Southernmost evidence of large European Ice Sheet-derived freshwater discharges during the Heinrich Stadials of the Last Glacial Period (Galician Interior Basin, Northwest Iberian Continental Margin)

The reconstruction of circum-Atlantic ice-sheets motions and instabilities is crucial to shedding light on the potential mechanisms that triggered and/or enhanced abrupt climate changes. Using environmagnetic and geochemical data, we provide a continuous and well-dated record of the evolution of the...

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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. (author), Mohamed, K.J. (author), Rubio, B. (author), Martins, V. (author)
Formato: article
Idioma:eng
Publicado em: 1000
Assuntos:
Neodymium and Strontium Isotopes
Magnetic properties
Heinrich Stadials
Ice Rafted Detritus
Meltwater
Last Glacial Period
Texto completo:http://hdl.handle.net/10773/17422
País:Portugal
Oai:oai:ria.ua.pt:10773/17422

Texto Completo

http://hdl.handle.net/10773/17422

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