Environment and Age of the Upper Devonian‒Carboniferous Zhulumute and Hongguleleng Formations,Junggar Basin,NW China:Ichnological and Palynological Aspects  

作　　者：MichałS TACHACZ Marcelina KONDAS PawełFILIPIAK MA Xueping 

机构地区：[1]Institute of Geological Sciences,Jagiellonian University in Kraków,Gronostajowa 3a,30-387 Kraków,Poland [2]University of Silesia in Katowice,Faculty of Natural Sciences,Będzińska 60,41-200 Sosnowiec,Poland [3]School of Earth and Space Sciences,Peking University,Beijing 100871,China

出　　处：《Acta Geologica Sinica(English Edition)》2021年第3期724-739,共16页地质学报（英文版）

基　　金：the National Natural Science Foundation of China (Grant #41872003)

摘　　要：Two Upper Devonian to Lower Carboniferous sections,namely the Bulongguoer and Haer(Gennaren area)in the Junggar Basin,Central Asian Orogenic Belt,in northwestern China were examined with regard to ichnology and palynology.The deposits of the Hongguleleng Formation and Namu Member of the Heishantou Formation,respectively,are mostly unbioturbated or poorly bioturbated,with poorly diversified trace fossils,which indicate unfavourable conditions for the burrowing benthic community during the Late Devonian and Early Carboniferous.The main factor governing the growth of the bioturbating population was the rapid sedimentation of fine-grained,volcanic material documented as tempestites,which buried the benthic fauna.In the Bulongguoer section,the presence of miospores Teichertospora torquata and Grandispora gracilis enabled identification of the broad Teichertospora torquata–Grandispora gracilis Miospore Zone from the transitional Frasnian/Famennian interval.More accurate identification of palynostratigraphical levels(DE and CZ Miospore zones)is only tentative.On the basis of palynofacies analysis,samples from the lower Bulongguoer section indicate deposition in more proximal conditions,whereas samples from the top of the section indicate deposition in a more distal environment.In the Haer section,only a general biostratigraphic indication for the Tournaisian was possible,owing to poor preservation of organic matter.

关 键 词：trace fossils PALYNOLOGY event deposition Frasnian/Famennian/Tournaisian XINJIANG 

分 类 号：P534.4[天文地球—古生物学与地层学] P532[天文地球—地质学]