5,583 research outputs found
J.C. Steyn Collection index
This index describes the J. C. Steyn collection which includes background material for 3 biographies by J.C. (Jaap) Steyn namely N.P. van Wyk Louw, P.J. Cillié and MER (M.E. Rothman). Prof. J.C. Steyn (1939-) is an educationist, linguist and author. Correspondence ; clippings ; photographs ; book reviews ; articles ; speeches ; varia compiled in 23 pamphlet boxes
Recommended from our members
Microfaunal evidence of age and depositional environments of the Cerro Prieto section (Plio-Pleistocene), Baja California, Mexico
Microfossils including benthic and planktic foraminifera, ostracodes, calcareous algae, fish skeletal material, and fragments of pelecypods were found in 14 core samples from depths of 185 to 1952 m in the Cerro Prieto geothermal field, providing evidence of both the age and depositional history of sediments comprising the 3000-m-thick Pliocene and Pleistocene section in this area. Ostracodes of brackish water and marine origin constitute the most common microfossils present in this sequence occurring in 8 samples; in situ littoral and neritic species of benthic foraminifera occur in 5 samples with planktic species present in 2 samples. Distributional patterns of ostracodes and foraminifera together with previously analyzed lithofacies (Lyons and van de Kamp, 1980) indicate that the Cerro Prieto section represents an intertonguing complex of alluvial, deltaic, estuarine, and shallow marine environments deposited along the front of the Colorado River delta as it prograded across the Salton Trough during Pliocene and Pleistocene time. Foraminiferal evidence indicates that a sand and shale unit commonly present at depths between 700 and 1100 m represents a significant mid-Pleistocene marine incursion in the Cerro Prieto area. Tentative correlation of the Cerro Prieto section with the well dated Palm Springs Formation of the Imperial Valley, California area suggests that the Pliocene/Pleistocene boundary occurs at a depth of approximately 2000 m in the area of well M-93. Reworked specimens of Cretaceous foraminifera and fragments of the Cretaceous pelecypod Inoceramus were found in five samples further substantiating the Colorado Plateau provenance of a significant portion of the Colorado River deltaic sediments in the Cerro Prieto area
Product Innovation Knowledge Transfer for Developing Countries: Towards a systematic Transfer Approach
The transfer of knowledge on product innovation to small- and medium-sized enterprises and local knowledge institutions in developing countries is expected to be one of the key drivers for competiveness and economical growth, and a part of the solution to environmental and social challenge. In that respect, this PhD study focuses on how the process of the current knowledge transfer takes place and how it can be improved. A combination of literature review and empirical research has resulted into a conceptual framework to describe the complex and dynamic process of product innovation knowledge transfer to developing countries. In order to improve this process, a systematic approach has been developed and operationalized by a needs assessment tool and a design manual: The UNEP Design for Sustainability for Developing Economies (D4S-DE) Manual (www.d4s-de.org). Both tools have been tested in practice by practitioners and have been evaluated by an academic review board.Design EngineeringIndustrial Design Engineerin
Where do we draw lines: professional relationship boundaries and the child and youth care practitioner
The question of professional relationship boundaries is a poignant one, in light of the many boundary grey-zones that are created by the variety of young people’s needs, practice settings and professional relationship contexts within the field of child and youth care. In order to support practitioners’ development of critical thought and awareness of professional boundaries, this paper applies a professional relationship boundaries conceptual framework to child and youth care work, and the literature is consulted to explore the impacts of boundary violations, influences on individual’s boundaries, cues to indicate blurring boundaries, and key strategies to maintain balanced boundaries
Dicranopalpus gallaecicus Wijnhoven & Martens & Prieto 2022, sp. nov.
Dicranopalpus gallaecicus sp. nov. urn:lsid:zoobank.org:act: F6BADA91-F315-4D06-BA39-B78ED74C522D Figs 4C–D, 5C, 6C, H, 9A, C, 13–16, 17A Dicranopalpus martini – Prieto et al. 2020: 50. Diagnosis Medium-sized species, males with dark prosoma, with pale patch in front of eye tubercle. Legs dark brown, femora lack trichomes. Etymology The name of the new species refers to the type locality in the north-westernmost Spanish autonomous community of Galicia, in Latin Gallaecia, here with masculine ending, and used as an adjective. Material examined Holotype SPAIN – Galicia • 1 ♂; Pontevedra, O Grove; 42.468° N, 08.898° W; 119 m a.s.l.; 23 Apr. 2019; H. Wijnhoven leg.; pine and eucalyptus forest, collected from loose strips of eucalyptus bark and from a rock face; deposited in collection of Naturalis Biodiversity Centre, Leiden, Netherlands; CHW 491. Paratypes SPAIN – Galicia • 1 ♀; same collection data as for holotype; deposited in collection of Naturalis Biodiversity Center, Leiden, Netherlands; CHW 492 • 6 ♂♂, 1 ♀; same collection data as for holotype; CHW 493 • 12 ♂♂; same collection data as for holotype; CHW 494 • 3 ♂♂; same collection data as for holotype; deposited in collection of C. Prieto, Spain; ZUPV ·6164 • 8 ♂♂, 1 ♀; same collection data as for holotype; deposited in Senckenberg Research Institute, Arachnology, Frankfurt am Main, Germany; CJM 8152. Additional material SPAIN – A Coruña, Santiago, Monte Pedroso • 2 ♀♀; 42.900° N, 8.561° W; 363 m a.s.l.; 12 May 1977; J.C. Otero leg.; pitfall trapping; ZUPV 5932 • 1 ♀; 42.899° N, 8.572° W; 320 m a.s.l.; 28 Oct. 1977; J.C. Otero leg.; ZUPV 5940 • 1 ♀; 42.890° N, 8.557° W; 280 m a.s.l.; 23 Apr. 1977; J.C. Otero leg.; ZUPV 5949. Description Male (holotype) LENGTH. 2.9, width of prosoma 1.9, BLI 1.9. DORSUM (Figs 4C, 15). Ground colour pale yellowish. Prosoma dark brown to almost black, anterior margin of prosoma, and area proximally of eye tubercle pale yellowish. Ozopores oval-shaped, small. Black saddle wide on prosoma, narrowing on opisthosomal tergites I–IV, widening on following tergites. Opisthosomal tergites with paramedian rows of white spots. Tergite IX and lateral margins of opisthosomal tergites pale. EYE TUBERCLE. Base pale yellowish, dorsally greyish, with silvery sheen most distinct around eyes, shallow, canaliculated, slightly wider than long, and somewhat tilted backwards, at less than its length from anterior margin of carapace, dorsally with a few minute black setae. Eyes with narrow black ring. VENTER AND COXAE. Uniformly pale yellowish, with scattered black setae. CHELICERAE (Fig. 5C). Pale yellowish, segment I with dorsolateral brown patch, segment II in dorsoproximal area dark; ventral spur distinct, segment I dorsally, and segment II dorsally and medially near cheliceral claw with stout black setae. PEDIPALPS (Figs 6C, H, 14A–C). Pale yellowish, femur in proximal half, and patella and tibia dorsally with dark brown patches; femoral apophysis pale, robust, about half as long as femur width at its base, femur on ventral side with sensilla chaetica that are slightly longer than other setae on femur; patella slender, apophysis stout, shorter than patella, rod-shaped, widest in distal half (Fig. 6H), in lateral view distinctly curved upwards (Fig. 14A). Tibia mediodistally with a protrusion (Fig. 6C). Tarsus straight, slightly bent ventrally in distal third section; claw pectinate (Fig. 14B). LEGS. Leg lengths I–IV (in parentheses femur lengths): 20 (3.6); 35 (6.2); 21 (3.6); 28 (5.1). Dark brown, trochanters, proximal femur portions, joints and pseudo-articulations paler, additional small pale spots on femora, particularly around the three isolated femoral dorsal slit sensilla (see Wijnhoven 2013, fig. 10B). Tibiae have lighter band in midsection. Leg segments cylindrical, dorsal and dorsolateral sides of femora with sensilla chaetica and a few small black spines. Patellae and tibiae densely covered with trichomes. Tibiae I–IV with 0, 4, 3 and 3 pseudo-articulations, respectively; metatarsi I–IV with 3, 6, 3 and 5 pseudo-articulations, respectively. Tarsi I–IV with 47, 66, 46 and 54 segments, respectively. Numerous bipterate setae on prolateral sides of metatarsus III and IV and in decreasing numbers on proximal tarsomeres 1–7 of leg III and 1–10 of leg IV. PENIS (Fig. 16). Long, robust; length 1.78; truncus slightly widening from base, narrowing in midsection, narrowest in the middle; intrinsic penial muscle in about the basal 2 /5. Glans ovoid, robust, dorsally and ventrally sclerotized and provided with canaliculi, dorsal cavity large, ovoid. Dorsal truncus to glans transition forming a sharp angle (Fig. 16E–F). Sensory setae missing. Stylus about as long as glans, distinctly S-curved; horns slender. VARIABILITY. In some specimens, the dorsal saddle is dark brown, and the tergites VII–VIII are a contrasting reddish-brown. Female LENGTH. 4.3, width of prosoma 2.5, BLI 1.1. DORSUM (Figs 4D, 15). Prosoma with dark brown spots, lateral margins near ozopores dark brown; anterior margin of prosoma and area proximally of eye tubercle silvery. Opisthosoma with small dark brown paramedian patches on tergites III–IV, tergites V–VI with extended dark brown paramedian patches, central area light brown. Opisthosomal tergites with paramedian pairs of white spots and transverse rows of small dark spots. VENTER AND COXAE. Pale yellowish, with scattered black setae. All coxae with subapical dark band. Margins of sternites dark. PEDIPALPS (Fig. 14D–E). Pale yellowish, with dark brown bands on basal half of femur, distal portion of patellar apophysis and tibial apophysis; tibia dark in midsection, dorsolaterally with dark brown elongated patch. Femoral apophysis robust, half as long as femur width, patellar apophysis large, reaching base of tibial apophysis, as thick as tibia. Mediodistal apophysis on tibia as long as wide. Tarsus straight, claw pectinate. LEGS. Leg lengths I–IV (in parentheses femur lengths): 16 (2.7); 29 (5.2); 17 (2.7); 24 (4.5). Colouration as in male. Patella, tibia and tarsus of all legs with trichomes. Tibia II with four pseudo-articulations; metatarsi I–IV with 3, 5, 3 and 4 pseudo-articulations, respectively. SEMINAL RECEPTACLES (Fig. 9A, C). Ovipositor with 22 segments, seminal receptacles in segments 6–8; two long tubes, each proximally with an additional lateral pocket. Distribution and ecology Dicranopalpus gallaecicus sp. nov. is a Spanish endemic species, its distribution probably being restricted to the Galician region (Fig. 13). The type locality (Fig. 17A) is a wooded slope consisting of a Pinus L. and Eucalyptus L’Hér. tree plantation, undergrowth mainly with Common gorse (Ulex europaeus L.). Individuals were present in considerable numbers, and could easily be collected especially on and among shed strips of Eucalyptus bark, hanging from the trees or laying on the forest floor. In two cases, individuals were found in resting position on a shaded rock face. Records based on photos (from https://www.biodiversidadvirtual.org/insectarium/; record number in parentheses) included (Fig. 13): 1 (sub)adult ♀, Pontevedra, Vigo, 21 Apr. 2017 (969655); 1 juv. ♀, Parque forestal do Vixiador, 8 Dec. 2018 (1194231); 1 juv., Parque forestal do Vixiador, 10 Feb. 2019 (1075602); 1 (sub)adult ♀, Pontevedra, Cercedo, 18 Mar. 2017 (985496); 1 ♀, Lugo, Villalba, 11 Jun. 2014 (593557); 1 juv. ♀, Lugo, Villalba, 19 Dec. 2014 (660313); 1 ♂, Lugo, Villalba, 1 Apr. 2015 (679111); 1 ♂, Lugo, Villalba, 17 Apr. 2016 (783897); 1 juv. ♀, Lugo, Villalba, 17 Feb. 2019 (1075059). A species of lower altitudes, with recorded altitudes between 119 and 428 m a.s.l. Phenology: juveniles have been found in December and February, subadults in March and April, adults from April to October, suggesting that eggs hatch in autumn, juveniles overwinter and adults appear in spring.Published as part of Wijnhoven, Hay, Martens, Jochen & Prieto, Carlos E., 2022, Revision of the genus Dicranopalpus from northern Spain and Corsica, with descriptions of two new species (Arachnida, Opiliones, Phalangioidea), pp. 39-73 in European Journal of Taxonomy 839 on pages 56-60, DOI: 10.5852/ejt.2022.839.1931, http://zenodo.org/record/711622
Anthropometry of the Beaver, Sekani, and Carrier Indians:
by J.C. Boileau GrantBulletin (National Museum of Canada) ; 81. Bulletin (National Museum of Canada). Anthropological series. ; 18
J.C. Painter letter to Benjamin Lundy
Letter from J.E. Painter to (presumably) Benjamin Lundy, answering a request for information about the history and operations of the Underground Railroad. Letter includes details of a story of an ex-slave transported on the Underground Railroad through Ohio and stories of the plight of other fugitive slaves crossing the Ohio River.
Benjamin Lundy (1789-1839) was a prominent Quaker abolitionist best known for his development of abolitionist periodicals. His "Genius of Universal Emancipation" was first published in 1821 from his home in Mt. Pleasant, Ohio, and enjoyed a wide circulation across the antebellum United States. In the 1820s, the young William Lloyd Garrison came to work for The Genius. Benjamin Lundy traveled widely seeking subscriptions to The Genius, giving talks about the anti-slavery movement, and observing and documenting the conditions of enslaved people across the Americas. He was also involved in the establishment of freed slave colonies in Mexico
Lamprospilus bicolor subsp. mirador Faynel & Prieto 2023, ssp. nov.
<i>Lamprospilus bicolor mirador</i> Faynel & Prieto, ssp. nov. <p>(Figures 11, 12, 32)</p> <p> <b>Type material.</b> Holotype male: PERU, Cuzco, Carretera Manu, Km 68, El Mirador, 1722 m, S13°04.108′, W71°33.229′, 1.VIII.2019, 14:00 (local time), C. Faynel leg., DNA sample ID CF-LYC-1022. The holotype will be deposited in MUSM.</p> <p> Paratypes (n = 35): <b>6 males</b>, RCCF: same locality as holotype, 31.VII.2019; <b>1 male</b>, RCCF: same locality as holotype, 31.VII.2019, 14:10, DNA sample ID CF-LYC-1020; <b>1 male</b>, RCCF:same locality as holotype, 5.VIII.2019; <b>3 males</b>, RCCF: same locality as holotype, 31.VII.2021; <b>6 males</b>, RCCF: same locality as holotype, 21.IX.2021; <b>3 males</b>, RCCF: same locality as holotype, 23.IX.2021; <b>1 male</b>, RCCP: same locality as holotype, 21.IX.2021; <b>2 males</b>, FILS: PERU, Puno, Sandia, 900 m, 21.VIII.2010, DNA sample ID CFC22432; same locality as holotype, 21.IX.2021; <b>2 males</b>, RCCF: BOLIVIA, La Paz, Caranavi, Taipiplaya, 994 m, 2.V.2019, S15°56′15.697″, W 67°28′4.292″, G. Siebel leg., DNA sample ID CF-LYC-1209 (will be deposited in CBF); La Paz, Caranavi, Antennes de Carrasco, 1660 m, 23.X.2020, S15°40.468′, W 67°29.364′, C. Faynel leg., DNA sample ID CF-LYC-1500; <b>2 females</b>, RCCF: ECUADOR, Tungurahua, Topo, Río Negro, 1300 m, 2011, J.C. Petit leg.; Morona-Santiago, Pablo Sexto, 1350 m, 9.I.2012, J.C. Petit leg.; <b>6 females</b>, RCCF: PERU, San Martín, Rioja, Naranjos, 15.VI.2020, DNA sample ID CF-LYC-1485; San Martín, Nuevo Cajamarca, 850 m, S5°56′, W77°19′, XI.2020, DNA sample ID CFLYC-1874; San Martín, Afluente, 1350 m, IV.2010; Huánuco, Flor de Café, 1450 m, S9°11′, W75°47′, 22.III.2021, DNA sample ID CF-LYC-1875; same locality as holotype, 8.VIII.2019, 13:10, DNA sample ID CF-LYC-1024; 23.IX.2021, 11:40, DNA sample ID CF-LYC-1647; <b>1 female</b>, RCCP: same locality as holotype, 15:30; <b>1 female</b>, FILS: PERU, Cuzco, Fundo Cadena, 900 m, -13.351, -70.841, 18.IX.2010.</p> <p> <b>Description.</b></p> <p> Male: Wings. Forewing average costal length measured from wing base to apex 14.8 mm (n = 22, min = 12.7 mm, max= 16.7 mm); same dorsal dull blue coloration and same ventral wing pattern as the nominal subspecies (Figures 9 and 11). The differences are 1) ventral coloration more grey than brown, 2) on forewing ventral surface the short median line at the end of the discal cell straight, not outwardly bent, 3) on hindwing ventral surface the postmedian line straight, not wavy, 3) a reduced orange spot on hindwing ventral surface veins CuA 1 -CuA 2 cell with the black inside broader (Figure 11).</p> <p>Male genitalia: Minor differences, for example brush organs less dense and dark compared with the nominal subspecies.</p> <p> Female: Wings. Forewing average costal length measured from wing base to apex 14.1 mm (n =5, min = 12.3 mm, max= 15.3 mm); same dorsal ground color light blue and same ventral wing pattern as in the nominal subspecies (Figures 10 and 12). The ventral wing surface pattern elements listed in the male description that separate <i>L. bicolor mirador</i> <b>ssp. nov.</b> from <i>L</i>. <i>bicolor bicolor</i> <b>sp. nov.</b> also apply to the female.</p> <p>Female genitalia: No differences with the genitalia of the nominal subspecies.</p> <p> <b>Etymology:</b> Named after the place known as El Mirador (“the viewpoint”) in the Cosñipata valley, where the first specimens were caught. A masculine noun in apposition.</p> <p> <b>Diagnosis:</b> The diagnostic characters are given in the male description. We found no other striking elements distinguishing this subspecies from the nominal subspecies described from Colombia (BIN: ACV4947) despite the high intersubspecific mean genetic distance was 4.01%. Moreover, the populations from Peru in the north (San Martín), center (Huánuco) and south (Cuzco), and northern Bolivia share the same barcode (BIN: ACP8506) with maximum divergence in BIN only 0.18% (p-dist). Based on previous data (Prieto <i>et al.</i> 2021), a distance of more than 4% often reveals a specific separation.</p> <p> <b>Distribution:</b> East slope of the Andean Cordillera, Yungas from Ecuador (Tungurahua and Morona-Santiago), to Peru (San Martín, Huánuco and Cuzco) and Northern Bolivia (La Paz). Altitudinal range 850–1720 m.</p> <p> <b>Remarks:</b> Males were commonly observed flying on a ridgetop, in the Cosñipata valley slopes, tree-topping around an isolated tree (2.5 m high) and landing in the middle of the tree (approximately at 1.5–2 m above the ground). They were active between 13:40 and 14:30 hours in August (eight observations) and between 14:40 and 16:30 hours in September (ten observations) with more sunny days. Females were found crossing male territories at 11:30, 13:10 and 15:30 hours. This species was recorded as “137 <i>Lamprospilus</i> <b>sp. n.</b> 1.” from the Cosñipata valley in February, August and November (Lamas <i>et al.</i>, 2021) between elevations 1050–1750 m and treated as an “uncommon species that resembles <i>L. coelicolor</i> and replaces it at higher elevations.”</p>Published as part of <i>Prieto, Carlos, Faynel, Christophe & Lorenc-Brudecka, Jadwiga, 2023, Integrative description of two new species and two new subspecies of Lamprospilus Geyer (Lepidoptera: Lycaenidae), pp. 145-159 in Zootaxa 5244 (2)</i> on pages 151-153, DOI: 10.11646/zootaxa.5244.2.3, <a href="http://zenodo.org/record/7656055">http://zenodo.org/record/7656055</a>
Turbulent wakes of plates with non-equilibrium similarity scalings
We have conducted hot wire anemometry measurements of six different axisymmetric turbulent wakes which demonstrate the existence in all these wakes of non-equilibrium mean flow profile scalings and of the underlying self-preservation and non-equilibrium dissipation scalings. These mean flow profile scalings are different from those of all documented canonical boundary-free turbulent shear flows to date, all of which have been established for very far downstream regions
Energy dissipation and flux laws for unsteady turbulence
Direct Numerical Simulations of spatially periodic unsteady turbulence show that the high Reynolds number scalings of the instantaneous energy dissipation rate and interscale energy flux at intermediate wavenumbers are qualitatively different from the well-known cornerstone scalings of equilibrium turbulence where and are time-dependent rms velocity and integral length-scales. Instead, they both scale as where and are length and velocity scales characterizing initial/overall unsteady turbulence conditions
- …
