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B. van de Schootbrugge

Researcher at Utrecht University

Publications -  19
Citations -  1775

B. van de Schootbrugge is an academic researcher from Utrecht University. The author has contributed to research in topics: Extinction event & Carbon cycle. The author has an hindex of 14, co-authored 19 publications receiving 1539 citations. Previous affiliations of B. van de Schootbrugge include Rutgers University & Goethe University Frankfurt.

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Paleoceanographic changes of the Late Pliensbachian-Early Toarcian interval: a possible link to the genesis of an Oceanic Anoxic Event

TL;DR: In this paper, the elemental and isotopic composition of belemnite calcite were studied in Pliensbachian and Toarcian sections from the Yorkshire coast, UK, and Southern Germany, to investigate oceanographic change during an interval prior to and including the Toarcians Oceanic Anoxic Event (OAE).
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Basinal restriction, black shales, Re‐Os dating, and the Early Toarcian (Jurassic) oceanic anoxic event

TL;DR: In this paper, a crossplot of Mo/total organic carbon (TOC) profiles through the Lower Toarcian black shales of the Cleveland Basin, Yorkshire, United Kingdom, and the Posidonia shale of Germany and Switzerland reveal water mass restriction during the interval from late tenuicostatum Zone times to early bifrons Zone times, times which include that of the putative Early Toarcians oceanic anoxic event.
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Floral changes across the Triassic/Jurassic boundary linked to flood basalt volcanism

TL;DR: In this paper, the authors present pollen, spore and geochemical analyses across the Triassic/Jurassic boundary from three drill cores from Germany and Sweden and conclude that the terrestrial vegetation shift is so severe and wide ranging that it is unlikely to have been triggered by greenhouse warming alone.
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Toarcian oceanic anoxic event: An assessment of global causes using belemnite C isotope records

TL;DR: In this article, the authors present C isotope records from belemnites (delta(13)C(bel)) sampled from two localities, calibrated with high-resolution ammonite biostratigraphy and Sr isotope stratigraphy, in Yorkshire (England) and Dotternhausen (Germany), that can be used to assess which model best explains the observed changes in carbon isotopes.