Wang Cheng-yuan
Abstract
A conodont species, Mesogondolella idahoensis, is found in south Mongolia near Chinese-Mongolian border from the Lugiingol Formation. This formation should be assigned to the Lower Permian Kungurian Stage rather than the Upper Permian as previously dated.
OpenAlex reports 1 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
A conodont species, Mesogondolella idahoensis, is found in south Mongolia near Chinese-Mongolian border from the Lugiingol Formation. This formation should be assigned to the Lower Permian Kungurian Stage rather than the Upper Permian as previously dated.
Key concepts: Conodont, Permian, Paleontology, Geology, Southeast asia, Stage (stratigraphy), Inner mongolia, Geography