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作 者:Jozef Michalik Daniela Rehkov
机构地区:[1]Slovakian Academy of Sciences,Geological Institute,Dubravska cesta 9,P.O.Box 106,840 05 Bratislava,Slovak Republic [2]Comenius University,Faculty of Natural Sciences,Department of Geology and Palaeontology,Mlynska dolina G-1,842 15 Bratislava,Slovak Republic
出 处:《Geoscience Frontiers》2011年第4期475-490,共16页地学前缘(英文版)
基 金:the APVV-0280-07,APVV-0248-07;APVV- 0465-06;APVT 51-011305;VEGA 0196 and 0065
摘 要:During the last decades,several integrated studies of Tethyan Jurassic/Cretaceous boundary sections from different countries were published with the objective to indicate problems for the selection of biological,chemical or physical markers suitable for identification of the Jurassic/Cretaceous boundary-the only system boundary within the Phanerozoic still not fixed by GSSP.Drawing the boundary between the Jurassic and Cretaceous systems is a matter of global scale discussions.The problem of proposing possible J/K boundary stratotypes results from lack of a global index fossils, global sea level drop,paleogeographic changes causing development of isolated facies areas,as well as from the effect of Late Cimmerian Orogeny.This contribution summarizes and comments data on J/K boundary interval obtained from several important Tethyan sections and shows still existing problems and discrepancies in its determination.During the last decades,several integrated studies of Tethyan Jurassic/Cretaceous boundary sections from different countries were published with the objective to indicate problems for the selection of biological,chemical or physical markers suitable for identification of the Jurassic/Cretaceous boundary-the only system boundary within the Phanerozoic still not fixed by GSSP.Drawing the boundary between the Jurassic and Cretaceous systems is a matter of global scale discussions.The problem of proposing possible J/K boundary stratotypes results from lack of a global index fossils, global sea level drop,paleogeographic changes causing development of isolated facies areas,as well as from the effect of Late Cimmerian Orogeny.This contribution summarizes and comments data on J/K boundary interval obtained from several important Tethyan sections and shows still existing problems and discrepancies in its determination.
关 键 词:J/K boundary Interregional correlation Biostratigraphic proxies Calpionellids NANNOFOSSILS
分 类 号:Q911[天文地球—古生物学与地层学]
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