Mid-Norian to Hettangian record and time-specific oolites during the end-Triassic Mass Extinction at Wadi Milaha, Musandam Peninsula, United Arab Emirates

Autor: Ingrid Urban, Isaline Demangel, Leopold Krystyn, Mikael Calner, Zsófia Kovács, Gerit Gradwohl, Simon Lernpeiss, Florian Maurer, Sylvain Richoz

Publikováno v: Journal of Asian Earth Sciences: X, Vol 9, Iss , Pp 100138- (2023)

The end-Triassic Mass Extinction (ETME) is generally regarded as a consequence of the environmental changes associated with the emplacement of the Central Atlantic Magmatic Province (CAMP) and ranks among the ‘big five’ mass extinctions in Earth

Externí odkaz: https://doaj.org/article/a9109324d66b45b5978cd7b616cbc987

Extent of the Upper Norian – Rhaetian Slatnik Formation in the Tolmin Nappe, eastern Southern Alps

Autor: Boštjan Rožič, Luka Gale, Tea Kolar-Jurkovšek

Publikováno v: Geologija, Vol 56, Iss 2, Pp 175-186 (2013)

In the Norian and Rhaetian the area of present-day Slovenia was divided into the Julian Carbonate Platform on in present north, the Dinaric Carbonate Platform in the present south and the intermediate Slovenian Basin. Main Dolomite or the Dachstein

Externí odkaz: https://doaj.org/article/769b356024df4b8a94d04e6ba71ddd2a

Sedimentary record of Upper Triassic impact in the Lagonegro Basin, southern Italy: Insights from highly siderophile elements and Re-Os isotope stratigraphy across the Norian/Rhaetian boundary

Autor: Sato H.[1], Ishikawa A.[2, Onoue T.[4], Tomimatsu Y.[4], Rigo M.[1

Publikováno v: Chemical geology 586 (2021): 1–20. doi:10.1016/j.chemgeo.2021.120506
info:cnr-pdr/source/autori:Sato H.[1], Ishikawa A.[2,3], Onoue T.[4], Tomimatsu Y.[4], Rigo M.[1,5]/titolo:Sedimentary record of Upper Triassic impact in the Lagonegro Basin, southern Italy: Insights from highly siderophile elements and Re-Os isotope stratigraphy across the Norian%2FRhaetian boundary/doi:10.1016%2Fj.chemgeo.2021.120506/rivista:Chemical geology/anno:2021/pagina_da:1/pagina_a:20/intervallo_pagine:1–20/volume:586

The Norian and Rhaetian transition (Late Triassic) is characterized by a faunal turnover in major pelagic groups, such as radiolarians, conodonts, and ammonoids. Although catastrophic events such as emplacements of large igneous provinces and/or extr

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fbcba7acea68232abc83bda3a764bba7

The Norian/Rhaetian boundary interval at Pignola-Abriola section (Southern Apennines, Italy) as a GSSP candidate for the Rhaetian Stage: an update

Autor: Bertinelli, A., Casacci, M., Concheri, Giuseppe, Gattolin, Giovanni, Godfrey, L., Katz, M. E., Maron, Matteo, Mazza, M., Mietto, Paolo, Muttoni, G., Rigo, Manuel, Sprovieri, M., Stellin, Fabio, Zaffani, Mariachiara

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::0d69a30ab075b51ab00733e94d827221
http://hdl.handle.net/11391/1401950

New biostratigraphical constraints for the Norian/Rhaetian boundary: data from Lagonegro Basin, Southern Apennines, Italy

Autor: Gloria Ciarapica, Manuel Rigo, Nicola Giordano, Angela Bertinelli

Giordano, N., Rigo, M., Ciarapica G. & Bertinelli A. 2010: New biostratigraphical constraints for the Norian/Rhaetian boundary: data from Lagonegro Basin, Southern Apennines, Italy. Lethaia. 10.1111/j.1502-3931.2010.00218.x. Four stratigraphic sectio

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f9bf761bed563deb629fe04763d1232e
http://hdl.handle.net/11577/2427217