Paleoenvironmental study of the Late Preclassic period in the Northern Mesoamerican Frontier

Bibliographic Data

ID12265755
AuthorsKurt H Wogau (0000-0002-2406-8304, Universidad Nacional Autonoma de Mexico, corresponding author), Benjamin Keenan (0000-0002-0274-8878, Swiss Federal Institute of Aquatic Science and Technology), Helge W Arz (0000-0002-1997-1718, Leibniz Institute for Baltic Sea Research Warnemünde), Harald Böhnel (0000-0002-3833-225X, Universidad Nacional Autonoma de Mexico), Harald N Böhnel (Universidad Nacional Autonoma de Mexico)
Year2023
Volume33
Issue11
Pages1291-1303
Publication date2023-07-29
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1177/09596836231185828
OpenAlexW4385380444
LanguageEN
Citations received2
References cited41

The Northern Mesoamerican Frontier was a complex multicultural region characterized by frequent human settlement changes and shifts in agricultural conditions during the Late Preclassic period (~400 BCE-150 CE). Here, we report a high-resolution paleoenvironmental record from the varved sedimentary sequence of the crater maar La Alberca which spans the Late Preclassic (~400 BCE-150 CE) to part of the Early Classic period (~150 CE-250 CE) corresponding to Late Chupicuaro phase (400 BCE-100 CE) and Mixtlan phase (0–250 CE). Our work aims to study the paleoenvironmental conditions during the rise of agriculture in the Northern Mesoamerican Frontier and provide insights related to landscape alteration by human activity. To reach these aims, a multiproxy investigation was conducted by means of varve counting, high-resolution XRF scans, magnetic susceptibility, pollen data and fecal stanol biomarkers as a proxy for human population change. Our results reveal two varve type. Type 1 is characterized by the alternation of detrital-organic layers and aragonite layers, type 2 by alternating detrital-organic layers with an organic layer formed by diatom frustules and aragonite layers. This study suggest that the increase of erosion by human activity during the Late Chupicuaro phase (400 BCE-100 CE) and the start of the Mixtlan phase (0–250 CE) coincide with a high percentage of Amaranthaceae pollen, a rise of sedimentation rates, increase in nutrient content and the increase of human waste flux interpreted with the (Coprostanol + epi) :((Coprostanol + epi)+cholestanol biomarker. Moreover, a wetter period (~137 BCE-37 CE) interpreted during the Late Chupiacuaro phase and the start of the Mixtlan phase could suggest favorable environmental conditions for the establishment of agriculture

Biology · Holocene · Period (music · Phytolith · Pollen · Population · Sediment · Varve · Archaeology and ancient environmental studies · Geology and Paleoclimatology Research · Pleistocene-Era Hominins and Archaeology · Ecology · Geology · Paleontology