The oceanic base of slope record of the Permian-Triassic crisis: view from Tethys (Oman)

The Oman Mountains provide some of the best sections of Permian and Triassic sediments from ocean sea floor to base-of-slope environments related to the distal South Tethyan margin. The central part of the range exposes the Buday'ah section of oceanic sediments in the so-called "Hawasina allochtons". The locality of Wadi Maqam in the north-western part of the Oman Mountains is among places where the thick Permian-Triassic base-of-slope sediments is exposed (Baud et al., 2001). Overlying 400 m of middle Permian limestones and dolomites, the upper Permian sediments consist of 50 m of ≈ 10 cm thick beds of cherts and dolomites rich in sponge spicules. The top of the Permian units is well bioturbated lime mudstone-wackestone, devoid of cherts and dated as late Changhsingian (Krystyn in Richoz et al., 2005). The boundary yellow shales are overlain by very thinly bedded, laminated microbial platy lime mudstone with H. parvus. The dramatic loss of the burrowing infauna indicates the appearance of oxygen-poor water. These Induan sediments are about 25 m thick and show at the top the first calcirudites, commonly clast-supported (edge-wise conglomerates), and are characterized by tabular clasts representing the sub- in situ reworking of the laminated, platy calcilutite. The very thick Smithian overlying litho-unit (up to 900 m) marks the onset on the base-of-slope of a deep-marine basin in which carbonate submarine fan deposits developed This very thick unit consists essentially of platy limestones, calcarenites and calcirudites. It comprises mainly grey-beige calcilutite, laminated and flaggy, interbedded with sparse beds of fine-grained calcarenite in cm beds. Channelized beds of intraformational calcirudite are also part of this succession which constitutes the greater part of the outcrop available. During the Spathian to Anisian, the sedimentation changes to terrigenous mudstone and siltstone that ended with Ladinian radiolarites.

Características de la vida planctónica y colonización de los organismos betónicos epilíticos durante el fenómeno El Niño

Durante «El Niño» (EN) de 1982 - 1983 se realizaron 2 experimentos en la Bahía de Ancón, a fin de reconocer las principales características de la reco­lonización en la biocenosis de Semimytilus algosus (zona mediolitoral), utilizando áreas cuadradas denudadas de 0,0625 m2 ; y en la de Aulacomya ater (a 5 metros de profundidad), colocando prismas triangulares de 0,2 m2 de área junto a un pequeño banco de este mitílido. Se analizaron periódicamente los cambios en el número de especies, densidad, biomasa, diversidad y velocidad de crecimiento de los principales coloniza­ dores. Paralelamente se tomaron datos oceanográficos y muestras periódicas de zooplancton y fitoplancton. En medio año de colonización, las características estructurales y tróficas de las 2 comunidades en suce­ sión han seguido patrones distintos, pero con un evidente proceso de tropicalización en ambos casos. Las larvas planctónicas con mayor abundancia a lo largo de todo el año pertenecieron al braquiópodo Discinisca lamellosa, a cirrípedos, gasterópodos y pelecípodos. En los experimentos, los mejores colonizadores primarios resultaron : Viva costata y Semimytilus algosus, en los cuadrados ; Hydroides parvus e Hydroides norvegica, en los prismas. Los mecanismos de competencia fueron más importantes en los cuadrados, destacando la ejercida por especies foráneas de aguas cálidas ( Pollicipes elegans, Pomatoceros sp.). En los prismas destacan los mecanismos de predación y resalta también la colonización por especies de aguas cálidas (Pomatoceros sp., Pteria sterna ) y por especies tradicionalmente escasas en la bahía (Argopecten purpuratus).

A new species of Nemopalpus Macquart (Diptera, Psychodidae) from Brazil

A new species of Nemopalpus Macquart (Diptera, Psychodidae) from Brazil. Nemopalpus parvus sp. nov. collected in the Atlantic rainforest of the state of Espírito Santo, in southeastern Brazil, is described and illustrated.

Nivel de ruido y efectos en el ecosistema por uso del zumbador en la pesca de suco Paralonchurus peruanus, Pacasmayo

En Pacasmayo, Región la Libertad, se efectuaron experimentos para determinación de ondas sonoras producidas por el zumbador utilizando equipos hidroacústicos y jaulas con peces en cautiverio, para evaluar su efecto en el ambiente biótico y abiótico. Se detectó incremento de oxígeno disuelto en el agua de mar (0,20 mL/L); fragmentación de diatomeas, presencia de quistes de esporas de Chaetoceros en superficie, disminución de la abundancia relativa de Acartia tonsa, Centropages brachiatus, Paracalanus parvus y Oithona setigera. El nivel de presión acústica generado por el zumbador estuvo dentro de la amplitud de onda máxima de 145 dB//1 μBar ref 1m, que no es letal en los peces; sin embargo, estos niveles de ondas acústicas afectarían el sistema sensorial, alterando su desplazamiento, orientación y equilibrio, ocasionando que los peces queden atrapados en la red de enmalle.

A unique Permian-Triassic boundary section from the Neotethyan Hawasina Basin, Central Oman Mountains

In the Wadi Wasit area (Central Oman Mountains), Dienerian breccias are widespread. These breccias consist mostly of Guadalupian reefal blocks, often dolomitised, and some rare small-sized blocks of lowermost Triassic bivalve-bearing limestones. A unique block, with a size of about 200 m(3), including Permian and earliest Triassic faunas has been studied in detail. The so-called Wadi Wasit block consists of three major lithological units. A basal unstratified grey limestone is rich in various reef-building organisms (rugose corals, calcareous sponges, stromatoporoids) and has been dated as Middle Permian. It is disconformably overlain by well- and thin-bedded light grey to yellowish coloured limestones rich in molluscs. Two major lithologies (Coquina Limestone respectively Bioclastic Limestone unit) characterise the shelly limestones, their contact seems gradual. These two units are well-dated; they are of Griesbachian age and contain three conodont zones, the Parvus Zone, the Staeschei Zone and the Sosioensis Zone, and two ammonoid zones, the Ophiceras tibeticum Zone and an 'unnamed interval'. The third unit consists of a grey marly limestone containing Neospathodus kummeli (basal Dienerian). It is the first record of well-dated basal Triassic sediments in the Arabian Peninsula. The Coquina Limestone is dominated by the bivalve Promyalina with some Claraia and Eumorphotis. This bivalve association is interpreted as a pioneering opportunistic assemblage. Towards the top of the Bioclastic Limestone unit, the faunal diversity increases and contains probably more than 20 taxa of bivalves, microgastropods, crinoids, brachiopods, ammonoids, echinoid spines, ostracods and conodonts. The generic diversity of this biofacies exceeds by far any other Griesbachian assemblage known. Our data give new evidence for the geodynamical history for the distal carbonate shelf bordering the Hawasina Basin. A break in the sedimentation characterises the Late Permian. The basal Triassic shows a steady transgression and the breccias may record a distinct gravitational collapse of platform margins linked with sea-level low stand at the end of Induan time (late Dienerian-basal Smithian). delta(13)C(carb) isotopic analyses were performed and yield typical Permian values of around 4parts per thousand for the Reefal Limestone, with a strong negative shift across the Permian-Triassic boundary. During the Griesbachian values shift positively from 0.5 to 3.1parts per thousand parallel to an increase in faunal diversity and probably primary productivity. The detailed faunal analysis and the discovery of an unexpected diversity give,us a new understanding of the recovery of the Early Triassic marine ecosystem.

Rapid marine recovery after the end-Permian mass-extinction event in the absence of marine anoxia

A new Early Triassic marine fauna is described from the Central Oman Mountains. The fauna is Griesbachian in age, on the basis of abundant conodonts and ammonoids, and was deposited in an oxygenated seamount setting off the Arabian platform margin. It is the first Griesbachian assemblage from a well-oxygenated marine setting and thus provides a test for the hypothesis that widespread anoxia prevented rapid recovery. The earliest Griesbachian (parvus zone) contains a low-diversity benthic fauna dominated by the bivalves Promyalina and Claraia. A similar level of recovery characterizes the immediate postextinction interval worldwide. However, the middle upper Griesbachian sedimentary rocks (isarcica and catinata zones) contain an incredibly diverse benthic fauna of bivalves, gastropods, articulate brachiopods, a new undescribed crinoid, echinoids, and ostracods. This fauna is more diverse and ecologically complex than the typical middle to late Griesbachian faunas described from oxygen-restricted settings worldwide. The level of postextinction recovery observed in the Oman fauna is not recorded elsewhere until the Spathian. These data support the hypothesis that the apparent delay in recovery after the end-Permian extinction event was due to widespread and prolonged benthic oxygen restriction: in the absence of anoxia, marine recovery is much faster.

Oeuvres médicales de GUY DE CHAULIAC, et recettes diverses.

Contient : Recueil de « receptes » ou remèdes contre différentes maladies, parmi lesquelles (p. 42) : « Dix rigles par quoy l'on peult entendre pourquoy les femmes ont chascun mois leurs fleurs, selon Me Benard de Gourdon. Cy commence le secret des dames, que fait entendre legerement le gouvernement des fleurs des dames... » ; « Le formulaire des aides des appostumes et pustules, ordonné à Paris par Me Guidon de Cailhac, cirurgien et maistre en medecine à Montpellier, l'an mil IIIcXL. Pour ce que selon la doctrine de Ga[lien]... — ... Explicit parvus Guido »

Sympodiomyces attinorum sp nov., a yeast species associated with nests of the leaf-cutting ant Atta sexdens

Four strains of a novel yeast species were isolated from laboratory nests of the leaf-cutting ant Atta sexdens in Brazil. Three strains were found in older sponges and one was in a waste deposit in the ant nests. Sequencing of the D1/D2 region of the large-subunit rRNA gene showed that the novel species, named Sympodiomyces attinorum sp. nov., is phylogenetically related to Sympodiomyces parvus. Unlike Sympodiomyces parvus, Sympodiomyces attinorum can ferment glucose, assimilate methyl alpha-D-glucoside, salicin and citrate, and grow at 37 degreesC, thus enabling these two species to be distinguished. Differentiation from other related species is possible on the basis of other growth characteristics. The type strain of Sympodiomyces attinorum is UNESP-S156(T) (=CBS 9734(T)=NRRL Y-27639(T)).

Karyotypic similarity among Barycholos temetzi and five species of the genus Eleutherodactylus from southeastern Brazil (Anura, Brachycephalidae)

Comparative cytogenetic analyses were carried out in six species of Brachycephalidae from southeastern Brazil. Barycholos ternetzi, Eleutherodactylus binotatus, Eleutherodactylus guentheri, Eleutherodactylus juipoca, Eleutherodactylus parvus and Eleutherodactylus sp. have 2n = 22 karyotypes with a marked variation in the morphology of chromosome pairs 8, 10 and 11, which are of telocentric or metacentric types, resulting in FN = 38, 40 and 44. Eleutherodactylus have a single chromosome pair bearing Ag-NOR, i.e. pair 1 in E. binotatus, pair 6 in E. guentheri and E. parvus, and pair 11 in E. juipoca and Eleutherodactylus sp. In contrast, B. ternetzi showed Ag-positive sites in the chromosome pairs 1, 4, 5, 9 and 11, and only one to three labelings per metdphase in each individual. Nevertheless, the main chromosome pair with Ag-NOR in the species seems to be the 11th, like in E. juipoca and Eleutherodactylus sp. The NOR site was confirmed by fluorescence in situ hybridization (FISH) technique in E. binotatus and in B. ternetzi, bearing 1p1p and 9p11p11p Ag-NOR pattern, respectively. All the species exhibited predominantly centromeric C-banding pattern, but interstitial bands have also been observed in some cases. In E. binotatus, there is an indication of geographical difference in the distribution of the interstitial C-bands. The fluorochromes GC-specific chromomycin A(3) (CMA(3)) and AT-specific 4',6-diamidino-2-phenylindole (DAPI), with distamycin A (DA) counterstaining, provided the molecular content of some repetitive regions in the karyotypes of the species. One male of E. binotatus presented an extensive heteromorphism, involving at least five different pairs, probably as a consequence of multiple reciprocal translocations. Such rearrangements might be responsible for the multivalent chain seen in the meiosis of this specimen, as well as in another male, although not exhibiting chromosome heteromorphism. The remaining males and those belonging to the other species have always shown 11 bivalents in diplotene and metaphase I cells. In all male specimens, metaphases II presented 11 chromosomes. Despite the observed discrepancies, the five species of Eleutherodactylus have a great uniformity in the 2n = 22 karyotypes, suggesting an assemblage of species from southeastern and southern Brazil, in contrast to northern and northeastern assemblage which is characterized by higher diploid numbers. Undoubtedly, B. ternetzi could be included in that proposed assemblage, due to its karyotypic similarity with the Eleutherodactylus species, as evidenced in the present study. This fact strongly supports the close relationships of both genera, previously inferred on the basis of several characters shared by their species. (C) 2006 Elsevier Ltd. All rights reserved.

Similaridade cariotípica entre Barycholos ternetzi e cinco espécies do gênero Eleutherodactylus do Sudoeste do Brasil (Anura, Leptodactylidae, Eleutherodactylinae)

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Ecologia alimentar das quatro espécies dominantes da anurofauna de serapilheira em um gradiente altitudinal na ilha de São Sebastião, SP

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Composição e abundância dos Copepoda (crustacea) planctônicos da costa do Amapá - Op. Norte IV (REVIZEE/SCORE NO)

A caracterização da composição de Copepoda planctônicos, na costa do Amapá foi estudada, a partir de amostras coletadas através do programa REVIZEE, durante a Operação Norte IV, em 2001, realizada pelo navio Oceanográfico “Antares”, pertencente à Marinha do Brasil (H-40). A área estudada está inserida na ZEE Norte brasileiro no trecho entre o Cabo Orange e o Delta do rio Parnaíba, enquadrando-se nas seguintes coordenadas geográficas, LAT. 02º 25,92’N e LONG. 049º11,98’W (est. 102); LAT. 03º36,14’N e LONG. 048º24,71’W (est. 107); LAT. 05º32,39’N e LONG. 050º13,11’W (est.130); LAT. 04º23,64’N e LONG. 051º02,58’W (est.134). As coletas foram realizadas através de arrastos verticais com rede de zooplâncton, com malha de 200 μm, dotadas de fluxômetro. Após as coletas, as amostras foram fixadas com formol neutro a 4 %. Também foram coletados os fatores hidrológicos, onde a temperatura da água variou de 23, 72 ºC a 28,87 ºC na plataforma continental, enquanto na região oceânica variou de 12,69 ºC a 28,87 ºC. A salinidade, na plataforma continental, variou 24,00 PSU a 36,42 PSU, e na região oceânica a variação foi de 33,98 PSU a 36,62 PSU. A costa do Amapá foi considerado um ambiente estável, devido as poucas variações de salinidade e temperatura. Foram identificadas 84 espécies de Copepoda, das quais, destacaram-se como as mais freqüentes, Clausocalanus furcatus, Oithona setigera, Paracalanus parvus, Macrosetella gracilis, Oncaea media, Corycaeus speciosus, Farranula gracilis, Subeucalanus pileatus e Paracalanus sp. As altas densidades e dominância ocorreram para as espécies, Nannocalanus minor, Corycaeus (Corycaeus) speciosus, Clausocalanus furcalocalanus pavo, Paracalanus parvus, Parvocalanus crassirostris, Oithona setigera, Macrosetella gracilis, Farranula gracilis, Subcalanus pileatus, Euterpina acutifrons e Oncaea media, consideradas como indicadoras de oligotrofia na área estudada. Dentre estas, a espécie Subeucalanus pileatus foi a que mais se destacou, a qual ocorreu na maioria das estações. A diversidade foi considerada alta na maioria das estações, exceto na estação 127 (considerada baixa), por estar sendo influenciada pela pluma amazônica. Enquanto, a densidade apresentou resultados menores que 100 org.m-³ indicando a região oceânica como um ambiente oligotrófico, e apesar disso, a comunidade de Copepoda encontra-se em grande diversidade na área.

Meiotic behavior of 18 species from eight families of terrestrial Heteroptera

Insects of the suborder Heteroptera are known for their odor, for being pests, or for being disease carriers. To gain better insight into the cytogenetic characteristics of heteropterans, 18 species of terrestrial Heteroptera belonging to eight families were studied. The presence of heteropycnotic corpuscles during prophase I, terminal or interstitial chiasmas, telomeric associations between chromosomes, ring disposals of autosomes during metaphase, and late migrations of the sex chromosomes during anaphase were analyzed. These features showed identical patterns to other species of Heteroptera previously described in the literature. Another studied characteristic was chromosome complements. The male chromosome complements observed were 2n = 12 chromosomes [10A + XY, Galgupha sidae (Amyot & Serville) (Corimelaenidae) and Pachycoris torridus (Scopoli) (Scutelleridae)]; 2n = 13 [10A + 2m + X0, Harmostes serratus (Fabricius), Harmostes apicatus (Stål), Jadera haematoloma (Herrich-Schaeffer), Jadera sanguinolenta (Fabricius), Jadera sp. (Rhopalidae)], and Neomegalotomus parvus (Westwood) (Alydidae); 2n = 13 [12A + X0, Stenocoris furcifera (Westwood) (Alydidae); 2n = 14 [12A + XY, Dictyla monotropidia (Stål) (Tingidae)]; 2n = 19 [18A + X0, Acanonicus hahni (Stål) (Coreidae)]; 2n = 21 [18A + 2m + X0, Acanthocephala sp. (Dallas) (Coreidae)]; 2n = 27 [24A + 2m + X0, Anisoscelis foliacea marginella (Dallas) (Coreidae)]; 2n = 18 [16A + XY, Oncopeltus fasciatus (Dallas) (Lygaeidae)]; 2n = 17 [14A + X1X2Y, Oxycarenus hyalinipennis (Costa) (Lygaeidae)]; 2n = 16 [12A + 2m + XY, Pachybrachius bilobatus (Say) (Lygaeidae)]; 2n = 26 [24A + XY, Atopozelus opsinus (Elkins) (Reduviidae)]; and 2n = 27 [24A + X1X2Y, Doldina carinulata (Stål) (Reduviidae)]. The diversity of the cytogenetic characteristics of Heteroptera was reflected in the 18 studied species. Thus, this study extends the knowledge of these characteristics, such as the variations related to chromosome complements, sex chromosome systems, and meiotic behavior.

Meiotic behavior of 18 species from eight families of terrestrial heteroptera

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

The recent eutrophication of Baldeggersee (Switzerland) as assessed by fossil diatom assemblages

Diatom analyses with an annual resolution were carried out on varves of the hypertrophic Baldeggersee (Central Swiss Plateau) for the timespan ad 1885 to 1993. They reveal seven major changes in the dominant planktonic diatoms. As a result of progressive nutrient enrichment, Baldeggersee changed in the 1910s from a Cyclotella to a Tabellaria fenestrata dominated assemblage, and eventually in the 1950s to a Stephanodiscus parvus dominated diatom assemblage. The timing and direction of diatom-assemblage changes in the varved sediment compare well with sedimentological and limnological observations. Partitioning of the variance in the diatom data revealed that TP is a stronger explanatory variable than temperature for these changes. A diatom-inferred total phosphorus (TP) reconstruction indicates three major steps in eutrophication, occurring at 1909, the mid-1950s and the mid-1970s. Comparison with TP measurements in the water column demonstrates that the diatom-TP inference model used is able to hindcast past TP concentrations reliably. The major steps in eutrophication led to decreases in diatom diversity and also resulted in a progressive increase of calcite grain-size. The lake restoration programme established since 1982 shows no direct impact on the composition of the diatom assemblages. However, the decrease in phosphorus loads since the mid-1970s is reflected in the diatom assemblages and in decreasing diatom-inferred TP concentrations.