| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 10499181 | Journal of Archaeological Science | 2012 | 9 Pages |
Abstract
⺠Oxygen isotope analysis was performed on prehistoric mussel shells dating to 6300-5300 cal BP. ⺠The analysis revealed that waters of the Santa Barbara Channel, CA, were cooler than historically. ⺠The results are consistent with those of previous regional oxygen isotope analyses. ⺠Collection of red abalone during the 6300-5300 cal BP period was facilitated by cool waters. ⺠Intertidal and subtidal water temperature variation is important in isotope data interpretation.
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Authors
Michael A. Glassow, H.B. Thakar, Douglas J. Kennett,
