Integrated stratigraphy across the Jurassic-Cretaceous boundary in the Rettenbacher section (Northern Calcareous Alps, Salzburg, Austria)

被引:1
|
作者
Elbra, T. [1 ]
Skupien, P. [2 ]
Bubik, M. [3 ]
Kostak, M. [4 ]
Matejova, M. Molcan [5 ]
Pruner, P. [1 ]
Rehakova, D. [5 ]
Svabenicka, L. [6 ]
Vankova, L. [1 ,4 ]
Cigler, V. [3 ]
Geist, J. [4 ]
Kdyr, S. [1 ,7 ]
Lukeneder, A. [8 ]
Rybova, P. [2 ]
Mazuch, M. [4 ]
Schnabl, P. [1 ]
Svobodova, A. [1 ]
Trubac, J. [7 ]
Ucar, H. [1 ,9 ]
机构
[1] Czech Acad Sci, Inst Geol, Rozvojova 269, CZ-16500 Prague, Czech Republic
[2] VSB Tech Univ Ostrava, Dept Geol Engn, 17 Listopadu 15, Poruba Ostrava 70833, Czech Republic
[3] Czech Geol Survey, Leitnerova 22, Brno 60200, Czech Republic
[4] Charles Univ Prague, Inst Geol & Palaeontol, Fac Sci, Albertov 6, Prague 2, Czech Republic
[5] Comenius Univ, Dept Geol & Palaeontol, Ilkovicova 6, SK-84215 Bratislava, Slovakia
[6] Czech Geol Survey, Klarov 131-3, Prague CZ-11821, Czech Republic
[7] Charles Univ Prague, Fac Sci, Inst Geochem Mineral & Mineral Resources, Albertov 6, Prague 2, Czech Republic
[8] Nat Hist Museum Vienna, Geol & Palaeontol Dept, Burgring 7, A-1010 Vienna, Austria
[9] Charles Univ Prague, Fac Sci, Inst Hydrogeol Engn Geol & Appl Geophys, Albertov 6, Prague 2, Czech Republic
关键词
Northern Calcareous Alps; Jurassic-Cretaceous boundary; Biostratigraphy; Magnetic properties; C -O stable isotopes; OXYGEN-ISOTOPE; JURASSIC/CRETACEOUS BOUNDARY; WESTERN CARPATHIANS; KUROVICE SECTION; LEUBE QUARRY; BIOSTRATIGRAPHY; EVOLUTION; CARBON; TETHYAN; RECONSTRUCTION;
D O I
10.1016/j.cretres.2024.105854
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Rettenbacher Quarry carbonate sequence in the Northern Calcareous Alps represents highly dynamic pelagic carbonate sedimentation in the lower slope environment. The section spans from upper Tithonian Crassicollaria colomi Subzone to middle Berriasian Calpionella elliptica Subzone. Radiolarian samples belong to Pseudodictyomitra carpatica Zone. Considerable redeposition of calpionellids, organic walled dinoflagellate cysts, calcareous nannofossils and foraminifera in the allodapic layers, as well as extensive normal polarity remagnetisation event with substantial clockwise rotation is documented. Quantitative predominance of genera Watznaueria and Cyclagelosphaera indicate strong nannofossil modification during diagenesis. The almost straight trend in the 313C with some slight carbon-isotope perturbations is recorded at Rettenbacher. Three significant and stratigraphically important negative excursions of the 313Ccarb values were identified - including tentative indication of a new "Negative peak 4" in the upper part of the Elliptica Subzone - and correlated with other sections confirming stability, respectively isochronity within carbon chemostratigraphy.
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页数:23
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