Overboard in the Mojave: the Field Guide
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Possibilities of Using Silicate Rock Powder: an Overview
GSF-101185; No of Pages 11 Geoscience Frontiers xxx (xxxx) xxx Contents lists available at ScienceDirect Geoscience Frontiers journal homepage: www.elsevier.com/locate/gsf Research Paper Possibilities of using silicate rock powder: An overview Claudete Gindri Ramos a,⁎, James C. Hower c,d, Erika Blanco a, Marcos Leandro Silva Oliveira a,b, Suzi Huff Theodoro e a Department of Civil and Environmental Engineering, Universidad de la Costa, Calle 58 #55-66, Barranquilla, Colombia b Departamento de Ingeniería Civil y Arquitectura, Universidad de Lima, Avenida Javier Prado Este 4600, Santiago de Surco 1503, Peru c Center for Applied Energy Research, University of Kentucky, 2540 Research Park Drive, Lexington, KY 40511, USA d Department of Earth & Environmental Sciences, University of Kentucky, Lexington, KY 40511, USA e Postgraduate Program of Environment and Rural Development (PPG-MADER), Área Universitária, 01, Vila Nossa Senhora de Fátima – Campus UnB, Planaltina, DF, Brazil article info abstract Article history: This study evaluates the on use of crushed rocks (remineralizers) to increase soil fertility levels and which con- Received 15 October 2020 tributed to increase agricultural productivity, recovery of degraded areas, decontamination of water, and carbon Received in revised form 15 February 2021 sequestration. The use of these geological materials is part of the assumptions of rock technology and, indirectly, Accepted 28 February 2021 facilitates the achievement of sustainable development goals related to soil management, climate change, and the Available online xxxx preservation of water resources. Research over the past 50 years on silicate rocks focused on soil fertility manage- Handling editor: Lily Wang ment and agricultural productivity. -
Mammalia, Carnivora) from the Blancan of Florida
THREE NEW PROCYONIDS (MAMMALIA, CARNIVORA) FROM THE BLANCAN OF FLORIDA Laura G. Emmert1,2 and Rachel A. Short1,3 ABSTRACT Fossils of the mammalian family Procyonidae are relatively abundant at many fossil localities in Florida. Analysis of specimens from 16 late Blancan localities from peninsular Florida demonstrate the presence of two species of Procyon and one species of Nasua. Procyon gipsoni sp. nov. is slightly larger than extant Procyon lotor and is distinguished by five dental characters including a lack of a crista between the para- cone and hypocone on the P4, absence of a basin at the lingual intersection of the hypocone and protocone on the P4, and a reduced metaconule on the M1. Procyon megalokolos sp. nov. is significantly larger than extant P. lotor and is characterized primarily by morphology of the postcrania, such as an expanded and posteriorly rotated humeral medial epicondyle, more prominent tibial tuberosity, and more pronounced radioulnar notch. Other than larger size, the dentition of P. megalokolos falls within the range of variation observed in extant P. lotor, suggesting that it may be an early member of the P. lotor lineage. Nasua mast- odonta sp. nov. has a unique accessory cusp on the m1 as well as multiple morphological differences in the dentition and postcrania, such as close appression of the trigonid of the m1 and a less expanded medial epicondyle of the humerus. We also synonymize Procyon rexroadensis, formerly the only known Blancan Procyon species in North America, with P. lotor due to a lack of distinct dental morphological features observed in specimens from its type locality in Kansas. -
The Great American Biotic Interchange: Patterns and Processes Author(S): S
The Great American Biotic Interchange: Patterns and Processes Author(s): S. David Webb Source: Annals of the Missouri Botanical Garden, Vol. 93, No. 2 (Aug., 2006), pp. 245-257 Published by: Missouri Botanical Garden Press Stable URL: http://www.jstor.org/stable/40035724 . Accessed: 08/04/2014 23:14 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Missouri Botanical Garden Press is collaborating with JSTOR to digitize, preserve and extend access to Annals of the Missouri Botanical Garden. http://www.jstor.org This content downloaded from 137.111.226.20 on Tue, 8 Apr 2014 23:14:05 PM All use subject to JSTOR Terms and Conditions THE GREAT AMERICAN BIOTIC S. David Webb2 INTERCHANGE: PATTERNS AND PROCESSES1 Abstract Whenthe Panamanianland bridgewas emplacedabout 2.7 Ma, it triggeredthe GreatAmerican Biotic Interchange(GABI), a major mingling of land mammal faunas between North and South America. Four families of northern immigrants (Procyonidae,Felidae, Tayassuidae,and Camelidae)diversified at moderaterates, while four others, Canidae, Mustelidae, Cervidae, and especially Muridae, evolved explosively. As a consequence, half of living South American genera are descendantsof northernimmigrants. The other major consequence of the interchangewas the conquest of tropical North Americaby immigrantsfrom Amazonia, an episode that justifies the term NeotropicalRealm. -
The Archaeology and Paleoclimate of the Mud Lake Basin, Nye County, Nevada
University of Nevada, Reno Changing Landscapes During the Terminal Pleistocene/Early Holocene: The Archaeology and Paleoclimate of the Mud Lake Basin, Nye County, Nevada A thesis submitted in partial fulfillment of the requirements for the degree of Masters of Arts in Anthropology By Lindsay A. Fenner Dr. Geoffrey M. Smith/Thesis Advisor May, 2011 © by Lindsay A. Fenner 2011 All Rights Reserved THE GRADUATE SCHOOL We recommend that the thesis prepared under our supervision by LINDSAY A. FENNER entitled Changing Landscapes During The Terminal Pleistocene/Early Holocene: The Archaeology And Paleoclimate Of The Mud Lake Basin, Nye County, Nevada be accepted in partial fulfillment of the requirements for the degree of MASTER OF ARTS Geoffrey M. Smith, Ph.D., Advisor Gary Haynes, Ph.D., Committee Member Kenneth D. Adams, Ph.D., Graduate School Representative Marsha H. Read, Ph. D., Associate Dean, Graduate School May, 2011 i ABSTRACT Archaeological investigation along Pleistocene lakeshores is a longstanding and common approach to prehistoric research in the Great Basin. Continuing in this tradition, this thesis considers the archaeological remains present from pluvial Mud Lake, Nye County, Nevada coupled with an examination of paleoclimatic conditions to assess land-use patters during the terminal Pleistocene/early Holocene. Temporally diagnostic lithic assemblages from 44 localities in the Mud Lake basin provide the framework for which environmental proxy records are considered. Overwhelmingly occupied by Prearchaic groups, comprising 76.6% of all diagnostic artifacts present, Mud Lake was intensively utilized right up to its desiccation after the Younger Dryas, estimated at 9,000 radiocarbon years before present. Intermittently occupied through the remainder of the Holocene, different land-use strategies were employed as a result of shifting subsistence resources reacting to an ever changing environment. -
Yucca Mountain Project Area Exists for Quality Data Development in the Vadose Zone Below About 400 Feet
< I Mifflin & Associates 2700 East Sunset Road, SufteInc. C2 Las Vegas, Nevada 89120 PRELIMINARY 7021798-0402 & 3026 FAX: 702/798-6074 ~ADd/tDaeii -00/( YUCCA MOUNTAIN PRO1. A Summary of Technical Support Activities January 1987 to June 1988 By: Mifflin & Associates, Inc. LaS Vegas, Nevada K) Submitted to: .State of Nevada Agency for Nuclear Projects Nuclear Waste Project Office Carson City, Nevada H E C El V E ii MAY 15 1989 NUCLEAR WASTE PROJECt OFFICE May 1989 Volume I 3-4:0 89110o3028905a, WASTE PLDR wM-11PDC 1/1 1 1 TABLE OF CONTENTS I. INTRO DUCTION ............................................................................................................................ page3 AREAS OF EFFORT A. Vadose Zone Drilling Program ............................................................................................. 4 Introduction .............................................................................................................................. 5 Issues ....................................................................................................................................... 7 Appendix A ............................................................................................................................... 9 B. Clim ate Change Program ....................................................................................................... 15 Introduction .............................................................................................................................. 16 Issues ...................................................................................................................................... -
Upper Neogene Stratigraphy and Tectonics of Death Valley — a Review
Earth-Science Reviews 73 (2005) 245–270 www.elsevier.com/locate/earscirev Upper Neogene stratigraphy and tectonics of Death Valley — a review J.R. Knott a,*, A.M. Sarna-Wojcicki b, M.N. Machette c, R.E. Klinger d aDepartment of Geological Sciences, California State University Fullerton, Fullerton, CA 92834, United States bU. S. Geological Survey, MS 975, 345 Middlefield Road, Menlo Park, CA 94025, United States cU. S. Geological Survey, MS 966, Box 25046, Denver, CO 80225-0046, United States dTechnical Service Center, U. S. Bureau of Reclamation, P. O. Box 25007, D-8530, Denver, CO 80225-0007, United States Abstract New tephrochronologic, soil-stratigraphic and radiometric-dating studies over the last 10 years have generated a robust numerical stratigraphy for Upper Neogene sedimentary deposits throughout Death Valley. Critical to this improved stratigraphy are correlated or radiometrically-dated tephra beds and tuffs that range in age from N3.58 Ma to b1.1 ka. These tephra beds and tuffs establish relations among the Upper Pliocene to Middle Pleistocene sedimentary deposits at Furnace Creek basin, Nova basin, Ubehebe–Lake Rogers basin, Copper Canyon, Artists Drive, Kit Fox Hills, and Confidence Hills. New geologic formations have been described in the Confidence Hills and at Mormon Point. This new geochronology also establishes maximum and minimum ages for Quaternary alluvial fans and Lake Manly deposits. Facies associated with the tephra beds show that ~3.3 Ma the Furnace Creek basin was a northwest–southeast-trending lake flanked by alluvial fans. This paleolake extended from the Furnace Creek to Ubehebe. Based on the new stratigraphy, the Death Valley fault system can be divided into four main fault zones: the dextral, Quaternary-age Northern Death Valley fault zone; the dextral, pre-Quaternary Furnace Creek fault zone; the oblique–normal Black Mountains fault zone; and the dextral Southern Death Valley fault zone. -
A World Revealed by Language: a New Seri Dictionary and Unapologetic Speculations on Seri Indian Deep History
A World Revealed by Language: A New Seri Dictionary and Unapologetic Speculations on Seri Indian Deep History JIM HILLS AND DAVID YETMAN Comcáac quih Yaza quih Hant Ihíip hac: Diccionario Seri-Español- Ingles, compiled by Mary Beck Moser and Stephen A. Marlett. Illustrated by Cathy Moser Marlett. Published by Plaza y Valdés Editores, Mexico City. 947 pages. ISBN: 970–722–453–3. The philosopher Ludwig Wittgenstein once mentioned that to imagine a language was to imagine a form of life (Wittgenstein 1953: 19). A comprehensive dictionary of any language exemplifies Wittgenstein’s point, but none more than the trilingual dictionary of the Seri language compiled by Mary Beck Moser and Steven Marlett. The work represents more than fifty years of research and over thirty years of living with the Seris in El Desemboque, Sonora, Mexico, in connection with the Summer Institute of Linguistics of the Wycliffe Bible Translators. The entries are in Seri, Spanish, and English, making the work of value to speakers of all three languages. The roughly six hundred Seris are already using the dictionary. Outsiders visiting them would be well advised to use it as well. The authors included Seri consultants at every step of the compilation. Seris reviewed the entries, suggesting changes and additions. Part of the dictionary’s usefulness lies in its incorporation not merely of single-word or phrase translations, but also of sentences or short paragraphs typically generated by Seris. This is critically important, since meanings are frequently so complex that a simple word-by-word translation simply will not do. As Moser and Marlett have realized, JIM HILLS is a longtime Seri hand and trader in Tucson, Arizona. -
Isobases of the Algonquin and Iroquois Beaches, and Their Significance1
BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA VOL. 21, PP. 227-248, PL. 5 JUNE 10, 1910 ISOBASES OF THE ALGONQUIN AND IROQUOIS BEACHES, AND THEIR SIGNIFICANCE1 BY JAMES WALTER GOl.DTHWAIT (Read before the Society December 28, 1909) CONTENTS Page Introduction ............................................................................................................... 227 The Algonquin w ater-p lan e.................................................................................... 229 Stage recorded by the Algonquin beach.......................................................229 Isobases of the upwarped portion of the Algonquin plane...................... 233 The horizontal portion of the Algonquin plane.......................................... 236 The “hinge line” or “isobase of zero” ............................................................ 239 The Algonquin plane as a datum plane........................................................ 240 The Iroquois w ater-plane........................................................................................ 241 Relative ages of the Iroquois beach and the Algonquin beach..............241 Isobases of the Iroquois plane........................................................................ 242 Comparison of the two water-planes.................................................................... 243 The isobases and the pre-Cambrian boundary.................................................... 245 Summary .................................................................................................................... -
UNIVERSITY of CALIFORNIA Los Angeles Southern California
UNIVERSITY OF CALIFORNIA Los Angeles Southern California Climate and Vegetation Over the Past 125,000 Years from Lake Sequences in the San Bernardino Mountains A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Geography by Katherine Colby Glover 2016 © Copyright by Katherine Colby Glover 2016 ABSTRACT OF THE DISSERTATION Southern California Climate and Vegetation Over the Past 125,000 Years from Lake Sequences in the San Bernardino Mountains by Katherine Colby Glover Doctor of Philosophy in Geography University of California, Los Angeles, 2016 Professor Glen Michael MacDonald, Chair Long sediment records from offshore and terrestrial basins in California show a history of vegetation and climatic change since the last interglacial (130,000 years BP). Vegetation sensitive to temperature and hydroclimatic change tended to be basin-specific, though the expansion of shrubs and herbs universally signalled arid conditions, and landscpe conversion to steppe. Multi-proxy analyses were conducted on two cores from the Big Bear Valley in the San Bernardino Mountains to reconstruct a 125,000-year history for alpine southern California, at the transition between mediterranean alpine forest and Mojave desert. Age control was based upon radiocarbon and luminescence dating. Loss-on-ignition, magnetic susceptibility, grain size, x-ray fluorescence, pollen, biogenic silica, and charcoal analyses showed that the paleoclimate of the San Bernardino Mountains was highly subject to globally pervasive forcing mechanisms that register in northern hemispheric oceans. Primary productivity in Baldwin Lake during most of its ii history showed a strong correlation to historic fluctuations in local summer solar radiation values. -
Spatially-Explicit Modeling of Modern and Pleistocene Runoff and Lake Extent in the Great Basin Region, Western United States
Spatially-explicit modeling of modern and Pleistocene runoff and lake extent in the Great Basin region, western United States Yo Matsubara1 Alan D. Howard1 1Department of Environmental Sciences University of Virginia P.O. Box 400123 Charlottesville, VA 22904-4123 Abstract A spatially-explicit hydrological model balancing yearly precipitation and evaporation is applied to the Great Basin Region of the southwestern United States to predict runoff magnitude and lake distribution during present and Pleistocene climatic conditions. The model iteratively routes runoff through, and evaporation from, depressions to find a steady state solution. The model is calibrated with spatially-explicit annual precipitation estimates and compiled data on pan evaporation, mean annual temperature, and total yearly runoff from stations. The predicted lake distribution provides a close match to present-day lakes. For the last glacial maximum the sizes of lakes Bonneville and Lahontan were well predicted by linear combinations of decrease in mean annual temperature from 0 to 6 °C and increases in precipitation from 0.8 to 1.9 times modern values. Estimated runoff depths were about 1.2 to 4.0 times the present values and yearly evaporation about 0.3 to 1 times modern values. 2 1. Introduction The Great Basin of the southwestern United States in the Basin and Range physiographic province contains enclosed basins featuring perennial and ephemeral lakes, playas and salt pans (Fig. 1). The Great Basin consists of the entire state of Nevada, western Utah, and portions of California, Idaho, Oregon, and Wyoming. At present it supports an extremely dry, desert environment; however, about 40 lakes (some reaching the size of present day Great Lakes) episodically occupied the Great Basin, most recently during the last glacial maximum (LGM) [Snyder and Langbein, 1962; Hostetler et al., 1994; Madsen et al., 2001]. -
Open-File/Color For
Questions about Lake Manly’s age, extent, and source Michael N. Machette, Ralph E. Klinger, and Jeffrey R. Knott ABSTRACT extent to form more than a shallow n this paper, we grapple with the timing of Lake Manly, an inconstant lake. A search for traces of any ancient lake that inundated Death Valley in the Pleistocene upper lines [shorelines] around the slopes Iepoch. The pluvial lake(s) of Death Valley are known col- leading into Death Valley has failed to lectively as Lake Manly (Hooke, 1999), just as the term Lake reveal evidence that any considerable lake Bonneville is used for the recurring deep-water Pleistocene lake has ever existed there.” (Gale, 1914, p. in northern Utah. As with other closed basins in the western 401, as cited in Hunt and Mabey, 1966, U.S., Death Valley may have been occupied by a shallow to p. A69.) deep lake during marine oxygen-isotope stages II (Tioga glacia- So, almost 20 years after Russell’s inference of tion), IV (Tenaya glaciation), and/or VI (Tahoe glaciation), as a lake in Death Valley, the pot was just start- well as other times earlier in the Quaternary. Geomorphic ing to simmer. C arguments and uranium-series disequilibrium dating of lacus- trine tufas suggest that most prominent high-level features of RECOGNITION AND NAMING OF Lake Manly, such as shorelines, strandlines, spits, bars, and tufa LAKE MANLY H deposits, are related to marine oxygen-isotope stage VI (OIS6, In 1924, Levi Noble—who would go on to 128-180 ka), whereas other geomorphic arguments and limited have a long and distinguished career in Death radiocarbon and luminescence age determinations suggest a Valley—discovered the first evidence for a younger lake phase (OIS 2 or 4). -
Harper Valley Groundwater Basin Bulletin 118
South Lahontan Hydrologic Region California’s Groundwater Harper Valley Groundwater Basin Bulletin 118 Harper Valley Groundwater Basin • Groundwater Basin Number: 6-47 • County: Kern, San Bernardino • Surface Area: 410,000 acres (640 square miles) Basin Boundaries and Hydrology This groundwater basin underlies Harper Valley in western San Bernardino and eastern Kern Counties of the central Mojave Desert. This basin is bounded on the east by nonwater-bearing rocks of Fremont Peak, Black Mountain, the Gravel Hills, and the Mud Hills. The basin is bounded on the west by a combination of surface drainage divides, portions of the Harper, Kramer Hills and Lockhart faults, and nonwater-bearing rocks of the Kramer Hills and other low-lying basement hills. The basin is bounded on the south by nonwater-bearing rocks of Mount General, Iron Mountain, and the Waterman Hills, and by subsurface drainage patterns. The basin is bounded on the north by nonwater-bearing rocks of the Rand Mountains (DWR 1964; Jennings and others 1962; Rogers 1967) Harper Valley is drained by numerous ephemeral streams towards Harper (dry) Lake (Jennings and others 1962; Rogers 1967). Floodwater from Grass Valley occasionally flows into Harper Valley via Black Canyon on the eastern side of the valley (DWR 1964). Average annual precipitation is about 5 inches and ranges from about 3 to 7 inches. Hydrogeologic Information Water Bearing Formations Quaternary lacustrine and alluvial deposits, including unconsolidated younger alluvial fan material and unconsolidated to semi-consolidated older alluvium, can be water-bearing within the basin. The younger alluvium generally lies above the groundwater surface; whereas, the older alluvium extends beneath the groundwater table (DWR 1971).