Southernmost indications of large freshwater discharges during the Heinrich Stadials (Galicia Interior Basin, Northwest Iberian Continental Margin)

The reconstruction of circum-Atlantic ice-sheet instabilities is of great importance to understanding the mechanisms that force abrupt climate changes. We have used enviromagnetic and geochemical data to explore these issues, providing a continuous and well-dated record of the evolution of glacial/i...

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Detalhes bibliográficos
Autor principal: Plaza Morlote, M. (author)
Outros Autores: Rey, D. (author), Santos, J. F. (author), Ribeiro, S. (author), Heslop, D. (author), Bernabeu, A. M. (author), Mohamed, K. J. (author), Rubio, B. (author), Martins, V. (author)
Formato: conferenceObject
Idioma:eng
Publicado em: 2017
Assuntos:
Galician Interior Basin
Last glacial period
Heinrich Stadials
EIS–LIS–AMOC dynamics
Texto completo:http://hdl.handle.net/10773/21149
País:Portugal
Oai:oai:ria.ua.pt:10773/21149

Texto Completo

http://hdl.handle.net/10773/21149

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