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4.15 Paleontological Resources

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4.15 Paleontological Resources 4.15 Paleontological Resources 4.15 Paleontological Resources Paleontological resources, or fossils, are the evidence of once-living organisms preserved in the geologic record. They include both the fossilized remains of ancient plants and animals and the traces thereof (e.g., track ways, imprints, burrows, eggshells, etc.). In general, fossils are greater than 5,000 years old (middle Holocene) and are typically preserved in sedimentary rocks. Although rare, fossils can also be preserved in volcanic rocks and low-grade metamorphic rocks under certain conditions. The LWEP EIR addressed paleontological resources in the LWEP EIR Section 3.12, Paleontological Resources, and concluded that impacts to paleontological resources would be less than significant with mitigation. 4.15.1 Environmental Setting California can be divided in to eleven geomorphologic provinces. Santa Barbara County lies at the junction of two of these provinces: the Transverse Ranges and the Coastal Ranges. The geology of Santa Barbara County is dominated by marine sediments ranging in age from Mesozoic to Pleistocene. Dibblee (1950) said of Santa Barbara County, “The complex structure and resultant physiography of Santa Barbara County were developed by the series of diastrophic event starting with the early Miocene Yuezan orogeny and culminating with Pleistocene Coast Range orogeny, caused by a recurrent stress system of increasing intensity, these events together constituting the local effect of the Cascadian revolution.” Petroleum production and mining of diatomite have been the main mineral extraction enterprises in Santa Barbara County. 4.15.1.1 Data Sources Geologic mapping The LWEP EIR reviewed geological maps to determine what geologic units occur in the Project footprint and powerline route. The geologic units that were used in that document were the Franciscan Formation, Espada Formation, Anita Shale/Juncal Formation, Matilija Formation, Cozy Dell Shale Formation, Sacate- Gaviota (Coldwater) Formation, Tranquillon Volcanics, Vaqueros Sandstone, Rincon Sandstone, Monterey Shale, Sisquoc Shale, Older Quaternary Dissected Surficial sediments, Quaternary Landslide and Fluvial deposits, and Quaternary surficial sediments. The LWEP Fiinal EIR concluded that the rocks at and near the surface of the Project area are composed primarily of Neogene (Miocene and Pliocene) marine sediments. The geologic mapping on which this assessment is based are the pertinent 7.5’ quadrangle mapping of the Thomas Dibblee Foundation, specifically the Lompoc, Lompoc Hills, and Tranquillon Mountains quadrangles (Dibblee, 1988a, 1988b, 1988c). The features of the Project are superimposed on these geologic maps in Figure 4.15.1. Museum Record Searches No paleontological survey was performed for the LWEP or for the present assessment. A paleontolog- ical records search was not requested for the LWEP, but there was a review of paleontological localities in Santa Barbara County from the UCMP paleontological locality online database. The conclusion was Final SEIR 4.15-1 October 2019 Project Boundary Geology Type (Source Dibblee, 1988) Qa Quaternary alluvium Tvqcg Vaqueros Sandstone Proposed Limits of Grading and Turbine Access Roads Qls Landslide deposits Tg-sa Gaviota-Sacate Formations, undivided Qoa Older dissected surficial sediments Tsass Proposed Transmission Line Sacate Formation Tsqd Sisquoc Shale Tcd Cozy Dell Shale "/ Proposed Substation Tmd Monterey Shale, diatomite facies Tma Matilija Sandstone ") Operation and Maintenance Building Tm Monterey Shale, upperr shale unit Tan Anita Shale fm 1$ Proposed Turbine WTG GE 1.79 80m Tml Monterey Shale, lower shale unit Franciscan Assemblage Tmls Monterey Shale, dolomite unit Ke Espada Formation 1$ Proposed Turbine WTG GE 3.8 81.5m Ttr Tranquillon Volcanic Formation Kh Honda Shale N-9 1$ N-8 N-7 1$ 1$ N-6 1$ N-5 W-7 1$ N-4 1$ W-13 1$ 1$ W-12 W-8 1$ N-3 1$ 1$ N-2 W-11 1$ 1$ W-6 W-3 ") E-3 "/ W-10 W-9 1$ 1$ N-1 1$ 1$ 1$ 1$ E-1 E-2 W-4 W-2 W-1 1$ 1$ W-5 1$ 1$ 1$ E-4 1$ 1$ E-7 E-8 E-5 E-6 1$ 1$ 1$ $ 1 Figure 4.15-1. Geological Map 1 0 F Miles 4.15 Paleontological Resources that there were 127 total localities within Santa Barbara County and that 17 were from the Franciscan melange, 56 were from the Vaqueros Formation, 3 were from the Rincon Formation, 12 were from the Monterey Formation, and 21 were from the Sisquoc Formation. Aspen requested a paleontological records search from the Vertebrate Paleontology Department of the Natural history Museum of Los Angeles County (LACM) for information on localities within the Project footprint and within one mile of it. Dr. Sam McLeod of that institution related that the institution had no localities in the Tranquillon Volcanics, Cody Dell Shale, or Gaviota-Sacate Formations undivided. He stated that there is a locality in the Vaqueros Formation just south of Lake Cachuma that produced five types of sharks. LACM locality 6590 lies in the Monterey Formation just west of the northern part of the Project area less than one mile north of Miguelito Park. It has produced fossils of the herring Etringus. LACM locality 4156 is in a diatomite quarry just west of 6590 and has produced teeth of the shark Isurus hastalis, as well as the skeletons of many bony fish species, including Xyne, Eclipes, Lompoquia, sparids, flounders, rockfish, Chauliodus, Hipposynghanthus, a bird, a sea lion Pithanotaria, and the sperm whale Scaldicetus. In the White Hills east of LACM 6590 is a locality within the Monterey Formation. It has produced teeth of the shark Isurus oxyrhinchus, and skeletons of numerous kinds of bony fishes. These include Lampanyctus, Thrysocles, Lompoquia, Scomber, Protanthias, Rhythmias, Pleuronichthys, Bathylagus, Sebastodes, Cyclothone, and Argyropelecus. The holotype of Protanthias fossilis came from this locality. Most of these specimens were published by Lore David in 1943. In the northeastern part of the Project area in the Santa Ynez Mountains is LACM locality 6589, listed as being in the Sisquoc Formation. Due to changing usages of the of the Sisquoc and Monterey formations, it is probable that some or all of these specimens come from the Monterey Formation. Bony fishes found there include serrivomerids, belonids, Zelosis, Scomberesox, Etringus, Ganolytes, Xyne, Eclipes, Physiculus, Microlepidium, Lampanyctus, scombrids, trichiurids, flounders, bathylagids, melanostomatids, Chauliodus, Cyclothone, Argyropelecus, and Hipposyngnathus imporcitor. Literature Search The LWEP concluded that geologic and paleontological research in the specific Project area has been limited. Aspen found that there is an extensive body of literature on the geological and paleontological resources of western Santa Barbara County, but the paleontological literature focuses on the fossils of the Monterey and Sisquoc formations. Aspen searched a compilation of Fierstine et al. (2012) for fossil fishes published from the Lompoc vicinity. Fierstine et al. (2012) record at least 47 species of bony fish that have been named on specimens from the Monterey and Sisquoc formations of this part of Santa Barbara County. Most of these were published by Dr. David Starr Jordan, one-time chancellor of Stanford University. Referred specimens of at least four kinds of fish have been described from this rock. Several kinds of birds and one mammal have been described from rocks of the Monterey and/or Sisquoc formations of the Project area. Aspen also searched the compilations of Jefferson (1991a, 1991b) to determine whether any Pleistocene vertebrate fossils were listed for the area. None were listed. Paleosensitivity Dr. McLeod advised in his records search report that excavations in the exposures of the Tranquillon Volcanics in the Project area will not uncover any recognizable fossils. Shallow excavations in the younger Quaternary Alluvium exposed in the drainages of the Project area are unlikely to encounter Final SEIR 4.15-3 October 2019 4.15 Paleontological Resources significant vertebrate fossil remains. Deeper excavations in those deposits that extend down into older sedimentary deposits, or any excavations in the exposures of the Cozy Dell Shale, Gaviota-Sacate Formations undivided, Vaqueros Sandstone, Miocene Monterey Shale Formation, or Sisquoc Forma- tion in the Project area; however, may well uncover significant vertebrate fossils. Dr. McLeod advised that any substantial excavations in the sedimentary deposits in the Project area, therefore, should be monitored closely to quickly and professionally recover any fossil remains discovered while not impeding development. He mentioned that sediment samples should be collected and processed to determine the small fossil potential in the Project area. Any fossils recovered during mitigation should be deposited in an accredited and permanent scientific institution for the benefit of current and future generations. The SVP standard guidelines contain a method of rating the paleontological sensitivity for any given formation. Other methods are utilized by the Bureau of Land Management. The LWEP employed the SVP methodology. Potential mitigation measures also follow an established protocol codified by the SVP. The present review utilizes the most recent version (2010) of the SVP guidelines. An ancillary matter in ranking the paleontological sensitivity of rock units is how one defines a significant paleontological resource. The SVP guidelines (2010) define a significant paleontological resource as fossils and fossiliferous deposits of identifiable vertebrate fossils, large or small,
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