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Appendix A Paleontological Analysis
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75B - FAIRVIEW BRIDGE PROJECT CD
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Appendix A Paleontological Analysis
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Vertebrate Paleontology Section <br />Telephone: (213) 763-3325 <br />e-mail: smcleod@nhm.org <br />23 February 2018 <br />LSA Associates, Inc. <br />20 Executive Park, Suite 200 <br />Irvine, California 92614 <br />Attn: Sarah Rieboldt, Ph.D., Senior Paleontological Resources Manager <br />re: Paleontological Resources Records Check for the proposed Fairview Street Widening and <br />Bridge Replacement Project, LSA Project # WKE1702, in the City of Santa Ana, Orange <br />County, project area <br />Dear Sarah: <br />I have thoroughly searched our paleontology collection records for the locality and <br />specimen data for the proposed Fairview Street Widening and Bridge Replacement Project, LSA <br />Project # WKE1702, in the City of Santa Ana, Orange County, project area as outlined on the <br />portion of the Anaheim USGS topographic quadrangle map that you sent to me via e-mail on 9 <br />February 2018. We do not have any vertebrate fossil localities that lie within the proposed <br />project area boundaries, but we do have localities nearby from the same sedimentary units that <br />may occur subsurface in the proposed project area. <br />The entire proposed project has surface deposits of younger Quaternary Alluvium, <br />derived as fluvial deposits from the Santa Ana River that flows through the northern portion of <br />the proposed project area. These deposits are unlikely to contain significant vertebrate fossils in <br />the uppermost layers, but older Quaternary deposits occurring at varying depths may well contain <br />significant fossil vertebrate remains. Our closest vertebrate fossil locality from older Quaternary <br />deposits is probably LACM 1339, south-southwest of the proposed project area in Costa Mesa <br />east of the Santa Ana River near the top of the mesa bluffs along Adams Avenue, that produced <br />fossil specimens of mammoth, Mammuthus, and camel, Camelidae, bones from sands <br />approximately 15 feet below the top of the mesa that is overlain by shell bearing silts and sands.
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