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Chihuahuan Desert Vegetation Development during the Past 10,000 Years According to Pollen and Sediment Data at Upper Arroyo, Saltillo, Mexico

Dados Bibliográficos

ID15801752
AutoresBruce Albert (Durham University, autor correspondente)
Ano2023
Volume6
Fascículo1
Páginas15-15
Data de publicação2023-02-13
Peer ReviewedSim
Open AccessSim
TipoARTICLE
PeriódicoQuaternary (JOURNAL)
Identificadores do periódicoISSN: 2571-550X • E-ISSN: 2571-550X
EditoraMultidisciplinary Digital Publishing Institute (PUBLISHER • CH)
DOI10.3390/quat6010015
OpenAlexW4320485821
IdiomaEN
Referências citadas21

Pollen and sediment data from a 10.5 m-deep alluvial exposure and a secondary tributary exposure at Upper Arroyo, a seasonal river, in Saltillo, Mexico, were examined with the aim of reconstructing the vegetation and environmental history during the Holocene as a whole. The role of climate change in Chihuahuan Desert flora development after 8800 BP was assessed, in addition to more local physiographic factors, such as erosion and accumulation, soil development and denudation, and hydrological entrenchment. Climate change appeared to have been a principal agent of vegetation change in the Early and Middle Holocene, with a periodic expansion of desert vegetation. A reduction in the environmental carrying capacities for mesophytic flora according to physiographic factors, such as soil erosion and channel entrenchment, was then identified after 2300 BP, also promoting azonal ecological niches for xerophytic vegetation in southern Coahuila, Mexico, that persist despite modern variations in precipitation

Climate change · Environmental change · Geography · Geomorphology · Holocene · Hydrology (agriculture · Physical geography · Sediment · Tributary · Vegetation (pathology · Archaeology and Natural History · Geology and Paleoclimatology Research · Tree-ring climate responses · Ecology · Geology · Oceanography

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