H
Harald Strauss
Researcher at University of Münster
Publications - 216
Citations - 15583
Harald Strauss is an academic researcher from University of Münster. The author has contributed to research in topics: Sulfur & δ34S. The author has an hindex of 54, co-authored 215 publications receiving 13734 citations. Previous affiliations of Harald Strauss include University of Göttingen & Ruhr University Bochum.
Papers
More filters
Journal ArticleDOI
87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater
Ján Veizer,Ján Veizer,Davin Ala,Karem Azmy,Peter Bruckschen,Dieter Buhl,Frank Bruhn,Frank Bruhn,Giles A.F. Carden,Giles A.F. Carden,Andreas Diener,Stefan Ebneth,Yves Goddéris,Yves Goddéris,Torsten Jasper,Christoph Korte,Frank Pawellek,Olaf G. Podlaha,Olaf G. Podlaha,Harald Strauss +19 more
TL;DR: In this article, a total of 2128 calcitic and phosphatic shells, mainly brachiopods with some conodonts and belemnites, were measured for their δ 18 O, δ 13 C and 87 Sr / 86 S values.
Journal ArticleDOI
87 Sr/ 86 Sr,δ 13 Candδ 18 Oevolution of Phanerozoic seawater
Ján Veizer,Davin Ala,Karem Azmy,Peter Bruckschen,Dieter Buhl,Frank Bruhn,Giles A.F. Carden,Andreas Diener,Stefan Ebneth,Yves Goddéris,Torsten Jasper,Christoph Korte,Frank Pawellek,Olaf G. Podlaha,Harald Strauss +14 more
TL;DR: In this article, a total of 2128 calcitic and phosphatic shells, mainly brachiopods with some conodonts and belemnites, were measured for their δ 18 O, δ 13 C and 87 Sr / 86 S values.
Journal ArticleDOI
The abundance of 13c in marine organic matter and isotopic fractionation in the global biogeochemical cycle of carbon during the past 800 ma
TL;DR: For the later Neoproterozoic, from 800 to 543 Ma (346 analyses), from the Cambrian through the Jurassic (1616 analyses), and from the Cretaceous and Cenozoic (2493 analyses) the abundance of 13 C in marine organic matter has been compiled as discussed by the authors.
Journal ArticleDOI
Ferruginous Conditions Dominated Later Neoproterozoic Deep-Water Chemistry
Donald E. Canfield,Simon W. Poulton,Andrew H. Knoll,Guy M. Narbonne,Gerry Ross,Tatiana Goldberg,Harald Strauss +6 more
TL;DR: It is reported that through much of the later Neoproterozoic, anoxia remained widespread beneath the mixed layer of the oceans; deeper water masses were sometimes sulfidic but were mainly Fe2+-enriched, marking a return to ocean chemistry not seen for more than one billion years of Earth history.
Journal ArticleDOI
The sulfur isotopic evolution of Phanerozoic seawater based on the analysis of structurally substituted sulfate in carbonates
A. Kampschulte,Harald Strauss +1 more
TL;DR: One hundred fifty-six biogenic calcites and 96 whole rock carbonate samples of Paleozoic and Mesozoic age have been analysed for their sulfur isotopic composition as mentioned in this paper, which substantially enhances our knowledge about secular variations of the global sulfur cycle during the Phanerozoic.