Javascript är avstängt eller blockerat i din webbläsare. Detta kan leda till att vissa delar av vår webbplats inte fungerar som de ska. Sätt på javascript för optimal funktionalitet och utseende.

Webbläsaren som du använder stöds inte av denna webbplats. Alla versioner av Internet Explorer stöds inte längre, av oss eller Microsoft (läs mer här: * https://www.microsoft.com/en-us/microsoft-365/windows/end-of-ie-support).

Var god och använd en modern webbläsare för att ta del av denna webbplats, som t.ex. nyaste versioner av Edge, Chrome, Firefox eller Safari osv.

Mikael Calner

Mikael Calner

Professor

Mikael Calner

A Late Silurian extinction event and anachronistic period

Författare

  • Mikael Calner

Summary, in English

Resurgence of microbialites and anachronistic facies in the aftermath of Phanerozoic extinction events has hitherto only been documented among the "major five." Based on the classical Silurian carbonate platform strata of Gotland, Sweden, a "minor" biotic event is herein for the first time related to a substantial increase in anachronistic facies. Strata deposited during and shortly after the Lau Event in the Baltic paleobasin (Eke and Burgsvik Formations) include evidence for reduced grazing and infaunal activity in contemporaneous shallow low-latitude seas, e.g., flat-pebble conglomerates, normal-marine stromatolites, mass occurrence of oncoids, and subtidal wrinkle structures (e.g., Kinneyia and microripples). The latter structures have recently been suggested to be restricted to Proterozoic-Cambrian and Early Triassic time and therefore are regarded as anomalous for the Phanerozoic. The co-occurrence of these facies and global extinctions among pentamerid brachiopods and conodonts suggests that minor extinction events also resulted in anachronistic periods, less devastating but fully comparable to those in the aftermath of the end-Ordovician and end-Permian mass extinctions. A global positive stable carbon isotope excursion and the last appearance datum of the conodont Polygnathoides siluricus may facilitate identification of the Late Silurian anachronistic period elsewhere.

Avdelning/ar

  • Berggrundsgeologi

Publiceringsår

2005

Språk

Engelska

Sidor

305-308

Publikation/Tidskrift/Serie

Geology

Volym

33

Issue

4

Dokumenttyp

Artikel i tidskrift

Förlag

Geological Society of America

Ämne

  • Geology

Nyckelord

  • Gotland
  • extinction
  • Silurian
  • anachronistic facies
  • wrinkle structures

Status

Published

ISBN/ISSN/Övrigt

  • ISSN: 0091-7613