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Paleoclimatic Significance of Late Quaternary Lacustrine and Alluvial Stratigraphy, Animas Valley, New Mexico

Bibliographic Data

ID24088877
AuthorsP Reed Krider (University of Arizona, corresponding author)
Year1998
Volume50
Issue3
Pages283-289
Publication date1998-11-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueQuaternary Research (JOURNAL)
Journal identifiersISSN: 0033-5894 • E-ISSN: 1096-0287
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1006/qres.1998.1997
OpenAlexW1980303170
LanguageEN
Citations received4
References cited18

Lacustrine and alluvial stratigraphic sequences in the southern Animas Valley of New Mexico allow reconstruction of late Quaternary climates. Four separate stands of late Quaternary Lake Cloverdale in the southern Animas Valley are recorded by lacustrine shoreline deposits. Soils and stratigraphic evidence show that three young lake highstands occurred during the Holocene and that a higher lake stand occurred 18,000 to 20,000 14 C yr B.P. Fluvial systems aggraded the southern Animas Valley during the middle to late Holocene. The late Quaternary stratigraphy shows that several periods during the late Holocene were characterized by higher effective precipitation than at any time since the last glacial maximum.

Alluvium · Fluvial · Holocene · Quaternary · Structural basin · Tectonics · Geological formations and processes · Geology · Geology and Paleoclimatology Research · Isotope Analysis in Ecology · Paleontology · Stratigraphy

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Unique citing works4
Citations per year0,17
Citation span2002 - 2011 (10)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 2
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