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Laminated sediments in a core from Alberca de Tacámbaro, western central Mexico, provide a high‐resolution record of palaeoclimatic variability for most of the Holocene. Using compositional and textural characteristics we identified 14 facies classified in biogenic, clastic and volcaniclastic groups, in which diatoms and other algal remains are the most common components. In addition to facies analysis,...
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