86,618 research outputs found
Elaphroptera montifacies Genise & Kimsey 1993
Elaphroptera montifacies Genise & Kimsey, 1993: 209 Paratypes: 1♂ (# MZSP 57214) ‘ Brazil, Santa Catarina, Nova Teutônia, ix.1964, Fritz Plaumann [col]’ ‘ Paratype Elaphroptera montifacies Genise & Kimsey’; 1♂ (# MZSP 57215) same data except ‘11.[19]66 ’.Published as part of Andrade, Tamires de O., Ramos, Kelli S., Onody, Helena C., dos Santos, Alvaro D. & Brandão, Carlos Roberto F., 2018, Type specimens of Pompiloidea, Thynnoidea and Vespoidea (Hymenoptera) deposited in the Museu de Zoologia da Universidade de São Paulo, Brazil, pp. 1-21 in Papéis Avulsos de Zoologia 58 on page 8, DOI: 10.11606/1807-0205/2018.58.39, http://zenodo.org/record/461350
The Brood Ball of Canthon (Canthon) Lituratus Germar (Coleoptera: Scarabaeidae: Scarabaeinae) and Its Fossil Counterpart Coprinisphaera cotiae Sánchez and Genise New Ichnospecies, with a Brief Review of South American Fossil Brood Balls
The brood ball of Canthon (Canthon) lituratus Germar is an elongated ovoid covered by a thin lining of soil and dung fibers. The provision is mostly composed of dung and scattered flakes of organic matter. The egg chamber, which is located in the upper part of the provision, shows no evidence of lining and is connected to the exterior through an elongated aeration conduit. This conduit, which acts as a filter, is filled with interlaced dung fibers. These brood ball features are compared with those reported for several coprophagous species of Canthon Hoffmansegg. The brood ball of C. lituratus is also compared with a similar new fossil brood ball from the Cenozoic of Patagonia: Coprinisphaera cotiae Sánchez and Genise, new ichnospecies. A brief review of South American fossil brood balls in the ichnogenera Coprinisphaera Sauer and Quirogaichnus Laza is also provided with illustrations of the types.Fil: Sánchez, María Victoria. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales "Bernardino Rivadavia"; ArgentinaFil: Genise, Jorge Fernando. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales "Bernardino Rivadavia"; Argentin
Glottynoides genisei Kimsey, 1991: 61 in Genise & Kimsey 1991
Glottynoides genisei Kimsey, 1991: 61 in Genise & Kimsey, 1991 Paratype: 1♂ (# MZSP 56880) ‘Argent[ina], Cordoba, Carlos Paz – Capilla del monte, 26.Feb.[19]66, C.C. Porter’ ‘ Paratype Glottynoides genisei L.S. Kimsey’.Published as part of Andrade, Tamires de O., Ramos, Kelli S., Onody, Helena C., dos Santos, Alvaro D. & Brandão, Carlos Roberto F., 2018, Type specimens of Pompiloidea, Thynnoidea and Vespoidea (Hymenoptera) deposited in the Museu de Zoologia da Universidade de São Paulo, Brazil, pp. 1-21 in Papéis Avulsos de Zoologia 58 on page 8, DOI: 10.11606/1807-0205/2018.58.39, http://zenodo.org/record/461350
Fig. 3 in Plasticity in the Nesting Behavior of Ontherus sulcator (Fabricius) (Coleoptera: Scarabaeidae: Scarabaeinae)
Fig. 3. Schematic drawings of Ontherus sulcator nests. A) Brood ball within a nesting chamber, 14 cm deep in the soil, and a short nearby storage burrow not connected to the soil surface or to the nesting chamber, B) Brood ball within a nesting chamber, 12 cm deep in the soil, and a long nearby storage burrow not connected to the soil surface or to the nesting chamber. Scale bars = 1.5 cm.Published as part of González-Vainer, Patricia, Cantil, Liliana F. & Genise, Jorge F., 2018, Plasticity in the Nesting Behavior of Ontherus sulcator (Fabricius) (Coleoptera: Scarabaeidae: Scarabaeinae), pp. 203-208 in The Coleopterists Bulletin 72 (1) on page 206, DOI: 10.1649/0010-065X-72.1.203, http://zenodo.org/record/538121
The Pupation Chamber of Dung Beetles (Coleoptera: Scarabaeidae: Scarabaeinae)
Sánchez, M. V., Krause, J. M., González, M. G., Dinghi, P. A., Genise, J. F. (2010): The Pupation Chamber of Dung Beetles (Coleoptera: Scarabaeidae: Scarabaeinae). The Coleopterists Bulletin 64 (3): 277-284, DOI: 10.1649/0010-065x-64.3.277.17, URL: http://dx.doi.org/10.1649/0010-065x-64.3.277.1
Citologia per agoaspirazione e riscontro istologico postoperatorio in 67 pazienti con nodulo tiroideo ipocaptante.
Predation of Soil-Nesting Centris muralis (Insecta: Apidae) by Armadillos (Zaedyus pichiy) (Mammalia: Cingulata) in La Rioja Province, Northwestern Argentina
This paper documents the predation of Centris muralis by Zaedyus pichiy. It presents the first detailed observations of the predation of solitary bee nests by a mammal in soils and reports the alternative use of soil mounds as a nesting site by Centris muralis.Fil: Sarzetti, Laura Cristina. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”; ArgentinaFil: Genise, Jorge Fernando. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”; Argentin
Escaping the Phagocytic Oxidative Burst: The Role of SODB in the Survival of Pseudomonas aeruginosa Within Macrophages
Reactive oxygen species (ROS) are small oxygen-derived molecules that are used to control infections by phagocytic cells. In macrophages, the oxidative burst produced by the NOX2 NADPH-oxidase is essential to eradicate engulfed pathogens by both oxidative and non-oxidative killing. Indeed, while the superoxide anion (O2-) produced by NOX2, and the other ROS derived from its transformation, can directly target pathogens, ROS also contribute to activation of non-oxidative microbicidal effectors. The response of pathogens to the phagocytic oxidative burst includes the expression of different enzymes that target ROS to reduce their toxicity. Superoxide dismutases (SODs) are the primary scavengers of O2-, which is transformed into H2O2. In the Gram-negative Salmonella typhimurium, periplasmic SODCI has a major role in bacterial resistance to NOX-mediated oxidative stress. In Pseudomonas aeruginosa, the two periplasmic SODs, SODB, and SODM, appear to contribute to bacterial virulence in small-animal models. Furthermore, NOX2 oxidative stress is essential to restrict P. aeruginosa survival in macrophages early after infection. Here, we focused on the role of P. aeruginosa SODs in the counteracting of the lethal effects of the macrophage oxidative burst. Through this study of the survival of sod mutants in macrophages and the measurement of ROS in infected macrophages, we have identified a dual, antagonistic, role for SODB in P. aeruginosa survival. Indeed, the survival of the sodB mutants, but not of the sodM mutants, was greater than that of the wild-type (WT) bacteria early after infection, and sodB-infected macrophages showed higher levels of O2- and lower levels of H2O2. This suggests that SODB contributes to the production of lethal doses of H2O2 within the phagosome. However, later on following infection, the sodB mutants survived less that the WT bacteria, which highlights the pro-survival role of SODB. We have explained this defensive role through an investigation of the activation of autophagy, which was greater in the sodB-infected macrophages
Traces within traces : holes, pits and galleries in walls and filling of insect trace fossils in paleosols
Fossil insect nests with constructed walls (ichnogenera Uruguay ROSELLI 1938, Palmiraichnus ROSELLI 1987, Rosellichnus GENISE and BOWN 1996), as well as fossil brood masses from dung beetles (Monesichnus ROSELLI 1987) often display pits or galleries made by inquilines, parasitoids, cleptoparasites and scavengers, which develop and/or feed inside them. Some of these "traces within traces" can be distinguished, using morphologic criteria, as separate ichnotaxa. Tombownichnus n. igen. is represented by circular to subcircular holes or paraboloid external pits occurring in discrete walls of chambers made of agglutinated soil material. T. plenus n. isp. consists of a complete perforation, mostly cylindrical in longitudinal section, which pierces whole thickness of the cell wall. Tombownichnus parabolicus n. isp. includes incomplete perforations, i.e. pits, parabolic, conic or subcylindrical in longitudinal section, on the external surface of the chamber wall. Lazaichnus fistulosus n. igen., n. isp. is composed of circular to subcircular holes occurring in constructed walls of chambers made of agglutinated soil material, which are connected to an internal gallery in their infillings. The trace fossils described herein may be the first formal records of this hitherto neglected but promising field of ichnologic research
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