Cryogenic cave carbonate and implications for thawing permafrost at Winter Wonderland Cave, Utah, USA

Winter Wonderland Cave contains perennial ice associated with two types of cryogenic cave carbonate (CCC) formed during the freezing of water. CCC(fine) is characterized by relatively high δ(13)C values, whereas CCC(coarse) exhibits notably low δ(18)O values indicating precipitation under (semi)clos...

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Bibliographic Details
Published in:Scientific Reports
Main Authors: Munroe, Jeffrey, Kimble, Kristin, Spötl, Christoph, Marks, Gabriela Serrato, McGee, David, Herron, David
Format: Text
Language:English
Published: Nature Publishing Group UK 2021
Subjects:
Article
Ice
permafrost
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7979826/
http://www.ncbi.nlm.nih.gov/pubmed/33742010
https://doi.org/10.1038/s41598-021-85658-9
Description
Summary:Winter Wonderland Cave contains perennial ice associated with two types of cryogenic cave carbonate (CCC) formed during the freezing of water. CCC(fine) is characterized by relatively high δ(13)C values, whereas CCC(coarse) exhibits notably low δ(18)O values indicating precipitation under (semi)closed-system conditions in a pool of residual water beneath an ice lid. Previous work has concluded that CCC(coarse) forms during permafrost thaw, making the presence of this precipitate a valuable indicator of past cryospheric change. Available geochronologic evidence indicates that CCC formation in this cave is a Late Holocene or contemporary process, and field observations suggest that the cave thermal regime recently changed in a manner that permits the ingress of liquid water. This is the first documented occurence of CCC(coarse) in the Western Hemisphere and one of only a few locations where these minerals have been found in association with ice. Winter Wonderland Cave is a natural laboratory for studying CCC genesis.

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