Nova espécie do gênero Galissus Dupont (Coleoptera, Cerambycidae) e chave para identificação das espécies

Galissus nigrescens sp. nov. é descrita da Costa Rica (Veragua Rainforest Reserve, Brisas de Veragua, Liverpool, Limón) e é fornecida chave para identificação das espécies.

Morphological analysis of Mecosarthron Buquet and Xixuthrus Thomson and Reevaluation of Generic Assignment of Xixuthrus domingoensis Fisher (Coleoptera, Cerambycidae, Prioninae)

The characters defining Mecosarthron Buquet, 1840 and Xixuthrus Thomson 1864 are discussed, along with a historical review of the literature that described and classified these taxa. Through morphological examination of these genera and most of the included species, we addressed the systematic placement of Xixuthrus domingoensis Fisher, 1932 that was placed in Mecosarthron by Ivie (1985). We restore its placement in the genus Xixuthrus. The first description of the female of X. domingoensis is provided, along with comparative redescriptions of Mecosarthron gounellei (Lameere, 1903), and M. buphagus Buquet, 1840. We include a key to the species currently in Mecosarthron.

Contribuição para o estudo dos Rhinotragini (Coleoptera, Cerambycidae). VI. Ecliptoides Tavakilian & Peñaherrera-Leiva, 2005

The genus Ecliptoides Tavakilian & Peñaherrera-Leiva, 2005, recently revised by Clarke (2009) to include three Bolivian species, is brought up-to-date by the inclusion of further South American species transferred from Eclipta Bates, 1873, and Odontocera Audinet-Serville, 1833. Three new species are described from Brazil: E. schmidi, E. tavakiliani, and E. hogani. Ommata eunomia var. rufula Melzer, 1934, and Ommata (Eclipta) plaumanni Fuchs, 1961, are revalidated and considered species of Ecliptoides. Species transferred from Eclipta to include Ecliptoides: E. bivitticollis (Fisher, 1952); E. eunomia (Newman, 1841); E. pilosipes (Peñaherrera-Leiva & Tavakilian, 2004); E. fanchonae (Tavakilian & Peñaherrera-Leiva, 2003); E. giuglarisi (Peñaherrera-Leiva & Tavakilian, 2004); E. vasconezi (Peñaherrera-Leiva & Tavakilian, 2004); E. vicina (Melzer, 1927); E. lauraceae (Peñaherrera-Leiva & Tavakilian, 2004); and E. bauhiniae (Peñaherrera-Leiva & Tavakilian, 2004). Species transferred from Odontocera to include Ecliptoides: O. quadrivittata Melzer, 1922; O. pusilla Gounelle, 1911; and O. monostigma (Bates, 1869). New synonymy: Ommata (Eclipta) collarti Fuchs, 1959 = Odontocera pusilla Gounelle, 1911 (= Ecliptoides pusillus). Lectotypes are designated for Ommata (Eclipta) vicina, and Ommata (Eclipta) collarti. New distribution records are provided for E. eunomia, E. pilosipes, E. plaumanni and E. fanchonae. A key to the species of Ecliptoides is given.

Contribuição para o estudo dos Rhinotragini (Coleoptera, Cerambycidae).VII. O gênero Ischasioides

Eclipta brasiliensis (Fisher, 1947) is transferred to Ischasioides Tavakilian & Peñaherrera-Leiva, 2003, and synonymized with I. crassitarsis (Gounelle, 1911). Ischasia m. atrocephala Fuchs, 1956 and Ischasia m. nigrovittata Fuchs, 1956, although without nomenclatural status, are confirmed as equal to I. crassitarsis. Ischasioides berkovae sp. nov. is described from Brazil. A key to the species of Ischasioides is provided.

Trypanosoma livingstonei: a new species from African bats supports the bat seeding hypothesis for the Trypanosoma cruzi clade

BACKGROUND: Bat trypanosomes have been implicated in the evolutionary history of the T. cruzi clade, which comprises species from a wide geographic and host range in South America, Africa and Europe, including bat-restricted species and the generalist agents of human American trypanosomosis T. cruzi and T. rangeli. METHODS: Trypanosomes from bats (Rhinolophus landeri and Hipposideros caffer) captured in Mozambique, southeast Africa, were isolated by hemoculture. Barcoding was carried out through the V7V8 region of Small Subunit (SSU) rRNA and Fluorescent Fragment Length barcoding (FFLB). Phylogenetic inferences were based on SSU rRNA, glyceraldehyde phosphate dehydrogenase (gGAPDH) and Spliced Leader (SL) genes. Morphological characterization included light, scanning and transmission electron microscopy. RESULTS: New trypanosomes from bats clustered together forming a clade basal to a larger assemblage called the T. cruzi clade. Barcoding, phylogenetic analyses and genetic distances based on SSU rRNA and gGAPDH supported these trypanosomes as a new species, which we named Trypanosoma livingstonei n. sp. The large and highly polymorphic SL gene repeats of this species showed a copy of the 5S ribosomal RNA into the intergenic region. Unique morphological (large and broad blood trypomastigotes compatible to species of the subgenus Megatrypanum and cultures showing highly pleomorphic epimastigotes and long and slender trypomastigotes) and ultrastructural (cytostome and reservosomes) features and growth behaviour (when co-cultivated with HeLa cells at 37°C differentiated into trypomastigotes resembling the blood forms and do not invaded the cells) complemented the description of this species. CONCLUSION: Phylogenetic inferences supported the hypothesis that Trypanosoma livingstonei n. sp. diverged from a common ancestral bat trypanosome that evolved exclusively in Chiroptera or switched at independent opportunities to mammals of several orders forming the clade T. cruzi, hence, providing further support for the bat seeding hypothesis to explain the origin of T. cruzi and T. rangeli.

Application of 137Cs and 210Pb radionuclides to determine sedimentation rates of recent sediments from admiraty Bay, Antarctica Peninsula

Studies about natural and artificial radionuclides in areas such as the Antarctic are key to understand natural and dynamic processes in marine environments. These studies are important to determine levels of radioactive elements and local sedimentation rates. Five marine sediment cores were collected in different points of Admiralty Bay, in the Antarctic Peninsula. The purpose of this study was to determine 137Cs, 226Ra and 210Pb and sedimentation rates at each site. 137Cs, 210Pb and 226Ra were assayed by gamma-counting through direct measurement of the peak at 661 keV, 47 keV and 609 keV, respectively. Sedimentation rates were obtained by 137Cs and 210Pb (CIC and CRS). The activities for 137Cs ranged from 0.84 to 7.09 Bq kg-1; to 226Ra from 6.77 to 31.07 Bq kg-1 and for 210Pb ranged from 1.10 to 36.90 Bq kg-1. The sedimentation rates obtained by the three models ranged from 0.11±0.01 cm y-1 to 0.46±0.05 cm y-1. The levels of 137Cs registered in this study, as well as in other studies in the Antarctic region indicate that global fallout is the main cause of artificial radionuclides present in this environment, since the Antarctic has not suffered a direct action of human activities that released radioactive elements. The possible grain size variations that occur in the studied points of Admiralty Bay may explain the differences found in the vertical distribution of radionuclides, because of the different values of sedimentation rates and respective dating determined in their profiles