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Early–Mid Pleistocene environments in the Valsequillo Basin, Central Mexico: a reassessment
Author(s) -
Metcalfe Sarah E.,
Leng Melanie J.,
Kirby Jason R.,
Huddart David,
Vane Christopher H.,
Gonzalez Silvia
Publication year - 2016
Publication title -
journal of quaternary science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.142
H-Index - 94
eISSN - 1099-1417
pISSN - 0267-8179
DOI - 10.1002/jqs.2851
Subject(s) - pleistocene , megafauna , geology , tephra , volcano , quaternary , pyroclastic rock , early pleistocene , structural basin , volcanic ash , rhyolite , paleontology , palynology , volcanic rock , pollen , ecology , biology
The Valsequillo Basin in Central Mexico has been of interest due to the presence of megafaunal remains and evidence for early human occupation, but research has been controversial. It has been suggested that extensive and deep lakes characterized the Early Pleistocene environment but sediment exposure is highly fragmentary and reliable dating has been difficult. Here we report, for the first time, Early Pleistocene palaeoenvironmental reconstructions using stable isotopes, diatoms, tephra and pollen. We studied several stratigraphic sections of mainly non‐volcanic rocks, containing the 1.3‐Ma Xalnene Ash as a stratigraphic marker. The isotope and other proxy data show that topographically low points in the basin were occupied by spring‐fed, shallow water lakes during the Early–Mid Pleistocene, with a trend to drier conditions. The basin was a dynamic volcaniclastic environment during this period, with the production of the Toluquilla volcanic sequence and other rhyolitic–dacitic volcanic ashes interbedded with the lake sediments at the sections studied. There is no evidence from the sections for extensive and deep lakes before or after deposition of the Xalnene Ash. Wetter conditions in the basin during the Early Pleistocene would have made it attractive for megafauna. Copyright © 2016 The Authors. Journal of Quaternary Science Published by John Wiley & Sons Ltd.