A new detailed pollen record of the penultimate glacial–interglacial–glacial cycle
corresponding to the late marine isotopic stages (MISs) 6–3 (146–35 ka ago) has been …

Thirty waterbodies on the Transmexican Volcanic Belt were studied using standardized de
México, México. methods, covering an altitudinal gradient from 737 to 4283 masl and …

The Zacapu lacustrine basin is located in the north-central part of the Michoacán-
Guanajuato volcanic field (MGVF), which constitutes the west-central segment of the Trans …

Central Mexico exhibits a complex environment with wide topographic, climatic, and
biological gradients. Lacustrine basins distributed along the region have been the source for …

Abstract A 27.15-m-long core from Lake Chapala, west-central Mexico (1520 masl)
possesses a continuous 15,000-year record of sediment accumulation with abundant …

Charcoal particles vary in size and form, but they can preserve morphological characteristics
used to infer the type of vegetation being burnt. To deduce potential fuel and fire type, we …

Seasonal dry tropical forest (STDF) is a widespread vegetation type in western Mexico.
Generally, this type of forest develops in semihumid habitats where lacustrine basins are …

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 …

Abstract The Alberca de Tacámbaro (AT) is located at a transitional zone between tropical
and temperate climates at the core of the North American Monsoon area. This location …

Sediments deposited in the Etzatlán-Magdalena Basin were analyzed to reconstruct the
paleohydrological variations and generate a new Holocene paleoclimate record for the less …