Zobrazeno 1 - 2
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pro vyhledávání: '"Di Stefano P.[1]"'
Publikováno v:
Frontiers in Earth Sciences 10 (2022). doi:10.3389/feart.2022.875466
info:cnr-pdr/source/autori:Todaro S.[1], Rigo M.[2,3], Di Stefano P.[1], Aiuppa A.[1], Chiaradia M.[4]/titolo:End-Triassic Extinction in a Carbonate Platform From Western Tethys: A Comparison Between Extinction Trends and Geochemical Variations/doi:10.3389%2Ffeart.2022.875466/rivista:Frontiers in Earth Sciences/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:10
Frontiers in earth science, Vol. 10 (2022) P. 875466
info:cnr-pdr/source/autori:Todaro S.[1], Rigo M.[2,3], Di Stefano P.[1], Aiuppa A.[1], Chiaradia M.[4]/titolo:End-Triassic Extinction in a Carbonate Platform From Western Tethys: A Comparison Between Extinction Trends and Geochemical Variations/doi:10.3389%2Ffeart.2022.875466/rivista:Frontiers in Earth Sciences/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:10
Frontiers in earth science, Vol. 10 (2022) P. 875466
The Triassic/Jurassic boundary section cropping out at Mt Sparagio in north-western Sicily (Italy) consists of a thick and continuous peritidal succession typical of a Tethyan carbonate platform. The combined chemostratigraphic and biostratigraphic s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3b6d16f7a2e9954e50b47649e36caca5
Publikováno v:
Sedimentary Geology 368 (2018): 105–113. doi:10.1016/j.sedgeo.2018.03.008
info:cnr-pdr/source/autori:Todaro S.[1], Rigo M.[2,3], Randazzo V.[1], Di Stefano P.[1,4]/titolo:The end-Triassic mass extinction: A new correlation between extinction events and delta13C fluctuations from a Triassic-Jurassic peritidal succession in western Sicily/doi:10.1016%2Fj.sedgeo.2018.03.008/rivista:Sedimentary Geology/anno:2018/pagina_da:105/pagina_a:113/intervallo_pagine:105–113/volume:368
info:cnr-pdr/source/autori:Todaro S.[1], Rigo M.[2,3], Randazzo V.[1], Di Stefano P.[1,4]/titolo:The end-Triassic mass extinction: A new correlation between extinction events and delta13C fluctuations from a Triassic-Jurassic peritidal succession in western Sicily/doi:10.1016%2Fj.sedgeo.2018.03.008/rivista:Sedimentary Geology/anno:2018/pagina_da:105/pagina_a:113/intervallo_pagine:105–113/volume:368
A new δ13Ccarb curve was obtained from an expanded peritidal succession in western Sicily and was used to investigate the relationships between isotopic signatures and biological events on carbonate platforms across the Triassic-Jurassic boundary (T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b3d0374f395991e1f565ef029bef986c
http://hdl.handle.net/10447/282458
http://hdl.handle.net/10447/282458
