Taphonomy and evolution of Lower Jurassic lithiotid bivalve accumulations in the Apennine Carbonate Platform (southern Italy)
Lower Jurassic Tethyan and Panthalassan marine shallow-water successions are characterized by aberrant li- thiotid bivalves belonging to the Lithiotis Fauna. Their widespread occurrence, often in rock-forming abundance, represents a global biofacies, mostly restricted to the Pliensbachian–early Toar...
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Online Access: | http://hdl.handle.net/11588/691681 https://doi.org/10.1016/j.palaeo.2017.10.017 https://www.sciencedirect.com/science/article/pii/S0031018217308738 |
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ftunivnapoliiris:oai:www.iris.unina.it:11588/691681 2024-09-09T20:01:46+00:00 Taphonomy and evolution of Lower Jurassic lithiotid bivalve accumulations in the Apennine Carbonate Platform (southern Italy) Posenato, Renato Bassi, Davide TRECALLI, ALBERTO PARENTE, MARIANO Posenato, Renato Bassi, Davide Trecalli, Alberto Parente, Mariano 2018 http://hdl.handle.net/11588/691681 https://doi.org/10.1016/j.palaeo.2017.10.017 https://www.sciencedirect.com/science/article/pii/S0031018217308738 eng eng info:eu-repo/semantics/altIdentifier/wos/WOS:000416501000020 volume:489 firstpage:261 lastpage:271 numberofpages:11 journal:PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY http://hdl.handle.net/11588/691681 doi:10.1016/j.palaeo.2017.10.017 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85033561905 https://www.sciencedirect.com/science/article/pii/S0031018217308738 Rock-forming bivalves Carbonate platforms T-OAE Global warming Ocean acidification info:eu-repo/semantics/article 2018 ftunivnapoliiris https://doi.org/10.1016/j.palaeo.2017.10.017 2024-06-17T15:19:32Z Lower Jurassic Tethyan and Panthalassan marine shallow-water successions are characterized by aberrant li- thiotid bivalves belonging to the Lithiotis Fauna. Their widespread occurrence, often in rock-forming abundance, represents a global biofacies, mostly restricted to the Pliensbachian–early Toarcian. Despite their wide occur- rence and their prominent role as carbonate producers in shallow-water platforms, the biogeographic and stratigraphic distribution of this group of bivalves and their evolutionary history are obscure, mostly because they commonly have not been identified at the generic or specific level. In particular, their evolution and demise in relation to important global palaeoenvironmental perturbations, such as the Pliensbachian-Toarcian boundary event and the early Toarcian oceanic anoxic event are not yet known in detail. In the Apennine Carbonate Platform of southern Italy, the Lithiotis Member, in the upper part of the Lower Jurassic Palaeodasycladus Limestones Formation, is characterized by the abundant occurrence of lithiotid bi- valves. They disappear abruptly in the lowermost beds of the overlying Oolitic-oncolitic Limestones Formation, at the onset of the early Toarcian Oceanic Anoxic Event. More than 60 lithiotid bivalve concentrations occur in a nearly 120 m-thick succession spectacularly exposed on freshly cut walls in a quarry west of Mercato San Severino (Salerno). Field observations on the taxonomic composition and fabric of the shell beds (packing, maximum shell size, degree of shell articulation and fragmentation) allowed to distinguish four taphofacies (A–D). Taphofacies A records the appearance and spreading of the lithiotids, with accumulations characterized mainly by small-sized and loosely packed shells. Taphofacies B records the acme of lithiotid bivalves, with densely packed accumulations of large shells. These two taphofacies yield prevailing articulated individuals, commonly in life position. Taphofacies C records a decrease of the shell packing and frequency of ... Article in Journal/Newspaper Ocean acidification IRIS Università degli Studi di Napoli Federico II Palaeogeography, Palaeoclimatology, Palaeoecology 489 261 271 |
institution |
Open Polar |
collection |
IRIS Università degli Studi di Napoli Federico II |
op_collection_id |
ftunivnapoliiris |
language |
English |
topic |
Rock-forming bivalves Carbonate platforms T-OAE Global warming Ocean acidification |
spellingShingle |
Rock-forming bivalves Carbonate platforms T-OAE Global warming Ocean acidification Posenato, Renato Bassi, Davide TRECALLI, ALBERTO PARENTE, MARIANO Taphonomy and evolution of Lower Jurassic lithiotid bivalve accumulations in the Apennine Carbonate Platform (southern Italy) |
topic_facet |
Rock-forming bivalves Carbonate platforms T-OAE Global warming Ocean acidification |
description |
Lower Jurassic Tethyan and Panthalassan marine shallow-water successions are characterized by aberrant li- thiotid bivalves belonging to the Lithiotis Fauna. Their widespread occurrence, often in rock-forming abundance, represents a global biofacies, mostly restricted to the Pliensbachian–early Toarcian. Despite their wide occur- rence and their prominent role as carbonate producers in shallow-water platforms, the biogeographic and stratigraphic distribution of this group of bivalves and their evolutionary history are obscure, mostly because they commonly have not been identified at the generic or specific level. In particular, their evolution and demise in relation to important global palaeoenvironmental perturbations, such as the Pliensbachian-Toarcian boundary event and the early Toarcian oceanic anoxic event are not yet known in detail. In the Apennine Carbonate Platform of southern Italy, the Lithiotis Member, in the upper part of the Lower Jurassic Palaeodasycladus Limestones Formation, is characterized by the abundant occurrence of lithiotid bi- valves. They disappear abruptly in the lowermost beds of the overlying Oolitic-oncolitic Limestones Formation, at the onset of the early Toarcian Oceanic Anoxic Event. More than 60 lithiotid bivalve concentrations occur in a nearly 120 m-thick succession spectacularly exposed on freshly cut walls in a quarry west of Mercato San Severino (Salerno). Field observations on the taxonomic composition and fabric of the shell beds (packing, maximum shell size, degree of shell articulation and fragmentation) allowed to distinguish four taphofacies (A–D). Taphofacies A records the appearance and spreading of the lithiotids, with accumulations characterized mainly by small-sized and loosely packed shells. Taphofacies B records the acme of lithiotid bivalves, with densely packed accumulations of large shells. These two taphofacies yield prevailing articulated individuals, commonly in life position. Taphofacies C records a decrease of the shell packing and frequency of ... |
author2 |
Posenato, Renato Bassi, Davide Trecalli, Alberto Parente, Mariano |
format |
Article in Journal/Newspaper |
author |
Posenato, Renato Bassi, Davide TRECALLI, ALBERTO PARENTE, MARIANO |
author_facet |
Posenato, Renato Bassi, Davide TRECALLI, ALBERTO PARENTE, MARIANO |
author_sort |
Posenato, Renato |
title |
Taphonomy and evolution of Lower Jurassic lithiotid bivalve accumulations in the Apennine Carbonate Platform (southern Italy) |
title_short |
Taphonomy and evolution of Lower Jurassic lithiotid bivalve accumulations in the Apennine Carbonate Platform (southern Italy) |
title_full |
Taphonomy and evolution of Lower Jurassic lithiotid bivalve accumulations in the Apennine Carbonate Platform (southern Italy) |
title_fullStr |
Taphonomy and evolution of Lower Jurassic lithiotid bivalve accumulations in the Apennine Carbonate Platform (southern Italy) |
title_full_unstemmed |
Taphonomy and evolution of Lower Jurassic lithiotid bivalve accumulations in the Apennine Carbonate Platform (southern Italy) |
title_sort |
taphonomy and evolution of lower jurassic lithiotid bivalve accumulations in the apennine carbonate platform (southern italy) |
publishDate |
2018 |
url |
http://hdl.handle.net/11588/691681 https://doi.org/10.1016/j.palaeo.2017.10.017 https://www.sciencedirect.com/science/article/pii/S0031018217308738 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_relation |
info:eu-repo/semantics/altIdentifier/wos/WOS:000416501000020 volume:489 firstpage:261 lastpage:271 numberofpages:11 journal:PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY http://hdl.handle.net/11588/691681 doi:10.1016/j.palaeo.2017.10.017 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85033561905 https://www.sciencedirect.com/science/article/pii/S0031018217308738 |
op_doi |
https://doi.org/10.1016/j.palaeo.2017.10.017 |
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Palaeogeography, Palaeoclimatology, Palaeoecology |
container_volume |
489 |
container_start_page |
261 |
op_container_end_page |
271 |
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