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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Bibliographic Details
Main Author: Oliveira, Dulce (author)
Other Authors: 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)
Format: article
Language:eng
Published: 2019
Subjects:
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
Online Access:http://hdl.handle.net/10400.1/13179
Country:Portugal
Oai:oai:sapientia.ualg.pt:10400.1/13179

Internet

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

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