Articles | Volume 14, issue 7
https://doi.org/10.5194/cp-14-1079-2018
https://doi.org/10.5194/cp-14-1079-2018
Research article
 | 
25 Jul 2018
Research article |  | 25 Jul 2018

Thermocline state change in the eastern equatorial Pacific during the late Pliocene/early Pleistocene intensification of Northern Hemisphere glaciation

Kim Alix Jakob, Jörg Pross, Christian Scholz, Jens Fiebig, and Oliver Friedrich

Viewed

Total article views: 3,587 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,128 1,141 318 3,587 227 106 104
  • HTML: 2,128
  • PDF: 1,141
  • XML: 318
  • Total: 3,587
  • Supplement: 227
  • BibTeX: 106
  • EndNote: 104
Views and downloads (calculated since 20 Nov 2017)
Cumulative views and downloads (calculated since 20 Nov 2017)

Viewed (geographical distribution)

Total article views: 3,587 (including HTML, PDF, and XML) Thereof 3,369 with geography defined and 218 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 14 Dec 2024
Download
Short summary
Eastern equatorial Pacific (EEP) thermocline dynamics during the intensification of Northern Hemisphere glaciation (iNHG; ~ 2.5 Ma) currently remain unclear. In light of this uncertainty, we generated geochemical, faunal and sedimentological data for EEP Site 849 (~ 2.75–2.4 Ma). We recorded a thermocline depth change shortly before the final phase of the iNHG, which supports the hypothesis that tropical thermocline shoaling may have contributed to substantial Northern Hemisphere ice growth.