Articles | Volume 10, issue 5
https://doi.org/10.5194/esurf-10-1041-2022
https://doi.org/10.5194/esurf-10-1041-2022
Research article
 | 
28 Oct 2022
Research article |  | 28 Oct 2022

Yukon River incision drove organic carbon burial in the Bering Sea during global climate changes at 2.6 and 1 Ma

Adrian M. Bender, Richard O. Lease, Lee B. Corbett, Paul R. Bierman, Marc W. Caffee, James V. Jones, and Doug Kreiner

Data sets

Charley River Cosmogenic Isotope Data Collected 2019-2021 A. M. Bender https://doi.org/10.5066/P9DRHQIS

Fortymile River cosmogenic isotope and luminescence data collected 2016-2019 A. M. Bender https://doi.org/10.5066/P9XVMTAK

5 meter Alaska Digital Elevation Models (DEMs) US Geological Survey https://earthexplorer.usgs.gov

Expedition 323 Scientists: Carbonate analysis from IODP Hole 323-U1341A K. Takahashi, A. C. Ravelo, A. Zarikian, and A. Carlos https://doi.org/10.1594/PANGAEA.828376

Expedition 323 Scientists: Carbonate analysis from IODP Hole 323-U1341B K. Takahashi, A. C. Ravelo, A. Zarikian, and A. Carlos https://doi.org/10.1594/PANGAEA.828377

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Short summary
To understand landscape evolution in the mineral resource-rich Yukon River basin (Alaska and Canada), we mapped and cosmogenic isotope-dated river terraces along the Charley River. Results imply widespread Yukon River incision that drove increased Bering Sea sedimentation and carbon sequestration during global climate changes 2.6 and 1 million years ago. Such erosion may have fed back to late Cenozoic climate change by reducing atmospheric carbon as observed in many records worldwide.