Holocene pore‐ice δ 18 O and δ 2 H records from drained thermokarst lake basins in the Old Crow Flats, Yukon, Canada
Abstract Thermokarst lakes form following the thaw of ice‐rich permafrost and drain after a few decades to millennia. Drained thermokarst lake basins (DTLBs) become epicenters for peat accumulation and re‐aggradation of ice‐rich permafrost. This re‐aggradation of permafrost may be interrupted by sub...
Published in: | Permafrost and Periglacial Processes |
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Main Authors: | , , , |
Other Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
2020
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Subjects: | |
Online Access: | http://dx.doi.org/10.1002/ppp.2073 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.2073 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.2073 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/ppp.2073 |