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Engineering Geology and Seismology for Public Schools and Hospitals in California
The Resources Agency California Geological Survey Michael Chrisman, Secretary for Resources Dr. John G. Parrish, State Geologist Engineering Geology and Seismology for Public Schools and Hospitals in California to accompany California Geological Survey Note 48 Checklist by Robert H. Sydnor, Senior Engineering Geologist California Geological Survey www.conservation.ca.gov/cgs July 1, 2005 316 pages Engineering Geology and Seismology performance–based analysis, diligent subsurface for Public Schools and Hospitals sampling, careful reading of the extensive geologic in California literature, thorough knowledge of the California Building Code, combined with competent professional geological work. by Robert H. Sydnor Engineering geology aspects of hospital and public California Geological Survey school sites include: regional geology, regional fault July 1, 2005 316 pages maps, site-specific geologic mapping, geologic cross- sections, active faulting, official zones of investigation Abstract for liquefaction and landslides, geotechnical laboratory The 446+ hospitals, 1,400+ skilled nursing facilities testing of samples, expansive soils, soluble sulfate ±9,221 public schools, and 109 community college evaluation for Type II or V Portland-cement selection, campuses in California are regulated under California and flooding. Code of Regulations, Title 24, California Building Code. Seismology aspects include: evaluation of historic These facilities are plan–checked by senior–level seismicity, probabilistic seismic hazard analysis of Registered Structural Engineers within the Office of earthquake ground–motion, use of proper code terms Statewide Health Planning and Development (OSHPD) (Upper–Bound Earthquake ground–motion and Design– for hospitals and skilled nursing facilities, and the Basis ground–motion), classification of the geologic Division of the State Architect (DSA) for public schools, subgrade by shear–wave velocity to select the correct community colleges, and essential services buildings. -
Guidebook Contains Preliminary Findings of a Number of Concurrent Projects Being Worked on by the Trip Leaders
TH FRIENDS OF THE PLEISTOCENE, ROCKY MOUNTAIN-CELL, 45 FIELD CONFERENCE PLIO-PLEISTOCENE STRATIGRAPHY AND GEOMORPHOLOGY OF THE CENTRAL PART OF THE ALBUQUERQUE BASIN OCTOBER 12-14, 2001 SEAN D. CONNELL New Mexico Bureau of Geology and Mineral Resources-Albuquerque Office, New Mexico Institute of Mining and Technology, 2808 Central Ave. SE, Albuquerque, New Mexico 87106 DAVID W. LOVE New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, NM 87801 JOHN D. SORRELL Tribal Hydrologist, Pueblo of Isleta, P.O. Box 1270, Isleta, NM 87022 J. BRUCE J. HARRISON Dept. of Earth and Environmental Sciences, New Mexico Institute of Mining and Technology 801 Leroy Place, Socorro, NM 87801 Open-File Report 454C and D Initial Release: October 11, 2001 New Mexico Bureau of Geology and Mineral Resources New Mexico Institute of Mining and Technology 801 Leroy Place, Socorro, NM 87801 NMBGMR OFR454 C & D INTRODUCTION This field-guide accompanies the 45th annual Rocky Mountain Cell of the Friends of the Pleistocene (FOP), held at Isleta Lakes, New Mexico. The Friends of the Pleistocene is an informal gathering of Quaternary geologists, geomorphologists, and pedologists who meet annually in the field. The field guide has been separated into two parts. Part C (open-file report 454C) contains the three-days of road logs and stop descriptions. Part D (open-file report 454D) contains a collection of mini-papers relevant to field-trip stops. This field guide is a companion to open-file report 454A and 454B, which accompanied a field trip for the annual meeting of the Rocky Mountain/South Central Section of the Geological Society of America, held in Albuquerque in late April. -
With Focus on the Genus Handleyomys and Related Taxa
Brigham Young University BYU ScholarsArchive Theses and Dissertations 2015-04-01 Evolution and Biogeography of Mesoamerican Small Mammals: With Focus on the Genus Handleyomys and Related Taxa Ana Villalba Almendra Brigham Young University - Provo Follow this and additional works at: https://scholarsarchive.byu.edu/etd Part of the Biology Commons BYU ScholarsArchive Citation Villalba Almendra, Ana, "Evolution and Biogeography of Mesoamerican Small Mammals: With Focus on the Genus Handleyomys and Related Taxa" (2015). Theses and Dissertations. 5812. https://scholarsarchive.byu.edu/etd/5812 This Dissertation is brought to you for free and open access by BYU ScholarsArchive. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. Evolution and Biogeography of Mesoamerican Small Mammals: Focus on the Genus Handleyomys and Related Taxa Ana Laura Villalba Almendra A dissertation submitted to the faculty of Brigham Young University in partial fulfillment of the requirements for the degree of Doctor of Philosophy Duke S. Rogers, Chair Byron J. Adams Jerald B. Johnson Leigh A. Johnson Eric A. Rickart Department of Biology Brigham Young University March 2015 Copyright © 2015 Ana Laura Villalba Almendra All Rights Reserved ABSTRACT Evolution and Biogeography of Mesoamerican Small Mammals: Focus on the Genus Handleyomys and Related Taxa Ana Laura Villalba Almendra Department of Biology, BYU Doctor of Philosophy Mesoamerica is considered a biodiversity hot spot with levels of endemism and species diversity likely underestimated. For mammals, the patterns of diversification of Mesoamerican taxa still are controversial. Reasons for this include the region’s complex geologic history, and the relatively recent timing of such geological events. -
Miocene Biostratigraphy and Biochronology of the Dove Spring Formation, Mojave Desert, California, and Characterization of the C
Miocene biostratigraphy and biochronology of the Dove Spring Formation, Mojave Desert, California, and characterization of the Clarendonian mammal age (late Miocene) in California DAVID P. WHISTLER Vertebrate Paleontology Section.Natural History Museum of Los Angeles County, Los Angeles, California 90007 DOUGLAS W. BURBANK Department of Geological Sciences, University of Southern California, Los Angeles, California 90089-0740 ABSTRACT ing on other continents (Savage and Russell, 1983). The characterization of the NMLMA has undergone continuous revision since 1941, but the The Dove Spring Formation (DSF) is an 1,800-m-thick succes- first comprehensive redefinition was recently completed after a 12-year sion of fluvial, lacustrine, and volcanic rocks that contains a nearly effort (Woodburne, 1987). Detailed studies of local successions, such as continuous sequence of diverse vertebrate fossil assemblages. When the Dove Spring Formation (DSF), provide the data needed for further the North American provincial mammalian ages were originally de- refinement of the North American terrestrial biochronologic system, fined in 1941, the fossil fauna of the DSF (now part of the Ricardo Due to rapid rates of speciation in fossil mammals during Cenozoic Group) was one of four fossil assemblages named as principal correla- time, it is possible to construct detailed biostratigraphic histories that often tives of the Clarendonian mammal age. Early radiometric work depict complex evolutionary patterns. Terrestrial vertebrates are influ- yielded a maximum age of 10.0 Ma for this fossil assemblage, and by enced by tectonic barriers and local environmental factors, however, and correlation to the Great Plains of the United States, this date was these animals become isolated into regional zoogeographic provincial as- considered representative of Clarendonian time. -
Palaeontologia Electronica New Rodents (Mammalia, Rodentia
Palaeontologia Electronica http://palaeo-electronica.org New rodents (Mammalia, Rodentia, Cricetidae) from the Verde Fauna of Arizona and the Maxum Fauna of California, USA, early Blancan Land Mammal Age Everett H. Lindsay and Nicholas J. Czaplewski ABSTRACT The cricetid rodent Postcopemys repenningi, new genus and new species, is described from the Verde fauna in Arizona and the Maxum fauna in California. Two other rodents, Postcopemys maxumensis, new species, and Jacobsomys dailyi are reported herein from the Maxum fauna. Jacobsomys dailyi is described and Postcope- mys valensis is reported (May et al. 2011) from the Warren fauna in southern Califor- nia. Jacobsomys verdensis had been reported from the Verde fauna by Czaplewski (1987a). These three faunas (the Warren and Maxum faunas in California and the Verde fauna in Arizona) are considered close to the Blancan/Hemphillian boundary, and the two genera Postcopemys and Jacobsomys are important small mammal taxa whose stage of evolution should prove useful for demonstrating the morphologic transi- tion between Copemys and extant Peromyscus via Postcopemys, and between Ben- sonomys and extant Oryzomys via Jacobsomys, as well as for ordering mammalian faunas relative to the Blancan/Hemphillian boundary. Everett H. Lindsay. Department of Geosciences, Gould-Simpson Building, University of Arizona, Tucson, Arizona 85721 USA [email protected] Nicholas J. Czaplewski. Oklahoma Museum of Natural History, 2401 Chautauqua Avenue, University of Oklahoma, Norman, Oklahoma 73072 USA [email protected] KEY WORDS: Cricetidae; Verde; Maxum; Blancan; fossils; Pliocene INTRODUCTION lection initially advocated by Hibbard (1949), and a virtual army of eager young students to apply those The last 50 years have seen an explosive collection methods. -
Palaeontologia Electronica Shrews, Lagomorphs, and Rodents
Palaeontologia Electronica http://palaeo-electronica.org Shrews, lagomorphs, and rodents (excluding Cricetidae) from the Pliocene Panace Formation, southeastern Nevada, USA Yun Mou ABSTRACT About 2,500 specimens of small mammal fossils were collected from 12 localities in the Pliocene Panaca Formation in Meadow Valley, southeastern Nevada. The most common taxa in the Panaca small mammal fauna are cricetid and heteromyid rodents, and lagomorphs. This assemblage of small mammals indicates that the Panaca local fauna represents the early Blancan Land Mammal Age. This paper describes and compares the small mammal taxa of the Panaca local fauna except for the cricetids, which are described in a separate paper in this volume. Yun Mou, 8159 East Pima Ridge Drive, Tucson, AZ 85715, USA. [email protected] KEY WORDS: early Blancan; NALMA; small mammals; local fauna INTRODUCTION lected earlier by Stock. Later still, both small and large mammals were collected by T. Galusha and The Panaca local fauna (l.f.) described by R. Emry, working for the American Museum of Nat- Chester Stock (1921) is located in Meadow Valley, ural History (AMNH). Some of those fossils were south of Panaca in Lincoln County, southeastern described by May (1981), Repenning (1987), and Nevada (Figure 1). Stock named the sediments the White (1987, 1991). Mou (1997) described a new Panaca Formation. The fossils from Panaca species of arvicolid rodent from the Panaca l.f., and described by Stock include Pliohippus sp., ?Teleo- later (1998) described the enamel schmelzmuster ceras sp., and Pliauchenia (now considered Hemi- of the new arvicolid rodent. Virtually all of these auchenia), genera that were generally assigned to small mammals collected from the Panaca area the Hemphillian North American Land Mammal are indicative of Blancan NALMA. -
Mammals of the Greater Gila Region Amanda K
University of New Mexico UNM Digital Repository Biology ETDs Electronic Theses and Dissertations 7-1-2016 Mammals of the Greater Gila Region Amanda K. Jones Follow this and additional works at: https://digitalrepository.unm.edu/biol_etds Recommended Citation Jones, Amanda K.. "Mammals of the Greater Gila Region." (2016). https://digitalrepository.unm.edu/biol_etds/123 This Thesis is brought to you for free and open access by the Electronic Theses and Dissertations at UNM Digital Repository. It has been accepted for inclusion in Biology ETDs by an authorized administrator of UNM Digital Repository. For more information, please contact [email protected]. i Amanda K. Jones Candidate Biology Department This thesis is approved, and it is acceptable in quality and form for publication: Approved by the Thesis Committee: Dr. Joseph Cook, Chairperson Dr. David Schmidly Dr. Ernie Valdez ii MAMMALS OF THE GREATER GILA REGION by AMANDA K. JONES BACHELORS OF SCIENCE IN BIOLOGY THESIS Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science Biology The University of New Mexico Albuquerque, New Mexico July 2016 iii Acknowledgments: I first want to thank my advisor, Joe Cook, for believing in me enough to give me this wonderful opportunity, and for your endless help on all aspects of this endeavor. You were an exceptional advisor. Your patience and humor were invaluable in helping me finish this project. I want to thank my committee members, Dave Schmidly and Ernie Valdez, for their help in the field, for their assistance with scientific guidance and editing, help identifying specimens, and for their collectively great attitudes. -
On the Ancestry of Woodrats
applyparastyle "fig//caption/p[1]" parastyle "FigCapt" applyparastyle "fig" parastyle "Figure" Journal of Mammalogy, XX(X):1–19, 2019 DOI:10.1093/jmammal/gyz105 Downloaded from https://academic.oup.com/jmammal/advance-article-abstract/doi/10.1093/jmammal/gyz105/5531474 by ASM Member Access user on 15 July 2019 On the ancestry of woodrats Robert A. Martin* and Richard J. Zakrzewski Department of Biological Sciences, Murray State University, Murray, KY 42071, USA (RAM) Department of Geosciences and Sternberg Museum of Natural History, Fort Hays State University, Hays, KS 67601, USA (RJZ) * Correspondent: [email protected] We evaluated the fossil record of extinct and extant woodrats, and generated a comprehensive phylogenetic hypothesis of woodrat origins and relationships based on these data. The galushamyinin cricetines are redefined and reclassified as a subtribe of the Neotomini, including Repomys, Miotomodon, Galushamys, Nelsonia, and a new extinct genus with two new species. The geographic distribution of Nelsonia, restricted to montane coniferous forests of western Mexico, suggests that this subtribe was mostly confined to western coniferous ecosystems or similar ecosystems at lower elevation during glacial advances. A second subtribe of the Neotomini includes a new archaic genus and species, Neotoma, Hodomys, and Xenomys. Lindsaymys, a possible neotominin from the late Clarendonian (late Miocene) of California, demonstrates an occlusal morphology consistent with ancestry for the Neotomini, but the presence of a fourth root on M1 is problematic and may preclude the known populations from filling that role. Molars identified as Neotoma sp. from the Hemphillian (latest Miocene or early Pliocene) Rancho el Ocote assemblage of Guanajuato, Mexico, may represent the earliest Xenomys. -
New Species of Sinocapra (Bovidae, Caprinae) from the Lower Pliocene Panaca Formation, Nevada, Usa
Palaeontologia Electronica http://palaeo-electronica.org NEW SPECIES OF SINOCAPRA (BOVIDAE, CAPRINAE) FROM THE LOWER PLIOCENE PANACA FORMATION, NEVADA, USA Jim I. Mead and Louis H. Taylor ABSTRACT A new species of Caprini is described from the early Pliocene (Blancan NALMA) Meadow Valley deposits of Panaca, Nevada, USA, and probably represents the earli- est caprine known from North America. The Meadow Valley fauna of the Panaca For- mation existed between 4.95 and 4.50 Ma ago. Comparative data indicate that Sinocapra willdownsi sp. nov. most closely resembles the extinct caprine Sinocapra minor, known only from the Yushe Basin, China. The Mazegou Formation locality, from which S. minor was collected, was deposited about 3.5 Ma ago. Morphological analy- sis also indicates that Sinocapra is more closely allied to sheep than to goats. Basal caprine ancestors were present in Europe during the late Miocene, but the earliest sheep, Ovis, appears in China at approximately 2.42 Ma ago. The earlier presence of the sheep-like Sinocapra in North America is problematic and may indicate an early migration from China. However, it may also indicate that Sinocapra evolved in North America from an ancestor that migrated from China even earlier, and later dispersed back to Asia. We postulate that Sinocapra migrated to North America from northeast- ern China during the latest Miocene or earliest Pliocene (late late Hemphillian NALMA). Jim I. Mead. Department of Geology and the Quaternary Sciences Program, Northern Arizona University, Flagstaff, Arizona 86011, and Museum of Northern Arizona, Flagstaff, Arizona, 86001, USA [email protected] Louis H. -
Whistler-Burbank Mojave Clarendonian GSAB 1992.Pdf
Downloaded from gsabulletin.gsapubs.org on January 30, 2015 Miocene biostratigraphy and biochronology of the Dove Spring Formation, Mojave Desert, California, and characterization of the Clarendonian mammal age (late Miocene) in California DAVID P. WHISTLER Vertebrate Paleontology Section.Natural History Museum of Los Angeles County, Los Angeles, California 90007 DOUGLAS W. BURBANK Department of Geological Sciences, University of Southern California, Los Angeles, California 90089-0740 ABSTRACT ing on other continents (Savage and Russell, 1983). The characterization of the NMLMA has undergone continuous revision since 1941, but the The Dove Spring Formation (DSF) is an 1,800-m-thick succes- first comprehensive redefinition was recently completed after a 12-year sion of fluvial, lacustrine, and volcanic rocks that contains a nearly effort (Woodburne, 1987). Detailed studies of local successions, such as continuous sequence of diverse vertebrate fossil assemblages. When the Dove Spring Formation (DSF), provide the data needed for further the North American provincial mammalian ages were originally de- refinement of the North American terrestrial biochronologic system, fined in 1941, the fossil fauna of the DSF (now part of the Ricardo Due to rapid rates of speciation in fossil mammals during Cenozoic Group) was one of four fossil assemblages named as principal correla- time, it is possible to construct detailed biostratigraphic histories that often tives of the Clarendonian mammal age. Early radiometric work depict complex evolutionary patterns. Terrestrial vertebrates are influ- yielded a maximum age of 10.0 Ma for this fossil assemblage, and by enced by tectonic barriers and local environmental factors, however, and correlation to the Great Plains of the United States, this date was these animals become isolated into regional zoogeographic provincial as- considered representative of Clarendonian time. -
Contributions to Vertebrate Palaeontology in Honour of Yukimitsu Tomida
Historical Biology An International Journal of Paleobiology ISSN: 0891-2963 (Print) 1029-2381 (Online) Journal homepage: http://www.tandfonline.com/loi/ghbi20 Contributions to vertebrate palaeontology in honour of Yukimitsu Tomida Louis L. Jacobs, Lawrence J. Flynn, Yuri Kimura, Yoshitsugu Kobayashi, Xiaoming Wang, Zhuding Qiu, Changzu Jin, Yingqi Zhang, Louis H. Taylor, Naoki Kohno & Alisa J. Winkler To cite this article: Louis L. Jacobs, Lawrence J. Flynn, Yuri Kimura, Yoshitsugu Kobayashi, Xiaoming Wang, Zhuding Qiu, Changzu Jin, Yingqi Zhang, Louis H. Taylor, Naoki Kohno & Alisa J. Winkler (2016) Contributions to vertebrate palaeontology in honour of Yukimitsu Tomida, Historical Biology, 28:1-2, 1-7, DOI: 10.1080/08912963.2015.1049839 To link to this article: http://dx.doi.org/10.1080/08912963.2015.1049839 Published online: 01 Oct 2015. Submit your article to this journal Article views: 124 View related articles View Crossmark data Citing articles: 1 View citing articles Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=ghbi20 Download by: [Australian Catholic University] Date: 19 October 2017, At: 01:00 Historical Biology, 2016 Vol. 28, Nos. 1–2, 1–7, http://dx.doi.org/10.1080/08912963.2015.1049839 EDITORIAL Contributions to vertebrate palaeontology in honour of Yukimitsu Tomida Downloaded by [Australian Catholic University] at 01:00 19 October 2017 q 2015 Taylor & Francis 2 L.L. Jacobs et al. The papers in this volume of Historical Biology, understanding continental drift (Elliot et al. 1970; Colbert organised and guest-edited by Drs Yuri Kimura, 1974). Yuki and his fellow graduate students were able to Lawrence J. -
Belen, Sevilleta Wildlife Refuge, and Northern Socorro Basin
TH FRIENDS OF THE PLEISTOCENE, ROCKY MOUNTAIN-CELL, 45 FIELD CONFERENCE PLIO-PLEISTOCENE STRATIGRAPHY AND GEOMORPHOLOGY OF THE CENTRAL PART OF THE ALBUQUERQUE BASIN OCTOBER 12-14, 2001 SEAN D. CONNELL New Mexico Bureau of Geology and Mineral Resources-Albuquerque Office, New Mexico Institute of Mining and Technology, 2808 Central Ave. SE, Albuquerque, New Mexico 87106 DAVID W. LOVE New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, NM 87801 JOHN D. SORRELL Tribal Hydrologist, Pueblo of Isleta, P.O. Box 1270, Isleta, NM 87022 J. BRUCE J. HARRISON Dept. of Earth and Environmental Sciences, New Mexico Institute of Mining and Technology 801 Leroy Place, Socorro, NM 87801 Open-File Report 454C and D Initial Release: October 11, 2001 New Mexico Bureau of Geology and Mineral Resources New Mexico Institute of Mining and Technology 801 Leroy Place, Socorro, NM 87801 NMBGMR OFR454 C & D INTRODUCTION This field-guide accompanies the 45th annual Rocky Mountain Cell of the Friends of the Pleistocene (FOP), held at Isleta Lakes, New Mexico. The Friends of the Pleistocene is an informal gathering of Quaternary geologists, geomorphologists, and pedologists who meet annually in the field. The field guide has been separated into two parts. Part C (open-file report 454C) contains the three-days of road logs and stop descriptions. Part D (open-file report 454D) contains a collection of mini-papers relevant to field-trip stops. This field guide is a companion to open-file report 454A and 454B, which accompanied a field trip for the annual meeting of the Rocky Mountain/South Central Section of the Geological Society of America, held in Albuquerque in late April.