author_facet Donnadieu, Yannick
Ramstein, Gilles
Fluteau, Frederic
Besse, Jean
Meert, Joseph
Donnadieu, Yannick
Ramstein, Gilles
Fluteau, Frederic
Besse, Jean
Meert, Joseph
author Donnadieu, Yannick
Ramstein, Gilles
Fluteau, Frederic
Besse, Jean
Meert, Joseph
spellingShingle Donnadieu, Yannick
Ramstein, Gilles
Fluteau, Frederic
Besse, Jean
Meert, Joseph
Geophysical Research Letters
Is high obliquity a plausible cause for Neoproterozoic glaciations?
General Earth and Planetary Sciences
Geophysics
author_sort donnadieu, yannick
spelling Donnadieu, Yannick Ramstein, Gilles Fluteau, Frederic Besse, Jean Meert, Joseph 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1029/2002gl015902 <jats:p>The main features of the low‐latitude Neoproterozoic glaciations remain the subject of controversial debates concerning possible triggers. Here we use an AGCM coupled with a slab ocean to test one of the earliest and simplest explanation for tropical glaciations: a higher obliquity of the Earth's rotation axis. We show that high obliquity may result in an extensive glaciation during the Sturtian episode (750 Ma), due to the location of continental masses in the tropical areas, but cannot produce a large glaciation in the case of mid to high latitude paleogeographies such as those thought to typify the Varangian‐Vendian episodes (620–580 Ma).</jats:p> Is high obliquity a plausible cause for Neoproterozoic glaciations? Geophysical Research Letters
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title Is high obliquity a plausible cause for Neoproterozoic glaciations?
title_unstemmed Is high obliquity a plausible cause for Neoproterozoic glaciations?
title_full Is high obliquity a plausible cause for Neoproterozoic glaciations?
title_fullStr Is high obliquity a plausible cause for Neoproterozoic glaciations?
title_full_unstemmed Is high obliquity a plausible cause for Neoproterozoic glaciations?
title_short Is high obliquity a plausible cause for Neoproterozoic glaciations?
title_sort is high obliquity a plausible cause for neoproterozoic glaciations?
topic General Earth and Planetary Sciences
Geophysics
url http://dx.doi.org/10.1029/2002gl015902
publishDate 2002
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description <jats:p>The main features of the low‐latitude Neoproterozoic glaciations remain the subject of controversial debates concerning possible triggers. Here we use an AGCM coupled with a slab ocean to test one of the earliest and simplest explanation for tropical glaciations: a higher obliquity of the Earth's rotation axis. We show that high obliquity may result in an extensive glaciation during the Sturtian episode (750 Ma), due to the location of continental masses in the tropical areas, but cannot produce a large glaciation in the case of mid to high latitude paleogeographies such as those thought to typify the Varangian‐Vendian episodes (620–580 Ma).</jats:p>
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author Donnadieu, Yannick, Ramstein, Gilles, Fluteau, Frederic, Besse, Jean, Meert, Joseph
author_facet Donnadieu, Yannick, Ramstein, Gilles, Fluteau, Frederic, Besse, Jean, Meert, Joseph, Donnadieu, Yannick, Ramstein, Gilles, Fluteau, Frederic, Besse, Jean, Meert, Joseph
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description <jats:p>The main features of the low‐latitude Neoproterozoic glaciations remain the subject of controversial debates concerning possible triggers. Here we use an AGCM coupled with a slab ocean to test one of the earliest and simplest explanation for tropical glaciations: a higher obliquity of the Earth's rotation axis. We show that high obliquity may result in an extensive glaciation during the Sturtian episode (750 Ma), due to the location of continental masses in the tropical areas, but cannot produce a large glaciation in the case of mid to high latitude paleogeographies such as those thought to typify the Varangian‐Vendian episodes (620–580 Ma).</jats:p>
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spelling Donnadieu, Yannick Ramstein, Gilles Fluteau, Frederic Besse, Jean Meert, Joseph 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1029/2002gl015902 <jats:p>The main features of the low‐latitude Neoproterozoic glaciations remain the subject of controversial debates concerning possible triggers. Here we use an AGCM coupled with a slab ocean to test one of the earliest and simplest explanation for tropical glaciations: a higher obliquity of the Earth's rotation axis. We show that high obliquity may result in an extensive glaciation during the Sturtian episode (750 Ma), due to the location of continental masses in the tropical areas, but cannot produce a large glaciation in the case of mid to high latitude paleogeographies such as those thought to typify the Varangian‐Vendian episodes (620–580 Ma).</jats:p> Is high obliquity a plausible cause for Neoproterozoic glaciations? Geophysical Research Letters
spellingShingle Donnadieu, Yannick, Ramstein, Gilles, Fluteau, Frederic, Besse, Jean, Meert, Joseph, Geophysical Research Letters, Is high obliquity a plausible cause for Neoproterozoic glaciations?, General Earth and Planetary Sciences, Geophysics
title Is high obliquity a plausible cause for Neoproterozoic glaciations?
title_full Is high obliquity a plausible cause for Neoproterozoic glaciations?
title_fullStr Is high obliquity a plausible cause for Neoproterozoic glaciations?
title_full_unstemmed Is high obliquity a plausible cause for Neoproterozoic glaciations?
title_short Is high obliquity a plausible cause for Neoproterozoic glaciations?
title_sort is high obliquity a plausible cause for neoproterozoic glaciations?
title_unstemmed Is high obliquity a plausible cause for Neoproterozoic glaciations?
topic General Earth and Planetary Sciences, Geophysics
url http://dx.doi.org/10.1029/2002gl015902