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Upper Eocene Orbitoid Foraminifera from the Western Santa Ynez Range, California and their stratigraphic significance

Woodring, W. P. (1930) Upper Eocene Orbitoid Foraminifera from the Western Santa Ynez Range, California and their stratigraphic significance. Transactions of the San Diego Society of Natural History, 6 (4). pp. 147-162. ISSN 0080-5947. https://resolver.caltech.edu/CaltechAUTHORS:20191127-072811497

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Abstract

In December, 1929, Dr. W.S.W. Kew and Mr. H.L. Driver invited me to visit with them a locality on the west side of Canada de los Sauces, on the south slope of the western Santa Ynez Range about two miles northwest of Sudden, where they had discovered well-preserved specimens of a small Discocyclina in a soft limestone. When we visited this locality we also found almost equally well-preserved specimens of a small stellate “Discocyclina.” K.E. Lohman and S.W. Lohman, of the California Institute of Technology, accompanied me on a later trip to the same locality in March, 1930, when additional material was collected and the stratigraphic interval between the limestone and the base of the Vaqueros formation was measured.


Item Type:Article
Related URLs:
URLURL TypeDescription
https://doi.org/10.5962/bhl.part.11695DOIArticle
Additional Information:© 1930 San Diego Society of Natural History.
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Balch Graduate School of the Geological Sciences47
Issue or Number:4
Record Number:CaltechAUTHORS:20191127-072811497
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20191127-072811497
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:100083
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:27 Nov 2019 17:56
Last Modified:10 Dec 2019 18:25

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