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Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12128/14760
Title: Middlesex/punctata Event in the Rhenish Basin (Padberg section, Sauerland, Germany) – Geochemical clues to the early-middle Frasnian perturbation of global carbon cycle
Authors: Pisarzowska, Agnieszka
Becker, R. Thomas
Aboussalam, Z. Sarah
Szczerba, Marek
Sobień, Katarzyna
Kremer, Barbara
Owocki, Krzysztof
Racki, Grzegorz
Keywords: Early–middle Frasnian; Rhenish Massif; Padberg Formation; Carbon isotope stratigraphy; Middlesex/punctata Event; Trace metal geochemistry
Issue Date: 2020
Citation: Global and Planetary Change, Vol. 191 (2020), Art. No. 103211
Abstract: A positive carbon stable isotope excursion of about 3‰is documented in the topmost lower Frasnian at Padberg, eastern Rhenish Massif, as a muted record of the worldwide early−middle Frasnian isotopic perturbation (punctata Event; up to 6–8‰ shift in both δ13Ccarb and δ13Corg elsewhere), comparable with the Appalachian δ13C curve. This German isotopic signature occurs in a 12 m thick calciturbidite succession and correlates well with the three-step chemostratigraphic pattern known from the Holy Cross Mountains, Poland. It is especially clear in the δ13Corg shifts, whilst δ13Ccarb (and elemental geochemical) proxies are partly biased by post-sedimentary alterations. The New York State, Polish, Nevada and Padberg conodont successions place the onset of the major positive δ13C excursion slightly beneath the early–middle Frasnian boundary, with Ancyrodella nodosa (previously Ad. gigas form 1) as the main conodont guide species, and coincident with the Middlesex transgression and spread of cold, nutrient-rich, poorly oxygenated water masses. In the light of geochemical proxies, enhanced primary production and oxygen deficiency occurred evidently in the Rhenish Basin during the punctata Event. Moderate Hg enrichments in the early Middlesex/punctata Event interval suggest a volcanic signature. However, conclusive data from other regions are required to differentiate between effects of the regionally wellknown synsedimenary magmatism and of a possible global volcanic trigger for the biogeochemical perturbation.
URI: http://hdl.handle.net/20.500.12128/14760
DOI: 10.1016/j.gloplacha.2020.103211
ISSN: 0921-8181
1872-6364
Appears in Collections:Artykuły (WNP)

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