The New Mexico Botanist, Issue No. 2
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Colorado Wildlife Action Plan: Proposed Rare Plant Addendum
Colorado Wildlife Action Plan: Proposed Rare Plant Addendum By Colorado Natural Heritage Program For The Colorado Rare Plant Conservation Initiative June 2011 Colorado Wildlife Action Plan: Proposed Rare Plant Addendum Colorado Rare Plant Conservation Initiative Members David Anderson, Colorado Natural Heritage Program (CNHP) Rob Billerbeck, Colorado Natural Areas Program (CNAP) Leo P. Bruederle, University of Colorado Denver (UCD) Lynn Cleveland, Colorado Federation of Garden Clubs (CFGC) Carol Dawson, Bureau of Land Management (BLM) Michelle DePrenger-Levin, Denver Botanic Gardens (DBG) Brian Elliott, Environmental Consulting Mo Ewing, Colorado Open Lands (COL) Tom Grant, Colorado State University (CSU) Jill Handwerk, Colorado Natural Heritage Program (CNHP) Tim Hogan, University of Colorado Herbarium (COLO) Steve Kettler, U.S. Fish and Wildlife Service (USFWS) Andrew Kratz, U.S. Forest Service (USFS) Sarada Krishnan, Colorado Native Plant Society (CoNPS), Denver Botanic Gardens Brian Kurzel, Colorado Natural Areas Program Eric Lane, Colorado Department of Agriculture (CDA) Paige Lewis, The Nature Conservancy (TNC) Ellen Mayo, U.S. Fish and Wildlife Service Mitchell McGlaughlin, University of Northern Colorado (UNC) Jennifer Neale, Denver Botanic Gardens Betsy Neely, The Nature Conservancy Ann Oliver, The Nature Conservancy Steve Olson, U.S. Forest Service Susan Spackman Panjabi, Colorado Natural Heritage Program Jeff Peterson, Colorado Department of Transportation (CDOT) Josh Pollock, Center for Native Ecosystems (CNE) Nicola Ripley, -
Appendix F3 Rare Plant Survey Report
Appendix F3 Rare Plant Survey Report Draft CADIZ VALLEY WATER CONSERVATION, RECOVERY, AND STORAGE PROJECT Rare Plant Survey Report Prepared for May 2011 Santa Margarita Water District Draft CADIZ VALLEY WATER CONSERVATION, RECOVERY, AND STORAGE PROJECT Rare Plant Survey Report Prepared for May 2011 Santa Margarita Water District 626 Wilshire Boulevard Suite 1100 Los Angeles, CA 90017 213.599.4300 www.esassoc.com Oakland Olympia Petaluma Portland Sacramento San Diego San Francisco Seattle Tampa Woodland Hills D210324 TABLE OF CONTENTS Cadiz Valley Water Conservation, Recovery, and Storage Project: Rare Plant Survey Report Page Summary ............................................................................................................................... 1 Introduction ..........................................................................................................................2 Objective .......................................................................................................................... 2 Project Location and Description .....................................................................................2 Setting ................................................................................................................................... 5 Climate ............................................................................................................................. 5 Topography and Soils ......................................................................................................5 -
By Douglas P. Klein with Plates by G.A. Abrams and P.L. Hill U.S. Geological Survey, Denver, Colorado
U.S DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY STRUCTURE OF THE BASINS AND RANGES, SOUTHWEST NEW MEXICO, AN INTERPRETATION OF SEISMIC VELOCITY SECTIONS by Douglas P. Klein with plates by G.A. Abrams and P.L. Hill U.S. Geological Survey, Denver, Colorado Open-file Report 95-506 1995 This report is preliminary and has not been edited or reviewed for conformity with U.S. Geological Survey editorial standards. The use of trade, product, or firm names in this papers is for descriptive purposes only, and does not imply endorsement by the U.S. Government. STRUCTURE OF THE BASINS AND RANGES, SOUTHWEST NEW MEXICO, AN INTERPRETATION OF SEISMIC VELOCITY SECTIONS by Douglas P. Klein CONTENTS INTRODUCTION .................................................. 1 DEEP SEISMIC CRUSTAL STUDIES .................................. 4 SEISMIC REFRACTION DATA ....................................... 7 RELIABILITY OF VELOCITY STRUCTURE ............................. 9 CHARACTER OF THE SEISMIC VELOCITY SECTION ..................... 13 DRILL HOLE DATA ............................................... 16 BASIN DEPOSITS AND BEDROCK STRUCTURE .......................... 20 Line 1 - Playas Valley ................................... 21 Cowboy Rim caldera .................................. 23 Valley floor ........................................ 24 Line 2 - San Luis Valley through the Alamo Hueco Mountains ....................................... 25 San Luis Valley ..................................... 26 San Luis and Whitewater Mountains ................... 26 Southern -
Stratigraphic Nomenclature of ' Volcanic Rocks in the Jemez Mountains, New Mexico
-» Stratigraphic Nomenclature of ' Volcanic Rocks in the Jemez Mountains, New Mexico By R. A. BAILEY, R. L. SMITH, and C. S. ROSS CONTRIBUTIONS TO STRATIGRAPHY » GEOLOGICAL SURVEY BULLETIN 1274-P New Stratigraphic names and revisions in nomenclature of upper Tertiary and , Quaternary volcanic rocks in the Jemez Mountains UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director U.S. GOVERNMENT PRINTING OFFICE WASHINGTON : 1969 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 15 cents (paper cover) CONTENTS Page Abstract.._..._________-...______.._-.._._____.. PI Introduction. -_-________.._.____-_------___-_______------_-_---_-_ 1 General relations._____-___________--_--___-__--_-___-----___---__. 2 Keres Group..__________________--------_-___-_------------_------ 2 Canovas Canyon Rhyolite..__-__-_---_________---___-____-_--__ 5 Paliza Canyon Formation.___-_________-__-_-__-__-_-_______--- 6 Bearhead Rhyolite-___________________________________________ 8 Cochiti Formation.._______________________________________________ 8 Polvadera Group..______________-__-_------________--_-______---__ 10 Lobato Basalt______________________________________________ 10 Tschicoma Formation_______-__-_-____---_-__-______-______-- 11 El Rechuelos Rhyolite--_____---------_--------------_-_------- 11 Puye Formation_________________------___________-_--______-.__- 12 Tewa Group__._...._.______........___._.___.____......___...__ 12 Bandelier Tuff.______________.______________... 13 Tsankawi Pumice Bed._____________________________________ 14 Valles Rhyolite______.__-___---_____________.________..__ 15 Deer Canyon Member.______-_____-__.____--_--___-__-____ 15 Redondo Creek Member.__________________________________ 15 Valle Grande Member____-__-_--___-___--_-____-___-._-.__ 16 Battleship Rock Member...______________________________ 17 El Cajete Member____..._____________________ 17 Banco Bonito Member.___-_--_---_-_----_---_----._____--- 18 References . -
(LOWER PENNSYLVANIAN) in the PERMIAN BASIN Wayne R. Wright Bureau of Economic Geol
DEPOSITIONAL HISTORY OF THE ATOKAN SUCCESSION (LOWER PENNSYLVANIAN) IN THE PERMIAN BASIN Wayne R. Wright Bureau of Economic Geology Jackson School of Geosciences The University of Texas at Austin Austin, Texas ABSTRACT Atokan-age units in the Permian Basin record a 2nd-order transgression, with aerially restricted, lower Atokan fluvial to shallow-marine siliciclastics followed by pervasive carbonate deposition. In general, Atokan-age siliciclastics dominated deposition in the west of the Permian Basin while carbonate deposition dominated throughout the rest of the basin. Predominance of carbonate facies across most of the Permian Basin is due to (1) lack of siliciclastic supply, (2) overall 2nd-order rising sea level, and (3) progradation of the Upper Marble Falls Formation onto the Eastern Shelf. Progradation was due partly to lower accommodation to the west and backstepping/retreat from encroaching Atokan deltaics to the east. The beginning of the Atokan is marked by a sea-level drop and subsequent lowstand conditions. A sequence boundary separates the Atokan from the underlying Morrowan carbonate section throughout the Permian Basin. Siliciclastic deposition in and around the Permian Basin is more aerially restricted than in the Morrowan. The earliest Atokan lowstand event is manifested in alluvial and fluvial incised-valley sediments in Lea County, New Mexico, and the Broken Bone Graben (Cottle County, Texas); fan- delta deposits in the Palo Duro Basin and Taylor Draw field (Upton County, Texas); and 1 post-Lower Marble Falls–pre-Upper Marble falls conglomerates (Gibbons Formation?) on the Llano Uplift. Following the lowstand event, a 2nd-order transgression appears to have dominated throughout the rest of the Atokan; however 3rd- and 4th-order, high- amplitude, sea-level fluctuations also occurred. -
December 2012 Number 1
Calochortiana December 2012 Number 1 December 2012 Number 1 CONTENTS Proceedings of the Fifth South- western Rare and Endangered Plant Conference Calochortiana, a new publication of the Utah Native Plant Society . 3 The Fifth Southwestern Rare and En- dangered Plant Conference, Salt Lake City, Utah, March 2009 . 3 Abstracts of presentations and posters not submitted for the proceedings . 4 Southwestern cienegas: Rare habitats for endangered wetland plants. Robert Sivinski . 17 A new look at ranking plant rarity for conservation purposes, with an em- phasis on the flora of the American Southwest. John R. Spence . 25 The contribution of Cedar Breaks Na- tional Monument to the conservation of vascular plant diversity in Utah. Walter Fertig and Douglas N. Rey- nolds . 35 Studying the seed bank dynamics of rare plants. Susan Meyer . 46 East meets west: Rare desert Alliums in Arizona. John L. Anderson . 56 Calochortus nuttallii (Sego lily), Spatial patterns of endemic plant spe- state flower of Utah. By Kaye cies of the Colorado Plateau. Crystal Thorne. Krause . 63 Continued on page 2 Copyright 2012 Utah Native Plant Society. All Rights Reserved. Utah Native Plant Society Utah Native Plant Society, PO Box 520041, Salt Lake Copyright 2012 Utah Native Plant Society. All Rights City, Utah, 84152-0041. www.unps.org Reserved. Calochortiana is a publication of the Utah Native Plant Society, a 501(c)(3) not-for-profit organi- Editor: Walter Fertig ([email protected]), zation dedicated to conserving and promoting steward- Editorial Committee: Walter Fertig, Mindy Wheeler, ship of our native plants. Leila Shultz, and Susan Meyer CONTENTS, continued Biogeography of rare plants of the Ash Meadows National Wildlife Refuge, Nevada. -
Zuni Fleabane (Erigeron Rhizomatus)
Zuni Fleabane (Erigeron rhizomatus) 5-Year Review: Summary and Evaluation U.S. Fish and Wildlife Service New Mexico Ecological Services Field Office Albuquerque, New Mexico 5-YEAR REVIEW Species reviewed: Zuni Fleabane (Erigeron rhizomatus) TABLE OF CONTENTS 1.0 GENERAL INFORMATION................................................................................................ 1 1.1 Reviewers...................................................................................................................... 1 1.2 Methodology used to complete the review ................................................................... 1 1.3 Background................................................................................................................... 1 1.3.1 FR Notice citation announcing initiation of this review................................... 1 1.3.2 Listing History .................................................................................................. 2 1.3.3 Associated rulemakings .................................................................................... 2 1.3.4 Review history .................................................................................................. 2 1.3.5 Species' recovery priority number at start of review ........................................ 2 1.3.6 Recovery plan ................................................................................................... 2 2.0 REVIEW ANALYSIS .......................................................................................................... -
Permian Basin, West Texas and Southeastern New Mexico
Report of Investigations No. 201 Stratigraphic Analysis of the Upper Devonian Woodford Formation, Permian Basin, West Texas and Southeastern New Mexico John B. Comer* *Current address Indiana Geological Survey Bloomington, Indiana 47405 1991 Bureau of Economic Geology • W. L. Fisher, Director The University of Texas at Austin • Austin, Texas 78713-7508 Contents Abstract ..............................................................................................................................1 Introduction ..................................................................................................................... 1 Methods .............................................................................................................................3 Stratigraphy .....................................................................................................................5 Nomenclature ...................................................................................................................5 Age and Correlation ........................................................................................................6 Previous Work .................................................................................................................6 Western Outcrop Belt ......................................................................................................6 Central Texas ...................................................................................................................7 Northeastern Oklahoma -
Cenozoic Thermal, Mechanical and Tectonic Evolution of the Rio Grande Rift
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 91, NO. B6, PAGES 6263-6276, MAY 10, 1986 Cenozoic Thermal, Mechanical and Tectonic Evolution of the Rio Grande Rift PAUL MORGAN1 Departmentof Geosciences,Purdue University,West Lafayette, Indiana WILLIAM R. SEAGER Departmentof Earth Sciences,New Mexico State University,Las Cruces MATTHEW P. GOLOMBEK Jet PropulsionLaboratory, CaliforniaInstitute of Technology,Pasadena Careful documentationof the Cenozoicgeologic history of the Rio Grande rift in New Mexico reveals a complexsequence of events.At least two phasesof extensionhave been identified.An early phase of extensionbegan in the mid-Oligocene(about 30 Ma) and may have continuedto the early Miocene (about 18 Ma). This phaseof extensionwas characterizedby local high-strainextension events (locally, 50-100%,regionally, 30-50%), low-anglefaulting, and the developmentof broad, relativelyshallow basins, all indicatingan approximatelyNE-SW •-25ø extensiondirection, consistent with the regionalstress field at that time.Extension events were not synchronousduring early phase extension and were often temporally and spatiallyassociated with major magmatism.A late phaseof extensionoccurred primarily in the late Miocene(10-5 Ma) with minor extensioncontinuing to the present.It was characterizedby apparently synchronous,high-angle faulting givinglarge verticalstrains with relativelyminor lateral strain (5-20%) whichproduced the moderuRio Granderift morphology.Extension direction was approximatelyE-W, consistentwith the contemporaryregional stress field. Late phasegraben or half-grabenbasins cut and often obscureearly phasebroad basins.Early phase extensionalstyle and basin formation indicate a ductilelithosphere, and this extensionoccurred during the climax of Paleogenemagmatic activity in this zone.Late phaseextensional style indicates a more brittle lithosphere,and this extensionfollowed a middle Miocenelull in volcanism.Regional uplift of about1 km appearsto haveaccompanied late phase extension, andrelatively minor volcanism has continued to thepresent. -
Mosaic of New Mexico's Scenery, Rocks, and History
Mosaic of New Mexico's Scenery, Rocks, and History SCENIC TRIPS TO THE GEOLOGIC PAST NO. 8 Scenic Trips to the Geologic Past Series: No. 1—SANTA FE, NEW MEXICO No. 2—TAOS—RED RIVER—EAGLE NEST, NEW MEXICO, CIRCLE DRIVE No. 3—ROSWELL—CAPITAN—RUIDOSO AND BOTTOMLESS LAKES STATE PARK, NEW MEXICO No. 4—SOUTHERN ZUNI MOUNTAINS, NEW MEXICO No. 5—SILVER CITY—SANTA RITA—HURLEY, NEW MEXICO No. 6—TRAIL GUIDE TO THE UPPER PECOS, NEW MEXICO No. 7—HIGH PLAINS NORTHEASTERN NEW MEXICO, RATON- CAPULIN MOUNTAIN—CLAYTON No. 8—MOSlAC OF NEW MEXICO'S SCENERY, ROCKS, AND HISTORY No. 9—ALBUQUERQUE—ITS MOUNTAINS, VALLEYS, WATER, AND VOLCANOES No. 10—SOUTHWESTERN NEW MEXICO No. 11—CUMBRE,S AND TOLTEC SCENIC RAILROAD C O V E R : REDONDO PEAK, FROM JEMEZ CANYON (Forest Service, U.S.D.A., by John Whiteside) Mosaic of New Mexico's Scenery, Rocks, and History (Forest Service, U.S.D.A., by Robert W . Talbott) WHITEWATER CANYON NEAR GLENWOOD SCENIC TRIPS TO THE GEOLOGIC PAST NO. 8 Mosaic of New Mexico's Scenery, Rocks, a n d History edited by PAIGE W. CHRISTIANSEN and FRANK E. KOTTLOWSKI NEW MEXICO BUREAU OF MINES AND MINERAL RESOURCES 1972 NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY STIRLING A. COLGATE, President NEW MEXICO BUREAU OF MINES & MINERAL RESOURCES FRANK E. KOTTLOWSKI, Director BOARD OF REGENTS Ex Officio Bruce King, Governor of New Mexico Leonard DeLayo, Superintendent of Public Instruction Appointed William G. Abbott, President, 1961-1979, Hobbs George A. Cowan, 1972-1975, Los Alamos Dave Rice, 1972-1977, Carlsbad Steve Torres, 1967-1979, Socorro James R. -
Plan for the Recovery of Desert Bighorn Sheep in New Mexico 2003-2013
PLAN FOR THE RECOVERY OF DESERT BIGHORN SHEEP IN NEW MEXICO 2003-2013 New Mexico Department of Game and Fish August 2003 Executive Summary Desert bighorn sheep (Ovis canadensis mexicana) were once prolific in New Mexico, occupying most arid mountain ranges in the southern part of the state. Over-hunting, and disease transmission from livestock are 2 primary reasons for the dramatic decline in bighorn sheep numbers throughout the west during the early 1900s. In 1980, desert bighorn were placed on New Mexico’s endangered species list. From 1992-2003, approximately 25% of bighorn were radiocollared to learn causes of mortality driving this species towards extinction. Approximately 85% of all known-cause non-hunter killed radiocollared individuals have been killed by mountain lions. Despite the lack of a native ungulate prey base in desert bighorn range, mountain lion populations remain high, leading to the hypothesis that mountain lions are subsidized predators feeding on exotic ungulates, including cattle. Lack of fine fuels from cattle grazing have resulted in a lack of fire on the landscape. This has lead to increased woody vegetation which inhibits bighorn’s ability to detect and escape from predators. Bighorn numbers in spring 2003 in New Mexico totaled 213 in the wild, and 91 at the Red Rock captive breeding facility. This is in spite of releasing 266 bighorn from Red Rock and 30 bighorn from Arizona between 1979 and 2002. Several existing herds of desert bighorn likely need an augmentation to prevent them from going extinct. The presence of domestic sheep and Barbary sheep, which pose risks to bighorn from fatal disease transmission and aggression, respectively, preclude reintroduction onto many unoccupied mountain ranges. -
SAN DIEGO COUNTY NATIVE PLANTS in the 1830S
SAN DIEGO COUNTY NATIVE PLANTS IN THE 1830s The Collections of Thomas Coulter, Thomas Nuttall, and H.M.S. Sulphur with George Barclay and Richard Hinds James Lightner San Diego Flora San Diego, California 2013 SAN DIEGO COUNTY NATIVE PLANTS IN THE 1830s Preface The Collections of Thomas Coulter, Thomas Nuttall, and Our knowledge of the natural environment of the San Diego region H.M.S. Sulphur with George Barclay and Richard Hinds in the first half of the 19th century is understandably vague. Referenc- es in historical sources are limited and anecdotal. As prosperity peaked Copyright © 2013 James Lightner around 1830, probably no more than 200 inhabitants in the region could read and write. At most one or two were trained in natural sciences or All rights reserved medicine. The best insights we have into the landscape come from nar- No part of this document may be reproduced or transmitted in any form ratives of travelers and the periodic reports of the missions’ lands. They without permission in writing from the publisher. provide some idea of the extent of agriculture and the general vegeta- tion covering surrounding land. ISBN: 978-0-9749981-4-5 The stories of the visits of United Kingdom naturalists who came in Library of Congress Control Number: 2013907489 the 1830s illuminate the subject. They were educated men who came to the territory intentionally to examine the flora. They took notes and col- Cover photograph: lected specimens as botanists do today. Reviewing their contributions Matilija Poppy (Romneya trichocalyx), Barrett Lake, San Diego County now, we can imagine what they saw as they discovered plants we know.