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Autor:
Julius Eberhard, Oliver E. Bevan, Georg Feulner, Stefan Petri, Jeroen van Hunen, James U.L. Baldini
The Cryogenian period (720–635 million years ago) in the Neoproterozoic era featured two phases of global or near-global ice cover, termed ‘Snowball Earth’. Climate models of all kinds indicate that the inception of these phases must have occur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3370d71aa5dd937ae8ef3e3918cf65a9
https://doi.org/10.5194/egusphere-egu23-7084
https://doi.org/10.5194/egusphere-egu23-7084
