Orbital forcing of ice sheets during snowball Earth

Orbital forcing of ice sheets during snowball Earth

The snowball Earth hypothesis—that a runaway ice-albedo feedback can cause global glaciation—seeks to explain low-latitude glacial deposits, as well as geological anomalies including the re-emergence of banded iron formation and “cap” carbonates. One of the most significant challenges to snowball Ea...

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Bibliographic Details
Main Authors: Mitchell, Ross, Gernon, T.M., Cox, Grant, Nordsvan, Adam, Kirscher, Uwe, Xuan, C., Liu, Yebo, Liu, X., He, X.
Format: Journal Article
Language:English
Published: NATURE PORTFOLIO 2021
Subjects:
Science & Technology
Multidisciplinary Sciences
Science & Technology - Other Topics
NEOPROTEROZOIC IRON-FORMATION
GLACIATION
SEDIMENTARY
HISTORY
CYCLES
AGE
Online Access:http://purl.org/au-research/grants/arc/FL150100133
http://hdl.handle.net/20.500.11937/90462

Internet

http://purl.org/au-research/grants/arc/FL150100133
http://hdl.handle.net/20.500.11937/90462

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