An Archaeological and Paleontological Chronology for Daisy Cave (CA-SMI-261), San Miguel Island, California
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
1996-01-01Keywords
environmentcoastal 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
Metadata
Show full item recordCitation
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.Journal
RadiocarbonAdditional 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
Articletext
Language
enISSN
0033-8222ae974a485f413a2113503eed53cd6c53
10.1017/S0033822200017689