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...
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 ...
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...
supported by the Strategic Priority Research Program of the Chinese Academy of Sciences(No.XDB26000000);the National Science and Technology Major Project of China(No.2017ZX05035002-001);the National Natural Science Foundation of China(Nos.41972162 and 41725007);the Estonian Research Council(No.PRG836)。
The age of the Silurian Lower Red Beds in the Upper Yangtze region remains debatable.Twenty-four samples were collected for conodont biostratigraphical studies from the Paiyunan Formation in the Sanbaiti Section,Huayi...
supported by the National Natural Science Foundation of China(Nos.41830320,45172002,41661134047)。
Based on a study of 49 conodont and 57 geochemical samples from the Upper Triassic,carbonate-dominated Dengdengqiao Formation,Qinling Basin,China,the Carnian conodonts and carbon isotope records are first reported.Two...
supported by the National Natural Science Foundation of China(Nos.41830320,45172002,41661134047)。
Mockina slovakensis,thought to have evolved from Epigondolella praeslovakensis,is an important species of the Norian(Upper Triassic),generally considered as the representative of the uppermost Alaunian to upper Sevati...
supported by the grants PRIN to Manuel Rigo(No.2017W2MARE);the China Scholarship Council to Yixing Du(No.201708510096);Development of conodont oxygen isotopic analysis by SHRIMP was supported by Australian Research Council Discovery to Ian S.Williams(No.DP1096252)。
During their last phase of evolution,the pectiniform conodont elements manifested an evident trend of simplification and miniaturization.This phase started from the late Norian(Sevatian)in the Late Triassic and the ev...