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Late Quaternary glacial stades in the Cordillera Central, Colombia, based on glacial geomorphology, tephra--soil stratigraphy, palynology, and radiocarbon dating
Using data from glacial geomorphology, tephra–soil stratigraphy and mineralogy, palynology, and radiocarbon dating, a sequence of glacial and bioclimatic stades and interstades has been identified for the last ca. 50000 yr in the Ruiz‐Tolima massif, Cordillera Central, Colombia. Six Pleistocene cold stades separated by warmer interstades occurred: before 48000, between 48000 and 33000, between 28000 and 21000, from≥ 16000 to ca. 14000, ca. 13000–12400, and ca. 11000–10000 yr BP. Although these radiocarbon ages
Tópico:
Geological and Tectonic Studies in Latin America
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38
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FuenteJournal of Quaternary Science: Published for the Quaternary Research Association