In:
Paleoceanography and Paleoclimatology, American Geophysical Union (AGU), Vol. 39, No. 5 ( 2024-05)
Abstract:
The first high‐resolution tropical sea surface temperature record shows that the Miocene Climatic Optimum was ∼1.5°C warmer than the Early Miocene in the eastern equatorial Atlantic The West African Monsoon intensified following warming at ∼17 Ma, resulting in variable surface ocean conditions forced by orbital cycles Intensification of the monsoon system caused increased dust supply and strong upwelling alternating with hyperstratification
Type of Medium:
Online Resource
ISSN:
2572-4517
,
2572-4525
DOI:
10.1029/2023PA004767
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2024
detail.hit.zdb_id:
2916554-4
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