cometadata/datacite-rtg-text-other-reclassification-records huggingface dataset:
Aspalathus
Creators: name: Stirton, C. H.
name: Muasya, A. M.
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Plantae
Tracheophyta
Magnoliopsida
Fabales
Fabaceae
Aspalathus

description: Key to Aspalathus of KwaZulu-Natal and Transkeian region of the Eastern Cape
To ease identification of Aspalathus we provide a key to the five species recorded in the KwaZulu-Natal Province as well as two others which partially overlap with them in the Eastern Cape Province.
1. Plants spiny or thorny; leaflets slightly flattened, grooved abaxially – A. spinifera
1*. Plants neither spiny nor thorny; leaflets acicular or sub-terete, not grooved abaxially – 2
2. Plants taller than 150 cm, erect; flowers 9–13 mm long, gathered in distinctive floral “pseudospikes” – 3
2*. Plants shorter than 150 cm, decumbent, spreading or ascending; flowers 4–8 (9) mm long, never gathered in distinctive floral “pseudospikes” – 4
3. Leaflets glabrous or glabrescent (rarely with scattered spreading hairs); keel blades densely pubescent – A. chortophila
3*. Leaflets covered with silvery-grey, appressed pubescence; keel blades glabrous – A. dahlgrenii
4. Plants 40–130 cm tall, erect, sparingly or moderately branched; densely leafy with leaf clusters crowded and overlapping on branches; several to numerous pale lemon yellow flowers gathered one per leaf cluster along seasonal shoots; calyx lobes linear, sericeous, as long as flowers, with narrow sinuses – A. gerrardii
4*. Plants 20–120 cm tall, spreading, rarely decumbent, closely branched; laxly leafy with leaf clusters distinctly separated along branches; 1 (2) light yellow or yellow flowers in a terminal leaf cluster on short lateral seasonal shoots or “umbellate”; calyx lobes narrowly triangular or subulate, glabrous, sub-glabrous or pubescent, much shorter than flowers, with broad sinuses – 5
5. Flowers dark yellow; calyx lobes long subulate, thickened, dark green; calyx tube pinkish, calyx teeth as long as tube; bracts and bracteoles linear – A. abbottii
5*. Flowers yellow or light lemon yellow; calyx lobes narrowly triangular or shortly subulate, not thickened, yellowish green or silvery; calyx tube green or pale green, shorter than tube, bracts and bracteoles subulate or linear-subulate – 6
6. Leaflets glabrous; flowers gathered into a terminal head-like umbels of up to 5 flowers or solitary on lateral short shoots or in combinations thereof, yellow; bracts and bracteoles unequal, bracteoles situated on lower parts of the calyx; calyx glabrous or subglabrous; standard acute, glabrous – A. simii
6*. Leaflets densely white or grey-puberulous or short tomentose; flowers solitary on lateral short shoots, one or few on each seasonal shoot, pale lemon yellow; bracts and bracteoles equal, bracteoles situated on upper part of pedicel; calyx densely pubescent; standard obtuse to retuse, densely tomentose or short-sericeous – A. frankenioides
description: Published as part of Stirton, C. H. & Muasya, A. M., 2016, Seven new species and notes on the genus Aspalathus (Crotalarieae, Fabaceae) *, pp. 35-46 in South African Journal of Botany 104 on page 36, DOI: 10.1016/j.sajb.2015.10.007, http://zenodo.org/record/10496237
Giustizia come equità e socialismo liberale
Creators: name: PASSONI, ANDREA
Publisher: name: Zenodo
Year: 2015
Subjects: Justice as fairness
Rawls
Coop
Capitalism
Social liberalism
Property-owning democracy
Socialismo liberale
Democrazia proprietaria
Giustizia come equità

description: Sebbene John Rawls sia uno dei filosofi più studiati e commentati del secolo scorso, alcuni aspetti del suo pensiero sono rimasti ai margini dell’attenzione accademica. È il caso, per esempio, della discussione rawlsiana in tema di “socialismo liberale”, regime che, insieme alla “democrazia proprietaria”, rappresenta per il filosofo americano quell’architettura istituzionale in grado di incarnare nel modo migliore lo spirito della sua giustizia come equità. Anche se questa mancanza può essere giustificata dallo scarso spazio riservato da Rawls stesso a tali questioni, un approfondimento in materia è fondamentale per dare pieno significato al concetto, tanto caro all’autore, di “utopia realistica”. Scopo di questo scritto è proprio quello di discutere l’idea rawlsiana di socialismo liberale: nello specifico, la tesi che cercherò di sostenere è che tale idea può essere riempita di significato – anche se certo non completamente – attraverso la promozione e lo sviluppo di un’economia di mercato di tipo cooperativo. In particolare, nella prima parte riassumerò brevemente alcuni tratti del pensiero rawlsiano. Dopo aver messo al centro dell’attenzione l’idea di socialismo liberale approfondirò le sue possibilità illustrando i tratti distintivi del modello cooperativo d’impresa. Successivamente confronterò tra loro un’economia di mercato di tipo cooperativo e un’economia di mercato di tipo capitalista, usando come metro di paragone i principi della giustizia come equità. Nell’ultima parte, infine, riprendendo le domande senza risposta poste da Rawls a proposito delle imprese gestite da lavoratori, affronterò alcune possibili obiezioni.
Polionemobius marblus Zhang & Shen & Tian & Liu & Li & He 2019, sp. nov.
Creators: name: Zhang, Ling
name: Shen, Chu-Ze
name: Tian, Di
name: Liu, Yun-Fei
name: Li, Kai
name: He, Zhu-Qing
Publisher: name: Zenodo
Year: 2019
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Orthoptera
Haglotettigoniidae
Polionemobius
Polionemobius marblus

description: Polionemobius marblus He sp. nov.
(Fig. 1 A–D, Fig. 2 A–C, Fig. 3 A&B)
Holotype: male, CHINA, Guangxi, Baise, Jingxi, Wuling, 19-iv-2019, coll. He Zhu-Qing.
Paratypes: 5 males & 6 females, same data as holotype.
Description. Male. Body small and pubescent. Head: as broad as pronotum, frontal rostrum two times as wide as 1st antennal article. Pronotum transverse, anterior margin as broad as posterior margin. Fore tibia with tympanum on outside surface; hind tibia with 3 external dorsal spurs and 4 internal dorsal spurs (the base one minute). Forewing not extending to apex of abdomen, one oblique vein, mirror small. Genitalia: epiphallus elongate, with a pair of inward middle lobes, which are shorter than lateral lobes as in Fig 2.
Female. Forewing short. Hind tibiae with three internal dorsal spurs. Ovipositor short and straight.
Coloration. Head brown with 7 longitudinal yellow stripes on vertex. 4th joint of maxillary palpus white, others black. Pronotum disk brown with black and yellow spots, lateral area black. Forewing yellow. Legs almost black with some small white spots, inner side of hind femur white with broken black stripe.
Etymology. marblus is used to describe its color pattern on legs.
Measurements (in mm). Male: body 6.18–6.27, pronotum length 1.38–1.50, forewing length 3.47–3.75, hind femur length 4.30–4.65; Female: body 5.05–5.86, pronotum length 1.55–1.69, forewing length 2.30–2.88, hind femur length 4.26–4.34, ovipositor length 2.10–2.35.
Distribution. China (Guangxi).
Song. Chirps continue 2.5– 7.1s with 0.56– 0.96s interval. Each chirp includes 18–33 pulses. Chirp rate is about 50 pulses/s (Fig. 3 A&B).
Remarks. This species prefers grasses. It is different with P. taprobanensis by in not having black spots on the forewing. This contrasts with P. annulicornis and also by the color of antenna, and differs from P. yunnanus in the body color.
description: Published as part of Zhang, Ling, Shen, Chu-Ze, Tian, Di, Liu, Yun-Fei, Li, Kai & He, Zhu-Qing, 2019, New and little-known crickets from Southern Guangxi, China (Orthoptera: Grylloidea: Gryllidae: Phalangopsidae; Trigonidiidae), pp. 544-550 in Zootaxa 4674 (5) on pages 546-548, DOI: 10.11646/zootaxa.4674.5.3, http://zenodo.org/record/3465076
Podocopida Sars 1866
Creators: name: Zaibi, Chahira
name: Scharf, Burkhard
name: Viehberg, Finn Andreas
name: Keyser, Dietmar
name: Kamoun, Fekri
Publisher: name: Zenodo
Year: 2013
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Ostracoda
Podocopida

description: Suborder Podocopina Sars, 1866
description: Published as part of Zaibi, Chahira, Scharf, Burkhard, Viehberg, Finn Andreas, Keyser, Dietmar & Kamoun, Fekri, 2013, Preliminary report on the living non-marine Ostracoda (Crustacea) from Tunisia with the description of a new Psychrodromus species, pp. 499-516 in Zootaxa 3626 (4) on page 502, DOI: 10.11646/zootaxa.3626.4.5, http://zenodo.org/record/223016
Ropalopus UNGARICUS UNGARICUS (HERBST 1784
Creators: name: Karpiński, Lech
name: Szczepański, Wojciech T.
name: Kruszelnicki, Lech
Publisher: name: Zenodo
Year: 2020
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Coleoptera
Cerambycidae
Ropalopus

description: ROPALOPUS UNGARICUS UNGARICUS (HERBST, 1784)
(FIGS 1A, J, 2A–D, 3F, G, 4A–D, 5E–G, 6A, B, P, Q, 7A, O, P, 8A, N, O, 9A, B, 10A, B, K, L, 11A–E, 12A–E, 13A–E, 14A, 16A, 17A–F; SUPPORTING INFORMATION, FIGS S1A, B, P, Q, S 2A, B, P, Q, S 3A, J, S 4A, 5A–C, P, Q, S 6A–C)
Callidium ungaricum Herbst in Fuesslins, 1784, Arch. Insectengesch. 5: 96.
Type material examined: Lectotype (herein designated) male with four labels: (1)? SYNTYPE, Callidium ungaricum Herbst, 1784 labelled by Museum für Naturkunde Berlin 2019 (red); (2) hungaricum Hbt × Banat.; (3) Hist.-Coll. (Coleoptera), Nr. 22087, Callidium hungaricum Fabr. Hungaria, Zool. Mus. Berlin; and (4) L E C T O T Y P E, Callidium ungaricum Herbst in Fuesslins, 1784, des., 2019 (red).
description: Published as part of Karpiński, Lech, Szczepański, Wojciech T. & Kruszelnicki, Lech, 2020, Revision of the Ropalopus ungaricus / insubricus group (Coleoptera: Cerambycidae: Callidiini) from the western Palaearctic region, pp. 1176-1216 in Zoological Journal of the Linnean Society 189 on page 1196, DOI: 10.1093/zoolinnean/zlz154, http://zenodo.org/record/5721563
Vorhisia vulpes Frizzell 1965
Creators: name: Stringer, Gary L.
name: Sloan, James Carson
Publisher: name: Zenodo
Year: 2023
Subjects: Biodiversity
Taxonomy
Animalia
Chordata
Siluriformes
Vorhisiidae
Vorhisia
Vorhisia vulpes

description: VORHISIA VULPES FRIZZELL, 1965b
FIG. 6D–H
Material— 1,537 specimens. Five specimens figured: DMNH 2021-09-12, DMNH 2021-09-13, DMNH 2021-09- 14, DMNH 2021-09-15, DMNH 2021-09- 16.
Description and Remarks— Vorhisia vulpes is one of most ubiquitous Late Cretaceous otoliths known in the USA and has been reported in the Fox Hills Formation (North Dakota), the Kemp Clay (Texas), the Ripley Formation (Mississippi), and the Severn Formation (Maryland) (Hoganson et al. 2019, Woodward 2003, Schwarzhans and Stringer 2020a, Stringer et al. 2020, and Huddleston and Savoie 1983). It has been classified primarily as an extinct siluriform, or perhaps an ariid, based on the large lapillus and similarities to extant ariid lapilli. One Arkadelphia Formation specimen was extremely large at 19.36 mm in length and 14.02 mm in height (Fig. 6H), which is rare, considering that it was recovered from a bore sample. Stringer et al. (2020) stated that Vorhisia probably represents an extinct family of the Siluriformes or Ostariophysi, but there is also the possibility that it could relate to an extinct higher taxonomic group or even a non-teleost fish as some extant Holostei have large lapilli.
To state that V. vulpes is the most common species in the upper Maastrichtian Arkadelphia Formation is an understatement. The total specimens in the Arkadelphia Formation assemblage is 2,109, and 1,537 of those (72.88%) are V. vulpes. The species is abundant in the Severn Formation (Huddleston and Savoie 1983), but noticeably less at 55%. Vorhisia vulpes is the most abundant species in the Kemp Clay, but its percentage is approximately 35% (Schwarzhans and Stringer 2020a). The percentage of V. vulpes in the Arkadelphia Formation certainly seems to indicate that the paleoenvironmental parameters were decidedly conducive for its growth and proliferation. Vorhisia vulpes has not been found in Europe although Cretaceous otoliths have been investigated in several areas (Nolf 2003, Schwarzhans 2010, Schwarzhans and Jagt 2021). Current studies indicate that the distribution of Vorhisia vulpes is limited to the USA. As noted by Schwarzhans and Stringer (2020a), V. vulpes was one of the most prominent and widespread teleostean species to succumb to the K-Pg extinction event in North America.
description: Published as part of Stringer, Gary L. & Sloan, James Carson, 2023, First Cretaceous teleostean otolith assemblage (Arkadelphia Formation, upper Maastrichtian) from Arkansas, USA, early Gadiformes, and the Western Interior Seaway, pp. 1-39 in PaleoBios 40 (1994) on page 12, DOI: 10.5070/P940361192., http://zenodo.org/record/10913416
Cypridocopina Jones 1901
Creators: name: Zaibi, Chahira
name: Scharf, Burkhard
name: Viehberg, Finn Andreas
name: Keyser, Dietmar
name: Kamoun, Fekri
Publisher: name: Zenodo
Year: 2013
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Ostracoda
Podocopida

description: Infraorder Cypridocopina Jones, 1901
description: Published as part of Zaibi, Chahira, Scharf, Burkhard, Viehberg, Finn Andreas, Keyser, Dietmar & Kamoun, Fekri, 2013, Preliminary report on the living non-marine Ostracoda (Crustacea) from Tunisia with the description of a new Psychrodromus species, pp. 499-516 in Zootaxa 3626 (4) on page 502, DOI: 10.11646/zootaxa.3626.4.5, http://zenodo.org/record/223016
Zeugomutilla recondita Cameron 1900
Creators: name: Lelej, Arkady S.
name: Williams, Kevin A.
name: Loktionov, Valery M.
name: Pang, Hong
name: Xu, Zai-Fu
Publisher: name: Zenodo
Year: 2017
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Hymenoptera
Mutillidae
Zeugomutilla
Zeugomutilla recondita

description: Zeugomutilla recondita (Cameron, 1900)
(Figs 28, 32, 35)
Mutilla recondita Cameron, 1900: 44, ♀, type locality: " Ceylon, Yerbury coll." (Sri Lanka, Trincomalee) [BMNH]; Turner 1911: 145, ♀; Nonveiller 1995: 33, 115, ♀ (Sri Lanka).
Zeugomutilla recondita: Lelej, 2005: 38, ♀ (Sri Lanka).
Diagnosis. Female. Body length 4.4–5.4 mm. Surface of pygidial plate in basal half with indefinite sculpture, apical half smooth and shining. Spots of golden setae on metasomal tergum 2 small, distance between them 1.3–1.5 × their diameter, if spots larger (Fig. 28) than distance between them 0.9 × their diameter; metasomal tergum 2 posteriorly with fringe of yellowish setae. Metasomal terga 3–4 with wide band of golden or yellowish setae, tergum 5 with black setae. Dorsoposterior propodeal border with median longer blunt tooth and four shorter ones from either side of this. Head and legs ferruginous to brown. Male. Unknown.
Material examined. Other material. Sri Lanka: Anuradhapura District: Padaviya, 20–23.vii.1978 (K. Krombein et al.), 1♀. Puttalam District, Panikka Villu in Wilpattu National Park, 22–23.i.1977 (K. Krombein et al.), 1♀. Trincomalee District: Trincomalee, 8–11.x.1977 (K. Krombein et al.), 1♀. Kandy District: Arupola, 27– 29.x.1972 (P. Karunaratne), 1♀; Udawattakele Sanctuary, 2100', 9–13.ii.1975 (K. Krombein et al.), 1♀; same place, 8–11.v.1975 (S. & P. Karunaratne), 1♀; same place, 5–15.vii.1976 (S. Karunaratne), 2♀; same place, 14– 16.x.1977 (K. Krombein et al.), 2♀; same place, 25–27.iv.1981 (K. Krombein et al.), 2♀. Kegalla District: Kitulgala, 25–26.x.1977, (K. Krombein et al.), 1♀; Kitulgala Makande, 3–4.ii.1979 (K. Krombein et al.), 1♀. Monaragala District, Angunakolapelessa, 21–23.i.1979 (K. Krombein et al.), 2♀; same place, 27–28.iii1981, (K. Krombein et al.), 5♀ [USNM].
Distribution. Sri Lanka (dry zone).
Remarks. The specimen from Kandy District: Udawattakele Sanctuary, 5–15.vii 1976, S. Karunaratne has additional label: " Pristomutilla recondita Cam. " (handwritten by B. Petersen). The head and legs vary in color from ferruginous to brown, but never have a discrete reddish spot contrasting with a dark brown head, as in Z. spinulosa.
description: Published as part of Lelej, Arkady S., Williams, Kevin A., Loktionov, Valery M., Pang, Hong & Xu, Zai-Fu, 2017, Review of the genus Zeugomutilla Chen, 1957 (Hymenoptera, Mutillidae, Mutillini), with description of two new species, pp. 1-15 in Zootaxa 4247 (1) on page 12, DOI: 10.11646/zootaxa.4247.1.1, http://zenodo.org/record/437934
Apateodus crenellatus ? Schwarzhans and Stringer 2020
Creators: name: Stringer, Gary L.
name: Sloan, James Carson
Publisher: name: Zenodo
Year: 2023
Subjects: Biodiversity
Taxonomy
Animalia
Chordata
Aulopiformes
Ichthyotringidae
Apateodus
Apateodus crenellatus

description: APATEODUS CRENELLATUS? SCHWARZHANS AND STRINGER,
2020b
FIG. 7A
Material— three specimens, specimen figured, DMNH 2021-09- 9.
Description and Remarks— The three Arkadelphia Formation specimens fit the description of Apateodus crenellatus presented in Stringer et al. (2020) from the Ripley Formation in northeastern Mississippi. Unfortunately, none of the thin, fragile specimens have a preserved rostrum like the holotype shown in Stringer et al. (2020, fig. 7 G–I). The outline of A. crenellatus appears to be more oval (sensu Smale et al. 1995), but if the long and moderately pointed rostrum is present, it is more ovate in outline (sensu Smale et al. 1995). The margins are variable, which may be related to erosion. The heterosulcoid sulcus appears to be more slightly ventral and extends across essentially the entire inner fac. The outer face is typically flat and smooth.
The classification of A. crenellatus has been debated for several decades since its initial discovery by Nolf and Dockery (1990) in the Coffee Sand (Campanian) of northeastern Mississippi. Its classification as an aulopiform was first suggested by Stringer et al. (2016) and Stringer et al. (2018). Its classification was confirmed when an otolith was discovered in situ by CT micro-scanning in A. corneti Forir (1887) by Schwarzhans et al. (2018a). This discovery and the subsequent revised taxonomy are also congruent with modern molecular-based phylogenetic and dating studies such as Near et al. (2012), Betancur-R. et al. (2013), Near et al. (2013), and Betancur-R et al. (2017).
description: Published as part of Stringer, Gary L. & Sloan, James Carson, 2023, First Cretaceous teleostean otolith assemblage (Arkadelphia Formation, upper Maastrichtian) from Arkansas, USA, early Gadiformes, and the Western Interior Seaway, pp. 1-39 in PaleoBios 40 (1994) on pages 12-14, DOI: 10.5070/P940361192., http://zenodo.org/record/10913416
Cyprididae Baird 1845
Creators: name: Zaibi, Chahira
name: Scharf, Burkhard
name: Viehberg, Finn Andreas
name: Keyser, Dietmar
name: Kamoun, Fekri
Publisher: name: Zenodo
Year: 2013
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Ostracoda
Podocopida
Cyprididae

description: Family Cyprididae Baird, 1845
description: Published as part of Zaibi, Chahira, Scharf, Burkhard, Viehberg, Finn Andreas, Keyser, Dietmar & Kamoun, Fekri, 2013, Preliminary report on the living non-marine Ostracoda (Crustacea) from Tunisia with the description of a new Psychrodromus species, pp. 499-516 in Zootaxa 3626 (4) on page 503, DOI: 10.11646/zootaxa.3626.4.5, http://zenodo.org/record/223016
Ropalopus UNGARICUS GALLICUS VARTANIS 2018
Creators: name: Karpiński, Lech
name: Szczepański, Wojciech T.
name: Kruszelnicki, Lech
Publisher: name: Zenodo
Year: 2020
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Coleoptera
Cerambycidae
Ropalopus

description: ROPALOPUS UNGARICUS GALLICUS VARTANIS, 2018
(FIGS 1B, C, K, 2E–G, 3H, 4E–G, 5H, 6C–E, R, 7B–D, Q, 8B, C, P, 9C, 10C, 11F–I, 12F–I, 13F–I, 14B, 16B, C; SUPPORTING INFORMATION, FIGS S1C–E, R, S 2C– E, R, S 3B, K, S 4B, S 5D, E, R, S 6D–F)
Distribution: South-eastern France (Fig. 20). This taxon was described from Aiguines, and several new localities in south-eastern France are herein added (Table 1). Most of these were incorrectly assigned to R. u. insubricus.
Diagnosis: Ropalopus u. gallicus is characterized by its relatively short elytra, the pronotum with its lustrous area predominantly slightly punctate and wrinkled (Fig. 2E), and the antennae, which are usually much shorter than the body in males. Moreover, the pubescence of the ventral side of the body is characteristic owing to the abundant long, whitish hairs (Fig. 16B), which is the best trait for distinguishing it from both of the closest taxa, R. u. ungaricus and R. u. insubricus (Fig. 16A and D, respectively). There are also clear differences in the shape of the lateral lobes (Fig. 12G), which are by far the shortest and widest in the discussed group. In contrast, the prosternal process (Fig. 9C) does not seem to differ from R. u. ungaricus (Fig. 9B). Body length: 17.0–20.0 mm.
Remarks: Despite its original classification as a subspecies of R. insubricus sensu e.g. Sama (2002) and Vartanis (2018), this taxon is evidently more closely related to R. u. ungaricus, but the elytra at the base are less frequently and less markedly wrinkled. The type locality of this taxon lies at medium elevation of ~ 1000 m a.s.l.; thus, although it overlaps, in part, with the range of elevations inhabited by R. u. ungaricus, it can be regarded as a transitional elevation between the latter and R. u. insubricus. The imagines were collected in the first days of July. This subspecies is indisputably associated ecologically with maple (Acer sp.) (Vartanis, 2018).
description: Published as part of Karpiński, Lech, Szczepański, Wojciech T. & Kruszelnicki, Lech, 2020, Revision of the Ropalopus ungaricus / insubricus group (Coleoptera: Cerambycidae: Callidiini) from the western Palaearctic region, pp. 1176-1216 in Zoological Journal of the Linnean Society 189 on page 1202, DOI: 10.1093/zoolinnean/zlz154, http://zenodo.org/record/5721563
Palaeogadus RATH 1859
Creators: name: Stringer, Gary L.
name: Sloan, James Carson
Publisher: name: Zenodo
Year: 2023
Subjects: Biodiversity
Taxonomy
Animalia
Chordata
Gadiformes
Merlucciidae
Palaeogadus

description: PALAEOGADUS CF. P. WELTONI SCHWARZHANS AND STRINGER,
2020a
FIG. 8A
Material— one small,slightly eroded specimen, DMNH 2021-09-23.
Description and Remarks— The one Arkadelphia Formation specimen assigned to Palaeogadus weltoni is very small and eroded. However, it was felt that it possessed enough gadid features to compare it to Palaeogadus cf. P. weltoni. Similarities include the overall oblong shape (sensu Smale et al. 1995), the slightly convex inner face; the tapered and rounded anterior and posterior margins that are almost alike; the homosulcoid-type sulcus; a broadly, gently arched dorsal margin; a very shallow ventral margin that approaches horizontal; and a prominent ventral furrow extending from under the anterior of the ostium to near the posterior of the cauda; the anterior and posterior ends of the ventral furrow appear to turn upwards. It compares very well to the one specimen of P. weltoni illustrated by Schwarzhans and Stringer (2020a) from the Kemp Clay in Texas and to the specimens shown by Stringer and Schwarzhans (2021) from the Severn Formation in Maryland. Palaeogadus is an extinct genus that is known from otoliths and skeletons from the early Paleogene of Europe (Schwarzhans 2003, fig. 20A–I).
description: Published as part of Stringer, Gary L. & Sloan, James Carson, 2023, First Cretaceous teleostean otolith assemblage (Arkadelphia Formation, upper Maastrichtian) from Arkansas, USA, early Gadiformes, and the Western Interior Seaway, pp. 1-39 in PaleoBios 40 (1994) on page 16, DOI: 10.5070/P940361192., http://zenodo.org/record/10913416
Zeugomutilla spinulosa Andre 1898, comb. nov.
Creators: name: Lelej, Arkady S.
name: Williams, Kevin A.
name: Loktionov, Valery M.
name: Pang, Hong
name: Xu, Zai-Fu
Publisher: name: Zenodo
Year: 2017
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Hymenoptera
Mutillidae
Zeugomutilla
Zeugomutilla spinulosa

description: Zeugomutilla spinulosa (André, 1898), comb. nov.
(Figs 29, 33)
Mutilla spinulosa André 1898: 26, ♀, type locality " Kurrachee [Pakistan, Karachi], Kanara [India, Karnataka], Poona [India, Maharashtra], Cochin [India, Kerala]" [MNHN]; Nonveiller 1995: 33, 115, ♀ (India).
Pristomutilla spinulosa: Lelej 2005: 36, ♀ (Pakistan, India: Maharashtra, Karnataka, Kerala).
Diagnosis. Female. Body length 5.5–7.2 mm. Dorsoposterior propodeal border with 8–12 strong teeth, median teeth longer. Surface of pygidial plate with indefinite sculpture in basal half, smooth and shining in apical half. Spots of whitish setae on metasomal tergum 2 small, distance between them 2.0 × their diameter and more. Metasomal terga 3–4 with median widened posterad large spot of whitish setae. Head brown with large reddishbrown spot on frons and vertex; legs brown. Male. Unknown.
Material examined. Other material. India: [Karnataka], 15 km N Bangalore, KT, 23–24.vii.1996, (K. Werner & L. Lorenz), 1♀ [MZUF]; [Tamil Nadu], Nedungadu P.O., Tanjore, Dt., 27.iv.1938 (P.S. Nathan & J. Lindemans), 2♀ [RMNH].
Distribution. India (Maharashtra, Karnataka, Kerala, Tamil Nadu), Pakistan (Karachi).
description: Published as part of Lelej, Arkady S., Williams, Kevin A., Loktionov, Valery M., Pang, Hong & Xu, Zai-Fu, 2017, Review of the genus Zeugomutilla Chen, 1957 (Hymenoptera, Mutillidae, Mutillini), with description of two new species, pp. 1-15 in Zootaxa 4247 (1) on page 13, DOI: 10.11646/zootaxa.4247.1.1, http://zenodo.org/record/437934
Biochemical and cellular insights into the Baz2B protein, a non-catalytic subunit of the chromatin remodeling complex
Creators: name: Breindl, Matthias
name: Spitzer, Dominika
name: Gerasimaitė, Rūta
name: Kairys, Visvaldas
name: Schubert, Thomas
name: Henfling, Ramona
name: Schwartz, Uwe
name: Lukinavičius, Gražvydas
name: Manelytė, Laura
Publisher: name: Universität Regensburg
Year: 2023
Subjects: subject: 570 Biowissenschaften, Biologie

description: Baz2B is a regulatory subunit of the ATP-dependent chromatin remodeling complexes BRF1 and BRF5, which control access to DNA during DNA-templated processes. Baz2B has been implicated in several diseases and also in unhealthy ageing, however limited information is available on the domains and cellular roles of Baz2B. To gain more insight into the Baz2B function, we biochemically characterized the TAM (Tip5/ARBP/MBD) domain with the auxiliary AT-hook motifs and the bromodomain (BRD). We observed alterations in histone code recognition in bromodomains carrying cancer-associated point mutations, suggesting their potential involvement in disease. Furthermore, the depletion of Baz2B in the Hap1 cell line resulted in altered cell morphology, reduced colony formation and perturbed transcriptional profiles. Despite that, super-resolution microscopy images revealed no changes in the overall chromatin structure in the absence of Baz2B. These findings provide insights into the biological function of Baz2B.
Tippaha mythica Schwarzhans and Stringer 2020
Creators: name: Stringer, Gary L.
name: Sloan, James Carson
Publisher: name: Zenodo
Year: 2023
Subjects: Biodiversity
Taxonomy
Animalia
Holocentriformes
Tippaha
Tippaha mythica

description: TIPPAHA MYTHICA SCHWARZHANS AND STRINGER, 2020a
FIG. 8C
Material— eight specimens including three complete well-preserved specimens, specimen figured, DMNH 2021-09- 25.
Description and Remarks—Tippaha mythica is certainly the most unique and impressive otolith in the Arkadelphia Formation assemblage based on its distinctive morphological characteristics. The basic outline is somewhat oblong to elliptic (sensu Smale et al. 1995), but there are numerous features that modify the shape. The convex inner face has a distinct and characteristic pseudobiostial sulcus that is primarily shallow except for a slightly deeper posterior portion of the cauda. An exceptional feature of the anterior portion of the cauda is the fading of its dorsal margin toward the moderately deep, well-marked, oval dorsal depression. There is no ventral furrow, but a long, obvious ventral depression is present under the sulcus. The most prominent feature is a long, fairly narrow predorsal projection that typically leans anteriorly at about 65– 750. The length of this conspicuous protuberance is often 25–30% of the length of the otolith. The outer face is usually irregular and nearly flat except for the massive predorsal protuberance.
Stringer et al. (2020) noted that T. mythica is probably the most distinct and remarkable otolith morphology presently known from the Cretaceous. In addition to the eight specimens from the Arkadelphia Formation, T. mythica is known from the Ripley Formation and the Owl Creek Formation, both Upper Cretaceous sites in northeastern Mississippi (Stringer et al. 2020) and the Providence Sand in Alabama, according to J. Ebersole, Director of Collections at McWane Science Center, Birmingham, Alabama (personal communication, 2020).
description: Published as part of Stringer, Gary L. & Sloan, James Carson, 2023, First Cretaceous teleostean otolith assemblage (Arkadelphia Formation, upper Maastrichtian) from Arkansas, USA, early Gadiformes, and the Western Interior Seaway, pp. 1-39 in PaleoBios 40 (1994) on pages 16-18, DOI: 10.5070/P940361192., http://zenodo.org/record/10913416
Eutawichthys maastrichtiensis
Creators: name: Stringer, Gary L.
name: Sloan, James Carson
Publisher: name: Zenodo
Year: 2023
Subjects: Biodiversity
Taxonomy
Animalia
Beryciformes
Eutawichthys
Eutawichthys maastrichtiensis

description: EUTAWICHTHYS MAASTRICHTIENSIS (NOLF AND STRINGER, 1996)
FIG. 8D
Material— 21 specimens, specimen figured, DMNH 2021-09- 26.
Description and Remarks— Eutawichthys maastrichtiensis has a nearly circular to slightly oval outline (sensu Smale et al. 1995). The dorsal margin is irregular, while the ventral margin can have crenulations that are often obliterated by erosion. The thin sagitta is only slightly convex with a distinctive, long sulcus (heterosulcoid type) that is wide and continuously curved. The cauda curves diagnostically dorsally in its posterior section. There is a depressed area that is fairly distinct above the center of the sulcus.
Eutawichthys maastrichtiensis was designated as an apogonid for many years, and there are certainly resemblances to the apogonids. Its designation as a berycid is discussed at length in Stringer et al. (2016) and is more congruent with molecular studies such as Betancur-R. et al. (2013) that indicate a much later divergence for the apogonids (around 45 Ma). The fossil-based genus Eutawichthys was erected by Schwarzhans et al. (2018b). Eutawichthys maastrichtiensis is known from several Cretaceous formations including the Severn Formation of Maryland (Huddleston and Savoie 1983), the Woodbury Formation of New Jersey (Stringer et al. 2016), the Eutaw Formation of Alabama (Schwarzhans et al. 2018a), the Tar Heel Formation of North Carolina (Stringer et al. 2018), the Coon Creek Formation of Tennessee (Stringer 2016b), the Ripley Formation of Mississippi (Stringer et al. 2020), and the Kemp Clay of Texas (Schwarzhans and Stringer 2020a).
description: Published as part of Stringer, Gary L. & Sloan, James Carson, 2023, First Cretaceous teleostean otolith assemblage (Arkadelphia Formation, upper Maastrichtian) from Arkansas, USA, early Gadiformes, and the Western Interior Seaway, pp. 1-39 in PaleoBios 40 (1994) on page 18, DOI: 10.5070/P940361192., http://zenodo.org/record/10913416
Amphicynodon Filhol 1881
Creators: name: WANG, XIAOMING
name: McKENNA, MALCOLM C.
name: DASHZEVEG, DEMBERELYIN
Publisher: name: Zenodo
Year: 2005
Subjects: Biodiversity
Taxonomy
Animalia
Chordata
Mammalia
Carnivora
Ursidae
Amphicynodon

description: Amphicynodon Filhol, 1881
COMMENT: Cirot and Bonis (1992) recently revised the taxonomy of the genus Amphicynodon and furnished a cladistic relationship for included species. However, their diagnosis of the genus is almost entirely based on primitive characters (Cirot and Bonis, 1992: 105): ‘‘arctoide primitive; crâne alongé et bas, bulle ossifiée, fosse supraméatale superficielle, canal de l’alisphénoide present,’’ which essentially describe the morphotypical condition for a basal arctoid but shed no light of whether or not the genus forms a natural clade. As such the concept of Amphicynodon remains a grade of small, primitive arctoids that are not easily placed in other genera of carnivorans of similar ages.
Ten species of Amphicynodon were recognized by Cirot and Bonis (1992; see Baskin and Tedford, 1996, for a possible North American species). With the exception of A. teilhardi and A. mongoliensis (see below), all are from Europe and most are produced from the classic Quercy fissure fills. As defined by Cirot and Bonis, their concept of Amphicynodon offers a measure of morphological consistency, despite primitive status of most of their features. The limited scope of their phylogenetic analysis (within the genus), however, does not permit a sense of overall relationships among basal arctoids, nor does it address the question of to what extent the genus might be paraphyletic, given that certain derived forms (such as Pachycynodon and Cephalogale) may have arisen from within the genus. Such questions are difficult to address because most of the species of Amphicynodon are still represented by fragmentary jaws and teeth only. A comprehensive analysis of basal arctoids at the species level is not feasible. Our Mongolian materials, though significantly improved over those available for previous studies, are still not as complete as their European counterparts.
description: Published as part of WANG, XIAOMING, McKENNA, MALCOLM C. & DASHZEVEG, DEMBERELYIN, 2005, Amphicticeps and Amphicynodon (Arctoidea, Carnivora) from Hsanda Gol Formation, Central Mongolia and Phylogeny of Basal Arctoids with Comments on Zoogeography, pp. 1-58 in American Museum Novitates 3483 on pages 27-28, DOI: 10.1206/0003-0082(2005)483[0001:AAAACF]2.0.CO;2, http://zenodo.org/record/4735171
Eutawichthys zideki
Creators: name: Stringer, Gary L.
name: Sloan, James Carson
Publisher: name: Zenodo
Year: 2023
Subjects: Biodiversity
Taxonomy
Animalia
Beryciformes
Eutawichthys
Eutawichthys zideki

description: EUTAWICHTHYS ZIDEKI (NOLF AND STRINGER, 1996)
FIG. 8E
Material— 287 specimens, specimen figured, DMNH 2021-09- 27.
Description and Remarks— Eutawichthys zideki is the most abundant species of this genus in the Arkadelphia Formation. It is characterized by an oval outline (sensu Smale et al. 1995), but larger specimens can become somewhat angular. Although the sulcus (heterosulcoid type) is not deeply impressed, it is distinct and extends for approximately 75% of the length of the inner face. The sulcus is almost horizontal, which is a distinguishing feature of the species. The ostium and cauda are approximately the same length, and the ostium is only slightly wider than the cauda. Eutawichthys zideki is geographically widespread in its distribution and has been reported from the Severn Formation of Maryland (Huddleston and Savoie 1983), the Woodbury Formation of New Jersey (Stringer et al. 2016), the Tar Heel Formation of North Carolina (Stringer et al. 2018), the Coon Creek Formation of Tennessee (Stringer 2016b), the Eutaw Formation of Alabama (Schwarzhans et al. 2018b), and the Ripley Formation of Mississippi (Stringer et al. 2020).
description: Published as part of Stringer, Gary L. & Sloan, James Carson, 2023, First Cretaceous teleostean otolith assemblage (Arkadelphia Formation, upper Maastrichtian) from Arkansas, USA, early Gadiformes, and the Western Interior Seaway, pp. 1-39 in PaleoBios 40 (1994) on page 18, DOI: 10.5070/P940361192., http://zenodo.org/record/10913416
Charged Particle Dynamics in Jovian Magnetosphere
Creators: name: Srivastava, Ayushi
name: Kakad, Bharati
name: Kakad, Amar
Publisher: name: Zenodo
Year: 2024
Subjects: Jupiter's Magnetosphere, Test Particle Simulation

description: Jupiter has the largest magnetosphere in our solar system, having a magnetic field ~20 times stronger than Earth. It hosts the strongest radiation belts. These belts derive their energy from the accumulation of high-energy charged particles, encompassing protons (~100 GeV), electrons (~ 100 MeV), and heavy ions like 𝑂+, 𝑂++, 𝑆+, 𝑆++, 𝑆+++ (~100 MeV) [1]. The origin of these particles can be attributed to the combined effects of solar wind and Io (one of Jupiter's moons), loading roughly 1000 kg of fresh material into Jupiter's magnetosphere every second. Predicting the trajectories of charged particles within Jupiter's magnetic field is crucial for ensuring space mission safety, protecting electronic equipment, and advancing our understanding of particle dynamics. Various theoretical models have been developed to predict particle trajectories, all of which are based on the gyro-center approximation [2]. This approximation neglects gyro motion and instead tracks the gyro center, assuming that particles gyrate near the magnetic field line. However, this approximation fails for highly energetic charged particles due to their larger gyroradius. Therefore, a three-dimensional relativistic model has been developed including all particle motions i.e. gyro, bounce, and drift by incorporating Jupiter's magnetic field (intrinsic + current source) to study their behavior thoroughly.
Psychrodromus
Creators: name: Zaibi, Chahira
name: Scharf, Burkhard
name: Viehberg, Finn Andreas
name: Keyser, Dietmar
name: Kamoun, Fekri
Publisher: name: Zenodo
Year: 2013
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Ostracoda
Podocopida
Cyprididae
Psychrodromus

description: Key to the species of the genus Psychrodromus (after Karanovic 2012, modified)
1. Length of the carapace at most 1.4 mm .................................................................... 2
- Length of carapace more than 1.6 mm ..................................................................... 6
2. Posterior seta/claw on the UR with a filamentous tip...................................... P. fontinalis (Wolf, 1920)
- Posterior seta/claw on the UR without a filamentous tip....................................................... 3
3. Posterior claw of the UR at the most ½ as long as anterior claw.......................... P. turcicus (Hartmann, 1964)
- Posterior claw of the UR longer than ½ of the anterior claw.................................................... 4
4. Dorsal margin of the carapace only slightly arched, carapace elongated, male clasping organ of maxilliped beside the 2 bristles one respectively two truncated setae......................................................... P. tunisicus n. sp.
- Dorsal margin of the carapace distinctly arched, not elongated, male clasping organ without truncated setae............. 5
5. Posterior margin of the carapace broadly rounded, posterior seta/claw on the UR very broad and very slightly narrowing from the basis to the tip....................................................... P. o l iv a c e u s (Brady & Norman, 1889)
- Posterior margin of the carapace slightly inclined, posterior seta/claw on the UR very narrow distally...................................................................................... P. betharrami Danielopol & Baltanás, 1993
6. Dorsal margin highly arched, greatest H in the middle from which point margin slopes equally towards anterior and posterior ends...................................................................... P. peristericus (Petkovski, 1959)
- Dorsal margin less arched, greatest H situated around the middle from which point margin inclined towards anterior end and more rounded towards posterior end........................................ P. robertsoni (Brady & Norman, 1889)
description: Published as part of Zaibi, Chahira, Scharf, Burkhard, Viehberg, Finn Andreas, Keyser, Dietmar & Kamoun, Fekri, 2013, Preliminary report on the living non-marine Ostracoda (Crustacea) from Tunisia with the description of a new Psychrodromus species, pp. 499-516 in Zootaxa 3626 (4) on page 507, DOI: 10.11646/zootaxa.3626.4.5, http://zenodo.org/record/223016
Lagriinae Latreille 1825
Creators: name: Nabozhenko, Maxim V.
name: Bukejs, Andris
name: Telnov, Dmitry
Publisher: name: Zenodo
Year: 2019
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Coleoptera
Tenebrionidae

description: Subfamily Lagriinae Latreille, 1825
Tribe Gonialaenini trib. nov.
Type genus: Gonialaena gen. nov., herewith designated
Diagnosis. Corresponds with the diagnosis of the type genus.
description: Published as part of Nabozhenko, Maxim V., Bukejs, Andris & Telnov, Dmitry, 2019, Gonialaenini, a new tribe of Lagriinae (Coleoptera: Tenebrionidae) from Eocene Baltic Amber, pp. 253-260 in Zootaxa 4565 (2) on page 254, DOI: 10.11646/zootaxa.4565.2.9, http://zenodo.org/record/2589961
Eutawichthys stringeri STRINGERI 2018
Creators: name: Stringer, Gary L.
name: Sloan, James Carson
Publisher: name: Zenodo
Year: 2023
Subjects: Biodiversity
Taxonomy
Animalia
Beryciformes
Eutawichthys

description: EUTAWICHTHYS CF. E. STRINGERI
FIG. 8F
Material— 48 specimens, specimen figured, DMNH 2021-09- 28.
Description and Remarks— The specimens assigned to Eutawichthys stringeri are characterized by an anterior margin with a broad, dorsally shifted rostrum, a broadly rounded dorsal margin, a broadly rounded posterior margin, and a moderately deep, gently and regularly curved convex ventral margin. The inner face is slightly convex with a shallow, moderately wide sulcus divided into an ostium and cauda. The ostium is curved upwards towards the dorsal margin of the rostrum. The cauda is about the same length as the ostium and is oriented upwards. The cauda has a rounded tip that ends well before the posterior margin.
Excellent figures of the ontogeny of E. stringeri are found in Schwarzhans et al. (2018b) and readily illustrate the differences between it and other species of Eutawichthys. The distribution of E. stringeri is not nearly as widespread as E. maastrichtiensis and E. zideki. It has only been previously reported from the Woodbury Formation (early–middle Campanian) of New Jersey (Stringer et al. 2016) and the Eutaw Formation (upper Santonian) of Alabama (Schwarzhans et al. 2018b), where it represents the most abundant species.
description: Published as part of Stringer, Gary L. & Sloan, James Carson, 2023, First Cretaceous teleostean otolith assemblage (Arkadelphia Formation, upper Maastrichtian) from Arkansas, USA, early Gadiformes, and the Western Interior Seaway, pp. 1-39 in PaleoBios 40 (1994) on pages 18-19, DOI: 10.5070/P940361192., http://zenodo.org/record/10913416
Emertonia andeep
Creators: name: Mathiske, Annabel
name: Thistle, David
name: Gheerardyn, Hendrik
name: Veit-Köhler, Gritta
Publisher: name: Zenodo
Year: 2021
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Hexanauplia
Harpacticoida
Paramesochridae
Emertonia
Emertonia andeep

description: Key to species of the Emertonia andeep -group
1. Outer spines of exp P2–P4 strongly serrated................................................................2.
- Outer spines at exp P2–P4 not distinctly serrated............................................................5.
2. P5 exp clearly separated from benp.......................................................................3.
- P5 exp fused with benp (only female known)................................................. E. berndi sp. nov.
3. Caudal ramus seta III almost twice as long as seta IV.........................................................4.
- Caudal ramus seta III shorter than seta IV.................................................... E. hessleri sp. nov.
4. Caudal ramus setae III and V with clearly visible internal structure, seta III naked....................... E. ilse sp. nov.
- Caudal ramus setae III and V without clearly visible internal structure, seta III unipinnate.............. E. serrata sp. nov.
5. Anal somite laterally with strong, chitinous, dorsally flexed appendages (distinct hook-like structures).............................................................................................. E. andeep (Veit-Köhler, 2004).
- Anal somite without such structures............ E. minor (Vasconcelos, Veit-Köhler, Drewes & Parreira dos Santos, 2009).
description: Published as part of Mathiske, Annabel, Thistle, David, Gheerardyn, Hendrik & Veit-Köhler, Gritta, 2021, Deep sea without limits-four new closely related species of Emertonia Wilson 1932 (Copepoda: Harpacticoida: Paramesochridae) show characters with a worldwide distribution, pp. 443-486 in Zootaxa 5051 (1) on page 478, DOI: 10.11646/zootaxa.5051.1.18, http://zenodo.org/record/5563861
Gonialaena Nabozhenko & Bukejs & Telnov 2019, gen. nov.
Creators: name: Nabozhenko, Maxim V.
name: Bukejs, Andris
name: Telnov, Dmitry
Publisher: name: Zenodo
Year: 2019
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Coleoptera
Tenebrionidae
Gonialaena

description: Gonialaena gen. nov.
Type species: Gonialaena groehni sp. nov., herewith designated
Diagnosis. Body slender, covered with long erect and shorter suberect setae dorsally and subdecumbent ones ventrally, legs and antennae long and slender. Eyes large, transverse, elongate-oval. Apical maxillary palpomere subcylindrical. Antennae long, about 3 terminal antennomeres extend beyond base of pronotum; antennomere 1 large and wide, 1.9× as wide as antennomere 2, antennomere 11 ovoid with tapered apex, subequal in size to antennomere 10. Pronotum nearly circular with lateral margins weakly and widely emarginate in basal half; anterior margin widely rounded. Anterior angles obsolete, vaguely expressed; posterior angles distinct, orthogonal. Lateral and anterior margins of pronotum not beaded. Prosternum in front of procoxae distinctly longer than the shortest diameter of one procoxal cavity. Elytra with rounded humeral angles and with 10 moderately deep striae of circular punctures, not merged. Interstriae covered with two kinds of setae: longer erect and shorter suberect ones. Epipleura reaching sutural elytral angle, very wide basally, becoming narrow apically. Metathoracic wings not present. Intercoxal process of abdominal ventrite 1 narrowly rounded apically. Narrow intersegmental membranes are present between 3–5 abdominal ventrites. Legs with long sparse erect setae and shorter denser subrecumbent hairs. Penultimate tarsomere not bilobed, insertion of terminal tarsomere central with regard the slightly cupuliform penultimate tarsomere (as in many Lagriinae; see Matthews & Bouchard (2008)).
Etymology. The name derives from the genera Goniadera Perty, 1832 and Laena Dejean, 1821 (Latin). Gender feminine.
Included species. The new genus at present only includes the type species.
description: Published as part of Nabozhenko, Maxim V., Bukejs, Andris & Telnov, Dmitry, 2019, Gonialaenini, a new tribe of Lagriinae (Coleoptera: Tenebrionidae) from Eocene Baltic Amber, pp. 253-260 in Zootaxa 4565 (2) on page 254, DOI: 10.11646/zootaxa.4565.2.9, http://zenodo.org/record/2589961