Integrated Magnetic Susceptibility and Geochemical Record of d13C Anomalies in the Berriasian and Valanginian Sections from the Tethyan Domain (Western Carpathians, Poland)

Grabowski, J.; Krzemiński, L.; Schnyder, J.; Sobien, K.; Hejnar, J.; Koptíková, Leona; Pszcólkowski, A.; Schnabl, Petr

doi:https://dx.doi.org/10.1007/978-3-319-04364-7_159

Number of the records: 1

Integrated Magnetic Susceptibility and Geochemical Record of d13C Anomalies in the Berriasian and Valanginian Sections from the Tethyan Domain (Western Carpathians, Poland)

1.

SYSNO ASEP	0429603
Document Type	C - Proceedings Paper (int. conf.)
R&D Document Type	Conference Paper
Title	Integrated Magnetic Susceptibility and Geochemical Record of d13C Anomalies in the Berriasian and Valanginian Sections from the Tethyan Domain (Western Carpathians, Poland)
Author(s)	Grabowski, J. (PL) Krzemiński, L. (PL) Schnyder, J. (FR) Sobien, K. (PL) Hejnar, J. (PL) Koptíková, Leona (GLU-S)_{RID, SAI} Pszcólkowski, A. (PL) Schnabl, Petr (GLU-S)_{RID, SAI, ORCID}
Source Title	STRATI 2013 : Proceedings of the 1st International Congress on Stratigraphy. - Cham : Springer International Publishing, 2014 / Rocha R. ; Pais J. ; Finney S. ; Kullberg J. C. - ISBN 978-3-319-04363-0
Pages	s. 847-851
Number of pages	5 s.
Publication form	Print - P
Action	STRATI 2013 : International Congress on Stratigraphy At the Cutting Edge of Stratigraphy
Event date	01.07.2013-07.07.2013
VEvent location	Lisboa
Country	PT - Portugal
Event type	WRD
Language	eng - English
Country	CH - Switzerland
Keywords	Berriasian ; Valanginian ; magnetic susceptibility ; major and trace elements
Subject RIV	DE - Earth Magnetism, Geodesy, Geography
Institutional support	GLU-S - RVO:67985831
UT WOS	000359019400159
DOI	10.1007/978-3-319-04364-7_159
Annotation	New magnetic susceptibility (MS), stable isotope, and geochemical (major and trace elements) data are presented from the three Berriasian–Valanginian pelagic sections from the Western Carpathians of Poland. MS correlates well with lithogenic influx and reflects exactly the short-term transgressive–regressive cycles in the interval below the d13C event (the Weissert event) recorded in the upper Valanginian. The pattern of changes in MS recorded for the Weissert event is more complicated, most probably also reflecting significant climatic changes. Redoxsensitive indicators (Th/U, Ce/Ce*) account for significantly oxygen-depleted conditions combined with relatively low content of productivity indicators (Alnormalized P, Ba, and Cu).
Workplace	Institute of Geology
Contact	Jana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
Year of Publishing	2015

Number of the records: 1