کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4715864 1638674 2014 10 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Triggers of Permo-Triassic boundary mass extinction in South China: The Siberian Traps or Paleo-Tethys ignimbrite flare-up?
ترجمه فارسی عنوان
عاملان انقراض جرم مرزی پرمو تریاس در جنوب چین: تله های سیبری یا پالو تتیس مگنبرتر به وجود می آیند؟
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات ژئوشیمی و پترولوژی
چکیده انگلیسی


• Stratigraphic evidence suggests causal link between the PTB extinction and volcanic ash.
• Geochemistry suggests that the PTB ash was from a Paleo-Tethyan continental magmatic arc.
• Isotopes in zircons from the PTB ash exclude the possibility of a Siberian Traps source.
• Ignimbrite flare-up is a trigger for the PTB main extinction horizon.

Assessment of the synchroneity between the Siberian Traps and the Permo-Triassic boundary (PTB) mass extinction has led to the proposition that the Siberian flood volcanism was responsible for the severest biotic crisis in the Phanerozoic. However, recent studies suggest that the Siberian Traps may have postdated the main extinction horizon. In this paper, we demonstrate, using stratigraphy, a time and intensity coincidence between PTB volcanic ash and the main extinction horizon. Geochemistry of the PTB volcanic ashes in five sections in South China indicates that they were derived from continental magmatic arc. Zircons extracted from the PTB volcanic ashes have negative εHf(t) (− 12.9 to − 2.0) and δ18O (6.8 to 10.9‰), consistent with an acidic volcanism and a crustal-derived origin, and therefore exclude a genetic link between the PTB mass extinction and the Siberian Traps. On the basis of spatial variation in the number of the PTB volcanic ash layers and the thickness of the ash layers in South China, we propose that the PTB volcanic ash may be related to Paleo-Tethys continental arc magmatism in the Kunlun area. Ignimbrite flare-up related to rapid plate subduction during the final assemblage of the Pangea super-continent may have generated a volcanic winter, which eventually triggered the collapse of ecosystem and ultimately mass extinction at the end of the Permian. The Siberian Traps may have been responsible for a greenhouse effect and so have been responsible for both a second pulse of the extinction event and Early Triassic ecological evolution.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Lithos - Volume 204, 1 September 2014, Pages 258–267
نویسندگان
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