Land surface temperature changes in Northern Iberia since 4000 yr BP, based on δ13C of speleothems
The surface temperature changes for the last 4000 years in northern inland Iberia (an area particularly sensitive to climate change) are determined by a high resolution study of carbon stable isotope records of stalagmites from three caves (Kaite, Cueva del Cobre, and Cueva Mayor) separated several...
Published in: | Global and Planetary Change |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier
2011
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Subjects: | |
Online Access: | https://eprints.ucm.es/id/eprint/20326/ https://eprints.ucm.es/id/eprint/20326/1/1-18111000191.pdf http://www.elsevier.com/wps/product/cws_home/503335/description https://doi.org/10.1016/j.gloplacha.2011.02.002 |