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Biotic recovery after the end-Triassic extinction event: Evidence from marine bivalves of the Neuquén Basin, Argentina

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Biotic recovery after the end-Triassic extinction event: Evidence from marine bivalves of the Neuquén Basin, Argentina

dc.contributor.author	Damborenea, Susana E.
dc.contributor.author	Echevarría, Javier
dc.contributor.author	Ros Franch, Sonia
dc.date.accessioned	2022-12-21T14:42:09Z
dc.date.available	2022-12-21T14:42:09Z
dc.date.issued	2017
dc.identifier.citation	Damborenea, Susana E. Echevarría, Javier Ros Franch, Sonia 2017 Biotic recovery after the end-Triassic extinction event: Evidence from marine bivalves of the Neuquén Basin, Argentina Palaeogeography Palaeoclimatology Palaeoecology 487 93 104
dc.identifier.uri	https://hdl.handle.net/10550/84848
dc.description.abstract	We analyze the Late Triassic extinction and Early Jurassic recovery of bivalve faunas within marine environments in the Atuel River area of the Neuquén Basin, Argentina. Data were collected from a hundred samples with invertebrates in a well-exposed uppermost Triassic to lower Jurassic section in the Neuquén Basin (southern Mendoza Province, Argentina) and allow a high-resolution reconstruction of the local diversity dynamics. The nearly continuous presence of marine stenohaline major taxa such as cnidarians, rhynchonelliform brachiopods, echinoderms and cephalopods indicates normal salinity throughout. All bivalve species were identified, and each occurrence was recorded in meters above the base. To analyze the systematic diversity trends, diversity curves were calculated on the basis of the first and last occurrence data for each bivalve species, and both total diversity and boundary crossers diversity were used. As a result, four main phases were identified: a) Triassic equilibrium phase (Rhaetian), with relatively high origination and extinction rates; b) extinction phase (latest Rhaetian to earliest Hettangian), with high extinction rates and low origination rates; c) recovery phase (late Early to early Late Hettangian), with high origination rates and almost null extinction rates; and d) Jurassic equilibrium phase (Late Hettangian-Sinemurian), again with similar and relatively high origination and extinction rates. The extinction and recovery phases are separated by a gap of about 135 m without identifiable benthonic invertebrates but with early Hettangian ammonites. On the other hand, bivalve palaeoecologic diversity seems to have been more homogeneous along the section, being dominated by attached epifaunal species, though before the extinction epifaunal habits were slightly surpassed by infaunal ones. Slight differences observed include a) shallow burrowers were more diverse during the Rhaetian than during the earliest Jurassic and b) epifaunal free-lying and semi-infaunal attached bivalves were more diverse after the Rhaetian extinction.
dc.language.iso	eng
dc.relation.ispartof	Palaeogeography Palaeoclimatology Palaeoecology, 2017, vol. 487, p. 93-104
dc.subject	Fauna marina
dc.subject	Mol·luscos
dc.subject	Vida (Biologia)
dc.title	Biotic recovery after the end-Triassic extinction event: Evidence from marine bivalves of the Neuquén Basin, Argentina
dc.type	journal article	es_ES
dc.date.updated	2022-12-21T14:42:10Z
dc.identifier.doi	10.1016/j.palaeo.2017.08.025
dc.identifier.idgrec	155962
dc.rights.accessRights	open access	es_ES