Effect of decreased solar luminosity on late Precambrian ice extent

Keywords

Geology, Deglaciation, Supercontinent, Precambrian, Glacial period

References

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Cited by

• Comings and Goings of Global Glaciations on a Neoproterozoic Tropical Platform in NamibiaPaul F. Hoffman, Alan J. Kaufman, Galen P. Halverson — 1998
• Climate sensitivity to changes in solar insolation in a simple coupled climate modelJørgen Bendtsen — 2002
• Low-latitude glaciation and rapid changes in the Earth's obliquity explained by obliquity–oblateness feedbackD. M. Williams, James F. Kasting, Lawrence A. Frakes — 1998
• Vulnerability of climate on Earth to sudden changes in insolationJørgen Bendtsen, Christian J. Bjerrum — 2002
• Neoproterozoic “snowball Earth”: Dynamic sea ice over a quiescent oceanJ. P. Lewis, Andrew J. Weaver, Stephen T. Johnston — 2003
• Factors that inhibit snowball Earth simulationChristopher J. Poulsen, Robert Jacob — 2004
• Role of the ocean in controlling atmospheric CO2 concentration in the course of global glaciationsAkira Oka, Eiichi Tajika, Ayako Abe‐Ouchi — 2011
• GCM response to Late Precambrian (∼590 Ma) ice—covered continentsSteven K. Baum, Thomas J. Crowley — 2001
• Precambrian tidal and glacial clastic deposits: implications for Precambrian Earth–Moon dynamics and palaeoclimateGeorge E. Williams — 1998
• The Neoproterozoic (1000–540 Ma) glacial intervals: No more snowball earth?Joseph G. Meert, Rob Van der Voo — 1994
• Ocean Circulation under Globally Glaciated Snowball Earth Conditions: Steady-State SolutionsYosef Ashkenazy, Hezi Gildor, Martin Lösch — 2014
• The Neoproterozoic climatic paradox: Equatorial palaeolatitude for Marinoan glaciation near sea level in South AustraliaP. W. Schmidt, George E. Williams — 1995
• GCM sensitivity test using increased rotation rate, reduced solar forcing and orography to examine low latitude glaciation in the neoproterozoicGregory S. Jenkins, L. A. Frakes — 1998
• A palaeomagnetic study of Empress 1A, a stratigraphic drillhole in the Officer Basin: evidence for a low-latitude position of Australia in the NeoproterozoicSergei Pisarevsky — 2001
• Glacio-epochs and the supercontinent cycle after ∼ 3.0 Ga: Tectonic boundary conditions for glaciationNick Eyles — 2008
• Precambrian clastic sedimentation systemsP.G. Eriksson, Kent C. Condie, Henrik Tirsgaard — 1998
• Climate forcings and the initiation of low‐latitude ice sheets during the Neoproterozoic Varanger glacial intervalMark A. Chandler, Linda E. Sohl — 2000
• Dehumidification over Tropical Continents Reduces Climate Sensitivity and Inhibits Snowball Earth InitiationRichard P. Fiorella, Christopher J. Poulsen — 2013
• Absence of a runaway ice-albedo feedback in the NeoproterozoicChristopher J. Poulsen — 2003
• Neoproterozoic ‘snowball Earth’ simulations with a coupled climate/ice-sheet modelWilliam T. Hyde, Thomas J. Crowley, Steven K. Baum — 2000

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