A History of Gila Monster (Heloderma Suspectum Cinctum) Records from California with Comments on Factors Affecting Their Distribution Jeffrey E
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Mammals of the California Desert
MAMMALS OF THE CALIFORNIA DESERT William F. Laudenslayer, Jr. Karen Boyer Buckingham Theodore A. Rado INTRODUCTION I ,+! The desert lands of southern California (Figure 1) support a rich variety of wildlife, of which mammals comprise an important element. Of the 19 living orders of mammals known in the world i- *- loday, nine are represented in the California desert15. Ninety-seven mammal species are known to t ':i he in this area. The southwestern United States has a larger number of mammal subspecies than my other continental area of comparable size (Hall 1981). This high degree of subspeciation, which f I;, ; leads to the development of new species, seems to be due to the great variation in topography, , , elevation, temperature, soils, and isolation caused by natural barriers. The order Rodentia may be k., 2:' , considered the most successful of the mammalian taxa in the desert; it is represented by 48 species Lc - occupying a wide variety of habitats. Bats comprise the second largest contingent of species. Of the 97 mammal species, 48 are found throughout the desert; the remaining 49 occur peripherally, with many restricted to the bordering mountain ranges or the Colorado River Valley. Four of the 97 I ?$ are non-native, having been introduced into the California desert. These are the Virginia opossum, ' >% Rocky Mountain mule deer, horse, and burro. Table 1 lists the desert mammals and their range 1 ;>?-axurrence as well as their current status of endangerment as determined by the U.S. fish and $' Wildlife Service (USWS 1989, 1990) and the California Department of Fish and Game (Calif. -
California Vegetation Map in Support of the DRECP
CALIFORNIA VEGETATION MAP IN SUPPORT OF THE DESERT RENEWABLE ENERGY CONSERVATION PLAN (2014-2016 ADDITIONS) John Menke, Edward Reyes, Anne Hepburn, Deborah Johnson, and Janet Reyes Aerial Information Systems, Inc. Prepared for the California Department of Fish and Wildlife Renewable Energy Program and the California Energy Commission Final Report May 2016 Prepared by: Primary Authors John Menke Edward Reyes Anne Hepburn Deborah Johnson Janet Reyes Report Graphics Ben Johnson Cover Page Photo Credits: Joshua Tree: John Fulton Blue Palo Verde: Ed Reyes Mojave Yucca: John Fulton Kingston Range, Pinyon: Arin Glass Aerial Information Systems, Inc. 112 First Street Redlands, CA 92373 (909) 793-9493 [email protected] in collaboration with California Department of Fish and Wildlife Vegetation Classification and Mapping Program 1807 13th Street, Suite 202 Sacramento, CA 95811 and California Native Plant Society 2707 K Street, Suite 1 Sacramento, CA 95816 i ACKNOWLEDGEMENTS Funding for this project was provided by: California Energy Commission US Bureau of Land Management California Wildlife Conservation Board California Department of Fish and Wildlife Personnel involved in developing the methodology and implementing this project included: Aerial Information Systems: Lisa Cotterman, Mark Fox, John Fulton, Arin Glass, Anne Hepburn, Ben Johnson, Debbie Johnson, John Menke, Lisa Morse, Mike Nelson, Ed Reyes, Janet Reyes, Patrick Yiu California Department of Fish and Wildlife: Diana Hickson, Todd Keeler‐Wolf, Anne Klein, Aicha Ougzin, Rosalie Yacoub California -
Use of Radiocarbon Ages to Narrow Groundwater Recharge Estimates in the Southeastern Mojave Desert, USA
hydrology Article Use of Radiocarbon Ages to Narrow Groundwater Recharge Estimates in the Southeastern Mojave Desert, USA Adam H. Love 1,* and Andy Zdon 2 1 Roux Associates, Inc., 555 12th Street, Suite 250, Oakland, CA 95607, USA 2 Partner Engineering and Science, Inc., 1761 E. Garry Avenue, Santa Ana, CA 92705, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-415-697-6200 Received: 2 August 2018; Accepted: 10 September 2018; Published: 13 September 2018 Abstract: Estimating groundwater recharge in arid or semiarid regions can be a difficult and complex task, since it is dependent on a highly variable set of spatial and temporal hydrologic parameters and processes that are dependent on the local climate, the land surface properties, and subsurface characteristics. As a result, traditional methods for estimating the recharge can result in a wide range of derived values. This is evident in the southeastern Mojave Desert, where calculated recharge estimates by previous investigators that range over an order of magnitude (from ~2500 to ~37,000 acre feet per year) are reported. To narrow down this large span of recharge estimates to narrower and more plausible values, this study evaluates the previous recharge estimates in this region, to examine the sources of variability in the reported results and to constrain the recharge estimates based on the hydrologic conditions and the radiocarbon age-dating of spring flows—even without knowledge of the precise subsurface hydrology. The groundwater age and perennial flow characteristics of springs in this study could not be derived from waters sourced solely from local recharge. -
Life History of the Coppertail Skink (Ctenotus Taeniolatus) in Southeastern Australia
Herpetological Conservation and Biology 15(2):409–415. Submitted: 11 February 2020; Accepted: 19 May 2020; Published: 31 August 2020. LIFE HISTORY OF THE COPPERTAIL SKINK (CTENOTUS TAENIOLATUS) IN SOUTHEASTERN AUSTRALIA DAVID A. PIKE1,2,6, ELIZABETH A. ROZNIK3, JONATHAN K. WEBB4, AND RICHARD SHINE1,5 1School of Biological Sciences A08, University of Sydney, New South Wales 2006, Australia 2Present address: Department of Biology, Rhodes College, Memphis, Tennessee 38112, USA 3Department of Conservation and Research, Memphis Zoo, Memphis, Tennessee 38112, USA 4School of Life Sciences, University of Technology Sydney, Broadway, New South Wales 2007, Australia 5Present address: Department of Biological Sciences, Macquarie University, New South Wales 2109, Australia 6Corresponding author, e-mail: [email protected] Abstract.—The global decline of reptiles is a serious problem, but we still know little about the life histories of most species, making it difficult to predict which species are most vulnerable to environmental change and why they may be vulnerable. Life history can help dictate resilience in the face of decline, and therefore understanding attributes such as sexual size dimorphism, site fidelity, and survival rates are essential. Australia is well-known for its diversity of scincid lizards, but we have little detailed knowledge of the life histories of individual scincid species. To examine the life history of the Coppertail Skink (Ctenotus taeniolatus), which uses scattered surface rocks as shelter, we estimated survival rates, growth rates, and age at maturity during a three-year capture-mark- recapture study. We captured mostly females (> 84%), and of individuals captured more than once, we captured 54.3% at least twice beneath the same rock, and of those, 64% were always beneath the same rock (up to five captures). -
Multi-National Conservation of Alligator Lizards
MULTI-NATIONAL CONSERVATION OF ALLIGATOR LIZARDS: APPLIED SOCIOECOLOGICAL LESSONS FROM A FLAGSHIP GROUP by ADAM G. CLAUSE (Under the Direction of John Maerz) ABSTRACT The Anthropocene is defined by unprecedented human influence on the biosphere. Integrative conservation recognizes this inextricable coupling of human and natural systems, and mobilizes multiple epistemologies to seek equitable, enduring solutions to complex socioecological issues. Although a central motivation of global conservation practice is to protect at-risk species, such organisms may be the subject of competing social perspectives that can impede robust interventions. Furthermore, imperiled species are often chronically understudied, which prevents the immediate application of data-driven quantitative modeling approaches in conservation decision making. Instead, real-world management goals are regularly prioritized on the basis of expert opinion. Here, I explore how an organismal natural history perspective, when grounded in a critique of established human judgements, can help resolve socioecological conflicts and contextualize perceived threats related to threatened species conservation and policy development. To achieve this, I leverage a multi-national system anchored by a diverse, enigmatic, and often endangered New World clade: alligator lizards. Using a threat analysis and status assessment, I show that one recent petition to list a California alligator lizard, Elgaria panamintina, under the US Endangered Species Act often contradicts the best available science. -
Providence Mountains State Recreation Area 38200 Essex Road Or P.O
Our Mission Providence The mission of California State Parks is to provide for the health, inspiration and In the middle of the education of the people of California by helping Mountains to preserve the state’s extraordinary biological Mojave Desert, Jack and diversity, protecting its most valued natural and State Recreation Area cultural resources, and creating opportunities Ida Mitchell shared with for high-quality outdoor recreation. thousands of fortunate visitors the cool beauty of the caverns’ magnificent “draperies” and “coral California State Parks supports equal access. pipes” formations. Prior to arrival, visitors with disabilities who need assistance should contact the park at (760) 928-2586. If you need this publication in an alternate format, contact [email protected]. CALIFORNIA STATE PARKS P.O. Box 942896 Sacramento, CA 94296-0001 For information call: (800) 777-0369 (916) 653-6995, outside the U.S. 711, TTY relay service www.parks.ca.gov Providence Mountains State Recreation Area 38200 Essex Road or P.O. Box 1 Essex, CA 92332 • (760) 928-2586 © 2010 California State Parks (Rev. 2017) V isitors to Providence Mountains State that left abundant shell-covered organisms Recreation Area are greeted by the sight on the sea floor. of jagged slopes of gray limestone, topped The shells and plant materials that settled by volcanic peaks of red rhyolite. Located on the sea bottom eventually became on the eastern slope of the Providence limestone. As the restless land heaved Mountains Range, the park lies within the upward, these formations were pushed boundaries of the 1.6-million acre Mojave above the level of the former ocean bed. -
The Imperial Valley Is Located About 150 Miles Southeast of Los Angeles
The Imperial Valley is located about 150 miles southeast of Los Angeles. It is a section of a much larger geologic structure -- the Salton Trough -- which is about 1,000 miles in length. The structure extends from San Gorgonio Pass southeast to the Mexican border, including the Gulf of California and beyond the tip of the Baja California Peninsula. The surrounding mountains are largely faulted blocks of the Southern California batholith of Mesozoic age, overlain by fragments of an earlier metamorphic complex. The valley basin consists of a sedimentary fill of sands and gravels ranging up to 15,000 feet in thickness. The layers slope gently down-valley, and contain several important aquifers. The valley is laced with major members of the San Andreas Fault system. Minor to moderate earthquake events are common, but severe shocks have not been experienced in recorded history. The entire trough, including the Gulf is an extension of the East Pacific Rise, a zone of separation in Earth's crust. Deep sea submergence instruments have observed many phenomena of crustal formation. The axis of the Rise, hence of the Salton Valley as well, is a great transform fault that is having the effect of separating an enormous slab of North America, consisting of the Baja Peninsula and coastal California away from the mainland, with movement to the northwest and out to sea as a terranne. Table of Contents Chapter 1 The San Jacinto and Santa Rosa Mountains Chapter 2 The Eastern Mountains Chapter 3 San Gorgonio Pass Chapter 4 The Hills Chapter 5 Desert Sand -
Birds of the California Desert
BIRDS OF THE CALIFORNIA DESERT A. Sidney England and William F. Laudenslayer, Jr. i INTRODUCTION i \ 1 The term, "California desert", as used herein, refers to a politically defined region, most of i which is included in the California Desert Conservation Area (CDCA) designated by the Federal Land ; and Management Act of 1976 (FLPMA). Of the 25 million acres in the CDCA, about one-half are i public lands, most of which are managed by the Bureau of Land Management (BLM) according to the "980 P California Desert Conservation Area Plan mandated by FLPMA. The California desert encompasses those portions of the Great Basin Desert (east of the White and lnyo Mountains and A south of the California-Nevada border), the Mojave Desert, and the Colorado Desert which occur " within California; it does not include areas of riparian, aquatic, urban, and agricultural habitats . adjacent to the Colorado River. (Also see chapters on Geology by Norris and Bioclimatology by E3irdsI4 are the most conspicuous vertebrates found in the California deserts. Records exist for at least 425 species (Garrett and Dunn 1981) from 18 orders and 55 families. These counts far exceed those for mammals, reptiles, amphibians and fish, and they are similar to totals for the entire state -- 542 species from 20 orders and 65 families (Laudenslayer and Grenfell 1983). These figures may seem surprisingly similar considering the harsh, arid climates often believed characteristic of I desert environments. However, habiiats found in the California desert range from open water and h marshes at the Salton Sea to pinyon-juniper woodland and limber pinelbristlecone pine forests on a few mountain ranges. -
Understanding the Source of Water for Selected Springs Within Mojave Trails National Monument, California
ENVIRONMENTAL FORENSICS, 2018 VOL. 19, NO. 2, 99–111 https://doi.org/10.1080/15275922.2018.1448909 Understanding the source of water for selected springs within Mojave Trails National Monument, California Andy Zdon, PG, CHg, CEGa, M. Lee Davisson, PGb and Adam H. Love, Ph.D.c aTechnical Director – Water Resources, PARTNER ENGINEERING AND SCIENCE, INC., Santa Ana, CA, Sacramento, CA; bML Davisson & Associates, Inc., Livermore, CA; cVice President/Principal Scientist, Roux Associates, Inc., Oakland, CA ABSTRACT KEYWORDS While water sources that sustain many of the springs in the Mojave Desert have been poorly Water resources; clipper understood, the desert ecosystem can be highly dependent on such resources. This evaluation mountains; bonanza spring; updates the water resource forensics of Bonanza Spring, the largest spring in the southeastern groundwater; forensics; Mojave Desert. The source of spring flow at Bonanza Spring was evaluated through an integration isotopes of published geologic maps, measured groundwater levels, water quality chemistry, and isotope data compiled from both published sources and new samples collected for water chemistry and isotopic composition. The results indicate that Bonanza Spring has a regional water source, in hydraulic communication with basin fill aquifer systems. Neighboring Lower Bonanza Spring appears to primarily be a downstream manifestation of surfacing water originally discharged from the Bonanza Spring source. Whereas other springs in the area, Hummingbird, Chuckwalla, and Teresa Springs, each appear to be locally sourced as “perched” springs. These conclusions have important implications for managing activities that have the potential to impact the desert ecosystem. Introduction above Bonanza Spring. Identification of future impacts General information and data regarding springs in the from water resource utilization becomes problematic if Mojave Desert are sparse, and many of these springs are initial baseline conditions are unknown or poorly under- not well understood. -
Prolonged Poststrike Elevation in Tongue-Flicking Rate with Rapid Onset in Gila Monster, <Emphasis Type="Italic">
Journal of Chemical Ecology, Vol. 20. No. 11, 1994 PROLONGED POSTSTRIKE ELEVATION IN TONGUE- FLICKING RATE WITH RAPID ONSET IN GILA MONSTER, Heloderma suspectum: RELATION TO DIET AND FORAGING AND IMPLICATIONS FOR EVOLUTION OF CHEMOSENSORY SEARCHING WILLIAM E. COOPER, JR. I'* CHRISTOPHER S. DEPERNO I and JOHNNY ARNETT 2 ~Department of Biology Indiana University-Purdue University Fort Wayne Fort Wayne. bldiana 46805 2Department of Herpetology Cincinnati Zoo and Botanical Garden Cincinnati, Ohio 45220 (Received May 6, 1994; accepted June 27, 1994) Abstract--Experimental tests showed that poststrike elevation in tongue-flick- ing rate (PETF) and strike-induced chemosensory searching (SICS) in the gila monster last longer than reported for any other lizard. Based on analysis of numbers of tongue-flicks emitted in 5-rain intervals, significant PETF was detected in all intervals up to and including minutes 41~-5. Using 10-rain intervals, PETF lasted though minutes 46-55. Two of eight individuals con- tinued tongue-flicking throughout the 60 rain after biting prey, whereas all individuals ceased tongue-flicking in a control condition after minute 35. The apparent presence of PETF lasting at least an hour in some individuals sug- gests that there may be important individual differences in duration of PETF. PETF and/or SICS are present in all families of autarchoglossan lizards stud- ied except Cordylidae, the only family lacking lingually mediated prey chem- ical discrimination. However, its duration is known to be greater than 2-rain only in Helodermatidae and Varanidae, the living representatives of Vara- noidea_ That prolonged PETF and S1CS are typical of snakes provides another character supporting a possible a varanoid ancestry for Serpentes. -
Lanfair Valley Groundwater Basin Bulletin 118
Hydrologic Region Colorado River California’s Groundwater Lanfair Valley Groundwater Basin Bulletin 118 Lanfair Valley Groundwater Basin • Groundwater Basin Number: 7-1 • County: San Bernardino • Surface Area: 157,000 acres (245 square miles) Basin Boundaries and Hydrology This basin underlies Lanfair Valley in eastern San Bernardino County. The valley slopes southeasterly with valley floor elevations ranging from 3,500 to 5,000 feet above sea level. The basin is bounded by impermeable rocks of the New York and Castle Mountains on the north, of the Piute Range on the east, of the Hackberry Mountain on the south, and of the Providence Mountains and Mid Hills on the west. Caruthers Creek flows intermittently southeastward during periods of heavy precipitation. Piute Spring discharges groundwater from Lanfair Valley to an adjacent valley and other smaller springs are found throughout the valley. Average annual precipitation ranges from 7 to 10 inches. Hydrogeologic Description Water Bearing Formations The primary water-bearing formations are Quaternary and Tertiary age unconsolidated deposits that include highly indurated sand, silt, clay and gravel. The maximum thickness of these deposits is not known; however, a boring log indicates a thickness of at least 550 feet locally. Wells in these deposits yield about 3 to 70 gpm (Friewald 1984). Restrictive Structures The Cedar Canyon fault crosses the northwest portion of the basin; however, it is unknown whether or not this fault is a barrier to groundwater. Recharge Areas The principal sources of recharge are likely percolation of runoff from surrounding mountains, percolation of precipitation to the valley floor, and subsurface inflow from adjacent basins. -
Fabuleux Parcs De La Californie: Déserts, Montagnes Et
Index Les numéros en bleu renvoient aux cartes. Le texte en vert renvoie aux parcs et réserves. A D Abbots Lagoon Trail 40 Dante’s View 17 Ahwahnee, The 28 Dead Giant 30 Alcatraz, île d’ 37 Death Valley National Park 14, 15 Arbres de Josué 13 Death Valley Scotty 14 Artist’s Palette 18 Del Norte Coast Redwoods Auto Log 24 State Park 41 Avenue of the Giants 41 Devastated Area 43 Drake Beach 39 B Badwater Basin 17 E Balconies Cave 35 Earthquake Trail 39 Barker Dam 8 El Capitan 30 Bear Gulch Cave 35 Elephant Seal Overlook 40 Big Tree Wayside Walk 42 Emerald Bay State Park 43 Borax Museum 16 Enderts Beach Road 42 Bridalveil Fall 30 F C Faille de San Andreas 39 California Tunnel Tree 32 Five Brooks Ranch 40 Californie 4, 5 Furnace Creek 16 Channel Islands National Marine Sanctuary 33 G Channel Islands National Park 33 Channel Islands National Park Visitor General Grant Tree 26 Center 35 General Sherman Tree 24 Chimney Rock 39 Geology Tour Road 7 Cholla Cactus Garden 7 Giant Forest 24 Cima Dome 13 Giant Forest Museum 24 Cinder Cones 10 Glacier Point 30 Coast Trail 40 Golden Gate National Cottonwood Spring 7 Recreation Area 37 Crystal Cave 24 Grizzly Giant 32 http://www.guidesulysse.com/catalogue/FicheProduit.aspx?isbn=9782765875406 H Lower Yosemite Fall Trail 28 Half Dome 30 Happy Isles 31 M Happy Isles Nature Center 31 Marin Headlands 37 Hetch Hetchy Valley 32 Mariposa Grove 32 Hidden Valley 8 Mesquite Flat Sand Dunes 18 High Peaks 35 Miner’s Ridge Trail 42 Historic Stovepipe Well 18 Mist Trail 31 Hole-in-the-Wall 11 Mitchell Caverns 13 Hospital Rock 24 Mojave National Preserve 8, 9 Humboldt Redwoods State Park 40 Moro Rock 24 Moro Rock/Crescent Meadow Road 24 I Mosaic Canyon 18 Mount Tamalpais State Park 38 Indian Beach Loop 40 Mount Vision Road 40 Inn at Death Valley 16 Muir Beach 38 Muir Beach Overlook 38 J Muir, John 32 Jedediah Smith Redwoods Muir Woods National Monument 38 State Park 41 John Muir 32 N Joshua Tree National Park 6 Nation’s Christmas Tree Ceremony 26 Jumbo Rocks 7 Newton B.