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    • Radiocarbon, Volume 38 (1996)
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    An Archaeological and Paleontological Chronology for Daisy Cave (CA-SMI-261), San Miguel Island, California

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    Author
    Erlandson, Jon M.
    Kennett, Douglas J.
    Ingram, B. Lynn
    Guthrie, Daniel A.
    Morris, Don P.
    Tveskov, Mark A.
    West, G. James
    Walker, Phillip L.
    Issue Date
    1996-01-01
    Keywords
    environment
    coastal environment
    San Miguel Island
    Santa Barbara County California
    cave environment
    floral studies
    Daisy Cave
    California
    faunal studies
    marine environment
    human activity
    biota
    archaeology
    Holocene
    Pleistocene
    United States
    Cenozoic
    Quaternary
    C 14
    carbon
    dates
    isotopes
    radioactive isotopes
    stable isotopes
    absolute age
    C 13
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    Citation
    Erlandson, J. M., Kennett, D. J., Ingram, B. L., Guthrie, D. A., Morris, D. P., Tveskov, M. A., ... & Walker, P. L. (1996). An archaeological and paleontological chronology for Daisy cave (CA-SMI-261), San Miguel Island, California. Radiocarbon, 38(2), 355-373.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    URI
    http://hdl.handle.net/10150/653529
    DOI
    10.1017/S0033822200017689
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    We provide detailed contextual information on 25 14C dates for unusually well-preserved archaeological and paleontological remains from Daisy Cave. Paleontological materials, including faunal and floral remains, have been recovered from deposits spanning roughly the past 16,000 yr, while archaeological materials date back to ca. 10,500 BP. Multidisciplinary investigations at the site provide a detailed record of environmental and cultural changes on San Miguel Island during this time period. This record includes evidence for the local or regional extinction of a number of animal species, as well as some of the earliest evidence for the human use of boats and other maritime activities in the Americas. Data from Daisy Cave contribute to a growing body of evidence that Paleoindians had adapted to a wide variety of New World environments prior to 10,000 BP. Analysis of shell-charcoal pairs, along with isotopic analysis of associated marine shells, supports the general validity of marine shell dating, but also provides evidence for temporal fluctuations in the reservoir effect within the Santa Barbara Channel region.
    Type
    Article
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200017689
    Scopus Count
    Collections
    Radiocarbon, Volume 38, Number 2 (1996)

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