<em>POLYGNATHUS ROSAE </em> N. SP. (CONODONTA) AND ITS BIOSTRATIGRAPHICAL CORRELATION POTENTIAL (LOWER EMSIAN, LOWER DEVONIAN)IN THE SPANISH CENTRAL PYRENEES

The problems around the Pragian/Emsian (P/E) boundary have been widely discussed by several authors, who have pointed out that the present Global Stratotype Section and Point (GSSP) in the Zinzilban section (Kitab Reserve, Uzbekistan), is much older than the traditional German Siegenian-Emsian bound...

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Main Authors: CARLOS MARTÍNEZ-PÉREZ, JOSÉ I. VALENZUELA-RÍOS, HÉCTOR BOTELLA
Format: Article
Language:English
Published: Milano University Press 2010-11-01
Series:Rivista Italiana di Paleontologia e Stratigrafia
Subjects:
Online Access:https://riviste.unimi.it/index.php/RIPS/article/view/6390
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author CARLOS MARTÍNEZ-PÉREZ
JOSÉ I. VALENZUELA-RÍOS
HÉCTOR BOTELLA
author_facet CARLOS MARTÍNEZ-PÉREZ
JOSÉ I. VALENZUELA-RÍOS
HÉCTOR BOTELLA
author_sort CARLOS MARTÍNEZ-PÉREZ
collection DOAJ
description The problems around the Pragian/Emsian (P/E) boundary have been widely discussed by several authors, who have pointed out that the present Global Stratotype Section and Point (GSSP) in the Zinzilban section (Kitab Reserve, Uzbekistan), is much older than the traditional German Siegenian-Emsian boundary, a fact that considerably reduces the duration of the traditional Pragian Stage. A comprehensive conodont study of two important sections (Isábena 1 and Baliera 6) demonstrates the presence of the conodont indexes for the P/E boundary in both senses (official and traditional) in the Spanish Central Pyrenees (SCP). Within the important conodont faunas registered, the presence of a new early polygnathid species Polygnathus rosae n. sp. stands out. Its stratigraphic range in the two sections is restricted to a short interval around the traditional beginning of the Emsian Stage. This particular distribution permits direct relation between both indexes, a better characterization of the P/E boundary in the traditional German sense and increases the palaeontological knowledge of this stratigraphic interval. Conodont records in the SCP suggest that Po. rosae n. sp. could be a good local index, too. In addition, Po. rosae n. sp. represents the last known step of the lineage Po. pireneaePo. rosae n. sp., a new early polygnathid lineage that supports the early radiation of the genus around the P/E boundary.
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spelling doaj.art-38830ad2226e4abb974e880b34eaf22f2023-09-03T04:56:24ZengMilano University PressRivista Italiana di Paleontologia e Stratigrafia0035-68832039-49422010-11-01116310.13130/2039-4942/63905701<em>POLYGNATHUS ROSAE </em> N. SP. (CONODONTA) AND ITS BIOSTRATIGRAPHICAL CORRELATION POTENTIAL (LOWER EMSIAN, LOWER DEVONIAN)IN THE SPANISH CENTRAL PYRENEESCARLOS MARTÍNEZ-PÉREZJOSÉ I. VALENZUELA-RÍOSHÉCTOR BOTELLAThe problems around the Pragian/Emsian (P/E) boundary have been widely discussed by several authors, who have pointed out that the present Global Stratotype Section and Point (GSSP) in the Zinzilban section (Kitab Reserve, Uzbekistan), is much older than the traditional German Siegenian-Emsian boundary, a fact that considerably reduces the duration of the traditional Pragian Stage. A comprehensive conodont study of two important sections (Isábena 1 and Baliera 6) demonstrates the presence of the conodont indexes for the P/E boundary in both senses (official and traditional) in the Spanish Central Pyrenees (SCP). Within the important conodont faunas registered, the presence of a new early polygnathid species Polygnathus rosae n. sp. stands out. Its stratigraphic range in the two sections is restricted to a short interval around the traditional beginning of the Emsian Stage. This particular distribution permits direct relation between both indexes, a better characterization of the P/E boundary in the traditional German sense and increases the palaeontological knowledge of this stratigraphic interval. Conodont records in the SCP suggest that Po. rosae n. sp. could be a good local index, too. In addition, Po. rosae n. sp. represents the last known step of the lineage Po. pireneaePo. rosae n. sp., a new early polygnathid lineage that supports the early radiation of the genus around the P/E boundary.https://riviste.unimi.it/index.php/RIPS/article/view/6390PolygnathidsPragian/Emsian BoundaryLower DevonianSpanish Central Pyrenees
spellingShingle CARLOS MARTÍNEZ-PÉREZ
JOSÉ I. VALENZUELA-RÍOS
HÉCTOR BOTELLA
<em>POLYGNATHUS ROSAE </em> N. SP. (CONODONTA) AND ITS BIOSTRATIGRAPHICAL CORRELATION POTENTIAL (LOWER EMSIAN, LOWER DEVONIAN)IN THE SPANISH CENTRAL PYRENEES
Rivista Italiana di Paleontologia e Stratigrafia
Polygnathids
Pragian/Emsian Boundary
Lower Devonian
Spanish Central Pyrenees
title <em>POLYGNATHUS ROSAE </em> N. SP. (CONODONTA) AND ITS BIOSTRATIGRAPHICAL CORRELATION POTENTIAL (LOWER EMSIAN, LOWER DEVONIAN)IN THE SPANISH CENTRAL PYRENEES
title_full <em>POLYGNATHUS ROSAE </em> N. SP. (CONODONTA) AND ITS BIOSTRATIGRAPHICAL CORRELATION POTENTIAL (LOWER EMSIAN, LOWER DEVONIAN)IN THE SPANISH CENTRAL PYRENEES
title_fullStr <em>POLYGNATHUS ROSAE </em> N. SP. (CONODONTA) AND ITS BIOSTRATIGRAPHICAL CORRELATION POTENTIAL (LOWER EMSIAN, LOWER DEVONIAN)IN THE SPANISH CENTRAL PYRENEES
title_full_unstemmed <em>POLYGNATHUS ROSAE </em> N. SP. (CONODONTA) AND ITS BIOSTRATIGRAPHICAL CORRELATION POTENTIAL (LOWER EMSIAN, LOWER DEVONIAN)IN THE SPANISH CENTRAL PYRENEES
title_short <em>POLYGNATHUS ROSAE </em> N. SP. (CONODONTA) AND ITS BIOSTRATIGRAPHICAL CORRELATION POTENTIAL (LOWER EMSIAN, LOWER DEVONIAN)IN THE SPANISH CENTRAL PYRENEES
title_sort em polygnathus rosae em n sp conodonta and its biostratigraphical correlation potential lower emsian lower devonian in the spanish central pyrenees
topic Polygnathids
Pragian/Emsian Boundary
Lower Devonian
Spanish Central Pyrenees
url https://riviste.unimi.it/index.php/RIPS/article/view/6390
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