Zobrazeno 1 - 10 of 11 pro vyhledávání: '"Regattieri E. [1]"'
1
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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2
Holocene Critical Zone dynamics in an Alpine catchment inferred from a speleothem multiproxy record. Disentangling climate and human influences
Autor: Regattieri E.[1, Zanchetta G.[1, Isola I.[3], Zanella E.[4], Drysdale R.N.[5, Hellstrom J.C.[7], Zerboni A.[8], Dallai L.[2], Tema E.[4], Lanci L.[9], Costa E.[4], Magri F[10]
Publikováno v: Scientific reports (Nature Publishing Group) 9 (2019). doi:10.1038/s41598-019-53583-7
info:cnr-pdr/source/autori:Regattieri E.[1,2], Zanchetta G.[1,3], Isola I.[3], Zanella E.[4], Drysdale R.N.[5,6], Hellstrom J.C.[7], Zerboni A.[8], Dallai L.[2], Tema E.[4], Lanci L.[9], Costa E.[4], Magri F[10]/titolo:Holocene Critical Zone dynamics in an Alpine catchment inferred from a speleothem multiproxy record: disentangling climate and human influences/doi:10.1038%2Fs41598-019-53583-7/rivista:Scientific reports (Nature Publishing Group)/anno:2019/pagina_da:/pagina_a:/intervallo_pagine:/volume:9
Scientific Reports, Vol 9, Iss 1, Pp 1-9 (2019)
Scientific Reports
Disentangling the effects of climate and human impact on the long-term evolution of the Earth Critical Zone is crucial to understand the array of its potential responses to the ongoing Global Change. This task requires natural archives from which loc
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::582c9a6a14524d4402cdd4a406477f09
http://hdl.handle.net/11573/1456176
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3
Frequency and dynamics of millenial-scale variability during Marine Isotope Stage 19: Insights from the Sulmona basin (central Italy)
Autor: Regattieri E.[1, Giaccio B.[3], Mannella G.[1], Zanchetta G.[1], Nomade S.[4], Tognarelli A.[1], Perchiazzi N.[1], Vogel H.[5], Boschi C.[2], Drysdale R.[6, Wagner B.[8+, Gemelli M.[1], Tzedakis P. [9]
Publikováno v: Quaternary science reviews 214 (2019): 28–43.
info:cnr-pdr/source/autori:Regattieri E.[1,2], Giaccio B.[3], Mannella G.[1], Zanchetta G.[1], Nomade S.[4], Tognarelli A.[1], Perchiazzi N.[1], Vogel H.[5], Boschi C.[2], Drysdale R.[6,7], Wagner B.[8+, Gemelli M.[1], Tzedakis P. [9]/titolo:Frequency and dynamics of millenial-scale variability during Marine Isotope Stage 19: Insights from the Sulmona basin (central Italy)./doi:/rivista:Quaternary science reviews/anno:2019/pagina_da:28/pagina_a:43/intervallo_pagine:28–43/volume:214
Among past interglacial periods, Marine Isotope Stage (MIS) 19 is particularly interesting because its orbital geometry is very similar to that of the present interglacial. Here we present a high-resolution (sub-centennial) multiproxy record covering
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::7526f879125e8ff3b98ad33ab6527b38
https://www.journals.elsevier.com/quaternary-science-reviews
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4
Stable isotope composition of fossil ahermatypic coral Cladocora caespitosa (L.) from Pleistocene raised marine terraces of the Livorno area (Central Italy)
Autor: Zanchetta G.[1], Bini M.[1, Montagna P.[3], Regattieri E.[1, Ragaini L.[1], Da Prato S.[4], Ciampalini A.[5], Dallai L.[4], Leone G.[1]
Publikováno v: Alpine and Mediterranean Quaternary 32 (2019): 73–86. doi:10.26382/AMQ.2019.12
info:cnr-pdr/source/autori:Zanchetta G.[1], Bini M.[1,2], Montagna P.[3], Regattieri E.[1,4], Ragaini L.[1], Da Prato S.[4], Ciampalini A.[5], Dallai L.[4], Leone G.[1]/titolo:Stable isotope composition of fossil ahermatypic coral Cladocora caespitosa (L.) from Pleistocene raised marine terraces of the Livorno area (Central Italy)/doi:10.26382%2FAMQ.2019.12/rivista:Alpine and Mediterranean Quaternary/anno:2019/pagina_da:73/pagina_a:86/intervallo_pagine:73–86/volume:32
The Livorno coastal area (coastal Tuscany) preserves evidences of several raised marine terraces. Stratigraphically they have been correlated with MIS 5e, 9c and MIS 11 sea-level high stands. However, no direct dating have been performed so far. Than
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::9f9b07e6322f81b636f74fe54de30592
http://www.cnr.it/prodotto/i/456664
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5
Middle Holocene climate variability from a stalagmite from Alilica Cave (Southern Balkans)
Autor: Regattieri E.[1, Isola I.[3], Zanchetta G.[1, Tognarelli A.[1], Hellstrom J.C.[4], Drysdale R.N.[5, Boschi C.[2], Milevski I.[7], Temovski M.[8]
Publikováno v: Alpine and Mediterranean Quaternary
32 (2019): 15–30. doi:10.26382/AMQ.2019.02
info:cnr-pdr/source/autori:Regattieri E.[1,2], Isola I.[3], Zanchetta G.[1,3], Tognarelli A.[1], Hellstrom J.C.[4], Drysdale R.N.[5,6], Boschi C.[2], Milevski I.[7], Temovski M.[8]/titolo:Middle Holocene climate variability from a stalagmite from Alilica Cave (Southern Balkans)/doi:10.26382%2FAMQ.2019.02/rivista:Alpine and Mediterranean Quaternary (Print)/anno:2019/pagina_da:15/pagina_a:30/intervallo_pagine:15–30/volume:32
We present a stable isotope (delta 13C and delta18O) and growth rate record from a southern Balkans stalagmite, LID1, deposited between ca. 8.4 and 4.1 ka. Both stable isotope time series show significant changes at the centennial-millennial time sca
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::a96b47d0e60e816a041617afdee54b84
https://publications.cnr.it/doc/456017
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6
Mineralogy and oxygen isotope profile of Pelecyora gigas (Veneridae, Bivalvia) from Tuscan Pliocene
Autor: Ragaini L.[1], Ficini F.[1], Zanchetta G.[1], Regattieri E.[1, Perchiazzi N.[1], Dallai L.[2]
Publikováno v: Alpine and Mediterranean Quaternary 32 (2019): 5–14. doi:10.26382/AMQ.2019.01
info:cnr-pdr/source/autori:Ragaini L.[1], Ficini F.[1], Zanchetta G.[1], Regattieri E.[1,2], Perchiazzi N.[1], Dallai L.[2]/titolo:Mineralogy and oxygen isotope profile of Pelecyora gigas (Veneridae, Bivalvia) from Tuscan Pliocene/doi:10.26382%2FAMQ.2019.01/rivista:Alpine and Mediterranean Quaternary/anno:2019/pagina_da:5/pagina_a:14/intervallo_pagine:5–14/volume:32
A specimen with joined valves of Pelecyora gigas, an extinct species, was collected in a sandy layer of Early Pliocene age in the northern part of the Siena Basin (Tuscany, Italy). XRD data demonstrated that the original mineralogical composition of
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::82bf1fb4397ebea2b0bfc351df2d4f75
https://publications.cnr.it/doc/456016
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7
New insights on ancient cetacean movement patterns from oxygen-isotope analyses of a Mediterranean Pleistocene whale barnacle
Autor: Collareta A.[1], Regattieri E.[1, Zanchetta G.[1, Lambert O.[4], Catanzariti R.[2], Bosselaers M.[4], Covelo P.[5], Varola A.[1], Bianucci G.[1]
Publikováno v: Neues Jahrbuch für Geologie und Paläontologie. Abhandlungen 288 (2018): 143–159. doi:10.1127/njgpa/2018/0729
info:cnr-pdr/source/autori:Collareta A.[1], Regattieri E.[1,2], Zanchetta G.[1,3], Lambert O.[4], Catanzariti R.[2], Bosselaers M.[4], Covelo P.[5], Varola A.[1], Bianucci G.[1]/titolo:New insights on ancient cetacean movement patterns from oxygen-isotope analyses of a Mediterranean Pleistocene whale barnacle/doi:10.1127%2Fnjgpa%2F2018%2F0729/rivista:Neues Jahrbuch für Geologie und Paläontologie. Abhandlungen/anno:2018/pagina_da:143/pagina_a:159/intervallo_pagine:143–159/volume:288
The fossil record of whale barnacles (Coronulidae) mostly consists of remains of Coronula in Plio-Pleistocene coastal deposits that have been interpreted as ancient mysticete breeding/calving areas. Based on such indirect evidence, it has been propos
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::400012bde239250dd975184eb7fde318
http://hdl.handle.net/11568/940748
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8
A MIS 9/MIS 8 speleothem record of hydrological variability from Macedonia (F.Y.R.O.M.)
Autor: Regattieri E.[1, 2, Zanchetta G.[1, Isola I.[4], Bajo P.[5], Perchiazzi N.[1], Drysdale R.N.[5, Boschi C.[3], Hellstrom J.C.[7], Francke A.[2, Wagner B. [2]
Publikováno v: Global and planetary change
162 (2018): 39–52. doi:10.1016/j.gloplacha.2018.01.003
info:cnr-pdr/source/autori:Regattieri E.[1,2,3], Zanchetta G.[1,4], Isola I.[4], Bajo P.[5], Perchiazzi N.[1], Drysdale R.N.[5,6], Boschi C.[3], Hellstrom J.C.[7], Francke A.[2,7], Wagner B. [2]/titolo:A MIS 9%2FMIS 8 speleothem record of hydrological variability from Macedonia (F.Y.R.O.M.)/doi:10.1016%2Fj.gloplacha.2018.01.003/rivista:Global and planetary change (Print)/anno:2018/pagina_da:39/pagina_a:52/intervallo_pagine:39–52/volume:162
Global and Planetary Change
Global and Planetary Change, Elsevier, 2018, 162, pp. 39-52
International audience; The period corresponding to Marine Isotope Stages 9 (MIS 9) offers the opportunity to study orbital and suborbital scale climate variability under boundary conditions different from those of better studied intervals such as th
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2b60d8632be8d281c8e53c76a4f7a422
https://hal.science/hal-02007608
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9
Duration and dynamics of the best orbital analogue to the present interglacial
Autor: Giaccio B.[1], Regattieri E.[1, 2, Zanchetta G.[1, Nomade S.[4], Renne P.R.[5, Sprain C.J.[5, Drysdale R.N.[7, Tzedakis P.C.[9], Messina P.[1], Scardia G.[1, 10], Sposato A.[1], Bassinot F.[4]
Publikováno v: Geology
Geology, 2015, 43 (7), pp.603-606. ⟨10.1130/G36677.1⟩
Geology, Geological Society of America, 2015, 43 (7), pp.603-606. ⟨10.1130/G36677.1⟩
Geology, vol 43, iss 7
Geology (Boulder Colo.) 43 (2015): 603–606. doi:10.1130/G36677.1
info:cnr-pdr/source/autori:Giaccio B.[1], Regattieri E.[1,2,3], Zanchetta G.[1,2,3], Nomade S.[4], Renne P.R.[5,6], Sprain C.J.[5,6], Drysdale R.N.[7,8], Tzedakis P.C.[9], Messina P.[1], Scardia G.[1,10], Sposato A.[1], Bassinot F.[4]/titolo:Duration and dynamics of the best orbital analogue to the present interglacial/doi:10.1130%2FG36677.1/rivista:Geology (Boulder Colo.)/anno:2015/pagina_da:603/pagina_a:606/intervallo_pagine:603–606/volume:43
Past orbital analogues to the current interglacial, such as Marine Isotope Stage 19c (MIS 19c, ca. 800 ka), can provide reliable reference intervals for evaluating the timing and the duration of the Holocene and factors inherent in its climatic progr
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::02fc8c1f8aa8ef7e9dd21490f5637b40
https://doi.org/10.1130/g36677.1
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10
Environmental variability between the penultimate deglaciation and the mid Eemian: Insights from Tana che Urla (central Italy) speleothem trace element record
Autor: Regattieri E.[1, Zanchetta G.[2, 3, 4] Drysdale R.N.[5, Isola I.[4], Woodhead J.D.[7], Hellstrom J.C.[7], Giaccio B.[1], Greig A.[7], Baneschi I.[3], Dotsika E. [8]
Publikováno v: Quaternary Science Reviews
Quaternary Science Reviews, Elsevier, 2016, 152, pp.80-92
Quaternary science reviews 152 (2016): 80–92. doi:10.1016/j.quascirev.2016.09.027
info:cnr-pdr/source/autori:Regattieri E.[1,3], Zanchetta G.[2,3,4] Drysdale R.N.[5,6], Isola I.[4], Woodhead J.D.[7], Hellstrom J.C.[7], Giaccio B.[1], Greig A.[7], Baneschi I.[3], Dotsika E. [8]/titolo:Environmental variability between the penultimate deglaciation and the mid Eemian: Insights from Tana che Urla (central Italy) speleothem trace element record/doi:10.1016%2Fj.quascirev.2016.09.027/rivista:Quaternary science reviews/anno:2016/pagina_da:80/pagina_a:92/intervallo_pagine:80–92/volume:152
International audience; A trace element record (Mg, Sr, Ba, Al, Si, P, Y, Zn) covering the ca. 133 ka to ca. 124 ka time interval was acquired from a flowstone core from Tana che Urla Cave (central Italy). It was compared with stable isotope data to
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6a6f6b6e59a13e714f40e963d590b725
https://hal.archives-ouvertes.fr/hal-02009232
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