The late Ordovician carbonate sedimentation as a major triggering factor of the Hirnantian glaciation
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چکیده
منابع مشابه
structure of tropical seas during the Late Ordovician Hirnantian glaciation Lipid biomarkers record fundamental changes in the microbial community
The Late Ordovician mass extinction was linked to climate cooling and glaciation of Gondwana during the terminal Ordovician Hirnantian Age (444.7–443.4 Ma). Extinction patterns have been well described for many marine taxa, but much less is known about marine microbial communities through this interval. To elucidate the structure of microbial communities in tropical marine basins through the La...
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ژورنال
عنوان ژورنال: Bulletin de la Société Géologique de France
سال: 2002
ISSN: 1777-5817,0037-9409
DOI: 10.2113/173.6.569