Applications of strontium isotopes in correlating Monterey Formation, California
Recent improvements in the accuracy with which the strontium-isotope evolution of seawater can be determined allows strontium isotopes to be used for correlating marine sediments at resolutions comparable to biostratigraphic methods. In this study, they geochemically and biostratigraphically analyzed outcrop sections along Naples Beach and Graves Creek, in order to correlate the Monterey formation with concurrent global paleo-oceanographic events. By correlating the /sup 87/SR//sup 86/SR ratio in these sediments with the strontium isotope vs. time curve for seawater derived from calcareous oozes in DSDP Corehole 590 (southwestern Pacific) and DSDP Corehole 575 (central Pacific), they determined ages at resolutions ranging from < 0.1 to 2.5 Ma. With an average resolution in the early Miocene of 200,000 years, strontium-isotope dating has enabled them to determine the onset of Monterey deposition with exceptional accuracy. Their results date the basal Monterey Formation at approximately 17.8 Ma in both the Salinas basin and the Santa Barbara-Ventura basin. This date corresponds to a major shift in the delta/sup 13/C seawater curves, supporting the inference that Monterey-type deposition was responsible for the sequestering of light carbon. Although the ratio increases monotonically in the lower Miocene at Graves Creek, this is not the situation in the coeval part of the Naples Beach section, where it reveals heretofore unidentified structure. The isotopic and biostratigraphic data indicate that the major hiatus in the Naples Beach section ranges from approximately 14 to 11 Ma, which is about 2 m.y. shorter than previously interpreted.
- Research Organization:
- Univ. of California, Los Angeles (USA)
- OSTI ID:
- 6594982
- Report Number(s):
- CONF-8804144-
- Journal Information:
- AAPG Bull.; (United States), Journal Name: AAPG Bull.; (United States) Vol. 72:3; ISSN AABUD
- Country of Publication:
- United States
- Language:
- English
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