NDLI: Biochronostratigraphy of the Reingraben Turnover (Hallstatt Facies Belt): Local black shale events controlled by regional tectonics, climatic change and plate tectonics

Content Provider	Springer Nature Link
Author	Hornung, Thomas Brandner, Rainer
Copyright Year	2005
Abstract	For the first time, two outcrops near Bad Dürrnberg (2 km SSW Hallein, Austria) allowed for a continuous multistratigraphical investigation of the Reingraben Turnover in the Hallstatt facies belt. After a phase of reefal sedimentation during the Julian 1 (Early Carnian), a sudden increase in terrigenous input (Reingraben Turnover) caused the breakdown of the carbonate factory at the beginning of the Julian 2 (late Early Carnian). In starved basins produced by syndepositional tectonism, black shales locally accumulated. Stable isotopes of oxygen and carbon do not suggest a change in seawater chemistry during the turnover. Shallow-water carbonate production resumed slowly during the Tuvalian (Late Carnian), and complete recovery was finished near the Carnian-Norian transition. Because similar events are recorded globally, climatic changes (monsoonal circulation) controlled by plate tectonics are favoured as triggers of the event.Based on lithology and microfacies, detailed sampling, and analysis of conodont faunas and the resulting detailed conodont zonation enabled us to establish the duration of the Reingraben Turnover (Julian 1/IIc to Julian 2/II).
Starting Page	460
Ending Page	479
Page Count	20
File Format	PDF
ISSN	01729179
Journal	Facies
Volume Number	51
Issue Number	1-4
e-ISSN	16124820
Language	English
Publisher	Springer-Verlag
Publisher Date	2005-06-10
Publisher Place	Berlin, Heidelberg
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	Carnian Tethys Northern Calcareous Alps Multistratigraphy Conodonts Microfacies Stable isotopes
Content Type	Text
Resource Type	Article
Subject	Geology Stratigraphy Paleontology

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