Improved blattoid insect and conchostracan zonation for the Late Carboniferous, Pennsylvanian, of Euramerica

Author:

Schneider Joerg W.12ORCID,Scholze Frank3ORCID,Ross Andrew J.4,Blake Bascombe M.5,Lucas Spencer G.6ORCID

Affiliation:

1. Technical University Bergakademie Freiberg, Geological Institute, Bernhard-von-Cotta-Straße 2, 09599 Freiberg, Germany

2. Kazan Federal University, Institute of Geology and Petroleum Technologies, Kremlyovskaya street 18, Kazan, Russia

3. Friedrich-Schiller-Universität Jena, Institute of Geosciences, Burgweg 11, D-07749 Jena, Germany

4. National Museum of Scotland, Department of Natural Sciences, Chambers St, Edinburgh EH1 1JF, UK

5. West Virginia Geological and Economic Survey, 1 Mont Chateau Road, Morgantown, West Virginia, USA

6. New Mexico Museum of Natural History, 1801 Mountain Road NW, Albuquerque, New Mexico 87104, USA

Abstract

AbstractFor the biostratigraphy of mixed continental-marine and purely continental sections in the palaeotropical belt of Euramerica, 9 insect and 8 conchostracan zones are newly defined or improved. These zones encompass the time interval from the Early Pennsylvanian (middle Bashkirian) up into the early Permian (early Asselian) of the Euramercian biotic province. They are linked as much as possible to the marine Standard Global Chronostrigraphic Scale by common occurrences of insects and/or conchostracans with conodonts in mixed marine-continental sections as well as by the thus far available and reliable radioisotopic ages of associated volcanic rocks. This insect and conchostracan zonation is an alternative tool to the well-established macro-plant biostratigraphy of the Pennsylvanian. In contrast to the latter, only single specimens of insects or conchostracans, even if more rare than plant remains, allow biostratigraphic dating with a similar high temporal resolution.

Publisher

Geological Society of London

Subject

Geology,Ocean Engineering,Water Science and Technology

Reference177 articles.

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