibTeX: 13
  • EndNote: 26
Views and downloads (calculated since 02 Oct 2020)
Cumulative views and downloads (calculated since 02 Oct 2020)

Viewed (geographical distribution)

Total article views: 2,090 (including HTML, PDF, and XML) Thereof 2,087 with geography defined and 3 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 16 May 2022
Download
Short summary
The Mediterranean Sea turned repeatedly into an oxygen-deprived basin during the geological past, as evidenced by distinct sediment layers called sapropels. We use here records of the last sapropel S1 retrieved in front of the Nile River to explore the relationships between riverine input and seawater oxygenation. We decipher the seasonal cycle of fluvial input and seawater chemistry as well as the decisive influence of primary productivity on deoxygenation at millennial timescales.