50 research outputs found
Lambertus Parvus - Vita Agritii ep. Treverensis
No full textLAMBERTUS PARVUS - VITA AGRITII EP. TREVERENSIS
Lambertus Parvus - Vita Agritii ep. Treverensis ( - )
Cover ( - )
Blank page (1r)
Lambertus : Vita, inventiones, miracula Matthiae apost. (2r)
Vita Agritii ep. Treverensis, Ausz. (8v)
Inventiones Matthiae apost. Treveri et miracula saeculi XII., Ausz. (12r)
Miracula Matthiae apost. (unvollst.) (14r)
Blank page ( - )
Grey chart ( - )
Cover ( -
Lambertus Parvus et Reinerus Sancti Jacobi Leodiensis, Chronicon Leodiense. - Vita Balderici episcopi Leodiensis.
No full textReliure moderne en cuir brun clair attribuable à l’atelier de Dubois d’Enghien à Bruxelles, couvrure en veau fauve sur ais de bois ornée de filets et de deux fers.Provenance : abbaye de Saint-Jacques de Liège.Ff. 1r°-48v° : Lambertus Parvus et Reinerus Sancti Jacobi Leodiensis, Chronicon Leodiense ; ff. 49r°-64v° : Vita Balderici episcopi Leodiensis.Fédération Wallonie-Bruxelles (plan PEP'S
Monoschelobates parvus Balogh and Mahunka 1969
No full textMonoschelobates parvus Balogh and Mahunka, 1969 (Figure 3) Diagnosis — Body size: 282 – 315 × 166 – 199. Rostrum rounded. Prodorsal setae long, setiform, barbed. Sensilli clavate, weakly barbed. Translamellar line represented by rudimentary parts. Prolamellar lines present. Notogaster with ten pairs of short setae. Aggenital setae absent. Leg claws serrate on dorsal side. Description — Measurements. Body length: 282-315 (six specimens); notogaster width: 166-199 (six specimens). Integument — Body color light brown. Body surface smooth. Prodorsum — Rostrum rounded. Lamellae located dorso-laterally, as long as half of prodorsum (in lateral view), without cusps. Translamellar line represented by rudimentary parts near to lamellae. Prolamellar and sublamellar lines distinct. Sublamellar porose areas (Al) very small (2 – 4 × 1 – 2), oval. Rostral (28-32), lamellar (36-45) and interlamellar (61 – 65) setae setiform, barbed. Sensilli (53 – 65) clavate, with well dilated head, having small barbs. Exobothridial setae (2) minute. A pair of elongate, narrow porose areas present (visible in dissected specimens) latero-posterior to interlamellar setae. Notogaster — Anterior notogastral margin convex medially. Dorsophragmata small. Ten pairs of thin, smooth notogastral setae present; setae c and la (8) slightly longer than others (4 – 6). Four pairs of sacculi (Sa, S1, S2, S3) oval, with small openings. Epimeral and lateral podosomal regions — Apodemes 1, 2, 3 and sejugal apodemes distinct. Epimeral setal formula: 3-1-3-3. Setae setiform, thin, smooth; medial setae 1a, 2a, 3a (4) shorter than others (8 – 12). Pedotecta I large, convex, pedotecta II rounded anteriorly. Discidia rounded distally. Circumpedal carinae distinct. Anogenital region — Four pairs of genital (4), two pairs of anal (4) and three pairs of adanal (8 – 12) setae setiform, thin, smooth. Aggenital setae absent. Lyrifissures iad in paraanal position. Legs — Each claw with several minute barbs on dorsal side. Formulae of leg setation and solenidia: I (1-5-3-4-19) [1-2-2], II (1-5-2-4-15) [1-1-2], III (2-3- 1-3-15) [1-1-0], IV (1-2-2-3-12) [0-1-0]; homology of setae and solenidia indicated in Table 1. Material examined — Three specimens (two females and one male): Ec-1 (1.IV.2009, collected by F. Marian). Three specimens (one female and two males): Ec-1 (1.X.2008, collected by F. Marian). Remarks — Ecuadorian specimens of Monoschelobates parvus are similar in general appearance to Brazilian specimens (Balogh and Mahunka 1969; Balogh and Balogh 1990), but there is a clear difference: prolamellar lines present versus absent in Brazilian specimens. Sometimes presence or absence of prolamellar lines or their partial development can vary in specimens of one species in Scheloribatidae: for example, prolamellar lines in Scheloribates fimbriatus Thor, 1930 - present (see Subbotina 1978), developed partially (Mahunka 1987), indistinctly visible or absent (data of first author, based on specimens from Western Europe); similar situation is known for Scheloribates (Bischeloribates) mahunkai Subías, 2010 (Ermilov 2013). Hence, we assume this difference to represent intraspecific variability in the case of M. parvus.Published as part of Ermilov, S. G., Sandmann, D., Marian, F. & Maraun, M., 2013, Perscheloribates Paratzitzikamaensis N. Sp., With Supplementary Descriptions Of Scheloribates Elegans And Monoschelobates Parvus (Acari, Oribatida, Scheloribatidae) From Ecuador, pp. 429-437 in Acarologia 53 (4) on pages 434-436, DOI: 10.1051/acarologia/20132104, http://zenodo.org/record/463996
SEASONAL CHANGES IN BODY SIZE AND OIL SAC VOLUME OF THREE PLANKTONIC COPEPODS, PARACALANUS PARVUS (CLAUS, 1863), PSEUDOCALANUS NEWMANI FROST, 1989 AND OITHONA SIMILIS CLAUS, 1866, IN A TEMPERATE EMBAYMENT: WHAT CONTROLS THEIR SEASONALITY?
No full textSeasonal changes in body size (prosome length: PL) and oil sac volume (OSV) of the three most numerically abundant copepods in Ishikari Bay, northern Sea of Japan, Paracalanus parvus (Claus, 1863), Pseudocalanus newmani Frost, 1989 and Oithona similis Claus, 1866, were studied using monthly samples collected through vertical hauls of a 100-mu m mesh NORPAC net from March, 2001 to May, 2002. Seasonal changes in PL were common for the three species and were more pronounced during a cold spring. PL was negatively correlated with temperature, and this relationship was described well using the Belehradek equation. Seasonal changes in OSV exhibited a species-specific pattern, i.e., OSV was greater during a warm summer for P. parvus and was greater during a cold spring for P. newmani and O. similis. The OSV peak period corresponded with the optimal thermal season of each species. The relative OSV to prosome volume of the small copepods (0.6-0.8%) was substantially lower than that of the large copepods (20-32%). These facts suggest that the oil sac of small copepods is not used for overwintering or diapauses or during periods of food scarcity, but is instead used as the primary energy source for reproduction, which occurs during the optimum thermal season of each species
Evaluation of the tardus-parvus pattern in patients with atherosclerotic and nonatherosclerotic renal artery stenosis
No full textObjective. The aim of this study was to evaluate the differences in the tardus-parvus pattern between atherosclerotic and nonatherosclerotic renal artery stenosis (RAS) and to explore the causes of these differences. Methods. In 81 patients, including a nonatherosclerotic group (29 cases of Takayasu arteritis and 22 cases of fibromuscular dysplasia) and an atherosclerotic group (n = 30), RAS was detected by color Doppler sonography and confirmed by renal arteriography. Doppler spectra were obtained at the upper, middle, and lower pole interlobar arteries, and the one with the most prolonged acceleration time (AT) was selected for recording the AT and resistive index (RI). Results. Renal angiography revealed 16 moderate RASs, 80 severe RASs, and 15 occlusions. No statistically significant differences were found in the AT between the atherosclerotic and nonatherosclerotic groups in the mild (P = .24), moderate (P = .63), and severe stenotic (P = .41) subgroups; however, there were statistically significant differences in the RI between the atherosclerotic and nonatherosclerotic groups in the mild (P < .001), moderate (P < .01), and severe (P < .001) subgroups. The RI values in the atherosclerotic group were much higher than those in the nonatherosclerotic group for the 3 stenotic subgroups. Conclusions. The AT measurement method used widely now cannot differentiate potential differences in pulsus-tardus waveforms between atherosclerotic and nonatherosclerotic RAS; however, it remains a useful approach to detect RAS. Different RI cutoff values should be established according to atherosclerotic and nonatherosclerotic RAS, and consideration of influencing factors for the RI will help reduce misdiagnosis.http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000245166400001&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701AcousticsRadiology, Nuclear Medicine & Medical ImagingSCI(E)EI5ARTICLE4419-4262
Additional file 1: of Conservation of genetic uniqueness of populations may increase extinction likelihood of endangered species: the case of Australian mammals
No full textAdditional information including microsatellite simulations exploring the relationship between genetic diversity and population-specific F ST (Appendix S1), a figure showing results of the simulations on population-specific F ST and genetic diversity along with regressions on observed data (Appendix S2), a table presenting observed and simulated regressions statistics for Fig. 1 and Appendix S2 (Appendix S3), a table on EPBC listed terrestrial mammal species and summary information (Appendix S4), extinction risk of populations of P. gunnii and B. parvus (Appendix S5), and a figure presenting extinction risk for populations of P. gunnii and B. parvus (Appendix S6) are available online. The authors are solely responsible for the content and functionality of these materials. Queries (other than absence of the material) should be directed to the corresponding author. (DOCX 569 kb
Pleistocene History and Molluscan Paleoecology of the Winameg Mastodon Site, Fulton County, OH
No full textAuthor Institution: Department of Geology, University of ToledoThe discovery of a mastodon skeleton in Fulton County, Ohio provided an opportunity to study the molluscan fauna and Late Wisconsinan history of this area. After the deposition of Lake Maumee sediments, a series of ponds developed in a beach ridge of Lake Maumee II, later to be filled in with sediments and vegetation. Eleven stratigraphic sections taken from a site in the village of Winameg exposed a lens-shaped deposit of shell marl capped by humus. Seventeen species of mollusks including four ctenobranchs, 10 aquatic pulmonates and 3 sphaeriids were recovered from the marl. During the early stages of the pond, Valvata tricarinata, Fossaria obrussa decampi, Gyraulus parvus, Helisoma anceps, and Pisidium casertanum were the dominant species. Fossaria obrussa decampi, Gyraulus parvus, Pbysella gyrina, and sphaeriids were probably the significant species in the late stages of pond succession due to the ephemeral nature of the small water body
Atmospheric methane removal by methane-oxidizing bacteria immobilized on porous building materials
No full textBiological treatment using Methane Oxidizing Bacteria (MOB) immobilized on carrier materials is considered as the best solution to mitigate methane emission at low concentrations (e.g., in animal houses). The porosity of the support is one of the most important factors for an efficient removal of methane. In animal houses, building materials having a high porosity may provide a niche for MOB. In this study, we evaluated the methane removal capacity of MOB immobilized on porous building materials.
Six different types of building materials and MOB were chosen for the experiments. Building materials were immersed in an MOB liquid culture (2.108 cells/ml) and after 24 hours the liquid were separated. The methane removal capacity of MOB was investigated by analyizing the evolution of the methane concentration in the headspace of a closed incubator containing the materials at starting concentrations of ~20 %(v/v) and ~50 ppmv.
MOB immobilized on Maastricht limestone and Ytong exhibited higher methane removal rates compared to when immobilized in other materials with M. parvus NCIMB 11129T in Maastricht limestone (0.1 mg CH4 (m3air h)-1) exhibited the highest rate at ~50 ppmv and M. trichosporium NCIMB 11131T in Maastricht limestone (1451 mg CH4 (m3air h)-1) at ~20 %(v/v). Both materials exhibited the highest macropores (i.e., pore diameter > 3 μm) volume. Therefore, they were likely to accommodate more bacteria and consequently higher methane removal rate by the MOB. M. parvus and M. trichosporium were able to remove methane for two months with decreasing activity. From this study it was shown that methane can be efficiently removed from the air by MOB immobilized on building materials
[[alternative]]Non-geniculate Coralline Algae from the Hengchun Limestone of ill
No full text[[abstract]]在岩石薄片下，依據植物體外表形態、葉狀體內部構造及生殖構造之 臺
地恆春石灰岩所產紅藻球中之無節珊瑚藻化石作分類研allinaceae和
Sporolithaceae二科，Corallinaceae中之e、Mastophoroideae和
Lithophylloideae三亞科，共七屬堙GSporolithon ptychoides，
Mesophyllum erubescens，urpurascens，Mesophyllum mesomorphum，
LithothamnionALithothamnion pulchrum，Lithothamnion johnsoni，
maemongense，Lithoporella parvus，Lithoporella，Hydrolithon
reinboldii，Hydrolithon laeve，Titan-，Lithophyllum kotschyanum
，Lithophyllum insipidum，sp. cf. quadratum，和Hydrolithon sp.，
Lithophyllum。每一個紅藻球中無節珊瑚藻化石出現之情形多有變化；每
L節珊瑚藻化石種屬組合不同，造成這些現象之原因尚不明i一步的加以研
究。
Permian-Triassic conodonts from Dajiang (Guizhou, South China) and their implication for the age of microbialite deposition in the aftermath of the End-Permian mass extinction
No full textThe widespread microbialites deposition that followed the End-Permian mass extinction in the Tethyan realm have been intensively studied because of the evidence they provide on the nature of this crisis and its aftermath. However, the age of the microbialite event remains controversial. New conodont collection across the Permian-Triassic (P-T) transition from Dajiang (Guizhou Province, South China) in this study enable us to discriminate four conodont zones, in ascending order, they are: Hindeodus parvus zone, Isarcicella lobata zone, Isarcicella isarcica zone and Hindeodus sosioensis zone. The age of microbialite in the P-T transition at the Dajiang Section is considered to be within the Hindeodus parvus zone and thus to clearly post-date the main extinction crisis. Reviewing the age of onset of microbialites throughout the Tethyan regions reveals two different ages: a Hindeodus changxingensis zone age is dominant in south-western and westernmost Tethys, whilst most other regions show microbialite deposition began in the Hindeodus parvus zone. Our investigation also indicates that two conodont changes occur at this time: an increase of hindeodid species immediately following a sequence boundary and the mass extinction, and a phase of extinction losses in the earliest Triassic Isarcicella isarcica zone during highstand developmen
