| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6350555 | Palaeogeography, Palaeoclimatology, Palaeoecology | 2012 | 12 Pages |
Abstract
⺠We reconstructed climate in the Valsequillo Basin between c. 40,000 and 8000 BP. ⺠Oxygen and carbon isotopes of shells were used as palaeoclimate proxies. ⺠Around 35,000 BP climate was similar to the present day. ⺠Between 35,000 and 20,000 BP conditions became drier. ⺠Post 20,000 BP conditions became increasingly humid again.
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Earth and Planetary Sciences
Earth-Surface Processes
Authors
Rhiannon E. Stevens, Sarah E. Metcalfe, Melanie J. Leng, Angela L. Lamb, Hilary J. Sloane, Edna Naranjo, Silvia González,