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Increased north African dust fluxes and higher productivity in the eastern equatorial Atlantic Ocean linked to stronger trade winds from about 2.7 million years ago

Increased north African dust fluxes and higher productivity in the eastern equatorial Atlantic Ocean linked to stronger trade winds from about 2.7 million years ago
Increased north African dust fluxes and higher productivity in the eastern equatorial Atlantic Ocean linked to stronger trade winds from about 2.7 million years ago
For at least the last 11 million years, the North African landscape has repeatedly oscillated on astronomical timescales between the dry dusty conditions of today and more humid, vegetated conditions such as those documented for the mid-Holocene. These changes were primarily driven by expansion and contraction of the tropical rainbelt in response to changes in summer insolation. However, other mechanisms are needed to explain temporal variability in the sensitivity of African humidity to this rhythmic forcing. A main interval of observed change is the Pliocene-Pleistocene transition (~3.5 to 2.4 Ma) when Africa is widely (but not universally) suggested to have become drier and dustier. Here we present new suborbitally resolved records of surface ocean temperature, foraminiferal stable isotopes and export productivity from the Northwest African margin and the eastern equatorial Atlantic Ocean and compare them to published records. We find strong coupling at astronomical timescales between productivity and dust fluxes throughout our study interval, indicating the sustained influence of the northeast trade winds on dust transport, upwelling strength and perhaps dust-driven ocean fertilization. We attribute observed increases in dust fluxes delivered to the NW African margin and eastern equatorial Atlantic to strengthening of the trade winds driven by the steepening latitudinal temperature gradients associated with the intensification of Northern Hemisphere glaciation. Taken together with published evidence of increased strength in the mid-latitude westerlies at this time, our results point to invigoration of large-scale atmospheric circulation globally during intensified glacial periods of the Pliocene-Pleistocene transition.
Africa, Atlantic, Pliocene, dust, productivity, temperature
2572-4525
Crocker, Anya J.
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Jewell, Amy M.
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Mitsunaga, Bryce A.
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Buchanan, Solana
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Brombacher, Anieke
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Hambach, Bastian
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Wilding, Megan R.
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Westerhold, Thomas
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Röhl, Ursula
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Russell, James M.
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Herbert, Timothy D.
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Xuan, Chuang
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Wilson, Paul A.
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Crocker, Anya J.
1215fbdd-ad43-408a-bd79-c54c6847e68c
Jewell, Amy M.
3de1a5a3-b62c-4069-a06e-b2fedb6456e7
Mitsunaga, Bryce A.
9ec9810e-c7aa-47b6-9598-1c5b7a33145b
Buchanan, Solana
78852e7e-2663-494d-a4b2-cdea5bddbcb8
Brombacher, Anieke
2a4bbb84-4743-4a36-973b-4ad2bf743154
Hambach, Bastian
d144b919-bc71-4793-89ee-7fdfdb7762bb
Wilding, Megan R.
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Westerhold, Thomas
79660823-916e-4655-8fc4-be646f3c05fc
Röhl, Ursula
17b133fa-b6ab-4a96-9daf-0fc2f5531845
Russell, James M.
e5d0ffb6-610d-4158-a4ad-7d02cc6ce3b5
Herbert, Timothy D.
67ad95e9-6e05-4e13-aa20-3465eed47249
Xuan, Chuang
3f3cad12-b17b-46ae-957a-b362def5b837
Wilson, Paul A.
f940a9f0-fa5a-4a64-9061-f0794bfbf7c6

Crocker, Anya J., Jewell, Amy M., Mitsunaga, Bryce A., Buchanan, Solana, Brombacher, Anieke, Hambach, Bastian, Wilding, Megan R., Westerhold, Thomas, Röhl, Ursula, Russell, James M., Herbert, Timothy D., Xuan, Chuang and Wilson, Paul A. (2025) Increased north African dust fluxes and higher productivity in the eastern equatorial Atlantic Ocean linked to stronger trade winds from about 2.7 million years ago. Paleoceanography and Paleoclimatology, 40 (1), [e2024PA004891]. (doi:10.1029/2024PA004891).

Record type: Article

Abstract

For at least the last 11 million years, the North African landscape has repeatedly oscillated on astronomical timescales between the dry dusty conditions of today and more humid, vegetated conditions such as those documented for the mid-Holocene. These changes were primarily driven by expansion and contraction of the tropical rainbelt in response to changes in summer insolation. However, other mechanisms are needed to explain temporal variability in the sensitivity of African humidity to this rhythmic forcing. A main interval of observed change is the Pliocene-Pleistocene transition (~3.5 to 2.4 Ma) when Africa is widely (but not universally) suggested to have become drier and dustier. Here we present new suborbitally resolved records of surface ocean temperature, foraminiferal stable isotopes and export productivity from the Northwest African margin and the eastern equatorial Atlantic Ocean and compare them to published records. We find strong coupling at astronomical timescales between productivity and dust fluxes throughout our study interval, indicating the sustained influence of the northeast trade winds on dust transport, upwelling strength and perhaps dust-driven ocean fertilization. We attribute observed increases in dust fluxes delivered to the NW African margin and eastern equatorial Atlantic to strengthening of the trade winds driven by the steepening latitudinal temperature gradients associated with the intensification of Northern Hemisphere glaciation. Taken together with published evidence of increased strength in the mid-latitude westerlies at this time, our results point to invigoration of large-scale atmospheric circulation globally during intensified glacial periods of the Pliocene-Pleistocene transition.

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More information

Submitted date: 12 March 2024
Accepted/In Press date: 21 December 2024
Published date: 17 January 2025
Keywords: Africa, Atlantic, Pliocene, dust, productivity, temperature

Identifiers

Local EPrints ID: 498159
URI: http://eprints.soton.ac.uk/id/eprint/498159
ISSN: 2572-4525
PURE UUID: 649b4617-d36f-452f-9b44-917d45f7c6ff
ORCID for Anya J. Crocker: ORCID iD orcid.org/0000-0001-9561-5750
ORCID for Anieke Brombacher: ORCID iD orcid.org/0000-0003-2310-047X
ORCID for Bastian Hambach: ORCID iD orcid.org/0000-0003-4546-5672
ORCID for Megan R. Wilding: ORCID iD orcid.org/0000-0003-0063-2238
ORCID for Chuang Xuan: ORCID iD orcid.org/0000-0003-4043-3073
ORCID for Paul A. Wilson: ORCID iD orcid.org/0000-0001-6425-8906

Catalogue record

Date deposited: 11 Feb 2025 17:59
Last modified: 11 Sep 2025 02:59

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Contributors

Author: Anya J. Crocker ORCID iD
Author: Amy M. Jewell
Author: Bryce A. Mitsunaga
Author: Solana Buchanan
Author: Bastian Hambach ORCID iD
Author: Thomas Westerhold
Author: Ursula Röhl
Author: James M. Russell
Author: Timothy D. Herbert
Author: Chuang Xuan ORCID iD
Author: Paul A. Wilson ORCID iD

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