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“…In the Puerto Escaño section (Southern Spain), the boundary between the ammonite Durangites and Jacobi Zones has been assigned to the base of the M19n Chron, while the base of the NKT Zone has been traced at the top of the M19n Chron (Svobodová & Košťák 2016). In the Western Carpathians, the FAD of N. steinmannii minor has been fixed in the middle part of the M19n Chron (Michalík et al 2016;Elbra et al 2018) which is slightly above the Tithonian-Berriasian boundary level determined from calpionellids. In Hungary, in the Lόkút section, the base of the NKT Zone has been determined at the top M19n2n Subchron (Grabowski et al 2017).…”
Section: Discussionmentioning
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“…In the Puerto Escaño section (Southern Spain), the boundary between the ammonite Durangites and Jacobi Zones has been assigned to the base of the M19n Chron, while the base of the NKT Zone has been traced at the top of the M19n Chron (Svobodová & Košťák 2016). In the Western Carpathians, the FAD of N. steinmannii minor has been fixed in the middle part of the M19n Chron (Michalík et al 2016;Elbra et al 2018) which is slightly above the Tithonian-Berriasian boundary level determined from calpionellids. In Hungary, in the Lόkút section, the base of the NKT Zone has been determined at the top M19n2n Subchron (Grabowski et al 2017).…”
Section: Discussionmentioning
“…However, the J/K boundary could not then be strictly determined. Recent bed-by-bed study confirmed a similar calpionellid distribution, with a biozonation, and the J/K boundary to be precisely located (Svobodová et al 2017;Švábenická et al 2017;Elbra et al 2018a).…”
Section: Introductionmentioning
“…Determining the Global Boundary Stratotype Section and Point (GSSP) for the Berriasian Stage in the Tethys has been the objective of elaborate research and discussions of the Berriasian Working Group during the past several years. Tethys was the largest depositional area during Tithonian and Berriasian times that is available for study by diverse stratigraphic methods, namely lithostratigraphy, biostratigraphy (based on calpionellids, nannofossils, dinoflagellates, radiolarians, foraminifers, ammonites and belemnites), as well as by magnetostratigraphy, geochemistry and sequence stratigraphy (Andreini et al 2007;Houša et al 2007;Michalík et al 2009Michalík et al , 2016Lukeneder et al 2010;Pruner et al 2010;Grabowski et al 2010a, b;Grabowski 2011;Michalík & Reháková 2011;Wimbledon et al 2011Wimbledon et al , 2013Petrova et al 2012;Guzhikov et al 2012;Lakova & Petrova 2013;López-Martínez et al 2013Schnabl et al 2015;Svobodová & Košťák 2016;Hoedemaeker et al 2016;Grabowski et al 2017;Kietzmann 2017;Lakova et al 2017;Wimbledon 2017;Elbra et al 2018a, b, Kowal-Kasprzyk & Reháková 2019.…”
Section: Introductionmentioning
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