DISCOVERY OF <em><em>PARATIROLITES</em></em> FROM THE BELLEROPHON FORMATION (UPPER PERMIAN, DOLOMITES, ITALY)

The first discovery of Paratirolites in the western Tethys is here described. The ammonoid was collected in the debris of the Bellerophon Fm. near Santa Cristina Valgardena (Bolzano, Dolomites). The specimen is contained in a small slab made of marly dark grey limestone with a biomicrofacies dominat...

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Main Authors: RENATO POSENATO, HERWIG PRINOTH
Format: Article
Language:English
Published: Milano University Press 1999-03-01
Series:Rivista Italiana di Paleontologia e Stratigrafia
Online Access:https://riviste.unimi.it/index.php/RIPS/article/view/5371
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author RENATO POSENATO
HERWIG PRINOTH
author_facet RENATO POSENATO
HERWIG PRINOTH
author_sort RENATO POSENATO
collection DOAJ
description The first discovery of Paratirolites in the western Tethys is here described. The ammonoid was collected in the debris of the Bellerophon Fm. near Santa Cristina Valgardena (Bolzano, Dolomites). The specimen is contained in a small slab made of marly dark grey limestone with a biomicrofacies dominated by ostracods. It probably comes from the Ostracod Assemblage beds (Badiota Facies), which are situated few metres below the Comelicania beds. The occurrence of Paratirolites allow us to date this segment of the upper Bellerophon Fm. to the late Dorashamian, and to define the Comelicania and Nankinella beds of the Dolomites as younger than the Phisonites - Comelicania (= Gruntallina) beds of the Transcaucasia (basal Dorashamian). This assemblage is equivalent to or younger than the Paratirolites Zone (late Dorashamian).
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spelling doaj.art-d907173e69da46aa9feba94b9b3d053c2023-09-02T15:36:30ZengMilano University PressRivista Italiana di Paleontologia e Stratigrafia0035-68832039-49421999-03-01105110.13130/2039-4942/53714689DISCOVERY OF <em><em>PARATIROLITES</em></em> FROM THE BELLEROPHON FORMATION (UPPER PERMIAN, DOLOMITES, ITALY)RENATO POSENATOHERWIG PRINOTHThe first discovery of Paratirolites in the western Tethys is here described. The ammonoid was collected in the debris of the Bellerophon Fm. near Santa Cristina Valgardena (Bolzano, Dolomites). The specimen is contained in a small slab made of marly dark grey limestone with a biomicrofacies dominated by ostracods. It probably comes from the Ostracod Assemblage beds (Badiota Facies), which are situated few metres below the Comelicania beds. The occurrence of Paratirolites allow us to date this segment of the upper Bellerophon Fm. to the late Dorashamian, and to define the Comelicania and Nankinella beds of the Dolomites as younger than the Phisonites - Comelicania (= Gruntallina) beds of the Transcaucasia (basal Dorashamian). This assemblage is equivalent to or younger than the Paratirolites Zone (late Dorashamian).https://riviste.unimi.it/index.php/RIPS/article/view/5371
spellingShingle RENATO POSENATO
HERWIG PRINOTH
DISCOVERY OF <em><em>PARATIROLITES</em></em> FROM THE BELLEROPHON FORMATION (UPPER PERMIAN, DOLOMITES, ITALY)
Rivista Italiana di Paleontologia e Stratigrafia
title DISCOVERY OF <em><em>PARATIROLITES</em></em> FROM THE BELLEROPHON FORMATION (UPPER PERMIAN, DOLOMITES, ITALY)
title_full DISCOVERY OF <em><em>PARATIROLITES</em></em> FROM THE BELLEROPHON FORMATION (UPPER PERMIAN, DOLOMITES, ITALY)
title_fullStr DISCOVERY OF <em><em>PARATIROLITES</em></em> FROM THE BELLEROPHON FORMATION (UPPER PERMIAN, DOLOMITES, ITALY)
title_full_unstemmed DISCOVERY OF <em><em>PARATIROLITES</em></em> FROM THE BELLEROPHON FORMATION (UPPER PERMIAN, DOLOMITES, ITALY)
title_short DISCOVERY OF <em><em>PARATIROLITES</em></em> FROM THE BELLEROPHON FORMATION (UPPER PERMIAN, DOLOMITES, ITALY)
title_sort discovery of em em paratirolites em em from the bellerophon formation upper permian dolomites italy
url https://riviste.unimi.it/index.php/RIPS/article/view/5371
work_keys_str_mv AT renatoposenato discoveryofememparatirolitesememfromthebellerophonformationupperpermiandolomitesitaly
AT herwigprinoth discoveryofememparatirolitesememfromthebellerophonformationupperpermiandolomitesitaly