Origin and Evolution of Enzymes with MIO Prosthetic Group: Microbial Coevolution After the Mass Extinction Event

Autor: Fei Peng, Ulrike Engel, Habibu Aliyu, Jens Rudat

Publikováno v: Frontiers in Genetics, Vol 13 (2022)

After major mass extinction events, ancient plants and terrestrial vertebrates were faced with various challenges, especially ultraviolet (UV) light. These stresses probably resulted in changes in the biosynthetic pathways, which employed the MIO (3,

Externí odkaz: https://doaj.org/article/6797824443ae4745a1f493d07103f16b

The last representatives of the Superfamily Wellerelloidea (Brachiopoda, Rhynchonellida) in the westernmost Tethys (Iberian paleomargins) prior to their demise in the early Toarcian Mass Extinction Event

Autor: José Francisco Baeza Carratalá, Fernando García Joral

Publikováno v: RUA. Repositorio Institucional de la Universidad de Alicante
Universidad de Alicante (UA)
E-Prints Complutense. Archivo Institucional de la UCM
instname

The last clade-level extinction episode affecting the Phylum Brachiopoda has been long-established in the Early Toarcian Mass Extinction Event (ETMEE) around the Pliensbachian-Toarcian transition, when several rhynchonellide groups became extinct and

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c7a87b85fa3891ebaf9ef11c2ad1a227
https://hdl.handle.net/10045/123461

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The Central Atlantic Magmatic Province (CAMP) in Morocco

Autor: Fida Medina, Alberto Zanetti, Mohamed Khalil Bensalah, Andrea Marzoli, Hervé Bertrand, Laurie Reisberg, Massimo Chiaradia, Hind El Hachimi, Sarah I Brownlee, Christian Tegner, Tiberio Cuppone, Renaud E. Merle, Nasrrddine Youbi, Fred Jourdan, Sara Callegaro, Joshua Davies, Paul R. Renne, Abdelkader Mahmoudi, Giuliano Bellieni, Stefano Crivellari, Christine Meyzen

Publikováno v: Journal of Petrology
Journal of Petrology, Oxford University Press (OUP), 2019, 60 (5), pp.945-996. ⟨10.1093/petrology/egz021⟩
Marzoli, A, Bertrand, H, Youbi, N, Callegaro, S, Merle, R, Reisberg, L, Chiaradia, M, Brownlee, S, Jourdan, F, Zanetti, A, Davies, J H F L, Cuppone, T, Mahmoudi, A, Medina, F, Renne, P R, Bellieni, G, Crivellari, S, El Hachimi, H, Bensalah, M K, Meyzen, C M & Tegner, C 2019, ' The Central Atlantic Magmatic Province (CAMP) in Morocco ', Journal of Petrology, vol. 60, no. 5, pp. 945-995 . https://doi.org/10.1093/petrology/egz021
Journal of Petrology, Vol. 60, No 5 (2019) pp. 945-996
Journal of petrology
60 (2019): 945–996. doi:10.1093/petrology/egz021
info:cnr-pdr/source/autori:Marzoli A.[1,19] Bertrand H.[2] Youbi N.[3,4] Callegaro S.[5], Merle R.[6] Reisberg L.[7], Chiaradia M.[8], Brownlee S.I.[9], Jourdan F.[10], Zanetti A.[11], Davies J.H.F.L.[8], Cuppone T.[1] Mahmoudi A.[12] Medina F.[13], Renne P.R.[14,15], Bellieni G.[1], Crivellari S.[16], El Hachimi H.[17], Bensalah M.K.[3,4] Meyzen C.M.[1] Tegner C. [18]/titolo:The Central Atlantic Magmatic Province (CAMP) in Morocco/doi:10.1093%2Fpetrology%2Fegz021/rivista:Journal of petrology (Print)/anno:2019/pagina_da:945/pagina_a:996/intervallo_pagine:945–996/volume:60
Journal of Petrology, 2019, 60 (5), pp.945-996. ⟨10.1093/petrology/egz021⟩

The Central Atlantic Magmatic Province (CAMP) is a large igneous province (LIP) composed of basic dykes, sills, layered intrusions and lava flows emplaced before Pangea break-up and currently distributed on the four continents surrounding the Atlanti

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::17899401d49ea698cd6154d882450dfd
https://hal.univ-lorraine.fr/hal-02405965/document

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