|کد مقاله||کد نشریه||سال انتشار||مقاله انگلیسی||ترجمه فارسی||نسخه تمام متن|
|4463291||1313621||2016||3 صفحه PDF||سفارش دهید||دانلود کنید|
• Fungal spores illustrated by Bercovici et al. (2015) conform to revision of Reduviasporonites by Foster et al. (2002).
• Presence of Reduviasporonites in the South-China terrestrial PTB sections is maintained.
• Contamination by modern fungal spores is unlikely, as it would affect most samples.
• Paleoecology and significance of PTB fungal spike event are still not fully elucidated.
The Permian–Triassic boundary interval in China comprises a significant record of faunal and floral changes during this important extinction event. Here we discuss the details of palynomorph preservation at the classical Western Guizhou and Eastern Yunnan sections in an effort to expand the stratigraphy and paleontology from these earlier studies.
Journal: Global and Planetary Change - Volume 143, August 2016, Pages 31–33