Late Precambrian–Early Cambrian stratigraphic and faunal succession of eastern California and the Precambrian–Cambrian boundary
- 1 March 1978
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 115 (2), 121-126
- https://doi.org/10.1017/s0016756800041169
Abstract
The Late Precambrian and Early Cambrian strata in eastern California and Nevada can be divided into 3 facies the Fallotaspis, the Nevadella and the Bonnia-Olenellus; the inter-relationships are outlined. Correlations with the Siberian Platform successions are discussed and the Precambrian–Cambrian boundary is tentatively placed within the beds of the upper Reed Dolomite in the White-lnyo Range.This publication has 7 references indexed in Scilit:
- Age of archaeocyathid assemblagesAmerican Journal of Science, 1974
- Lower Cambrian trilobites from the Sekwi Formation type section, Mackenzie Mountains, northwestern CanadaPublished by Natural Resources Canada/CMSS/Information Management ,1972
- Upper Precambrian and lower Cambrian strata in the southern Great Basin, California and NevadaPublished by US Geological Survey ,1970
- Phanerozoic-Cryptozoic and Related Transitions: New EvidenceScience, 1966
- An unusual Lower Cambrian trilobite fauna from NevadaProfessional Paper, 1964
- Helicoplacoidea: A New Class of EchinodermsScience, 1963
- LOWER CAMBRIAN-PRECAMBRIAN SUCCESSION, WHITE-INYO MOUNTAINS, CALIFORNIAGSA Bulletin, 1962