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Foraminiferal biostratigraphy of the Visean–Serpukhovian (Mississippian) boundary interval at slope and platform sections in southern Guizhou (South China)

Published online by Cambridge University Press:  20 May 2016

John R. Groves ,
Wang Yue ,
Qi Yuping ,
Barry C. Richards ,
Katsumi Ueno  and
Wang Xiangdong
John R. Groves
Affiliation:
Department of Earth Science, University of Northern Iowa, Cedar Falls, IA 50614-0335, USA
Wang Yue
Affiliation:
State Key Laboratory of Paleobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Science, 39 East Beijing Road, Nanjing 210008, China
Qi Yuping
Affiliation:
State Key Laboratory of Paleobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Science, 39 East Beijing Road, Nanjing 210008, China
Barry C. Richards
Affiliation:
Geological Survey of Canada, 3303 33rd Street, NW, Calgary AB, T2L 2A7, Canada
Katsumi Ueno
Affiliation:
Department of Earth System Science, Fukuoka University, Fukuoka 814-0180, Japan
Wang Xiangdong
Affiliation:
State Key Laboratory of Paleobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Science, 39 East Beijing Road, Nanjing 210008, China
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Abstract

The Visean–Serpukhovian boundary is not yet defined by a Global Stratotype Section and Point (GSSP) but it is recognizable operationally by the appearance of the conodont Lochriea ziegleri in the L. nodosa–L. ziegleri chronocline. Foraminiferal successions across this boundary in the type area of the Serpukhovian Stage (Moscow Basin, Russia), elsewhere in Russia and in the central United States suggest that the appearances of Asteroarchaediscus postrugosus, Janischewskina delicata, Eolasiodiscus donbassicus, and specimens controversially referred to “Millerella tortula” are reliable, auxiliary indices to the base of the Serpukhovian. In southern Guizhou Province, China, Visean–Serpukhovian rock sequences from slope and platform settings have yielded rich associations of conodonts and foraminifers, respectively. The Nashui section is a leading candidate for the Serpukhovian GSSP because its slope deposits contain an uninterrupted record of conodont occurrences including the L. nodosa–L. ziegleri transition. Foraminifers recovered from the Nashui section are comparatively rare and include none of the basal Serpukhovian indices. In contrast, the nearby Yashui section represents a platform interior setting in which foraminifers flourished and conodonts were nearly absent. The base of the Serpukhovian at Yashui is marked approximately by the appearance of “tortula-like” specimens. Although it is not possible to correlate biostratigraphically between the Nashui and Yashui sections, the occurrence of “tortula-like” specimens at the Yashui section allows correlation with the mid-Venevian Substage of the Moscow Basin at a level coinciding with the appearance of L. ziegleri. Together, the slope and platform sections comprise an informative biostratigraphic reference area for micropaleontologic characterization of the Visean–Serpukhovian boundary in southern Guizhou.

Type
Research Article
Information
Journal of Paleontology , Volume 86 , Issue 5 , September 2012 , pp. 753 - 774
Copyright
Copyright © The Paleontological Society 

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