cometadata/datacite-rtg-text-other-reclassification-records huggingface dataset:
title: Unsaturated Zone Studies at the Proposed Low-Level Radioactive Waste Disposal Facility, Eagle Flat Basin, Texas
Creators: name: Scanlon, Bridget R.
name: Xiang, Jiannan
name: Goldsmith, Richard S.
Publisher: name: The University of Texas at Austin
Year: 1993
Subjects: subject: unsaturated zone
subject: radioactive waste
subject: waste disposal
subject: Eagle Flat Basin
subject: Texas

description: Hydrologic studies were conducted to characterize unsaturated zone processes at the proposed low-level radioactive waste disposal site and surrounding area in southern Hudspeth County, Texas. The study area is in northwest Eagle Flat basin, which is within the Basin and Range Physiographic Province. Fractured Cretaceous bedrock crops out to the southeast of the site. The thickness of the basin-fill sediments at the proposed site ranges from 164 feet (50 m) to approximately 656 feet (200 m). Northwest Eagle Flat basin is an internally drained basin that drains through the ephemeral Blanca Draw into Grayton Lake playa. The climate in the study area is subtropical arid and the long-term average annual rainfall is 12.6 inches (320 mm). Unsaturated zone studies were conducted in ephemeral stream and interstream geomorphic settings. In addition to studies of areas typical of these settings, the impact of pseudofissures, an earth fissure, and borrow pits on shallow zone unsaturated processes was also investigated. To evaluate unsaturated zone processes, 57 boreholes were drilled in the various geomorphic settings for collection of soil samples and installation of monitoring equipment. Soil samples were analyzed in the laboratory for particle size, water content, water potential, and chloride concentration. Water potential data are used to evaluate the direction of the driving force for water movement. Chloride concentration data provide information on water fluxes because chloride concentrations are inversely proportional to water flux; low chloride concentrations indicate high water fluxes because chloride is flushed through the soil, whereas high chloride concentrations indicate low water fluxes because chloride is concentrated by evapotranspiration. In addition to laboratory analyses, a monitoring program was initiated by installing neutron probe access tubes in the different geomorphic settings to monitor water content. Field psychrometers were installed to a depth of 60.7 feet (18.5 m) in the interstream setting to monitor water potential and temperature. Hydraulic conductivity was also measured in the field using permeameter tests, constant-head borehole infiltration tests, and multistep constant-head borehole infiltration tests.
title: Consolidation of Geologic Studies of Geopressured-Geothermal Resources in Texas: Barrier-Bar Tidal-Channel Reservoir Facies Architecture, Jackson Group, Prado Field, South Texas
Creators: name: Seni, Steven J.
name: Choh, Suk-Joo
Publisher: name: The University of Texas at Austin
Year: 1993
Subjects: subject: geothermal energy
subject: geopressured zones
subject: reservoirs
subject: facies
subject: Jackson Group
subject: Prado Field
subject: South Texas

description: Sandstone reservoirs in the Jackson barrier/strandplain play are characterized by low recovery efficiencies and thus contain a large hydrocarbon resource target potentially amenable to advanced recovery techniques. Prado field, Jim Hogg County, South Texas, has produced over 23 million barrels of oil and over 32 million cubic feet of gas from combination structural-stratigraphic traps in the Eocene lower Jackson Group. Hydrocarbon entrapment at Prado field is a result of anticlinal nosing by differential compaction and updip pinch-out of barrier bar sandstone. Relative base-level lowering resulted in forced regression that established lower Jackson shoreline sandstones in a relatively distal location in central Jim Hogg County. Reservoir sand bodies at Prado field comprise complex assemblages of barrier-bar, tidal-inlet fill, back-barrier bar, and shoreface environments. Subsequent progradation built the barrier-bar system seaward 1 to 2 miles. Within the barrier-bar system, favorable targets for hydrocarbon reexploration are concentrated in tidal-inlet facies because they possess the greatest degree of depositional heterogeneity.
Foundations of ghost stability
Creators: name: Díez, Verónica Errasti
name: Rifà, Jordi Gaset
name: Staudt, Georgina
Publisher: name: arXiv
Year: 2024
Subjects: subject: High Energy Physics - Theory (hep-th)
subject: General Relativity and Quantum Cosmology (gr-qc)
subject: Mathematical Physics (math-ph)
subject: FOS: Physical sciences

description: We present a new method to analytically prove global stability in ghost-ridden dynamical systems. Our proposal encompasses all prior results and consequentially extends them. In particular, we show that stability can follow from a conserved quantity that is unbounded from below, contrary to expectation. Novel examples illustrate all our results. Our findings take root on a careful examination of the literature, here comprehensively reviewed for the first time. This work lays the mathematical basis for ulterior extensions to field theory and quantization, and it constitutes a gateway for inter-disciplinary research in dynamics and integrability.
description: 2 figures; 20 pages, plus appendices and references. v2: Journal version
title: Strategies for Reserve Growth in Tirrawarra Field
Creators: name: Tyler, N.
name: Hamlin, H. Scott
name: Dutton, Shirley P.
Publisher: name: The University of Texas at Austin
Year: 1993
Subjects: subject: reserves
subject: growth strategies
subject: Tirrawarra Field

description: The Tirrawarra Sandstone, a fluvial-lacustrine sandstone reservoir of earliest Permian age, lies at a depth of approximately 10,000 feet, and current volumetric mapping shows an original oil in place (OOIP) of 127 million barrels. The cumulative production to December 1992 is 17.2 million barrels. The average net pay thickness is 60 feet over an area of 12,000 acres, with an average porosity of approximately 10 percent and an initial oil saturation of roughly 70 percent. The reservoir contains a volatile oil with a solution gas-oil ratio (GOR) of 2714 standard cubic feet per reservoir cubic foot (scf/rcf) (C5+/C4-). At the initial pressure of 4,280 pounds per square inch absolute (psia) and temperature of 285Â°F, the oil formation volume factor was 2.9 reservoir barrels per stock tank barrel (rb/stb) (C5+), and the oil viscosity was 0.09 centipoise. Early reviews and production trends indicated that recovery would be low without some method of improved or enhanced recovery. Laboratory and screening studies using reservoir oil and various injection fluids resulted in the conclusion that satellite separator gas from several local Patchawarra Formation gas (PCSG) reservoirs, gas from the de-ethanizer tower at the nearby Moomba gas plant, and CO2 were all first contact miscible at or above 3,200 psia. A pilot seven-spot pattern in the area of best reservoir productivity was started up in 1984, using PCSG as an injection fluid. After the production decline in this area was largely arrested, four more patterns (approximately seven spots) were added over the next couple of years. Three more have been added during 1992-93. Injection of the Moomba de-ethanizer gas was phased in during 1987. Due to the low permeability range in the Tirrawarra Sandstone (0.1-10 millidarcies), all but three production and injection wells have undergone hydraulic fracture stimulation to ensure injection and offtake is on a commercial scale. The induced fracture orientation is unknown. Fracture half-lengths are between 200 and 500 feet with well spacing of 1,800 to 2,400 feet. Radioactive tracers were placed in the first five injectors in 1985 and 1986, and active sampling occurred until mid-1991. Results were disappointing, most likely due to injection of insufficient amounts of two of the tracers and questionable analytical practices by the laboratory; however, there was a clear indication of uniform sweep.
Tetrapetalonema zakii Nagaty
Creators: name: Muniz-Pereira, Luís C.
name: Vieira, Fabiano M.
name: Luque, José L.
Publisher: name: Zenodo
Year: 2009
Subjects: Biodiversity
Taxonomy
Animalia
Nematoda
Secernentea
Spirurida
Onchocercidae
Tetrapetalonema
Tetrapetalonema zakii

description: Tetrapetalonema zakii (Nagaty)
Leontopithecus rosalia (Linnaeus), unspecified site of infection, unspecified locality (Vicente et al. 1997).
description: Published as part of Muniz-Pereira, Luís C., Vieira, Fabiano M. & Luque, José L., 2009, Checklist of helminth parasites of threatened vertebrate species from Brazil, pp. 1-45 in Zootaxa 2123 on page 9, DOI: 10.5281/zenodo.188170
title: Physical Environment at the King Ranch Training Site
Creators: name: Wermund, E. G.
Publisher: name: The University of Texas at Austin
Year: 1993
Subjects: subject: land use
subject: King Ranch
subject: Texas

description: The King Ranch training site of the Texas Army National Guard is a relatively pristine site that has suffered little physical abuse. Except for possible past overgrazing (as evidenced by the mesquite growth), the land has been used only as pasture. There is no record of major historical storms, but even a major hurricane would not damage the land. Surficial damages to the land surface and its vegetation are possible both when soils are saturated and during drought. Hurricanes are likely to make access to the site difficult; floodwaters from the Santa Gertrudis, Tranquitas, San Fernando, and Carreta Creeks would make U.S. Highway 77 impassable (Federal Emergency Management Agency, 1984). The fact that average annual precipitation is exceeded by evaporation indicates the potential for major drought. A drought would impact National Guard activities by limiting transportation because areas devegetated by traffic are attacked by wind deflation. During very dry periods, National Guard equipment and vehicles may potentially cause range fires.
Additional file 1: of Collaborative care for depression in general practice: study protocol for a randomised controlled trial
Creators: name: Brinck-Claussen, Ursula
name: Curth, Nadja
name: Davidsen, Annette
name: Mikkelsen, John
name: Lau, Marianne
name: Lundsteen, Merete
name: Csillag, Claudio
name: Christensen, Kaj
name: HjorthĂ¸J, Carsten
name: Nordentoft, Merete
name: Eplov, Lene
Publisher: name: Figshare
Year: 2017
Subjects: subject: Biotechnology
subject: 69999 Biological Sciences not elsewhere classified
subject: FOS: Biological sciences
subject: Science Policy
subject: Mental Health

description: SPIRIT 2013 checklist: recommended items to address in a clinical trial protocol and related documents*. (DOC 124 kb)
title: Determining Recent Sedimentation Rates of the Trinity River, Texas
Creators: name: White, William Allen, 1939-
name: Morton, Robert A.
Publisher: name: The University of Texas at Austin
Year: 1993
Subjects: subject: sedimentation
subject: Trinity River
subject: Texas

description: Replacement of wetlands by water and flats in the lower alluvial valley and delta of the Trinity River suggests that relative sea-level rise and reductions in sediment supply have rendered the fluvial-deltaic system incapable of maintaining sufficient elevation to prevent its submergence. The Trinity River transports the greatest load of suspended sediment of all rivers emptying into Texas bays (Longley, 1992a), and therefore, it has the greatest potential for delivering enough sediment to offset subsidence.
Additional file 1: Figure S1. of Genome-wide mapping of transcriptional enhancer candidates using DNA and chromatin features in maize
Creators: name: Rurika Oka
name: Zicola, Johan
name: Weber, Blaise
name: Anderson, Sarah
name: Hodgman, Charlie
name: Gent, Jonathan
name: Jan-Jaap Wesselink
name: Springer, Nathan
name: Hoefsloot, Huub
name: Turck, Franziska
name: Stam, Maike
Publisher: name: Figshare
Year: 2017
Subjects: subject: Genetics
subject: FOS: Biological sciences
subject: Molecular Biology
subject: 69999 Biological Sciences not elsewhere classified
subject: 80699 Information Systems not elsewhere classified
subject: FOS: Computer and information sciences
subject: 19999 Mathematical Sciences not elsewhere classified
subject: FOS: Mathematics
subject: Infectious Diseases
subject: FOS: Health sciences

description: The tissues used in this study. Figure S2. Reproducibility of RNA-seq data. Figure S3. Randomised distributions of features over genomic regions within the uniquely mappable part of the genome. Figure S4. (A) The size distributions of the different features in base pairs and (B) the distributions of the gene expression levels in the two tissues. Figure S5. Characteristics of enhancer-overlapping TEs. Figure S6. Examples of (A, B) enhancers that contain TEs and (C, D) TEs that contain an enhancer. Figure S7. Example of data on tb1 enhancer. Figure S8. Asymmetric H3K9ac enrichment at candidate DHSs. Figure S9. Average profiles of the enhancer candidates in V2-IST and husk for each category. Figure S10. Heatmaps of chromatin, DNA and transcript features at TSSs. Figure S11. Average profiles of randomly selected TSSs in V2-IST and husk for each category. Figure S12. Comparison of expression levels between genes and enhancer candidates in V2-IST and husk. Figure S13. Heatmaps and average profiles of H3K9ac and H3K4me3 at (A, B, D) candidates and (A, C, E) TSSs. Figure S14. ChIP-qPCR data on H3K9ac and H3K4me1 enrichment at enhancer candidate regions. Figure S15. DNase I experiments resulting in the libraries sequenced and analysed in this study. Table S1. Sequencing datasets generated in this study. Table S2. Number of DHSs that overlap between replicates. Table S3. Number of H3K9ac peaks that overlap between replicates. Table S4. Number of TEs (for RLG family with and without candidates) and enhancers that carried the GGCCCA motif. Supplemental Methods. (PDF 2730 kb)
Cibicidoides ungerianus
Creators: name: Bergh, Eugene W.
name: Compton, John S.
Publisher: name: Zenodo
Year: 2022
Subjects: Biodiversity
Taxonomy
Chromista
Foraminifera
Globothalamea
Rotaliida
Cibicididae
Cibicidoides
Cibicidoides ungerianus

description: Cibicidoides ungerianus (d’Orbigny, 1846)
Pl. 6, figs. 1a–c
Rotalina ungeriana d’Orbigny, 1846, p. 157, pl. 8, figs. 16–18; Papp & Schmid, 1985, p. 60, pl. 51, figs. 7–11.
Description: The test surface is calcareous and perforate. The test is trochospiral, subcircular in outline and thinly biconvex in side view. The spiral and umbilical sides are coarsely perforate. The chambers in the final whorl gradually increase in size toward the apertural end. The test margin has a thick keel and the chambers are separated by thick sutures with the earlier chambers not clearly visible. The aperture is an interio-marginal slit extending onto the umbilical lip.
Remarks: This species is less abundant than C. pseudoungerianus in this study, forming minor (<5%) components in the samples. The tests are generally large, measuring up to approximately 1 mm in diameter.
This species differs from C. pseudoungerianus by its more macroperforate test surface, particularly on the umbilical side. Cushman (1922b) re-identified the figured specimen of Truncatulina ungeriana as Truncatulina pseudoungeriana (= Cibicidoides pseudoungerianus). The chambers in the final whorl of C. ungerianus are more inflated, whereas the chambers in the final whorl of C. pseudoungerianus are lobulated, more tapered and flattened towards the margins.
Life strategy: Species of the genus Cibicidoides are generally unattached, epifaunal to shallow-infaunal under oxic conditions (Pezelj et al., 2013 and references therein), preferring muddy substrates (Murray, 1991).
Regional occurrence: This species is recorded to occur in middle Miocene sediments on the Namibian outer continental shelf, south of the Kunene River mouth (this study).
description: Published as part of Bergh, Eugene W. & Compton, John S., 2022, Taxonomy of Middle Miocene foraminifera from the northern Namibian continental shelf, pp. 1-55 in Zootaxa 5091 (1) on page 27, DOI: 10.11646/zootaxa.5091.1.1, http://zenodo.org/record/5840434
Tetrameres paradoxus Diesing
Creators: name: Muniz-Pereira, Luís C.
name: Vieira, Fabiano M.
name: Luque, José L.
Publisher: name: Zenodo
Year: 2009
Subjects: Biodiversity
Taxonomy
Animalia
Nematoda
Secernentea
Spirurida
Habronematidae
Tetrameres
Tetrameres paradoxus

description: Tetrameres paradoxus Diesing
Diomedea exulans Linnaeus, proventricle, unspecified locality (Vicente et al. 1995).
Tetrameres sp.
Crax blumenbachii Spix, ventricle, Espírito Santo (Travassos 1945b) (CHIOC 15886).
description: Published as part of Muniz-Pereira, Luís C., Vieira, Fabiano M. & Luque, José L., 2009, Checklist of helminth parasites of threatened vertebrate species from Brazil, pp. 1-45 in Zootaxa 2123 on page 9, DOI: 10.5281/zenodo.188170
title: Trends and Status of Wetland and Aquatic Habitats in the Galveston Bay Stream, Texas
Creators: name: White, William Allen, 1939-
name: Tremblay, Thomas A.
name: Wermund, E. G.
Publisher: name: The University of Texas at Austin
Year: 1993
Subjects: subject: ecology
subject: aquatic habitats
subject: trends
subject: Galveston Bay
subject: Texas

description: Wetland and aquatic habitats are essential biological components of the Galveston Bay Estuarine System. Understanding the spatial and temporal distribution of these habitats is critical if they are to be effectively protected and managed. This report presents results of an investigation sponsored by the Galveston Bay National Estuary Program (GBNEP) to determine the trends and status of wetlands and aquatic habitats in the Galveston Bay system through aerial photographic analysis supported by field surveys.
Report on the observed climate, projected climate, and projected biodiversity changes for Tarangire National Park, Tanzania under differing levels of warming
Creators: name: Price, Jeff
name: Forstenhäusler, Nicole
name: Graham, Erin
name: Osborn, Timothy J.
name: Warren, Rachel
Publisher: name: Zenodo
Year: 2024

description: Tarangire National Park is among the bottom 22% of all non-marine protected areas, globally. Overall, the biodiversity of the park is projected to be sensitive to climate change once warming levels exceed 2.0°C and will require increasing levels of adaptation. Averaged over the entire area, with 4°C warming (global, above pre-industrial), the area is projected to remain climatically suitable for only 34.8% of its terrestrial biodiversity (fungi, plants, invertebrates, and vertebrates), with none of its area remaining an overall refugia (remaining climatically suitable for >75% of the species) for biodiversity. If warming levels were held to 2°C, only 6.2% of the area would remain a climatic refugia and the area would remain climatically suitable for only 66% of its terrestrial biodiversity. Even with 1.5°C warming, only 35.5% of the area would remain a climate refugia for biodiversity.

Between 1961-1990 and 1991-2020 the average monthly temperature has increased by 0.4° - 0.7°C. With warming levels of 1.5°C, the new average monthly temperature for all months is equivalent to that experienced 1 in 20 years. Ten months have seen decreases in precipitation with only January and August seeing increases. Models project that May-November will become drier, the rest wetter.  The number of months classified as being in severe drought have increased slightly between 1961-1990 and 1986-2015. With warming, the number of months in severe drought are projected to increase.     

Some additional adaptation will be required, even with 1.5°C warming.  Once warming levels have surpassed 2°C, substantial adaptation will be needed as the entire area will be starting to transform into new ecosystems and new species assemblages.
Salvia (Calosphace) (sect. Pennellia) Epling 1939
Creators: name: Martínez-Gordillo, Martha
name: Fragoso-Martínez, Itzi
name: Salas-Morales, Silvia H.
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Plantae
Tracheophyta
Magnoliopsida
Lamiales
Lamiaceae
Salvia

description: Key to the species of Salvia subg. Calosphace sect. Pennellia
1. Perennial herb, branched; stem color purple, leaf blades lanceolate, oblong-lanceolate to oblong-ovate, margin crenate-serrate, lower leaf surface hirtellous, green; lower corolla lip 7–10 mm long ............................................................................... S. pennellii
- Perennial herb, unbranched; stem color tan brown, leaf blades elliptic or oblong-elliptic, margin serrulate, lower leaf surface tomentose, whitish; lower corolla lip 4–8 mm long ...................................................................................................... S. robertoana
description: Published as part of Martínez-Gordillo, Martha, Fragoso-Martínez, Itzi & Salas-Morales, Silvia H., 2016, Salvia robertoana (Lamiaceae), a new species from Oaxaca, Mexico, pp. 271-278 in Phytotaxa 269 (4) on page 275, DOI: 10.11646/phytotaxa.269.4.2, http://zenodo.org/record/4779711
Large-Scale Wave-Driven Interactions and Plasma-Neutral Coupling in the Low-Latitude Ionosphere-Thermosphere
Creators: name: Khadka, Sovit M
name: Gasperini, Federico
name: Stolle, Claudia
name: Oberheide, Jens
Publisher: name: Zenodo
Year: 2024

description: This manuscript [2024JA032535RR] has been accepted for publication in Journal of Geophysical Research - Space Physics in May 07, 2024.
title: Evaluation of Preferential Flow in Playa Settings Near the Pantex Plant
Creators: name: Xiang, Jiannan
name: Hovorka, Susan D.
name: Goldsmith, Richard S.
Publisher: name: The University of Texas at Austin
Year: 1993
Subjects: subject: hydrology
subject: playas
subject: preferential flow
subject: Pantex Plant
subject: Texas

description: Analysis of water movement through the unsaturated zone is critical for understanding recharge and contaminant transport at DOE's Pantex Plant. Although preferential flow pathways such as root tubules, cracks, and fissures (Seven, 1991) may not be important volumetrically from a groundwater recharge standpoint, such flow may play a critical role in rapidly transporting contaminants to the groundwater and bypassing much of the soil matrix. Previous studies found that flow along preferential pathways may be up to two orders of magnitude higher than that predicted by homogeneous flow models (Richard and Steenhuis, 1988). In order to accurately evaluate pathways for contaminant transport, it is necessary to understand the spatial distribution of preferential flow pathways. The objective of this study was to delineate the spatial distribution of preferential pathways and evaluate the controls on such pathways.
title: Numerical Modeling of Preferential Flow at the Pantex Plant Area
Creators: name: Xiang, Jiannan
name: Scanlon, Bridget R.
Publisher: name: The University of Texas at Austin
Year: 1993
Subjects: subject: hydrology
subject: modeling
subject: preferential flow
subject: Pantex Plant
subject: Texas

description: The objective of this study was to analyze preferential flow based on observations from four ponding tests conducted in the vicinity of the Pantex Plant. According to soil profiles exposed after the field ponding tests (Xiang et al., 1993), we derived the hydraulic conductivity of an equivalent homogeneous soil as that of the actual heterogeneous soil. Models of four different types of subsurface flow were considered. These include flow through the soil matrix, through root tubules, between ped faces, and along soil-filled cracks. The results of numerical simulations of matrix flow were similar to field observations of matrix flow from ponding tests. To evaluate preferential flow, different values of hydraulic conductivity were used. The simulations show that preferential flow results in an increased rate of water movement because of the higher equivalent hydraulic conductivity.
Heterolepa dutemplei
Creators: name: Bergh, Eugene W.
name: Compton, John S.
Publisher: name: Zenodo
Year: 2022
Subjects: Biodiversity
Taxonomy
Chromista
Foraminifera
Globothalamea
Rotaliida
Cibicididae
Heterolepa
Heterolepa dutemplei

description: Heterolepa dutemplei (d’Orbigny, 1846)
Pl. 6, figs. 2a–c
Rotalina dutemplei d’Orbigny, 1846, p. 157, pl. 8, figs. 19–21.
Heterolepa dutemplei Papp & Schmid, 1985, p. 61, pl. 52, figs. 1–6; Loeblich & Tappan, 1988, p. 632, pl. 709, figs. 1–8; Oblak, 2007, p. 305, pl. 4, figs. 2a–c; Holbourn et al., 2013, p. 294 –295.
Cibicidoides dutemplei van Morkhoven et al., 1986, p. 112, pl. 35.
Description: The test wall is calcareous and macroperforate. The test is trochospiral and mainly planoconvex in side view, with the umbilical side very convex. The earlier chambers form a slightly convex shape on the spiral side. The approximately eight chambers in the final whorl gradually increase in size toward the apertural end. The chambers are separated by flush, less perforate sutures, covering almost the entire earlier chambers of the inner whorl. The sutures on the spiral side are oblique. The aperture is an interio-marginal slit, extending along the inflated apertural chamber on the umbilical side.
Remarks: Heterolepa dutemplei is a minor (<5%) component in the samples of all three cores. Tests are relatively moderate to large in size, measuring up to 1 mm in diameter.
Life strategy: This species has a bathymetric distribution from the shelf to the upper slope (van Marle, 1988; Holbourn e t al., 2013), adapted to muddy substrates in organic-rich environments and oxic to suboxic conditions (e.g., Debenay-Redois, 1997; Peryt, 2013; Rahiminejad et al., 2016; Roslim et al., 2019).
Global stratigraphic range: Heterolepa dutemplei has been documented in Palaeocene (Stojanova and Petrov, 2014) to Recent strata (e.g., van Marle, 1988; Szarek e t al., 2006).
Regional occurrence: This study records Heterolepa dutemplei to occur in middle Miocene sediments on the outer continental shelf of Namibia, south of the Kunene River mouth.
description: Published as part of Bergh, Eugene W. & Compton, John S., 2022, Taxonomy of Middle Miocene foraminifera from the northern Namibian continental shelf, pp. 1-55 in Zootaxa 5091 (1) on pages 27-28, DOI: 10.11646/zootaxa.5091.1.1, http://zenodo.org/record/5840434
Ascaridia hermaphrodita Froelich
Creators: name: Muniz-Pereira, Luís C.
name: Vieira, Fabiano M.
name: Luque, José L.
Publisher: name: Zenodo
Year: 2009
Subjects: Biodiversity
Taxonomy
Animalia
Nematoda
Secernentea
Ascaridida
Ascaridiidae
Ascaridia
Ascaridia hermaphrodita

description: Ascaridia hermaphrodita (Froelich)
Amazona vinacea (Kuhl), intestine, unspecified locality (Diesing 1851; Travassos 1930; Serra-Freire & Bianchin 1978; Vicente et al., 1995).
Anodorhynchus hyacinthinus (Latham), small intestine, Rio de Janeiro (Barros et al. 2002) (CHIOC 34434). Aratinga solstitialis (Linnaeus), intestine, unspecified locality (Vicente et al. 1995).
description: Published as part of Muniz-Pereira, Luís C., Vieira, Fabiano M. & Luque, José L., 2009, Checklist of helminth parasites of threatened vertebrate species from Brazil, pp. 1-45 in Zootaxa 2123 on page 9, DOI: 10.5281/zenodo.188170
MOESM1 of Enzyme adsorption-induced activity changes: a quantitative study on TiO2 model agglomerates
Creators: name: Márquez, Augusto
name: Kocsis, Krisztina
name: Zickler, Gregor
name: Bourret, Gilles
name: Feinle, Andrea
name: Hüsing, Nicola
name: Himly, Martin
name: Duschl, Albert
name: Berger, Thomas
name: Diwald, Oliver
Publisher: name: Figshare
Year: 2017
Subjects: subject: Biochemistry
subject: Physiology
subject: FOS: Biological sciences
subject: 59999 Environmental Sciences not elsewhere classified
subject: FOS: Earth and related environmental sciences
subject: 39999 Chemical Sciences not elsewhere classified
subject: FOS: Chemical sciences
subject: Ecology
subject: 69999 Biological Sciences not elsewhere classified

description: Additional file 1. Transmission electron micrographs, hydrolysis plots, IR spectra and fitting results.
Heterolepa broeckhiana
Creators: name: Bergh, Eugene W.
name: Compton, John S.
Publisher: name: Zenodo
Year: 2022
Subjects: Biodiversity
Taxonomy
Chromista
Foraminifera
Globothalamea
Rotaliida
Cibicididae
Heterolepa
Heterolepa broeckhiana

description: Heterolepa broeckhiana (Karrer, 1878)
Pl. 6, figs. 3–4
Rotalina broeckhiana Karrer, 1878, p. 98, pl. 5, fig. 26.
Gyroidina broeckhiana Belford, 1966, pp. 167, 168, pl. 29, figs. 1–7, text-figs. 21–10, 21–11; Jones, 1994, p. 106, pl. 107, fig. 4.
Description: The test wall is calcareous and microperforate. The test is trochospiral, subcircular in outline and unequally biconvex in side view and in cross-section. Approximately six to eight chambers are visible externally in the final whorl. The chambers gradually increase in size toward the terminal apertural end and are separated by slightly depressed sutures. The sutures on the spiral side are radial and straight on the umbilical side. The aperture is an extraumbilical to interio-marginal slit.
Remarks: The relative abundances of this species are moderate to high (<10%) in the three cores. Tests in this study are relatively large, measuring up to 1 mm in diameter.
Life strategy: The genus Heterolepa has a shelf to upper slope distribution in well oxygenated environments (Rögl and Spezzaferri, 2003).
Regional occurrence: This study is the first to document this species in midddle Miocene strata in the region and occurs on the Namibian outer continental shelf, south of the Kunene River mouth (this study).
description: Published as part of Bergh, Eugene W. & Compton, John S., 2022, Taxonomy of Middle Miocene foraminifera from the northern Namibian continental shelf, pp. 1-55 in Zootaxa 5091 (1) on page 28, DOI: 10.11646/zootaxa.5091.1.1, http://zenodo.org/record/5840434
title: Internal Geometry of a Modern Carbonate Grainstone Shoal--an Analog for Hydrocarbon Reservoir Heterogeneity
Creators: name: Bebout, Don G.
name: Major, R. P.
Publisher: name: The University of Texas at Austin
Year: 1994
Subjects: subject: petroleum
subject: reservoirs
subject: carbonate rocks
subject: shoals
subject: heterogeneity

description: We chose the ooid sand shoals of the Joulters Cays area of Great Bahama Bank for detailed sedimentological study to investigate the patterns of internal heterogeneity within a modern carbonate sand belt and to develop criteria for predicting the lateral extent of carbonate sand facies. Major facies identified from cores were (1) crossbedded, well-sorted ooids, (2) burrowed, poorly sorted ooids, and (3) poorly sorted ooids and mud containing Thalassia. Clast-rich zones and mud layers were also encountered. We propose that upon burial and compaction, the poorly sorted ooids and mud containing Thalassia will likely retain negligible porosity and permeability, whereas both the crossbedded, well-sorted ooids and burrowed poorly sorted ooids will likely maintain their high initial porosity and permeability. However, study of many ancient subsurface reservoirs indicates that the crossbedded, well-sorted ooids can undergo considerable cementation and have low resultant porosity and permeability. Thus, in many settings, the burrowed, poorly sorted ooids could retain the highest porosity and permeability. Additional cementation within the clast-rich zones, which occur in both the crossbedded, well-sorted ooids and burrowed, poorly sorted ooids, will result in thin, low-porosity barriers within a reservoir. Locally the surface configuration of the modern shoal complex at Joulters Cays was altered significantly by the passing of Hurricane Andrew in August 1992. Prominent wash over bars were planed off, and well-sorted ooids were deposited in low areas of the shoal where poorly sorted and mud-rich deposits of ooids had previously accumulated. The post-hurricane configuration of the shoal demonstrates how a single short-term depositional event contributed significantly to the internal heterogeneity of the shoal complex.
Draconarius absentis Wang
Creators: name: Wang, XIN-PING
name: Griswold, CHARLES E.
name: Miller, JEREMY A.
Publisher: name: Zenodo
Year: 2010
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Arachnida
Araneae
Agelenidae
Draconarius
Draconarius absentis

description: Draconarius absentis Wang 2003
(Figs 6-15, 533)
Draconarius absentis Wang 2003: 517, figs 7A-D (male holotype, male and female paratypes from Baoshan, Yunnan, China, in HNU and CAS, examined).
Additional material examined. CHINA: Yunnan: Longling County: 1♀, Longjiang Township, Xiao Hei Shan Nature Reserve (Gu Cheng Shan), N24.82886°, E098.75917°, 2010 m, in the forest, May 26, 2005, H.M. Yan (HNU, CASENT9025595). Longyang County: 1♀, 40 km of the road Bawan-Tengchong, Bawan village, Baoshan City, N24° 55459', E98° 45309', 2320 m, October 16, 2003, G. Tang (HNU, CASENT9020405); 1♀, 25 km of the road Bawan-Tengchong, Bawan village, Baoshan City, N24° 56220', E98° 49335', 2380 m, October 14, 2003, G. Tang (CAS, CASENT9020418); 1♀, 39-41 km of the road Bawan-Tengchong, Bawan village, Baoshan City, N24° 55625', E98° 45155', 2416 m, October 12, 2003, G. Tang (HNU, CASENT9020358); 2♀, 22-25 km of the road Bawan-Tengchong, Bawan village, Baoshan City, N24° 56220', E98° 49335', 2380 m, October 14, 2003, G. Tang (1♀, CAS CASENT9020414; 1♀, HNU, CASENT9020413). Tengchong County: 1♀, 51 km of the road Bawan-Tengchong, Dahaoping village, N24° 58527', E98° 43797', 2018 m, October 17, 2003, G. Tang (CAS, CASENT9020386); 1♀, Yong-An Bridge, Jietou Township, N25° 16212', E98° 35567', 1492 m, October 22, 2003, G. Tang (CAS, CASENT9020410).
Diagnosis: The female of this species can be easily distinguished from other Draconarius by the absence of epigynal teeth, the presence of a distinct, continuous, strongly sclerotized anterior atrial margin, the anteriorly and laterally extending copulatory ducts, and the short spermathecae (Figs 6, 12-13). The male is similar to D. tangi sp. nov. in having a broad, anteriorly extending conductor and prolaterally originating embolus, but can be distinguished by the small patellar apophysis, the slightly trifurcate conductor, the filiform embolus and the absence of a median apophysis (Figs 9-11).
Description: See Wang (2003). Photos of habitus, eyes, labium and genitalia are provided in this study (Figs 6-15).
Distribution: China (Yunnan: Longling, Longyang, Tengchong) (Fig. 533).
description: Published as part of Wang, XIN-PING, Griswold, CHARLES E. & Miller, JEREMY A., 2010, Revision of the genus Draconarius Ovtchinnikov 1999 (Agelenidae: Coelotinae) in Yunnan, China, with an analysis of the Coelotinae diversity in the Gaoligongshan Mountains, pp. 1-127 in Zootaxa 2593 on pages 17-19
Melonis affinis
Creators: name: Bergh, Eugene W.
name: Compton, John S.
Publisher: name: Zenodo
Year: 2022
Subjects: Biodiversity
Taxonomy
Chromista
Foraminifera
Globothalamea
Rotaliida
Melonidae
Melonis
Melonis affinis

description: Melonis affinis (Reuss, 1851)
Pl. 6, fig. 5
Nonionina affinis Reuss, 1851, p. 72, pl. 5, fig. 32.
Noniona barleeana Williamson, 1858, p. 32, pl. 3, figs. 68–69.
Nonionina crassula Parker & Jones, 1857, p. 14, pl. 11, figs. 5–7.
Nonion barleeanum Cushman, 1930, p. 11, pl. 4, fig. 5.
Melonis barleeanum Loeblich & Tappan, 1988, pl. 696, figs. 5–6; Hermelin, 1989, p. 88, pl. 17, fig. 12; Milker & Schmiedl, 2012, p. 115, fig. 26.11–26.12; Holbourn et al., 2013, p. 354.
Melonis barleeanus Loeblich & Tappan, 1994, p. 159, pl. 347, figs. 1–5.
Melonis affinis Milker et al., 2009, p. 218, pl. 3, fig. 20; Milker and Schmiedl, 2012, p. 115, fig. 26.9–10.
Description: The test wall is calcareous and perforate. The test is planispiral and symmetrical in side view. The periphery of the test is rounded. Up to twelve chambers in the final whorl are separated by smooth, slightly curved sutures. The chamber walls are coarsely perforate and the sutures very finely perforate. The sutures radiate from the umbilical region, becoming thinner toward the test margin. The chambers gradually increase in size toward the apertural end. The aperture is an interio-marginal slit.
Remarks: The relative abundances of Melonis affinis decrease toward the deeper cores, forming minor (<10%) to trace (<1%) components in the samples of all three cores. The tests are moderate in size, measuring up to 0.5 mm in diameter.
Life strategy: This species lives unattached in mostly infaunal and muddy substrates (Murray, 1991). M. affinis is most abundant in oxic conditions, but is also tolerant of dysoxic and suboxic conditions (Kaiho, 1994; Murray, 2006). The species is also associated with the nitrate reduction zone (Fontanier et al., 2002) on the shelf to slope (Holbourn et al., 2013).
Global stratigraphic range: This species occurs from the Oligocene to Recent (Holbourn et al., 2013).
Regional occurrence: Melonis affinis is recorded to occur in middle Miocene sediments on the outer continental shelf of Namibia, south of the Kunene River mouth (this study) and in moderate abundances during the late Miocene to Pliocene along the slope of northern Namibia to the southwestern slope of South Africa (Wefer et al., 1998). Wefer et al. (1998) recorded the occurrence of M. affinis (= M. barleeanus) only in low to moderate (<2 to <20%) abundances along the slope off the Walvis Ridge during the Pleistocene.
description: Published as part of Bergh, Eugene W. & Compton, John S., 2022, Taxonomy of Middle Miocene foraminifera from the northern Namibian continental shelf, pp. 1-55 in Zootaxa 5091 (1) on pages 28-29, DOI: 10.11646/zootaxa.5091.1.1, http://zenodo.org/record/5840434
Draconarius agrestis Wang
Creators: name: Wang, XIN-PING
name: Griswold, CHARLES E.
name: Miller, JEREMY A.
Publisher: name: Zenodo
Year: 2010
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Arachnida
Araneae
Agelenidae
Draconarius
Draconarius agrestis

description: Draconarius agrestis Wang, 2003
(Figs 31-36, 534)
Draconarius agrestis Wang 2003: 519, figs 10A-B (holotype and paratype males from Tengchong, Yunnan, China, in HNU and CAS, examined).
Additional material examined: CHINA: Yunnan: Longling County: 1♂, Bawan District, Nankang Yakou, 2180 m, N24.83178°, E98.76472°, understory of good forest on E-facing slope; night collecting, May 25, 2005, C. Griswold & D. Kavanaugh (CAS, CASENT9022319).
Diagnosis: This species is similar to D. pseudoagrestis sp. nov. and differs only in minor features in the male palp: the short, less posteriorly extending conductor and the absence of denticles on distal conductor (Figs 31-33).
Description: Male. See Wang (2003). Photos of male habitus, eyes, labium and palp are provided in this study (Figs 3136).
Female. Unknown.
Distribution: China (Yunnan: Longling) (Fig. 534).
description: Published as part of Wang, XIN-PING, Griswold, CHARLES E. & Miller, JEREMY A., 2010, Revision of the genus Draconarius Ovtchinnikov 1999 (Agelenidae: Coelotinae) in Yunnan, China, with an analysis of the Coelotinae diversity in the Gaoligongshan Mountains, pp. 1-127 in Zootaxa 2593 on pages 21-23
Ascaridia sergiomeitrai Pereira
Creators: name: Muniz-Pereira, Luís C.
name: Vieira, Fabiano M.
name: Luque, José L.
Publisher: name: Zenodo
Year: 2009
Subjects: Biodiversity
Taxonomy
Animalia
Nematoda
Secernentea
Ascaridida
Ascaridiidae
Ascaridia
Ascaridia sergiomeitrai

description: Ascaridia sergiomeitrai Pereira
Pipile jacutinga (Spix), unspecified site of infection, unspecified locality (Serra-Freire & Bianchin 1978).
description: Published as part of Muniz-Pereira, Luís C., Vieira, Fabiano M. & Luque, José L., 2009, Checklist of helminth parasites of threatened vertebrate species from Brazil, pp. 1-45 in Zootaxa 2123 on page 9, DOI: 10.5281/zenodo.188170
Draconarius anceps Wang, Griswold & Miller, 2010, sp. nov.
Creators: name: Wang, XIN-PING
name: Griswold, CHARLES E.
name: Miller, JEREMY A.
Publisher: name: Zenodo
Year: 2010
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Arachnida
Araneae
Agelenidae
Draconarius
Draconarius anceps

description: Draconarius anceps sp. nov.
(Figs 37-43, 533)
Type material: Holotype. ♀, CHINA: Yunnan: Tengchong County: Houqiao, 16 km N of Danzha village at Zhaobitang Forest Park Station, N25.55771, E098.20885, 2500 m, May 29, 2006, D. Kavanaugh, R.L. Brett & D.Z. Dong, deposited in HNU (CASENT9025594).
Etymology: The species name is derived from Latin word “anceps”, which means "two-headed, double", and refers to the laterally extending diverticula on spermathecae, in addition to the spermathecal heads that extending anteriorly; adjective.
Diagnosis: This species seems to be similar to D. guoi sp. nov. in having a similar atrium and triangular spermathecae, differing only in minor features in the female epigynum. This new species has a pair of short atrial ridges that are limited to the anterior part of the atrium (Fig. 37), while the atrial ridges of D. guoi sp. nov. are long, extending posteriorly to the epigastric furrow (Figs 180-181).
Description: Female (holotype). Medium sized Coelotinae, total length 8.90 (Fig. 41). Dorsal shield of prosoma 4.00 long, 2.20 wide; opisthosoma 4.90 long, 3.75 wide. AME smallest, approximately half the size of other eyes, which are subequal (AME 0.10, ALE 0.18, PME 0.18, PLE 0.17); AME separated from each other by slightly less than their diameter, from ALE by half of AME diameter; PME separated from each other by about 2 /3 of their diameter, from PLE by slightly less than PME diameter (AME-AME 0.08, AME-ALE 0.05, ALE-PLE 0.08, PME-PME 0.12, PME-PLE 0.15, AME-PME 0.14) (Fig. 42). Chelicerae with 3 promarginal and 2 retromarginal teeth. Labium with length and width subequal (L / W =1.00) (Fig. 43). Epigynal teeth absent; atrium small, with anterior atrial margin slightly protruding posteriorly; atrial ridges short, limited to anterior part of atrium; copulatory ducts indistinct from dorsal view; spermathecae short, broad, separated by slightly less than their width, with lateral diverticula; speramathecal heads distinct, arising anteriorly (Figs 37-40).
Male. Unknown.
Distribution: China (Yunnan: Tengchong) (Fig. 533).
description: Published as part of Wang, XIN-PING, Griswold, CHARLES E. & Miller, JEREMY A., 2010, Revision of the genus Draconarius Ovtchinnikov 1999 (Agelenidae: Coelotinae) in Yunnan, China, with an analysis of the Coelotinae diversity in the Gaoligongshan Mountains, pp. 1-127 in Zootaxa 2593 on pages 23-24
Anomalinoides helicinus
Creators: name: Bergh, Eugene W.
name: Compton, John S.
Publisher: name: Zenodo
Year: 2022
Subjects: Biodiversity
Taxonomy
Chromista
Foraminifera
Globothalamea
Rotaliida
Anomalinidae
Anomalinoides
Anomalinoides helicinus

description: Anomalinoides helicinus (Costa, 1855)
Pl. 6, figs. 6–7
Nonionina helicina Costa, 1855, p. 123, pl. 1, figs. 18a–c.
Anomalina helicina Christodolou, 1960, p. 89, pl. 8, figs. 5a–c.
Description: The test wall is calcareous with coarsely perforate chambers and smooth sutures separating the chambers. The test is rounded and trochospiral, with a small central boss. The approximately twelve chambers in the final whorl gradually increase in size and become inflated toward the apertural end. The curved radial sutures appear slightly raised between the coarsely perforate chambers on the umbilical side. The sutures are curved away from the apertural end. A flap extends from each suture between chambers, slightly extending over the umbilicus. The aperture is an arched interio-marginal slit against the margin of the previous whorl with an upper lip.
Remarks: The relative abundances of A. helicinus are minor (<5%) in all three cores. The tests are moderate in size, measuring 0.6 mm in diameter.
Life strategy: This species is epifaunal-shallow infaunal (Pérez-Asensio et al., 2012).
Regional occurrence: Anomalinoides helicinus occurs in middle Miocene sediments on the Namibian outer continental shelf, south of the Kunene River mouth (this study).
description: Published as part of Bergh, Eugene W. & Compton, John S., 2022, Taxonomy of Middle Miocene foraminifera from the northern Namibian continental shelf, pp. 1-55 in Zootaxa 5091 (1) on page 29, DOI: 10.11646/zootaxa.5091.1.1, http://zenodo.org/record/5840434
title: Occurance and Movement of Ground Water in Austin Chalk and Eagle Ford and Ozan Formations at the Superconducting Super Collider (SSC) Site, Ellis County, Texas
Creators: name: Dutton, Alan R.
name: Collins, Edward W.
name: Hovorka, Susan D.
name: Mace, Robert E. (Robert Earl), 1967-
name: Scanlon, Bridget R.
name: Xiang, Jiannan
Publisher: name: The University of Texas at Austin
Year: 1994
Subjects: subject: Austin Chalk
subject: Eagle Ford Formation
subject: Ozan Formation
subject: Superconducting Super Collider
subject: Ellis County
subject: Texas

description: This report defines hydrologic properties and describes rates and modes of groundwater flow in weathered and unweathered Austin Chalk and Ozan (lower Taylor Marl) and Eagle Ford Formations at the Superconducting Super Collider (SSC) site in Ellis County, Texas. Fractures probably are the primary conduit of groundwater flow in these formations because unfractured bedrock has low hydraulic conductivity. Distribution and fabric of detrital versus authigenic clays, rather than total clay content, influence the mechanical properties and log-response character of chalk and marl. The middle Austin Chalk typically has lower fracture intensity and abundance, greater ductility, lower porosity, and lower average hydraulic conductivity than the upper and lowermost Austin. Precipitation over upland drainage divides percolates into the ground and moves downward through the soil zone and weathered bedrock to the water table. Water levels in both weathered and unweathered bedrock generally mimic topography, reflecting a dynamic balance between the rate of recharge from precipitation and rates of discharge by evapotranspiration, flow to springs and seeps, and pumping of wells. Groundwater percolates along vertical fractures and horizontal bedding-plane joints and through the more permeable sedimentary layers. Flow paths are generally eastward but bend toward discharge points in springs and seeps in the valley bottoms and stream banks. Vertical movement is retarded by unfractured, low-permeability beds. Only a small amount (<1 percent) of the groundwater moving through the surficial weathered bedrock moves downward into unweathered, low-permeability bedrock. Vertical circulation of groundwater in fractured zones locally is deep. At the eastern side of the SSC, groundwater moves downward from the Ozan into the Austin beneath the upland drainage divides but upward from the Austin through the Ozan beneath stream valleys.
Ascaridia serrata Schneider
Creators: name: Muniz-Pereira, Luís C.
name: Vieira, Fabiano M.
name: Luque, José L.
Publisher: name: Zenodo
Year: 2009
Subjects: Biodiversity
Taxonomy
Animalia
Nematoda
Secernentea
Ascaridida
Ascaridiidae
Ascaridia
Ascaridia serrata

description: Ascaridia serrata (Schneider)
Pipile jacutinga (Spix), unspecified site of infection, Mato Grosso do Sul (Vicente et al. 1995).
description: Published as part of Muniz-Pereira, Luís C., Vieira, Fabiano M. & Luque, José L., 2009, Checklist of helminth parasites of threatened vertebrate species from Brazil, pp. 1-45 in Zootaxa 2123 on page 9, DOI: 10.5281/zenodo.188170
Non-Landau quantum phase transition in modulated SU(N) Heisenberg spin chains
Creators: name: Capponi, Sylvain
name: Devos, Lukas
name: Lecheminant, Philippe
name: Totsuka, Keisuke
name: Vanderstraeten, Laurens
Publisher: name: arXiv
Year: 2024
Subjects: subject: Strongly Correlated Electrons (cond-mat.str-el)
subject: Quantum Gases (cond-mat.quant-gas)
subject: FOS: Physical sciences

description: We investigate the nature of the quantum phase transition in modulated SU(N) Heisenberg spin chains. In the odd-N case, the transition separates a trivial non-degenerate phase to a doubly-degenerate gapped chiral PSU(N) symmetry-protected topological (SPT) phase which breaks spontaneously the inversion symmetry. The transition is not an Ising transition associated to the breaking of the $\mathbb{Z}_2$ inversion symmetry, but is governed by the delocalization of the edge states of the SPT phase. In this respect, a modulated SU(N) Heisenberg spin chain provides a simple example in one dimension of a non-Landau phase transition which is described by the SU(N)$_1$ conformal field theory. We show that the chiral SPT phase exhibits fractionalized spinon excitations, which can be confined by changing the model parameters slightly.
description: 13 pages, 12 figures