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A new marine vertebrate assemblage from the Late Neogene Purisima Formation in Central California, part II: Pinnipeds and Cetaceans Robert W. BOESSENECKER Department of Geology, University of Otago, 360 Leith Walk, P.O. Box 56, Dunedin, 9054 (New Zealand) and Department of Earth Sciences, Montana State University 200 Traphagen Hall, Bozeman, MT, 59715 (USA) and University of California Museum of Paleontology 1101 Valley Life Sciences Building, Berkeley, CA, 94720 (USA) [email protected] Boessenecker R. W. 2013. — A new marine vertebrate assemblage from the Late Neogene Purisima Formation in Central California, part II: Pinnipeds and Cetaceans. Geodiversitas 35 (4): 815-940. http://dx.doi.org/g2013n4a5 ABSTRACT e newly discovered Upper Miocene to Upper Pliocene San Gregorio assem- blage of the Purisima Formation in Central California has yielded a diverse collection of 34 marine vertebrate taxa, including eight sharks, two bony fish, three marine birds (described in a previous study), and 21 marine mammals. Pinnipeds include the walrus Dusignathus sp., cf. D. seftoni, the fur seal Cal- lorhinus sp., cf. C. gilmorei, and indeterminate otariid bones. Baleen whales include dwarf mysticetes (Herpetocetus bramblei Whitmore & Barnes, 2008, Herpetocetus sp.), two right whales (cf. Eubalaena sp. 1, cf. Eubalaena sp. 2), at least three balaenopterids (“Balaenoptera” cortesi “var.” portisi Sacco, 1890, cf. Balaenoptera, Balaenopteridae gen. et sp. indet.) and a new species of rorqual (Balaenoptera bertae n. sp.) that exhibits a number of derived features that place it within the genus Balaenoptera. is new species of Balaenoptera is relatively small (estimated 61 cm bizygomatic width) and exhibits a comparatively nar- row vertex, an obliquely (but precipitously) sloping frontal adjacent to vertex, anteriorly directed and short zygomatic processes, and squamosal creases. -
Appendices D Through I
Appendix D Operation & Maintenance Appendix D. Operation and Maintenance Plan Operation and Maintenance Plan This document presents the operation and maintenance (O&M) plan for Western Area Power Administration’s (Western) Sierra Nevada Region (SNR) transmission line systems. 1.0 Inspection/System Management In compliance with Western’s Reliability Centered Maintenance Program, Western would conduct aerial, ground, and climbing inspections of its existing transmission infrastructure since initial construction. The following paragraphs describe Western’s inspection requirements. Aerial Inspections Aerial inspections would be conducted a minimum of every 6 months by helicopter or small plane over the entire transmission system to check for hazard trees1 or encroaching vegetation, as well as to locate damaged or malfunctioning transmission equipment. Typically, aerial patrols would be flown between 50 and 300 feet above Western’s transmission infrastructure depending on the land use, topography, and infrastructure requirements. In general, the aerial inspections would pass over each segment of the transmission line within a one-minute period. Ground Inspections Annual ground inspections would check access to the towers/poles, tree clearances, fences, gates, locks, and tower hardware, and ensure that each structure would be readily accessible in the event of an emergency. They would allow for the inspection of hardware that would not be possible by air, and identify redundant or overgrown access roads that should be permanently closed and returned to their natural state. Ground inspections would typically be conducted by driving a pickup truck along the ROW and access roads. Detailed ground inspections would be performed on 20 percent of all lines and structures annually, for 100 percent inspection every 5 years. -
Sediment Provenance and Dispersal of Neogene–Quaternary Strata of the Southeastern San Joaquin Basin and Its Transition Into the GEOSPHERE; V
Research Paper THEMED ISSUE: Origin and Evolution of the Sierra Nevada and Walker Lane GEOSPHERE Sediment provenance and dispersal of Neogene–Quaternary strata of the southeastern San Joaquin Basin and its transition into the GEOSPHERE; v. 12, no. 6 southern Sierra Nevada, California doi:10.1130/GES01359.1 Jason Saleeby1, Zorka Saleeby1, Jason Robbins2, and Jan Gillespie3 13 figures; 2 tables; 2 supplemental files 1Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, USA 2Chevron North America Exploration and Production, McKittrick, California 93251, USA 3Department of Geological Sciences, California State University, Bakersfield, California 93311, USA CORRESPONDENCE: jason@ gps .caltech .edu CITATION: Saleeby, J., Saleeby, Z., Robbins, J., and ABSTRACT INTRODUCTION Gillespie, J., 2016, Sediment provenance and dis- persal of Neogene–Quaternary strata of the south- eastern San Joaquin Basin and its transition into We have studied detrital-zircon U-Pb age spectra and conglomerate clast The Sierra Nevada and Great Valley of California are structurally coupled the southern Sierra Nevada, California: Geosphere, populations from Neogene–Quaternary siliciclastic and volcaniclastic strata and move semi-independently within the San Andreas–Walker Lane dextral v. 12, no. 6, p. 1744–1773, doi:10.1130/GES01359.1. of the southeastern San Joaquin Basin, as well as a fault-controlled Neo- transform system as a microplate (Argus and Gordon, 1991; Unruh et al., 2003). gene basin that formed across the southernmost Sierra Nevada; we call this Regional relief generation and erosion of the Sierra Nevada are linked to sub- Received 9 May 2016 Accepted 31 August 2016 basin the Walker graben. -
USGS Professional Paper 1740
Age, Stratigraphy, and Correlations of the Late Neogene Purisima Formation, Central California Coast Ranges By Charles L. Powell II1, John A. Barron1, Andrei M. Sarna-Wojcicki1, Joseph C. Clark2, Frank A. Perry3, Earl E. Brabb4, and Robert J. Fleck1 Abstract Counties inland to the San Andreas Fault (fig. 1). These scat- tered outcrops have been grouped as the Purisima Formation The Purisima Formation is an important upper Miocene because they are all fine- to coarse-grained clastic rocks, with and Pliocene stratigraphic unit in central California, cropping dark andesitic fragments and locally abundant silicic tephra, out from the coast at Point Reyes north of San Francisco to and occupy the same stratigraphic position at their various more extensive exposures in the Santa Cruz Mountains to the exposures. Since first described by Haehl and Arnold (1904), south. The fine-grained rocks in the lower parts of the Puri- the Purisima Formation has been considered to be of Pliocene sima Formation record a latest Miocene transgressive event, or of late Miocene to Pliocene age. Differing age assignments whereas the middle and upper parts of the formation consist have resulted from the wide stratigraphic range of many com- of increasingly clastic-rich siltstones and sandstones resulting monly encountered megafossils and from the lack of agree- from uplift of adjacent coastal regions and the Sierra Nevada ment on the placement of the Miocene-Pliocene Series bound- during Pliocene transgressive and regressive sea-level events. ary between the provincial megafaunal chronology and that Exposures of the Purisima occur in three different, fault- of international usage. -
Qt53v080hx.Pdf
UC Berkeley PaleoBios Title A new Early Pliocene record of the toothless walrus Valenictus (Carnivora, Odobenidae) from the Purisima Formation of Northern California Permalink https://escholarship.org/uc/item/53v080hx Journal PaleoBios, 34(0) ISSN 0031-0298 Author Boessenecker, Robert W. Publication Date 2017-06-15 DOI 10.5070/P9341035289 Peer reviewed eScholarship.org Powered by the California Digital Library University of California PaleoBios 34:1-6, June 15, 2017 PaleoBios OFFICIAL PUBLICATION OF THE UNIVERSITY OF CALIFORNIA MUSEUM OF PALEONTOLOGY Boessenecker, Robert W. (2017). A New Early Pliocene Record of the Toothless Walrus Valenictus (Carnivora, Odobenidae) from the Purisima Formation of Northern California. Cover photo: Life restoration of the extinct Pliocene walrus Valenictus and flightless auks (Mancalla) hauled out on the rocky shore of the uplifted Coast Ranges of California (top right); cliff exposures of the Purisima Formation near Santa Cruz, from where Valenictus was collected by Wayne Thompson (left); bivalves, chiefly Clinocardium meekianum, exposed in the Purisima Formation near the locality (bottom). Photo credit and original artwork: Robert W. Boessenecker. Citation: Boessenecker, Robert W. 2017. A New Early Pliocene Record of the Toothless Walrus Valenictus (Carnivora, Odobenidae) from the Puri- sima Formation of Northern California. PaleoBios, 34. ucmp_paleobios_35289 A New Early Pliocene Record of the Toothless Walrus Valenictus (Carnivora, Odobenidae) from the Purisima Formation of Northern California ROBERT W. BOESSENECKER1,2 1Department of Geology and Environmental Geosciences, College of Charleston, Charleston, SC 29424; [email protected] 2University of California Museum of Paleontology, University of California, Berkeley, CA 94720 The walrus (Odobenus rosmarus) is a large tusked molluskivore that inhabits the Arctic and is the sole living member of the family Odobenidae. -
Active Tectonics at Wheeler Ridge, Southern San Joaquin Valley, California
Active tectonics at Wheeler Ridge, southern San Joaquin Valley, California E. A. Keller* Environmental Studies Program and Department of Geological Sciences, University of California, Santa Barbara, California 93106 R. L. Zepeda 1342 Grove Street, Alameda, California 94501 T. K. Rockwell Department of Geological Sciences, San Diego State University, San Diego, California 91282 T. L. Ku Department of Earth Sciences, University of Southern California, Los Angeles, California 90089-0740 W. S. Dinklage Department of Geological Sciences, University of California, Santa Barbara, California 93106 ABSTRACT INTRODUCTION where geomorphic surfaces are folded over the anticlinal axis (Zepeda et al., 1986). In addition, Wheeler Ridge is an east-west–trending Buried reverse faults associated with actively the 1952 Kern County earthquake was centered anticline that is actively deforming on the up- deforming folds are known to produce large earth- below Wheeler Ridge, but not on the Wheeler per plate of the Pleito–Wheeler Ridge thrust- quakes. Several recent, large California earth- Ridge thrust fault; therefore the potential earth- fault system. Holocene and late Pleistocene de- quakes are examples: M = 6.7, Northridge, 1994; quake hazard in the area is clear. formation is demonstrated at the eastern end M = 6.1, Whittier Narrows, 1987; MS = 6.4, The primary goals of the research at Wheeler of the anticline where Salt Creek crosses the Coalinga, 1983, and MS = 7.7, Kern County, Ridge are (1) to characterize the tectonic geomor- anticlinal axis. Uplift, tilting, and faulting, as- 1952. Detailed investigations of folding associ- phology; (2) to develop the Pleistocene chronol- sociated with the eastward growth of the anti- ated with concealed reverse faults are therefore ogy; and (3) to test the hypothesis that climatic cline, are documented by geomorphic surfaces necessary in order to better understand earthquake perturbations are responsible for most Pleistocene that are higher and older to the west. -
Summary of North American Blancan Nonmarine Mollusks1
MALACOLOGIA , 1966, 4(1): 1-172 SUMMARY OF NORTH AMERICAN BLANCAN NONMARINE MOLLUSKS1 D. W. Taylor U. S. Geological Survey, and Research Associate, University of Michigan Museum of Zoology, Ann Arbor, Michigan, U. S. A. ABSTRACT All known North American nonmarine mollusks of Blancan (late Pliocene and early Pleistocene) age have been here fitted into the available framework of associated fossils, physical stratigraphy and radiogenic potassium-argon dates. Many of the independently dated molluscan assemblages are so similar to other faunas that most of the fossils summarized can be assigned confidently to the Blancan age. These assignments permitted compilation of lists of last appear- ances of genera and families that are unknown during or after Blancan times. About 50-55 Blancan assemblages are known, and together with about 10-15 older or younger faunas included for convenience of discussion they are summarized under 57 local geographic headings (map, Fig. 1). For each local assemblage the following data have been given so far as possi- ble: location, previous references to mollusks, stratigraphic unit and most recent geologic maps, number of species of mollusks, mention of other fossils from the same locality or formation, age, institution where fossils are preserved, and most recent topographic maps. The detail of treatment varies widely, according to available information, progress of knowledge since previous liter- ature and the usefulness of new information. Lists of species are included usually only if the fauna is revised or first recorded in this paper, but the references to previous work are intended to be complete. The Blancan faunas from the Great Plains region (Nebraska, Kansas, Okla- homa, Texas), and from Arizona, are generally similar and include mainly widespread living species. -
Pdf/15/4/1164/4799287/1164.Pdf 1164 by California Inst of Technology User on 06 August 2019 Research Paper
Research Paper GEOSPHERE Late Cenozoic structure and tectonics of the southern Sierra Nevada–San Joaquin Basin transition, California GEOSPHERE, v. 15, no. 4 Jason Saleeby and Zorka Saleeby Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, USA https://doi.org/10.1130/GES02052.1 ■ ABSTRACT the San Joaquin Basin is widely known for its Neogene deep-marine condi- 17 figures; 3 tables; 1 set of supplemental files tions that produced prolific hydrocarbon reserves (Hoots et al., 1954). Rarely This paper presents a new synthesis for the late Cenozoic tectonic, paleogeo- in the literature are the late Cenozoic geologic features of these two adjacent CORRESPONDENCE: [email protected] graphic, and geomorphologic evolution of the southern Sierra Nevada and adja- regions discussed in any depth together. The late Cenozoic features of these cent eastern San Joaquin Basin. The southern Sierra Nevada and San Joaquin Ba- two regions speak to a number of significant issues in tectonics and geomor- CITATION: Saleeby, J., and Saleeby, Z., 2019, Late Cenozoic structure and tectonics of the southern Si- sin contrast sharply, with the former constituting high-relief basement exposures phology. These include: (1) the Earth’s surface responses to geologically rapid erra Nevada–San Joaquin Basin transition, Califor- and the latter constituting a Neogene marine basin with superposed low-relief changes in the distribution of mantle lithosphere loads; (2) the stability of nia: Geosphere, v. 15, no. 4, p. 1164–1205, https:// uplifts actively forming along its margins. Nevertheless, we show that Neogene cover strata–basement transition zones and the time scales over which pro- doi .org /10.1130 /GES02052.1. -
Geology and Paleontology of the Late Miocene Wilson Grove Formation at Bloomfield Quarry, Sonoma County, California
Geology and Paleontology of the Late Miocene Wilson Grove Formation at Bloomfield Quarry, Sonoma County, California 2 cm 2 cm Scientific Investigations Report 2019–5021 U.S. Department of the Interior U.S. Geological Survey COVER. Photographs of fragments of a walrus (Gomphotaria pugnax Barnes and Raschke, 1991) mandible from the basal Wilson Grove Formation exposed in Bloomfield Quarry, just north of the town of Bloomfield in Sonoma County, California (see plate 8 for more details). The walrus fauna at Bloomfield Quarry is the most diverse assemblage of walrus yet reported worldwide from a single locality. cm, centimeter. (Photographs by Robert Boessenecker, College of Charleston.) Geology and Paleontology of the Late Miocene Wilson Grove Formation at Bloomfield Quarry, Sonoma County, California By Charles L. Powell II, Robert W. Boessenecker, N. Adam Smith, Robert J. Fleck, Sandra J. Carlson, James R. Allen, Douglas J. Long, Andrei M. Sarna-Wojcicki, and Raj B. Guruswami-Naidu Scientific Investigations Report 2019–5021 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DAVID BERNHARDT, Secretary U.S. Geological Survey James F. Reilly II, Director U.S. Geological Survey, Reston, Virginia: 2019 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit https://www.usgs.gov/ or call 1–888–ASK–USGS (1–888–275–8747). For an overview of USGS information products, including maps, imagery, and publications, visit https://store.usgs.gov/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. -
On the Reconciliation of Biostratigraphy and Strontium Isotope Stratigraphy of Three Southern Californian Plio-Pleistocene Formations
On the reconciliation of biostratigraphy and strontium isotope stratigraphy of three southern Californian Plio-Pleistocene formations Alexandra J. Buczek1, Austin J.W. Hendy2, Melanie J. Hopkins1, and Jocelyn A. Sessa3,† 1 Division of Paleontology, American Museum of Natural History, Central Park West & 79th Street New York, New York 10024, USA 2 Department of Invertebrate Paleontology, Natural History Museum of Los Angeles County, 900 Exposition Blvd., Los Angeles, California 90007, USA 3 Department of Biodiversity, Earth and Environmental Science, Academy of Natural Sciences of Drexel University, 1900 Benjamin Franklin Parkway, Philadelphia, Pennsylvania 19103, USA ABSTRACT INTRODUCTION 2006; Powell et al., 2009; Squires, 2012; Ven- drasco et al., 2012). Based primarily on regional The San Diego Formation, Pico Forma- The mid-Pliocene warm period (ca 3 Ma; macrofossil and microfossil biostratigraphy, tion, Careaga Sandstone, and Foxen Mud- Jansen et al., 2007) was a time of high global these units are hypothesized to be late Pliocene stone of southern California are thought to temperatures (2 °C to 3 °C above pre-industrial to early Pleistocene in age (Figs. 1 and 3), but no be late Pliocene to early Pleistocene; however, temperatures) and high atmospheric CO2 con- numerical ages exist to confirm this hypothesis. numerical ages have not been determined. centrations (360–400 ppm) (Jansen et al., 2007). Previous age determinations must be revisited Following assessment of diagenetic altera- These climatic conditions, combined with the -
New 87 Sr/88 Sr Data from Invertebrate Macrofossils in the Neogene Etchegoin Formation, San Joaquin Basin, California K.B
New 87 Sr/88 Sr data from invertebrate macrofossils in the Neogene etchegoin formation, San Joaquin basin, California K.B. Loomis Isochron/West, Bulletin of Isotopic Geochronology, v. 58, pp. 17-21 Downloaded from: https://geoinfo.nmt.edu/publications/periodicals/isochronwest/home.cfml?Issue=58 Isochron/West was published at irregular intervals from 1971 to 1996. The journal was patterned after the journal Radiocarbon and covered isotopic age-dating (except carbon-14) on rocks and minerals from the Western Hemisphere. Initially, the geographic scope of papers was restricted to the western half of the United States, but was later expanded. The journal was sponsored and staffed by the New Mexico Bureau of Mines (now Geology) & Mineral Resources and the Nevada Bureau of Mines & Geology. All back-issue papers are available for free: https://geoinfo.nmt.edu/publications/periodicals/isochronwest This page is intentionally left blank to maintain order of facing pages. 17 NEW "Sr/««Sr DATA FROM tNVERTEBRATE MACROFOSSILS IN THE NEOGENE ETCHEGOIN FORMATION, SAN JOAQUIN BASIN, CALIFORNIA KAREN B. LOOMIS ARCO Exploration and Production Technology, Piano, TX 75075 The Etchegoin Group, comprised of the Jacalitos, previously unpublished ®^Sr/®®Sr data from marine inverte Etchegoin, and San Joaquin formations, forms the upper brate macrofossils suggesting that the Etchegoin part of the sedimentary fill of the San Joaquin forearc basin Formation in the west-central San Joaquin basin ranges of central California. This stratigraphic sequence is locally from late Miocene to early Pliocene in age. fossiliferous (i.e., containing plant fossils, invertebrate and vertebrate macrofossils) and consists of siltstone, sand METHODS stone, conglomerate, and rare tuff beds deposited in shallow-marine, marginal-marine, and nonmarine environ The Etchegoin Group was studied in the Jacalitos, ments during the late Neogene regression of the San Kreyenhagen, and Kettleman hills in the western San Joaquin Sea (Loomis, 1990a, 1990b). -
Geologic Names of North America Introduced in 19364955
Geologic Names of North America Introduced in 19364955 ^GEOLOGICAL SURVEY BULLETIN 1056-A Names of North America Introduced in 1936-1955 By DRUID WILSON, WILLIAM J. SANDO? and RUDOLPH W. KOPF Prepared with the assistance of BARBARA BEDETTE, JEAN L. EGGLETON, GRACE C. KEROHER, CAROLYN MANN, WILLIAM G. MELTON, JR., KATHERINE DENNISON PALMER, and JACK E. SMEDLEY GEOLOGIC NAMES OF NORTH AMERICA -G E O L O G I C AL SURVEY BULLETIN 1056-A A compilation of new geologic names of North America, including Greenland, the finest Indies, the Pacific Island pos sessions of the United States, and the Trust Territory of the Pacific Islands UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1957 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director ' For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1. (paper cover) FOEEWOBD The "Lexicon of geologic names of the United States" by M. Grace Wilmarth, published in 1938 and reprinted in 1951 and 1957, met a long standing need and continuing demand for a compilation of geologic names. Plans made for future compilations as new names and revisions appeared were interrupted during the years of World War II. In 1952 a sustained effort was begun toward review of geo logic publications necessary to furnish a background for preparation of a new edition. After the review was brought up to date in 1956, the present compilation was prepared in order to furnish to the geo logic profession, as quickly as possible, some of the essential data concerning the new names that have appeared since 1935.