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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2,171
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PDF: 1,421
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Total: 3,762
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Views and downloads (calculated since 08 Jun 2022)
Cumulative views and downloads
(calculated since 08 Jun 2022)
Total article views: 2,907 (including HTML, PDF, and XML)
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1,623
1,139
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2,907
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HTML: 1,623
PDF: 1,139
XML: 145
Total: 2,907
Supplement: 142
BibTeX: 179
EndNote: 204
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Total article views: 855 (including HTML, PDF, and XML)
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548
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Total: 855
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Views and downloads (calculated since 08 Jun 2022)
Cumulative views and downloads
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Viewed (geographical distribution)
Total article views: 3,762 (including HTML, PDF, and XML)
Thereof 3,604 with geography defined
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Total article views: 2,907 (including HTML, PDF, and XML)
Thereof 2,799 with geography defined
and 108 with unknown origin.
Total article views: 855 (including HTML, PDF, and XML)
Thereof 805 with geography defined
and 50 with unknown origin.
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...
