Abstract
Two ancient cloud forests in the Mexican Pacific were reconstructed to reveal signals of past ecosystem responses to climate anomalies during the Late Holocene, Little Ice Age (~AD 1350–1850) and Medieval Climate Anomaly (~AD 800–1350). Applying palaeoecological techniques, two organic sediment cores were extracted from forest hollows: one from the cloud forest of the Acer Forest State Park (AFSP) and one from the Sierra de Manantlan Biosphere Reserve (SMBR), both in the state of Jalisco, Mexico.
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