Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Samuel Mailliot"'
Publikováno v:
SEDICI (UNLP)
Universidad Nacional de La Plata
instacron:UNLP
Universidad Nacional de La Plata
instacron:UNLP
A large, broadly elliptical coccolith of the genus Similiscutum (Biscutaceae) was observed in sediments dated from the Lower Jurassic (upper Pliensbachian to Toarcian) coming from different localities of western Tethys, namely Portugal (Lusitanian Ba
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fba8ec91e347816c43f474447cbc4680
https://jm.copernicus.org/articles/42/1/2023/
https://jm.copernicus.org/articles/42/1/2023/
Autor:
María José Comas-Rengifo, Kate Littler, Maria Cristina Cabral, Luís V. Duarte, Serge Elmi, Hugh C. Jenkyns, Luiz Carlos Veiga de Oliveira, Antonio Goy, René Mouterde, Samuel Mailliot, Guillaume Suan, Christiane Ruget, Stephen P. Hesselbo, Nicola Perilli, Susana Pinto, Bernard Pittet, Emanuela Mattioli, María Luisa Osete, Rogério Rocha, Juan J. Gómez
Publikováno v:
Episodes Journal of International Geoscience
Episodes Journal of International Geoscience, 2016, ⟨10.18814/epiiugs/2016/v39i3/99741⟩
Episodes Journal of International Geoscience, Seoul National University, 2016, ⟨10.18814/epiiugs/2016/v39i3/99741⟩
Digital.CSIC. Repositorio Institucional del CSIC
instname
Episodes Journal of International Geoscience, 2016, ⟨10.18814/epiiugs/2016/v39i3/99741⟩
Episodes Journal of International Geoscience, Seoul National University, 2016, ⟨10.18814/epiiugs/2016/v39i3/99741⟩
Digital.CSIC. Repositorio Institucional del CSIC
instname
The Global Stratotype Section and Point (GSSP) for the base of Toarcian Stage, Lower Jurassic, is placed at the base of micritic limestone bed 15e at Ponta do Trovão (Peniche, Lusitanian Basin, Portugal; coordinates: 39°22'15''N, 9°23'07''W), 80km
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5b3375f1301e9cccb09d1988f53bcb2e
https://hal.science/hal-01403277
https://hal.science/hal-01403277
Publikováno v:
Global and Planetary Change. 65:134-145
In this account we present estimates of nannofossil fluxes in four sections and one borehole all belonging to the Early Jurassic western Tethys. This study aims to map the distribution of pelagic carbonate production across the Early Toarcian anoxic
Publikováno v:
Paleoceanography. 23
Calcareous nannoplankton were profoundly affected by environmental perturbations coincident with the early Toarcian oceanic anoxic event (T-OAE). We quantify the abundance of nannofossils across the T-OAE at three locations in Western Europe, where t
Publikováno v:
Paleoceanography. 23
The timing and causal relationships between the pronounced negative C isotope excursion and paleoenvironmental perturbations associated with the Toarcian oceanic anoxic event (Early Jurassic) remain unclear, particularly because biotic crises and car
Autor:
Ivan Bour, Luís V. Duarte, Guillaume Suan, Samuel Mailliot, Bernard Pittet, Emanuela Mattioli
Publikováno v:
Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
Annual Review of Earth and Planetary Sciences
Annual Review of Earth and Planetary Sciences, Annual Reviews, 2008, 267, pp.666-679
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
Annual Review of Earth and Planetary Sciences
Annual Review of Earth and Planetary Sciences, Annual Reviews, 2008, 267, pp.666-679
The marked 3-8[per mille sign] negative carbon isotope excursion associated with the Early Toarcian oceanic anoxic event (OAE; ~ 183 myr ago) in the Early Jurassic period is thought to represent one of the most important perturbations of the C-cycle
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ddc57dd5d03e253f0a989ac27c459b88
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology
Palaeogeography, Palaeoclimatology, Palaeoecology, Elsevier, 2006, 240, pp.562-586. ⟨10.1016/j.palaeo.2006.02.016⟩
Palaeogeography, Palaeoclimatology, Palaeoecology, Elsevier, 2006, 240, pp.562-586. ⟨10.1016/j.palaeo.2006.02.016⟩
International audience; During the Early Toarcian, major paleoenvironnemental and paleoceanographical changes occurred, leading to an oceanic anoxic event (OAE) and to a perturbation of the carbon isotope cycle. Although the standard biochronology of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1b39e8cd85437516f45592658ba5edef
https://hal.archives-ouvertes.fr/hal-00144732
https://hal.archives-ouvertes.fr/hal-00144732