High-resolution dynamics of Early Jurassic marine extinctions: the case of Pliensbachian–Toarcian ammonites (Cephalopoda).
13 pages International audience The Pliensbachian–Toarcian interval was marked by major environmental disturbances and by a second-order mass extinction. Here, we reappraise the taxonomic, spatiotemporal and selective dynamics of extinctions over the whole interval, by analysing a high-resolution da...
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ftunivnantes:oai:HAL:hal-00445515v1 2023-05-15T15:08:07+02:00 High-resolution dynamics of Early Jurassic marine extinctions: the case of Pliensbachian–Toarcian ammonites (Cephalopoda). Dera, Guillaume Neige, Pascal Dommergues, Jean-Louis Fara, Emmanuel Laffont, Rémi Pellenard, Pierre Biogéosciences UMR 6282 (BGS) Université de Bourgogne (UB)-Centre National de la Recherche Scientifique (CNRS) 2010-01 https://hal.archives-ouvertes.fr/hal-00445515 https://doi.org/10.1144/0016-76492009-068 en eng HAL CCSD info:eu-repo/semantics/altIdentifier/doi/10.1144/0016-76492009-068 hal-00445515 https://hal.archives-ouvertes.fr/hal-00445515 doi:10.1144/0016-76492009-068 Journal of the Geologcal Society https://hal.archives-ouvertes.fr/hal-00445515 Journal of the Geologcal Society, 2010, 167 (1), pp.21-33. ⟨10.1144/0016-76492009-068⟩ [SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology [SDV.BID]Life Sciences [q-bio]/Biodiversity info:eu-repo/semantics/article Journal articles 2010 ftunivnantes https://doi.org/10.1144/0016-76492009-068 2022-08-30T22:43:33Z 13 pages International audience The Pliensbachian–Toarcian interval was marked by major environmental disturbances and by a second-order mass extinction. Here, we reappraise the taxonomic, spatiotemporal and selective dynamics of extinctions over the whole interval, by analysing a high-resolution dataset of 772 ammonite species from NW Tethyan and Arctic domains. On average, 40–65% of ammonite species disappeared during each subchronozone, but higher extinction pulses (reaching 70–90%) prevailed from the Margaritatus to the Dispansum Chronozone. The main extinctions, corresponding to the Gibbosus, Pliensbachian–Toarcian boundary, Semicelatum, Bifrons–Variabilis, and Dispansum events, differed in their dynamics, suggesting episodes of ecological stress related to climate change, regression, disturbance in the carbon cycle or anoxia. The multi-pulsed volcanic activity in the Karoo–Ferrar province could well have triggered these ecological changes. In addition, ammonites experienced a morphological bottleneck during the Gibbosus event, 1 Ma before the Early Toarcian diversity collapse. Typically, drops in richness were related both to high extinctions and to declines in origination rates. This feature could result from strengthened ecological stresses related to the temporal overlap of environmental disturbances. After the Early Toarcian crisis, the recovery of ammonites was rapid (2 Ma) and probably influenced by a coeval marine transgression. Article in Journal/Newspaper Arctic Climate change Université de Nantes: HAL-UNIV-NANTES Arctic Journal of the Geological Society 167 1 21 33 |
institution |
Open Polar |
collection |
Université de Nantes: HAL-UNIV-NANTES |
op_collection_id |
ftunivnantes |
language |
English |
topic |
[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology [SDV.BID]Life Sciences [q-bio]/Biodiversity |
spellingShingle |
[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology [SDV.BID]Life Sciences [q-bio]/Biodiversity Dera, Guillaume Neige, Pascal Dommergues, Jean-Louis Fara, Emmanuel Laffont, Rémi Pellenard, Pierre High-resolution dynamics of Early Jurassic marine extinctions: the case of Pliensbachian–Toarcian ammonites (Cephalopoda). |
topic_facet |
[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology [SDV.BID]Life Sciences [q-bio]/Biodiversity |
description |
13 pages International audience The Pliensbachian–Toarcian interval was marked by major environmental disturbances and by a second-order mass extinction. Here, we reappraise the taxonomic, spatiotemporal and selective dynamics of extinctions over the whole interval, by analysing a high-resolution dataset of 772 ammonite species from NW Tethyan and Arctic domains. On average, 40–65% of ammonite species disappeared during each subchronozone, but higher extinction pulses (reaching 70–90%) prevailed from the Margaritatus to the Dispansum Chronozone. The main extinctions, corresponding to the Gibbosus, Pliensbachian–Toarcian boundary, Semicelatum, Bifrons–Variabilis, and Dispansum events, differed in their dynamics, suggesting episodes of ecological stress related to climate change, regression, disturbance in the carbon cycle or anoxia. The multi-pulsed volcanic activity in the Karoo–Ferrar province could well have triggered these ecological changes. In addition, ammonites experienced a morphological bottleneck during the Gibbosus event, 1 Ma before the Early Toarcian diversity collapse. Typically, drops in richness were related both to high extinctions and to declines in origination rates. This feature could result from strengthened ecological stresses related to the temporal overlap of environmental disturbances. After the Early Toarcian crisis, the recovery of ammonites was rapid (2 Ma) and probably influenced by a coeval marine transgression. |
author2 |
Biogéosciences UMR 6282 (BGS) Université de Bourgogne (UB)-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Dera, Guillaume Neige, Pascal Dommergues, Jean-Louis Fara, Emmanuel Laffont, Rémi Pellenard, Pierre |
author_facet |
Dera, Guillaume Neige, Pascal Dommergues, Jean-Louis Fara, Emmanuel Laffont, Rémi Pellenard, Pierre |
author_sort |
Dera, Guillaume |
title |
High-resolution dynamics of Early Jurassic marine extinctions: the case of Pliensbachian–Toarcian ammonites (Cephalopoda). |
title_short |
High-resolution dynamics of Early Jurassic marine extinctions: the case of Pliensbachian–Toarcian ammonites (Cephalopoda). |
title_full |
High-resolution dynamics of Early Jurassic marine extinctions: the case of Pliensbachian–Toarcian ammonites (Cephalopoda). |
title_fullStr |
High-resolution dynamics of Early Jurassic marine extinctions: the case of Pliensbachian–Toarcian ammonites (Cephalopoda). |
title_full_unstemmed |
High-resolution dynamics of Early Jurassic marine extinctions: the case of Pliensbachian–Toarcian ammonites (Cephalopoda). |
title_sort |
high-resolution dynamics of early jurassic marine extinctions: the case of pliensbachian–toarcian ammonites (cephalopoda). |
publisher |
HAL CCSD |
publishDate |
2010 |
url |
https://hal.archives-ouvertes.fr/hal-00445515 https://doi.org/10.1144/0016-76492009-068 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Climate change |
genre_facet |
Arctic Climate change |
op_source |
Journal of the Geologcal Society https://hal.archives-ouvertes.fr/hal-00445515 Journal of the Geologcal Society, 2010, 167 (1), pp.21-33. ⟨10.1144/0016-76492009-068⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1144/0016-76492009-068 hal-00445515 https://hal.archives-ouvertes.fr/hal-00445515 doi:10.1144/0016-76492009-068 |
op_doi |
https://doi.org/10.1144/0016-76492009-068 |
container_title |
Journal of the Geological Society |
container_volume |
167 |
container_issue |
1 |
container_start_page |
21 |
op_container_end_page |
33 |
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1766339533214842880 |