Terrestrial‐marine dust fluxes, pedogenic carbonate δ13C values, and various paleovegetation proxies suggest that Africa experienced gradual cooling and drying across the Pliocene‐Pleistocene (Plio‐Pleistocene) boundary (2.58 million years ago [Ma]). However, the timing, magnitude, resolution, and relative influences of orbitally‐driven changes in high latitude glaciations and low latitude insolation differ by region and proxy. To disentangle these forcings and investigate equatorial eastern African climate across the Plio‐Pleistocene boundary, we generated a high‐resolution (∼3,000‐year) data set of compound‐specific
- Award ID(s):
- 2150228
- NSF-PAR ID:
- 10484222
- Editor(s):
- Ham, David; Añel, Juan Antonio; Kerkweg, Astrid; Lo, Min-Hui; Neale, Richard; Sander, Rolf; Ullrich, Paul
- Publisher / Repository:
- European Scientific Union
- Date Published:
- Journal Name:
- Geoscientific Model Development
- Edition / Version:
- 1
- Volume:
- 16
- Issue:
- 23
- ISSN:
- 1991-9603
- Page Range / eLocation ID:
- 7143 to 7170
- Subject(s) / Keyword(s):
- ["sea surface temperature","remote sensing"]
- Format(s):
- Medium: X Size: 26.5MB Other: pdf
- Size(s):
- ["26.5MB"]
- Sponsoring Org:
- National Science Foundation
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- Free Publicly Accessible Full Text
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Accepted Manuscript1.0
- Journal Article:
- https://doi.org/10.5194/gmd-16-7143-2023
