Natural Sources of Salinity in the Brazos River, Texas with PARTICULAR REFERENCE to the CROTON and SALT CROTON CREEK BASINS
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Distributions of Extinction Times from Fossil Ages and Tree Topologies: the Example of Some Mid-Permian Synapsid Extinctions Gilles Didier, Michel Laurin
Distributions of extinction times from fossil ages and tree topologies: the example of some mid-Permian synapsid extinctions Gilles Didier, Michel Laurin To cite this version: Gilles Didier, Michel Laurin. Distributions of extinction times from fossil ages and tree topologies: the example of some mid-Permian synapsid extinctions. 2021. hal-03258099v2 HAL Id: hal-03258099 https://hal.archives-ouvertes.fr/hal-03258099v2 Preprint submitted on 20 Sep 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributions of extinction times from fossil ages and tree topologies: the example of some mid-Permian synapsid extinctions Gilles Didier1 and Michel Laurin2 1 IMAG, Univ Montpellier, CNRS, Montpellier, France 2 CR2P (\Centre de Pal´eontologie { Paris"; UMR 7207), CNRS/MNHN/SU, Mus´eumNational d'Histoire Naturelle, Paris, France September 16, 2021 Abstract Given a phylogenetic tree that includes only extinct, or a mix of extinct and extant taxa, where at least some fossil data are available, we present a method to compute the distribution of the extinction time of a given set of taxa under the Fossilized-Birth-Death model. Our approach differs from the previous ones in that it takes into account (i) the possibility that the taxa or the clade considered may diversify before going extinct and (ii) the whole phylogenetic tree to estimate extinction times, whilst previous methods do not consider the diversification process and deal with each branch independently. -
University of Texas Bulletin No
University of Texas Bulletin No. 2607: February IS, 1926 THE SAN ANGELO FORMATION THE GEOLOGY OF FOARD COUNTY J. W. BEEDE AND D. D. CHRISTNER BUREAU OF ECONOMIC GEOLOGY J. A. Udden, Director E. H. Sellards, Associate Director PUBLISHED BY THE UNIVERSITY OF TEXAS AUSTIN Publications of the University of Texas Publications Committee : Frederic Duncalf C. T. McCormick D. G. Cooke E. K.McGinnis J. L.Henderson H. J. MULLER E. J. Mathews Hal G Weaver The University publishes bulletins four times a month, so numbered that the first two digits of the number show the year of issue, the last two the position in the yearly series. (For example, No. 2201 is the first bulletin of the year 1922.) These comprise the official publications of the University, publications on humanistic and scientific sub- jects, bulletins prepared by the Divisionof Extension, by the Bureau of Economic Geology, and other bulletins of general educational interest. With the exception of special num- bers, any bulletin willbe sent to a citizen of Texas free on request. Allcommunications about University publications should be addressed to University Publications, University of Texas, Austin. oiSi§ste> UNIVERSITY OP TEXAS PRESS. AUSTIN University of Texas Bulletin No. 2607: February 15, 1926 THE SAN ANGELO FORMATION THE GEOLOGY OF FOARD COUNTY J. W. BEEDE AND D. D. CHRISTNER BUREAU OF ECONOMIC GEOLOGY J. A. Udden, Director E. H. Sellards, Associate Director PUBLISHED BYTHE UNIVERSITYFOUR TIMES AMONTH,AND ENTERED AS SECOND-CLASS MATTER AT THE POSTOFFICE AT AUSTIN,TEXAS, UNDER THEACT OF AUGUST 24, 1912 The benefits of education and of useful knowledge, generally diffused through a community, are essential to the preservation of a free govern- ment. -
Stream Monitoring and Educational Program in the Red River Basin
Stream Monitoring and Educational U.S. Department of the Interior Program in the Red River Basin, U.S. Geological Survey Texas, 1996–97 100 o 101 o 5 AMARILLO NORTH FORK 102 o RED RIVER 103 o A S LT 35o F ORK RED R IV ER 1 4 2 PRAIRIE DOG TOWN PEASE 3 99 o WICHITA FORK RED RIVER 7 FALLS CHARLIE 6 RIVE R o o 34 W 8 98 9 I R o LAKE CHIT 21 ED 97 A . TEXOMA o VE o 10 11 R 25 96 RI R 95 16 19 18 20 DENISON 17 28 14 15 23 24 27 29 22 26 30 12,13 LAKE PARIS KEMP LAKE LAKE KICKAPOO ARROWHEAD TEXARKANA EXPLANATION 0 40 80 120 MILES Reach 1—Lower Red River (mainstem) Basin Red River Basin in Texas Reach 2—Wichita River Basin NEW OKLAHOMA Reach 3—Pease River Basin MEXICO ARKANSAS Reach 4—Prairie Dog Town Fork Red River Basin Reach 5—North Fork and Salt Fork Red River TEXAS Basins 12 LOUISIANA USGS streamflow-gaging and water-quality station and reference number (table 1) 22 USGS streamflow-gaging station and reference number (table 1) Figure 1. Location of Red River Basin, Texas, and stream-monitoring stations. This fact sheet presents the 1996–97 Texas Panhandle, and becomes the Texas- 200,000 acre-feet are in the basin (fig. 1): stream monitoring and outreach activities Oklahoma boundary. It then flows Lake Kemp, Lake Kickapoo, Lake of the U.S. Geological Survey (USGS), through southwestern Arkansas and into Arrowhead, and Lake Texoma. -
Index of Surface Water Stations in Texas
1 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY I AUSTIN, TEXAS INDEX OF SURFACE WATER STATIONS IN TEXAS Operated by the Water Resources Division of the Geological Survey in cooperation with State and Federal Agencies Gaging Station 08065000. Trinity River near Oakwood , October 1970 UNITED STATES DEPARTMENT OF THE INTERIOR Geological Survey - Water Resources Division INDEX OF SURFACE WATER STATIONS IN TEXAS OCTOBER 1970 Copies of this report may be obtained from District Chief. Water Resources Division U.S. Geological Survey Federal Building Austin. Texas 78701 1970 CONTENTS Page Introduction ............................... ................•.......•...•..... Location of offices .........................................•..•.......... Description of stations................................................... 2 Definition of tenns........... • . 2 ILLUSTRATIONS Location of active gaging stations in Texas, October 1970 .•.•.•.••..•••••..•.. 1n pocket TABLES Table 1. Streamflow, quality, and reservoir-content stations •.•.•... ~........ 3 2. Low-fla.o~ partial-record stations.................................... 18 3. Crest-stage partial-record stations................................. 22 4. Miscellaneous sites................................................. 27 5. Tide-level stations........................ ........................ 28 ii INDEX OF SURFACE WATER STATIONS IN TEXAS OCTOBER 1970 The U.S. Geological Survey's investigations of the water resources of Texas are con ducted in cooperation with the Texas Water Development -
South Texas Electric Cooperative, Inc
CULTURAL RESOURCES REPORT FOR THE PROPOSED RED GATE POWER PLANT AND LATERAL PROJECT, HIDALGO AND STARR COUNTIES, TEXAS INTENSIVE ARCHEOLOGICAL SURVEY Prepared for South Texas Electric Cooperative, Inc by Debra L. Beene, Joseph M. Sanchez, and Timothy B. Griffith Principal Investigators: Brandon S. Young and Timothy B. Griffith AUGUST 2014 CULTURAL RESOURCES REPORT FOR THE PROPOSED RED GATE POWER PLANTAND LATERAL PROJECT HIDALGO AND STARR COUNTIES, TEXAS INTENSIVE ARCHEOLOGICAL SURVEY By Debra L. Beene, Joseph M. Sanchez, and Timothy B. Griffith Prepared for South Texas Electric Cooperative, Inc. Principal Investigators: Brandon S. Young and Timothy B. Griffith August 2014 ABSTRACT Between 2012 and 2014, archeologists from Blanton & Associates, Inc., at the request of the South Texas Electric Cooperative, Inc., conducted an intensive, non-collection, archeological survey of the proposed Red Gate Power Plant project in Hidalgo and Starr Counties, Texas. The area of potential effect (APE) comprised the 336-acre power plant site property in Hidalgo County, and an 891-acre, 24.5-mile proposed natural gas pipeline right-of-way in Hidalgo and Starr Counties. Investigation of the power plant APE discovered one mid to late twentieth century historic residential complex (41HG238), with an associated corral and minor structures. Based on the recent date of construction, lack of integrity, and paucity of buried material, site 41HG238 is recommended as ineligible for inclusion in the National Register of Historic Places (NHRP). Investigation of the pipeline APE did not discover any additional archeological resources. In summary, no NHRP-eligible sites were discovered, no artifacts were collected, and curation was unnecessary. CULTURAL RESOURCES REPORT FOR THE PROPOSED RED GATE POWER PLANT AND i LATERAL PROJECT, HIDALGO AND STARR COUNTIES, TEXAS MANAGEMENT SUMMARY PROJECT TITLE: Cultural Resources Survey for the Proposed Red Gate Power Plant and Lateral Project, Hidalgo and Starr Counties, Texas. -
Stormwater Management Program 2013-2018 Appendix A
Appendix A 2012 Texas Integrated Report - Texas 303(d) List (Category 5) 2012 Texas Integrated Report - Texas 303(d) List (Category 5) As required under Sections 303(d) and 304(a) of the federal Clean Water Act, this list identifies the water bodies in or bordering Texas for which effluent limitations are not stringent enough to implement water quality standards, and for which the associated pollutants are suitable for measurement by maximum daily load. In addition, the TCEQ also develops a schedule identifying Total Maximum Daily Loads (TMDLs) that will be initiated in the next two years for priority impaired waters. Issuance of permits to discharge into 303(d)-listed water bodies is described in the TCEQ regulatory guidance document Procedures to Implement the Texas Surface Water Quality Standards (January 2003, RG-194). Impairments are limited to the geographic area described by the Assessment Unit and identified with a six or seven-digit AU_ID. A TMDL for each impaired parameter will be developed to allocate pollutant loads from contributing sources that affect the parameter of concern in each Assessment Unit. The TMDL will be identified and counted using a six or seven-digit AU_ID. Water Quality permits that are issued before a TMDL is approved will not increase pollutant loading that would contribute to the impairment identified for the Assessment Unit. Explanation of Column Headings SegID and Name: The unique identifier (SegID), segment name, and location of the water body. The SegID may be one of two types of numbers. The first type is a classified segment number (4 digits, e.g., 0218), as defined in Appendix A of the Texas Surface Water Quality Standards (TSWQS). -
Distributions of Extinction Times from Fossil Ages and Tree Topologies: the Example of Some Mid-Permian Synapsid Extinctions
bioRxiv preprint doi: https://doi.org/10.1101/2021.06.11.448028; this version posted June 11, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. Distributions of extinction times from fossil ages and tree topologies: the example of some mid-Permian synapsid extinctions Gilles Didier1 and Michel Laurin2 1IMAG, Univ Montpellier, CNRS, Montpellier, France 2CR2P (“Centre de Recherches sur la Paléobiodiversité et les Paléoenvironnements”; UMR 7207), CNRS/MNHN/UPMC, Sorbonne Université, Muséum National d’Histoire Naturelle, Paris, France June 11, 2021 Abstract Given a phylogenetic tree of extinct and extant taxa with fossils where the only temporal infor- mation stands in the fossil ages, we devise a method to compute the distribution of the extinction time of a given set of taxa under the Fossilized-Birth-Death model. Our approach differs from the previous ones in that it takes into account the possibility that the taxa or the clade considered may diversify before going extinct, whilst previous methods just rely on the fossil recovery rate to estimate confidence intervals. We assess and compare our new approach with a standard previous one using simulated data. Results show that our method provides more accurate confidence intervals. This new approach is applied to the study of the extinction time of three Permo-Carboniferous synapsid taxa (Ophiacodontidae, Edaphosauridae, and Sphenacodontidae) that are thought to have disappeared toward the end of the Cisuralian, or possibly shortly thereafter. The timing of extinctions of these three taxa and of their component lineages supports the idea that a biological crisis occurred in the late Kungurian/early Roadian. -
Application and Utility of a Low-Cost Unmanned Aerial System to Manage and Conserve Aquatic Resources in Four Texas Rivers
Application and Utility of a Low-cost Unmanned Aerial System to Manage and Conserve Aquatic Resources in Four Texas Rivers Timothy W. Birdsong, Texas Parks and Wildlife Department, 4200 Smith School Road, Austin, TX 78744 Megan Bean, Texas Parks and Wildlife Department, 5103 Junction Highway, Mountain Home, TX 78058 Timothy B. Grabowski, U.S. Geological Survey, Texas Cooperative Fish and Wildlife Research Unit, Texas Tech University, Agricultural Sciences Building Room 218, MS 2120, Lubbock, TX 79409 Thomas B. Hardy, Texas State University – San Marcos, 951 Aquarena Springs Drive, San Marcos, TX 78666 Thomas Heard, Texas State University – San Marcos, 951 Aquarena Springs Drive, San Marcos, TX 78666 Derrick Holdstock, Texas Parks and Wildlife Department, 3036 FM 3256, Paducah, TX 79248 Kristy Kollaus, Texas State University – San Marcos, 951 Aquarena Springs Drive, San Marcos, TX 78666 Stephan Magnelia, Texas Parks and Wildlife Department, P.O. Box 1685, San Marcos, TX 78745 Kristina Tolman, Texas State University – San Marcos, 951 Aquarena Springs Drive, San Marcos, TX 78666 Abstract: Low-cost unmanned aerial systems (UAS) have recently gained increasing attention in natural resources management due to their versatility and demonstrated utility in collection of high-resolution, temporally-specific geospatial data. This study applied low-cost UAS to support the geospatial data needs of aquatic resources management projects in four Texas rivers. Specifically, a UAS was used to (1) map invasive salt cedar (multiple species in the genus Tamarix) that have degraded instream habitat conditions in the Pease River, (2) map instream meso-habitats and structural habitat features (e.g., boulders, woody debris) in the South Llano River as a baseline prior to watershed-scale habitat improvements, (3) map enduring pools in the Blanco River during drought conditions to guide smallmouth bass removal efforts, and (4) quantify river use by anglers in the Guadalupe River. -
Beetle - Mania Is a Ne Wsletter on Biological Control of Saltcedar in Texas, and Is Written and Produced by Allen Knutson , Texas A&M Agrilife Extension
BEETLE - MANIA IS A NE WSLETTER ON BIOLOGICAL CONTROL OF SALTCEDAR IN TEXAS, AND IS WRITTEN AND PRODUCED BY ALLEN KNUTSON , TEXAS A&M AGRILIFE EXTENSION. TO BE INCLUDED ON THE MAILING LIST, PLEASE CONTACT ALLEN KNUTSON. BEETLE - MANIA BIOLOGICAL CONTROL OF SALTCEDAR IN TEXAS VOL. 4 NO. 2 SUMMER - F A L L 2 0 1 2 2012. 2012. A A Very Very Good Good Year Year for for : TamariskSaltcedar Leaf Leaf Beetles Beetles in in Texas Texas ! ! The saltcedar leaf beetle feeds only on During 2012, saltcedar leaf seem to favor increase of river miles. However, follow- beetle populations increased saltcedar leaf beetles. If the ing the prolonged freeze, of saltcedar and athel. and dispersed at many loca- winter of 2012-2013 is again February 2011, none were Athel is a closely tions across the state and mild, leaf beetles should re- found and this species is now related species that more saltcedar trees were turn in force next year. believed to be absent from this grows along the Rio defoliated than ever before. There are now three spe- region. A second species, the After the early February cies of leaf beetle established subtropical leaf beetle Grande River in 2011 freeze, beetle popula- in Texas; the Uzbek beetle in (Tunisian) was released at five Texas. tions were low or absent at the Panhandle, the Mediterra- sites on the Pecos River in many sites last summer. nean (Crete) leaf beetle on 2010-2011 and quickly estab- However, the mild winter of the Upper Colorado River, lished and increased. During If saltcedar or 2011-2012 favored survival of and the subtropical leaf beetle 2012, this species, originally athel trees are not overwintering beetles. -
Comanche Peak Units 3 and 4 COLA
Comanche Peak Nuclear Power Plant, Units 3 & 4 COL Application Part 3 - Environmental Report CHAPTER 2 ENVIRONMENTAL DESCRIPTION TABLE OF CONTENTS Section Title Page 2.0 ENVIRONMENTAL DESCRIPTION............................................................................ 2.0-1 2.1 STATION LOCATION ................................................................................................. 2.1-1 2.1.1 REFERENCES..................................................................................................... 2.1-2 2.2 LAND........................................................................................................................... 2.2-1 2.2.1 THE SITE AND VICINITY .................................................................................... 2.2-1 2.2.1.1 The Site........................................................................................................... 2.2-1 2.2.1.2 The Vicinity...................................................................................................... 2.2-2 2.2.2 TRANSMISSION CORRIDORS AND OFF-SITE AREAS..................................... 2.2-5 2.2.3 THE REGION........................................................................................................ 2.2-6 2.2.4 REFERENCES:..................................................................................................... 2.2-7 2.3 WATER ...................................................................................................................... 2.3-1 2.3.1 HYDROLOGY ...................................................................................................... -
Matching the Hatch for the TX Hill Country[2]
MATCHING THE HATCH FOR THE TX HILL COUNTRY Tying and choosing proper fly patterns to increase your success on the water. Matt Bennett Fly Geek Custom Flies [email protected] Why should you listen to me? • Fishing the Austin area since 2008 • LWFF – 2012 through 2015 • Fly Geek Custom Flies – 2015 – now • Past Austin Fly Fishers President • Current TX Council Vice President Overview of the TX Hill Country Llano River near Kingsland Guadalupe River at Lazy L&L Brushy Creek near Round Rock Characteristics of Hill Country Rivers ¨ There’s a bunch! Guadalupe, Comal, San Marcos, Colorado, Llano, Blanco, Nueces, Frio, Sabinal, Concho, Lampasas and associated feeder creeks ¨ Majority are shallow and wadeable in stretches ¨ Extremely Clear Water (some clearer than others) ¨ Sandy, limestone and granite bottoms with lots of granite boulders/outcroppings ¨ Extreme flooding events YEARLY on average. Sept 11, 1952 – Lake Travis rises 57 feet in 14 hours. 23-26” of rain Guadalupe River, July 17,1987 Llano River / Lake LBJ – Nov. 4 2000 Why does flooding matter to fishing? ¨ Because of the almost-annual flooding / drought cycle of our rivers, they are constantly changing ¨ Holes get filled in and dug out, gravel gets moved around, banks get undercut ¨ We have to constantly relearn our fisheries to stay successful on the water ¨ Choosing the right flies with the proper triggers is an important part of your success on the water Overview of our forage Baitfish, crawfish, insects, and other terrestrials Why is forage important? ¨ #1 rule of all fishing – know your forage! ¨ Knowing the common forage where you fish increases your chances of success as it clues you in on what flies you should be fishing ¨ Forage base will vary between water bodies, time of year, species targeted, and more, as well as year-to-year. -
1 Supplementary Materials and Methods 1 S1 Expanded
1 Supplementary Materials and Methods 2 S1 Expanded Geologic and Paleogeographic Information 3 The carbonate nodules from Montañez et al., (2007) utilized in this study were collected from well-developed and 4 drained paleosols from: 1) the Eastern Shelf of the Midland Basin (N.C. Texas), 2) Paradox Basin (S.E. Utah), 3) Pedregosa 5 Basin (S.C. New Mexico), 4) Anadarko Basin (S.C. Oklahoma), and 5) the Grand Canyon Embayment (N.C. Arizona) (Fig. 6 1a; Richey et al., (2020)). The plant cuticle fossils come from localities in: 1) N.C. Texas (Lower Pease River [LPR], Lake 7 Kemp Dam [LKD], Parkey’s Oil Patch [POP], and Mitchell Creek [MC]; all representing localities that also provided 8 carbonate nodules or plant organic matter [POM] for Montañez et al., (2007), 2) N.C. New Mexico (Kinney Brick Quarry 9 [KB]), 3) S.E. Kansas (Hamilton Quarry [HQ]), 4) S.E. Illinois (Lake Sara Limestone [LSL]), and 5) S.W. Indiana (sub- 10 Minshall [SM]) (Fig. 1a, S2–4; Richey et al., (2020)). These localities span a wide portion of the western equatorial portion 11 of Euramerica during the latest Pennsylvanian through middle Permian (Fig. 1b). 12 13 S2 Biostratigraphic Correlations and Age Model 14 N.C. Texas stratigraphy and the position of pedogenic carbonate samples from Montañez et al., (2007) and cuticle were 15 inferred from N.C. Texas conodont biostratigraphy and its relation to Permian global conodont biostratigraphy (Tabor and 16 Montañez, 2004; Wardlaw, 2005; Henderson, 2018). The specific correlations used are (C. Henderson, personal 17 communication, August 2019): (1) The Stockwether Limestone Member of the Pueblo Formation contains Idiognathodus 18 isolatus, indicating that the Carboniferous-Permian boundary (298.9 Ma) and base of the Asselian resides in the Stockwether 19 Limestone (Wardlaw, 2005).