Zobrazeno 1 - 10
of 179
pro vyhledávání: '"Catanzariti, R."'
Publikováno v:
Neues Jahrbuch für Geologie und Paläontologie. Abhandlungen 299 (2021): 237–249. doi:10.1127/njgpa/2021/0966
info:cnr-pdr/source/autori:Di Cencio A.[1,2], Dulai A.[3], Catanzariti R.[4], Casati S.[1], Collareta A.[5,6]/titolo:First record of the brachiopod Lingula ? from the Pliocene of Tuscany (Italy): the youngest occurrence of lingulides in the Mediterranean Basin/doi:10.1127%2Fnjgpa%2F2021%2F0966/rivista:Neues Jahrbuch für Geologie und Paläontologie. Abhandlungen/anno:2021/pagina_da:237/pagina_a:249/intervallo_pagine:237–249/volume:299
info:cnr-pdr/source/autori:Di Cencio A.[1,2], Dulai A.[3], Catanzariti R.[4], Casati S.[1], Collareta A.[5,6]/titolo:First record of the brachiopod Lingula ? from the Pliocene of Tuscany (Italy): the youngest occurrence of lingulides in the Mediterranean Basin/doi:10.1127%2Fnjgpa%2F2021%2F0966/rivista:Neues Jahrbuch für Geologie und Paläontologie. Abhandlungen/anno:2021/pagina_da:237/pagina_a:249/intervallo_pagine:237–249/volume:299
We report on new fossils of chitinophosphatic brachiopods from Upper Pliocene (Piacenzian) marginal-marine clayey sands cropping out at La Serra (Tuscany, central Italy). Based on their morphological characters, these specimens are here assigned to t
Akademický článek
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Autor:
Barbero, E., Delavari, M., Dolati, A., Pandolfi, L., Saccani, E., Marroni, M., Dirosa, M., Zaccarini, F., Catanzariti, R., Chiari, M., Luciani, V.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3709::035263a6a1bc93efc2783e104ce909c4
http://hdl.handle.net/11392/2478176
http://hdl.handle.net/11392/2478176
Autor:
Coccioni R., Montanari A., Bosch S., Catanzariti R., Frontalini F., Jovane L., Lermen Kochhann M. V., Pelosi N., Sabatino N., Savian J. F., Sprovieri M.
Publikováno v:
From the Guajira Desert to the Apennines, and from Mediterranean Microplates to the Mexican Killer Asteroid: Honoring the Career of Walter Alvarez, edited by Koeberl C.; Claeys P.; Montanari A., pp. 311–346. Boulder: Geological Society Of America, Inc., 2022
At present, the Global Stratotype Section and Point (GSSP) for the base of the Bartonian remains the only GSSP of the Paleogene System to be defined by the Inter- national Subcommission on Paleogene Stratigraphy (ISPS) and the International Commissio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_____10604::841be30299a218493df26c8a089e59d2
https://openportal.ispc.cnr.it/doc?id=people______::fd1fad4e9b716f32cd96fbc5b329a766
https://openportal.ispc.cnr.it/doc?id=people______::fd1fad4e9b716f32cd96fbc5b329a766
Autor:
Özcan E.[1], Yücel A.O.[1], Catanzariti R.[2], Kaygili S.[3], Okay A.I.[1, Simmons M.D.[5], Pignatti J.[6], Abbasi I.A.[7], Erbil U.[4
Publikováno v:
Swiss journal of palaeontology
140 (2021): 1–30. doi:10.1186/s13358-021-00219-x
info:cnr-pdr/source/autori:Özcan E.[1], Yücel A.O.[1], Catanzariti R.[2], Kaygili S.[3], Okay A.I.[1,4],Simmons M.D.[5], Pignatti J.[6], Abbasi I.A.[7], Erbil U.[4,8]/titolo:Multiple Orbitoides d'Orbigny lineages in the Maastrichtian? Data from the Central Sakarya Basin (Turkey) and Arabian Platform successions (Southeastern Turkey and Oman)/doi:10.1186%2Fs13358-021-00219-x/rivista:Swiss journal of palaeontology (Print)/anno:2021/pagina_da:1/pagina_a:30/intervallo_pagine:1–30/volume:140
Swiss Journal of Palaeontology, Vol 140, Iss 1, Pp 1-30 (2021)
140 (2021): 1–30. doi:10.1186/s13358-021-00219-x
info:cnr-pdr/source/autori:Özcan E.[1], Yücel A.O.[1], Catanzariti R.[2], Kaygili S.[3], Okay A.I.[1,4],Simmons M.D.[5], Pignatti J.[6], Abbasi I.A.[7], Erbil U.[4,8]/titolo:Multiple Orbitoides d'Orbigny lineages in the Maastrichtian? Data from the Central Sakarya Basin (Turkey) and Arabian Platform successions (Southeastern Turkey and Oman)/doi:10.1186%2Fs13358-021-00219-x/rivista:Swiss journal of palaeontology (Print)/anno:2021/pagina_da:1/pagina_a:30/intervallo_pagine:1–30/volume:140
Swiss Journal of Palaeontology, Vol 140, Iss 1, Pp 1-30 (2021)
The standard reconstruction of species of Orbitoides d’Orbigny into a single lineage during the late Santonian to the end of the Maastrichtian is based upon morphometric data from Western Europe. An irreversible increase in the size of the embryoni
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2b5d5e3ddea99ea9fec2ef597429f358
https://publications.cnr.it/doc/460061
https://publications.cnr.it/doc/460061
Autor:
Kochhann M.V.L.[1], Savian J.F.[2], Tori F.[3], Catanzariti R.[4], Coccioni R.[5], Frontalini F.[6], Jovane L.[7], Florindo F.[8], Monechi S.[3
Publikováno v:
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
Palaeogeography, palaeoclimatology, palaeoecology 577 (2021): 1–17. doi:10.1016/j.palaeo.2021.110563
info:cnr-pdr/source/autori:Kochhann M.V.L.[1], Savian J.F.[2], Tori F.[3], Catanzariti R.[4], Coccioni R.[5], Frontalini F.[6], Jovane L.[7], Florindo F.[8], Monechi S.[3,9]/titolo:Orbital tuning for the middle Eocene to early Oligocene Monte Cagnero Section (Central Italy): Paleoenvironmental and paleoclimatic implications/doi:10.1016%2Fj.palaeo.2021.110563/rivista:Palaeogeography, palaeoclimatology, palaeoecology/anno:2021/pagina_da:1/pagina_a:17/intervallo_pagine:1–17/volume:577
Universidade de São Paulo (USP)
instacron:USP
Palaeogeography, palaeoclimatology, palaeoecology 577 (2021): 1–17. doi:10.1016/j.palaeo.2021.110563
info:cnr-pdr/source/autori:Kochhann M.V.L.[1], Savian J.F.[2], Tori F.[3], Catanzariti R.[4], Coccioni R.[5], Frontalini F.[6], Jovane L.[7], Florindo F.[8], Monechi S.[3,9]/titolo:Orbital tuning for the middle Eocene to early Oligocene Monte Cagnero Section (Central Italy): Paleoenvironmental and paleoclimatic implications/doi:10.1016%2Fj.palaeo.2021.110563/rivista:Palaeogeography, palaeoclimatology, palaeoecology/anno:2021/pagina_da:1/pagina_a:17/intervallo_pagine:1–17/volume:577
During the middle Eocene to early Oligocene Earth transitioned from a greenhouse to an icehouse climate state. The interval comprises the Middle Eocene Climatic Optimum (MECO; ~40 Ma) and a subsequent long-term cooling trend that culminated in the Eo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::25d2779570a6438a03abca3922cdc1c0
Autor:
D'Onofrio R.[1], Zaky A.S.[2, Frontalini F.[4], Luciani V.[1], Catanzariti R.[5], Francescangeli F.[6], Giorgioni M.[7], Coccioni R.[4], Özcan E.[8], Jovane L.[9]
Publikováno v:
Applied sciences 11 (2021): 1–25. doi:10.3390/app112311339
info:cnr-pdr/source/autori:D'Onofrio R.[1], Zaky A.S.[2,3], Frontalini F.[4], Luciani V.[1], Catanzariti R.[5], Francescangeli F.[6], Giorgioni M.[7], Coccioni R.[4], Özcan E.[8], Jovane L.[9]/titolo:Impact of the Middle Eocene Climatic Optimum (MECO) on Foraminiferal and Calcareous Nannofossil Assemblages in the Neo-Tethyan Baskil Section (Eastern Turkey): Paleoenvironmental and Paleoclimatic Reconstructions/doi:10.3390%2Fapp112311339/rivista:Applied sciences/anno:2021/pagina_da:1/pagina_a:25/intervallo_pagine:1–25/volume:11
Applied Sciences; Volume 11; Issue 23; Pages: 11339
D’Onofrio, Roberta; Zaky, Amr S.; Frontalini, Fabrizio; Luciani, Valeria; Catanzariti, Rita; Francescangeli, Fabio; Giorgioni, Martino; Coccioni, Rodolfo; Özcan, Ercan; Jovane, Luigi (2021). Impact of the Middle Eocene Climatic Optimum (MECO) on Foraminiferal and Calcareous Nannofossil Assemblages in the Neo-Tethyan Baskil Section (Eastern Turkey): Paleoenvironmental and Paleoclimatic Reconstructions. Applied Sciences, 11(23), p. 11339. MDPI 10.3390/app112311339
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
Applied Sciences, Vol 11, Iss 11339, p 11339 (2021)
info:cnr-pdr/source/autori:D'Onofrio R.[1], Zaky A.S.[2,3], Frontalini F.[4], Luciani V.[1], Catanzariti R.[5], Francescangeli F.[6], Giorgioni M.[7], Coccioni R.[4], Özcan E.[8], Jovane L.[9]/titolo:Impact of the Middle Eocene Climatic Optimum (MECO) on Foraminiferal and Calcareous Nannofossil Assemblages in the Neo-Tethyan Baskil Section (Eastern Turkey): Paleoenvironmental and Paleoclimatic Reconstructions/doi:10.3390%2Fapp112311339/rivista:Applied sciences/anno:2021/pagina_da:1/pagina_a:25/intervallo_pagine:1–25/volume:11
Applied Sciences; Volume 11; Issue 23; Pages: 11339
D’Onofrio, Roberta; Zaky, Amr S.; Frontalini, Fabrizio; Luciani, Valeria; Catanzariti, Rita; Francescangeli, Fabio; Giorgioni, Martino; Coccioni, Rodolfo; Özcan, Ercan; Jovane, Luigi (2021). Impact of the Middle Eocene Climatic Optimum (MECO) on Foraminiferal and Calcareous Nannofossil Assemblages in the Neo-Tethyan Baskil Section (Eastern Turkey): Paleoenvironmental and Paleoclimatic Reconstructions. Applied Sciences, 11(23), p. 11339. MDPI 10.3390/app112311339
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
Applied Sciences, Vol 11, Iss 11339, p 11339 (2021)
The Middle Eocene Climatic Optimum (MECO; ~40 Ma), which interrupted for ~500–600 kyr the long-term cooling trend culminating at the Eocene/Oligocene boundary, still requires a comprehensive understanding of the biotic resilience. Here we present a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e4726550f77183ae19120d7e194183ce
http://www.cnr.it/prodotto/i/460709
http://www.cnr.it/prodotto/i/460709
Autor:
Barbero E.[1], Pandolfi L.[2, Delavari M.[4], Dolati A.[4], Saccani E.[1], Catanzariti R.[3], Luciani V.[1], Chiari M.[5], Marroni M.[2
Publikováno v:
Geoscience Frontiers, Vol 12, Iss 3, Pp 101106-(2021)
Geosciences Frontiers 12 (2021): 1–25. doi:10.1016/j.gsf.2020.12.001
info:cnr-pdr/source/autori:Barbero E.[1], Pandolfi L.[2,3], Delavari M.[4], Dolati A.[4], Saccani E.[1], Catanzariti R.[3], Luciani V.[1], Chiari M.[5], Marroni M.[2,3]/titolo:The western Durkan Complex (Makran Accretionary Prism, SE Iran): A Late Cretaceous tectonically disrupted seamounts chain and its role in controlling deformation style/doi:10.1016%2Fj.gsf.2020.12.001/rivista:Geosciences Frontiers/anno:2021/pagina_da:1/pagina_a:25/intervallo_pagine:1–25/volume:12
Geosciences Frontiers 12 (2021): 1–25. doi:10.1016/j.gsf.2020.12.001
info:cnr-pdr/source/autori:Barbero E.[1], Pandolfi L.[2,3], Delavari M.[4], Dolati A.[4], Saccani E.[1], Catanzariti R.[3], Luciani V.[1], Chiari M.[5], Marroni M.[2,3]/titolo:The western Durkan Complex (Makran Accretionary Prism, SE Iran): A Late Cretaceous tectonically disrupted seamounts chain and its role in controlling deformation style/doi:10.1016%2Fj.gsf.2020.12.001/rivista:Geosciences Frontiers/anno:2021/pagina_da:1/pagina_a:25/intervallo_pagine:1–25/volume:12
The Durkan Complex is a key tectonic element of the Makran accretionary prism (SE Iran) and it has been interpreted as representing a continental margin succession. We present here a multidisciplinary study of the western Durkan Complex, which is bas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ed0402df3079bdb32551b0bd7a827287
http://hdl.handle.net/11392/2431976
http://hdl.handle.net/11392/2431976
Autor:
Barbero, E., Delavari, M., Dolati, A., Pandolfi, L., Marroni, M., Saccani, E., Catanzariti, R., Chiari, M., Luciani, V., Di Rosa, M., Zaccarini, F.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3709::552e1ae9f6c040c19973e166450b6385
http://hdl.handle.net/11392/2478154
http://hdl.handle.net/11392/2478154