A palynoflora of southern Xinjiang, China, and the proximity of the Tarim Plate to western Gondwana during the Llandovery (Silurian)
Wang, Kai1,2,3; Liu, Bing-Cai1,2,3; Wang, Yi1,2; Xu, Hong-He1,2
刊名JOURNAL OF ASIAN EARTH SCIENCES
2023-10-01
卷号255页码:13
关键词Palynomorphs Cryptospores Kalpintag Formation Llandovery Tarim
ISSN号1367-9120
DOI10.1016/j.jseaes.2023.105769
通讯作者Xu, Hong-He(hhxu@nigpas.ac.cn)
英文摘要The Tarim Plate, an independent continent during the Paleozoic, is of significance in understanding life and environment evolution; however, its paleogeography during the early Silurian is poorly known. Palynology, especially on land-derived palynomorphs, provides independent evidence for paleogeography as a supplement to paleomagnetic data. Here we recognize a Llandovery palynoflora of the Kalpintag Formation from two sections (Arisu and East Dawangou) in the northwestern Tarim Basin, southern Xinjiang, China, the paleontological evidence of which suggests that the Tarim Plate was proximal to western Gondwana during the early Silurian. The palynoflora consists of moderately diverse cryptospores with eight genera and twelve species, as represented by Laevolancis chibrikovae, Sphaerasaccus glabellus, Dyadospora murusdensa, Pseudodyadospora laevigata, P. petasus, and Tetrahedraletes medinensis. The monad S. glabellus reported herein is the first record from China. Other palynomorphs include a large number of sphaeromorph acritarchs, some tubes and cuticle-like sheets, and a few scolecodonts. The various kinds of meiosis process and predetermined diversity of older cryprospore producers in the Tarim Basin, together with ecological factors, contribute to the evolution of the Kalpintag cryptospore producers. By taxonomic comparisons of global coeval sporomorph records, combined with quantitative analyses (Cluster Analysis and Nonmetric Multidimensional Scaling Analysis), the Kalpintag palynoflora shows more closely related to those in northern Chad, northeastern Libya and central Saudi Arabia. The geographical zonation of sporomorphs might emerge in the Llandovery. The geographical proximity of the Tarim Plate to western Gondwana during that time is also suggested.
资助项目National Key Ramp;D Program of China[2022YFF0800200] ; Chinese Academy of Sciences[CAS-WX2021SF-0205]
WOS关键词ANGLO-WELSH BASIN ; LATE ORDOVICIAN ; PARANA BASIN ; MICROFOSSIL RECORD ; ANTICOSTI-ISLAND ; EVIDENCE BEARING ; LAND PLANTS ; CRYPTOSPORES ; EVOLUTION ; AGE
WOS研究方向Geology
语种英语
出版者PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号WOS:001058936500001
资助机构National Key Ramp;D Program of China ; Chinese Academy of Sciences
内容类型期刊论文
源URL[http://ir.nigpas.ac.cn/handle/332004/42665]  
专题中国科学院南京地质古生物研究所
通讯作者Xu, Hong-He
作者单位1.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China
2.Chinese Acad Sci, Ctr Excellence Life & Paleoenvironment, Nanjing 210008, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
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GB/T 7714
Wang, Kai,Liu, Bing-Cai,Wang, Yi,et al. A palynoflora of southern Xinjiang, China, and the proximity of the Tarim Plate to western Gondwana during the Llandovery (Silurian)[J]. JOURNAL OF ASIAN EARTH SCIENCES,2023,255:13.
APA Wang, Kai,Liu, Bing-Cai,Wang, Yi,&Xu, Hong-He.(2023).A palynoflora of southern Xinjiang, China, and the proximity of the Tarim Plate to western Gondwana during the Llandovery (Silurian).JOURNAL OF ASIAN EARTH SCIENCES,255,13.
MLA Wang, Kai,et al."A palynoflora of southern Xinjiang, China, and the proximity of the Tarim Plate to western Gondwana during the Llandovery (Silurian)".JOURNAL OF ASIAN EARTH SCIENCES 255(2023):13.
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