Start | View Uploaded Presentations | Author Index | Meeting Information GSA Annual Meeting in Seattle, Washington, USA 2017 Paper No. 2794 Presentation Time: 9:00 AM6:30 PM
BIOSTRATIGRAPHIC CONSTRAINT ON TONIAN SUCCESSIONS IN EASTERN NORTH CHINA BLOCK TANG, Qing1, PANG, Ke2, CHEN, Lei3, WAN, Bin4, XIAO, Shuhai1, ZHOU, Chuanming5, YUAN, Xunlai6 and HUA, Hong7, (1)Department of Geosciences, Virginia Tech, Blacksburg, VA 24061, (2)Department of Geosciences, Virginia Tech, Blacksburg, VA 24061; Chinese Academy of Sciences, Nanjing Institute of Geology and Paleontology, Nanjing, 210008, China, (3)College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, 266590, China, (4)Chinese Academy of Sciences, Nanjing Institute of Geology and Paleontology, Nanjing, 210008, China, (5)Laboratory of Economic Stratigraphy and Palaeogeography, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, 210008, China, (6)State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, 210008, China, (7)Northwest University Xi'an, Department of Geology, Xi'an 710069, China, Xi'an, 710069, China,
[email protected] Neoproterozoic is a critical era for the early evolution of life and its environment on the Earth. Neoproterozoic successions are widely distributed on the eastern margin of North China Block, including Shandong, southern Liaoning, northern Anhui, and northern Jiangsu provinces (also known as the JiaoLiaoXuHuai region). These successions are important for their abundant geobiological records and their key role in filling out a complete Neoproterozoic of China. However, the exact depositional ages of these successions have long been debated and were variously interpreted as Tonian (~1000–720 Ma), Cryogenian (~720–635 Ma), Ediacaran (~635–541 Ma), and even Cambrian. This is largely because the paleontological record of these strata is poorly documented and diagnostic Neoproterozoic fossils are rare. Recently, the biostratigraphy of Tonian has seen significant progress with several taxa proposed as diagnostically Tonian fossils, including the acanthomorphic acritarch Trachyhystrichosphaera aimika, VaseShaped Microfossils (VSM), and carbonaceous compression macrofossils of the ChuariaTawuiaPararenicolaProtoarenicola association. Therefore, it is important to critically reassess the paleontological record of the Neoproterozoic successions in Jiao LiaoXuHuai region. Our investigation, using low manipulation maceration technique and combined optical and electron microscopy, has revealed important Tonian fossils from these successions, including T. aimika from the Tumen Group and VSM from the Penglai Group in Shandong Province. Integrated with previously reported Tonian assemblages from the Huainan and Feishui groups in northern Anhui Province, the Huaibei Group in northern Jiangsu and northern Anhui provinces, and the Jinxian Group in southern Liaoning Province, our data suggest that the Neoproterozoic successions in the JiaoLiaoXuHuai region are mainly Tonian deposits. This is consistent with the available geochronological and chemostratigraphic data from these successions, which are overlain by Cambrian strata, with a >200 myr break in between.
Session No. 279Booth# 366 T254. The CoEvolution of Life and Its Environment during the Precambrian: The “Boring Billion” and MidProterozoic Emergence of Complex Life (Posters) Tuesday, 24 October 2017: 9:00 AM6:30 PM Halls 4EF (Washington State Convention Center) Geological Society of America Abstracts with Programs. Vol. 49, No. 6 doi: 10.1130/abs/2017AM300409 © Copyright 2017 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions. Back to: T254. The CoEvolution of Life and Its Environment during the Precambrian: The “Boring Billion” and MidProterozoic Emergence of Complex Life (Posters)
