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Update on the Birds of Isla Guadalupe, Baja California
UPDATE ON THE BIRDS OF ISLA GUADALUPE, BAJA CALIFORNIA LORENZO QUINTANA-BARRIOS and GORGONIO RUIZ-CAMPOS, Facultad de Ciencias, Universidad Autónoma de Baja California, Apartado Postal 1653, Ense- nada, Baja California, 22800, México (U. S. mailing address: PMB 064, P. O. Box 189003, Coronado, California 92178-9003; [email protected] PHILIP UNITT, San Diego Natural History Museum, P. O. Box 121390, San Diego, California 92112-1390; [email protected] RICHARD A. ERICKSON, LSA Associates, 20 Executive Park, Suite 200, Irvine, California 92614; [email protected] ABSTRACT: We report 56 bird specimens of 31 species taken on Isla Guadalupe, Baja California, between 1986 and 2004 and housed at the Colección Ornitológica del Laboratorio de Vertebrados de la Facultad de Ciencias, Universidad Autónoma de Baja California, Ensenada, along with other sight and specimen records. The speci- mens include the first published Guadalupe records for 10 species: the Ring-necked Duck (Aythya collaris), Long-billed Curlew (Numenius americanus), Bonaparte’s Gull (Larus philadelphia), Ash-throated Flycatcher (Myiarchus cinerascens), Warbling Vireo (Vireo gilvus), Tree Swallow (Tachycineta bicolor), Yellow Warbler (Dendroica petechia), Magnolia Warbler (Dendroica magnolia), Yellow-headed Blackbird (Xan- thocephalus xanthocephalus), and Orchard Oriole (Icterus spurius). A specimen of the eastern subspecies of Brown-headed Cowbird (Molothrus ater ater) and a sight record of the Gray-cheeked Thrush (Catharus minimus) are the first reported from the Baja California Peninsula (and islands). A photographed Franklin’s Gull (Larus pipixcan) is also an island first. Currently 136 native species and three species intro- duced in North America have been recorded from the island and nearby waters. -
UNIVERSITY of CALIFORNIA, SAN DIEGO Phainopepla Nestlings
UNIVERSITY OF CALIFORNIA, SAN DIEGO Phainopepla nestlings adjust begging behaviors to different male and female parental provisioning rules A thesis submitted in partial satisfaction of the requirements for the Master of Science degree in Biology by Jeanne Marie Messier Committee in charge: Professor Sandra L. Vehrencamp, Chair Professor David S. Woodruff Professor Joshua R. Kohn Professor Trevor D. Price 2000 The Thesis of Jeanne Marie Messier is approved, and it is acceptable in quality and form for publication on microfilm and electronically: __________________________________________________________ __________________________________________________________ __________________________________________________________ __________________________________________________________ Chair University of California, San Diego 2000 iii DEDICATION This Thesis is dedicated to Anne and John Messier, in memory of their daughter Jeanne. iv TABLE OF CONTENTS Signature page........................................................................................................ iii Dedication.............................................................................................................. iv Table of Contents................................................................................................... v List of Figures........................................................................................................ vi List of Tables........................................................................................................ -
Black Mountains Area (Hydrographic Basin 13-215)
STATE OF NEVADA DEPARTMENT OF CONSERVATION AND NATURAL RESOURCES DIVISION OF WATER RESOURCES JASON KING, P.E. STATE ENGINEER BLACK MOUNTAINS AREA (HYDROGRAPHIC BASIN 13-215) GROUNDWATER PUMPAGE INVENTORY CALENDAR YEAR 2014 Field Investigated by: John Guillory, P.E. Report Prepared by: John Guillory, P.E. TABLE OF CONTENTS ABSTRACT ................................................................................................................................... 1 HYDROGRAPHIC BASIN SUMMARY ................................................................................... 2 PURPOSE AND SCOPE .............................................................................................................. 3 DESCRIPTION OF THE STUDY AREA .................................................................................. 3 GROUNDWATER LEVELS ....................................................................................................... 3 FIGURE 1. PHYSIOGRAPHIC MAP OF BLACK MOUNTAINS AREA, HYDROGRAPHIC BASIN 13-215. ..................................................................................................................................... 4 METHODS TO ESTIMATE PUMPAGE .................................................................................. 5 PUMPAGE BY MANNER OF USE ........................................................................................... 6 APPENDIX A. BLACK MOUNTAINS AREA HISTORICAL PUMPAGE. ......................... 7 APPENDIX B. BLACK MOUNTAINS AREA GROUNDWATER PUMPAGE FOR CALENDAR YEAR 2014 BY MANNER -
Utah Geological Association Publication 30.Pub
Utah Geological Association Publication 30 - Pacific Section American Association of Petroleum Geologists Publication GB78 239 CENOZOIC EVOLUTION OF THE NORTHERN COLORADO RIVER EXTEN- SIONAL CORRIDOR, SOUTHERN NEVADA AND NORTHWEST ARIZONA JAMES E. FAULDS1, DANIEL L. FEUERBACH2*, CALVIN F. MILLER3, 4 AND EUGENE I. SMITH 1Nevada Bureau of Mines and Geology, University of Nevada, Mail Stop 178, Reno, NV 89557 2Department of Geology, University of Iowa, Iowa City, IA 52242 *Now at Exxon Mobil Development Company, 16825 Northchase Drive, Houston, TX 77060 3Department of Geology, Vanderbilt University, Nashville, TN 37235 4Department of Geoscience, University of Nevada, Las Vegas, NV 89154 ABSTRACT The northern Colorado River extensional corridor is a 70- to 100-km-wide region of moderately to highly extended crust along the eastern margin of the Basin and Range province in southern Nevada and northwestern Arizona. It has occupied a criti- cal structural position in the western Cordillera since Mesozoic time. In the Cretaceous through early Tertiary, it stood just east and north of major fold and thrust belts and also marked the northern end of a broad, gently (~15o) north-plunging uplift (Kingman arch) that extended southeastward through much of central Arizona. Mesozoic and Paleozoic strata were stripped from the arch by northeast-flowing streams. Peraluminous 65 to 73 Ma granites were emplaced at depths of at least 10 km and exposed in the core of the arch by earliest Miocene time. Calc-alkaline magmatism swept northward through the northern Colorado River extensional corridor during early to middle Miocene time, beginning at ~22 Ma in the south and ~12 Ma in the north. -
Biological Resources and Management
Vermilion flycatcher The upper Muddy River is considered one of the Mojave’s most important Common buckeye on sunflower areas of biodiversity and regionally Coyote (Canis latrans) Damselfly (Enallagma sp.) (Junonia coenia on Helianthus annuus) important ecological but threatened riparian landscapes (Provencher et al. 2005). Not only does the Warm Springs Natural Area encompass the majority of Muddy River tributaries it is also the largest single tract of land in the upper Muddy River set aside for the benefit of native species in perpetuity. The prominence of water in an otherwise barren Mojave landscape provides an oasis for regional wildlife. A high bird diversity is attributed to an abundance of riparian and floodplain trees and shrubs. Contributions to plant diversity come from the Mojave Old World swallowtail (Papilio machaon) Desertsnow (Linanthus demissus) Lobe-leaved Phacelia (Phacelia crenulata) Cryptantha (Cryptantha sp.) vegetation that occur on the toe slopes of the Arrow Canyon Range from the west and the plant species occupying the floodplain where they are supported by a high water table. Several marshes and wet meadows add to the diversity of plants and animals. The thermal springs and tributaries host an abundance of aquatic species, many of which are endemic. The WSNA provides a haven for the abundant wildlife that resides permanently or seasonally and provides a significant level of protection for imperiled species. Tarantula (Aphonopelma spp.) Beavertail cactus (Opuntia basilaris) Pacific tree frog (Pseudacris regilla) -
June-July 2021
Phainopepla Published by the San Fernando Valley Audubon Society A 501(c)(3) non-profit organization A Chapter of National Audubon Society For Nature Education and the Conservation of Wildlife Vol. 72 No. 3 June / July 2021 General Membership Meeting: — Zoom Presentation Online General Membership Thursday, June 24, 2021 Meetings 7:00—8:00 p.m. Please join us for our Guest Speaker: Krise Stein online presentations From: Southern Sierra Research StaEon from the comfort of PresentaEon Title: Successes and Future Developments of the Motus your home! Wildlife Tracking System ————————————————— Become a NEW member Please click here to register. Your first year is FREE! Go to SFVAudubon.org Clean Up of Haskell Creek in the Sepulveda Basin Wildlife Reserve ————————————————— Saturday June 19, 2021 8:30AM – Noon Additional Changes at National Audubon Society Leadership Effective April 23, 2021, David an Fernando Valley Audubon Society is partnering with Friends of the Los Angeles River (FoLAR) Ringer, Chief Network and S Communications Officer, National and the Resource Conserva?on District of the Santa Monica Mountains for a greatly needed cleanup. Audubon Society, announced his departure. Along with Elizabeth Please register soon to volunteer to help Haskell Creek at hFps://www.eventbrite.com/e/the-great-la- Sorrell, they will begin a new v e n t u r e t o g e t h e r t o h e l p river-cleanup-haskell-creek-registra?on-151737560127. nonprofit organizations and companies do more for the As FoLAR’s announcement says, The River needs YOU! This summer, join FoLAR and our partners for a e n v i r o n m e n t a n d f o r series of small, in-person cleanups to collect trash and prevent waste from pollu?ng our watershed and communities. -
Biology 2 Lab Packet for Practical 4 Birds
Bio 2 – Lab Practicum 4 1 Biology 2 Lab Packet For Practical 4 Birds Bio 2 – Lab Practicum 4 2 CLASSIFICATION: Domain: Eukarya Kingdom: Animalia Phylum: Chordata – Chordates Class: Aves – Birds Order: Struthioniformes - Ostriches Order: Galliformes - Quail Order: Rheiformes – Rheas Order: Gruiformes – Coots Order: Casuariiformes – Cassowaries Order: Charadriiformes – Gulls and Allies Order: Apterygiformes – Kiwis Order: Columbiformes – Pigeons Order: Sphenisciformes - Penguins Order: Psittaciformes – Parrots Order: Gaviiformes - Loons Order: Cuculiformes – Roadrunners Order: Podicipediformes – Grebes Order: Strigiformes - Owls Order: Procellariiformes – Tube noses Order: Caprimulgiformes – Nighthawks Order: Pelicaniformes – Pelicans Order: Apodiformes – Hummingbirds Order: Ciconiiformes – Herons/Egrets Order: Trogonifomes – Trogons Order: Phoenicopteriformes - Flamingos Order: Coraciformes – Kingfishers Order: Anseriformes – Ducks Order: Piciformes – Woodpeckers Order: Falconiformes – Raptors Order: Passeriformes - Songbirds Introduction – Birds Although chordates vary widely in appearance, they are distinguished as a phylum by the presence of four anatomical features that appear sometime during their life time. They exhibit deuterostome development and bilateral symmetry. Chordates only comprise 5% of the animal species but may be the most commonly known phylum. Birds are endothermic homeotherms which have adapted to many different ecosystems in the world. Station 1 – Class: Aves 1. What three adaptations do birds have for flight? 2. What do all species of birds have? 3. What dinosaurs did birds emerge within? When did they show up? 4. Where are birds found? Bio 2 – Lab Practicum 4 3 Station 2 – Evolutionary History - Archaeopteryx 1. What characteristics are seen in Archaeopteryx that are bird-like? 2. What characteristics are seen in Archaeopteryx that are reptile-like? Station 3 – General Characteristics - Feathers 1. What are feathers made of? 2. -
DRAFT SUPPLEMENTAL SPECIAL-STATUS SPECIES SCREENING ANALYSIS Kirkland High Quality Pozzolan Mining and Reclamation Plan of Operations
DRAFT SUPPLEMENTAL SPECIAL-STATUS SPECIES SCREENING ANALYSIS Kirkland High Quality Pozzolan Mining and Reclamation Plan of Operations Prepared for: U.S. Department of the Interior Bureau of Land Management, Hassayampa Field Office 21605 North 7th Avenue, Phoenix, Arizona 85027 AZA 37212 May 4, 2018 WestLand Resources, Inc. 4001 E. Paradise Falls Drive Tucson, Arizona 85712 5202069585 Kirkland High Quality Pozzolan Draft Supplemental Special-Status Mining and Reclamation Plan of Operations Species Screening Analysis TABLE OF CONTENTS 1. INTRODUCTION AND BACKGROUND ...................................................................................... 1 2. METHODS ................................................................................................................................................ 1 3. RESULTS ................................................................................................................................................... 3 4. REFERENCES ....................................................................................................................................... 31 TABLES Table 1. Bureau of Land Management Phoenix District Sensitive Species Potential to Occur Screening Analysis Table 2. Arizona Species of Greatest Conservation Need Potential to Occur Screening Analysis Table 3. Migratory Bird Potential to Occur Screening Analysis APPENDICES Appendix A. Bureau of Land Management, Arizona – Bureau Sensitive Species List (February 2017) Appendix B. Arizona Game and Fish Department Environmental -
Avian Use of Xeroriparian Ecosystems in the North American Warm Deserts1
This file was created by scanning the printed publication. Errors identified by the software have been corrected; however, some errors may remain. Avian Use of Xeroriparian Ecosystems in the North American Warm Deserts1 2 2 R. Roy Johnson and Lois T. Haight Abstract.--Results of xeroriparian avian censuses are compared with paired desert upland censuses for various sub divisions of the Sonoran Desert. With few exceptions xero riparian habitat supports 5 to 10 times the population densi ties and species diversity of surrounding desert uplands. INTRODUCTION AND BACKGROUND The value of riparian ecosystems as avian habi classified the vegetation associated with these tat was first quantified in the late 1960's and early wash systems (Lowe and Brown 1973, Brown et al. 1970's (Carothers and Johnson 1971, Johnson 1971, 1979). Carothers et al. 1974). These earlier avian investi gations, however, dealt entirely with wet riparian In 1980 we began avian investigations at Organ ecosystems (hydroriparian and mesoriparian) and Pipe Cactus National Monument in the same region although dry riparian habitats had been defined a where Hensley (1954) had conducted his earlier stu decade earlier as "desert riparian" (Lowe 1961), dies. We are measuring species distribution and little has been done either qualitatively or quanti abundance of birds in various habitats during the tatively to further characterize these xeroriparian different seasons of the year. Dry watercourses and ecosystems. their attendant xeroriparian vegetation often con stitute almost 10% of the habitat of an area3. These earlier avian studies were concerned with This is especially noticeable for 1st, 2nd, and species diversity and population densities of breed 3rd order washes in desert faotnills (Johnson et al. -
Baja California & the Sea of Cortez
BAJA CALIFORNIA & THE SEA OF CORTEZ: AMONG THE GREAT WHALES JANUARY 19–27, 2018 Humpback Whale © Michael O’Brien LEADER: MICHAEL O’BRIEN LIST COMPILED BY: MICHAEL O’BRIEN VICTOR EMANUEL NATURE TOURS, INC. 2525 WALLINGWOOD DRIVE, SUITE 1003 AUSTIN, TEXAS 78746 WWW.VENTBIRD.COM BAJA CALIFORNIA & THE SEA OF CORTEZ: AMONG THE GREAT WHALES January 19–27, 2018 By Michael O’Brien Amazing natural beauty, delightful weather, and spectacular sunrises and sunsets were hallmarks of our 2018 Baja cruise aboard the National Geographic Sea Bird . With fascinating wildlife sightings at every turn, and an accomplished and friendly team of naturalists on board, our group had a fun-filled, relaxing, and educational vacation. Our adventure began among massive white sand dunes, mangrove thickets, and tranquil waters of Magdalena Bay on the Pacific side of the peninsula. The shallow bays and waterways here are famous for their concentrations of Gray Whales, which gather here in winter to raise their calves, protected from Killer Whales, which stay in deeper offshore waters. We found several mothers with newborn calves and had many wonderful encounters, sometimes just a few feet from our Zodiacs! Although newborn Gray Whales average sixteen feet long and weigh a full ton, they are comical to watch as they learn how to swim, often surfacing awkwardly and tumbling in the process. Aside from Gray Whales, Magdalena Bay offered an amazing abundance and diversity of birdlife. A walk along the dune-mangrove interface yielded an interesting array of land birds, including “Mangrove” Yellow Warbler, Lark Bunting, and both “Belding’s” and “Large-billed” Savannah Sparrows (two subspecies that occur primarily in southern California and Baja). -
Birds of Cibola National Wildlife Refuge
U.S. Fish & Wildlife Service Birds of Cibola National Wildlife Refuge Cibola National Wildlife Refuge is located Common Name Sp S F W Common Name Sp S F W along the lower Colorado River 20 miles Ducks, Geese, and Swans ___*Sora C C C C south of Blythe, California. Approximately ___Fulvous Whistling-Duck X X ___*Common Moorhen C C C C two-thirds of the refuge is in Arizona and one- ___Gr. White-fronted Goose U U ___*American Coot A A A A third is in California and encompasses 18,555 ___Snow Goose C C Cranes acres. The refuge was established in 1964 to ___Ross’s Goose U U ___Sandhill Crane O C mitigate the loss of fish and wildlife habitat ___Brant X Stilts and Avocets involved in the channelization projects along ___Canada Goose O A A ___*Black-necked Stilt C U C U the Colorado River. ___Tundra Swan O O ___American Avocet U R U R The main portion of the refuge is alluvial ___Wood Duck U U Plovers river bottom with dense growths of salt cedar, ___Gadwall U C C ___Black-bellied Plover R mesquite, and arrowweed along with several ___Eurasian Wigeon O ___Snowy Plover O O R hundred acres of revegetated cottonwood ___American Wigeon U C A ___Semipalmated Plover O O and willow habitat. Through this flows the ___*Mallard C U C A ___*Killdeer A A C C Colorado River, in both a dredged channel and ___Blue-winged Teal O O Sandpipers, Phalaropes, and Allies a portion of its original channel. -
The Geology of the Tuff of Bridge Spring: Southern Nevada and Northwestern Arizona
UNLV Theses, Dissertations, Professional Papers, and Capstones 12-1993 The geology of the Tuff of Bridge Spring: Southern Nevada and northwestern Arizona Shirley Ann Morikawa University of Nevada, Las Vegas Follow this and additional works at: https://digitalscholarship.unlv.edu/thesesdissertations Part of the Geochemistry Commons, Geology Commons, Stratigraphy Commons, and the Volcanology Commons Repository Citation Morikawa, Shirley Ann, "The geology of the Tuff of Bridge Spring: Southern Nevada and northwestern Arizona" (1993). UNLV Theses, Dissertations, Professional Papers, and Capstones. 1453. The Geology of the TufT of Bridge Spring: Southern Nevada and Northwestern Arizona by Shirley Ann Morikawa A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology Geoscience Department University of Nevada, Las Vegas December, 1993 © 1994 Shirley Ann Morikawa All Rights Reserved The thesis of Shirley Ann Morikawa for the degree of Master of Science in Geology is approve . r, Ernest M. Duebendorfer, Ph.D. Graduate Faculty Representaf , Donna E.Weistrop, Ph.D. Dean of the Graduate College, Ronald W. Smith, Ph.D. University of Nevada, Las Vegas December, 1993 ii Abstract The Tuff of Bridge Spring (TBS) is a regionally-widespread, andesite to rhyolite (59 .50 to 74.91 wt. %) ash-flow tuff of mid-Miocene age (ca. 15.2 Ma) that is exposed in the northern Colorado River extensional corridor of southern Nevada and northwestern Arizona. Determination of the areal distribution, geochronology, lithology, geochemistry, and internal stratigraphy of the TBS is important for its establishment as a reliable stratigraphic reference horizon for tectonic reconstructions of the extensional corridor during the middle Miocene.