New constraints on equatorial temperatures during a Late Neoproterozoic snowball Earth glaciation

Intense glaciation during the end of Cryogenian time (∼635 million years ago) marks the coldest climate state in Earth history – a time when glacial deposits accumulated at low, tropical paleolatitudes. The leading idea to explain these deposits, the snowball Earth hypothesis, predicts globally froz...

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Veröffentlicht in:	Earth and planetary science letters 2014-11, Vol.406, p.110-122
Hauptverfasser:	Ewing, Ryan C., Eisenman, Ian, Lamb, Michael P., Poppick, Laura, Maloof, Adam C., Fischer, Woodward W.
Format:	Artikel
Sprache:	eng
Schlagworte:	aeolian Cryogenian Deformation Earth Estimates Freezing Geology Grounds paleoclimate periglacial Sand snowball Earth Surface temperature
Online-Zugang:	Volltext
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