Pregled bibliografske jedinice broj: 1266535
The Carnian (Late Triassic) carbon isotope excursion: new insights from the terrestrial realm
The Carnian (Late Triassic) carbon isotope excursion: new insights from the terrestrial realm // Abstracts
Beč, Austrija, 2016. 6899, 1 (predavanje, međunarodna recenzija, sažetak, znanstveni)
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Naslov
The Carnian (Late Triassic) carbon isotope
excursion: new insights from the terrestrial realm
Autori
Miller, Charlotte ; Kürschner, Wolfram ; Peterse, Francien ; Baranyi, Viktoria ; Reichart, Gert-Jan
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Abstracts
/ - , 2016
Skup
EGU General Assembly Conference
Mjesto i datum
Beč, Austrija, 17.04.2016. - 22.04.2016
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Carnian Pluvial Episode, C cycle, biomarkers
Sažetak
The geological record contains evidence for numerous pronounced perturbations in the global carbon cycle, some of which are associated with eruptions from large igneous provinces (LIP), and consequently, ocean acidification and mass extinction. In the Carnian (Late Triassic), evidence from sedimentology and fossil pollen points to a significant change in climate, resulting in biotic turnover: during a period termed the 'Carnian Pluvial Event' (CPE). Additionally, during the Carnian, large volumes of flood basalts were erupted from the Wrangellia LIP (western North America). Evidence from the marine realm suggests a fundamental relationship between the CPE, a global 'wet' period, and the injection of light carbon into the atmosphere from the LIP. Here we provide the first evidence from the terrestrial realm of a significant negative δ13C excursion through the CPE recorded in the sedimentary archive of the Wiscombe Park Borehole, Devon (UK). Both total organic matter and plant leaf waxes reflect a gradual carbon isotope excursion of ~-5‰ during this time interval. Our data provides evidence for the global nature of this isotope excursion, supporting the hypothesis that the excursion was likely the result of an injection of light carbon into the atmosphere from the Wrangellia LIP.
Izvorni jezik
Engleski
Znanstvena područja
Geologija