Estudos cromossômicos em anuros das famílias Hylidae rafinesque, 1815 e Leptodactylidae werner, 1896 (Amphibia: Anura)

Embora exista uma grande diversidade de complementos cromossômicos em Leptodactylidae (2n = 18 a 2n = 26) e Hylidae (2n = 20 a 2n = 32), a elevada fragmentação de dados limita o acesso a informações sobre as origens e os mecanismos responsáveis por esta diversidade. Isto provavelmente tem influenciado que os dados citogenéticos tenham sido principalmente utilizados na caracterização do status de espécies mais do que incluídos amplamente em análises filogenéticas. Este trabalho aborda, por meio de dados citogenéticos, aspectos evolutivos de três grandes grupos de anuros de ampla distribuição na região Neotropical. O gênero Leptodactylus é agrupado com Hydrolaetare, Paratelmatobius e Scythrophrys na família Leptodactylidae. Os antecedentes cromossômicos neste gênero indicam variações nos números diplóides de 2n = 18 a 2n = 26, assim como variações nos números fundamentais (número de braços autossômicos, NF) e nas posições das Regiões Organizadoras do Nucléolo (NOR). Os resultados das análises de 26 espécies de Leptodactylus empregando diversas técnicas representa, provavelmente, a análise citogenética mais inclusiva realizada no gênero Leptodactylus até o momento, e os resultados constituem um marco para a proposição de hipóteses consistentes de evolução cromossômica no gênero. A tribo Lophyiohylini agrupa atualmente 81 espécies distribuídas em 10 gêneros. A informação citogenética é escassa e restrita apenas a 12 espécies. São aqui apresentados comparativamente dados citogenéticos em espécies dos gêneros Argenteohyla, Itapotihyla, Phyllodytes, Trachycephalus e Osteocephalus. Os resultados indicam que, com exceção de O. buckleyi (2n = 26; NF = 50) e P. edelmoi (2n = 22; NF = 44), todas as demais espécies analisadas coincidem com os dados citogenéticos disponíveis, que indicam um 2n = 24 (NF = 48) na maioria das espécies cariotipadas, com NOR e constrições secundarias (CS) localizadas no par 11. Entretanto, em Phyllodytes edelmoi e Argentohyla siemersi pederseni, essas regiões localizam-se nos pares 2 e 5, respectivamente. Blocos heterocromáticos foram associados às CS adicionais (sítios frágeis) em Osteocephalus, mas não em Trachycephalus. Dados citogenéticos nos gêneros Nyctimantis e Tepuihyla, assim como técnicas com maior poder de resolução e estudos mais inclusivos, são necessários para compreender melhor a evolução cromossômica da tribo. A tribo Dendropsophini atualmente agrupa os gêneros Scinax, Pseudis, Scarthyla, Sphaenorhynchus, Xenohyla e Dendropsophus. Os dados citogenéticos registrados em todos os gêneros revelaram uma elevada diversidade cariotípica com grandes variações nos números diplóides (2n = 22 em Scarthyla; 2n = 24 em Scinax e Xenohyla; 2n = 24, 24 +1-2B e 26 em Sphaenorhynchus; 2n = 24 e 28 em Pseudis; e, 2n = 30 em Dendropsophus). O 2n = 24 observado em X. truncata indica que o 2n = 30constitui uma sinapomorfia do gênero Dendropsophus. A localização das NOR no par 7 é uma característica compartilhada por espécies dos gêneros Scarthyla, Xenohyla, Pseudis e Sphaenorhynchus, com algumas exceções nos dois últimos (P. caraya e S. carneus). Entretanto, o gênero Dendropsophus exibe uma interessante diversidade em relação a número e localização das NOR. Por outro lado, a distribuição de heterocromatina apresentou padrões variáveis, particularmente gênero Pseudis. Embora exista uma excepcional variação cromossômica neste grupo, a informação fragmentária em alguns gêneros dificulta a formulação de hipóteses consistentes sobre o papel dos cromossomos na evolução do grupo.

Caracterização de isolados de ceratocystis sp., avaliação de resistência clonal de eucalipto e sensibilidade deste fungo a diferentes fungicidas

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Chromosome Evolution in Dendropsophini (Amphibia, Anura, Hylinae)

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

RNA Interference of Endochitinases in the Sugarcane Endophyte Trichoderma virens 223 Reduces Its Fitness as a Biocontrol Agent of Pineapple Disease

The sugarcane root endophyte Trichoderma virens 223 holds enormous potential as a sustainable alternative to chemical pesticides in the control of sugarcane diseases. Its efficacy as a biocontrol agent is thought to be associated with its production of chitinase enzymes, including N-acetyl-beta-D-glucosaminidases, chitobiosidases and endochitinases. We used targeted gene deletion and RNA-dependent gene silencing strategies to disrupt N-acetyl-beta-D-glucosaminidase and endochitinase activities of the fungus, and to determine their roles in the biocontrol of soil-borne plant pathogens. The loss of N-acetyl-beta-D-glucosaminidase activities was dispensable for biocontrol of the plurivorous damping-off pathogens Rhizoctonia solani and Sclerotinia sclerotiorum, and of the sugarcane pathogen Ceratocystis paradoxa, the causal agent of pineapple disease. Similarly, suppression of endochitinase activities had no effect on R. solani and S. sclerotiorum disease control, but had a pronounced effect on the ability of T. virens 223 to control pineapple disease. Our work demonstrates a critical requirement for T. virens 223 endochitinase activity in the biocontrol of C. paradoxa sugarcane disease, but not for general antagonism of other soil pathogens. This may reflect its lifestyle as a sugarcane root endophyte.

Epicoccum nigrum P16, a Sugarcane Endophyte, Produces Antifungal Compounds and Induces Root Growth

Background: Sugarcane is one of the most important crops in Brazil, mainly because of its use in biofuel production. Recent studies have sought to determine the role of sugarcane endophytic microbial diversity in microorganism-plant interactions, and their biotechnological potential. Epicoccum nigrum is an important sugarcane endophytic fungus that has been associated with the biological control of phytopathogens, and the production of secondary metabolites. In spite of several studies carried out to define the better conditions to use E. nigrum in different crops, little is known about the establishment of an endophytic interaction, and its potential effects on plant physiology. Methodology/Principal Findings: We report an approach based on inoculation followed by re-isolation, molecular monitoring, microscopic analysis, plant growth responses to fungal colonization, and antimicrobial activity tests to study the basic aspects of the E. nigrum endophytic interaction with sugarcane, and the effects of colonization on plant physiology. The results indicate that E. nigrum was capable of increasing the root system biomass and producing compounds that inhibit the in vitro growth of sugarcane pathogens Fusarium verticillioides, Colletotrichum falcatum, Ceratocystis paradoxa, and Xanthomomas albilineans. In addition, E. nigrum preferentially colonizes the sugarcane surface and, occasionally, the endophytic environment. Conclusions/Significance: Our work demonstrates that E. nigrum has great potential for sugarcane crop application because it is capable of increasing the root system biomass and controlling pathogens. The study of the basic aspects of the interaction of E. nigrum with sugarcane demonstrated the facultative endophytism of E. nigrum and its preference for the phylloplane environment, which should be considered in future studies of biocontrol using this species. In addition, this work contributes to the knowledge of the interaction of this ubiquitous endophyte with the host plant, and also to a better use of microbial endophytes in agriculture.

Symbiotische Mikroorganismen aus dem Termitendarm

Symbiotische Mikroorganismen aus dem Termitendarm Es ist eine bekannte Tatsache, dass die Hauptaufgabe der Darmflora der niederen Termite im Abbau von Holz liegt. Im Laufe der Millionen Jahre alten Entwicklung der Termiten hat sich in ihrem Darm ein Ökosystem aufgebaut, das aus Protozoen, Archaeen, Bakterien und Hefen besteht. Ziel der vorliegenden Arbeit war die teilweise Erforschung der symbiotischen Zusammenhänge in diesem ökologischen System. Es wurden dabei zwei Gebiete genauer untersucht: Cellulolytische Bakterien im Darm von niederen Termiten Die bisher vorherrschende Meinung sah in den Protozoen die Hauptkomponenten des Celluloseabbaus in Termiten. In dieser Arbeit gelang es 164 cellulolytische Bakterienstämme aus sieben niederen Termitenarten zu isolieren und zu identifizieren. Diese Vielzahl cellulolytischer Bakterienarten könnte ein Indiz dafür sein, dass Bakterien beim Holzabbau von Termiten eine effizientere Rolle spielen als angenommen. Oberflächenbakterien von Mixotricha paradoxa, einem Flagellaten aus dem Darm der niederen Termite Mastotermes darwiniensisMixotricha paradoxa ist ein Beispiel der seltenen Form einer Bewegungssymbiose zwischen Protozoen und Bakterien. Der Flagellat wird von Spirochäten, die auf seiner Oberfläche befestigt sind, vorangetrieben. Zusätzlich leben noch stäbchenförmige Bakterien auf der Hülle. Drei Spirochätenarten und das stäbchenförmige Bakterium konnten identifiziert und lokalisiert werden. Es wird angenommen, dass alle drei Spirochätenarten Mitglieder der Bewegungssymbiose sind.

Syntagma De Ponderibus & Mensuris

Vorlage d. Digitalisats aus d. Besitz d. Theol. Hochschule St. Georgen

Biostratigraphy of sediment core CRP-3 from the Ross Sea, Antarctica

Early Oligocene siliceous microfossils were recovered in the upper c. 193 m of the CRP-3 drillcore. Although abundance and preservation are highly variable through this section, approximately 130 siliceous microfossil taxa were identified, including diatoms, silicoflagellates, ebridians, chrysophycean cysts, and endoskeletal dinoflagellates. Well-preserved and abundant assemblages characterize samples in the upper c. 70 m and indicate deposition in a coastal setting with water depths between 50 and 200 m. Abundance fluctuations over narrow intervals in the upper c. 70 mbsf are interpreted to reflect environmental changes that were either conducive or deleterious to growth and preservation of siliceous microfossils. Only poorly-preserved (dissolved, replaced, and/or fragmented) siliceous microfossils are present from c. 70 to 193 mbsf. Diatom biostratigraphy indicates that the CRP-3 section down to c. 193 mbsf is early Oligocene in age. The lack of significant changes in composition of the siliceous microfossil assemblage suggests that no major hiatuses are present in this interval. The first occurrence (FO) of Cavitatus jouseanus at 48.44 mbsf marks the base of the Cavitatus jouseanus Zone. This datum is inferred to be near the base of Subchron C12n at c. 30.9 Ma. The FO of Rhizosolenia antarctica at 68.60 mbsf marks the base of the Rhizosolenia antarctica Zone. The FO of this taxon is correlated in deep-sea sections to Chron C13 (33.1 to 33.6 Ma). However, the lower range of R. antarctica is interpreted as incomplete in the CRP-3 drillcore, as it is truncated at an underlying interval of poor preservation: therefore, an age of c. 33.1 to 30.9 Ma is inferred for interval between c. 70 and 50 mbsf. The absence of Hemiaulus caracteristicus from diatom-bearing interval of CRP-3 further indicates an age younger than c. 33 Ma (Subchron C13n) for strata above c. 193 mbsf. Siliceous microfossil assemblages in CRP-3 are significantly different from the late Eocene assemblages reported CIROS-1 drillcore. The absence of H. caracteristicus, Stephanopyxis splendidus, and Pterotheca danica, and the ebridians Ebriopsis crenulata, Parebriopsis fallax, and Pseudoammodochium dictyoides in CRP-3 indicates that the upper 200 m of the CRP-3 drillcore is equivalent to part of the stratigraphic interval missing within the unconformity at c. 366 mbsf in CIROS-1.

Jurassic microfossils of DSDP Hole 79-547B

The first marine incursion of the incipient North Atlantic Ocean is recorded in the uppermost Triassic to Lower Jurassic sequence of DSDP Site 547 off central Morocco. A lithologic change from continental red beds below to slope breccias and hemipelagic carbonates above indicates that a carbonate ramp was probably established by Sinemurian time along the Moroccan continental margin and that subsidence in the adjacent basin was rapid in the early phases of continental rift. Foraminifers recovered from the Liassic (Sinemurian-Pliensbachian) basinal deposits are diverse and well preserved. The faunas are compositionally similar to contemporaneous neritic assemblages of Europe and the Grand Banks of Newfoundland. The Middle Jurassic in Hole 547B is characterized by regressive deposits that are poor in foraminifers. The major Late Jurassic "Atlantic" transgression is again represented by basinal deposits consisting of limestone breccias and pelagic carbonates. Foraminifers recovered from this interval are transitional between Late Jurassic assemblages reported from deep-sea deposits in the North Atlantic and typical Late Jurassic neritic assemblages of Europe. The Late Jurassic assemblages of Hole 547B are primarily dominated by nodosariids and spirillinids with moderate abundances of simple arenaceous forms. Nonreticulate epistominids occur very rarely in the Upper Jurassic of Hole 547B. It is tentatively suggested that these represent upper bathyal assemblages.

Neogene diatoms of the Japan Sea

A series of excellent upper Miocene through Quaternary diatomaceous sequences recovered at four sites during Leg 127 was examined for diatoms. The diagenetic transition from opal-A to opal-CT is a diachronic horizon from the uppermost part of the Denticulopsis katayamae Zone (8.5 Ma) at Hole 797B to the uppermost part of the Neodenticula kamtschatica Zone (5.73 Ma) at Hole 795A. The diatom zonation of Koizumi (1985) best divides the upper Miocene to Quaternary sequences above the opal-A/opal-CT boundary and also is useful to date carbonate concretions including diatoms below the boundary. Forty diatom datum levels were evaluated biostratigraphically based on the sediment accumulation rate curve, and several isochronous datum levels are newly proposed for the Japan Sea area. A warm-water current did not penetrated into the Japan Sea through the Tsushima strait during the late Miocene and Pliocene time, because subtropical warm-water diatoms are essentially not present in such sediment samples. The occurrences of diatom are cyclic throughout the Quaternary sediments and are affected by eustatic sea level changes.

Late middle Eocene to late Oligocene radiolarian biostratigraphy of ODP Hole 113-689B of Maud Rise, Southern Ocean

We propose a new biostratigraphic scheme comprising the Eucyrtidium spinosum, Eucyrtidium antiquum (new), Lychnocanoma conica (emended), Clinorhabdus robusta (emended) and Stylosphaera radiosa (emended) Zones, in ascending order, in Eocene to Oligocene sediments drilled on Maud Rise in Southern Atlantic Ocean (Site 689, Ocean Drilling Program Leg 113). The bases of these zones are defined by the lowermost occurrences of E. spinosum, E. antiquum, L. conica, C. robusta and the uppermost occurrence of Axoprunum irregularis (?), respectively. From correlation to the magnetostratigraphic data, the E. spinosum, E. antiquum, L. conica, C. robusta and S. radiosa Zones are assigned to the late middle Eocene through late Eocene (Subchrons C17n2 to C13r), earliest Oligocene (C13n to C11n), late early Oligocene (C11n to C10n2), early late Oligocene (C10n1 to C8r) and latest Oligocene (C8r to C7An), respectively. The four boundary datum levels and supplementary datum levels such as the lowermost occurrences of A. irregularis (?), Dicolocapsa microcephala and Lithomelissa challengerae may be recognized in other ODP sites in the Southern Ocean. The first occurrence of E. antiquum approximates the Eocene-Oligocene boundary in Southern Ocean but the last occurrences of many species such as Periphaena decora, D. microcephala and the Lithomelissa sphaerocephalis group are commonly diachronous between high latitude sites. Two new species, Theocyrtis (?) triapenna and Spirocyrtis parvaturris, are described.