A proposed new global stratotype for Aeronian Stage of the Silurian System: Hlásná Třebaň section, Czech Republic. (12th October 2017)

• Record Type: Journal Article
• Authors: Štorch, Petr; Manda, Štěpán; Tasáryová, Zuzana; Frýda, Jiří; Chadimová, Leona; Melchin, Michael J.
• Is Part Of: Lethaia. Volume 51:Number 3(2018)
• Page Start: 357
• Page End: 388
• Publication Date: 2017-10-12
• Subjects: Aeronian -- geochemistry -- graptolites -- GSSP proposal -- Silurian; Paleontology -- Periodicals; Geology, Stratigraphic -- Periodicals; 560
• DOI: 10.1111/let.12250
• Languages: English
• ISSNs: 0024-1164

Abstract

Abstract : The current Global Stratotype Section and Point (GSSP) for the Aeronian Stage (Llandovery Series, Silurian System), on Trefawr track in the Llandovery area of Wales, is an inadequate marker for precise, global, correlation. The International Subcommission on Silurian Stratigraphy has, therefore, undertaken the selection of a new GSSP for this level. The lowest occurrence of the graptolite Demirastrites triangulatus, 1.38 m above the base of the black‐shale succession of the Želkovice Formation at the Hlásná Třebaň section in Central Bohemia, is proposed to mark the base of the Aeronian Stage. The section, which fulfils all formal requirements for stratotype of a chronostratigraphical unit, should be considered as a candidate for the new GSSP. An abundant, well‐preserved, diverse graptolite fauna occurs through the section along with common chitinozoans, which indicate that the Spinachitina maennili Biozone spans the boundary interval. The section comprises the lower–middle Aeronian ( D. triangulatus–Lituigraptus convolutus graptolite biozones) along with underlying Rhuddanian ( Akidograptus ascensus–Coronograptus cyphus biozones) and Hirnantian strata. Several graptolite genera of primary importance in global correlation ( Demirastrites, Petalolithus, Rastrites and Campograptus ) first appear in the lower part of the triangulatus Biozone. The structurally simple section is somewhat condensed, but there is a uniform succession of black shale without any evidence of disconformity in the broad boundary interval. The Corg isotope record exhibits a minor positive excursion just above the base of the triangulatus Biozone, whereas TOC and N isotope and elemental geochemical records provide evidence for uninterrupted sedimentation under stable, anoxic conditions.