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• W2065099063 abstract "Research Article| August 01, 1975 Early Tertiary ages from the coastal belt of the Franciscan complex, northern California William R. Evitt; William R. Evitt 1Department of Geology, Stanford University, Stanford, California 94305 Search for other works by this author on: GSW Google Scholar Sarah T. Pierce Sarah T. Pierce 1Department of Geology, Stanford University, Stanford, California 94305 Search for other works by this author on: GSW Google Scholar Author and Article Information William R. Evitt 1Department of Geology, Stanford University, Stanford, California 94305 Sarah T. Pierce 1Department of Geology, Stanford University, Stanford, California 94305 Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1975) 3 (8): 433–436. https://doi.org/10.1130/0091-7613(1975)3<433:ETAFTC>2.0.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation William R. Evitt, Sarah T. Pierce; Early Tertiary ages from the coastal belt of the Franciscan complex, northern California. Geology 1975;; 3 (8): 433–436. doi: https://doi.org/10.1130/0091-7613(1975)3<433:ETAFTC>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Dinoflagellates and angiosperm pollen from the Coastal belt of the Franciscan complex and Yager Formation in northern California establish an early Tertiary age no older than Eocene for numerous localities between Cape Mendocino and Fort Bragg. Until recently, the Coastal belt of the Franciscan complex has been mapped as Cretaceous. Several species of Wetzeliella Eisenack, a distinctive dinoflagellate genus that ranges in age from Paleocene to Miocene but is characteristic of Eocene strata, are especially conspicuous in samples from many of these localities. A few samples from the same area have yielded assemblages of Cretaceous palynomorphs. Evidence of redeposition of a Jurassic dinoflagellate species into Lower Cretaceous, lower Tertiary, and Eocene sediments and of Cretaceous dinoflagellates into lower Tertiary sediments appears in several samples. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2065099063 title "Early Tertiary ages from the coastal belt of the Franciscan complex, northern California" @default.
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