Zobrazeno 1 - 2
of 2
pro vyhledávání: '"Nomade S.[4]"'
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
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
https://www.journals.elsevier.com/quaternary-science-reviews
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
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