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Jurassic transgressions and regressions in the Caucasus (northern Neotethys Ocean) and their influences on the marine biodiversity Palaeogeography, Palaeoclimatology, Palaeoecology 251 422
Biostratigraphy and paleoenvironment of the marly transgression of Weißenbachalm Lower Gosau-Subgroup (Upper Turonian-Lower Santonian Grabenbach-Formation, Northern Calcareous Alps, Styria) Abhandlungen der Geologischen Bundesanstalt
the middle/late Anisian boundary (Middle Triassic) and the transgression of the Prezzo Limestone in eastern Lombardy-Giudicarie (Italy). — Swiss Journal of Geosciences, 101 , pp. 61 – 84 . Mundil
Permian), regional subsidence resulted in thick continental sediments. From the Middle–Late Permian, the sediment accumulation was influenced by a regional transgression. The sea-level rise changed the type of sedimentation (Late Permian): above the
western part of the Tethys Ocean ( Fig. 2 ). The Mesozoic sedimentary cycle as preserved in the TDR began with a latest Paleozoic transgression. By the end of the Triassic an extensive, coherent, few km-thick Dachstein-type platform developed ( Haas, 1988
-off criteria, and red where they do not In the case of the Bobrikovsky Formation, the basis of the split was sedimentological change, which could be identified on the well logs throughout the region. Transgressive lagoon-estuary and barrier island facies in the
Tournaisian reefal and other carbonate facies. A cyclic transgressive-regressive marine deposition took place following the Tournaisian, producing a thick interfingering nearshore deltaic/interdeltaic marine and continental-coastal clastic sequence. The
et al., 1999a ) which is Badenian in age ( Kelemen et al., 2021 ); kaolinite deposition was partly coeval with marine sediments of the grabens around the KH ( Fodor et al., 2021 ). The transgression of Lake Pannon reached the area of the KH
,261 ± 52 cal BP (4,364–4,260 BC), i.e., at the beginning of the Copper Age ( Raczky 1988 , 1995 ; Vaday 2004 ; Szilágyi 2008 ). The transition of the late Neolithic and Copper Ages was a time-transgressive process ( Gyucha et al. 2004 , 2006
Olenekian ( Szulc 1999 , 2000 ), and the westernmost communication to the Tethys was effective during the Anisian ( Feist-Burkhardt et al. 2008a ; Götz and Gast 2010 ). Major transgressive phases are recognized by phytoplankton peaks ( Götz and Feist
