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Neoproterozoic Glaciations and the Fossil Record

2013
Sedimentary, geochronological, and δ 13 C chemostratigraphic data require that at least three glaciations-the Sturtian, Marinoan, and Gaskiers in geochronological order-occurred in the Neoproterozoic glacial interval (NGI; ca. 750-580 Ma); at least the Gaskiers glaciation has not been demonstrated global in nature.
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The Neoproterozoic Geology of the Tarim Craton

2015
The Upper Proterozoic of the Tarim craton can be divided into the upper and lower parts. The lower part belongs to the Qingbaikouan System (1.0–0.85 Ga), including epimetamorphic carbonate–clastic rock series in the northeastern and southwestern margins of the craton, and blueschists in the northwestern margin of the craton.
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Trace Fossils: Neoproterozoic

2011
Sören Jensen   +2 more
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Neoproterozoic Atmospheres and Glaciation

2014
Y. Donnadieu, Y. Goddéris, G. Le Hir
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A full-plate global reconstruction of the Neoproterozoic

Gondwana Research, 2017
Andrew S Merdith   +2 more
exaly  

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