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Collaborative Research: Geomorphic controls on sediment age, ice preservation, and carbon — NSF Award to Montana State University

Over half the Earth’s soil carbon resides in permafrost soils, defined as ground frozen for two years or longer, that are rapidly thawing at high latitudes. The cascading effects of this thaw include surface changes that threaten infrastructure, wholesale ecological change, and the release of carbon dioxide into the at

Award titleCollaborative Research: Geomorphic controls on sediment age, ice preservation, and carbon
Award ID2424218
AwardeeMontana State University
CityBOZEMAN
StateMT
Amount obligated$699,508
Principal investigatorJean Dixon
ProgramXC-Crosscutting Activities Pro, ANS-Arctic Natural Sciences
Start date08/15/2024
AbstractOver half the Earth’s soil carbon resides in permafrost soils, defined as ground frozen for two years or longer, that are rapidly thawing at high latitudes. The cascading effects of this thaw include surface changes that threaten infrastructure, wholesale ecological change, and the release of carbon dioxide into the atmosphere, all of which may be irreversible. Understanding potential future changes in these environments requires critical information about the modern variability of sediment, gro
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