cometadata/datacite-rtg-text-other-reclassification-records huggingface dataset:
A constraint-based analysis of the intonational realization of focus in Northern Bizkaian Basque
Creators: name: Gorka, Elordieta
Publisher: name: Walter de Gruyter
Year: 2007

description: This paper analyzes patterns of prosodic prominence and intonational phrasing of narrowly focused words in a variety of Northern Bizkaian Basque. One type of speaker can only single out words intonationally if they are accented and constitute APs by themselves, while the other type can have prominence on any word which is accented, regardless of whether it constitutes an AP by itself. Lexically unaccented words which fail to get a derived pitch accent by occurring immediately before the verb cannot be singled out, and are pronouncedin the same AP with the following word. These restrictions are analyzed in the framework of Optimality Theory, and are shown to derive from the interplay of five constraints. A constraint penalizing the insertion of accents dominates the constraint that demands that contrastively focalized words are intonationally singled out. This accounts for the impossibility of highlighting a lexically unaccented word unless it gets a derived accent. The difference between the two types of speakers is explained as a difference in the relativeranking of two other constraints. One of these enforces the alignment of thetonal sequence %L H- with the left edge of an AP, and of a pitch accent withthe right edge of an AP. The other requires the presence of an ip-boundary atthe left edge of the focused word. More restrictive speakers rank the formerhigher than the latter, and less restrictive speakers have the opposite ranking.
title: Geology of Hood Spring quadrangle, Brewster County, Texas
Creators: name: Graves, Roy William
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1954
Subjects: subject: Geology -- Texas -- Brewster County

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: RI0021. Accompanied by 3 fold-outs. Plate I : Geologic map and structure sections of Hood Spring quadrangle, Texas. Plate VII : Geologic map and structure sections of Maravillas Creek area, Hood Spring quadrangle, Texas. Plate VIII : Geologic map and structure sections of Tinaja Range area, Hood Spring quadrangle, Texas
description: The Hood Spring quadrangle, in the central part of Brewster County, Texas, contains a segment of the southeast rim of the Marathon basin. It includes a part of the complexly folded and faulted Paleozoic rocks that occur in the center of the Marathon basin and also includes Cretaceous rocks exposed in the Maravillas scarp. This scarp has three stratigraphically separate cuestas that are formed by southeastward gently dipping beds. The southwestern corner of the quadrangle contains a faulted and folded segment of the Santiago Mountain range. Rocks of Cambrian (Dagger Flat formation), Ordovician (Marathon, Alsate, Fort Pena, Woods Hollow, and Maravillas formations), Devonian (Caballos novaculite), and Pennsylvanian (Tesnus formation)ages occur in the area of Paleozoic outcrops. A conodont fauna from the upper part of the Caballos novaculite indicates a Middle to Upper Devonian age for those beds. Most of the Cretaceous rocks exposed in the quadrangle belong to the Comanche series (Glen Rose, Maxon, Walnut-ComanchePeak, Edwards, Kiamichi, Georgetown, Grayson, and Buda formations) and are similar to equivalent age strata in central Texas. Gulf series rocks (Boquillas and Terlingua formations) have a restricted occurrence in the southwestern corner of the quadrangle contains a faulted and folded segment of the Santiago Mountain range. Tertiary intrusions include plugs, dikes, and sills of rhyolite, trachyte, and basalt which cut Cretaceous and Paleozoic rocks. These intrusives belong to the southern Trans-Pecos Texas suite of alkalic igneous rocks.
Cuon alpinus
Creators: name: Jo, Yeong-Seok
name: Baccus, John T.
name: Koprowski, John L.
Publisher: name: Zenodo
Year: 2018
Subjects: Biodiversity
Taxonomy
Animalia
Chordata
Mammalia
Carnivora
Canidae
Cuon
Cuon alpinus

description: Cuon alpinus (Pallas, 1811) —Dhole
Canis alpinus Pallas, 1811 p.34; Type locality- Amur, Russia.
Cuon alpinus: Kishida & Mori, 1931 p.379; Kuroda, 1938 p.37; Ellerman & Morrison-Scott, 1951 p.233; Won, 1968 p.268; Han, 1994 p.46; Won & Smith, 1999 p.15.
Cuon alpinus alpinus: Won, 1968 p.268; Yoon, 1992 p.97.
Range: The original distribution of the dhole ranged throughout the Korean Peninsula (Jo & Baccus 2015). Presence of dholes around Mt. Baekdu (3 individuals observed in 1988 at Chail-peak Plateau) in extreme northeastern Korea were reported until the 1990s (Jin & Ouh 1990; Fig. 57), but the current status of dholes remains uncertain.
Remarks: The populations of northeastern Asia -including Korea- were classified as C. a. alpinus (Pallas, 1811).
Conservation status: The North Korean government designated C. alpinus as an Endangered Species (MAB National Committee of DPR Korea 2002; Democratic People’s Republic of Korea 2007). The South Korean population became exterminated before the 1970s, with no conservation action taking place in South Korea (Jo & Baccus 2015). All populations of northeastern Asia are considered extinct (Venkataraman & Johnsingh 2004). CITES lists the species on Appendix II.
description: Published as part of Jo, Yeong-Seok, Baccus, John T. & Koprowski, John L., 2018, Mammals of Korea: a review of their taxonomy, distribution and conservation status, pp. 1-216 in Zootaxa 4522 (1) on pages 88-89, DOI: 10.11646/zootaxa.4522.1.1, http://zenodo.org/record/2610198
title: Correlation between surface and subsurface sections of the Ellenburger group of Texas
title: Ellenburger group of Texas
titleType: AlternativeTitle
Creators: name: Hendricks, Leo
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1952
Subjects: subject: Geology, Stratigraphic -- Ordovician

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: RI0011. Accompanied by 6 foldouts. Plate I : Index map of Llano uplift showing area where Ellenburger has been mapped in detail by Cloud and Barnes. Plate II : Correlation of Ellenburger Sections in Central Texas. Plate III : Correlation of Ellenburger Sections from Central to North Texas. Plate IV : Correlations of Ellenburger Sections across North-Central Texas. Plate V : Correlations of Ellenburger Sections from Central to West Texas. Plate VI : Regional Correlation of the Ellenburger Group (from Cloud and Barnes, 1946)
description: The Ellenburger of Texas was first defined as a marine limestone formation of Cambrian and Ordovician age (Paige, 1912), but recently it has been subdivided into several formations and the term Ellenburger given group status (Cloud and Barnes, 1948). The group forms an important unit in the geology of Texas, its known extent in both surface and subsurface covering approximately one-half of the State (fig. 1). Consequently the Ellenburger has received the attention of many geologists over a period of more than forty years. The greatest amount of information concerning the Ellenburger has come from wells drilled in exploration for oil and gas. This information from the subsurface is the basis for present concepts of the lateral extent and regional changes m thickness and lithologic character of the group (Sellards, 1933b). The top of the group serves as an important key horizon for mapping structure in the subsurface of large parts of north, central, and southwest Texas (Sellards and Hendricks, 1946). Data from well samples and cores have been used to make qualitative subdivisions and correlations within the formation (Cole, 1942, p. 1398; Crowley and Hendricks, 1945, p. 413). No paleontological correlations are possible from well data because well samples and cores from the Ellenburger are practically barren of fossils.
title: Geology of Cathedral Mountain quadrangle, Brewster County, Texas
Creators: name: McAnulty, William Noel, 1913-
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1955
Subjects: subject: Geology -- Texas -- Brewster County

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: RI0025. Accompanied by 1 foldout. Plate 1 : Geologic Map of Cathedral Mountain Quadrangle, Brewster County, Texas, with structure sections. Reprinted from Bulletin of the Geological Society of America, vol. 66, no. 5, May, 1955
description: Rocks exposed in the Cathedral Mountain quadrangle in the southeastern DavisMountains of Trans-Pecos Texas are assigned to the Word formation and to Capitan limestone in the Permian Guadalupe series; to the Maxon sandstone, Edwards limestone, Georgetown limestone, and Grayson (Del Rio) marl in the Cretaceous Comanche series; to the Buda limestone and Boquillas limestone in the Cretaceous Gulf series; and to the Buck Hill volcanic series in the Tertiary. Volcanic rocks up to 4600 feet thick cover most of the quadrangle. The volcanic succession, similar to that in Buck Hill and other quadrangles to the south, is divided into the Pruett tuff, Crossen trachyte, Sheep Canyon basalt, Potato Hill andesite, Cottonwood Spring basalt, Duff formation, and Rawls basalt. Vertebrate fossils indicate a late Eocene (Duchesne) age for the Pruett tuff (restricted to the lowermost tuff, sandstone, and conglomerate beds). The top of the Eocene is placed at a prominent disconformity between the Crossen trachyte and the Sheep Canyon basalt; it is suggested the overlying lava and tuff layers are Oligocene and younger (?). Some of the many intrusive bodies of alkalic microsyenite which are younger than the volcanic rocks have effected much local deformation of the layered rocks. Quaternary alluvium is present along streams and over valley flats. Northward across the quadrangle, the Crossen trachyte gains appreciable quartz, the Potato Hill andesite changes from highly porphyritic to nonporphyritic, and the Duff formation changes from dominantly rhyolite tuff to lava, tuff, and conglomerate (Decie member). Effects of five crustal disturbances mid-Mesozoic, late Cretaceous, pre-upper Eocene, and three in the late Cenozoic are apparent. Differential erosion of the intruded, folded, and faulted volcanic succession has roughened and diversified the landscape.
Additional file 6: Figure S2. of Unraveling the evolution and coevolution of small regulatory RNAs and coding genes in Listeria
Creators: name: Cerutti, Franck
name: Mallet, Ludovic
name: Painset, Anaïs
name: Hoede, Claire
name: Moisan, Annick
name: Bécavin, Christophe
name: Duval, Mélodie
name: Dussurget, Olivier
name: Cossart, Pascale
name: Gaspin, Christine
name: Chiapello, Hélène
Publisher: name: Figshare
Year: 2017
Subjects: subject: Biochemistry
subject: Medicine
subject: Microbiology
subject: FOS: Biological sciences
subject: Genetics
subject: Evolutionary Biology
subject: 69999 Biological Sciences not elsewhere classified
subject: 110309 Infectious Diseases
subject: FOS: Health sciences
subject: 60506 Virology
subject: Computational Biology

description: Multiple alignment of rli133. This figure represents the multiple alignment of rli133 sequences in strains where it is present. Red denotes a fully conserved position. The phylogenetic tree at the left corresponds to a Maximum Likelihood tree computed from the corresponding multiple alignment. (PDF 1413 kb)
title: Geology of Agua Fria quadrangle, Brewster County, Texas
Creators: name: Moon, C. Gardley
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1953
Subjects: subject: Geology -- Texas -- Brewster County

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: RI0015. "Reprinted from Bulletin of the Geological Society of America, vol. 64, no. 2, February 1953."
description: The 15-minute Agua Fria quadrangle in southwestern Brewster County, Texas, is arid, sparsely vegetated, and includes diverse topographic features that result chiefly from complex structure and variation in rock resistance to erosion. The mountainous and more complicated southern part of the area has suffered much deformation by igneous intrusions and faulting. The Comanche series is represented by the Devils River limestone, Grayson marl, and Buda limestone. A disconformity separates it from the overlying gradational Gulf series which consists of the Boquillas,Terlingua, and Aguja formations. Because the Boquillas-Terlingua boundary problem is critical and unsettled, lithologic members and paleontologic zones in that section are described in considerable detail. A distinctive 50-foot rock unit, herein named the Fizzle Flat lentil, occurs about the middle of the Boquillas-Terlingua sequence. A widespread angular unconformity separates the Gulf series from the Tertiary Buck Hill volcanic series. Quaternary terrace gravels occur at different levels, and other alluvial deposits have been mapped. The Tertiary hypabyssal igneous rocks are alkalic and form stocks, laccoliths, plugs, sills, dikes, and bysmaliths or trap-door domes. Several lava flows are preserved in the southwest part of the quadrangle. Metamorphic effects generally are slight. The area is part of the Big Bend sunken block. Except where influenced by intrusive masses, a pattern of northwesterly normal faults establishes the structural trend of the area. Step faults are common. Most of the major faults are downthrown to the southwest with the huge intervening blocks tilted gently to the northeast. That much of the fault pattern was established during the Laramide revolution and that faulting recurred along the old lines of weakness fairly late in Tertiary time are postulated.
Tachyagetes cinerascens
Creators: name: Gadallah, Neveen S.
name: Schmid-Egger, Christian
name: Brothers, Denis J.
Publisher: name: Zenodo
Year: 2020
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Hymenoptera
Pompilidae
Tachyagetes
Tachyagetes cinerascens

description: Tachyagetes cinerascens (Saunders, 1901)
Distribution in the Arabian Peninsula: United Arab Emirates (Schmid-Egger 2017).
Extralimital distribution: Malta, North Africa (Schmid-Egger 2017).
description: Published as part of Gadallah, Neveen S., Schmid-Egger, Christian & Brothers, Denis J., 2020, Biodiversity of the aculeate wasps (Hymenoptera: Aculeata) of the Arabian Peninsula: Vespoidea, Pompilidae, pp. 153-173 in Zootaxa 4754 (1) on page 166, DOI: 10.11646/zootaxa.4754.1.16, http://zenodo.org/record/3719039
title: Cretaceous of Llano Estacado of Texas
Creators: name: Brand, John Paul
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1953
Subjects: subject: Geology -- Llano Estacado
subject: Geology, Stratigraphic -- Cretaceous

description: Issued also as Thesis (Ph. D.), University of Texas, 1952.
description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: RI0020. Issued also as Thesis (Ph. D.), University of Texas, 1952.
description: Rocks of Cretaceous age crop out along the western margins of the deeper playa basins and along the southern and southeastern margins of the Llano Estacado. The Trinity group, containing only the Paluxy sandstone; the Fredericksburg group, consisting of the Walnut, Comanche Peak, Edwards, and Kiamichi formations; and the Washita group, containing only a portion of the Duck Creek formation, have been identified in the Llano Estacado. Formations of the Trinity and Fredericksburg groups are similar lithologically and paleontologically to equivalent units in the Callahan Divide and in the northern edge of the Edwards Plateau. Zonations, applicable to northern and central Texas and Pecos County, Texas, can be extended to the isolated Cretaceous exposures in the Llano Estacado. Cretaceous strata in the Llano Estacado dip to the southeast at the rate of 7 to 8 feet per mile. Structures in the underlying Triassic and Paleozoic do not appear to be reflected in Cretaceous strata. Likewise, the locations of the isolated Cretaceous remnants do not appear to be governed by known structures in underlying units. The Comanche Peak and Edwards limestone and the Kiamichi and Duck Creek shales are chemically suitable for the manufacture of Portland cement. The Edwards limestone is a suitable road ballast material. The sand and gravel of the Paluxy formation could be utilized in concrete aggregate.
Simultaneous input and state estimation for systems with arbitrary inherent delay
Creators: name: Smith, Malcolm
name: Gakis, Grigorios
Publisher: name: Apollo - University of Cambridge Repository
Year: 2025

description: The purpose of this paper is to present a filtering algorithm for simultaneous input and state estimation for linear discrete-time systems of any inherent delay. It generalises previous work which was restricted to systems with an inherent delay of less than or equal to one. The algorithm includes the Kalman filter which is itself a special case of a system with an inherent delay of zero. The approach uses a standard characterisation of a system’s inherent delay in terms of its rank indices. Two judiciously chosen rank decompositions of a Toeplitz matrix of the system’s Markov parameters are used to develop the algorithm. The filter is illustrated on a simple two–mass system with an inherent delay of two.
Canis Linnaeus 1758
Creators: name: Jo, Yeong-Seok
name: Baccus, John T.
name: Koprowski, John L.
Publisher: name: Zenodo
Year: 2018
Subjects: Biodiversity
Taxonomy
Animalia
Chordata
Mammalia
Carnivora
Canidae
Canis

description: Genus Canis Linnaeus, 1758
A single species C. lupus occurred in Korea.
description: Published as part of Jo, Yeong-Seok, Baccus, John T. & Koprowski, John L., 2018, Mammals of Korea: a review of their taxonomy, distribution and conservation status, pp. 1-216 in Zootaxa 4522 (1) on page 90, DOI: 10.11646/zootaxa.4522.1.1, http://zenodo.org/record/2610198
Toxodera Audinet-Serville 1869
Creators: name: Schwarz, Christian J.
name: Konopik, Oliver
Publisher: name: Zenodo
Year: 2014
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Mantodea
Toxoderidae
Toxodera

description: Toxodera Audinet-Serville, 1869
= Eutoxodera Werner, 1930
Highly specialized stick mimics. There are four confirmed species in Borneo restricted to old-growth forests; all are rarely found. The SE Asian Toxoderini, recently revised by Roy (2009b), are understorey dwellers, other aspects of their ecology are, however, completely unknown. Males may be attracted to lights.
Toxodera maculata Ouwens, 1913
= Toxodera vana Yang, 1997
Distribution. S China, Laos, Thailand, Malay Peninsula, Sumatra, Java, Borneo (Roy 2009b).
Toxodera fimbriata Werner, 1930
= Toxodera spinigera Beier, 1931
Distribution. Myanmar, Malay Peninsula, Sumatra, Borneo (Roy 2009b). Bornean records. Sabah: Kinabalu (Beier 1931).
Toxodera maxima Roy, 2009
Distribution. Malay Peninsula, Borneo (Roy 2009b).
Bornean records. Sabah: Danum Valley (CSUB, living specimen depicted in Roy 2009b, page 105) Remarks. Females up to 168 mm long. This species was previously confused with Toxodera denticulata Audinet-Serville, 1837. A damaged specimen found in the SMSM collection deposited under this name may belong to T. maxima. Definite records of T. denticulata from Borneo are lacking.
Toxodera hauseri Roy, 2009
Distribution. Thailand, Malay Peninsula, Java, Borneo (Roy 2009b). Remarks. Roy (2009b) does not mention any Bornean specimen, but there is a photographic record of this species from Poring Hot Springs (Anker, pers. com.).
description: Published as part of Schwarz, Christian J. & Konopik, Oliver, 2014, An annotated checklist of the praYing mantises (Mantodea) of Borneo, including the results of the 2008 scientific expedition to Lanjak Entimau Wildlife SanctuarY, Sarawak, pp. 130-168 in Zootaxa 3797 (1) on page 155, DOI: 10.11646/zootaxa.3797.1.12, http://zenodo.org/record/226038
title: Mineral resources of south Texas, region served through the Port of Corpus Christi
Creators: name: Maxwell, Ross A.
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1962
Subjects: subject: Mines and mineral resources -- Texas

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: RI0043. Part of illustrative matter in pocket. Includes bibliographies.
description: This report is a compilation of all available data on mineral resources (exclusive of oil and gas) in 39 south Texas counties. Information from published and unpublished sources was checked and supplemented by field investigations. The study was carried out in cooperation with the Corpus Christi Chamber of Commerce to provide an inventory of mineral resources in the trade area served through the Port of Corpus Christi.The rock and mineral resources in the northwestern part of the trade area in and associated with Cretaceous formations include high-calcium limestone, Portland cement materials, clay for structural clay products, asphaltic limestone, gravel, and limited amounts of low-grade manganese, barite, celestite, and guano. The principal mineral resources in the Tertiary and Quaternary formations of the Gulf Coastal Plain are uranium minerals, industrial sand, gravel, bleaching clay, drilling mud, expanded clay aggregate, structural clay products materials, caliche for road surfacing, crushed stone, peat, lignite, bituminous and cannel coal, salt, gypsum, sulfur, and oyster shell.
Using local constraint conjunction to discover constraints: the case of Mandarin Chinese
Creators: name: Van De Weijer, Jeroen M.
Publisher: name: Walter de Gruyter
Year: 2012

description: This paper discusses a restriction in synchronic Mandarin Chinese which involves voiced stops, rising tone and nasal codas. The paper argues that this restriction can be described only as the result of the combined action of two constraints, i.e. a 'local constraint conjunction'. We discuss the exact formulation of this conjunction and note that, in Optimality Theory, the two constraints in a conjunction should also be instantiated separately. In this way, local constraint conjunctions provide a novel way of discovering constraints.
Tachyagetes deserticus
Creators: name: Gadallah, Neveen S.
name: Schmid-Egger, Christian
name: Brothers, Denis J.
Publisher: name: Zenodo
Year: 2020
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Hymenoptera
Pompilidae
Tachyagetes
Tachyagetes deserticus

description: Tachyagetes deserticus (Priesner, 1955)
Distribution in the Arabian Peninsula: Bahrain, Oman, United Arab Emirates (Wolf 1986).
Extralimital distribution: Italy, North Africa (Priesner 1955; Wolf 1970a, 1986, 2004a).
description: Published as part of Gadallah, Neveen S., Schmid-Egger, Christian & Brothers, Denis J., 2020, Biodiversity of the aculeate wasps (Hymenoptera: Aculeata) of the Arabian Peninsula: Vespoidea, Pompilidae, pp. 153-173 in Zootaxa 4754 (1) on page 166, DOI: 10.11646/zootaxa.4754.1.16, http://zenodo.org/record/3719039
title: Devonian-Mississippian transition in central Texas
Creators: name: Cloud, Preston, 1912-1991
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1957
Subjects: subject: Geology -- Texas
subject: Geology, Stratigraphic -- Paleozoic

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: RI0031. Reprinted from Bulletin of the Geological Society of America, vol. 68, no. 7, July, 1957. Key sections of the Houy formation (fold. sheet) inserted.
description: The Devonian-Mississippian transition outcrops of central Texas are here described summarily and assigned to a new stratigraphic unit, the Houy Formation. The beds included are mainly Upper Devonian, but partly Lower Mississippian. Locally a basal fraction may be Middle Devonian. Although the deposits included are diverse and their associations complex, the maximum surface thickness so far known is only about 17 feet. The principal subdivisions, in their usual ascending order, are the Ives Breccia Member (Plummer in Bullard and Plummer, 1939), the Doublehorn Shale Member (new), and a thin unnamed phosphoritic interval. Commonly, however, one or more of these members is absent, and rocks not assigned to any member are present. The Ives Breccia Member includes lag deposits of detrital chert of varied age and source. The Doublehorn Shale Member includes black, fissile, spore-bearing shale of Late Devonian age which in a few exposures grades upward into shale of Early Mississippian age. The phosphatic beds are partly Late Devonian and partly Early Mississippian. Remnants of the Doublehorn Shale Member have been found only along the eastern side of the Llano region, but the other units are more widely distributed, and rocks assignable to the Houy Formation are to be looked for between Ordovician and Upper Mississippian deposits anywhere around the Llano region. Although most abundant in the upper beds, phosphatic inclusions occur locally throughout the Houy Formation. This gives a stamp of unity to the sequence and distinguishes it from the immediately underlying beds as well as from the overlying Chappel Limestone of later Early Mississippian age. The Houy is also a unit of more than average radioactivity and is readily detected in the subsurface by radioactive drill-hole logging. It correlates with the Late Devonian and earliest Mississippian black-shale sequences of other Midcontinent and Midwestern areas. Four of the six conodont zones (Hass, 1947; 1956a; 1956b) in deposits of this age in Ohio, Tennessee, Oklahoma, and Arkansas are recognized also in central Texas.
Additional file 1: of “Is it menopause or bipolar?”: a qualitative study of the experience of menopause for women with bipolar disorder
Creators: name: Perich, Tania
name: Ussher, Jane
name: Parton, Chloe
Publisher: name: Figshare
Year: 2017
Subjects: subject: Microbiology
subject: FOS: Biological sciences
subject: Sociology
subject: FOS: Sociology
subject: 69999 Biological Sciences not elsewhere classified
subject: 19999 Mathematical Sciences not elsewhere classified
subject: FOS: Mathematics
subject: Developmental Biology
subject: 111714 Mental Health
subject: FOS: Health sciences

description: Consolidated criteria for reporting qualitative studies. (DOCX 14 kb)
title: Comanchean stratigraphy of Kent Quadrangle, Trans-Pecos Texas
Creators: name: Brand, John Paul
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1958
Subjects: subject: Geology -- Texas
subject: Geology, Stratigraphic -- Cretaceous

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: RI0034. "Reprinted from Bulletin of the American Association of Petroleum Geologists, vol. 42, no. 2, February, 1958."
description: At the northern end of the Coahuila platform, the thinned Comanchean sequence consists of the newly named Sixshooter group of carbonate formations underlain by the newly named Yearwood formation. The Sixshooter group consists, in descending order, of the Buda limestone, the newly named Boracho limestone composed of the newly named San Martine and Levinson members, and the Finlay limestone at the base. Beneath the Finlay is the Cox sandstone, and beneath the Cox, the Yearwood formation, which consists of an upper limestone member previously called Rustler (Permian) and a basal conglomeratic sandstone member that rests unconformably on Permian formations. The Buda and Boracho are biostratigraphically correlative with the Washita group of central Texas; similarly, the basal part of the Levinson member and all the Finlay limestone are correlative with Fredericksburg formations. Whether any part of the Cox sandstone is contemporaneous with the Trinity group is speculative. The Yearwood is probably a Trinity, though possibly a Fredericksburg, correlative.
title: Studies of Cenozoic geology along eastern margin of Texas High Plains, Armstrong to Howard Counties
Creators: name: Frye, John Chapman, 1912-
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1957
Subjects: subject: Geology -- Texas
subject: Geology, Stratigraphic -- Cenozoic

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: RI0032.
description: The eastern margin of the High Plains in central western Texas affords particularly good opportunity for study of late Cenozoic geology. The topography of the area is dominated by the southernmost segment of the late Tertiary mantle of fluvial sediments, isolated from the central and northern High Plains by the valley of the Canadian River. The eastern escarpment presents many exposures and the canyons that extend into the plains contain, in addition, a nearly complete sequence of Pleistocene terraces and deposits. The Canadian River, which crosses the Texas Panhandle north of the area under study, flows by way of the Arkansas River to the Mississippi. However, in the Plains to the south are the headwaters of drainage to Red River (which enters the Mississippi just above its delta) and of the Brazos and the Colorado rivers, each of which takes its independent course to the Gulf of Mexico. Therefore, the Pleistocene histories of adjacent High Plains canyons are indicative of independent drainage systems. These geographic relationships that place nearby streams under control of three different base level situations give special significance to late Cenozoic correlations in this region. Field work on which this report is based has been discontinuously distributed over a decade. Several short periods were spent in the field from 1945 through 1949 when work was directed primarily toward correlation of Kansan age deposits with deposits in the northern Great Plains and with the glacial section of the Mid-West. This study was carried on largely by use of the distinctive petrography of the Pearlette volcanic ash bed and by fossil molluscan faunas (Frye, Swineford, and Leonard, 1948), but was accompanied by a reconnaissance of Pliocene and Pleistocene stratigraphy of the region. Field work directed specifically toward the present report consisted of several weeks in the fall of 1954 and summers of 1955 and 1956 under the auspices of the Bureau of EconomicGeology of The University of Texas. It is our purpose here to present the results of the regional integrated attack on the problems of correlation by use of fossil molluscan faunas, fossil seed floras, physiographic history, buried soils, lithology, and previously described volcanic ash petrography. From this approach there has emerged the basis for a framework of stratigraphic classification consistent with other parts of the Great Plains region. The data used are relatively widely spaced along the eastern margin of the Plains, and further detailed work is needed in this region to produce a desirable degree of refinement and certainty.
Protoxodera Werner 1930
Creators: name: Schwarz, Christian J.
name: Konopik, Oliver
Publisher: name: Zenodo
Year: 2014
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Mantodea
Toxoderidae
Protoxodera

description: Protoxodera Werner, 1930
Toxodera (Protoxodera) Werner, 1930
Monotypic. Rarely found, restricted to old-growth forests. Arboricolous, in the understorey.
Protoxodera monstrosa Werner, 1930 §
Toxodera (Protoxodera) monstrosa Werner, 1930
Distribution. Malay Peninsula, Sumatra, Nias, N Borneo (Werner 1930, Beier 1976, Roy 2009b). Bornean records. Sabah: Sugut (Deeleman-Reinhold 1957).
description: Published as part of Schwarz, Christian J. & Konopik, Oliver, 2014, An annotated checklist of the praYing mantises (Mantodea) of Borneo, including the results of the 2008 scientific expedition to Lanjak Entimau Wildlife SanctuarY, Sarawak, pp. 130-168 in Zootaxa 3797 (1) on page 155, DOI: 10.11646/zootaxa.3797.1.12, http://zenodo.org/record/226038
Canis lupus Linnaeus 1758
Creators: name: Jo, Yeong-Seok
name: Baccus, John T.
name: Koprowski, John L.
Publisher: name: Zenodo
Year: 2018
Subjects: Biodiversity
Taxonomy
Animalia
Chordata
Mammalia
Carnivora
Canidae
Canis
Canis lupus

description: Canis lupus Linnaeus, 1758 —Eurasian Wolf
Canis lupus Linnaeus, 1758 p.39; Type locality- Sweden; Ellerman & Morrison-Scott, 1951 p.218; Won, 1968 p.249; Corbet, 1978 p.161; Han, 1994 p.46; Won & Smith, 1999 p.15; Oh, 2004a p.147.
Lupus laniger Hodgson, 1847a p.474; Type locality- Tibet
C. chanco Gray, 1863 p.94; Type locality- Chinese Tartary.
C. lupus coreanus Abe, 1923 p.383; Type locality- Korea; Kishida & Mori, 1931 p.379.
C. lupus laniger: Kuroda, 1938 p.36.
C. lupus chanco: Tate, 1947 p.160; Ellerman & Morrison-Scott, 1951 p.219; Won, 1958 p.441; Won, 1967 p.139; Won, 1968 p.251; Yoon, 1992 p.91.
Range: The original distribution of the Eurasian wolf extended throughout the Korean Peninsula (Jo & Baccus 2015). The population declined severely during the Japanese incursion (1910–1945). Several individuals were recorded around Mt. Baekdu until the 1990s (Jin & Ouh 1990), but their current status is uncertain (Fig. 58).
Remarks: The Korean wolf was first classified as C. l. coreanus Abe, 1923, which then was synonymized with C. l. chanco (Won 1967). However, the designation of C. l. chanco as a synonym of C. l. lupus was disputed, because C l. chanco was the name for the Tibetan wolf with a distribution in Central Asia. Although wolves in Korea were classified as C. l. chanco, Korea was outside the distribution compared to the countries listed within the distribution. Abe (1936) stated that C. l. coreanus in the Korean Peninsula was clearly different from the continental form. Recent mtDNA results indicated that coreanus is a synonym of the subspecies C. l. lupus Linnaeus, 1758 (Aggarwal et al. 2003, 2007).
Conservation status: The Red Data Book of South Korea listed C. lupus as ‘Regionally Extinct’ (NIBR 2012). Since wild populations had almost reached extirpation, the North Korean Government classified this species as ‘Vulnerable’ (MAB National Committee of DPR Korea 2002). In 1997, the Ministry of Environment designated C. lupus as an endangered species in South Korea. The wolf became exterminated in South Korea and across most of North Korea in the last century (Jo & Baccus 2015). C. lupus has protection under CITES Appendix II.
description: Published as part of Jo, Yeong-Seok, Baccus, John T. & Koprowski, John L., 2018, Mammals of Korea: a review of their taxonomy, distribution and conservation status, pp. 1-216 in Zootaxa 4522 (1) on pages 90-92, DOI: 10.11646/zootaxa.4522.1.1, http://zenodo.org/record/2610198
Disjunctive Lexical Stratification
Creators: name: Jurgec, Peter
Publisher: name: MIT Press
Year: 2010

description: In many languages, loanwords allow patterns that are absent in the native phonology. The opposite pattern, in which loanwords only allow a subset of the structures attested in native words, is cross-linguistically rare but attested. This paper presents the third type of language, in which the sets of native and foreign phonotactic patterns are disjunctive. In Slovenian, there is no overlap between the sets of front vowels appearing before tautosyllabic [r] in native words and in loanwords. Disjunctive distributions are directly relevant to the theory of lexical indexation since they require indexed markedness constraints in addition to indexed faithfulness constraints.
Additional file 1: of It does matter where you come from: mothersâ   experiences of childbirth in midwife obstetric units, Tshwane, South Africa
Creators: name: Sarie Oosthuizen
name: Bergh, Anne-Marie
name: Pattinson, Robert
name: Grimbeek, Jackie
Publisher: name: Figshare
Year: 2017
Subjects: subject: Medicine
subject: Microbiology
subject: FOS: Biological sciences
subject: Cell Biology
subject: 59999 Environmental Sciences not elsewhere classified
subject: FOS: Earth and related environmental sciences
subject: Sociology
subject: FOS: Sociology
subject: Developmental Biology

description: Anonymous questionnaire for mothers of newborn babies. (PDF 78Â kb)
title: The Hill-Schuler local fauna of Upper Trinity River, Dallas and Denton Counties, Texas
Creators: name: Slaughter, Bob H.
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1962
Subjects: subject: Paleontology -- Pleistocene
subject: Paleontology -- Texas -- Dallas County
subject: Paleontology -- Texas -- Denton County

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: RI0048. Bibliography: p. [64]-66.
description: The Pemberton Hill-Lewisville (T-2) terrace deposits of the Trinity River in Dallas and Denton Counties are divided into four consecutive members. Sixty-three vertebrates, 32 mollusks, and several insects and plants were collected from 3 members and are discussed in the report. The terrace deposits are tentatively referred to as the Sangamon interglacial on the basis of two radiocarbon dates in excess of 3700 years BP and on the association of the giant bison with a typical interglacial fauna. Other Trinity River terraces and local archeology are described and stratigraphic and faunal relationships with other well-known fossil localities in Texas, Oklahoma, and Kansas are suggested.
Next Generation of Ultraprecise Magnetic Sensors
Creators: name: University Of California Office Of The President
Publisher: name: University of California Office of the President
publisherIdentifier: https://ror.org/00dmfq477
publisherIdentifierScheme: ROR
Year: 2024

description: We propose to demonstrate unprecedented sensitivity in an alkali-vapor atomic magnetometer operating in Earth’s magnetic field. Alkali-vapor magnetometers are the world’s most sensitive magnetic-field measurement devices. The best laboratory instruments are capable of measuring field changes smaller than 0.2 femtotesla (4 parts per trillion of Earth’s magnetic field) by very accurately measuring the precession frequency of a coherent sample of atomic spins. Recently our group has discovered a new wall coating for alkali-vapor cells which promises to improve this sensitivity dramatically (UCB invention disclosure B10-139). A major factor in determining a magnetometer’s precision is the spin-coherence lifetime of its atoms. This new coating material exhibits the longest coherence time ever measured in an alkali vapor [1], an improvement of two orders of magnitude over any existing technology. Although several companies do sell alkali-vapor magnetometers intended for Earth’s-field use, the sensitivity of these commercial devices tends to be dramatically worse than that of their low-field laboratory counterparts. These devices generally do not employ antirelaxation-coated cells, partly because it requires sophisticated atomic physics expertise to take advantage of such long coherence times in an Earth’s-field magnetometer. We have demonstrated ultraprecise magnetometers in the laboratory and are working on a prototype designed to operate in Earth’s field. Further investment in this project will lead to vast improvements in the precision of commercial atomic magnetometers. We intend to employ this new wall coating in conjunction with novel atomic physics techniques (e.g., spin locking and spin squeezing) to achieve a longer spin-coherence lifetime than has ever been demonstrated at geophysical fields. In the past year we have demonstrated a dramatic reduction in systematic heading-dependent errors in Earth’s-field atomic magnetometers (publication and UCB invention disclosure pending). Our group has the unique combination of atomic physics expertise and intellectual investment needed to take full advantage of this new antirelaxation coating technology and translate this intellectual property into the next generation of Earth’s-field magnetic sensors. [1] M. V. Balabas, T. Karaulanov, M. P. Ledbetter, and D. Budker. “Polarized Alkali-Metal Vapor with Minute-Long Transverse Spin-Relaxation Time” Physical Review Letters 105, 4 (2010).
Tachyagetes emiratus Wolf 1987
Creators: name: Gadallah, Neveen S.
name: Schmid-Egger, Christian
name: Brothers, Denis J.
Publisher: name: Zenodo
Year: 2020
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Hymenoptera
Pompilidae
Tachyagetes
Tachyagetes emiratus

description: Tachyagetes emiratus Wolf, 1987
Distribution in the Arabian Peninsula: United Arab Emirates (Wolf 1987).
Extralimital distribution: No records.
description: Published as part of Gadallah, Neveen S., Schmid-Egger, Christian & Brothers, Denis J., 2020, Biodiversity of the aculeate wasps (Hymenoptera: Aculeata) of the Arabian Peninsula: Vespoidea, Pompilidae, pp. 153-173 in Zootaxa 4754 (1) on page 166, DOI: 10.11646/zootaxa.4754.1.16, http://zenodo.org/record/3719039
Paratoxodera Wood-Mason 1889
Creators: name: Schwarz, Christian J.
name: Konopik, Oliver
Publisher: name: Zenodo
Year: 2014
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Mantodea
Toxoderidae
Paratoxodera

description: Paratoxodera Wood-Mason, 1889
Highly specialized stick mimics. Four species in Borneo, all rarely found, restricted to old-growth forests. Arboricolous, in the understorey.
Paratoxodera cornicollis Wood-Mason, 1889 §
Paratoxodera cornicollis Wood-Mason, 1889
= Paratoxodera cornicollis borneana Beier, 1931
Distribution. Malay Peninsula, Sumatra, Java, Borneo (Roy 2009b).
Bornean records. Sarawak: Lanjak Entimau (1 m, CSUB); Brunei (Beier 1931a).
Remarks. Bornean P. c or n i c o l l i s specimens usually lack the second metazonal lobe, which prompted Beier (1931a) to establish a new subspecies (P. cornicollis borneana). Listed as valid species in Ehrmann (2002), but shown to be only a variety by Roy (2009b).
Paratoxodera meggitti Uvarov, 1927
Distribution. S China, Myanmar, Malay Peninsula, Borneo (Uvarov 1927, Roy 2009b). Bornean records. Sabah: Crocker Range (Roy 2009b).
Paratoxodera polyacantha Roy, 2009
Distribution. Sabah: Labuk River (Roy 2009b).
Paratoxodera marshallae Roy, 2009
Distribution. Sumatra, N Borneo (Roy 2009b). Bornean records. Sabah: Tawau Hills (Roy 2009b).
description: Published as part of Schwarz, Christian J. & Konopik, Oliver, 2014, An annotated checklist of the praYing mantises (Mantodea) of Borneo, including the results of the 2008 scientific expedition to Lanjak Entimau Wildlife SanctuarY, Sarawak, pp. 130-168 in Zootaxa 3797 (1) on page 156, DOI: 10.11646/zootaxa.3797.1.12, http://zenodo.org/record/226038
Additional file 1: of Using root metaphors to analyze communication between nurses and patients: a qualitative study
Creators: name: Álvarez, Isabel
name: Selva, Laia
name: Medina, José
name: Sáez, Salvador
Publisher: name: Figshare
Year: 2017
Subjects: subject: Sociology
subject: FOS: Sociology
subject: 69999 Biological Sciences not elsewhere classified
subject: FOS: Biological sciences
subject: Developmental Biology
subject: Science Policy

description: Letter from the University. (PDF 560 kb)
title: Pleistocene geology of Red River Basin in Texas
Creators: name: Frye, John Chapman, 1912-
Publisher: name: University of Texas at Austin. Bureau of Economic Geology
Year: 1963
Subjects: subject: Geology -- Texas -- Red River Valley
subject: Geology, Stratigraphic -- Pleistocene

description: To obtain a print version of this publication visit: https://store.beg.utexas.edu/ and search for: RI0049. Bibliography: p. [33]
description: The Red River rises in northeastern New Mexico and extends across northern Texas and east of the Panhandle serves as the northern border of that State. The late Cenozoic geology of the Red River basin has been studied intensively in northwestern Texas and in Louisiana. This report summarizes the results of our studies of the late Cenozoic geology of the Red River basin in Texas. Late Tertiary terrace deposits have been identified as far east as Montague County and deposits of Nebraskan age have been recognized somewhat farther east. Terrace deposits of late Kansan and early Wisconsinan age have been traced essentially throughout the basin in Texas. In north-central and northeastern Texas the names Hardeman, Ambrose, and Cooke are proposed for the alluvial terraces that were formed during late Kansan and early and late Wisconsinan time. In northeastern Texas we found pimple mounds occurring on all terrace surfaces older than Wisconsinan. Varied and diagnostic faunas of fossil mollusks are reported from Kansan, early Wisconsinan, and late Wisconsinan deposits throughout most of the basin in northern Texas, and Pearlette volcanic ash occurs locally in the deposits of Kansan age. The Pleistocene history of the Red River has been a succession of alternating episodes of valley deepening, accompanied by progressive headward encroachment of nickpoints in northwestern Texas, and less extensive valley alluviation.
It is all downhill from here: a typological study of the role of syllable contact in Romance languages
Creators: name: Pons-Moll, Claudia
Publisher: name: Walter de Gruyter
Year: 2011

description: The purpose of this paper is to explore, on the basis of a quite extensive set of processes drawn from Romance languages, the nature and the effects of the SYLLABLE CONTACT constraint in Optimality Theory. In order to achieve that, we investigate and formalize a) the process of regressive manner assimilation that applies in some varieties of Catalan as well as in Lenguadocian Occitan, 2) the processes of onset strengthening and epenthesis that occur in Catalan, 3) the process of 's' rhotacism that is found in Majorcan Catalan, in some dialects of Sardinian and in some dialects of Galician, among other Romance languages, 4) the process of 's' gliding that arises in Lenguadocian Occitan, and, finally, 5) the selection between epenthesis and deletion in word-initial consonantal clusters violating the minimum sonority distance constraints in Catalan. The analysis of these processes, most of them not considered in the literature devoted to SYLLABLE CONTACT, leads to some important theoretical implications: a) SYLLABLE CONTACT should not be regarded as a single constraint which categorically bans coda-onset clusters with rising sonority, but it should be decomposed into a universal hierarchy of constraints targeting all possible sonority distances between adjacent heterosyllabic segments, as originally suggested by Murray & Vennemann (1983), formalized in OT terms by Bat-El (1996) and Gouskova (2001, 2002, 2004), and applied to Romance languages in Pons (2003b, 2004a, 2005b); b) the sonority scale in Catalan should distinguish flaps and trills, the latter being less sonorous, as previously proposed for Catalan and other Romance languages in Bonet & Mascaró; (199&), Parker (2002), Pons (2004a, 2005b); c) the sonority scale of Catalan should treat separately voiced and voiceless stops, the latter being less sonorous, as traditionally put forward in some studies devoted to syllable structure (see, for instance, Steriade 1982, for Attic Greek; Davis 1990, for Italian; and Blevins 1995).
When is less more? Faithfulness and minimal links in wh-chains
Creators: name: Legendre, Geraldine
name: Smolensky, Paul
name: Wilson, Colin
Publisher: name: MIT Press
Year: 1998

description: In the domain of wh-questions, we explore the application of OT to syntactic explanation based on the principle of Minimal Links ('Shortest Move'). We develop a family of constraints called MinLink, and argue: (a) OT allows a strong but flexible MinLink to be constructed directly from general principles, and (b) the resulting MinLink explains a broad range of cross-linguistic (overt and covert) extraction facts. In addition, we argue for certain general solutions to fundamental questions for comparison-based syntactic formalisms: What structures compete? What is the 'input'? How is language-particular ineffability possible? How are marked outputs possible?
Hillaire, N. (2007). Le futur antérieur de l'œuvre d'art. Multitudes, Hors-série n°1, La Transmission (5), 145-160.
Creators: name: Hillaire, Norbert
Publisher: name: Zenodo
Year: 2007

description: Certaines œuvres se présentent comme de véritables pièges à retardement, intégrant à leur propre poïèse la problématique et l’incertitude de leur réception future. Elles s’inscrivent ainsi dans une temporalité de futur antérieur, se positionnant comme des œuvres "à effet-retour" ou "à effet-retard". Ces œuvres anticipent non seulement les conditions techniques actuelles, mais également celles à venir, en ce qui concerne la mémoire et la transmission. Hillaire, N. (2007).