中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
PALEOENVIRONMENTAL DISTRIBUTION OF ORDOVICIAN CALCIMICROBIAL ASSOCIATIONS IN THE TARIM BASIN, NORTHWEST CHINA

文献类型:期刊论文

作者Liu, Lijing1; Wu, Yasheng1; Jiang, Hongxia1; Wu, Naiqin2; Jia, Lianqi1
刊名PALAIOS
出版日期2017-07-01
卷号32期号:7页码:462-489
ISSN号0883-1351
DOI10.2110/palo.2016.054
文献子类Article
英文摘要The stratigraphic and facies distribution of 20 calcimicrobial genera (including calcified cyanobacteria and associated problematic calcified microfossils) are reported for the entire Ordovician succession in the Tarim Basin in northwestern China based on examination of drill cores and 8500 thin sections from 64 wells from the Tabei, Bachu, Tazhong, and Tadong uplifts. A total of ten calcimicrobial associations are recognized in the Lower to Upper Ordovician based on taxonomic composition and distribution within four paleoenvironment types: reef (marginal and patch reef), open platform/bank (marginal and patch bank), lagoon, and tidal flat. The temporal distribution of the calcimicrobial genera closely follows changes in sedimentary environments; an extensive literature survey reveals similar relationships in much of the Paleozoic and Mesozoic. Based on their paleoenvironmental preferences, calcimicrobes can be classified into five paleohabitat types: (1) reef-adapted (Acuasiphonoria, Razumovskia, Phacelophyton, Gomphosiphon, Epiphyton, Renalcis, and Izhella); (2) open platform/bank-adapted (Subtifloria and Bevocastria); (3) both reef and open platform/bank-adapted (Bija, Apophoretella, Rothpletzella, and Wetheredella); (4) lagoon-adapted (Hedstromia, Cayeuxia, Zonotrichites, Ortonella, and Garwoodia), and (5) not only reef and open platform/bank-adapted but also tolerant of tidal flat conditions (Girvanella and Proaulopora). The occurrences of these calcimicrobes in strata not only can indicate ancient sedimentary facies but also can reveal paleoecological parameters of ancient seas, such as nutrient levels (e.g., N and P), predation pressure, and sea level, especially in strata absence of other well-studied facies fossils.
WOS关键词CARBONATE PLATFORM MARGIN ; SEA-LEVEL FLUCTUATION ; SOUTH CHINA ; NW CHINA ; LIANGLITAG FORMATION ; CALCAREOUS ALGAE ; MICROBIAL REEFS ; TAZHONG AREA ; CALCIFIED CYANOBACTERIA ; MARINE CYANOBACTERIA
WOS研究方向Geology ; Paleontology
语种英语
WOS记录号WOS:000406237100004
出版者SEPM-SOC SEDIMENTARY GEOLOGY
资助机构National Natural Science Foundation of China(41502004 ; 41502148 ; 41372121) ; National Natural Science Foundation of China(41502004 ; 41502148 ; 41372121) ; National Natural Science Foundation of China(41502004 ; 41502148 ; 41372121) ; National Natural Science Foundation of China(41502004 ; 41502148 ; 41372121)
源URL[http://ir.iggcas.ac.cn/handle/132A11/61835]  
专题地质与地球物理研究所_中国科学院油气资源研究重点实验室
通讯作者Wu, Yasheng
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
推荐引用方式
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Liu, Lijing,Wu, Yasheng,Jiang, Hongxia,et al. PALEOENVIRONMENTAL DISTRIBUTION OF ORDOVICIAN CALCIMICROBIAL ASSOCIATIONS IN THE TARIM BASIN, NORTHWEST CHINA[J]. PALAIOS,2017,32(7):462-489.
APA Liu, Lijing,Wu, Yasheng,Jiang, Hongxia,Wu, Naiqin,&Jia, Lianqi.(2017).PALEOENVIRONMENTAL DISTRIBUTION OF ORDOVICIAN CALCIMICROBIAL ASSOCIATIONS IN THE TARIM BASIN, NORTHWEST CHINA.PALAIOS,32(7),462-489.
MLA Liu, Lijing,et al."PALEOENVIRONMENTAL DISTRIBUTION OF ORDOVICIAN CALCIMICROBIAL ASSOCIATIONS IN THE TARIM BASIN, NORTHWEST CHINA".PALAIOS 32.7(2017):462-489.

入库方式: OAI收割

来源:地质与地球物理研究所

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