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Hydrological changes during the Roman Climatic Optimum in northern Tuscany (Central Italy) as evidenced by speleothem records and archaeological data

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

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

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::846b48bf276b8219e9999d4a382ed4d9
https://doi.org/10.1002/jqs.3224

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Interstadial conditions over the Southern Alps during the early penultimate glacial (MIS 6): a multiproxy record from Rio Martino Cave (Italy)

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

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

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Mid-Holocene relative sea-level changes along Atlantic Patagonia: New data from Camarones, Chubut, Argentina

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

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

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New findings of the Campanian Ignimbrite ash within slope deposits of the Treska valley (former Yugoslav Republic of Macedonia)

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

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

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Last Interglacial Sea-level highstand deduced from notches and inner margins of marine terraces at Puerto Deseado, Santa Cruz Province, Argentina

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

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

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Abrasive notches along the Atlantic Patagonian coast and their potential use as sea level markers: the case of Puerto Deseado (Santa Cruz, Argentina)

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

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

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Middle- to late-Holocene relative sea-level changes at Puerto Deseado (Patagonia, Argentina)

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

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

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New insights on the Holocene marine transgression in the Bahía Camarones (Chubut, Argentina)

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

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

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Stratigraphy, petrography and chronology of speleothem deposition at Tana Che Urla (Lucca, Italy): paleoclimatic implications

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

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

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