Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Isola I. [2]"'
Autor:
Bini M.[1, 2, Zanchetta G.[1, Regattieri E.[4, Isola I.[2, Drysdale R.N.[5, Fabiani F.[7], Genovesi S.[7], Hellstrom J.C.[8]
Publikováno v:
JQS. Journal of quaternary science 35 (2020): 791–802. doi:10.1002/jqs.3224
info:cnr-pdr/source/autori:Bini M.[1,2,3], Zanchetta G.[1,3], Regattieri E.[4,2], Isola I.[2,4], Drysdale R.N.[5,6], Fabiani F.[7], Genovesi S.[7], Hellstrom J.C.[8]/titolo:Hydrological changes during the Roman Climatic Optimum in northern Tuscany (Central Italy) as evidenced by speleothem records and archaeological data/doi:10.1002%2Fjqs.3224/rivista:JQS. Journal of quaternary science/anno:2020/pagina_da:791/pagina_a:802/intervallo_pagine:791–802/volume:35
info:cnr-pdr/source/autori:Bini M.[1,2,3], Zanchetta G.[1,3], Regattieri E.[4,2], Isola I.[2,4], Drysdale R.N.[5,6], Fabiani F.[7], Genovesi S.[7], Hellstrom J.C.[8]/titolo:Hydrological changes during the Roman Climatic Optimum in northern Tuscany (Central Italy) as evidenced by speleothem records and archaeological data/doi:10.1002%2Fjqs.3224/rivista:JQS. Journal of quaternary science/anno:2020/pagina_da:791/pagina_a:802/intervallo_pagine:791–802/volume:35
Study of the climate in the Mediterranean basin during different historical periods has taken on a particular importance, particularly regarding its role (together with other factors) in the evolution of human settlement patterns. Although the Roman
Autor:
Regattieri E.[1, Querci S.[3], Zanchetta G.[3, 4, Zanella E.[6], Isola I.[2, Drysdale R.N. [7], Hellstrom J.C.[8], Magrì F.[9]
Publikováno v:
Quaternary science reviews 257 (2021). doi:10.1016/j.quascirev.2021.106856
info:cnr-pdr/source/autori:Regattieri E.[1,2], Querci S.[3], Zanchetta G.[3,4,5], Zanella E.[6], Isola I.[2,1], Drysdale R.N. [7], Hellstrom J.C.[8], Magrì F.[9]/titolo:Interstadial conditions over the Southern Alps during the early penultimate glacial (MIS 6): a multiproxy record from Rio Martino Cave (Italy)/doi:10.1016%2Fj.quascirev.2021.106856/rivista:Quaternary science reviews/anno:2021/pagina_da:/pagina_a:/intervallo_pagine:/volume:257
info:cnr-pdr/source/autori:Regattieri E.[1,2], Querci S.[3], Zanchetta G.[3,4,5], Zanella E.[6], Isola I.[2,1], Drysdale R.N. [7], Hellstrom J.C.[8], Magrì F.[9]/titolo:Interstadial conditions over the Southern Alps during the early penultimate glacial (MIS 6): a multiproxy record from Rio Martino Cave (Italy)/doi:10.1016%2Fj.quascirev.2021.106856/rivista:Quaternary science reviews/anno:2021/pagina_da:/pagina_a:/intervallo_pagine:/volume:257
Identifying the hydrological and environmental response of the European Alpine region to different combinations of climate boundary conditions is crucial to advance the reliability of predictive climate models and thus shape climate adaptation polici
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7363c2c66c8a0a213d6a5e519e16d1ad
Autor:
Bini M.[1, Isola I.[2, 3] Zanchetta G.[1, 2] Pappalardo M.[1], Ribolini A.[1], Ragaini L.[1], Baroni C.[1, Boretto G.[4], Fuck E.[5], Morigi C.[1], Salvatore M.C.[1, Bassi D.[6] Marzaioli F.[7], Terrasi F. [7]
Publikováno v:
SEDICI (UNLP)
Universidad Nacional de La Plata
instacron:UNLP
Holocene (Lond. Online) 28 (2018): 56–64. doi:10.1177/0959683617714596
info:cnr-pdr/source/autori:Bini M.[1,2], Isola I.[2,3] Zanchetta G.[1,2] Pappalardo M.[1], Ribolini A.[1], Ragaini L.[1], Baroni C.[1,3], Boretto G.[4], Fuck E.[5], Morigi C.[1], Salvatore M.C.[1,3], Bassi D.[6] Marzaioli F.[7], Terrasi F. [7]/titolo:Mid-Holocene relative sea-level changes along Atlantic Patagonia: New data from Camarones, Chubut, Argentina/doi:10.1177%2F0959683617714596/rivista:Holocene (Lond. Online)/anno:2018/pagina_da:56/pagina_a:64/intervallo_pagine:56–64/volume:28
Universidad Nacional de La Plata
instacron:UNLP
Holocene (Lond. Online) 28 (2018): 56–64. doi:10.1177/0959683617714596
info:cnr-pdr/source/autori:Bini M.[1,2], Isola I.[2,3] Zanchetta G.[1,2] Pappalardo M.[1], Ribolini A.[1], Ragaini L.[1], Baroni C.[1,3], Boretto G.[4], Fuck E.[5], Morigi C.[1], Salvatore M.C.[1,3], Bassi D.[6] Marzaioli F.[7], Terrasi F. [7]/titolo:Mid-Holocene relative sea-level changes along Atlantic Patagonia: New data from Camarones, Chubut, Argentina/doi:10.1177%2F0959683617714596/rivista:Holocene (Lond. Online)/anno:2018/pagina_da:56/pagina_a:64/intervallo_pagine:56–64/volume:28
This paper concerns the relative sea-level changes associated with the Atlantic Patagonian coast derived from sea-level index points whose elevation was determined by a differential global position system (DGPS). Bio encrustations from outcrops locat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2082dd8589942efb90b8094c84bdc18a
http://hdl.handle.net/11392/2381984
http://hdl.handle.net/11392/2381984
Autor:
Zanchetta G.[1, 2, Bini M.[1], Isola I.[2], Regattieri E.[4, Ribolini A.[1], Milevski I.[6], Sulpizio R.[7
Publikováno v:
Italian Journal of Geosciences (Testo stamp.) 136 (2017): 198–205. doi:10.3301/IJG.2016.16
info:cnr-pdr/source/autori:Zanchetta G.[1,2,3], Bini M.[1], Isola I.[2], Regattieri E.[4,5], Ribolini A.[1], Milevski I.[6], Sulpizio R.[7,8]/titolo:New findings of the Campanian Ignimbrite ash within slope deposits of the Treska valley (former Yugoslav Republic of Macedonia)/doi:10.3301%2FIJG.2016.16/rivista:Italian Journal of Geosciences (Testo stamp.)/anno:2017/pagina_da:198/pagina_a:205/intervallo_pagine:198–205/volume:136
info:cnr-pdr/source/autori:Zanchetta G.[1,2,3], Bini M.[1], Isola I.[2], Regattieri E.[4,5], Ribolini A.[1], Milevski I.[6], Sulpizio R.[7,8]/titolo:New findings of the Campanian Ignimbrite ash within slope deposits of the Treska valley (former Yugoslav Republic of Macedonia)/doi:10.3301%2FIJG.2016.16/rivista:Italian Journal of Geosciences (Testo stamp.)/anno:2017/pagina_da:198/pagina_a:205/intervallo_pagine:198–205/volume:136
In this paper, we describe the first finding of the campanian Ignimbrite tephra layer in a subaerial succession in the Former Yugoslav republic of Macedonia. the tephra is interbedded within slope deposits mixed with colluvial loess. the identificati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::1eb1665ce1f9a9c03a2b0bcbff50b44d
http://www.cnr.it/prodotto/i/372964
http://www.cnr.it/prodotto/i/372964
Autor:
Bini M.[1, 2] Zanchetta G.[1, 2] Ribolini A.[1], Salvatore M.C.[1, 3] Baroni C.[1, Pappalardo M.[1], Isola I.[2], Isla F.I.[4] Fucks E.[5], Boretto G.[6] Morigi C.[1, Ragaini L.[1], Marzaioli F.[8], Passariello I.[8]
Publikováno v:
Geografia fisica e dinamica quaternaria (Testo stamp.) 40 (2017): 29–39. doi:10.4461/GFDQ2017.40.3
info:cnr-pdr/source/autori:Bini M.[1,2] Zanchetta G.[1,2] Ribolini A.[1], Salvatore M.C.[1,3] Baroni C.[1,3], Pappalardo M.[1], Isola I.[2], Isla F.I.[4] Fucks E.[5], Boretto G.[6] Morigi C.[1,7], Ragaini L.[1], Marzaioli F.[8], Passariello I.[8]/titolo:Last Interglacial Sea-level highstand deduced from notches and inner margins of marine terraces at Puerto Deseado, Santa Cruz Province, Argentina/doi:10.4461%2FGFDQ2017.40.3/rivista:Geografia fisica e dinamica quaternaria (Testo stamp.)/anno:2017/pagina_da:29/pagina_a:39/intervallo_pagine:29–39/volume:40
info:cnr-pdr/source/autori:Bini M.[1,2] Zanchetta G.[1,2] Ribolini A.[1], Salvatore M.C.[1,3] Baroni C.[1,3], Pappalardo M.[1], Isola I.[2], Isla F.I.[4] Fucks E.[5], Boretto G.[6] Morigi C.[1,7], Ragaini L.[1], Marzaioli F.[8], Passariello I.[8]/titolo:Last Interglacial Sea-level highstand deduced from notches and inner margins of marine terraces at Puerto Deseado, Santa Cruz Province, Argentina/doi:10.4461%2FGFDQ2017.40.3/rivista:Geografia fisica e dinamica quaternaria (Testo stamp.)/anno:2017/pagina_da:29/pagina_a:39/intervallo_pagine:29–39/volume:40
A detailed geomorphological survey was undertaken in the area of Puerto Deseado (Santa Cruz Province, Argentina) to reconstruct the Relative Sea-level (RSL) position during the Last Interglacial highstand. The presence of active and well-preserved ab
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::6a6a6150444174a5c3403e7fac9d25fd
Autor:
Bini M.[1], Isola I.[2], Pappalardo M.[1], Ribolini A.[1] Favalli M.[2] Ragaini L.[1] Zanchetta G. [1, 2
Publikováno v:
Earth surface processes and landforms
39 (2014): 1550–1558. doi:10.1002/esp.3612
info:cnr-pdr/source/autori:Bini M.[1], Isola I.[2], Pappalardo M.[1], Ribolini A.[1] Favalli M.[2] Ragaini L.[1] Zanchetta G. [1,2,3]/titolo:Abrasive notches along the Atlantic Patagonian coast and their potential use as sea level markers: the case of Puerto Deseado (Santa Cruz, Argentina)./doi:10.1002%2Fesp.3612/rivista:Earth surface processes and landforms (Print)/anno:2014/pagina_da:1550/pagina_a:1558/intervallo_pagine:1550–1558/volume:39
39 (2014): 1550–1558. doi:10.1002/esp.3612
info:cnr-pdr/source/autori:Bini M.[1], Isola I.[2], Pappalardo M.[1], Ribolini A.[1] Favalli M.[2] Ragaini L.[1] Zanchetta G. [1,2,3]/titolo:Abrasive notches along the Atlantic Patagonian coast and their potential use as sea level markers: the case of Puerto Deseado (Santa Cruz, Argentina)./doi:10.1002%2Fesp.3612/rivista:Earth surface processes and landforms (Print)/anno:2014/pagina_da:1550/pagina_a:1558/intervallo_pagine:1550–1558/volume:39
Patagonia Argentina is a key area for the study of sea level changes in the southern hemisphere, but the availability of reliable sea level markers in this area is still problematic. In fact the storm deposits (beach ridge) commonly used here to reco
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::6f2e93b03fec33fcaeae9f37227da1e9
Autor:
Zanchetta G.[1, 2, Bini M.[1], Isola I.[2], Pappalardo M.[1], Ribolini A.[1], Consoloni I.[1], Boretto G.[4], Fucks E.[1], Ragaini L.[1], Terrasi F. [6]
Publikováno v:
Holocene (Sevenoaks) 24 (2014): 307–317. doi:10.1177/0959683613518589
info:cnr-pdr/source/autori:Zanchetta G.[1,2,3], Bini M.[1], Isola I.[2], Pappalardo M.[1], Ribolini A.[1], Consoloni I.[1], Boretto G.[4], Fucks E.[1], Ragaini L.[1], Terrasi F. [6]/titolo:Middle-to late-Holocene relative sea-level changes at Puerto Deseado (Patagonia, Argentina)./doi:10.1177%2F0959683613518589/rivista:Holocene (Sevenoaks)/anno:2014/pagina_da:307/pagina_a:317/intervallo_pagine:307–317/volume:24
CIC Digital (CICBA)
Comisión de Investigaciones Científicas de la Provincia de Buenos Aires
instacron:CICBA
info:cnr-pdr/source/autori:Zanchetta G.[1,2,3], Bini M.[1], Isola I.[2], Pappalardo M.[1], Ribolini A.[1], Consoloni I.[1], Boretto G.[4], Fucks E.[1], Ragaini L.[1], Terrasi F. [6]/titolo:Middle-to late-Holocene relative sea-level changes at Puerto Deseado (Patagonia, Argentina)./doi:10.1177%2F0959683613518589/rivista:Holocene (Sevenoaks)/anno:2014/pagina_da:307/pagina_a:317/intervallo_pagine:307–317/volume:24
CIC Digital (CICBA)
Comisión de Investigaciones Científicas de la Provincia de Buenos Aires
instacron:CICBA
Stratigraphic, morphologic and radiocarbon data from Puerto Deseado coastal area (Santa Cruz Province, Argentina) indicate that the Holocene coastline formed in response to the discontinuous aggradation of coarse gravely beaches since c. 6300 cal. yr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e107a4979d5528711af72fcad35a459b
Autor:
Zanchetta G. [1, 2, 5], Consoloni I. [1], Isola I. [2], Pappalardo M. [1], Ribolini A. [1], Aguirre M. [3, 4], Fucks E. [4], Baneschi I. [5], Bini M. [1], Ragaini L.[1], Terrasi F. [6], Boretto G. [7]
Publikováno v:
CIC Digital (CICBA)
Comisión de Investigaciones Científicas de la Provincia de Buenos Aires
instacron:CICBA
Italian Journal of Geosciences (Online) 131 (2012): 19–31.
info:cnr-pdr/source/autori:Zanchetta G. [1, 2, 5]; Consoloni I. [1]; Isola I. [2]; Pappalardo M. [1]; Ribolini A. [1]; Aguirre M. [3, 4]; Fucks E. [4]; Baneschi I. [5]; Bini M. [1]; Ragaini L.[1]; Terrasi F. [6]; Boretto G. [7]/titolo:New insights on the Holocene marine transgression in the Bahia Camarones (Chubut, Argentina)./doi:/rivista:Italian Journal of Geosciences (Online)/anno:2012/pagina_da:19/pagina_a:31/intervallo_pagine:19–31/volume:131
Comisión de Investigaciones Científicas de la Provincia de Buenos Aires
instacron:CICBA
Italian Journal of Geosciences (Online) 131 (2012): 19–31.
info:cnr-pdr/source/autori:Zanchetta G. [1, 2, 5]; Consoloni I. [1]; Isola I. [2]; Pappalardo M. [1]; Ribolini A. [1]; Aguirre M. [3, 4]; Fucks E. [4]; Baneschi I. [5]; Bini M. [1]; Ragaini L.[1]; Terrasi F. [6]; Boretto G. [7]/titolo:New insights on the Holocene marine transgression in the Bahia Camarones (Chubut, Argentina)./doi:/rivista:Italian Journal of Geosciences (Online)/anno:2012/pagina_da:19/pagina_a:31/intervallo_pagine:19–31/volume:131
The stratigraphic reconstruction of the northern sector of the Bahía Camarones (Chubut, Argentina) allowed to improve our understanding of the Holocene marine transgression in the area. The first phase of the maximum of the transgression, is interpr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::795723a73643c1944d1a76e8fc83458d
http://hdl.handle.net/11591/188182
http://hdl.handle.net/11591/188182
Autor:
Regattieri E. [1], Isola I. [2], Zanchetta G. [1,2,5], Drysdale R. [3], Hellstrom J. [4], Baneschi I. [5]
Publikováno v:
Geografia fisica e dinamica quaternaria (Testo stamp.) 35 (2012): 141–152.
info:cnr-pdr/source/autori:Regattieri E. [1]; Isola I. [2]; Zanchetta G. [1,2,5]; Drysdale R. [3]; Hellstrom J. [4]; Baneschi I. [5]/titolo:Stratigraphy, petrography and chronology of speleothem deposition at Tana Che Urla (Lucca, Italy): paleoclimatic implications/doi:/rivista:Geografia fisica e dinamica quaternaria (Testo stamp.)/anno:2012/pagina_da:141/pagina_a:152/intervallo_pagine:141–152/volume:35
info:cnr-pdr/source/autori:Regattieri E. [1]; Isola I. [2]; Zanchetta G. [1,2,5]; Drysdale R. [3]; Hellstrom J. [4]; Baneschi I. [5]/titolo:Stratigraphy, petrography and chronology of speleothem deposition at Tana Che Urla (Lucca, Italy): paleoclimatic implications/doi:/rivista:Geografia fisica e dinamica quaternaria (Testo stamp.)/anno:2012/pagina_da:141/pagina_a:152/intervallo_pagine:141–152/volume:35
n this work we present the results of a stratigraphic and lithologic study of a flowstone from Tana che Urla Cave, Apuan Alps (central Italy) which grew intermittently between ca. 160 and 8 ka. The studied succession consists of an alternation of two
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::bc6bc124828fc392f162605981291213
https://publications.cnr.it/doc/208549
https://publications.cnr.it/doc/208549