Zobrazeno 1 - 10 of 21 pro vyhledávání: '"PE10_6"'
1
An Exceptionally Preserved Terrestrial Record of LIP Effects on Plants in the Carnian (Upper Triassic) Amber-Bearing Section of the Dolomites, Italy
Autor: Guido Roghi, Piero Gianolla, Evelyn Kustatscher, Alexander R. Schmidt, Leyla J. Seyfullah
Publikováno v: Frontiers in Earth Science. 10
The Carnian Pluvial Episode (CPE) has been recognized as a time of plant radiations and originations, likely related to observed swift changes from xerophytic to more hygrophytic floras. This suggests that the increasing humidity causally resulting f
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::634132b36e64b627ea070a6ed78dda1a
https://doi.org/10.3389/feart.2022.900586
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3
Neanderthals’ hunting seasonality inferred from combined cementochronology, mesowear and microwear analysis : case studies from the alpine foreland in Italy
Autor: Alessandra Livraghi, Florent Rivals, William Rendu, Marco Peresani
Herbivore teeth are a valuable source of information for inferring the hunting season of past hunter-gatherers, the spatial–temporal organization of their activities, their socio-economic organization, and their adaptation to the seasonal fluctuati
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2d6b59302e16827531ea2a0d5e87c3bd
http://hdl.handle.net/11392/2479155
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4
Disentangling climate signal from tectonic forcing: The Triassic Aghdarband Basin (Turan Domain, Iran)
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
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
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5
Environmental and climatic context of the hominin occurrence in northeastern Italy from the late Middle to Late Pleistocene inferred from small-mammal assemblages
Autor: Juan Manuel López-García, Marco Peresani, Claudio Berto
Publikováno v: Repositório Científico de Acesso Aberto de Portugal
Repositório Científico de Acesso Aberto de Portugal (RCAAP)
instacron:RCAAP
The environmental and climatic evolution of the late Middle Pleistocene to Late Pleistocene of the northeastern Italy is determined for Marine Isotope Stage 7 (MIS 7) to MIS 3 on the basis of a study of the small-mammal (insectivore, bat and rodent)
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::10009fdeb11c47457008ac00009df032
https://doi.org/10.1016/j.quascirev.2019.05.025
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9
A monotypic stand of Neocalamites iranensis n. sp. from the Carnian Pluvial Episode (Late Triassic) of the Aghdarband area, NE Iran (Turan Plate)
Autor: Mazaheri-Johari M.[1], Kustatscher E.[2, Roghi G.[4], Ghasemi-Nejad E.[5], Gianolla P.[1]
Publikováno v: Rivista italiana di paleontologia e stratigrafia (Online) 127 (2021): 189–209. doi:10.13130/2039-4942/15646
info:cnr-pdr/source/autori:Mazaheri-Johari M.[1], Kustatscher E.[2,3], Roghi G.[4], Ghasemi-Nejad E.[5], Gianolla P.[1]/titolo:A monotypic stand of Neocalamites iranensis n. sp. from the Carnian Pluvial Episode (Late Triassic) of the Aghdarband area, NE Iran (Turan Plate)/doi:10.13130%2F2039-4942%2F15646/rivista:Rivista italiana di paleontologia e stratigrafia (Online)/anno:2021/pagina_da:189/pagina_a:209/intervallo_pagine:189–209/volume:127
RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA ; Vol. 127 No. 2 (2021)
Rivista italiana di Paleontologia e Stratigrafia; V. 127 N. 2 (2021)
Rivista Italiana di Paleontologia e Stratigrafia, Vol 127, Iss 2 (2021)
The Aghdarband Basin in the Kopeh-Dagh Range (NE Iran) is one of the most important areas for unraveling the evolution of the Turan plate (southern margin of Eurasia) during the last phase of the closure of the Paleotethys and to reconstruct the hist
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::60e8e74df989b9ca0acc8f2d75b0c26b
https://riviste.unimi.it/index.php/RIPS
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10
Hunter-gatherers across the great Adriatic-Po region during the Last Glacial Maximum: Environmental and cultural dynamics
Autor: Peresani M.[1, Monegato G.[2], Ravazzi C.[3], Bertola S.[1], Margaritora D.[1], Breda M.[1, Fontana A.[5], Fontana F.[1], Jankovic I.[6, Karavanic I.[8, Komso D.[9], Mozzi P.[5], Pini R.[3], Furlanetto G.[3, 10], De Amicis M.G.M.[10], Perhoc Z.[11], Posth C.[12], Ronchi L.[5], Rossato S.[2, Vukosavljevic N.[8], Zerboni A.[13]
Publikováno v: Quaternary international 581-582 (2021): 128–163. doi:10.1016/j.quaint.2020.10.007
info:cnr-pdr/source/autori:Peresani M.[1,3], Monegato G.[2], Ravazzi C.[3], Bertola S.[1], Margaritora D.[1], Breda M.[1,4], Fontana A.[5], Fontana F.[1], Jankovic I.[6,7], Karavanic I.[8,7], Komso D.[9], Mozzi P.[5], Pini R.[3], Furlanetto G.[3,10], De Amicis M.G.M.[10], Perhoc Z.[11], Posth C.[12], Ronchi L.[5], Rossato S.[2,5], Vukosavljevic N.[8], Zerboni A.[13]/titolo:Hunter-gatherers across the great Adriatic-Po region during the Last Glacial Maximum: Environmental and cultural dynamics/doi:10.1016%2Fj.quaint.2020.10.007/rivista:Quaternary international/anno:2021/pagina_da:128/pagina_a:163/intervallo_pagine:128–163/volume:581-582
During the Last Glacial Maximum (LGM, 30 to 16.5 ka ago), the Great Adriatic-Po Region (GAPR) was deeply affected by the spread of glaciers from the Alps to the southern foreland and by the dropping of the sea level to ~ -120 m amsl. The combination
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5c3265a28fd5355709ce13a3046467ec
http://hdl.handle.net/11392/2425164
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