Stable isotope signature of the Middle Holocene climatic change in the SW Iberia

Between 7.5 kyr and 4 kyr a fluvial limestone tuffs system developed in the south-western corner of Iberia. This system is characterised by a segmented up to 60 meters thick limestone sequence dated by radiocarbon. The system is calcite dominated, and the other coeval mineral constituents comprise i...

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Bibliographic Details
Main Author: Ribeiro, Carlos (author)
Other Authors: Terrinha, Pedro (author), Candeias, António (author), Voelker, Antje (author)
Format: lecture
Language:por
Published: 2012
Subjects:
Stable isotopes
Climate change
SW Iberia
Holocene
Online Access:http://hdl.handle.net/10174/6724
Country:Portugal
Oai:oai:dspace.uevora.pt:10174/6724

Internet

http://hdl.handle.net/10174/6724

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