The Precambrian Climate
Author:
Publisher
Springer International Publishing
Link
http://link.springer.com/content/pdf/10.1007/978-3-030-24982-3_26
Reference31 articles.
1. Bodiselitsch, B., Koeberl, C., Master, S., & Reimold, W. U. (2005). Estimating duration and intensity of Neoproterozoic snowball Glaciations from Ir Anomalies. Science, 308(5719), 239–242.
2. Caldeira, K., & Kasting, J. F. (1992). Susceptibility of the early earth to irreversible Glaciation caused by carbon dioxide clouds. Nature, 359, 226–228.
3. Catling, D. C., & Claire, M. W. (2005). How Earth’s atmosphere evolved to an oxic state: A status report. Earth and Planetary Science Letters, 237, 1–20.
4. Donnadieu, Y., Fluteau, F., Ramstein, G., Ritz, C., & Besse, J. (2003). Is there a conflict between the Neoproterozoic Glacial deposits and the Snowball Earth interpretation: An improved understanding with numerical modeling. Earth and Planetary Science Letters, 08, 101–112.
5. Donnadieu, Y., Goddéris, Y., Ramstein, G., Nédelec, A., & Meert, J. G. (2004). Snowball EARTH triggered by continental break-up through changes in runoff. Nature, 428, 303–306.
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