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Autor:
Mazaheri-Johari M.[1], Roghi G.[2], Caggiati M.[1], Kustatscher E.[3, Ghasemi-Nejad E.[5], Zanchi A.[6], Gianolla P.[1]
Publikováno v:
Palaeogeography, palaeoclimatology, palaeoecology 586 (2022). doi:10.1016/j.palaeo.2021.110777
info:cnr-pdr/source/autori:Mazaheri-Johari M.[1], Roghi G.[2], Caggiati M.[1], Kustatscher E.[3,4], Ghasemi-Nejad E.[5], Zanchi A.[6], Gianolla P.[1]/titolo:Disentangling climate signal from tectonic forcing: The Triassic Aghdarband Basin (Turan Domain, Iran)/doi:10.1016%2Fj.palaeo.2021.110777/rivista:Palaeogeography, palaeoclimatology, palaeoecology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:586
info:cnr-pdr/source/autori:Mazaheri-Johari M.[1], Roghi G.[2], Caggiati M.[1], Kustatscher E.[3,4], Ghasemi-Nejad E.[5], Zanchi A.[6], Gianolla P.[1]/titolo:Disentangling climate signal from tectonic forcing: The Triassic Aghdarband Basin (Turan Domain, Iran)/doi:10.1016%2Fj.palaeo.2021.110777/rivista:Palaeogeography, palaeoclimatology, palaeoecology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:586
The Middle–Upper Triassic Aghdarband Basin, NE Iran, consists of a strongly deformed marine and non-marine stratigraphic succession, deposited along the southern margin of Asia in a highly complex tectonic context related to a back-arc setting. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8e40dd37b2f0e4e77f6964b6152a1ea7
http://hdl.handle.net/10281/338795
http://hdl.handle.net/10281/338795
Publikováno v:
Review of Palaeobotany and Palynology, 296, 1. Elsevier Saunders
Review of palaeobotany and palynology 296 (2022). doi:10.1016/j.revpalbo.2021.104544
info:cnr-pdr/source/autori:Nowak H.[1], Kustatscher E.[1,2,3], Roghi G.[4], Van Konijnenburg-van Cittert J.H.A.[5,6]/titolo:Variability of in situ spores in some leptosporangiate ferns from the Triassic in Italy and Austria/doi:10.1016%2Fj.revpalbo.2021.104544/rivista:Review of palaeobotany and palynology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:296
Review of palaeobotany and palynology 296 (2022). doi:10.1016/j.revpalbo.2021.104544
info:cnr-pdr/source/autori:Nowak H.[1], Kustatscher E.[1,2,3], Roghi G.[4], Van Konijnenburg-van Cittert J.H.A.[5,6]/titolo:Variability of in situ spores in some leptosporangiate ferns from the Triassic in Italy and Austria/doi:10.1016%2Fj.revpalbo.2021.104544/rivista:Review of palaeobotany and palynology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:296
Spores or pollen from a single species or even an individual plant or sporangium may vary in morphology and size to a point that equivalent forms found dispersed in the sediment have been described as different species or even genera. In addition, no
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e6d1eafbf8ae922e02f547a627ed5906
https://dspace.library.uu.nl/handle/1874/414240
https://dspace.library.uu.nl/handle/1874/414240
Publikováno v:
Rivista italiana di paleontologia e stratigrafia (Testo stamp.) 128 (2022): 105–127.
info:cnr-pdr/source/autori:Forte G.[1], Kustatscher E.[1,2,3], Ragazzi E.[4], Roghi G.[5]/titolo:Amber droplets in the Southern Alps (NE Italy): a link between their occurrences and main humid episodes in the Triassic/doi:/rivista:Rivista italiana di paleontologia e stratigrafia (Testo stamp.)/anno:2022/pagina_da:105/pagina_a:127/intervallo_pagine:105–127/volume:128
info:cnr-pdr/source/autori:Forte G.[1], Kustatscher E.[1,2,3], Ragazzi E.[4], Roghi G.[5]/titolo:Amber droplets in the Southern Alps (NE Italy): a link between their occurrences and main humid episodes in the Triassic/doi:/rivista:Rivista italiana di paleontologia e stratigrafia (Testo stamp.)/anno:2022/pagina_da:105/pagina_a:127/intervallo_pagine:105–127/volume:128
The Anisian amber from the "Voltzia beds" of the Recoaro area, produced by Voltzia recubariensis, represents the most ancient Triassic amber known so far. The discovery of amber in the Anisian localities of Kühwiesenkopf/Monte Prà della Vacca and P
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::4b03efe3f039a0fcc9b1a2aa42a4a4d1
http://www.cnr.it/prodotto/i/464699
http://www.cnr.it/prodotto/i/464699
Autor:
Matamales- Andreu R.[1, Mujal E.[1, Dinarès-Turell J.[4], Kustatscher E.[5, Roghi G.[7], Oms O.[8], Galobart A.[1, Fortuny J.[1]
Publikováno v:
Dipòsit Digital de Documents de la UAB
Universitat Autònoma de Barcelona
Earth-science reviews 228 (2022). doi:10.1016/j.earscirev.2022.103948
info:cnr-pdr/source/autori:Matamales-Andreu R.[1,2], Mujal E.[1,3], Dinarès-Turell J.[4], Kustatscher E.[5,6], Roghi G.[7], Oms O.[8], Galobart A.[1,9], Fortuny J.[1]/titolo:Early-middle Permian ecosystems of equatorial Pangaea: Integrated multi-stratigraphic and palaeontological review of the Permian of Mallorca (Balearic Islands, western Mediterranean)/doi:10.1016%2Fj.earscirev.2022.103948/rivista:Earth-science reviews/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:228
Universitat Autònoma de Barcelona
Earth-science reviews 228 (2022). doi:10.1016/j.earscirev.2022.103948
info:cnr-pdr/source/autori:Matamales-Andreu R.[1,2], Mujal E.[1,3], Dinarès-Turell J.[4], Kustatscher E.[5,6], Roghi G.[7], Oms O.[8], Galobart A.[1,9], Fortuny J.[1]/titolo:Early-middle Permian ecosystems of equatorial Pangaea: Integrated multi-stratigraphic and palaeontological review of the Permian of Mallorca (Balearic Islands, western Mediterranean)/doi:10.1016%2Fj.earscirev.2022.103948/rivista:Earth-science reviews/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:228
Altres ajuts: CERCA Programme/Generalitat de Catalunya The Cisuralian-Guadalupian (early-middle Permian) was a period of climate transition between the Carboniferous icehouse conditions to the latest Permian-Early Triassic hothouse. The landmasses ha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::142115fd79a3a1bebfe2c4cbfffc0f7c
https://ddd.uab.cat/record/251863
https://ddd.uab.cat/record/251863
Publikováno v:
In Palaeogeography, Palaeoclimatology, Palaeoecology 2010 290(1):89-106
Akademický článek
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