122,723 research outputs found
The Lambe-Lambe theater as a methodology for teaching theatrical language in basic education in the city of Manaus
No full textThis Course Completion Work is a report developed from artistic-pedagogical experiences in the Supervised Curricular Internships with children from Kindergarten, Elementary School and High School students. My goal is to observe the potential of Lambe-Lambe Theater as a methodology of theatrical language in basic education. Thus, I bring reports, results, challenges and problems faced during this process, contributing to the development of internships and studies about the popularization of the Lambe-Lambe Theater. I show my most vulnerable side, in which my worst nightmare becomes one of my greatest desires and dreams: the actor going to meet a classroom, experiencing all the challenges and learnings that teaching has to teach.Este Trabalho de Conclusão de Curso é um relato desenvolvido a partir de experiências artístico-pedagógicas nos Estágios Curriculares Supervisionados com crianças do Ensino Infantil, do Ensino Fundamental e estudantes do Ensino Médio. Tenho como objetivo observar a potencialidade do Teatro Lambe-Lambe como metodologia da linguagem teatral na educação básica. Assim, trago relatos, resultados, desafios e problemas enfrentados no decorrer desse processo, contribuindo para o desenvolvimento de estágios e estudos acerca da popularização do Teatro Lambe-Lambe. Mostro o meu lado mais vulnerável, na qual, o meu pior pesadelo se torna uns dos meus maiores desejos e sonhos: o ator indo ao encontro de uma sala de aula, vivenciando todos os desafios e aprendizados que a docência tem a ensinar
Afiks pada Caption Akun Lambe Turah di Instagram
Full text linkABSTRAK
Deola Indriana Sukmawijaya. 2021. “Afiks pada Caption Akun Lambe Turah di Instagram”. Skripsi Jurusan Sastra Indonesia. Fakultas Ilmu Budaya. Universitas Andalas, Padang. Pembimbing I, Prof. Dr. Nadra, M.S., dan pembimbing II, Dra. Sri Wahyuni, M.Ed.
Masalah yang dibahas dalam penelitian ini adalah: 1) Apa saja jenis afiks yang terdapat pada caption akun Lambe Turah di instagram? dan 2) Bagaimana proses pembentukan kata menggunakan afiks dan makna afiks yang terdapat pada caption akun Lambe Turah di instagram?. Tujuan penelitian ini adalah: 1) Mendeskripsikan jenis afiks yang terdapat pada caption akun Lambe Turah di instagram dan 2) Menjelaskan proses pembentukan kata menggunakan afiks dan makna afiks yang terdapat pada caption akun Lambe Turah di instagram.
Pada tahap penyediaan data, digunakan metode simak dengan teknik dasar berupa teknik sadap dan teknik lanjutannya berupa teknik catat dan teknik Simak Bebas Libat Cakap (SBLC). Pada tahap analisis data, digunakan metode agih dengan teknik dasar berupa teknik Bagi Unsur Langsung (BUL) dan teknik lanjutan berupa teknik ganti dan teknik perluas. Pada tahap penyajian analisis data, digunakan metode penyajian data secara formal dan informal.
Berdasarkan hasil analisis data, jenis afiks yang terdapat pada caption akun Lambe Turah di instagram terdiri atas prefiks, sufiks, simulfiks, konfiks, dan kombinasi afiks. Prefiks yang ditemukan pada caption akun Lambe Turah adalah {meN-}, {ter-}, {ber-}, {se-}, {ke-}, dan {peN-}. Kemudian, sufiks yang ditemukan adalah {-an}, {-in}, {-i}, {-wati}, dan {-wan}. Simulfiks yang ditemukan adalah {N-}. Konfiks yang ditemukan adalah {ke-an}, {ber-an}, {per-an}, {peN-an}, {per-in}, {peN-in}, dan {di-kan}. Selanjutnya, kombinasi afiks yang ditemukan adalah {N-in}, {keter-an}, {ter-kan}, {ber-kan}, {diber-kan}, {di-in}, {di-i}, {peN-an}, {meN-i}, dan {meN-kan}. Dari 29 jenis afiks yang ditemukan, 22 diantaranya merupakan jenis afiks yang sama dengan teori Kridalaksana dan 7 jenis afiks lainnya baru ditemukan pada caption akun Lambe Turah di instagram.
Proses pembentukan kata mengunakan afiks yang terdapat pada caption akun Lambe Turah di instagram, yaitu proses pemunculan fonem, proses pengekalan fonem, proses pelesapan fonem, dan proses peluluhan fonem. Selain itu, ditemukan beberapa data pada proses pembentukan kata menggunakan afiks yang berbeda dengan teori Kridalakasana, seperti mempesona, terraba, bepartisipasi, perresmian, mensukseskan, mengkirimkan, memrioritaskan, penkeepan, ngicipin, dan mempacari. Selanjutnya, makna yang terdapat pada caption akun Lambe Turah di instagram adalah makna gramatikal.
Kata kunci: afiks, caption, instagram, Lambe Turah, jenis, proses, makn
PLATE XV. Fig. 1 in New genera and species from the Belly River Series (mid-Cretaceous)
No full textPLATE XV. Fig. 1. Ornithomimus altus, Lambe, caudal vertebra, superior view, natural size. Page 52. Fig. 2. View of right side of same. Fig. 3. Ornithomimus altus, caudal vertebra, superior view natural size. Page 52. Fig. LL. The same, inferior view. Fig. 5. The same, right side. Fig (S. Ornithomimus altus, left sidc of lumhar vertebra of small individual natural size. Fig. 7. The same, superior view. Fig. S. The same, anterior view. Fig. Ü. Terminal phalanx of megalosauroid dinosaur, lateral view; natural size. Fig. 10. The same, proximal view. z, prezygapophysis i, postzygapoplıysis; s, neural spine e, transverse process. Fig, ll. Tooth of Deinorloıı cnrplanatus', Cope, side view; four times the natural size. Page 45). Fig. 12. Transverse section of the same. Fig. 13. Ptilodus primaevus, Lambe, right man libular rztmus,c.\' ternal view; enlarged four times. Page 79. Fig. 1 -1. The same, internal view. pflf, fourtli prernolar; mf, first molar i, socket for incisor; n, socket for second molar. Fig. 15. Boreodon matutinus, Lambe, premolar. side view, four times natural size. Page TQ c, cingulum. Fig. 16. Right maxillary bone, (provisionally associated with Scapherpelnu tectmn), external view, four times thc natural size. Fig. ii. Inferior' view of the samc, similarly cnlargcd. Page 32. Fig. is. Prcınaxillary bone of Diphyodus longirostris, Lambe, inferior view; enlarged four times. Page 30. Fig. 19. Transverse section of samc, similarly enlarged. t, tooth-base m, interspace.Published as part of Lambe L. M., 1902, Geological Survey of Canada Contributions to Canadian Palaeontology 3 on pages 25-81, DOI: 10.5281/zenodo.323376
Stereocephalus tutus Lambe 1902
No full textStereocephalus tutus. Sp. nov. Plate XI, plate XII, figs. 1, 2, 3, 4 and 5, and plate XXI, figs. 6, 7 and 8. The speeimen of Which views from above, from the side and from below are given on plates XI and XII, represents part of the plate-protected cranium of a herbivorous dinosaur, that is, apparently, quite distinct from any hitherto described. With the head was found a transverse series of coössified sharply keeled scutes which will be described farther on. The part of the head preserved is strongly convex transversely, but only moderately so from front to back. Goôssified plates cover the whole of the upper surface and are continued down on the vertical sides. They are arranged with a certain amount of bilateral symmetry, are quite small at the centre and toward the back, but are larger in front and very much more so on the sides. They are for the most part irregularly five or six sided, with rather undulatory surfaces that are marked by an irregular, raised, structural cross-hatching, feebly suggestive of the surface markings of the plates of Nodosaurus textilis, Marsh. Small vascular openings and grooves are also numerous on the surface. The edges of the plates are as a rule angular and sometimes raised. Each plate has its limit defined by a deep circumscribing furrow, so that although they are coôssified and form a continuous surface covering to the head, they do not lose their individuality. A rounded node, or an incipient keel is noticed on some of the plates. The removal of sandstone from the lower surface of the specimen revealed the bones of the palatal region (plate XII. fig. 2). The interpretation of these elements are as indicated by the letters. The back ends, only, of the palatines (P) are seen, meeting the pterygoids in a suture indicated at “ s. From here the latter bones (pt.) extend backward on either side of interpterygoid vacuities (v.). The ridge (pb.) represents the presphenoid and basisphenoid elements; it is bent posteriorly to one side in the specimen, which has been subjected to considerable pressure from above and is somewhat crushed behind. From this intel'pretation of the bones of the palate it would appear that the part of the armature preserved covers the upper part of the head near the union of the nasals With the frontals. No indication of the 01'bits can be detected and it is probable that they were placed far forward in the head. Part of a rib, having a T-shaped transverse section (Plate XII, fig. 5), such as is characteristic of the heavily armoured Slegosauría, was found separately but in the same locality, and is provisionally associated with S. tutus. The finding of such a rib is sufficient evidence of itself to prove the existence, during the time of the deposition ofthe Belly River series, of a large dinosaur having a heavy protective covering of bony plates [table omitted] With the 11ead,just described, Were five keeled, bony scutes or plates that have since been found to fit together in the form of an arch (plate XII, figs. 3 and 4), Whose sides curve forward as well as (lownward. This oblique curve places the lower, paired scutes, as seen when the arch is viewed from above, a little in advance of the upper pair which is again slightly in advance of the median plate The scutes rest on and are ossified to a thickness of bone that constitutes the inner, continuous surface of the arch. This band of bone, ornamented above by paired ossicles, suggests the possibility of its being the back border of the posterior crest of the species to which the head armature, above mentioned, belonged. This suggestion is given credence from the fact that the concave edge of the band of bone on which the scutes rest is fractured, whilst the convex edge appears to be intact. Numbering the ossicles from the right, the junction between Nos. 1 and 2 was perfect, as were also those between Nos. 3, 4 and 5, but iii the case of Nos. 2 and 3 the fractured edges did not fit with sufiicient exactness to remove all doubt as to their being placed side by side, although the continuity and symmetry of the curve of the under surface seemed complete. It is possible that one or two scutes are missing froın between Nos. 2 and 3, especially as fragments of similarly shaped scutes were found at the same spot. If an additional soute completed the series it probably would have been the mate of the present median one, or if two were required to fill the gap (if such a gap exists) one would be on the median line, the other would correspond with No. 3 to form another pair. The addition of one or two scutes to the series would result only in extending and possibly flattening the curve. The median sente is apparently symmetrical, the others are asymmetrical, forming pairs with reversed lateral proportions. The scutes have an irregularly oval basal outline, are sharply keeled, with sloping sides shallowly excavated from the keel downward but convexly curved from front to back, their basal edges are defined by an engirdling furrow below which, at a lower level, they are laterally expanded to meet each other in a plane surface. A very small ossicle rises above this intermediate basal surface between Nos. 3 and 4. Vascular markings are conspicuous on the sides of the scutes. From the appearance of the outer, basal edges of scutes Nos. 1 and 5, it seems probable that these scutes constituted the lateral terminations of the series. [table omitted] Belly River series, Red Deer river, 1897. The tooth shown in fig. 12, is of the Stegosaurían type. It differs from those, of the Red Deer river district, referred to the two species of Palœoscincus, and is about twice as large as those of P. costatus. 1 t is figured here with the idea that it may eventually prove to belong to S. tutus. It was collected below Berry creek, on Red Deer river, in 1901. A spinous dermal plate of massive proportions, fig. 13, A and B, is referred to this species on account of its similarity, in structure and surface markings, to the postcranial keeled scutes described above. This specimen was collected in 1897. Another large plate similar in general proportions to the above and nearly as large, as Well as numerous others of different sizes and of a variety of shapes, were collected in 1901.Published as part of Lambe L. M., 1902, New genera and species from the Belly River Series (mid-Cretaceous), pp. 25-81 in Geological Survey of Canada Contributions to Canadian Palaeontology 3 on pages 55-57, DOI: 10.5281/zenodo.323376
EXPLANATION OF PLATE I Left lateral aspect of skull of Stephanosaurus marginatus; one- fifth the natural size. Abbreviations.-D, lateral temporal fossa; DN, dentary; J, jugal; L, lachrymal; MX, maxilla; N, nasal; NO, nasal opening; OR, orbit; PD, predentary; PF, prefrontal; PM, premaxilla; Q, quadrate; QJ, quadrato-jugal; S, squamosal; SA, surangular. in On a new genus and species of carnivorous dinosaur from the Belly River Formation of Alberta, with a description of the skull of Stephanosaurus marginatus from the same horizon
No full textEXPLANATION OF PLATE I Left lateral aspect of skull of Stephanosaurus marginatus; one- fifth the natural size. Abbreviations.-D, lateral temporal fossa; DN, dentary; J, jugal; L, lachrymal; MX, maxilla; N, nasal; NO, nasal opening; OR, orbit; PD, predentary; PF, prefrontal; PM, premaxilla; Q, quadrate; QJ, quadrato-jugal; S, squamosal; SA, surangular.Published as part of Lambe, LM, 1914, On a new genus and species of carnivorous dinosaur from the Belly River Formation of Alberta, with a description of the skull of Stephanosaurus marginatus from the same horizon, pp. 13-21 in The Ottawa Naturalist 28 on page 20, DOI: 10.5281/zenodo.337109
O FOTÓGRAFO NO JARDIM DO CIDADÃO: MEMÓRIA DE UM LAMBE-LAMBE
Full text link This article proposes possible inflections for the senses that photographs made of the city and in the city acquire with the passing of time and it relates some of these inflections with the permanence of personages whose function and activity do not justify anymore in the universe of contemporary photographic making. The reflection is established on the trajectory of the „lambe-lambe‟ Edgar Borges that has been working as a photographer for almost forty years at Coronel Pedro Osório Square in the city of Pelotas, Rio Grande do Sul. The Edgar's work is emphasized as a popular craft, a street work, besides standing out the techniques and the photographic language used by the photographer throughout his trajectory. It is observed, as an aspect of the same importance the presence of the wooden ponies as a scenic element used by the photographer to cdefine his work in the interior of the square. Finally, such inflections contribute for discussions about photography and memory. O artigo propõe possíveis inflexões para os sentidos que fotografias da cidade e feitas na cidade adquirem com o passar do tempo e relaciona algumas dessas inflexões com a permanência de personagens cuja função e atividade exercida já não se justificam no universo do fazer fotográfico contemporâneo. A reflexão estabelece-se sobre a trajetória de quase quarenta anos do retratista lambe-lambe Edgar Borges que até hoje atua na Praça Coronel Pedro Osório na cidade de Pelotas, Rio Grande do Sul. Enfatiza-se o trabalho de Edgar como um ofício popular, de rua, além de ressaltar as técnicas e a linguagem fotográfica utilizada pelo retratista ao longo de sua trajetória. Observa-se, como aspecto de igual importância a presença dos cavalinhos de madeira enquanto elemento cênico utilizado pelo fotógrafo, para definir o seu trabalho no interior da praça. Por fim, tais inflexões contribuem para as discussões sobre fotografia e memória
Une initiation à la connaissance du climat britannique. The English Climate, de H. Lambe
No full textGodard Alain. Une initiation à la connaissance du climat britannique. The English Climate, de H. Lambe. In: Annales de Géographie, t. 77, n°419, 1968. pp. 100-101
Fig. 7 in New genera and species from the Belly River Series (mid-Cretaceous)
No full textFig. 7. Part of the carapace of Neurankylus eximius, one-third the natural size. N. 3, //, &c., neural bones;, C. 3, 4> £&«, costal bones;.spy, suprapyg-al bone; r, rib-end. The heavy lines indicate tlie boundaries of the epidermal shields, the sinuous ones the sutures between the bones, and the dotted ones the parts restored.Published as part of Lambe L. M., 1902, New genera and species from the Belly River Series (mid-Cretaceous), pp. 25-81 in Geological Survey of Canada Contributions to Canadian Palaeontology 3 on page 42, DOI: 10.5281/zenodo.323376
Suberites concinnus Lambe 1895
No full textSuberites concinnus Lambe, 1895 Figs. 20, 21 Suberites montiniger: Koltun 1966; Austin 1985; Austin & Ott 1987 Non: Suberites montiniger Carter, 1880 Material examined. Syntype: CNM 1900–2822 (previously 2553), Bering I., Commander Islands, USSR, (55 º 0.1 ′N, 166 º 16.4 ′W), found on beach, coll. L. Stejneger, 1882–1883. Other material: RBCM 976-1038 - 6, Hatie I., Portland Canal, BC, (55 º 17 'N, 129 º 59 'W), Mar. 23, 1976, coll. P. Lambert; RBCM 974 - 224 - 2, Winter Inlet, BC, (approx. 54 º 49 'N, 130 º 26 'W), no depth, Jun. 13, 1974, 3 specimens; RBCM 974 - 552 - 1, Wales I., BC, (approx. 54 º 42 'N, 130 º 28 'W), no depth, Jul. 29, 1974; RBCM 974 - 390 - 5, Grace Point, BC, (approx 54 º 38 'N, 130 º 26 'W), no depth, 1974, coll. P. Lambert; RBCM 974 - 230, Brundage Inlet, Dundas I., BC, (approx. 54 º 37 'N, 130 º 50 'W), no depth, Jun. 19, 1974; RBCM 974 - 563 - 2, Coghlan Arch near Banks I., BC, (approx. 54 º 27 'N, 130 º 41 'W), no depth, 1974; RBCM 976 - 104 - 21, Langara I., BC, (approx. 54 º N, 133 º W), Apr. 30, 1976; KML 1060, KML sta. 174 / 76., Houston Stewart Channel, BC, (52 º 09.5'N – 131 º 05.6'W), 24 m depth, Aug. 31, 1976, coll. W.C. Austin; KML 1058, KML 602 / 77, Houston Stewart Channel, BC, (approx. 52 º 9 'N, 131 º 5 'W), 1977, coll., W.C. Austin; CMN H 31, Kitasu Bay, BC, (approx. 51 ° 27 'N, 127 º 44 'W), no depth, Jul. 20, 1964, coll. E.L. Bousfield; KML 1057, PEI 169, Dimsey Point, Rivers Inlet, BC, (51 º 27 'N, 127 º 44 'W), 5 m depth, no date, coll. & photo N. McDaniel; KML 1056, KML sta. 270 / 70, Pine I., BC, (50 º 58.5 'N, 127 º 43.7 'W), 20 m depth, Sept. 15, 1970, coll. W.C. Austin; RBCM 977 - 158 - 5, Boxer Pt., Nigei I., BC, (50 º 50 'N, 127 º 39 'W), 25 m depth, no date, coll. unknown.; RBCM 977 - 139 -08, Minstrel I., BC, (approx. 50 º 37 'N, 126 º 17 'W), 25 m depth, Jul. 8, 1977; KML 1059, PEI 83, Steep I. W of Gowland Harbour,, BC, (50 º 4.8 'N, 123 º 15.3 'W), 20 m depth, Mar. 6, 1977, coll. & photo, N. McDaniel; KML 124 / 76, East of Effingham I., BC, (48 º 52.7 'N, 125 º 17.2 'W), 24, 50 m depth, Jul. 26, 1976, coll. W.C. Austin; KML 1061, KML sta. 124 / 76, E of Effingham I., BC, (48 º 52.7 'N, 131 º 05.6'W), 24–50 m depth, no date, coll. W.C. Austin. Field images without vouchers: Gordon Rock, E of Malcolm Island, BC, (approx. 50 º 35 'N, 126 º 53 'W), photo N. McDaniel; Plumper Rock, E. of Malcolm I., Weynton Pass, 4 km NW of NW Point on Hanson I., BC, (approx. 50 º 35 'N, 126 º 49 'W), photo N. McDaniel; Discovery Passage, BC, (approx. 50 ºN, 125 º 11 'W), 4 photos N. McDaniel; Race Rocks, BC, (approx. 48 º 18 'N, 123 º 32 'W), photo N. McDaniel; Active Pass, BC, (approx. 48 º 52 'N, 123 º 18 'W), photo N. McDaniel. Comparative material: Suberites montiniger, NOAA 27218, Stefansson Sd., Beaufort Sea, (70 º 19 'N, 147 º 35 'W), 6 m depth, no date, coll. unknown. Description. Macroscopic features. (Fig. 20 A–E). Irregularly globular, typically 11 cm long by 7 cm wide by 5 cm thick. Oscula range from one to many; in life may be on short chimneys. Soft and porous alive; contracts 70 % to moderately hard to soft rubbery texture when preserved in alcohol. In life surface may be white to orange covering a brownish orange to white interior. Microscopic features. (Fig. 20 F). Surface megascleres in tufts oriented vertically. Choanosomal megascleres randomly oriented. Together these form layer about 300 µm thick. Spicules (Fig. 21 A–I). Megascleres of KML 1056 examined in detail; exclusively styles, most straight, some with slight bend. No difference in spicule type or size between the ectosome and choanosome. Megascleres of nine additional specimens from range of BC localities examined for presence of styles and incipient subtylostyles summarized in Tables 11 and 12, and Figs. 21 E–G). SEMs from a specimen of Suberites montiniger from the Beaufort Sea included for comparison (NOAA, cat. 27218) (Figs. 21 H–I). KML 1056 Location Spicule Type Fig. Length Width Ectosome Style 21 A–B 190 –(224)– 260 5 –(5.0)– 6 Choanosome Style 21 C–D 200 –(229)– 250 5 –(5.2)– 6 Microscleres absent. Remarks. We searched for records of Suberites from the northern hemisphere with styles or subtylostyles but not tylostyles. Three species are recorded in the Porifera database by van Soest et al. (2012): Suberites concinnus Lambe, 1895, Suberites montiniger Carter, 1880, and Suberites montalbidus Carter, 1880. Suberites montalbidus invariably has centrotylote microxea or microstrongyles (Carter 1880; Vosmaer 1882; Fristedt 1885, 1887; Lambe 1895) and so can be excluded from further consideration. Lambe’s specimens of S. concinnus ranged from the Gulf of Alaska to Bering I. at the west end of the Aleutians. Burton (1935) recorded a typical specimen from Saghalien Bay, Kol, Sea of Okhosk from 3– 8 m. Lambe (1895) described and figured the smooth styles in his specimens. They ranged from 229–301 x 5 µm. The maximum size is 40 µm larger than that found in the material we examined. However, we did not search for the largest spicule but rather measured a random sample of 20 spicules. Koltun (1966) placed S. concinnus in synonymy with Suberites montiniger (Carter 1880). His rationale was not explicit. He stated that, typically, the megasclere size range in S. montiniger is 200–270 x 3–6 µm, comparable to the size range we find in S. concinnus. But Koltun also observed that a few specimens had megascleres ranging from 330–600 x 10 µm—much longer than we find in specimens in British Columbia or southern Alaska. The megascleres in our specimen of S. montiniger from the Beaufort Sea are significantly longer (Table 12, mean 318 Μm) than in our specimens of S. concinnus (means 212–237 Μm). The megascleres in Koltun’s material were characterized as subtylostyles not styles. One might surmise that Koltun did not consider the difference between styles and subtylostyles as significant. Our examination of spicules in nine additional specimens (Table 11) revealed one example with significant numbers of incipient subtylostyles. But 50 % of the spicules were styles. It was collected in the same region as many of the other specimens with a low % of subtylostyles. On the other hand, 99 % of the spicules observed were subtylostyles and 1 % were styles on examination of a specimen we consider to be Suberites montiniger sensu strictu from the Beaufort Sea. The subtylostyles in this specimen of S. montiniger have a significantly longer swollen head (Fig. 21 H, I) than the incipient subtylostyles of one specimen of S. concinnus (Fig. 21 F, G). Except for Koltun (1966) who merged the two species, neither Carter (1880), Vosmaer (1882) nor Hentschel (1916) mentioned the relative proportion of styles to subtylostyles among megascleres in their descriptions of S. montiniger. Suberites montiniger and S. cocinnus may differ in biogeographic zones. Records of S. montiniger are from 70–80 degrees N in the Barents Sea and Greenland Sea (Carter 1880; Vosmaer 1882; Hentschel 1916, 1929; Swartschewsky 1906) and from the Beaufort Sea (this paper). Records of S. concinnus are from 50–60 degrees N in the Sea of Okhotsk, Bering Sea, Gulf of Alaska and British Columbia (Lambe 1895, Burton 1935, this paper). One exception is an identification of S. montiniger from 48 degrees N in the northern part of the Sea of Japan by Burton (1935). We suggest that this record needs verification. Topsent (1915), Hentschel (1916) and Koltun (1966) note that a specimen referred to S. montiniger by Lambe (1895) is not this species as it has subtylostyles averaging 16 Μm in diameter compared to 5–6 Μm for S. montiniger. We agree but will not attempt to assign it to another species. Conclusions. In our opinion the difference in prevalence of styles versus subtylostyles and differences in spicule mean size and range, coupled with largely different zoogeographic zones (Arctic vs. cold temperate and boreal) supports maintaining S. concinnus as a separate species from S. montiniger. The one specimen among eleven which has a significant number of (incipient) subtylostyles (RBCM 974 - 563 - 2, Table 11) may be an anomaly or possibly a hybrid. Also, these subtylostyles are different from those in our specimen of S. montiniger: the tyle is shorter and with a more angular apex. Finally, the size range and mean of spicules in RBCM 974 - 563 - 2 fit the other S. concinnus specimens, not the S. montiniger specimen (NOAA 27218) (Table 12). Bathymetric range. 3 to 118 m depth. Geographic distribution. Sea of Okhotsk (Russia) east to the Gulf of Alaska (USA) and south to southern BC (Canada). Ecology. This species is restricted to current swept rocks.Published as part of Austin, William C., Ott, Bruce S., Reiswig, Henry M., Romagosa, Paula & G, Neil, 2014, Taxonomic review of Hadromerida (Porifera, Demospongiae) from British Columbia, Canada, and adjacent waters, with the description of nine new species, pp. 1-84 in Zootaxa 3823 (1) on pages 53-57, DOI: 10.11646/zootaxa.3823.1.1, http://zenodo.org/record/28637
A Multi-Language Comparison of Influences on Author Verification using Character N-Grams
No full textWe create a new multi-language corpus for author verification based on Wikipedia talkpages, and evaluate the influence that differences in topic and time have on character n-gram author profiles. Topic alignment between two texts is found to increase author verification precision, and an authors writing style is found to change over time, but not more significantly after 3 years than after 1 year.Information ArchitectureWISElectrical Engineering, Mathematics and Computer Scienc
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