cometadata/datacite-rtg-text-other-reclassification-records huggingface dataset:
Hansenisca soldanii
Creators: name: Bergh, Eugene W.
name: Compton, John S.
Publisher: name: Zenodo
Year: 2022
Subjects: Biodiversity
Taxonomy
Chromista
Foraminifera
Globothalamea
Rotaliida
Gavelinellidae
Hansenisca
Hansenisca soldanii

description: Hansenisca soldanii (d’Orbigny, 1826)
Pl. 6, figs. 8a-b; pl. 7, figs. 1a–c
Gyroidina soldanii d’Orbigny, 1826, p. 278; d’Orbigny, 1846, pl. 8, figs. 10–12; Papp & Schmid, 1985, p. 60, pl. 50, figs. 4–9. Gyroidinoides soldanii Lowry, 1987, p. 254, pl. 15, figs. 9a–b; Jones, 1994, p. 106, pl. 107, figs. 6–7; Kender et al., 2008, p.
519, pl. 25, figs. 1–5; Holbourn et al., 2013, p. 278.
Description: The test wall is calcareous and microperforate. The test is trochospiral and planoconvex to slightly unequally biconvex in side view. The spiral side is flat to slightly convex and the umbilical side highly convex. The approximately eight chambers in the final whorl gradually increase in size toward the apertural end and are separated by slightly depressed straight sutures. The sutures are radial on the spiral side and straight on the umbilical side. The umbilical sutures may be faint to slightly visible. The aperture is an interio-marginal slit, produced on a flap of the terminal chamber, extending onto the umbilical region.
Remarks: This species occurs in minor to moderate abundances in the cores. The tests are moderately large, measuring up to 0.9 mm in diameter.
Life strategy: This species is epifaunal to shallow-infaunal (Pérez-Asensio et al., 2012), suboxic, unattached, preferring muddy substrates (Murray, 1991) on the slope (Holbourn et al., 2013).
Global stratigraphic range: Hansenisca soldanii occurs from the Oligocene to Recent (Jones, 1994).
Regional occurrence: Kender et al. (2008) reported H. soldanii (= Gyroidinoides soldanii) from the Miocene in the Congo Basin. This study extends the spatial distribution of the species to the middle Miocene of the outer continental shelf of Namibia, south of the Kunene River mouth. This species also occurs in minor (<1%) to moderate (<50%) abundances along the slope of Namibia and southwestern South Africa from the late Miocene to Pleistocene. The highest abundances were recorded on the slope between Walvis Bay and Lüderitz, Namibia (Wefer et al., 1998). Lowry (1987) reported H. soldanii in surface sediments off the coast of northern Namibia to around the entire coastline of South Africa.
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 29-30, DOI: 10.11646/zootaxa.5091.1.1, http://zenodo.org/record/5840434
Additional file 1: of Effectiveness and cost-effectiveness of embedded simulation in occupational therapy clinical practice education: study protocol for a randomised controlled trial
Creators: name: Imms, Christine
name: Chu, Eli
name: Guinea, Stephen
name: Sheppard, Loretta
name: Froude, Elspeth
name: Carter, Rob
name: Darzins, Susan
name: Ashby, Samantha
name: Gilbert-Hunt, Susan
name: Gribble, Nigel
name: Nicola-Richmond, Kelli
name: Merrolee Penman
name: Gospodarevskaya, Elena
name: Mathieu, Erin
name: Symmons, Mark
Publisher: name: Figshare
Year: 2017
Subjects: subject: Medicine
subject: 19999 Mathematical Sciences not elsewhere classified
subject: FOS: Mathematics
subject: Science Policy

description: SPIRIT checklist. These are our responses to the standard SPIRIT checklist. (PDF 173 kb)
Draconarius argenteus Wang, Yin, Peng & Xie
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 argenteus

description: Draconarius argenteus (Wang, Yin, Peng & Xie 1990)
(Fig. 533)
Coelotes argenteus Wang et al. 1990: 229, figs 117-119 (male holotype from Jinhong, Yunnan, China, in HNU, examined). Song et al. 1999: 374, figs 218C, J.
Draconarius argenteus: Wang, 2003: 521, figs 12A-B.
Diagnosis: The male is similar to D. nudulus Wang 2003 in lacking a patellar apophysis and having a short conductor, but can be distinguished by the short RTA (half or less than half of tibial length), the spoon-shaped median apophysis, and the slightly lobed embolic base.
Description: Male. See Wang et al. (1990) and Wang (2003).
Female. Unknown.
Distribution: China (Yunnan: Jinhong) (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 page 24
title: Geologic, Geochemical and Geographic Controls on Norm in Produced Water From Texas Oil, Gas, and Geothermal Reservoirs
Creators: name: Fisher, R. Stephen
Publisher: name: The University of Texas at Austin
Year: 1994
Subjects: subject: geochemistry
subject: produced water
subject: NORM
subject: radioactive materials
subject: Texas

description: Water from Texas oil, gas, and geothermal wells contains natural radioactivity that ranges from several hundred to several thousand picocuries per liter (pCi/L). This natural radioactivity in produced fluids and the scale that forms in producing and processing equipment can lead to increased concerns for worker safety and additional costs for handling and disposing of water and scale. Naturally occurring radioactive materials (NORM) in oil and gas operations are mainly caused by concentrations of radium-226 (226Ra) and radium-228 (228Ra), daughter products of uranium-238 (238U) and thorium-232 (232Th), respectively, in barite scale. We examined (1) the geographic distribution of high NORM levels in oil-producing and gas-processing equipment, (2) geologic controls on uranium (U), thorium (Th), and radium (Ra) in sedimentary basins and reservoirs, (3) mineralogy of NORM scale, (4) chemical variability and potential to form barite scale in Texas formation waters, (5) Ra activity in Texas formation waters, and (6) geochemical controls on Ra isotopes in formation water and barite scale to explore natural controls on radioactivity. Our approach combined extensive compilations of published data, collection and analyses of new water samples and scale material, and geochemical modeling of scale precipitation and Ra incorporation in barite.
Aspidodera raillieti Travassos
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
Aspidoderidae
Aspidodera
Aspidodera raillieti

description: Aspidodera raillieti Travassos
Tolypeutes tricinctus (Linnaeus), intestine, Piauí, NHR (CHIOC 4446 b).
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 10, DOI: 10.5281/zenodo.188170
Globoquadrina dehiscens
Creators: name: Bergh, Eugene W.
name: Compton, John S.
Publisher: name: Zenodo
Year: 2022
Subjects: Biodiversity
Taxonomy
Chromista
Foraminifera
Globothalamea
Rotaliida
Catapsydracidae
Globoquadrina
Globoquadrina dehiscens

description: Globoquadrina dehiscens (Chapman, Parr & Collins, 1934)
Pl. 7, figs. 2–3
Globorotalia dehiscens Chapman et al., 1934, p. 569, pl. 11, fig. 36.
Globoquadrina dehiscens dehiscens Jenkins, 1960. P. 354, pl. 3, fig. 3a–c.
Globoquadrina dehiscens Jenkins, 1960, p. 355, pl. 3, fig. 4a–c; Kennett & Srinivasan, 1983, p. 184, pl. 45, figs. 7–9; Kender et al., 2008, p. 521, pl. 29, fig. 1.
Description: The test surface is cancellate. The test is trochospiral and roughly quadrate in outline. There are four chambers visible in the final whorl. The sutures between chambers are strongly incised. The spiral side is nearly flat. The aperture is dentate and central to the four final chambers.
Remarks: The relative abundances of Globoquadrina dehiscens form a minor component (<10%) of the planktic foraminiferal assemblage in core 2658. In the deeper cores (2670 and 2682), the relative abundances of Globoquadrina dehiscens are below 5%. The tests are relatively small to moderate in size, measuring up to 0.5 mm in diameter.
Environmental preferences: This species has been associated with tropical to temperate surface waters (Kennett & Srinivasan, 1983; Bicchi et al., 2003).
Global stratigraphic range: Globoquadrina dehiscens has been documented to occur in strata dated to the early to late Miocene – Aquitanian to Messinian (Kennett & Srinavasan, 1983; Wade et al., 2011).
Regional occurrence: This species has been recorded in Miocene-aged strata of the Congo Basin (Kender, 2007) to the northern Namibian outer continental shelf, south of the Kunene River mouth (this study) and the southwestern shelf of South Africa (Compton et al., 2004).
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 30, DOI: 10.11646/zootaxa.5091.1.1, http://zenodo.org/record/5840434
Globorotalia archeomenardii Bolli 1957
Creators: name: Bergh, Eugene W.
name: Compton, John S.
Publisher: name: Zenodo
Year: 2022
Subjects: Biodiversity
Taxonomy
Chromista
Foraminifera
Globothalamea
Rotaliida
Globorotaliidae
Globorotalia
Globorotalia archeomenardii

description: Globorotalia archeomenardii Bolli, 1957
Pl. 7, figs. 4a–c
Globorotalia archeomenardii Bolli, 1957, p. 119, pl. 28, fig. 11; Bolli et al., 1985, p. 223, pl. 32, fig. 6; Kender et al., 2008, p. 521.
Description: The wall surface is smooth and macroperforate. The test has a keeled margin, is compressed, unequally biconvex, with up to five crescent-shaped chambers visible on the umbilical side, rapidly increasing toward the apertural end. The chambers increase in size toward the terminal end. Earlier chambers are slightly pustulose on the umbilical side opposite the apertural opening. The sutures are depressed, oblique, radial and slightly curved. The aperture is an extra-umbilical slit.
Remarks: Specimens of G. archeomenardii are not very abundant and only occur as trace in some of the samples. The tests are moderate in size, measuring 0.4 mm in width and 0.65 mm in length.
This species is placed within the Globorotalia menardii group or ‘ Menardella’ lineage and identified as G. archeomenardii based on its keeled margin, chamber arrangement, outline and test structure. G. archeomenardii differs from its descendent G. praemenardii in being smaller and has a more biconvex outline in side view and equatorial section. Its spiral side is also more curved. This species differs from G. menardii in generally being smaller, more lobate and having a less developed or thinner keel (Kennett & Srinivasan, 1983). G. menardii is more rounded in outline and has more chambers in its last whorl, usually up to six or six and a half.
G. archeomenardii is considered to have evolved from Globorotalia praescitula in tropical conditions during the early Miocene (Kennett & Srinivasan, 1983).
Global stratigraphic range: This species has been recorded to occur in the Miocene from the Burdigalian to the Serravalian (Kennett & Srinivasan, 1983; Wade et al., 2011; BouDagher-Fadel, 2015).
Environmental preferences: G. archeomenardii is recorded to occur in subtropical to tropical waters (BouDagher-Fadel, 2015).
Regional occurrence: This species occurs in middle Miocene strata from the Congo Basin (Kender et al., 2008) to the outer continental shelf of Namibia, 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 pages 30-31, DOI: 10.11646/zootaxa.5091.1.1, http://zenodo.org/record/5840434
Globigerina bulloides d'Orbigny 1826
Creators: name: Bergh, Eugene W.
name: Compton, John S.
Publisher: name: Zenodo
Year: 2022
Subjects: Biodiversity
Taxonomy
Chromista
Foraminifera
Globothalamea
Rotaliida
Globigerinidae
Globigerina
Globigerina bulloides

description: Globigerina bulloides d’Orbigny, 1826
Pl. 7, figs. 5–6
Globigerina bulloides d’Orbigny, 1826, p. 277; Lowry, 1987, p. 354, pl. 24, figs. 1a–c; Banner & Blow, 1960, p. 3, pl. 1, figs. 1a–c; Bé & Hamlin, 1967, p. 98, fig. 8; Hayward, 1983, p. 64, figs. 2C–E; Bolli et al., 1985, p. 321, figs. 4.1–2; Spezzaferri et al., 2018a, p. 183, pl. 6.2, figs.1–16.
Description: The test wall is calcareous and macroperforate, with the test being covered with short bases from which spines of the living form would extend between pores. The chambers are globular in shape and trochospirally arranged. There are four spherical enlarging chambers in the final whorl, with the terminal chamber being the largest. The sutures between chambers on all sides are depressed. One large aperture is formed in an asymmetric arch in the final chamber and is umbilically positioned.
Remarks: This species is a major component (<80% of the planktic assemblage) in samples of all three cores. The tests are up to 0.5 mm in diameter.
This species might be confused with those of Globigerinella when viewed from the umbilical angle, but there are differences among the various species. Globigerina bulloides is different from its Globigerinella counterparts by the location of its aperture, trochospire and pore density. In G. bulloides, the large aperture is located more centrally or umbilical, compared to Globigerinella obesa and Globigerinella siphonifera. The trochospire in Globigerinella spp. is also lower compared to G. bulloides. This species also has a higher pore density and the final chamber is less inflated compared to that of Globigerinella. The terminal chamber is also closer in size to the preceding chambers, whereas the chambers increase in size more rapidly in G. obesa. G. bulloides also has one less chamber in the final whorl compared to Globigerinella praesiphonifera. G. bulloides and Globigerinella, however, form different phylogenetic lineages (Spezzaferri et al., 2018a).
Environmental preferences: G. bulloides is a good indicator of upwelling conditions, particularly along the fringes of upwelling centers (Giraudeau, 1993). This species also occurs in transitional to temperate ocean waters (Kucera, 2007).
Global stratigraphic range: This species has a long stratigraphic time range, having been documented to occur from the upper Oligocene to Recent (Kennett & Srinivasan, 1983; Bolli et al., 1985).
Regional occurrence: This is an abundant species ranging from the Neogene to Quaternary along the continental margin of northern Namibia (this study) and South Africa (Lowry, 1987; Giraudeau, 1993; Wefer et al., 1998; Rau, 2002; Rau et al., 2002).
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 31-32, DOI: 10.11646/zootaxa.5091.1.1, http://zenodo.org/record/5840434
Reentrant topological phase in half-Heusler compounds
Creators: name: Araújo, Augusto L.
name: de Lima, Felipe Crasto
name: Fazzio, Adalberto
Publisher: name: arXiv
Year: 2024
Subjects: subject: Materials Science (cond-mat.mtrl-sci)
subject: FOS: Physical sciences

description: Half-Heusler compounds are known for their various compositions and multifunctional properties including topological phases. In this study, we investigate the topological classification of this class of materials based on the ordering of the $Γ_6$, $Γ_8$ states, and a previously overlooked $Γ_6^*$ state, during an adiabatic expansion process. Using first-principles calculations based on density functional theory, we observed that the non-trivial topology is governed by a three-band mechanism. We provide a simple model derived from $k\cdot p$ Hamiltonian that interprets the topological phase in half-Heusler systems. Additionally, we explore the robustness of the topological phase under tension and a new perspective on the topological nature of half-Heusler compounds.
title: Outcrop Characterization of Low-Accommodation Fluvial-Deltaic Reservoir Analogs: Field Guide to Selected Outcrops of the Lower Cretaceous Fall River Formation, Black Hills of South Dakota and Wyoming
Creators: name: Gardner, Michael H.
name: Willis, Brian J.
name: Dutton, Shirley P.
name: Dharmasamadhi, W.
name: Gabel, Scott Thomas
name: Broquet, Charl
name: Geesaman, Richard C.
name: Kreisa, Ron
Publisher: name: The University of Texas at Austin
Year: 1994
Subjects: subject: petroleum
subject: reservoirs
subject: outcrops
subject: fluvial-deltaic systems
subject: Fall River Formation
subject: Cretaceous
subject: Black Hills
subject: South Dakota
subject: Wyoming

description: Hydrocarbon recovery efficiency is controlled by reservoir heterogeneities resulting from geometric arrangements of strata, or "stratal architecture." Maximizing recovery requires an increased understanding of geologic processes that govern stratal architecture. Reservoir characterization studies integrate geologic descriptions of reservoir architecture with reservoir engineering to more effectively recover hydrocarbons. Fluvial-deltaic strata form the most heterogeneous class of siliciclastic reservoirs, with an average recovery efficiency ranging from 24 to 69% and averaging 40% (Galloway and others, 1988). Accordingly, it is of particular interest to determine controls on stratal architecture in fluvial-deltaic reservoirs. Traditional reservoir characterization relates depositional systems to variations in stratigraphic architecture (Fisher and others, 1969). Depositional systems are a three-dimensional linkage of contemporaneous facies assemblages that are governed by a common suite of depositional processes (Brown and Fisher, 1977). This approach has provided important insights but fails to view heterogeneities within a stratigraphic context.
Draconarius curiosus 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 curiosus

description: Draconarius curiosus Wang 2003
(Figs 70-76, 535)
Draconarius curiosus Wang 2003: 526, figs 23A-D (male holotype, male and female paratypes from Tengchong County, Yunnan, China, in HNU and CAS, examined).
Diagnosis: The female is similar to D. griswoldi Wang 2003 by the absence of epigynal teeth and laterally extending copulatory ducts, but can be distinguished by the coiled spermathecae (Figs 70-71; Wang 2003: figs 23A-B). The male can be easily distinguished from all other coelotines by the absence of a median apophysis and the presence of a broad, distally enlarged embolus (Figs 72-74).
Description: See Wang (2003). Photos of habitus, eyes, labium and genitalia are provided in this study (Figs 70-76).
Distribution: China (Yunnan: Tengchong) (Fig. 535).
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 30-31
title: Depositional and Structural Challenges of the Wilcox Lobo Natural Gas Trend, South Texas
Creators: name: Hamlin, H. Scott
name: Dickerson, Patricia Wood
name: Hentz, Tucker F.
Publisher: name: The University of Texas at Austin
Year: 1994
Subjects: subject: natural gas
subject: Wilcox Lobo Trend
subject: deposition
subject: structure
subject: South Texas

description: To increase understanding and utilization of gas resources in the Wilcox Lobo play of South Texas, this report reviews current geological knowledge of the Lobo trend. An additional objective of this report is to identify areas where advancements in geological understanding could lead to substantial improvements in efficient development of the Wilcox Lobo trend natural gas resource. According to published accounts, Lobo sandstones formed in a variety of depositional environments in both shallow and deep marine waters. During and after deposition, the Lobo experienced repeated episodes of erosion, faulting, and diagenesis. Thus, accurate prediction of reservoir sandstone attributes is difficult, and this difficulty is cited by operators as a significant challenge to efficiently targeting the remaining gas resource. Knowledge that would aid in the emergence of this resource includes information on sandstone correlation and accurate zone identification, depositional systems and facies interpretations, controls on fault pattern variability, and, to a lesser extent, recognition of diagenetic patterns and faults and fractures that are below seismic resolution. Geologic challenges of the Lobo trend are opportunities for targeting increasingly smaller and more difficult-to-detect compartments with advanced technology.
Aspidodera vazi Proenca
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
Aspidoderidae
Aspidodera
Aspidodera vazi

description: Aspidodera vazi Proença
Tolypeutes tricinctus (Linnaeus), unspecified site of infection, Piauí, NHR (CHIOC 4446c).
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 10, DOI: 10.5281/zenodo.188170
Globigerina concinna Reuss 1850
Creators: name: Bergh, Eugene W.
name: Compton, John S.
Publisher: name: Zenodo
Year: 2022
Subjects: Biodiversity
Taxonomy
Chromista
Foraminifera
Globothalamea
Rotaliida
Globigerinidae
Globigerina
Globigerina concinna

description: Globigerina concinna Reuss, 1850
Pl. 7, figs. 7-8
Globigerina concinna Reuss, 1850, p. 373, pl. 47, fig. 8; Cushman and Stainforth, 1945, pl. 13, fig. 1; Bolli et al., 1985, p. 321, fig. 4.17–20.
Description: The wall surface is cancellate spinose. The test is trochospirally arranged, with five globular chambers in the final whorl. The sutures are straight and depressed. The aperture is large and umbilical.
Remarks: The relative abundance of G. concinna in this study is trace (<1%) in samples of all three cores. The tests are relatively moderate in size, measuring up to 0.5 mm in diameter.
This species is similar to an older form, Ciperoella ciperoensis (previously Globigerina ciperoensis), but differs in its size, chambers and aperture. The chambers of G. concinna increase in size more rapidly and its test is generally larger compared to C. ciperoensis. The aperture of G. concinna is also larger and more asymmetrical than C. ciperoensis. The two species, furthermore, occur in different stratigraphic ranges. C. ciperoensis occurs in the Oligocene, whereas G. concinna occurs in middle Miocene strata (Bolli et al., 1985).
Environmental preferences: Species in the G. concinna group is regarded to be adapted to tropical and subtropical conditions (BouDagher-Fadel, 2015).
Global stratigraphic range: G. concinna has been documented to occur from the Burdigalian in the early Miocene to the Serravallian in the middle Miocene (BouDagher-Fadel, 2015).
Regional occurrence: This study records the first, and to date, only occurrence in the region of this species in the middle Miocene of the northern Namibian 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 32, DOI: 10.11646/zootaxa.5091.1.1, http://zenodo.org/record/5840434
title: Identification of Remaining Oil Resource Potential in the Frio Fluvial/Deltaic Sandstone Play, South Texas
Creators: name: Holtz, Mark H.
name: McRae, Lee E.
Publisher: name: The University of Texas at Austin
Year: 1994
Subjects: subject: resources
subject: Frio Formation
subject: fluvial-deltaic systems
subject: South Texas

description: The Frio Fluvial/Deltaic Sandstone (Vicksburg Fault Zone) oil play of South Texas has produced nearly 1 billion stock tank barrels (BSTB) of oil, yet still contains about 1.2 BSTB of unrecovered mobile oil and an even greater amount of residual oil resources (1.5 BSTB). More than half of the reservoirs in this depositionally complex play have been abandoned, and large volumes of oil may remain unproduced unless advanced characterization techniques are applied to define incompletely drained and untapped reservoirs as suitable targets for near-term recovery. Interwell-scale geological facies models of Frio fluvial/deltaic reservoirs will be combined with engineering assessments and geophysical evaluations to characterize Frio fluvial/deltaic reservoir architecture, flow unit boundaries, and the controls that these characteristics exert on the location and volume of unrecovered mobile and residual oil. These results will lead directly to the identification of specific opportunities to exploit these heterogeneous reservoirs for incremental recovery by recompletion and strategic infill drilling. Reservoir attribute data were statistically analyzed from oil and gas fields throughout the geographic area covered by the Frio Fluvial/Deltaic Sandstone oil play. General reservoir attributes analyzed in detail included porosity, initial water saturation, residual oil saturation, net pay, reservoir area, and fluid characteristics. Statistical analysis of variance demonstrated no difference between oil reservoir attributes and gas reservoir attributes, indicating that oil and gas reservoirs are subsets of a larger genetically similar population. Probability functions that describe attribute frequency distributions were determined for use in risk-adjusting resource calculations. Different functions were found to be most applicable for the various petrophysical reservoir attributes.
Draconarius curvus 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 curvus

description: Draconarius curvus sp. nov.
(Figs 77-83, 536)
Type material: Holotype. ♀, CHINA: Yunnan: Tengchong County: Wuhe, Xiao Di Fang River, N24.8486 0, E098.75913°, 2040 m, beating along the river, May 23, 2005, H.M. Yan & K.J. Guo (HNU, CASENT9025617).
Etymology: The species name is derived from Latin word “curvus”, which means “bent”, and refers to the coiled copulatory ducts; adjective.
Diagnosis: The female can be easily recognized by the absence of epigynal teeth, the coiled copulatory ducts, and the widely separated, round spermathecae (Figs 77-78).
Description: Female (holotype). Median sized Coelotinae, total length 5.70 (Fig. 81). Dorsal shield of prosoma 2.35 long, 1.95 wide; opisthosoma 3.40 long, 2.75 wide. AME smallest, 2 /3 size of other eyes, which are subequal (AME 0.08, ALE 0.12, PME 0.12, PLE 0.12); anterior eyes close together, separated by half of AME diameter; PME separated from each other by half of their diameter, from PLE by slightly more than half of their diameter (AME-AME 0.04, AME-ALE 0.04, ALE-PLE 0. 04, PME-PME 0.06, PME-PLE 0.08, AME-PME 0.07) (Fig. 82). Chelicera with 3 promarginal and 3 retromarginal teeth. Labium wider than long (L / W =0.88) (Fig. 83). Epigynum without epigynal teeth; atrium small, two times wider than long, close to epigastric furrow; copulatory ducts originating posteriorly, strongly coiled with at least two to three coils; spermathecal bases small, round, widely separated by two times their width; spermathecal stalks slender, anteriorly extending and converging, covered by copulatory ducts in dorsal view; spermathecal heads arising distally, slightly extending laterally (Figs 77-80).
Male. Unknown.
Distribution: China (Yunnan: Tengchong) (Fig. 536).
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 31-33
wolf
Creators: name: Hope, Cat
name: Ek, Robert
Publisher: name: Monash University
Year: 2025
Subjects: classificationCode: 360302
subject: Music composition and improvisation
classificationCode: 360304
subject: Music performance

description: For bass clarinet, Music in Motion hardware and modular synthesiser.Cat Hope for and with Robert Ek (2023)The score is proportional, and read vertically (lowest pitches on the right, highest on the left). The lowest note written for the clarinet should be as low as possible on the instrument; the lowest notes on the synthesiser should be on the cusp of human hearing. The motion of the clarinetist should control the modular frequency via their movement. The envelope is described by the range of green shapes. They dynamic is a consistently medium soft, with entries and exits starting and ending at nothing.The score should be read in the Decibel ScorePlayer application on an iPad. The modular should be run through 2 x subwoofer speakers, one for each part.Program NoteThis piece explores the ways bass clarinet and modular synthesis interact timbrally, using movement as a way to blend them choreographically as well as sonically.Acknowledgements
This piece was composed with support of the Hamburg Institute for Advanced Study.
Performances
Sounds of Stockholm Festival, December 2023 by Robert Ek (listen here)TENOR, Zurich, April, 2024 by Robert Ek (watch here)
Hypnos Theatre, Malmo, December 2024 by Robert Ek
Globigerinella obesa
Creators: name: Bergh, Eugene W.
name: Compton, John S.
Publisher: name: Zenodo
Year: 2022
Subjects: Biodiversity
Taxonomy
Chromista
Foraminifera
Globothalamea
Rotaliida
Globigerinidae
Globigerinella
Globigerinella obesa

description: Globigerinella obesa (Bolli, 1957)
Pl. 7, figs. 9–10
Globorotalia obesa Bolli, 1957, p. 119, pl. 29, figs 2–3.
Globigerina praebulloides Blow, 1959, pl. 8, fig. 47; Kender, 2007, p. 202, pl. 49, fig. 7.
Globigerinella obesa Bolli et al., 1985, p. 206, fig. 26.44; Kennett & Srinivasan, 1983, p. 234, pl. 59, figs 2–5; Kender et al., 2008, p. 202, pl. 29, fig. 4; Spezzaferri et al., 2018a, p. 198, pl. 6.1, figs. 14–17; pl. 6.8, figs. 1–23.
Description: The wall surface is cancellate-spinose. The test is trochospirally arranged with the chambers globular in shape, which rapidly enlarge towards the terminal end. Four chambers are visible in the final whorl in umbilical view, with straight depressed sutures. The test is biconvex in marginal view and has a lobate outline in umbilical view.A thin imperforate lip may border the apertural arch. The aperture extends from the umbilical to extra-umbilical region, forming an arched shape visible in the peripheral margin view.
Remarks: The relative abundance of G. obesa in this study is trace (<1%) in samples of all three cores. The tests are relatively moderate in size, measuring up to 0.5 mm in diameter.
G. obesa is ancestral to Globigerinella siphonifera, which later gave rise to Globigerinella calida. This species evolved from G. archaeobulloides and is different from that species in its aperture, which is more umbilical to extraumbilical towards the margin of the test. It also differs from G. bulloides in this way and has a more inflated terminal chamber compared to its initial chambers. G. obesa is different from G. praesiphonifera in having four chambers in the last whorl, whereas G. praesiphonifera has five (Spezzaferri et al., 2018a). Globigerina praebulloides is synonymised and now accepted as G. obesa.
Environmental preferences: G. obesa has been identified as a warm to temperate species (Bicchi et al., 2003).
Global stratigraphic range: G. obesa has been recorded in Oligocene to lower Pliocene strata (Kennett & Srinivasan, 1983).
Regional occurrence: This species has been recorded to occur in middle Miocene strata from the Congo Basin (Kender et al., 2008) to the northern 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 pages 32-33, DOI: 10.11646/zootaxa.5091.1.1, http://zenodo.org/record/5840434
title: Evaluation of the Ground Penetrating Radar (GPR) Survey at TDCJ Playa, Carson County
Creators: name: Hovorka, Susan D.
Publisher: name: The University of Texas at Austin
Year: 1994
Subjects: subject: ground-penetrating radar (GPR)
subject: survey
subject: playas
subject: Carson County
subject: Texas

description: A ground-penetrating radar (GPR) survey conducted at TDCJ playa, Carson County, imaged soil structures to depths of 2 to 4 m. Layering in soils, including the modern soils and several buried horizons, is parallel to the surface throughout the transect, which runs from the upland, down the slope of the playa lake basin, to the edge of the ephemeral playa lake. Little evidence of truncation of soil horizons is apparent on the images, suggesting that the playa basins are part of an accretionary rather than an incised landscape. Two trenches (1.9 to 2.5 m deep) and four boreholes near the GPR line confirm the horizontal structure of the soil and also document lateral changes not apparent on GPR. Interpretation of GPR is limited because of uncertainty in matching the GPR image to observed soil features, artificial changes in the character of the GPR image at segment boundaries, and sloping features on GPR images that could not be recognized in trenches.
Draconarius catillus 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 catillus

description: Draconarius catillus sp. nov.
(Figs 62-69, 535)
Type material: Holotype. ♂, CHINA: Yunnan: Fugong County: 1 km E Yaping Pass, turning rocks among dormant bamboo, N27.20854°, E98.20854°, 3506 m, May 6, 2004, C. Griswold (HNU, CASENT 9020765).
Paratype. CHINA: Yunnan: Lushui County: 1♂, Feng Xue Yakou, 100 m S of Pianma Road, N25.97288°, E98.68336°, 3150 m, Rhododendron/Bamboo thicket, pitfall traps, May 11-21, 2005, C. Griswold, D. Kavanaugh & K.J. Guo (CAS, CASENT9022109).
Etymology: The species name is derived from Latin word “catillus”, which means "small bowl, dish, plate", and refers to the broad, dish-shaped conductor; noun in apposition.
Diagnosis: The male is similar to D. nudulus Wang 2003 in having a short conductor, a proximally originating embolus, and in lacking a patellar apophysis, but can be distinguished by the large, distally protruding cymbial furrow and the spoon-shaped median apophysis (Figs 62-63).
Description: Male (holotype). Medium sized Coelotinae, total length 7.45 (Fig. 67). Dorsal shield of prosoma 4.10 long, 2.85 wide; opisthosoma 3.35 long, 2.10 wide. AME smallest, half the size of ALE; ALE largest; PME slightly larger than AME, PLE slightly smaller than ALE (AME 0.07, ALE 0.14, PME 0.09, PLE 0.12); AME separated from each other by their diameter, from ALE by 1.5 times AME diameter; PME separated from each other by approximately 1.5 times PME diameter, from PLE by slightly less than two times PME diameter (AME-AME 0.07, AME-ALE 0.10, PME-PME 0.12, PME-PLE 0.16, AME-PME 0.12) (Fig. 68). Chelicera with 3 promarginal and 2 retromarginal teeth. Labium longer than wide (L / W =1.16) (Fig. 69). Palp without a patellar apophysis; RTA more than half of tibial length, with a sharply protruding distal end; lateral tibial apophysis broad, close to RTA; cymbial furrow large, slightly less than cymbial length, with distal end slightly protruding beyond cymbium; conductor broad, short, with a large basal lamella and a dorsal apophysis; median apophysis spoon-shaped, elongated, free-standing along anterior edge; embolus long, filiform, proximal in origin, with thread arising at 6- o’clock-position, running half an oval, extending posteriorly to middle part of tibia and anteriorly coiling beyond distal part of bulb (Figs 62-66).
Female. Unknown.
Distribution: China (Yunnan: Lushui, Fugong) (Fig. 535).
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 28-29
Heterakis arquata Scheneider
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
Heterakidae
Heterakis
Heterakis arquata

description: Heterakis arquata (Scheneider)
Psophia viridis obscura Pelzeln, instetine, Rondônia (Vicente et al. 1995) (CHIOC 0 7, 859a̅f, 4448).
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 10, DOI: 10.5281/zenodo.188170
Additional file 1: of The impact of retirement on age related cognitive decline â   a systematic review
Creators: name: Meng, Annette
name: NexĂ¸, Mette
name: Borg, Vilhelm
Publisher: name: Figshare
Year: 2017
Subjects: subject: Medicine
subject: Physiology
subject: FOS: Biological sciences
subject: 39999 Chemical Sciences not elsewhere classified
subject: FOS: Chemical sciences
subject: Sociology
subject: FOS: Sociology
subject: 69999 Biological Sciences not elsewhere classified
subject: Developmental Biology
subject: Science Policy

description: Quality assessment check list. Description of data: The quality assessment list that was used in the evaluation of the studies. (DOCX 16Â kb)
Globigerinoides subquadratus Bronnimann 1954
Creators: name: Bergh, Eugene W.
name: Compton, John S.
Publisher: name: Zenodo
Year: 2022
Subjects: Biodiversity
Taxonomy
Chromista
Foraminifera
Globothalamea
Rotaliida
Globigerinidae
Globigerinoides
Globigerinoides subquadratus

description: Globigerinoides subquadratus Brönnimann, 1954
Pl. 7, figs. 11–12
Globigerinoides subquadratus Brönnimann, 1954, p. 680, pl. 1, fig. 8; Kennett & Srinivasan, 1983, p. 74, pl. 10, fig. 4; pl. 16, figs. 1–3.
Description: The wall surface is macroperforate and cancellate-spinose. The test is trochospiral, sub-globular to sub-quadrate in shape and semi-circular in cross section. The chambers are sub-rounded to sub-quadrate in shape, with two basal chambers on the umbilical side, separated by a straight deep incised suture, which is overarched by a large chamber. The final chamber comprises approximately half the size of the test. The primary aperture is large and forms an arch symmetrically above the two basal chambers in apertural view. Two supplementary apertures form on the spiral side of the test along sutures of earlier chambers.
Remarks: The relative abundances of Gs. subquadratus are major (<25%) in samples along the Mio-Pliocene contact of all three cores, increasing in abundance in the deeper cores. The tests of Gs. subquadratus are relatively small, measuring 0.3 mm in diameter.
This species is very similar to Globigerinoides ruber,but are stratigraphically separate and can be morphologically differentiated. Gs. subquadratus is identified in the Miocene, whereas Gs. ruber is extant and occurs in younger strata. Morphologically, the shape and outline of the test and chambers of Gs. subquadratus is more quadrate in shape compared to Gs. ruber (Bolli et al., 1985).
Environmental preferences: Gs. subquadratus is associated with Neogene tropical environments (Brönnimann et al., 1971; Wade et al., 2011).
Global stratigraphic range: This species occurs in Miocene strata from the Aquitanian to Tortonion (Kennett & Srinivasan, 1983; Wade et al., 2011).
Regional occurrence: Gs. subquadratus has been identified in middle Miocene strata from the Congo Basin (Kender et al., 2008) and the northern 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 33, DOI: 10.11646/zootaxa.5091.1.1, http://zenodo.org/record/5840434
Heterakis oscari Travassos, Pinto & Muniz
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
Heterakidae
Heterakis
Heterakis oscari

description: Heterakis oscari Travassos, Pinto & Muniz
Crax blumenbachii Spix, intestine, Mato Grosso do Sul (Travassos et al. 1927; 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 10, DOI: 10.5281/zenodo.188170
Draconarius degeneratus Liu & Li, comb. 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 degeneratus

description: Draconarius degeneratus (Liu & Li 2009) comb. nov.
(Fig. 536)
Coelotes degeneratus Liu & Li 2009: 666, figs 1-6 (male holotye, male and female paratypes from Jianshui County, Yunnan, in IZCAS, not examined).
Diagnosis: This species is similar to D. uncatus (Liu & Li 2009) in having a long patellar apophysis and a short, slender conductor in the male, and a similar female epigynum, but can be distinguished by the prolaterally originated embolus in the male and the broad epigynal teeth in the female (Liu & Li 2009: figs 1-6).
Description: See Liu & Li (2009).
Distribution: China (Yunnan: Jianshui) (Fig. 536).
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 page 33
Additional file 1: of Retroclavicular approach vs infraclavicular approach for plexic bloc anesthesia of the upper limb: study protocol randomized controlled trial
Creators: name: PL Langlois
name: AF Gil-Blanco
name: D Jessop
name: Y Sansoucy
name: F DâAragon
name: N Albert
name: P Echave
Publisher: name: Figshare
Year: 2017
Subjects: subject: 19999 Mathematical Sciences not elsewhere classified
subject: FOS: Mathematics
subject: Science Policy
subject: Computational Biology

description: SPIRIT 2013 checklist of recommended items to address in a clinical trial protocol. Corresponds to the checklist of required items in a protocol and the corresponding pages in this manuscript. (DOC 121 kb)
The Earth Defeats Me
Creators: name: Hope, Cat
Publisher: name: Monash University
Year: 2025
Subjects: classificationCode: 360302
subject: Music composition and improvisation

description: For 2 sustaining instruments and partition concrete.

This piece was co-composed with French music concrete artist Lionel Marchetti. It is scored for two sustaining instruments and an audio track created by Marchetti, which you can hear on its own here.The work is performed on the Decibel ScorePlayer ipad application. The file contains Marchetti's audio file synchronised with the score - you will need to run the audio from the ipad into two bass amps. You can also play the film whilst reading the score - it has the partition concrete embedded in it.
All other instructions are in the score. If you need help with how to upload the score into the player, go here. This is a partner piece to another piece by Cat Hope/Lionel Marchetti, 'The Last Days of Reality' for bass flute and tam tam, composed in 2018. A digital an hard copy of the score is available from Material Press.In 2021, Karl Ockelford made a film for this work, which was premiered in live performancer in Malmo, Sweden, in 2024.PERFORMANCESPremiere: Shock of the New, Perth, 2015. Performed by Cat Hope and Lindsay Vickery
TENOR Conference, Anglica Ruskin University, Cambridge UK, July 2016.
Forum Neue Musik in der Christianskirche, Hamburg, Germany, November 2017.
Feature4d on the 'Last Days of Reality' album on Room 40, 2018.Malmo, Sweden, December 2024.
Additional file 2: of Effectiveness and cost-effectiveness of daily all-over-body application of emollient during the first year of life for preventing atopic eczema in high-risk children (The BEEP trial): protocol for a randomised controlled trial
Creators: name: Chalmers, Joanne
name: Haines, Rachel
name: Mitchell, Eleanor
name: Thomas, Kim
name: Brown, Sara
name: Ridd, Matthew
name: Lawton, Sandra
name: Simpson, Eric
name: Cork, Michael
name: Sach, Tracey
name: Bradshaw, Lucy
name: Montgomery, Alan
name: Boyle, Robert
name: Williams, Hywel
Publisher: name: Figshare
Year: 2017
Subjects: subject: Medicine
subject: Microbiology
subject: FOS: Biological sciences
subject: Pharmacology
subject: Biotechnology
subject: Sociology
subject: FOS: Sociology
subject: Developmental Biology
subject: 111714 Mental Health
subject: FOS: Health sciences
subject: 110309 Infectious Diseases

description: Diagnostic criteria (UK Working Party Diagnostic Criteria for Atopic Dermatitis). (DOCX 11 kb)
Heterakis psophiae Travassos
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
Heterakidae
Heterakis
Heterakis psophiae

description: Heterakis psophiae Travassos
Psophia viridis obscura Pelzeln, intestine, Rondônia (Vicente et al. 1995) (CHIOC 0 6 ̅ holotype and allotype, 855, 856a̅c – paratype, 9665 – paratype, 20847 – paratype).
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 10, DOI: 10.5281/zenodo.188170
Trilobatus bisphericus
Creators: name: Bergh, Eugene W.
name: Compton, John S.
Publisher: name: Zenodo
Year: 2022
Subjects: Biodiversity
Taxonomy
Chromista
Foraminifera
Globothalamea
Rotaliida
Globigerinidae
Trilobatus
Trilobatus bisphericus

description: Trilobatus bisphericus (Todd, 1954)
Pl. 8, figs. 1–2
Globigerinoides bisphericus Todd, 1954, p. 681, pl. 1, fig.1; Reed, 1965, p. 83, pl. 15, fig. 1–2; Bolli et al., 1985, p. 199, pl. 24, fig.8; Kender et al., 2008, p. 520, pl. 27, figs. 5, 8.
Globigerinoides sicanus Kennett & Srinivasan, 1983, p. 62, pl. 13, fig. 4–6.
Description: The wall surface is macroperforate and cancellate. The test is rounded and circular in cross section. The three to four chambers in the final whorl are globular in shape. The larger chamber envelops earlier chambers, hiding the umbilicus. The sutures are strongly depressed. Secondary apertures form along deep sutures.
Remarks: The relative abundances of T. bisphericus are trace (<1%) in samples of all three cores. The tests are small, measuring 0.3 mm in diameter.
Bolli et al. (1985) note Trilobatus trilobus (previously Globigerinoides trilobus) to be ancestral to T. bisphericus.
Environmental preferences: This species is recorded to be adapted to warm waters (Bicchi et al., 2003), as well as being a cosmopolitan species (BouDagher-Fadel, 2015).
Global stratigraphic range: T. bisphericus is an indicator species of the early to middle Miocene – Burdigalian to Langhian (Kennett & Srinivasan, 1983; Bolli et al., 1985; BouDagher-Fadel, 2015).
Regional occurrence: This species is recorded to occur in middle Miocene strata in the Congo Basin (Kender et al., 2008) to the northern 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 pages 33-34, DOI: 10.11646/zootaxa.5091.1.1, http://zenodo.org/record/5840434