Unexpected weak seasonal climate in the western Mediterranean region during MIS 31, a high-insolation forced interglacial

Marine Isotope Stage 31 (MIS 31) is an important analogue for ongoing and projected global warming, yet key questions remain about the regional signature of its extreme orbital forcing and intra-interglacial variability. Based on a new direct land-sea comparison in SW Iberian margin IODP Site U1385...

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Detalhes bibliográficos
Autor principal: Oliveira, Dulce (author)
Outros Autores: Goni, Maria F. Sanchez (author), Naughton, Filipa (author), Polanco-Martinez, J. M. (author), Jiménez-Espejo, Francisco J. (author), Grimalt, Joan O. (author), Martrat, Belen (author), Voelker, Antje (author), Trigo, Ricardo (author), Hodell, David (author), Abrantes, Fatima (author), Desprat, Stephanie (author)
Formato: article
Idioma:eng
Publicado em: 2019
Assuntos:
Antarctic ice-sheet
North-Atlantic Ocean
Middle pleistocene transition
Millennial-scale changes
Isotope stage 31
Midpleistocene transition
Lake elgygytgyn
Equatorial insolation
Iberian Peninsula
Tropical Pacific
Texto completo:http://hdl.handle.net/10400.1/13179
País:Portugal
Oai:oai:sapientia.ualg.pt:10400.1/13179

Texto Completo

http://hdl.handle.net/10400.1/13179

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