Articles | Volume 15, issue 1
https://doi.org/10.5194/cp-15-105-2019
https://doi.org/10.5194/cp-15-105-2019
Review article
 | 
16 Jan 2019
Review article |  | 16 Jan 2019

The 4.2 ka event, ENSO, and coral reef development

Lauren T. Toth and Richard B. Aronson

Viewed

Total article views: 4,836 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
3,131 1,614 91 4,836 91 107
  • HTML: 3,131
  • PDF: 1,614
  • XML: 91
  • Total: 4,836
  • BibTeX: 91
  • EndNote: 107
Views and downloads (calculated since 31 Aug 2018)
Cumulative views and downloads (calculated since 31 Aug 2018)

Viewed (geographical distribution)

Total article views: 4,836 (including HTML, PDF, and XML) Thereof 4,303 with geography defined and 533 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 14 Dec 2024
Download
Short summary
We explore the hypothesis that a shift in global climate 4200 years ago (the 4.2 ka event) was related to the El Niño–Southern Oscillation (ENSO). We summarize records of coral reef development in the tropical eastern Pacific, where intensification of ENSO stalled reef growth for 2500 years starting around 4.2 ka. Because corals are highly sensitive to climatic changes, like ENSO, we suggest that records from coral reefs may provide important clues about the role of ENSO in the 4.2 ka event.