Comment on“First Record of Hindeodus-Isarcicella Population in Lower Triassic of Slovenia”by Tea Kolar-Jurkovek and Bogdan Jurkovek in Palaeogeography,Palaeoclimatology,Palaeoecology,252:72-81  

作　　者：WU Yasheng JIANG Hongxia 

机构地区：[1]Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029

出　　处：《Acta Geologica Sinica(English Edition)》2009年第2期425-428,共4页地质学报（英文版）

基　　金：supported by the National Natural Science Foundation of China(no.:40472015).

摘　　要：Some conodonts described by Tea Kolar-Jurkovsek and Bogdan Jurkovsek （2007） from the Permian-Triassic boundary section in the Ziri area of western Slovenia are revised in this paper. One specimen that they assigned to Hindeodus parvus is tentatively regarded as Hindeodus cf. scalaris Wu 2005. Two specimens that they assigned to lsarcicella sp. A is changed to Hindeodus parvus. One specimen that they described as lsarcicella lobata Perri and Farabegoli is changed to Hindeodus crenatus Wu （2006）. One specimen that they assigned to Isarcicella turgida （Kozur, Mostler and Rahimi-Yazd） is changed to Hindeodus cf. parvus. Since these revisions, the three conodont zones that they defined have been correspondingly revised. Their first zone may belong to Hindeodus parvus zone, but it is not certain. Their second zone is changed to the Hindeodus parvus zone, and their third one remains as is.Some conodonts described by Tea Kolar-Jurkovsek and Bogdan Jurkovsek （2007） from the Permian-Triassic boundary section in the Ziri area of western Slovenia are revised in this paper. One specimen that they assigned to Hindeodus parvus is tentatively regarded as Hindeodus cf. scalaris Wu 2005. Two specimens that they assigned to lsarcicella sp. A is changed to Hindeodus parvus. One specimen that they described as lsarcicella lobata Perri and Farabegoli is changed to Hindeodus crenatus Wu （2006）. One specimen that they assigned to Isarcicella turgida （Kozur, Mostler and Rahimi-Yazd） is changed to Hindeodus cf. parvus. Since these revisions, the three conodont zones that they defined have been correspondingly revised. Their first zone may belong to Hindeodus parvus zone, but it is not certain. Their second zone is changed to the Hindeodus parvus zone, and their third one remains as is.

关 键 词：CONODONT Permian-Triassic boundary Hindeodus parvus Slovenia 

分 类 号：P618.130.2[天文地球—矿床学] TS202.3[天文地球—地质学]