IF 2.7 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Gui-chun Wu , Zhan-sheng Ji , Gary G. Lash
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引用次数: 0

摘要

牙形石生物地层学研究表明,三叠纪LSB处于碳酸盐岩台地环境,而非突出陆块。下三叠统的沉积序列可分为灰岩为主和白云岩为主。在灰岩为主的剖面上建立了较完整的早-晚三叠世牙形石序列。相比之下,在白云岩为主的剖面上只描述了一个粗略的早三叠世硬齿目-厚齿目动物群。本文对LSB西部狮泉河地区白云岩为主的类型演替进行了研究,首次发现了3个早三叠世和2个中三叠世牙形石动物群。它们依次为:晚Griesbachian -早Smithian Hadrodontina-Pachycladina区系、史密斯ian Pachycladina shiquania n. sp.区系、Spathian triassospathdus homeri- triassospthodus triangularis组合带、早期ladian Neogondolella transita-Neogondolella excelsa-Neogondolella cornuta区系、Late ladian Budurovignathus c . diebeli- pseudofurnishus murcianus区系。早至中三叠世牙形石动物群的恢复使白云岩为主的三叠纪地层得到了更有力的重新定义。石泉河地区的牙形石序列与其他地区的牙形石序列对比表明,牙形石序列优先沿低古纬度白云岩为主的地层发育。在古地理分布上,石泉河地区与欧洲的亲缘关系比与美国西部的亲缘关系更近,形成了下三叠统Pachycladina动物群和Ladinian物种Neogondolella excelsa,以及更为丰富的Budurovignathus物种。此外,一个新发现的物种Pachycladina shiquania n. sp保存完好的平台状元件为Pachycladina仪器的P1和P2元件提供了澄清。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Newly discovered Early to Middle Triassic Conodont faunas in the Shiquanhe area, western Lhasa Block, Xizang (Tibet) and their biostratigraphic and palaeobiogeographic implications
Conodonts have taken on a significant role in elucidating the sedimentary setting as well as geological history of the Lhasa Block (LSB) of Xizang (Tibet). Conodont biostratigraphic research indicates that the LSB was in carbonate platform setting rather than an emergent land mass during Triassic. Lower Triassic sedimentary successions of the LSB are classified as limestone-dominated and dolomite-dominated types. A relatively complete Early to Late Triassic conodont succession has been established for the limestone-dominated sections. In contrast, only a rough Early Triassic Hadrodontina-Pachycladina fauna has been described from dolomite-dominated sections. Our investigations of the dolomite-dominated type succession of the Shiquanhe area of the western LSB document for the first time three Early Triassic and two Middle Triassic conodont faunas. They are, in ascending order, the Late Griesbachian to Early Smithian Hadrodontina (revised from previously described Hadrodontina-Pachycladina) fauna, the Smithian Pachycladina shiquania n. sp. fauna, the Spathian Triassospathodus homeri-Triassospathodus triangularis Assemblage Zone, the Early Ladinian Neogondolella transita-Neogondolella excelsa-Neogondolella cornuta fauna, and the Late Ladinian Budurovignathus cf. diebeli-Pseudofurnishius murcianus fauna. The recovered Early to Middle Triassic conodont faunas permit more robust redefinition of the dolomite-dominated Triassic strata. Correlations of the conodont succession of the Shiquanhe area with those in other areas confirm that ellisoniids-bearing conodont successions existed preferentially along dolomite-dominated strata of low paleo-latitude. They also confirm that the Shiquanhe area had a closer relationship with Europe than with the western USA in palaeobiogeographic distribution in yielding the Lower Triassic species Pachycladina fauna and Ladinian species Neogondolella excelsa and a more diverse Budurovignathus species. Moreover, well-preserved platform-like elements of a newly described species Pachycladina shiquania n. sp. provide clarification of the true P1 and P2 elements of the Pachycladina apparatus.
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来源期刊
CiteScore
5.90
自引率
10.00%
发文量
398
审稿时长
3.8 months
期刊介绍: Palaeogeography, Palaeoclimatology, Palaeoecology is an international medium for the publication of high quality and multidisciplinary, original studies and comprehensive reviews in the field of palaeo-environmental geology. The journal aims at bringing together data with global implications from research in the many different disciplines involved in palaeo-environmental investigations. By cutting across the boundaries of established sciences, it provides an interdisciplinary forum where issues of general interest can be discussed.
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