2,677 research outputs found
Julio Tenorio family
No full textJulio Tenorio family: Julio Tenorio and Candelaria Martinez Tenorio seated on couch. Standing behind, R-L: Filimon Tenorio, Audilio Tenorio and Heraldo Tenorio, their sons. Filimon married Rosemary Gilliam, they had one child, Valerie. Geraldo married Antonia Villegas, their children are John, Jody, Sylvia and Viola. Audio married Patricia Ortiz, they had one child, Donna. Audilio died in August 201
Cordelina Gonzales, Katie and Barbara Tenorio, Joe Gonzales, Jr.
No full textChildren standing at the side of a coupe. L-R: Cordelina Gonzales, Barbara Adela Tenorio (in front; later Christianson Twining), Maria Catalina Tenorio (Katie), Joe Gonzales Jr. Bosque and Sandias in background
Beatrice Espalin Tenorio and her sister Ava Maria Espalin Griego
No full textL-R: Beatrice Espalin Tenorio and her sister, Ava Maria Espalin Griego (Beatrice died in 1984
Lysley Tenorio, 36th Annual ODU Literary Festival
No full textLysley Tenorio is the author of Monstress (2012). His stories have appeared in The Atlantic, Zoetrope: AII-Story, Ploughshares, Manoa, The Chicago Tribune, and The Best New American Voices and Pushcart Prize anthologies. A former Stegner Fellow at Stanford, he has received a Whiting Writer\u27s Award and fellowships from the MacDowell Colony, Yaddo and the National Endowment for the Arts. He teaches at Saint Mary\u27s College of California and lives in San Francisco
Profundiconus virginiae Tenorio & Castelin 2016
No full text<i>Profundiconus virginiae</i> Tenorio & Castelin, 2016 <p>Figs 2, 16I–L, N, 20</p> <p> <i>Profundiconus virginiae</i> Tenorio & Castelin, 2016: 22, figs 9a–d, g, 10.</p> <p> <i>Profundiconus</i> n. sp. h – Puillandre <i>et al.</i> 2014: supplementary material 1 (unfigured).</p> <p> <i>Profundiconus</i> cf. <i>cakobaui</i> (non <i>Conus cakobaui</i> Moolenbeek, R ̂ckel & Bouchet, 2008) – Tenorio 2015a: 45 (unfigured).</p> <p> <i>Profundiconus virginiae</i> – Monnier <i>et al.</i> 2018a: 143.</p> Material examined <p>3 lots (3 specimens). See Supp. file 1.</p> Type material <p> <b>Holotype</b> NEW CALEDONIA • 42.5 mm; Coral Sea, Plateau des Chesterfield, off New Caledonia, stn DW2613; 19°37′ S, 158°42′ E; 519–522 m depth; 19 Oct. 2005; EBISCO expedition; MNHN-IM-2007-30854 (Fig. 16I–J).</p> Figured material <p>NEW CALEDONIA • Paratype, 33.7 mm; Plateau des Chesterfield, off New Caledonia, stn DW2609; 19º33′ S, 158º40′ E; 431‒436 m depth; 19 Oct. 2005; EBISCO expedition; MNHN-IM-2007-30858 (Fig. 16K, N) • paratype, 16.3 mm (fragment); Plateau des Chesterfield, off New Caledonia, stn DW2610; 19º34′ S, 158º41′ E; 486‒494 m depth; 19 Oct. 2005; EBISCO expedition; MNHN-IM-2000-30789 (Fig. 16L).</p> Geographical distribution and bathymetry <p>Coral Sea, Plateau des Chesterfield, at depths between 400‒ 600 m. This species can be considered endemic.</p> Remarks <p> Shell moderately small to medium sized (maximum length 42.5 mm). Multispiral protoconch with 3–3.5 whorls, white, glossy and translucent (Fig. 16L). Radular tooth (Fig. 16N) medium- to large-sized, rather elongated. Anterior portion of tooth shorter than posterior section, with one barb and a pointed, well-defined blade which covers 40–43% of anterior portion of tooth. External cusp present, laterally expanded and serrated, with 5–6 small denticles. Characteristic fringe of closely spaced projections pointing towards apex located immediately below waist. Shaft fold present. Large and prominent basal spur on top of slanted base of tooth. This is a very rare species known from very few specimens only. In the phylogeny (Fig. 2) the two sequenced individuals of <i>P. virginiae</i> form a monophyletic group that is the sister group of <i>P. zardoyai</i>, <i>P. vaubani</i>, and <i>P. kanakinus</i>.</p>Published as part of <i>Tenorio, Manuel J. & Puillandre, Nicolas, 2023, Revision of the deep-water cone snail fauna from New Caledonia (Gastropoda, Conoidea), pp. 1-134 in European Journal of Taxonomy 896</i> on pages 30-31, DOI: 10.5852/ejt.2023.896.2291, <a href="http://zenodo.org/record/8405510">http://zenodo.org/record/8405510</a>
El Tlacuache Núm. 932 (2020). 932 Año 19 (2020) mayo. El Tlacuache
No full text- La pandemia COVID 19, un mar de angustias, dilemas y retos, I por Luis Miguel Morayta Mendoza. - Los virus y el Antropoceno. Las señales previas del desastre por Eduardo Corona Martínez. - Los huertos familiares en tiempos del COVID 19 por María Alejandra Elizabeth Olvera Carbajal. - Ante el Coronavirus , la ciudad en abandono por Erick Alvarado Tenorio
Afonsoconus Tucker & Tenorio 2013
No full textGenus Afonsoconus Tucker & Tenorio, 2013 Type species Chelyconus kinoshitai Kuroda, 1956, by original designation. Diagnosis SHELL (Fig. 1 A–H). Elongated conical to cylindrical shell; spire low and conical in shape; posterior notch deep and cords present on whorl tops; columella twisted, but without anterior notch; shell and spire coloration variable; operculum small, ovate-shaped; periostracum thin and translucent, with multiple fine spiral rows of small tufts. RADULAR TOOTH (Fig. 1 I–J). Narrow and elongated, with a large to medium relative size; waist indistinct; anterior section equal or slightly longer than the posterior section; tooth serrated with a fairly long row of small serrations; terminating cusp small; barb and blade very short; blade barely twice as long as barb; base large; basal spur present; basal ligament present (not shown in Fig. 1 I–J). Geographic distribution The species included in the genus occur in the Indo-Pacific region. Geologic range Recent. Remarks Afonsoconus is here treated as a genus, following Tucker & Tenorio (2013) and Monnier et al. (2018), but Puillandre et al. (2014) ranked it as a subgenus within Conus. There are currently two species included in genus Afonsoconus (WoRMS editorial board 2018).A number of taxon names associated with A. kinoshitai are considered synonyms (forms). These are tamikoanus Shikama, 1973, calliginosus Shikama, 1979 and brontodes Shikama, 1979, and were already presented in the Introduction (vide supra). The name Conus (Chelyconus) wistaria Shikama, 1970 has occasionally been associated to A. kinoshitai especially among amateur shell collectors, but the name actually applies to a color form of Pionoconus fulmen (Röckel et al. 1995; Filmer 2012; Tucker & Tenorio 2013). The food habits of the species in Afonsoconus are not known, but the radular morphology (Fig. 1 I–J) suggests that they prey on worms. Based upon conotoxin analysis, it has been inferred that A. kinoshitai is a piscivorous species (Bulaj et al. 2005; Puillandre et al. 2010). However, this is not supported by direct observation of prey capture (Olivera et al. 2015). In analogous fashion, other species of Conidae in the genera Embrikena Iredale, 1937 and Asprella have been considered piscivorous based upon the presence of certain conotoxins in their chemical repertoire (Olivera et al. 2015). However, this assumption is not supported either by direct observation of prey capture nor by the morphology of the respective radular teeth of these species, which are more consistent with a vermivorous feeding mode (Tucker & Tenorio 2013). Several conotoxins have been identified for A. kinoshitai, most notably the μ-conotoxin μ-KIIIA (Bulaj et al. 2005; Zhang et al. 2007; Khoo et al. 2009). This conotoxin blocks mammalian neuronal tetrodotoxin (TTX) resistant voltage-gated sodium channels (VGSCs) and is a potent analgesic (Bulaj et al. 2005; Zhang et al. 2007; McArthur et al. 2011). Phylogenetic analyses Afonsoconus is recovered as a monophyletic group with high support (Posterior Probability PP = 1) (Fig. 3). The Afonsoconus clade is sister to the Textilia clade (Puillandre et al. 2014), which contains fish-eating species characterised by their polished and shining subcylindrical to cylindrical shells (Fig. 2), and by their harpoon-shaped radular teeth (Fig. 2). Afonsoconus is clearly split in three subclades, each of them fully supported (PP = 1), and with high genetic distances between them (> 8%). Conversely, genetic distances within each subclade are all <1%, except between the two samples of kinoshitai, with a genetic distance of 5.4%. The three subclades correspond to different geographic regions, one with specimens from the Philippines, another with specimens from New Caledonia, and a third one containing the specimens from the Mozambique Channel (BIOMAGLO expedition). The specimens from the Philippines and New Caledonia correspond respectively to the species A. kinoshitai and A. bruuni. According to the phylogenetic relationships and the genetic distances, the specimens from the Mozambique Channel deserve specific status, and this new species is hereby introduced. It is interesting to note that the observed p-distance between the two specimens of A. kinoshitai from GenBank (sequences FJ937341.1 and KJ550543.1) is consistent with a separation at the species level, as found for other species of cone snails (e.g., Duda et al. 2008; Puillandre et al. 2011). Both specimens come from the Philippines, and one of them (sequence KJ550543.1) appears labelled in GenBank as Conus kinoshitai tamikoae (= tamikoanus). Given the fact that the tamikoanus from Japan / China is a synonym (form) of A. kinoshitai, as recognised by its author in Shikama (1979), the results of the phylogeny actually suggest that there may be at least two different species of Afonsoconus in the Philippines. If we accept that the specimen associated with the sequence FJ937341.1 is A. kinoshitai, the other one would be a putative new species, morphologically similar to the form tamikoanus according to its label. The specimens from the Philippines labelled as tamikoanus are treated as a subspecies of A. bruuni in Raybaudi-Massilia (2008), or as a full species in Monnier et al. (2018). It is likely that the tamikoanus -like specimen in GenBank is a representative of the taxon featured in Raybaudi-Massilia (2008) and in Monnier et al. (2018). Unfortunately, no voucher specimen or photo thereof is associated with the GenBank sequence KJ550543.1, so any further taxonomical claim on this matter would be merely speculative at this stage. Description of new speciesPublished as part of Tenorio, Manuel J., Monnier, Eric & Puillandre, Nicolas, 2018, Notes on Afonsoconus Tucker & Tenorio, 2013 (Gastropoda, Conidae), with description of a new species from the Southwestern Indian Ocean, pp. 1-20 in European Journal of Taxonomy 472 on pages 8-10, DOI: 10.5852/ejt.2018.472, http://zenodo.org/record/382507
Profundiconus smirnoides Tenorio 2015
No full textProfundiconus smirnoides Tenorio, 2015 Figs 2, 14–15 Profundiconus smirnoides Tenorio, 2015b: 4, pls 1–3. Conus smirna (non C. smirna Bartsch & Rehder, 1943) – Marshall 1981: 499, fig. 3h–i. — Richer de Forges & Estival 1986: 16, unnumbered fig. — Röckel et al. 1995a: 563, fig. 21; 1995b: pl. 27 figs 6–7. — Moolenbeek et al. 2008: pl. 3 fig. 26. — Puillandre et al. 2015: 4. Profundiconus smirnoides – Monnier et al. 2018a: 136. Material examined 42 lots (51 specimens). See Supp. file 1. Type material Holotype NEW CALEDONIA • 71.8 mm; off Île des Pins, off New Caledonia, stn DW3125; 22º55.5′ S, 167º17.1′ E; 480–500 m depth; 30 Oct. 2008; TERRASSES expedition; MNHN-IM-2009-18220 (Fig. 14A). Figured material NEW CALEDONIA • 73.7 mm; Norfolk Ridge, Jumeau Est, off New Caledonia, stn DW3053; 23°45′ S, 168°16′ E; 410‒440 m depth; 19 Oct. 2008; TERRASSES expedition; MNHN (Fig. 14B) • 81.5 mm; S Lansdowne, off New Caledonia, stn DW2635; 21º03′ S, 160º45′ E; 80‒397 m depth; 21 Oct. 2005; EBISCO expedition; MNHN (Fig. 14C) • 79.7 mm; Norfolk Ridge, Banc Introuvable, off New Caledonia, stn DW1699; 24º40′ S, 168º40′ E; 581‒600 m depth; 24 Jun. 2001; NORFOLK 1 expedition; MNHN (Fig. 14D) • 76.9 mm; Norfolk Ridge, Banc Introuvable, off New Caledonia, stn DW1699; 24º40′ S, 168º40′ E; 581‒600 m depth; 24 Jun. 2001; NORFOLK 1 expedition; MNHN (Fig. 14E) • 52 mm; Norfolk Ridge, off New Caledonia, stn DW819; 23º45′ S, 168º16′ E; 478‒486 m depth; 28 Nov. 1993; BATHUS 3 expedition; MNHN (Fig. 14F) • 63.4 mm; off New Caledonia, stn DW197; 18º51′ S, 163º21′ E; 550 m depth; 20 Sep. 1985; MUSORSTOM 4 expedition; MNHN (Fig. 14G) • 81.4 mm; Norfolk Ridge, off New Caledonia, stn DW169; 23º37′ S, 167º42′ E; 447‒450 m depth; 29 Jan. 1993; SMIB 8 expedition; MNHN (Fig. 14H, M) • 39.9 mm; Norfolk Ridge, off New Caledonia, stn DW187; 23º17′ S, 168º06′ E; 390‒540 m depth; 31 Jan. 1993; SMIB 8 expedition; MNHN (Fig. 14I) • 97.9 mm; Banc Kaimon Maru, off New Caledonia, stn DW65; 24º47′ S, 168º09′ E; 245‒275 m depth; 3 Sep. 1985; BIOCAL expedition; MNHN (Fig. 14J) • 39.9 mm; Norfolk Ridge, Banc Eponge, off New Caledonia, stn CP08; 24º54′ S, 168º21′ E; 540 m depth; 11 Aug. 1999; LITHIST expedition; MNHN (Fig. 14K–L). Geographical distribution and bathymetry Coral Sea (Lansdowne Bank), New Caledonia including Grand Passage, Loyalty Islands, Norfolk Ridge, and northern New Zealand (Wanganella Bank, and possibly Kermadec Ridge), at depths between 80 and 1150 m, mostly between 450 and 600 m. There is a report of a dead specimen collected off Fiji (Moolenbeek et al. 2008), suggesting an extension of the range to this area. Remarks Shell moderately large to large (maximum length 98.0 mm), narrowly conoid-cylindrical with a high to very high spire. Protoconch multispiral, of 3.0–3.5 whorls, brown, smooth (Fig. 14L). Radular tooth (Fig. 14M) medium- to large-sized, very elongated, with anterior section longer than half of total tooth length in adult specimens. Waist indistinct, with barb and one pointed blade covering less than one quarter of anterior portion. Serrations absent. There is an external cusp starting at the base of the adapical opening, almost equal in size to the blade on the opposite side of the tooth. This external cusp is short, pointed and non-serrated. Immediately below the indistinct waist, there is a small oblique fringe with a serrated edge consisting of 4–5 blunt denticles pointing towards the anterior portion. A shaft fold is present, although difficult to detect in adults due to the elongation of the tooth. Slanted base, with a large basal spur present. Several specimens of P. smirnoides (cox1 gene fragment) have been sequenced (Fig. 2). The placement of this species in the Profundiconus clade is confirmed, although the relationships with other species of Profundiconus, most notably with P. teramachii, were not resolved satisfactorily (Tenorio & Castelin 2016).Published as part of Tenorio, Manuel J. & Puillandre, Nicolas, 2023, Revision of the deep-water cone snail fauna from New Caledonia (Gastropoda, Conoidea), pp. 1-134 in European Journal of Taxonomy 896 on pages 21-22, DOI: 10.5852/ejt.2023.896.2291, http://zenodo.org/record/840551
Profundiconus neocaledonicus Tenorio & Castelin 2016
No full text<i>Profundiconus neocaledonicus</i> Tenorio & Castelin, 2016 <p>Figs 2, 10–11</p> <p> <i>Profundiconus neocaledonicus</i> Tenorio & Castelin, 2016: 33, figs 15a–j, 16a–c, 17.</p> <p> <i>Conus profundorum</i> (non <i>Chelyconus</i> (<i>Profundiconus</i>) <i>profundorum</i> Kuroda, 1956) – Rolán & RaybaudiMassilia 1994: 33, pl. 11 fig. 82. — Röckel <i>et al.</i> 1995a: 563, fig. 22; 1995b: 381, pl. 27 fig. 16.</p> <p> <i>Profundiconus</i> cf. <i>profundorum</i> – Puillandre <i>et al.</i> 2014: supplementary material 1 (unfigured).</p> <p> <i>Profundiconus neocaledonicus</i> – Monnier <i>et al.</i> 2018a: 128.</p> Material examined <p>100 lots (about 150 specimens). See Supp. file 1.</p> Type material <p> <b>Holotype</b> NEW CALEDONIA • 45.9 mm; Norfolk Ridge, Banc Crypthélia, off New Caledonia, stn DW3076; 23°14′ S, 168°13′; 390–570 m depth; 23 Oct. 2008; TERRASSES expedition; MNHN-IM-2009-18227 (Fig. 10A).</p> Figured material <p>NEW CALEDONIA • 61.3 mm; SE part of Mont Vauban, off New Caledonia, stn DW3889; 22°25′ S, 171°41′ E; 354 m depth; 19 Sep. 2011; EXBODI expedition; MNHN (Fig. 10B, L–M) • 52.6 mm; Norfolk Ridge, off New Caledonia, stn DW167; 23º38′ S, 167º43′ E; 430‒452 m depth; 29 Jan. 1993; SMIB 8 expedition; MNHN (Fig. 10C) • 54.5 mm; off S New Caledonia, stn CC1; 24º55′ S, 168º22′ E; 500 m depth; 28 Oct. 1986; CHALCAL 2 expedition; MNHN (Fig. 10D) • 67.3 mm; Norfolk Ridge, Banc N, off New Caledonia, stn DW1657; 23º28′ S, 167º52′ E; 305‒332 m depth; 19 Jun. 2001; NORFOLK 1 expedition; MNHN (Fig. 10E) • 65.1 mm; Loyalty Ridge, off New Caledonia, stn DW406; 20º41′ S, 167º07′ E; 373 m depth; 15 Feb. 1989; MUSORSTOM 6 expedition; MNHN (Fig. 10F) • 92 mm; Norfolk Ridge, Banc P, off New Caledonia, stn DW1732; 23º29′ S, 168º16′ E; 347‒1063 m depth; 27 Jun. 2001; NORFOLK 1 expedition; MNHN (Fig. 10G) • 44.3 mm; off S New Caledonia, stn DW22; 23º03′ S, 167º19′ E; 503 m depth; 24 May 1987; SMIB 3 expedition; MNHN (Fig. 10H) • 53.4 mm; Norfolk Ridge, off New Caledonia, stn CP811; 23º41′ S, 168º15′ E; 383–408 m depth; 28 Nov. 1993; BATHUS 3 expedition; MNHN (Fig. 10I) • 71.8 mm; off S New Caledonia, stn DW82; 23º14′ S, 168º04′ E; 304 m depth; 31 Oct. 1986; CHALCAL 2 expedition; MNHN (Fig. 10J) • 39.9 mm; Norfolk Ridge, Île des Pins, off New Caledonia, stn DW2156; 22º54′ S, 167º15′ E; 468‒500 m depth; 5 Nov. 2003; NORFOLK 2 expedition; MNHN (Fig. 10K).</p> Geographical distribution and bathymetry <p> New Caledonia: Norfolk Ridge and Loyalty Islands, typically at depths between 300 and 600 m, although some individuals come from beyond 1000 m deep. Some specimens have been sampled in the Coral Sea (Argo Bank) and in the Grand Passage area. A couple of empty shells resembling <i>P. neocaledonicus</i> from Aliguay Island, Philippines have been examined, but their identity was not confirmed by radular or DNA studies. This observation might suggest an extension of the distribution range to the Philippines, but would require additional evidence (Tenorio & Castelin 2016).</p> Remarks <p> Medium-sized to moderately large (maximum length 92.0 mm). Protoconch multispiral of 3 or more whorls, white to pale violet-brown (Fig. 10L). Radular tooth (Fig. 10M) rather small. Anterior portion of tooth shorter than posterior section, with pointed blade covering about one half of apical portion of tooth. External cusp present, not much widened laterally and with indistinct serrations, with only 0–3 small blunt denticles. Characteristic fringe of closely spaced projections pointing towards apex located immediately below waist. Shaft fold present. Large and prominent basal spur on top of slanted base of tooth. In the phylogeny (Fig. 2), the specimens of <i>P. neocaledonicus</i> are grouped in a clade sister to another large one containing specimens of <i>P. teramachii</i> mixed with some individuals of <i>P. smirnoides</i>.</p>Published as part of <i>Tenorio, Manuel J. & Puillandre, Nicolas, 2023, Revision of the deep-water cone snail fauna from New Caledonia (Gastropoda, Conoidea), pp. 1-134 in European Journal of Taxonomy 896</i> on pages 16-18, DOI: 10.5852/ejt.2023.896.2291, <a href="http://zenodo.org/record/8405510">http://zenodo.org/record/8405510</a>
Conus vulcanus Tenorio et Afonso, 2004
No full textCatálogo do Museo de Historia Natural USC. n. inventario 10014
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