ASGP (2014), vol. 84: 1–33
INTEGRATED STRATIGRAPHY OF THE MIDDLE–UPPER JURASSIC OF THE KRÍŽNA NAPPE, TATRA MOUNTAINS
Renata JACH(1), Nevenka DJERIĆ(2), Špela GORIČAN(3) & Daniela REHÁKOVÁ(4)
1) Institute of Geological Sciences, Jagiellonian University, Oleandry 2a, 30-063 Kraków, Poland, e-mail: renata.jach at uj.edu.pl
2) Faculty of Mining and Geology, Belgrade University, Djusina 7, Belgrade, Serbia, e-mail: djeranen at rgf.bg.ac.rs
3) Ivan Rakovec Institute of Palaeontology, ZRC SAZU, Novi trg 2, SI-1000 Ljubljana, Slovenia, e-mail: spela at zrc-sazu.si
4) Department of Geology and Palaeontology, Faculty of Natural Sciences, Comenius University, Mlynská dolina G-1, 842 15 Bratislava, Slovakia, e-mail: rehakova at fns.uniba.sk
Jach, R., Djerić, N., Goričan, Š. & Reháková, D., 2014. Integrated stratigraphy of the Middle–Upper Jurassic of the Krížna Nappe, Tatra Mountains. Annales Societatis Geologorum Poloniae, 84: 1–33.
Abstract: Middle–Upper Jurassic pelagic carbonates and radiolarites were studied in the Krížna Nappe of the Tatra Mountains (Central Western Carpathians, southern Poland and northern Slovakia). A carbon isotope stra- tigraphy of these deposits was combined with biostratigraphy, based on radiolarians, calcareous dinoflagellates and calpionellids. In the High Tatra and Belianske Tatra Mountains, the Bajocian and part of the Bathonian are represented by a thick succession of spotted limestones and grey nodular limestones, while in the Western Tatra Mountains by relatively thin Bositra-crinoidal limestones. These deposits are referable to a deeper basin and a pelagic carbonate platform, respectively. The various carbonate facies are followed by deep-water biosiliceous facies, namely radiolarites and radiolarian-bearing limestones of Late Bathonian–early Late Kimmeridgian age. These facies pass into Upper Kimmeridgian–Lower Tithonian pelagic carbonates with abundant Saccocoma sp. The bulk-carbonate isotope composition of the carbonate-siliceous deposits shows positive and negative δ13C excursions and shifts in the Early Bajocian, Late Bajocian, Early Bathonian, Late Bathonian, Late Callovian, Middle Oxfordian and Late Kimmeridgian. Additionally, the δ13C curves studied show a pronounced increasing trend in the Callovian and a steadily decreasing trend in the Oxfordian–Early Tithonian. These correlate with the trends known from the Tethyan region. The onset of Late Bathonian radiolarite sedimentation is marked by a decreasing trend in δ13C. Increased δ13C values in the Late Callovian, Middle Oxfordian and Late Kimmeridgian (Moluccana Zone) correspond with enhanced radiolarian production. A significant increase in CaCO3 content is recorded just above the Late Callovian δ13C excursion, which coincides with a transition from green to variegated radiolarites.
Manuscript received 11 November 2013, accepted 14 April 2014
