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作 者:Mohsen Yazdi-Moghadam Mehdi Sarfi Mohammad Sharifi Aliakbar Taghipour
机构地区:[1]National Iranian Oil Company Exploration Directorate,Sheikh Bahaie Square,Tehran,1994814695,Iran [2]School of Earth Sciences,Damghan University,Damghan,3671641167,Iran [3]Department of Earth Sciences,Faculty of Sciences,University of Kurdistan,Sanandaj,Iran
出 处:《Journal of Palaeogeography》2023年第2期246-262,共17页古地理学报(英文版)
基 金:supported financially by National Iranian Oil Company Exploration Directorate。
摘 要:Postmiogypsinella intermedia Sirel and Gedik,2011 is reported for the first time from the shallow-marine limestones of the upper Chattian Qom Formation,Central Iran.This miogypsinid species has so far only been recorded from the upper Oligocene of Malatya(type locality)and Sivas(Central Anatolia)in eastern Turkey and from the upper Oligocene of the Prebetic Domain,SE Spain.The new record from Central Iran,paleobiogeographically located at the Eurasian margin of the Tethyan Seaway between the Western and Eastern Tethys realms,indicates that the paleogeographic distribution of this species has to be extended eastwards as far as Central Iran.This observation is not unexpected,since miogypsinid foraminifers with eccentric embryonic-nepionic apparatus(e.g.,Miogypsinella,Miogypsinoides,Miogypsina)are usually widely distributed.The accompanying larger benthic foraminifera,including Miogypsinoides complanatus(Schlumberger),Miogypsinoides formosensis Yabe and Hanzawa,Spiroclypeus margaritatus(Schlumberger),Operculina complanata(Defrance),and Risananeiza pustulosa Boukhary et al.,indicate the late Chattian age(corresponding to SBZ 23 Biozone).Postmiogypsinella intermedia is indicative of a shallow-marine middle ramp environment with oligotrophic conditions and inhabited the relatively deeper part of the photic zone.
关 键 词:Larger foraminifera Miogypsinidae BIOSTRATIGRAPHY Qom Formation Central Iran
分 类 号:Q915[天文地球—古生物学与地层学] P534.614[生物学—古生物学]
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