dc.description.abstract | This doctoral thesis presents the results of the pioneering archaeological
investigation conducted in the Northern Mexican Highlands with the aim to
evaluate the existing indicators of the earliest human occupations at the end of
the Pleistocene and discover new evidence of ancient cultural manifestations
through a systematic exploration of an endorheic basic in the Zacatecas desert,
a region never studied before. An exhaustive survey and analysis of the
available literature on Mexican prehistory establishes the weak points of the
local paradigms, differentiating between academic myths and objective realities.
A complete historiography of the topic of the earliest humans in Mexico has
been achieved, for the first time. The study of several collections of flaked stone
artefacts, in different cities in Mexico, show new indicators of the presence of
bearers of the Late Paleoamerican cultures, in regions where their presence
had been weakly confirmed. The most important part of the research consisted
in fieldwork realised during two long seasons; the first one dedicated to the
surface explorations and the second one to excavations. Thirty-five new
archaeological sites were discovered in the first phase, most of them open
campsites reminiscent of hunter-gatherer societies, with a richness of stone
artefacts on their surface. They indicate a long cultural sequence, going from
the Late Pleistocene to the Late Holocene and the historic periods. Four sites
were further studied by fourteen test excavation units: Dunas de Milpa Grande,
San José de las Grutas, the Chiquihuite Cave and Ojo de Agua. Two new
archaeological cultures were identified, one at Dunas (an interesting
assemblage of limestone and basalt flaked stone tools) and another one at San
José (a limestone concave-based points complex). First indicators of ʻolder than
Clovisʼ human presence have also been obtained. The palaeoenvironmental
data provide a preliminary reconstruction of the Late Pleistocene-Early
Holocene landscape of the basin, based on geology, extinct fauna, phytolith and
mollusc analyses. Radiocarbon and OSL results support a first cultural and
paleoclimatic model for the study area. This investigation also discovered the
first case of a “black mat” in Mexico: a black layer of sediment deposited under
specific environmental conditions during the Younger Dryas cooling event. | en_GB |