Bulk sediment parameter of three sediment cores from permafrost lowlands, Alaska Arctic Coastal Plain

Arctic lowland landscapes have been modified by thermokarst lake processes throughout the Holocene. Thermokarst lakes form as a result of ice-rich permafrost degradation and they may expand over time through thermal and mechanical shoreline erosion. We studied proximal and distal sedimentary records...

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Bibliographic Details
Main Authors: Lenz, Josefine, Jones, Benjamin M, Wetterich, Sebastian, Tjallingii, Rik, Fritz, Michael, Arp, Chistopher D, Rudaya, Natalia, Grosse, Guido
Format: Dataset
Language:English
Published: PANGAEA 2016
Subjects:
Ice
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.864814
https://doi.org/10.1594/PANGAEA.864814