Articles | Volume 17, issue 5
Clim. Past, 17, 2091–2117, 2021
https://doi.org/10.5194/cp-17-2091-2021
Clim. Past, 17, 2091–2117, 2021
https://doi.org/10.5194/cp-17-2091-2021

Research article 15 Oct 2021

Research article | 15 Oct 2021

Climate, cryosphere and carbon cycle controls on Southeast Atlantic orbital-scale carbonate deposition since the Oligocene (30–0 Ma)

Anna Joy Drury et al.

Viewed

Total article views: 1,869 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,317 532 20 1,869 95 21 29
  • HTML: 1,317
  • PDF: 532
  • XML: 20
  • Total: 1,869
  • Supplement: 95
  • BibTeX: 21
  • EndNote: 29
Views and downloads (calculated since 04 Sep 2020)
Cumulative views and downloads (calculated since 04 Sep 2020)

Viewed (geographical distribution)

Total article views: 1,607 (including HTML, PDF, and XML) Thereof 1,601 with geography defined and 6 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 16 Jan 2022
Download
Short summary
We use the first high-resolution southeast Atlantic carbonate record to see how climate dynamics evolved since 30 million years ago (Ma). During ~ 30–13 Ma, eccentricity (orbital circularity) paced carbonate deposition. After the mid-Miocene Climate Transition (~ 14 Ma), precession (Earth's tilt direction) increasingly drove carbonate variability. In the latest Miocene (~ 8 Ma), obliquity (Earth's tilt) pacing appeared, signalling increasing high-latitude influence.