Captorhinid reptiles from the lower Permian Pedra de Fogo Formation, Piauí, Brazil: the earliest herbivorous tetrapods in Gondwana.

The Pedra de Fogo Formation in the Parnaíba Basin of northeastern Brazil hosts a recently discovered lacustrine fauna and provides the only known record of the Captorhinidae in South America. Here, new captorhinid remains from this unit are described. Two partial mandibles, including one formerly ascribed to the genus Captorhinus, are here referred to Captorhinikos sp. a genus previously described from North America. The natural mould of a large mandible probably represents a new taxon within the captorhinid subclade Moradisaurinae, and a small skull roof is regarded as Captorhinidae indet. Captorhinids are generally considered to have been herbivores or omnivores. The Pedra de Fogo captorhinids likely played an important ecological role as primary consumers in the palaeoenvironment of this geological unit, which is also known for its extensive record of petrified forests. The new finds reinforce the close relationships between the continental faunas of palaeotropical western Gondwana and palaeoequatorial North America during the Cisuralian.

A taxonomic review of the brachiopod genus Australocoelia (Boucot amp; Gill, 1956) in the Devonian of Brazil.

The rhynchonellide brachiopod genus Australocoelia was widely distributed across the Southern Hemisphere in the Devonian with three species recognized; A. palmata, A. peruviana and A. polyspera. In Brazil, A. palmata was initially reported from the Ponta Grossa and São Domingos formations (Paraná Basin), later recorded from the western border of the Parnaíba Basin (Pimenteira Formation, State of Tocantins), and is now shown to occur on the eastern border of the same basin (Pimenteira Formation, State of Piauí). In this paper, we describe a fourth species from the Paraná Basin as Australocoelia boucoti n. sp. It differs from A. palmata and the other species of Australocoelia in features of ornamentation and interspace, in addition to paleoecological characteristics.

Spectroscopic analysis and X-ray diffraction of trunk fossils from the Parnaíba Basin, Northeast Brazil.

The Parnaiba Sedimentary Basin is of the Paleozoic age and is located in Northeast Brazil, covering the states of Piauí, Maranhão and Tocantins and a small part of Ceará and Pará. In this work we applied several chemical analytical techniques to characterize trunk fossils found in the Parnaíba Sedimentary Basin, collected from four different sites, and discuss their fossilization process. We performed a study of the trunk fossils through X-ray diffraction, energy dispersive spectroscopy, infrared and Raman spectroscopy. The analysis allow us to identify the different compositions which are present in the trunk fossils: kaolinite (Al2Si2O5(OH)4), hematite (Fe2O3) and quartz (SiO2). Based in these results we were able to identify that the main fossilization mechanism of the trunk fossil was silicification. Furthermore, through Raman spectroscopy, we have observed the presence of carbonaceous materials in the Permian fossils, as evidenced by the D and G Raman bands. The relative intensities and bandwidths of the D and G bands indicated that the carbon has a low crystallinity. Thus, most of trunk fossils analyzed were permineralized and not petrified, because there is the presence of carbon that characterizes the partial decomposition of the organic matter in some trunks.

The zooplankton biodiversity of some freshwater environments in Parnaíba basin (Piauí, Northeastern Brazil) / Diversidade do zooplâncton de alguns ambientes de água doce na bacia do rio Parnaíba (Piauí, Nordeste do Brasil)

The plankton fauna of the state of Piauí, Northeastern Brazil, especially in the Parnaíba basin, is still poorly known; the results of most studies of the subject have not been published and can only be found in grey literature (unpublished scientific works), such as course completion work and consulting reports. Thus, this paper presents data from samples taken recently from different water bodies in Piauí and represents the second study to be published on the region's zooplankton since the pioneering work of Spandl (1926). A total of 38 species were recorded, including 23 new occurrences of rotifers, 10 of cladocerans and 2 of copepods for the state of Piauí. The greatest richness was observed for the rotifers, of which the genus Brachionus must be highlighted, especially at the Joana reservoir. Among the crustaceans, the greatest richness was observed at the Bezerra reservoir, where cladocerans of the genus Bosmina were prominent. The rotifers Brachionus havanaensis Rousselet, 1911 and Filinia longiseta (Ehrenberg, 1834); the cladocerans Diaphanosoma spinulosum Herbst, 1967 and Moina micrura Kurz, 1874; and the copepods Notodiaptomus cearensis Wright, 1936 and Thermocyclops decipiens Kiefer, 1927 occurred in all or in most environments in which the respective groups were studied. The results presented here expand the taxonomic list of zooplankton for the state of Piauí, including a total fauna of 30 species of rotifers, 15 of cladocerans and 3 of copepods. The zooplankton richness was considered low in the studied reservoirs compared to other freshwater ecosystems from Northeastern Brazil; however, the few studies developed in the Parnaíba basin suggest that the diversity for these organisms should be higher.(AU)

A fauna planctônica do Estado do Piauí, Nordeste do Brasil, especialmente para a Bacia do Rio Parnaíba, é ainda pouco conhecida; o resultado da maioria dos estudos não é publicado, podendo ser encontrado apenas em bibliografia cinzenta (não publicada cientificamente), tais como trabalhos de finalização de curso e relatórios de consultorias. Assim, o presente trabalho apresenta dados de amostragens recentes realizadas em diferentes corpos d'água do Piauí, consistindo no segundo estudo publicado sobre o zooplâncton da região, após o trabalho pioneiro de Spandl (1926). Registrou-se um total de 38 espécies, incluindo 23 novas ocorrências de rotíferos, dez novas ocorrências de cladóceros e dois novos registros de copépodes para o estado do Piauí. A maior riqueza foi observada para os rotíferos, com destaque para o gênero Brachionus, sobretudo no Açude Joana. Entre os crustáceos, foi observada uma maior riqueza no Açude Bezerra, destacando-se os cladóceros do gênero Bosmina. Os rotíferos Brachionus havanaensis Rousselet, 1911 e Filinia longiseta (Ehrenberg, 1834), os cladóceros Diaphanosoma spinulosum Herbst, 1967 e Moina micrura Kurz, 1874, e os copépodes Notodiaptomus cearensis Wright, 1936 e Thermocyclops decipiens Kiefer, 1927 ocorreram em todos ou na maioria dos ambientes onde os respectivos grupos foram estudados. Os resultados apresentados aqui ampliam a lista taxonômica do zooplâncton do Estado do Piauí, em uma fauna total de 30 espécies de rotíferos, 15 de cladóceros e três de copépodes. A riqueza do zooplâncton nos ambientes estudados foi considerada baixa em comparação com outros ecossistemas de água doce da Região Nordeste do Brasil; porém, os poucos estudos desenvolvidos na Bacia do Rio Parnaíba sugerem que a diversidade destes organismos seja maior.(AU)

The zooplankton biodiversity of some freshwater environments in Parnaíba basin (Piauí, Northeastern Brazil) / Diversidade do zooplâncton de alguns ambientes de água doce na bacia do rio Parnaíba (Piauí, Nordeste do Brasil)

The plankton fauna of the state of Piauí, Northeastern Brazil, especially in the Parnaíba basin, is still poorly known; the results of most studies of the subject have not been published and can only be found in grey literature (unpublished scientific works), such as course completion work and consulting reports. Thus, this paper presents data from samples taken recently from different water bodies in Piauí and represents the second study to be published on the region's zooplankton since the pioneering work of Spandl (1926). A total of 38 species were recorded, including 23 new occurrences of rotifers, 10 of cladocerans and 2 of copepods for the state of Piauí. The greatest richness was observed for the rotifers, of which the genus Brachionus must be highlighted, especially at the Joana reservoir. Among the crustaceans, the greatest richness was observed at the Bezerra reservoir, where cladocerans of the genus Bosmina were prominent. The rotifers Brachionus havanaensis Rousselet, 1911 and Filinia longiseta (Ehrenberg, 1834); the cladocerans Diaphanosoma spinulosum Herbst, 1967 and Moina micrura Kurz, 1874; and the copepods Notodiaptomus cearensis Wright, 1936 and Thermocyclops decipiens Kiefer, 1927 occurred in all or in most environments in which the respective groups were studied. The results presented here expand the taxonomic list of zooplankton for the state of Piauí, including a total fauna of 30 species of rotifers, 15 of cladocerans and 3 of copepods. The zooplankton richness was considered low in the studied reservoirs compared to other freshwater ecosystems from Northeastern Brazil; however, the few studies developed in the Parnaíba basin suggest that the diversity for these organisms should be higher.

A fauna planctônica do Estado do Piauí, Nordeste do Brasil, especialmente para a Bacia do Rio Parnaíba, é ainda pouco conhecida; o resultado da maioria dos estudos não é publicado, podendo ser encontrado apenas em bibliografia cinzenta (não publicada cientificamente), tais como trabalhos de finalização de curso e relatórios de consultorias. Assim, o presente trabalho apresenta dados de amostragens recentes realizadas em diferentes corpos d'água do Piauí, consistindo no segundo estudo publicado sobre o zooplâncton da região, após o trabalho pioneiro de Spandl (1926). Registrou-se um total de 38 espécies, incluindo 23 novas ocorrências de rotíferos, dez novas ocorrências de cladóceros e dois novos registros de copépodes para o estado do Piauí. A maior riqueza foi observada para os rotíferos, com destaque para o gênero Brachionus, sobretudo no Açude Joana. Entre os crustáceos, foi observada uma maior riqueza no Açude Bezerra, destacando-se os cladóceros do gênero Bosmina. Os rotíferos Brachionus havanaensis Rousselet, 1911 e Filinia longiseta (Ehrenberg, 1834), os cladóceros Diaphanosoma spinulosum Herbst, 1967 e Moina micrura Kurz, 1874, e os copépodes Notodiaptomus cearensis Wright, 1936 e Thermocyclops decipiens Kiefer, 1927 ocorreram em todos ou na maioria dos ambientes onde os respectivos grupos foram estudados. Os resultados apresentados aqui ampliam a lista taxonômica do zooplâncton do Estado do Piauí, em uma fauna total de 30 espécies de rotíferos, 15 de cladóceros e três de copépodes. A riqueza do zooplâncton nos ambientes estudados foi considerada baixa em comparação com outros ecossistemas de água doce da Região Nordeste do Brasil; porém, os poucos estudos desenvolvidos na Bacia do Rio Parnaíba sugerem que a diversidade destes organismos seja maior.

Nutrient release by a Brazilian sedimentary zeolite

This report describes the characterization of a sedimentary occurrence from the Parnaíba Basin, Brazil, containing the zeolite stilbite intertwined with smectitic clay mineral. The head samples from different sites present a wide content range of the zeolitic phase - 15 percent to 50 percent. The use of simple separation techniques - conventional gravitic treatments - yields concentrates containing about 67 percent of the zeolitic component. Assays with the amendments of these concentrates with plant nutrients yield release rates matching those reported for similar commercial products.

São apresentadas as propriedades físico-químicas de uma ocorrência sedimentar da Bacia do Parnaíba, Brasil, da zeólita estilbita, agregada a uma argila esmectítica. As amostras de diferentes sítios apresentam uma ampla variação do mineral zeolítico: entre 15 por cento a 50 por cento. A utilização de espirais concentradoras foi suficiente para obtenção de concentrados contendo até 67 por cento do mineral. Ensaios laboratoriais do concentrado dopado com fertilizantes revelam taxas de liberação de nutrientes comparáveis aos obtidos com produtos comerciais similares.

Flood-dominated fluvio-deltaic system: a new depositional model for the Devonian Cabeças Formation, Parnaíba Basin, Piauí, Brazil

The depositional model of the Cabeças Formation is re-evaluated in the context of the Devonian paleogeography of the Parnaíba Basin, and with particular reference to similarities between the formation's facies associations on the eastern border of the basin and the flood-dominated fluvio-deltaic system facies that have been discussed in recent literature. The widespread occurrence and nature of sigmoidal clinoforms (with asymptotic cross-stratification and climbing ripples) of the Cabeças Formation are here considered as strong evidence of flood-influenced depositional settings. Sandy strata of the Passagem Member, in the vicinity of Pimenteiras and Picos (Piauí State), are interpreted as the distal part of fine-grained mouth-bar deposits interbedded with delta-front sandstone lobes showing hummocky cross-stratification. Richly fossiliferous levels, with diverse megainvertebrates and plant cuticles, occur within the delta-front lobes and the distal mouth-bar deposits, reflecting continuation of shallow marine conditions.

O modelo deposicional da Formação Cabeças é reinterpretado no presente estudo com base no contexto paleogeográfico da Bacia do Parnaíba durante o Devoniano e na similaridade entre as fácies encontradas na Formação Cabeças com as fácies características dos sistemas flúvio-deltaicos dominados por inundações. O tipo das clinoformas sigmoidais (com estratificação cruzada assintótica e laminação cruzada cavalgante), e a sua predominância na Formação Cabeças, são consideradas como as principais evidências da influência de inundações nesta unidade. Depósitos do Membro Passagem, localizados nos arredores das cidades de Pimenteiras e Picos, são interpretados como o componente distal de um tipo de barra de desembocadura com a predominância de arenitos finos a conglomeráticos, intercalados com lobos arenosos tabulares de frente deltaica com estratificação cruzada hummocky. Diversos intervalos fossilíferos, com abundantes macrofósseis de invertebrados e fragmentos vegetais, ocorrem tanto nos lobos de frente deltaica quanto nos depósitos distais de barra de desembocadura, ainda no contexto de um paleoambiente marinho raso.