1,008 research outputs found

    The C-terminal extension of the beta 7 subunit and activator complexes stabilize nascent 20 S proteasomes and promote their maturation

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    The eukaryotic 20 S proteasome is formed by dimerization of two precursor complexes containing the maturation factor Ump1. beta 7/Pre4 is the only one of the 14 subunits forming the 20 S proteasome that is absent from these precursor complexes in Saccharomyces cerevisiae. Increased expression of Pre4 leads to a reduction in the level of precursor complex, indicating that Pre4 incorporation into these complexes is rate-limiting for their dimerization. When we purified these precursor complexes, we observed co-purification of Blm10, a large protein known to attach to the alpha ring surface of proteasomes. In contrast to single mutants lacking either Blm10 or the C-terminal extension of Pre4, a mutant lacking both grew extremely poorly, accumulated very high levels of precursor complexes, and was impaired in beta subunit maturation. The effect of blm10 Delta on proteasome biogenesis is modest, apparently because the 19 S regulatory particle is capable of substituting for Blm10, as long as precursor complex dimers are stabilized by the Pre4Cterminus. We found that a mutation (sen3/rpn2) affecting the Rpn2 subunit inhibits attachment of the 19 S activator to the 20 S particle or its precursors. Although the sen3 mutation alone had no apparent effect on precursor complex dimerization and active site maturation, the sen3 blm10 double mutant was impaired in these processes. Together these data demonstrate that Blm10 and the 19 S activator have a partially redundant function in stabilizing nascent 20 S proteasomes and in promoting their activation.info:eu-repo/semantics/publishedVersio

    Cladistic analysis and new classification of the Family Tubulariidae (Hydrozoa, Anthomedusae)

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    O Gênero Eudendrium (Hydrozoa, Anthomedusae, Eudendriidae) no Brasil

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    Molecules Clarify a Cnidarian Life Cycle – The “Hydrozoan” Microhydrula limopsicola Is an Early Life Stage of the Staurozoan Haliclystus antarcticus

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    Background: Life cycles of medusozoan cnidarians vary widely, and have been difficult to document, especially in the most recently proposed class Staurozoa. However, molecular data can be a useful tool to elucidate medusozoan life cycles by tying together different life history stages. Methodology/Principal Findings: Genetic data from fast-evolving molecular markers (mitochondrial 16S, nuclear ITS1, and nuclear ITS2) show that animals that were presumed to be a hydrozoan, Microhydrula limopsicola (Limnomedusae, Microhydrulidae), are actually an early stage of the life cycle of the staurozoan Haliclystus antarcticus (Stauromedusae, Lucernariidae). Conclusions/Significance: Similarity between the haplotypes of three markers of Microhydrula limopsicola and Haliclystus antarcticus settles the identity of these taxa, expanding our understanding of the staurozoan life cycle, which was thought to be more straightforward and simple. A synthetic discussion of prior observations makes sense of the morphological, histological and behavioral similarities/congruence between Microhydrula and Haliclystus. The consequences are likely to be replicated in other medusozoan groups. For instance we hypothesize that other species of Microhydrulidae are likely to represent life stages of other species of Staurozoa.45Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)[2004/09961-4]Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)[55.7333/2005-9]Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)[490348/2006-8]Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)[305735/2006-3]Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)[474672/2007-7]National Science Foundation (NSF) [0531779

    Podocoryna tenuis (Hydrozoa) en aguas templadas del Atlántico Sudoccidental: datos adicionales sobre las etapas del ciclo de vida respaldan su sinónimo con Podocoryna humilis

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    Two species of Hydractiniidae (Hydrozoa) with metagenetic life cycle have been recorded for the temperate region of the southwestern Atlantic Ocean: the medusa stage of Podocoryna tenuis and the polyp stage of P. humilis. Both the adult medusa of P. humilis and the polyp stage of P. tenuis are unknown, but it is possible that they are different stages of the same species, a hypothesis still to be tested. Colonies of P. humilis growing on the southern king crab Lithodes santolla collected at the Atlantic Patagonian coast, and two small medusae released from these hydroid colonies were analyzed. Medusa of P. humilis were kept alive for 3 days and they were morphologically compared with the medusae of P. tenuis sorted out from ~ 2,500 plankton samples along the Atlantic Patagonian coast. The study of these specimens allowed reassessing the taxonomic status of P. humilis and P. tenuis from the southwestern Atlantic Ocean. Polyp and young medusa stages of P. humilis were described, and additional information was recovered to better describe the medusa stage of P. tenuis. New morphologic and biogeographic evidences in order to propose the synonymy between P. tenuis and P. humilis were discussed.Se han registrado dos especies de Hydractiniidae (Hydrozoa) con ciclo de vida metagenético para la región templada del suroeste del Océano Atlántico: la etapa de medusa de Podocoryna tenuis y la etapa de pólipo de P. humilis. Tanto la medusa adulta de P. humilis como el estadio de pólipo de P. tenuis son desconocidos, pero es posible que se trate de diferentes estadios de una misma especie, hipótesis aún por contrastar. Se analizaron colonias de P. humilis que crecían sobre la centolla Lithodes santolla recolectadas en la costa atlántica de la Patagonia, y dos pequeñas medusas liberadas de estas colonias de hidroides. Las medusas de P. humilis se mantuvieron vivas durante 3 días y se compararon morfológicamente con las medusas de P. tenuis seleccionadas de ~ 2.500 muestras de plancton a lo largo de la costa atlántica patagónica. El estudio de estos especímenes nos permitió reevaluar el estado taxonómico de P. humilis y P. tenuis del Océano Atlántico Sudoccidental. Se describen las etapas de pólipo y medusa joven de P. humilis, y se recuperó información adicional para describir mejor la etapa de medusa de P. tenuis. Se discuten las nuevas evidencias morfológicas y biogeográficas para proponer la sinonimia entre P. tenuis y P. humilis

    The taxonomic position of the pelagic 'staurozoan' Tessera gemmaria as a ceriantharian larva

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    Based on 16 specimens from the Southwestern Atlantic coast (Argentina and Brazil) we reinterpret the taxonomic position of Tessera gemmaria Goy, 1979, a stauromedusa considered as incertae sedis for a long time. Using external morphology histological preparations and molecular data (16S and COI) we conclude that T. gemmaria is an early stage of a cerinula,the long-lived planktonic larval stage of the Ceriantharia (Anthozoa).Tessera gemmaria Goy, 1979, a stauromedusa considered as incertae sedis for a long time. Using external morphology histological preparations and molecular data (16S and COI) we conclude that T. gemmaria is an early stage of a cerinula,the long-lived planktonic larval stage of the Ceriantharia (Anthozoa).Fil: Rodriguez, Carolina Soledad. Universidad Nacional de Mar del Plata; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mar del Plata; ArgentinaFil: Marques, Antonio C.. Universidade de Sao Paulo; BrasilFil: Stampar, Sérgio N.. Universidade de Sao Paulo; BrasilFil: Morandini, André C.. Universidade de Sao Paulo; BrasilFil: Christiansen, Ernesto. Instituto Nacional de Investigaciones y Desarrollo Pesquero; ArgentinaFil: Genzano, Gabriel Nestor. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mar del Plata. Instituto de Investigaciones Marinas y Costeras. Universidad Nacional de Mar del Plata. Facultad de Ciencias Exactas y Naturales. Instituto de Investigaciones Marinas y Costeras; ArgentinaFil: Mianzan, Hermes Walter. Instituto Nacional de Investigaciones y Desarrollo Pesquero; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mar del Plata; Argentin

    Phylogenetics of Hydroidolina (Hydrozoa: Cnidaria)

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    Hydroidolina is a group of hydrozoans that includes Anthoathecata, Leptothecata and Siphonophorae. Previous phylogenetic analyses show strong support for Hydroidolina monophyly, but the relationships between and within its subgroups remain uncertain. In an effort to further clarify hydroidolinan relationships, we performed phylogenetic analyses on 97 hydroidolinan taxa, using DNA sequences from partial mitochondrial 16S rDNA, nearly complete nuclear 18S rDNA and nearly complete nuclear 28S rDNA. Our findings are consistent with previous analyses that support monophyly of Siphonophorae and Leptothecata and do not support monophyly of Anthoathecata nor its component subgroups, Filifera and Capitata. Instead, within Anthoathecata, we find support for four separate filiferan clades and two separate capitate clades (Aplanulata and Capitata sensu stricto). Our data however, lack any substantive support for discerning relationships between these eight distinct hydroidolinan clade

    Phylogenetics of Hydroidolina (Hydrozoa: Cnidaria)

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    This is the published version, also available here: http://dx.doi.org/10.1017/S0025315408002257.Hydroidolina is a group of hydrozoans that includes Anthoathecata, Leptothecata and Siphonophorae. Previous phylogenetic analyses show strong support for Hydroidolina monophyly, but the relationships between and within its subgroups remain uncertain. In an effort to further clarify hydroidolinan relationships, we performed phylogenetic analyses on 97 hydroidolinan taxa, using DNA sequences from partial mitochondrial 16S rDNA, nearly complete nuclear 18S rDNA and nearly complete nuclear 28S rDNA. Our findings are consistent with previous analyses that support monophyly of Siphonophorae and Leptothecata and do not support monophyly of Anthoathecata nor its component subgroups, Filifera and Capitata. Instead, within Anthoathecata, we find support for four separate filiferan clades and two separate capitate clades (Aplanulata and Capitata sensu stricto). Our data however, lack any substantive support for discerning relationships between these eight distinct hydroidolinan clades
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