作者: Zsófia Kovács , Isaline Demangel , Sylvain Richoz , Dorothee Hippler , Andre Baldermann
DOI: 10.1016/J.GLOPLACHA.2020.103255
关键词: Sedimentary basin 、 Climate change 、 Carbonate 、 Tectonics 、 Supercontinent 、 Biostratigraphy 、 Evaporite 、 Paleontology 、 Radiogenic nuclide 、 Geology
摘要: Abstract The Late Triassic time interval witnessed several important biological turnovers, extinctions and onset of new life forms. Therefore, it is crucial to better constrain the tectonic, climatic oceanographic framework at this time. radiogenic strontium isotopic composition (87Sr/86Sr) seawater, recorded in marine carbonates sensitive variations continental weathering oceanic spreading rates. This makes a powerful proxy for palaeo-environmental reconstructions an excellent global stratigraphic correlation tool sediment records. In study, we present extended 87Sr/86Sr dataset across late Norian - Hettangian interval, established from carbonate successions Austria Turkey. well-established biostratigraphy high sampling resolution allow evaluating changes record with constraint than previous studies. An exceptionally sharp trend towards unradiogenic values has been observed latest early Rhaetian 0.70800 0.70779. Considering climate change, updated tectonic models actual dating magmatic events, possible explanations are: (i) enhanced dissolution pre-Norian carbonates, (ii) widespread evaporites (iii) reorganization sedimentary basins due break-up supercontinent Pangea. At very end Choristoceras marshi Zone, Rhaetian, reversed. likely related environmental emplacement Central Atlantic Magmatic Province.