First remains of neoginglymodian actinopterygians from the Jurassic of Monte Nerone area (Umbria-Marche Apennine, Italy)

Autores
Romano, Marco; Cipriani, Angelo; Fabbi, Simone; Citton, Paolo
Año de publicación
2019
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Since the early nineteenth century, the structural high of Mt. Nerone in the Umbria-Marche-Sabina Domain (UMS - Central/ Northern Apennines, Italy) attracted scholars from all over Europe due to the wealth of fossil fauna preserved in a well-exposed Mesozoic sedimentary succession. Several geo-palaeontological studies were focused on the abundant and diverse invertebrate fauna, whereas contributions dealing with Mesozoic vertebrates were to date virtually lacking. Recently, the first material referable to hybodont sharks, consisting of an articulated crushing dentition, was described from the area and referred to Asteracanthus cf. A. magnus. In this contribution, we report the first evidence of ginglymodian actinopterygians from the Upper Jurassic of Mt. Nerone. The material is represented by seven highly tritorial isolated teeth collected from three classic fossiliferous localities of the area (i.e. Pian del Sasso, Fosso Pisciarello, I Ranchi). The general morphology of the material under study allow us to conservatively refer the teeth to the Neoginglymodi, a clade formed by Lepisosteiformes and Semionotiformes. The occurrence of durophagous organisms, to date represented by hybodont sharks and ginglymodian fishes, reveals interesting palaeoecological scenarios characterizing the pelagic carbonate platform-basin system of Mt. Nerone, which were most likely triggered by large-scale geodynamic processes. The complex submarine palaeotopography, inheritance of the Western Tethys Early Jurassic rifting, aroused the establishment of new infaunal and epifaunal communities opening up unexplored trophic niches for durophagous predators. The particular geodynamic setting of the UMS Domain, consisting of predominantly interconnected structural highs and lows, and the relative evolution of a diverse invertebrate fauna characterized by terebratulid, ostreids, limids, brachiopods, crustaceans, and gastropods, attracted both hybodontids and durophagous ginglymodians in the Tethyan realm, influencing their dispersal during the Late Jurassic.
Fil: Romano, Marco. University of the Witwatersrand; Sudáfrica. Università degli Studi di Roma "La Sapienza"; Italia. Apennine Team; Italia
Fil: Cipriani, Angelo. Università degli Studi di Roma "La Sapienza"; Italia. Apennine Team; Italia
Fil: Fabbi, Simone. Università degli Studi di Roma "La Sapienza"; Italia. Apennine Team; Italia. Consiglio Nazionale delle Ricerche; Italia
Fil: Citton, Paolo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; Argentina. Universidad Nacional de Río Negro. Sede Alto Valle. Instituto de Investigaciones en Paleobiología y Geología; Argentina. Università degli Studi di Roma "La Sapienza"; Italia. Apennine Team; Italia. Consiglio Nazionale delle Ricerche; Italia
Materia
GINGLYMODIAN ACTINOPTERYGIANS
LATE JURASSIC
LEPIDOTES
PALAEOECOLOGY
PELAGIC CARBONATE PLATFORM
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/125811

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network_name_str CONICET Digital (CONICET)
spelling First remains of neoginglymodian actinopterygians from the Jurassic of Monte Nerone area (Umbria-Marche Apennine, Italy)Romano, MarcoCipriani, AngeloFabbi, SimoneCitton, PaoloGINGLYMODIAN ACTINOPTERYGIANSLATE JURASSICLEPIDOTESPALAEOECOLOGYPELAGIC CARBONATE PLATFORMhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1https://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Since the early nineteenth century, the structural high of Mt. Nerone in the Umbria-Marche-Sabina Domain (UMS - Central/ Northern Apennines, Italy) attracted scholars from all over Europe due to the wealth of fossil fauna preserved in a well-exposed Mesozoic sedimentary succession. Several geo-palaeontological studies were focused on the abundant and diverse invertebrate fauna, whereas contributions dealing with Mesozoic vertebrates were to date virtually lacking. Recently, the first material referable to hybodont sharks, consisting of an articulated crushing dentition, was described from the area and referred to Asteracanthus cf. A. magnus. In this contribution, we report the first evidence of ginglymodian actinopterygians from the Upper Jurassic of Mt. Nerone. The material is represented by seven highly tritorial isolated teeth collected from three classic fossiliferous localities of the area (i.e. Pian del Sasso, Fosso Pisciarello, I Ranchi). The general morphology of the material under study allow us to conservatively refer the teeth to the Neoginglymodi, a clade formed by Lepisosteiformes and Semionotiformes. The occurrence of durophagous organisms, to date represented by hybodont sharks and ginglymodian fishes, reveals interesting palaeoecological scenarios characterizing the pelagic carbonate platform-basin system of Mt. Nerone, which were most likely triggered by large-scale geodynamic processes. The complex submarine palaeotopography, inheritance of the Western Tethys Early Jurassic rifting, aroused the establishment of new infaunal and epifaunal communities opening up unexplored trophic niches for durophagous predators. The particular geodynamic setting of the UMS Domain, consisting of predominantly interconnected structural highs and lows, and the relative evolution of a diverse invertebrate fauna characterized by terebratulid, ostreids, limids, brachiopods, crustaceans, and gastropods, attracted both hybodontids and durophagous ginglymodians in the Tethyan realm, influencing their dispersal during the Late Jurassic.Fil: Romano, Marco. University of the Witwatersrand; Sudáfrica. Università degli Studi di Roma "La Sapienza"; Italia. Apennine Team; ItaliaFil: Cipriani, Angelo. Università degli Studi di Roma "La Sapienza"; Italia. Apennine Team; ItaliaFil: Fabbi, Simone. Università degli Studi di Roma "La Sapienza"; Italia. Apennine Team; Italia. Consiglio Nazionale delle Ricerche; ItaliaFil: Citton, Paolo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; Argentina. Universidad Nacional de Río Negro. Sede Alto Valle. Instituto de Investigaciones en Paleobiología y Geología; Argentina. Università degli Studi di Roma "La Sapienza"; Italia. Apennine Team; Italia. Consiglio Nazionale delle Ricerche; ItaliaSocietà Geologica Italiana2019-02info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/125811Romano, Marco; Cipriani, Angelo; Fabbi, Simone; Citton, Paolo; First remains of neoginglymodian actinopterygians from the Jurassic of Monte Nerone area (Umbria-Marche Apennine, Italy); Società Geologica Italiana; Italian Journal of Geosciences; 138; 1; 2-2019; 88-1022038-17192038-1727CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.3301/IJG.2018.28info:eu-repo/semantics/altIdentifier/url/https://www.italianjournalofgeosciences.it/297/article-964/first-remains-of-neoginglymodian-actinopterygians-from-the-jurassic-of-monte-nerone-area-umbria-marche-apennine-italy.htmlinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T10:05:16Zoai:ri.conicet.gov.ar:11336/125811instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-03 10:05:16.463CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv First remains of neoginglymodian actinopterygians from the Jurassic of Monte Nerone area (Umbria-Marche Apennine, Italy)
title First remains of neoginglymodian actinopterygians from the Jurassic of Monte Nerone area (Umbria-Marche Apennine, Italy)
spellingShingle First remains of neoginglymodian actinopterygians from the Jurassic of Monte Nerone area (Umbria-Marche Apennine, Italy)
Romano, Marco
GINGLYMODIAN ACTINOPTERYGIANS
LATE JURASSIC
LEPIDOTES
PALAEOECOLOGY
PELAGIC CARBONATE PLATFORM
title_short First remains of neoginglymodian actinopterygians from the Jurassic of Monte Nerone area (Umbria-Marche Apennine, Italy)
title_full First remains of neoginglymodian actinopterygians from the Jurassic of Monte Nerone area (Umbria-Marche Apennine, Italy)
title_fullStr First remains of neoginglymodian actinopterygians from the Jurassic of Monte Nerone area (Umbria-Marche Apennine, Italy)
title_full_unstemmed First remains of neoginglymodian actinopterygians from the Jurassic of Monte Nerone area (Umbria-Marche Apennine, Italy)
title_sort First remains of neoginglymodian actinopterygians from the Jurassic of Monte Nerone area (Umbria-Marche Apennine, Italy)
dc.creator.none.fl_str_mv Romano, Marco
Cipriani, Angelo
Fabbi, Simone
Citton, Paolo
author Romano, Marco
author_facet Romano, Marco
Cipriani, Angelo
Fabbi, Simone
Citton, Paolo
author_role author
author2 Cipriani, Angelo
Fabbi, Simone
Citton, Paolo
author2_role author
author
author
dc.subject.none.fl_str_mv GINGLYMODIAN ACTINOPTERYGIANS
LATE JURASSIC
LEPIDOTES
PALAEOECOLOGY
PELAGIC CARBONATE PLATFORM
topic GINGLYMODIAN ACTINOPTERYGIANS
LATE JURASSIC
LEPIDOTES
PALAEOECOLOGY
PELAGIC CARBONATE PLATFORM
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Since the early nineteenth century, the structural high of Mt. Nerone in the Umbria-Marche-Sabina Domain (UMS - Central/ Northern Apennines, Italy) attracted scholars from all over Europe due to the wealth of fossil fauna preserved in a well-exposed Mesozoic sedimentary succession. Several geo-palaeontological studies were focused on the abundant and diverse invertebrate fauna, whereas contributions dealing with Mesozoic vertebrates were to date virtually lacking. Recently, the first material referable to hybodont sharks, consisting of an articulated crushing dentition, was described from the area and referred to Asteracanthus cf. A. magnus. In this contribution, we report the first evidence of ginglymodian actinopterygians from the Upper Jurassic of Mt. Nerone. The material is represented by seven highly tritorial isolated teeth collected from three classic fossiliferous localities of the area (i.e. Pian del Sasso, Fosso Pisciarello, I Ranchi). The general morphology of the material under study allow us to conservatively refer the teeth to the Neoginglymodi, a clade formed by Lepisosteiformes and Semionotiformes. The occurrence of durophagous organisms, to date represented by hybodont sharks and ginglymodian fishes, reveals interesting palaeoecological scenarios characterizing the pelagic carbonate platform-basin system of Mt. Nerone, which were most likely triggered by large-scale geodynamic processes. The complex submarine palaeotopography, inheritance of the Western Tethys Early Jurassic rifting, aroused the establishment of new infaunal and epifaunal communities opening up unexplored trophic niches for durophagous predators. The particular geodynamic setting of the UMS Domain, consisting of predominantly interconnected structural highs and lows, and the relative evolution of a diverse invertebrate fauna characterized by terebratulid, ostreids, limids, brachiopods, crustaceans, and gastropods, attracted both hybodontids and durophagous ginglymodians in the Tethyan realm, influencing their dispersal during the Late Jurassic.
Fil: Romano, Marco. University of the Witwatersrand; Sudáfrica. Università degli Studi di Roma "La Sapienza"; Italia. Apennine Team; Italia
Fil: Cipriani, Angelo. Università degli Studi di Roma "La Sapienza"; Italia. Apennine Team; Italia
Fil: Fabbi, Simone. Università degli Studi di Roma "La Sapienza"; Italia. Apennine Team; Italia. Consiglio Nazionale delle Ricerche; Italia
Fil: Citton, Paolo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; Argentina. Universidad Nacional de Río Negro. Sede Alto Valle. Instituto de Investigaciones en Paleobiología y Geología; Argentina. Università degli Studi di Roma "La Sapienza"; Italia. Apennine Team; Italia. Consiglio Nazionale delle Ricerche; Italia
description Since the early nineteenth century, the structural high of Mt. Nerone in the Umbria-Marche-Sabina Domain (UMS - Central/ Northern Apennines, Italy) attracted scholars from all over Europe due to the wealth of fossil fauna preserved in a well-exposed Mesozoic sedimentary succession. Several geo-palaeontological studies were focused on the abundant and diverse invertebrate fauna, whereas contributions dealing with Mesozoic vertebrates were to date virtually lacking. Recently, the first material referable to hybodont sharks, consisting of an articulated crushing dentition, was described from the area and referred to Asteracanthus cf. A. magnus. In this contribution, we report the first evidence of ginglymodian actinopterygians from the Upper Jurassic of Mt. Nerone. The material is represented by seven highly tritorial isolated teeth collected from three classic fossiliferous localities of the area (i.e. Pian del Sasso, Fosso Pisciarello, I Ranchi). The general morphology of the material under study allow us to conservatively refer the teeth to the Neoginglymodi, a clade formed by Lepisosteiformes and Semionotiformes. The occurrence of durophagous organisms, to date represented by hybodont sharks and ginglymodian fishes, reveals interesting palaeoecological scenarios characterizing the pelagic carbonate platform-basin system of Mt. Nerone, which were most likely triggered by large-scale geodynamic processes. The complex submarine palaeotopography, inheritance of the Western Tethys Early Jurassic rifting, aroused the establishment of new infaunal and epifaunal communities opening up unexplored trophic niches for durophagous predators. The particular geodynamic setting of the UMS Domain, consisting of predominantly interconnected structural highs and lows, and the relative evolution of a diverse invertebrate fauna characterized by terebratulid, ostreids, limids, brachiopods, crustaceans, and gastropods, attracted both hybodontids and durophagous ginglymodians in the Tethyan realm, influencing their dispersal during the Late Jurassic.
publishDate 2019
dc.date.none.fl_str_mv 2019-02
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/125811
Romano, Marco; Cipriani, Angelo; Fabbi, Simone; Citton, Paolo; First remains of neoginglymodian actinopterygians from the Jurassic of Monte Nerone area (Umbria-Marche Apennine, Italy); Società Geologica Italiana; Italian Journal of Geosciences; 138; 1; 2-2019; 88-102
2038-1719
2038-1727
CONICET Digital
CONICET
url http://hdl.handle.net/11336/125811
identifier_str_mv Romano, Marco; Cipriani, Angelo; Fabbi, Simone; Citton, Paolo; First remains of neoginglymodian actinopterygians from the Jurassic of Monte Nerone area (Umbria-Marche Apennine, Italy); Società Geologica Italiana; Italian Journal of Geosciences; 138; 1; 2-2019; 88-102
2038-1719
2038-1727
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.3301/IJG.2018.28
info:eu-repo/semantics/altIdentifier/url/https://www.italianjournalofgeosciences.it/297/article-964/first-remains-of-neoginglymodian-actinopterygians-from-the-jurassic-of-monte-nerone-area-umbria-marche-apennine-italy.html
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Società Geologica Italiana
publisher.none.fl_str_mv Società Geologica Italiana
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instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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