109,351 research outputs found
Doriprismatica rossi Matsuda & Gosliner 2018, sp. nov.
Doriprismatica rossi Matsuda and Gosliner, sp. nov. Figures (2I, 11C, 13D, E, 14A–E) Doriprismatica sp. 5 Gosliner et al. 2015: p. 240, upper left photo. Doriprismatica sp. B Matsuda & Gosliner 2017. Type material. Holotype: CASIZ-192281, one specimen, dissected, 31 mm preserved, Saudi Arabia, Red Sea, West Manghar Island, night dive, 8 March 2013, T. Gosliner, Red Sea Biodiversity Cruise 2013, orig. fixative 95% EtOH. This specimen was tissue sampled (foot) for DNA analysis in Matsuda & Gosliner (2017), GenBank: KT600690 (COI). Etymology. Doriprismatica rossi is named after the first author’s brother, Ross Kyo Matsuda. Distribution. Known only from the Saudi Arabian Red Sea. External morphology. The mantle of Doriprismatica rossi sits high on the sides of the body above the foot and tapers posteriorly (Fig. 11C). The mantle has small conical tubercles over its entire surface. The mantle edge has the characteristic semi-permanent undulations, including two sets of permanent large folds, the first slightly behind the rhinophores and the second anterior to the gill. The mantle and foot are a burgundy-charcoal color that is covered with small white spots that are denser towards the edge of the mantle. Larger burgundy spots speckle the mantle over the white. A black band runs the edge of the mantle and is bordered on both sides first by thin electric blue bands and then followed by thicker mustard colored bands (Fig. 2I). The gill is two-thirds of the way back on the mantle and consists of approximately 14 unipinnate lamellae arranged in a spiral and forming an arc that opens posteriorly around the anus. Some of the lamellae have branching tips of up to four prongs while others are single and they become shorter at the ends of the arch. All of the gill branches are held close to the surface of the mantle. The gill stalk is a greener mustard color that fades to white, and two dark lines run up the inward and outward facing sides midway-up that join at the tip. The base of the rhinophores are a cream and mustard color and the rhinophores are dark charcoal that is dusted with white that gives them a frosted appearance. The rhinophores have approximately 15 closely packed lamellae. Behind the rhinophores are two burgundy-charcoal patches on the mantle that are not covered in white dots. The genital opening is on the right side of the body below the mantle and behind the rhinophores. Internal anatomy. Radular structure (Fig. 14A–E). The oral tube is approximately three times as long as the buccal bulb (Fig. 13E). The radular ribbon is long and of medium width (Fig. 14D) (radular formula for 35 mm preserved specimen is approximately 165 x 25.0.25). A row of rachidian teeth is absent (Fig. 14A). The first lateral tooth has a long central cusp with three to four, large, well-defined downward-pointing denticles on both sides. The inner and mid-lateral teeth (Fig. 14B) have a longer central cusp with the same number of denticles on the outer edge, however with no denticles on the inner edge. The outer teeth (Fig. 14C) are only slightly reduced and have only one denticle on the outer edge. The jaw plates are composed of long bifid rodlets that are slightly curved (Fig. 14E). Reproductive system (Fig. 13D). The vagina is of medium length and narrow and connects with the receptaculum seminis duct before reaching the receptaculum seminis sac and bursa copulatrix. The penial bulb is long and convoluted leading to a shorter muscular vas deferens. A long, twisted prostate gland connects to the base of the ampulla adjacent to the albumen gland. Remarks. Doriprismatica rossi is sister to Doriprismatica marinae sp. nov., and together they are sister to the clade containing D. atromarginata and D. sibogae. Doriprismatica rossi has its own unique color pattern and together with D. paledentata is the only species in the genus with three distinct marginal bands. These two species are unique in having mantle tubercles. The mantle of D. rossi is more oval that D. atromarginata and D. sibogae. The mantle bands are continuous, unlike in D. atromarginata and D. sibogae whose mantle bands include areas with slight interruptions. The mantle bands are similar in color to D. paladentata, however the bands on D. paladentata are much lighter and the body is teardrop-shaped with a broader anterior. The mantle of D. paladentata is covered with white spots, however the overall color of the mantle is a very light cream. The rhinophores and gills of D. paladentata, D. atromarginata and D. sibogae all stand out dark against the body, which is not the case for D. rossi. The radula for D. rossi differs from that of D. atromarginata by having a slightly longer central cusp, and resemble more closely those of D. sibogae (Rudman 1986, fig. 6, specimen from Fiji). The ABGD analysis supports D. rossi as a distinct species (Fig. 5). The p-distance values between D. rossi and D. marinae is 2%, which while seemingly small, is consistent with the p-distances between and within other species of Doriprismatica (Matsuda & Gosliner 2017) (Fig. 5). Their general body form is markedly different. The p-distances between individuals of D. atromarginata is 1% and between specimens of D. paladentata is 0, and the p-distances that separate D. atromarginata and D. sibogae is 3%.Published as part of Matsuda, Shayle B. & Gosliner, Terrence M., 2018, Glossing over cryptic species: Descriptions of four new species of Glossodoris and three new species of Doriprismatica (Nudibranchia: Chromodorididae), pp. 501-529 in Zootaxa 4444 (5) on pages 521-523, DOI: 10.11646/zootaxa.4444.5.1, http://zenodo.org/record/143722
Letter from T. Ando to The Dominguez Estate Company,
Requesting a current address for Mr. M. Matsuda. For reply see item csudh_rsp_030
Highly diastereoselective Heck–Matsuda reaction with pyrazolyl diazonium salts
The Heck–Matsuda (HM) reaction is a powerful synthetic approach
cut out for C–C bonds formation under mild conditions. We
demonstrated that pyrazolyl diazonium salts are suitable reagents
in this protocol, allowing us to deliver highly substituted cyclopentenols and cyclopentenamines with an excellent degree of
diastereoselectivity and a control of enantioselectivit
Glossodoris buko Matsuda & Gosliner 2018, sp. nov.
Glossodoris buko, Matsuda & Gosliner sp. nov. Figures (1A–C, 2A, 3A–E, 4C–D) Glossodoris pallida (Rüppell & Leuckart 1830), misidentification, Rudman 1990: figs. 9c, 10e–f; Gosliner et al. 2008: 240, third photo; Turner & Wilson 2008; Gosliner et al. 2015: 237, upper right photo. Glossodoris xantholeuca Ehrenberg 1831: 92; Rudman 1984. Glossodoris sp. A Matsuda & Gosliner 2017. Type Material. Holotype: CASIZ-223284 (ex CASIZ- 191102 B) 4 mm preserved, Papua New Guinea, Madang Province, Bilbil Island, coll: V. Knutson, 10 November 2012, orig. fixative 95% EtOH, GenBank: KT600713 (COI). Paratypes: CASIZ- 191102 A, 13 specimens,1 dissected, 3–8 mm, same collection data as holotype. CASIZ- 0 86381, 6 specimens, 1 dissected, 6.5–11 mm, Papua New Guinea, North Coast, North of Madang, approx. 1 km South of Cape Croisilles, South side of The Quarry, coll: T.M. Gosliner, 13 June 1992, orig. fixative Bouin’s solution. CASIZ-181594, one specimen 6 mm preserved, Philippines, Bohol Island, Panglao, Pontog Lagoon I, reef wall with small caves, coll: T.M. Gosliner, Y. Camacho, J. Templado, M. Malaquias, M. Poddubetskaia, 2 Jul 2004, Panglao Expedition 2004, 17–25 meters, orig. fixative 95% EtOH. CASIZ-177264, one specimen, Philippines, Luzon Island, Batangas Province, Tingloy, Caban Island, Layaglayag, coll: T. Gosliner, A. Valdés, M. Pola, L. Witzel, B. Moore, A. Alejandrino, 16 Mar 2008. Comparative material of Glossodoris pallida (Figs. 1D–1E): CASIZ-173393, one specimen, dissected, 9 mm preserved, Madagascar, Iles Radama, Nosy Valiha, W of Nosy Valiha, coll: T.M. Gosliner, 20 Oct 2005, 12– 13 m, orig. fixative Bouin’s solution. CASIZ-173395, one specimen, dissected, 9 mm preserved, Madagascar, Iles Radama, Nosy Kalakajoro, West of Nosy Kalakajoro and Nosy Beratia, coll: T.M. Gosliner, 19 Oct 2005, 13– 15 m, orig. fixative Bouin’s solution. CASIZ-176997, one specimen, 14.5 mm preserved, Mozambique, Inhambane Province, Jangamo, Pandane Beach, coll: M. Pola and J. Reis, 6 Feb 2008, 1.5 meters, orig. fixative 95% EtOH. CASIZ-175548, one specimen 4 mm preserved (large portion missing from tissue sample), Madagascar, Iles Radama, Nosy Kalakajoro, coll: S. Fahey and T. M. Gosliner, 13 Oct 2005, CAS-WCS Radama Islands Expedition, 15-20 meters, orig. fixative 95% EtOH. CASIZ-194338, one specimen, dissected, 6 mm preserved, Madagascar, South Madagascar, “Pointe Evatra, crique fond rocheux et gazon d’algues”, coll. South Madagascar Expedition, 30 Apr 2006 – May 2010, 3–8 meters, orig. fixative 95% EtOH. CASIZ-175554, one specimen, dissected, 2 mm preserved, Madagascar, Iles Radama, Nosy Faly, NW of Nosy Faly, coll: S. Fahey and T.M. Gosliner, CAS-WCS Radama Islands Expedition, 13–16 meters, orig. fixative 95% EtOH. Etymology. The name Glossodoris buko comes from buko (young coconut) owing to the resemblance of this species to the cream-colored coconut meat from the Philippines, where this species is found. Geographical Distribution. Specimens identified by Matsuda & Gosliner (2017) range from the Philippines to Papua New Guinea and Australia (Turner & Wilson 2008). External Morphology. Glossodoris buko has a long and slender body that is transparent white in color (Fig. 1A–C). There is an opaque white band that starts anteriorly on the mantle, narrows between the rhinophores and then widens again and narrows between the two major folds in the middle of the mantle, and ends circling the gills (Fig. 2A). In most specimens, the band is continuous, however there was a break in the band posterior to the rhinophores in some. A white opaque band runs the length of the foot on both sides and connects posteriorly. The mantle edge is rippled with the semi-permanent undulations that are characteristic of all Glossodoris. One primary pair of undulations midway on the mantle is identifiable by an indentation of the white dorsal band. A thin, light yellow marginal band runs the length of the outer edge of the mantle and opaque white mantle dermal formations that appear as a thick white band that lies partly under the yellow band. The degree and number of the smaller semi-permanent undulations varies between individuals, but larger specimens have more pronounced undulations. A yellow band borders the foot, however no white band is visible due to the absence of mantle dermal formations. The rhinophores are elongate and conical with 11–12 lamellae. The bases of the rhinophores are white and the tips are yellow. The gill forms a semicircle surrounding the anus opening posteriorly, consisting of approximately 5–8 unipinnate branches. The lamellae are white with yellow tips and are shorter at the ends of the arc. The genital pore is located on the right side of the body below the mantle and behind the rhinophores. Internal Anatomy. Radula and buccal armature (Fig. 3A–E). The radular ribbon (Fig. 3E) is short and wide with a radula formula for a preserved specimen of 3 mm of approximately 28 x 14.1.14 (CASIZ- 191102 A) and 13.1.13 for a 6.5 mm preserved specimen (CASIZ-086381). The rachidian tooth (Fig. 3A) is very reduced and quasi-triangular. The first lateral tooth is almost bilaterally symmetrical. It is wide and has a relatively short triangular pointed central cusp. There are approximately five well-defined denticles, each about half the length of the central cusp, that point down and outward on the inner and outer sides of the central cusp. The mid-lateral teeth (Fig. 3B) are longer and have a shorter central cusp with approximately 6–8 loosely packed and well defined denticles solely on the outer edge. Unlike the first lateral, the central cusp on the mid-laterals is almost indistinguishable from the denticles next to it. The denticles in the mid-laterals are almost indistinguishable in size and shape from the central cusp, and maintain this shape and their size integrity to the edge of the ribbon (Fig. 3C). The jaw rodlets are short and well-spaced with distinct gaps between rodlets. They are predominantly bifid (Fig. 3D) with a few trifid rodlets. The ventral side of the buccal mass has a glandular sheath covering the oral tube that contains numerous densely packed white opaque glands (Fig. 4D). Reproductive system (Fig. 4C). The penial bulb is long and folded and leads to a coiled vas deferens followed by an approximately equal in length prostate gland. The receptaculum seminis duct and the vagina are relatively short. The receptaculum seminis is slightly smaller than the bursa copulatrix, and they are found adjacent to each other rather than being aligned linearly. Remarks. At first glance, G. buko and G. pallida could be easily confused, as there are few external morphological differences (Fig. 1; Rudman 1984: fig 1b; Gosliner et al. 2015: 237, upper right fig.; Matsuda & Gosliner 2017: fig. 1). The holotype of G. pallida was collected from the Red Sea and subsequently examined by Rudman (1984) together with a specimen from Tanzania. Both specimens share the same color pattern, radular structure and reproductive system morphology as the five specimens of G. pallida we comparatively examined here from Madagascar and Mozambique (Figs. 1D–F, 3F–J). In Rudman’s (1990) G. pallida description, he noted that specimens from East Australia have yellow gills and rhinophores, which are consistent with G. buko, whereas his Tanzania and Sudan specimens, the rhinophores and gills are white. However, he further remarks that yellow tips were reported from specimens in the Red Sea and Reunion Island, indicating that yellow tips may not be a consistent identifier for G. buko. The rhinophores and gills of our G. pallida specimens from Madagascar and Mozambique all have frosted yellow tips, although the yellow is not as bright as in the G. buko specimens. The most striking differences between the two species are found in the radula, jaws and buccal mass. The radular ribbon of G. pallida (Fig. 3J) is elongate (~ 85 x 23.1.23 CASIZ-173395), whereas it is short and squat in G. buko (Fig. 3E) (~ 28 x 14.1.14) for specimens of comparable size. This is confirmed in Rudman’s G. pallida specimen from the Red Sea (type locality), which has a radular formula of 108(+4) x 39.1.39 (15 mm specimen alive) and 23.1.23 for his Australian specimen (9 mm preserved) (Rudman 1984), and while no length was reported, the number of lateral teeth and presence of a rachidian tooth suggest that this specimen is likely G. buko. Glossodoris pallida has a more prominent and pointed rachidian tooth (Fig. 3F), whereas the rachidians are significantly reduced and amorphous in G. buko. There are also significant dissimilarities in the lateral teeth. The East African G. pallida specimens examined here share the same lateral tooth structure as Rudman’s Red Sea specimen (1984), with a long narrow hook-shaped central cusp with well-defined short denticles resting flat against the outer edge (Fig. 3G, H). Glossodoris buko has a lateral tooth that is broad and concave with a central cusp that is almost indistinguishable from the denticles in size and shape that shares no similarities with G. pallida. These differences are also visible in the jaw. Glossodoris pallida’ s rodlets are long, curved, and tightly packed with bifid tips where one of the points protrudes from slightly below the adjacent rodlet (Fig. 3I). Glossodoris buko has short and loosely packed rodlets that are less consistent in shape (Fig. 3D). Finally, the large glandular sheath on the ventral side of the buccal mass in G. buko (Fig. 4D) is not present in G. pallida (Fig. 4B). The reproductive system appears similar to the description by Rudman (1983) for G. pallida from Tanzania and the Red Sea and examined here from Madagascar (Fig. 4A). The only noteworthy distinction in the reproductive systems of the two species is that the ejaculatory portion of the vas deferens of G. pallida (Fig. 4A) contains many more convolutions than does that of G. buko (Fig. 4C). Glossodoris buko is distinct from G. pallida in both internal morphology as shown here, and based on molecular analyses (Matsuda & Gosliner 2017). This distinction is also maintained geographically. Glossodoris pallida has only been recorded off the coast of eastern Africa and the Red Sea, and G. buko is solely from the western Pacific. Matsuda & Gosliner’s (2017) phylogeny of Glossodoris provides support for the splitting of the previously hypothesized Glossodoris pallida into two distinct species. This is further supported through p-distance values (Matsuda & Gosliner 2017). Within G. buko, a grade and one clade are supported (a grade from the Philippines and a clade from Australia and Papua New Guinea). However, there were no observed morphological differences and only a 5–6% p-distance between them and these were not recovered as distinct lineages in the ABGD analysis conducted by Matsuda and Gosliner (Fig. 5). This strongly supports that the western Pacific specimens represent a single species distinct from the Indian Ocean specimens (Matsuda & Gosliner 2017).Published as part of Matsuda, Shayle B. & Gosliner, Terrence M., 2018, Glossing over cryptic species: Descriptions of four new species of Glossodoris and three new species of Doriprismatica (Nudibranchia: Chromodorididae), pp. 501-529 in Zootaxa 4444 (5) on pages 503-508, DOI: 10.11646/zootaxa.4444.5.1, http://zenodo.org/record/143722
Letter, [Author unclear] to Paulina T. Merritt
Handwritten letter to Paulina Merritt from an unknown author, October 1, 1876.
Applicative Bidirectional Programming with Lenses
A bidirectional transformation is a pair of mappings between source and view data objects, one in each direction. When the view is modified, the source is updated accordingly with respect to some laws. One way to reduce the development and maintenance effort of bidirectional transformations is to have specialized languages in which the resulting programs are bidirectional by construction---giving rise to the paradigm of bidirectional programming.
In this paper, we develop a framework for applicative-style and higher-order bidirectional programming, in which we can write bidirectional transformations as unidirectional programs in standard functional languages, opening up access to the bundle of language features previously only available to conventional unidirectional languages. Our framework essentially bridges two very different approaches of bidirectional programming, namely the lens framework and Voigtlander’s semantic bidirectionalization, creating a new programming style that is able to bag benefits from both
Movie data: Resident Autonomous Underwater Vehicle: Underwater System for Prolonged and Continuous Monitoring Based at a Seafloor Station
These movies show the experiments in sea and tank environments
Data of each figures: Resident Autonomous Underwater Vehicle: Underwater System for Prolonged and Continuous Monitoring Based at a Seafloor Station
These are each figure's data. The file name shows information of data
Enhancing Semantic Bidirectionalization via Shape Bidirectionalizer Plug-ins
Matsuda et al. (2007) and Voigtlander (2009) have introduced two techniques that given a source-to-view function provide an update propagation function mapping an original source and an updated view back to an updated source, subject to standard consistency conditions. Previously, we developed a synthesis of the two techniques, based on a separation of shape and content aspects (Voigtlander et al. 2010). Here, we carry that idea further, reworking the technique of Voigtlander such that any shape bidirectionalizer (based on the work of Matsuda et al. or not) can be used as a plug-in, to good effect. We also provide a data-type-generic account, enabling wider reuse, including the use of
pluggable bidirectionalization itself as a plug-in
Model of superconducting vortices in layered materials for the interpretation of transmission electron microscopy images
More realistic simulations of the magnetic field and electron optical phase shift associated to pancake vortices in layered high-T-c superconducting specimen require a number of layers larger than 7, the practical upper limit set by the discrete algebraic approach followed so far. This goal can be achieved by resorting to a continuum approximation of the screening layers above and below the one containing the pancake vortex. It is thus possible to increase the number of layers and to investigate more exotic vortex core structures than those represented by the pancakes pinned at tilted columnar defects. In particular it will be shown how recently observed dumbbell-like contrast features in the out-of-focus images of superconducting vortices forming a large angle with the specimen surfaces can be interpreted as due to a kinked structure of the pancakes
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