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Palynological analyses of fluvio-glacial sediments from Mesa del Caballo (3500 m a.s.l.), in the Venezuelan Andes, allowed reconstruction of palaeoenvironments of high altitudes close to the Last Glacial Maximum. A stadial, called El Caballo, is reported at 16.5 ka B.P. The estimated average temperature was around 7°C lower than today, and coincides with the Colombian Fuquene stadial and the global...
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