University of Vermont, Rubenstein School of the Environment and
Natural Resources, 80 Colchester Avenue, Burlington, Vermont 05405, USA
Marc W. Caffee
Purdue University, Department of Physics and Astronomy and Department of Earth, Atmospheric, and Planetary Sciences, 525 Northwestern Avenue, West Lafayette, Indiana 47907, USA
James V. Jones
Geological survey, Alaska Science Center, 4210 University Drive,
Anchorage, Alaska 99508, USA
Doug Kreiner
Geological survey, Alaska Science Center, 4210 University Drive,
Anchorage, Alaska 99508, USA
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2,124
1,385
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3,629
209
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PDF: 1,385
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Total: 3,629
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Cumulative views and downloads
(calculated since 08 Jun 2022)
Total article views: 2,792 (including HTML, PDF, and XML)
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1,583
1,113
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2,792
99
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HTML: 1,583
PDF: 1,113
XML: 96
Total: 2,792
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BibTeX: 133
EndNote: 172
Views and downloads (calculated since 28 Oct 2022)
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Total article views: 837 (including HTML, PDF, and XML)
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541
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Total: 837
Supplement: 110
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Views and downloads (calculated since 08 Jun 2022)
Cumulative views and downloads
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Total article views: 3,629 (including HTML, PDF, and XML)
Thereof 3,471 with geography defined
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Total article views: 2,792 (including HTML, PDF, and XML)
Thereof 2,684 with geography defined
and 108 with unknown origin.
Total article views: 837 (including HTML, PDF, and XML)
Thereof 787 with geography defined
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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.
To understand landscape evolution in the mineral resource-rich Yukon River basin (Alaska and...
