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

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

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

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

Stratigraphic evidence for a ' pluvial phase ' between ca. 8200-7100 ka from Renella Cave (Central Italy)

Autor: I. Baneschi, Leonardo Piccini, Isabelle Couchoud, Ilaria Isola, John Hellstrom, Eleonora Regattieri, L.V. Zhornyak, G. Zanchetta, Russell N. Drysdale

Publikováno v: Quaternary Science Reviews
Quaternary Science Reviews, Elsevier, 2010, 30 (3-4), pp. 409-417. ⟨10.1016/j.quascirev.2010.12.003⟩
Quaternary science reviews 40 (2011): 409–417.
info:cnr-pdr/source/autori:Zhornyak, L.V. (1); Zanchetta, G. (1,2,3); Drysdale, R.N. (4); Hellstrom, J.C. (5); Isola, I. (2); Regattieri, E. (1) ;Piccini, L. (6); Baneschi, I. (3); Couchoud, I. (7)/titolo:Stratigraphic evidence for a "pluvial phase" between ca 8200-7100 ka from Renella cave (Central Italy)./doi:/rivista:Quaternary science reviews/anno:2011/pagina_da:409/pagina_a:417/intervallo_pagine:409–417/volume:40

International audience; A stratigraphic and chronological study of the upper level of Renella Cave (Apuan Alps, Central Italy) reveals that two episodes of flowstone accumulation bracket a thick clastic layer deposited between ca 8.2 and 7.1 ka. This

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c4efb6a8f8b60c04b32daecfd07c86d5
https://hal.archives-ouvertes.fr/halsde-00804678