funded by the National Research Foundation of Korea grants to BSL (No.2020R1A2C1099624) and to SJC (No.2021R1A2C1009687)
We reestablished the Serratognathus bilobatus Biozone in the Taebaek Group of Korea,where Serratognathus bilobatus was first reported by Lee(1970),based on new data from the uppermost Dumugol Formation to the Lower Ma...
supported by the National Natural Science Foundation of China(grant No.42172002).
The conodont genus Idiognathodus is one of the most important taxa in Pennsylvanian biostratigraphy.However,numerous unnamed species prevent us from understanding the evolutionary history of the genus and lower the po...
supported by the Centro de Investigaciones Geol ogicas Aplicadas (CIGEA) (FCEFy NUNC);the Secretaría de Ciencia y Tecnología (Se Cy T-UNC),Universidad Nacional de C ordoba,Argentina。
One of the largest Ordovician sea-level rises is the Evae transgression,which occurs in the lower part of the Oepikodus evae Biozone,indicative of a late Floian age.Specifically,the characteristics associated with the...
Conodonts,as a biotic group,next to ammonoids,pollen and spores,crustaceans and vertebrates,provide proxy clues for environment and age assessments of the rocks in which they occur.Conodonts are widely used for Triass...
financially supported by the China Geological Survey (Nos. DD20230219, DD20221635-004, DD20190054);the National Natural Science Foundation of China (Nos. 42272030, 41502013, 41772022, 41661134047);the Project of the Ministry of Science and Innovation of Spain (No. PID2020-117373GA-I00) to Carlos Martínez-Pérez.
Articulated natural assemblages contain direct evidence of the element numbers,morphologies,positions and structures for reconstructing the feeding apparatuses of conodont animals,but these kind of materials are very ...
The Late Devonian-early Carboniferous deposits of the Anarak section in northeastern Isfahan,Central Iran,evaluated based on conodont biostratigraphy,sedimentary environment and sequence stratigraphy.According to the ...
Conodont animal is an extinct group of marine animals.The conodont elements and their hard skeletal remains are originally from the head region of this kind of animal,and they are considered to be functioned as“teeth...
supported by the National Natural Science Foundation of China(Nos.41572078,41872106,42072013);the BGEG and GPMR laboratory funds(Nos.GKZ18Y660,GPMR201609)。
The Late Paleozoic Taiyuan Formation in North China is mainly composed of a mixed shallow-marine carbonate and terrigenous clastic deposits.Its basal limestones have been constrained in the late Pennsylvanian to Early...
funded by the Geological Survey of New South Wales。
Seven conodont biozones are recognized in the carbonate-dominated shelf-marine Middle Ordovician developed in the intracratonic sedimentary basins(Canning,Amadeus and Georgina)of central and north-western Australia,in...
The Ireviken Event was the first Middle Paleozoic event consisting of synchronised faunal,isotopic and facies change to be recognised.An analysis of the conodont faunas throughout the Boree Creek/Borenore Limestone su...