Summary Table: Characteristics of the Ecoregions of New Mexico 2 0
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An Environmental History of the Middle Rio Grande Basin
United States Department of From the Rio to the Sierra: Agriculture Forest Service An Environmental History of Rocky Mountain Research Station the Middle Rio Grande Basin Fort Collins, Colorado 80526 General Technical Report RMRS-GTR-5 Dan Scurlock i Scurlock, Dan. 1998. From the rio to the sierra: An environmental history of the Middle Rio Grande Basin. General Technical Report RMRS-GTR-5. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 440 p. Abstract Various human groups have greatly affected the processes and evolution of Middle Rio Grande Basin ecosystems, especially riparian zones, from A.D. 1540 to the present. Overgrazing, clear-cutting, irrigation farming, fire suppression, intensive hunting, and introduction of exotic plants have combined with droughts and floods to bring about environmental and associated cultural changes in the Basin. As a result of these changes, public laws were passed and agencies created to rectify or mitigate various environmental problems in the region. Although restoration and remedial programs have improved the overall “health” of Basin ecosystems, most old and new environmental problems persist. Keywords: environmental impact, environmental history, historic climate, historic fauna, historic flora, Rio Grande Publisher’s Note The opinions and recommendations expressed in this report are those of the author and do not necessarily reflect the views of the USDA Forest Service. Mention of trade names does not constitute endorsement or recommendation for use by the Federal Government. The author withheld diacritical marks from the Spanish words in text for consistency with English punctuation. Publisher Rocky Mountain Research Station Fort Collins, Colorado May 1998 You may order additional copies of this publication by sending your mailing information in label form through one of the following media. -
Late Paleozoic Tectonic and Sedimentologic History of the Penasco Uplift, North-Central New Mexico
RICE UNIVERSITY LATE PALEOZOIC TECTONIC AND SEDIMENTOLOGIC HISTORY OF THE PENASCO UPLIFT, NORTH-CENTRAL NEW MEXICO by ROY DONALD ADAMS A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE MASTER OF ARTS APPROVED, THESIS COMMITTEE: 0^ (3- /jtd&i obfe B. Anderson, Chairman Assistant Professor pf Geology KT Rudy R. Schwarzer, Adjunct Assistant Professor of GSology John /E. Warme Professor of Geology Donald R. Baker Professor of Geology Houston, Texas May, 1980 ABSTRACT LATE PALEOZOIC TECTONIC AND SEDIMENTOLOGIC HISTORY OF THE PENASCO UPLIFT, NORTH-CENTRAL NEW MEXICO Roy Donald Adams The Paleozoic Peiiasco Uplift, located on the site of the present Nacimiento Mountains of north-central New Mexico, acted as a sediment source and modifier of regional sedimentation patterns from Middle Pennsylvanian to Early Permian time. The earliest history of the uplift is still poorly defined. Orogenic activity may have started as early as the Late Mississippian, or there may have been quiescence until after deposition of the Morrow-age Osha Canyon Formation and prior to deposition of the Atoka-age Sandia Formation. Coarse, arkosic siliciclastic sediments inter- bedded with fossilferious carbonates in the Madera Formation indicate that by early Desmoinesian time the Peiiasco Uplift had risen sufficiently to expose and erode Precambrian rocks. Paleotransport indicators in the arkosic sediments show transport away from the uplift. Throughout the remainder of the Pennsylvanian, the Peiiasco Uplift was a sediment source. The siliciclastic sediments derived from the Peiiasco Uplift formed a wedge that prograded out onto and interfingered with carbonate sediments of a shallow normal marine shelf. A change in paleotransport directions from northeasterly to southwesterly occurs on the east side of the Peiiasco Uplift and is due to the arrival of a flood of siliciclastic sediments derived from the Uncompahgre-San Luis Uplift to the northeast. -
A Phylogeny of the Hubbardochloinae Including Tetrachaete (Poaceae: Chloridoideae: Cynodonteae)
Peterson, P.M., K. Romaschenko, and Y. Herrera Arrieta. 2020. A phylogeny of the Hubbardochloinae including Tetrachaete (Poaceae: Chloridoideae: Cynodonteae). Phytoneuron 2020-81: 1–13. Published 18 November 2020. ISSN 2153 733 A PHYLOGENY OF THE HUBBARDOCHLOINAE INCLUDING TETRACHAETE (CYNODONTEAE: CHLORIDOIDEAE: POACEAE) PAUL M. PETERSON AND KONSTANTIN ROMASCHENKO Department of Botany National Museum of Natural History Smithsonian Institution Washington, D.C. 20013-7012 [email protected]; [email protected] YOLANDA HERRERA ARRIETA Instituto Politécnico Nacional CIIDIR Unidad Durango-COFAA Durango, C.P. 34220, México [email protected] ABSTRACT The phylogeny of subtribe Hubbardochloinae is revisited, here with the inclusion of the monotypic genus Tetrachaete, based on a molecular DNA analysis using ndhA intron, rpl32-trnL, rps16 intron, rps16- trnK, and ITS markers. Tetrachaete elionuroides is aligned within the Hubbardochloinae and is sister to Dignathia. The biogeography of the Hubbardochloinae is discussed, its origin likely in Africa or temperate Asia. In a previous molecular DNA phylogeny (Peterson et al. 2016), the subtribe Hubbardochloinae Auquier [Bewsia Gooss., Dignathia Stapf, Gymnopogon P. Beauv., Hubbardochloa Auquier, Leptocarydion Hochst. ex Stapf, Leptothrium Kunth, and Lophacme Stapf] was found in a clade with moderate support (BS = 75, PP = 1.00) sister to the Farragininae P.M. Peterson et al. In the present study, Tetrachaete elionuroides Chiov. is included in a phylogenetic analysis (using ndhA intron, rpl32- trnL, rps16 intron, rps16-trnK, and ITS DNA markers) in order to test its relationships within the Cynodonteae with heavy sampling of species in the supersubtribe Gouiniodinae P.M. Peterson & Romasch. Chiovenda (1903) described Tetrachaete Chiov. with a with single species, T. -
Monitoring Changes on the Sheyenne National Grassland Using Multitemproal Landsat Data
University of North Dakota UND Scholarly Commons Theses and Dissertations Theses, Dissertations, and Senior Projects January 2017 Monitoring Changes On The heS yenne National Grassland Using Multitemporal Landsat Data Stefano Potter Follow this and additional works at: https://commons.und.edu/theses Recommended Citation Potter, Stefano, "Monitoring Changes On The heyS enne National Grassland Using Multitemporal Landsat Data" (2017). Theses and Dissertations. 2137. https://commons.und.edu/theses/2137 This Thesis is brought to you for free and open access by the Theses, Dissertations, and Senior Projects at UND Scholarly Commons. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of UND Scholarly Commons. For more information, please contact [email protected]. MONITORING CHANGES ON THE SHEYENNE NATIONAL GRASSLAND USING MULTITEMPROAL LANDSAT DATA By Stefano Marano Potter Bachelor of Science, University of Minnesota – Twin Cities, 2010 A Thesis Submitted to the Graduate Faculty of the University of North Dakota In partial fulfillment of the requirements For the degree of Master of Science Grand Forks, North Dakota May 2017 PERMISSION Title Monitoring Changes on the Sheyenne National Grassland using Multitemporal Landsat Data Department Earth System Science and Policy Degree Master of Science In presenting this thesis in partial fulfillment of the requirements for a graduate degree from the University of North Dakota, I agree that the library of this University shall make it freely available for inspection. I further agree that permission for extensive copying for scholarly purposes may be granted by the professor who supervised by thesis work or, in his absence, by the Chairperson of the department or the dean of the School of Graduate Studies. -
Land Areas of the National Forest System, As of September 30, 2019
United States Department of Agriculture Land Areas of the National Forest System As of September 30, 2019 Forest Service WO Lands FS-383 November 2019 Metric Equivalents When you know: Multiply by: To fnd: Inches (in) 2.54 Centimeters Feet (ft) 0.305 Meters Miles (mi) 1.609 Kilometers Acres (ac) 0.405 Hectares Square feet (ft2) 0.0929 Square meters Yards (yd) 0.914 Meters Square miles (mi2) 2.59 Square kilometers Pounds (lb) 0.454 Kilograms United States Department of Agriculture Forest Service Land Areas of the WO, Lands National Forest FS-383 System November 2019 As of September 30, 2019 Published by: USDA Forest Service 1400 Independence Ave., SW Washington, DC 20250-0003 Website: https://www.fs.fed.us/land/staff/lar-index.shtml Cover Photo: Mt. Hood, Mt. Hood National Forest, Oregon Courtesy of: Susan Ruzicka USDA Forest Service WO Lands and Realty Management Statistics are current as of: 10/17/2019 The National Forest System (NFS) is comprised of: 154 National Forests 58 Purchase Units 20 National Grasslands 7 Land Utilization Projects 17 Research and Experimental Areas 28 Other Areas NFS lands are found in 43 States as well as Puerto Rico and the Virgin Islands. TOTAL NFS ACRES = 192,994,068 NFS lands are organized into: 9 Forest Service Regions 112 Administrative Forest or Forest-level units 503 Ranger District or District-level units The Forest Service administers 149 Wild and Scenic Rivers in 23 States and 456 National Wilderness Areas in 39 States. The Forest Service also administers several other types of nationally designated -
Final Report: Lesser Prairie-Chicken Survey − Kiowa and Rita Blanca National Grasslands, 2014
Final Report: Lesser Prairie-Chicken Survey − Kiowa and Rita Blanca National Grasslands, 2014 Project Manager: Angela Dwyer, Rocky Mountain Bird Observatory, 230 Cherry St., Fort Collins, CO 80521 ([email protected]) Project Director: David Hanni, Rocky Mountain Bird Observatory, 230 Cherry St., Fort Collins, CO 80521 ([email protected]) Introduction The Lesser Prairie-Chicken (Tympanuchus pallidicinctus) (LEPC) occupies grassland habitat consisting of sand sagebrush (Artemisia filifolia), sand shinnery oak (Quercus havardii) and mixed grass vegetation communities of the southern Great Plains. Since the 19th century, LEPC and the habitat upon which they depend has diminished across their historical range (Crawford and Bolen 1976, Taylor and Guthery 1980a), with recent estimates of current occupied range totaling approximately 17% of the estimated area of their historical range. Causes for this reduction in occupied range are primarily attributed to habitat loss and fragmentation (USFWS 2012). Habitat loss has been caused by conversion of native prairie to cropland (Bent 1932, Copelin 1963, Taylor and Guthery 1980) and long term fire suppression (Woodward et al. 2001) leading to tree invasion (Fuhlendorf et al. 2002). Grazing management practices would help improve habitat if managed to benefit LEPC. Heavily grazed fields that leave no residual vegetation for broods can be detrimental to LEPC (Sell 1979, Hunt and Best 2010). Habitat fragmentation has resulted from a combination of habitat loss and degradation caused by oil and gas development (Hunt 2004) and suspected effects of wind energy development (Pruett et al. 2009). The LEPC is not thought to occur in Kiowa and Rita Blanca National Grasslands (KRB) (Giesen 2003), however some parcels within the grasslands are managed for LEPC. -
Central Mixedgrass Prairie Ecological System (Central Shortgrass Prairie Ecoregion Version)
CENTRAL MIXEDGRASS PRAIRIE ECOLOGICAL SYSTEM (CENTRAL SHORTGRASS PRAIRIE ECOREGION VERSION) ECOLOGICAL INTEGRITY ASSESSMENT Draft of June 29, 2007 Prepared by: Karin Decker Colorado Natural Heritage Program Colorado State University 254 General Services Building Fort Collins, CO 80523 Table of Contents A. INTRODUCTION ........................................................................................................ 3 A.1 Classification Summary ........................................................................................... 3 A.2 Ecological System Description ................................................................................ 5 A.2.1 Environment....................................................................................................... 5 A.2.2 Vegetation & Ecosystem.................................................................................... 6 A.2.3 Dynamics ........................................................................................................... 8 A.2.4 Landscape......................................................................................................... 10 A.2.5 Size................................................................................................................... 11 A.3 Ecological Integrity................................................................................................ 12 A.3.1 Threats.............................................................................................................. 12 A.3.2 Justification of Metrics.................................................................................... -
Geology and Ground-Water Resources of San Miguel County, New Mexico
GEOLOGY AND GROUND - WATER RESOURCES OF SAN MIGUEL COUNTY, NEW MEXICO GROUND-WATER REPORT 2 Geology and Ground-Water Resources of San Miguel County, New Mexico BY R. L. GRIGGS AND G. E. HENDRICKSON Prepared in cooperation with The United States Bureau of Reclamation New Mexico Bureau of Mines & Mineral Resources and the New Mexico State Engineer NEW MEXICO BUREAU OF MINES AND MINERAL RESOURCES SOCORRO 1951 NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Eugene Callaghan, Director THE REGENTS MEMBERS EX-OFFICIO The Honorable Edwin L. Mechem ...................... Governor of New Mexico Tom Wiley ............................................... Superintendent of Public Instruction APPOINTED MEMBERS Thomas M. Cramer, President ...................................................... Carlsbad Holm 0. Bursum, Jr., Secretary-Treasurer ........................................ Socorro Frank C. DiLuzio ..................................................................... Los Alamos A. A. Kemnitz .................................................................................... Hobbs Cooper Shapley ............................................................................... Deming Contents Page ABSTRACT .............................................................................................................. 9 INTRODUCTION ............................................................................................... 11 Location, area, and accessibility 11 Previous investigations -
Prairie Dog Empire: a Saga of the Shortgrass Prairie
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln University of Nebraska Press -- Sample Books and Chapters University of Nebraska Press 2005 Prairie Dog Empire: A Saga of the Shortgrass Prairie Paul A. Johnsgard University of Nebraska - Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/unpresssamples Part of the Arts and Humanities Commons Johnsgard, Paul A., "Prairie Dog Empire: A Saga of the Shortgrass Prairie" (2005). University of Nebraska Press -- Sample Books and Chapters. 6. https://digitalcommons.unl.edu/unpresssamples/6 This Article is brought to you for free and open access by the University of Nebraska Press at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in University of Nebraska Press -- Sample Books and Chapters by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. 1 2 3 4 5 6 7 8 9 10 Prairie Dog Empire 11 [First Page] 12 13 [-1], (1) 14 15 Lines: 0 to 22 16 17 ——— 18 * 388.16002pt PgVar ——— 19 Normal Page 20 * PgEnds: PageBreak 21 22 23 [-1], (1) 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 Kim—UofNPress/Pagei//Prairie Dog Empire: A Saga of the Shortgrass Prairie / Paul A. Johnsgard 1 Other Titles by Paul A. Johnsgard 2 Published by the University of Nebraska Press 3 4 Lewis and Clark on the Great Plains: A Natural History 5 The Nature of Nebraska: Ecology and Biodiversity 6 This Fragile Land: A Natural History of the Nebraska Sandhills 7 Crane Music: A Natural History -
The Geology of New Mexico As Understood in 1912: an Essay for the Centennial of New Mexico Statehood Part 2 Barry S
Celebrating New Mexico's Centennial The geology of New Mexico as understood in 1912: an essay for the centennial of New Mexico statehood Part 2 Barry S. Kues, Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico, [email protected] Introduction he first part of this contribution, presented in the February Here I first discuss contemporary ideas on two fundamental areas 2012 issue of New Mexico Geology, laid the groundwork for an of geologic thought—the accurate dating of rocks and the move- exploration of what geologists knew or surmised about the ment of continents through time—that were at the beginning of Tgeology of New Mexico as the territory transitioned into statehood paradigm shifts around 1912. Then I explore research trends and in 1912. Part 1 included an overview of the demographic, economic, the developing state of knowledge in stratigraphy and paleontol- social, cultural, and technological attributes of New Mexico and its ogy, two disciplines of geology that were essential in understand- people a century ago, and a discussion of important individuals, ing New Mexico’s rock record (some 84% of New Mexico’s surface institutions, and areas and methods of research—the geologic envi- area is covered by sediments or sedimentary rocks) and which were ronment, so to speak—that existed in the new state at that time. advancing rapidly through the first decade of the 20th century. The geologic time scale and age of rocks The geologic time scale familiar to geologists working in New The USGS did not adopt the Paleocene as the earliest epoch of the Mexico in 1912 was not greatly different from that used by modern Cenozoic until 1939. -
Cynodonteae Tribe
POACEAE [GRAMINEAE] – GRASS FAMILY Plant: annuals or perennials Stem: jointed stem is termed a culm – internodial stem most often hollow but always solid at node, mostly round, some with stolons (creeping stem) or rhizomes (underground stem) Root: usually fibrous, often very abundant and dense Leaves: mostly linear, sessile, parallel veins, in 2 ranks (vertical rows), leaf sheath usually open or split and often overlapping, but may be closed Flowers: small in 2 rows forming a spikelet (1 to several flowers), may be 1 to many spikelets with pedicels or sessile to stem; each flower within a spikelet is between an outer limna (bract, with a midrib) and an inner palea (bract, 2-nerved or keeled usually) – these 3 parts together make the floret – the 2 bottom bracts of the spikelet do not have flowers and are termed glumes (may be reduced or absent), the rachilla is the axis that hold the florets; sepals and petals absent; 1-6 but often 3 stamens; 1 pistil, 1-3 but usually 2 styles, ovary superior, 1 ovule – there are exceptions to most everything!! Fruit: seed-like grain (seed usually fused to the pericarp (ovary wall) or not) Other: very large and important family; Monocotyledons Group Genera: 600+ genera; locally many genera 2 slides per species WARNING – family descriptions are only a layman’s guide and should not be used as definitive POACEAE [GRAMINEAE] – CYNODONTEAE TRIBE Sideoats Grama; Bouteloua curtipendula (Michx.) Torr. var. curtipendula - Cynodonteae (Tribe) Bermuda Grass; Cynodon dactylon (L.) Pers. (Introduced) - Cynodonteae (Tribe) Egyptian Grass [Durban Crowfoot]; Dactyloctenium aegyptium (L.) Willd (Introduced) [Indian] Goose Grass; Eleusine indica (L.) Gaertn. -
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