新疆轮南油田上奥陶统良里塔格组生物类群和古生态地层学  

Biota and palaeoecology of the Upper Ordovician Lianglitag Formation in Lunnan Oil Field,Xinjiang,NW China

作　　者：张园园[1] 王冠[2] 张云峰[3] 李越[1] ZHANG Yuan-yuan;WANG Guan;ZHANG Yun-feng;LI Yue(State Key Laboratory of Paleobiology and Stratigraphy,Nanjing Institute of Geology,Chinese Academy of Sciences,Nanjing 210008,China;Key Laboratory of Ocean and Marginal Sea Geology,South China Sea Institute of Oceanology,Chinese Academy of Sciences,Guangzhou,510301,China;School of Geoscience and Technology,Southwest Peroleum University,Chengdu,610500,China)

机构地区：[1]现代古生物学和地层学国家重点实验室,中国科学院南京地质古生物研究所,南京210008 [2]中国科学院边缘海与大洋地质重点实验室,中国科学院南海海洋研究所,广州510301 [3]西南石油大学地球科学与技术学院,成都610500

出　　处：《古生物学报》2023年第1期98-112,共15页Acta Palaeontologica Sinica

基　　金：国家自然科学基金(41702028)资助。

摘　　要：南疆塔里木板块北部轮南油田在上奥陶统良里塔格组沉积期显示大致由东向西加深的陆表海缓坡地貌,19口钻井岩芯灰岩中可鉴定出钙质微生物Renalcis、Girvanella、Wetheredella、Garwoodia、Phacelophyton yushanensis、Hedstroemia?和Halysis;钙藻类Vermiporella、Dasyporella、Plexavaria和Solenopora;后生动物类型含海绵、珊瑚、苔藓虫、三叶虫、腕足动物、棘皮动物、腹足类、介形类等。不同钻井之间的古生态地层单元对比显示生物礁和灰泥丘主要发育于轮南油田西部井区,而东部井区则多为台内碎屑滩相沉积;海底地貌差异,特别是向西水深加大可视为控制轮南油田良里塔格组生态组合展布的主要因素。Ordovician carbonate deposits in the Tarim Block are considered as key targets for oil-gas explorations.Limestones of the Upper Ordovician Lianglitag Formation in Lunnan Oil Field,Tabei Uplift of northern Tarim Block,are considered to be economically significant reservoirs.The present paper demonstrates biotic and taphonomic features of the limestones in drill cores of 19 wells from Lunnan Oil Field.Index profiles of grain size,sorting and rounding,as well as grain/matrix ratio,are comprehensively described for ecological unit divisions in individual wells;palaeoecological correlations between the wells are outlined.The limestone-dominated sequences of the Lianglitag Formation were deposited on a westward deepening ramp in an epicontinental sea setting,in which high-clarity water and warm and shallow marine-floor were favorable for the thriving of the benthic biota.Intraclasts with diverse components and fabrics were identified under a polarizing microscope;abundant non-skeletal grains and fossils were also examined.Biotic structures are composed of calcimicrobes of Renalcis,Girvanella,Wetheredella,Garwoodia,Phacelophyton yushanensis,Hedstroemia and Halysis;calcareous algae of Vermiporella,Dasyporella,Dimorphosiphon,Plexavaria,Solenopora;metazoans of sponges,corals,bryozoa,trilobites,brachiopods,echinodermata,gastropods,ostracoda and others.Bioclasts are the key components in these limestones.With respect to lithological categories,the limestones are grouped into three microfacies types:Type 1 represents reefal units distinguished by coarse autochthonous bindstones and bafflestones in many wells.Bindstones,dominated by microbial and calcareous algal(e.g.,Verminporella,Hedstroemia)fabrics binding peloids,bioclasts and intraclasts,are more common.Stomatopora-algal frameworks occur sparsely in several drill cores.The reefal units are mostly several meters in thickness and low relief morphology.Calcimicrobial forms and calcareous algae are notable components in most reef-building units.Calcimicrobes and calcareous al

关 键 词：生物组成 古生态单元 良里塔格组 上奥陶统 塔里木板块北部 

分 类 号：P618.13[天文地球—矿床学] Q911[天文地球—地质学]