Quaternary paleoenvironments and relative sea-level changes in Marajo Island (Northern Brazil): Facies, delta(13)C, delta(15)N and C/N

The reconstruction of physical environments of Amazonian areas is of great interest to determine the dynamic evolution of the Amazon drainage basin. However. few studies have emphasized the Quaternary deposits in this region. which is mostly due to the lack of natural exposures imposed by the low topography. This work integrates facies analysis. radiocarbon dating, delta(13)C, delta(15)N, and C/N of an 124 m-thick core from an area located at the mouth of the Amazon River. northeastern Amazonia. The study records deposits up to 50.795 (14)C yr B P. in age. which formed in a variety of depositional environments including fluvial channel, tidal flat, outer estuarine basin to shallow marine. inner estuarine basin, estuarine channel and lagoon. Facies interpretation was significantly improved with the inclusion of delta(13)C, delta(15)N, and C/N analyses of organic matter extracted from the sediments The obtained values conform to a transitional. mostly estuarine paleosetting evolved during successive relative sea-level fluctuations. The results suggest fluvial deposition between 40,950 (+/- 590) and 50.795 (14)C yr B P, with a rise in relative sea level that commenced between 35,567 (+/- 649) and 39,079 (+/- 1114) (14)C yr B P. An overall transgression took place until 29,340 (+/- 340) (14)C yr B P., after which the relative sea level dropped, favoring valley rejuvenation and incision. Following this time up to 10,479 (+/- 34) (14)C yr B.P. a rise in relative sea level filled up the valley with estuarine deposits After 10.479(+/- 34) (14)C yr B.P., the estuary was replaced by a lagoon At the end of the Holocene, the coastline prograided approximately 45 km northward, replaci ng the lagoon by a lake system Despite the influence of eustatic fluctuations. regional tectonics played a significant role to create new space where these Late Pleistocene and Holocene sediments accumulated. (C) 2009 Elsevier B V All rights reserved.

Equine infectious anemia on Marajo Island at the mouth of the Amazon river

Abstract: Equine infectious anemia (EIA) is a transmissible and incurable disease caused by a lentivirus, the equine infectious anemia virus (EIAV). There are no reports in the literature of this infection in Equidae on Marajo Island. The objective of this study was to diagnose the disease in the municipalities of Cachoeira do Arari, Salvaterra, Santa Cruz do Arari and Soure, on Marajó Island, state of Pará, Brazil. For serological survey samples were collected from 294 horses, over 5-month-old, males and females of puruca and marajoara breeds and from some half-breeds, which were tested by immunodiffusion in Agar gel (AGID). A prevalence of 46.26% (136/294) positive cases was found. EIA is considered endemic in the municipalities studied, due to the ecology of the region with a high numbered population of bloodsucking insect vectors and the absence of official measures for the control of the disease.

Archaeological Mounds in Marajo Island in Northern Brazil: A Geological Perspective Integrating Remote Sensing and Sedimentology

Earthen mounds with archaeological artifacts have been well known in Marajo Island since the 19th century. Their documented dimensions are impressive, e.g., up to 20m high, and with areas large as 90 ha. The mounds, locally known as lesos, impose a significant. relief on the very low-lying landscape of this region, which averages 4 to 6 in above present. sea level. These features have been traditionally interpreted as artificial constructions of the Marajoara culture, designed for defense, cemetery purposes, or escape from flooding. Here, we provide sedimentological and geomorphological data that suggest an alternative origin for these structures that is more consistent with their monumental sizes. Rather than artificial, the Marajoara tesos seem to consist of natural morphological features related to late Pleistocene and Holocene fluvial, and possibly tidal-influenced, paleochannels and paleobars that became abandoned as depositional conditions changed through dine. Although utilized and modified by the Marajoara since at least 2000 years ago, these earthen mounds contain a significant non-anthropogenically modified sedimentary substratum. Therefore, the large Marajoara tesos are not entirely artificial. Ancient, Marajoara cultures took advantage of these natural, preexisting elevated surfaces to base their communities and develop their activities, locally increasing the sizes of these fluvial landforms. This alternative interpretation suggests less cumulative labor investment, in the construction of the mounds and might. have significant implications for reconstructing the organization of the Marajoara culture. (C) 2009 Wiley Periodicals, Inc.

Palaeodrainage on Marajo Island, northern Brazil, in relation to Holocene relative sea-level dynamics

A large area in northeastern Marajo Island, northern Brazil, has been characterized geomorphologically, applying information acquired from Landsat imagery. This study was combined with detailed sedimentologic analysis of continuous cores, which provided a record of depositional settings developed in this area through the Holocene. The results revealed well-preserved, meandering to anastomosed drainage networks of wide palaeochannels that were superimposed by a narrower palaeochannel system. In both cases, the sedimentary record consists of sands, heterolithic deposits and muds, locally rich in plant debris. The strata are organized into fining upward successions that reach approximately 18 m thick in the wide channels and 4 m thick in the narrow channels. Sedimentary features suggestive of a coastal location for the wider palaeochannels and reworking of sediments by tidal currents include the prevalence of well to moderately sorted, rounded to sub-rounded, fine- to medium-grained sands displaying foreset packages separated by mud couplets, suggestive of tidal cycles. The data presented herein point to a rise in relative sea level reaching the Lake Arari area during the early to late/mid Holocene. This event was followed by a relative sea level drop. Tectonics seem to have contributed to an overall lowering in relative sea level in the study area since the mid-Holocene, which does not follow the same pattern recorded in other areas along the northern Brazilian coast.

Quaternary tectonics in a passive margin: Marajo Island, northern Brazil

Marajo Island is located in a passive continental margin that evolved from rifting associated with the opening of the Equatorial South Atlantic Ocean in the Late Jurassic/Early Cretaceous period. This study, based on remote sensing integrated with sedimentology, as well as subsurface and seismographic data available from the literature, allows discussion of the significance of tectonics during the Quaternary history of marginal basins. Results show that eastern Marajo Island contains channels with evidence of tectonic control. Mapping of straight channels defined four main groups of lineaments (i.e. NNE-SSW, NE-SW, NW-SE and E-W) that parallel main normal and strike-slip fault zones recorded for the Amazon region. Additionally, sedimentological studies of late Quaternary and Holocene deposits indicate numerous ductile and brittle structures within stratigraphic horizons bounded by undeformed strata, related to seismogenic deformation during or shortly after sediment deposition. This conclusion is consistent with subsurface Bouguer mapping suggestive of eastern Marajo Island being still part of the Marajo graben system, where important fault reactivation is recorded up to the Quaternary. Together with the recognition of several phases of fault reactivation, these data suggest that faults developed in association with rift basins might remain active in passive margins, imposing important control on development of depositional systems. Copyright (C) 2007 John Wiley & Sons, Ltd.

Low genetic diversity associated with low prevalence of Anaplasma marginale in water buffaloes in Marajo Island, Brazil

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The last mangroves of Marajo Island - Eastern Amazon: Impact of climate and/or relative sea-level changes

The dynamics, over the last 7500 years, of a mangrove at Marajo Island in northern Brazil were studied by pollen and sedimentary facies analyses using sediment cores. This island, located at the mouth of the Amazon River. is influenced by riverine inflow combined with tidal fluctuations of the equatorial Atlantic Ocean. Herbaceous vegetation intermingled with rainforest dominates the central area of the island, while varzea is the main vegetation type along the littoral. In particular, the modem northeastern coastal zone is covered by a mosaic of dense rainforest, herbaceous vegetation, mangroves, varzea, and restinga. The integration of pollen data and fades descriptions indicates a tidal mud flat colonized by mangroves in the interior of Marajo Island between similar to 7500 cal yr BP and similar to 3200 cal yr BP. During the late Holocene, mangroves retracted to a small area (100-700 m in width) along the northeastern coastal plain. Mangrove expansion during the early and mid Holocene was likely caused by the post-glacial sea-level rise which, combined with tectonic subsidence, led to a rise in tidal water salinity. Salinity must have further increased due to low river discharge resulting from increased aridity during the early and mid Holocene. The shrinking of the area covered by mangrove vegetation during the late Holocene was likely caused by the increase in river discharge during the late Holocene, which has maintained relatively low tidal water salinity in Marajo Island. Tidal water salinity is relatively higher in the northeastern part of the island than in others, due to the southeast-northwest trending current along the littoral. The mixing of marine and riverine freshwater inflows has provided a refuge for mangroves in this area. The increase in flow energy during the last century is related to landward sand migration, which explains the current retraction of mangroves. These changes may indicate an increased exposure to tidal influence driven by the relative sea-level rise, either associated with global fluctuations or tectonic subsidence, and/or by an increase in river water discharge. (C) 2012 Elsevier B.V. All rights reserved.

Facies, delta(13)C, delta(15)N and C/N analyses in a late Quaternary compound estuarine fill, northern Brazil and relation to sea level

The present work integrates sedimentary facies, (14)C dating, delta(13)C, delta(15)N, and C/N with geologic and geomorphologic data available from literature. The aim was to characterize the depositional settings of a late Quaternary estuary in northeastern Marajo Island and analyze its evolution within the context of relative sea level fluctuations. The data derive from four continuous cores along a proximal-to-distal transect of a paleoestuary, previously recognized using remote sensing information. Fifteen sediment samples recorded ages ranging from 42,580 +/- 1430 to 3184 +/- 37 (14)C yr B.P. Fades analysis indicated fine- to coarse-grained sands with parallel lamination or cross stratification, massive or laminated muds and heterolithic deposits. delta(13)C (-28.1 parts per thousand to -19.7 parts per thousand, mean = -23.0 parts per thousand), delta(15)N (+ 14.8 parts per thousand to + 4.7 parts per thousand, mean = + 9.2 parts per thousand) and C/N (14.5 to 1.5, mean = 7.9) indicate mostly marine and freshwater phytoplankton sources for the organic matter. The results confirm a large late Quaternary paleoestuary in northeastern Marajo Island. The distribution of delta(13)C, delta(15)N, and C/N, together with fades associations, led to identify depositional settings related to fluvial channel, floodplain, tidal channel/tidal flat, central basin, tidal delta, and tidal inlet/sand barrier. These deposits are consistent with a wave-dominated estuary. Variations in stratigraphy and geochemistry are controlled by changes in relative sea level, revealing a main transgression from an undetermined time around 42,000 (14)C yr B.P. and 29,340 (+/- 200) (14)C yr B.P., which is synchronous to the overall drop in sea level after the last interglacial. Following this period, and probably until 9110 +/- 37 (14)C yr B.P., i.e., during a time interval encompassing two glacial episodes including the Last Glacial and the Younger Dryas, there was a pronounced drop in sea level, recorded by the development of a major erosional discontinuity due to valley re-incision. Sea level rose again until 5464 +/- 40 (14)C yr B.P, just before the main worldwide mid-Holocene transgressive peak. Mid to late Holocene coastal progradation ended the Marajo paleoestuarine history, and promoted the establishment of continental conditions throughout the island. The divergence comparing the Marajo sea level behavior with the eustatic curve allows hypothesizing that post-rifting tectonics along the Brazilian Equatorial margin influenced the sedimentary evolution of the studied paleoestuary. Considering that sedimentary facies in estuarine settings are highly variable both laterally and vertically, the present integration of facies with isotope and elemental analyses was crucial to provide a more precise interpretation of the Late Pleistocene and Holocene Marajo paleoestuary, and analyze its sea level history within the eustatic and tectonic context. (C) 2010 Elsevier B.V. All rights reserved.

Coexistence of forest and savanna in an Amazonian area from a geological perspective

Question: How can the coexistence of savanna and forest in Amazonian areas with relatively uniform climates be explained? Location: Eastern Marajo Island, northeast Amazonia, Brazil. Methods: The study integrated floristic analysis, terrain morphology, sedimentology and delta(13)C of soil organic matter. Floristic analysis involved rapid ecological assessment of 33 sites, determination of occurrence, specific richness, hierarchical distribution and matrix of floristic similarity between paired vegetation types. Terrain characterization was based on analysis of Landsat images using 4(R), 5(G) and 7(B) composition and digital elevation model (DEM). Sedimentology involved field descriptions of surface and core sediments. Finally, radiocarbon dating and analysis of delta(13)C of soil profile organic matter and natural ecotone forest-savanna was undertaken. Results: Slight tectonic subsidence in eastern Marajo Island favours seasonal flooding, making it unsuitable for forest growth. However, this area displays slightly convex-up, sinuous morphologies related to paleochannels, covered by forest. Terra-firme lowland forests are expanding from west to east, preferentially occupying paleochannels and replacing savanna. Slack, running water during channel abandonment leads to disappearance of varzea/gallery forest at channel margins. Long-abandoned channels sustain continuous terra-firme forests, because of longer times for more species to establish. Recently abandoned channels have had less time to become sites for widespread tree development, and are either not vegetated or covered by savanna. Conclusion: Landforms in eastern Marajo Island reflect changes in the physical environment due to reactivation of tectonic faults during the latest Quaternary. This promoted a dynamic history of channel abandonment, which controlled a set of interrelated parameters (soil type, topography, hydrology) that determined species location. Inclusion of a geological perspective for paleoenvironmental reconstruction can increase understanding of plant distribution in Amazonia.

Renal and cardiovascular effects of Bothrops marajoensis venom and phospholipase A(2)

Bothrops marajoensis is found in the savannah of Marajo Island in the State of Par S and regions of Amapa State, Brazil. The aim of the work was to study the renal and cardiovascular effects of the B. marajoensis venom and phospholipase A(2) (PLA(2)). The venom was fractionated by Protein Pack 5PW. N-terminal amino acid sequencing of sPLA(2) showed amino acid identity with other lysine K49sPLA(2)s of snake venom. B. marajoensis venom (30 mu g/mL) decreased the perfusion pressure, renal vascular resistance, urinary flow, glomerular filtration rate and sodium tubular transport. PLA(2) did not change the renal parameters. The perfusion pressure of the mesenteric bed did not change after infusion of venom. In isolated heart, the venom decreased the force of contraction and increased PP but did not change coronary flow. In the arterial pressure, the venom and PLA(2) decreased mean arterial pressure and cardiac frequency. The presence of atrial flutter and late hyperpolarisation reversed, indicating QRS complex arrhythmia and dysfunction in atrial conduction. In conclusion, B. marajoensis venom and PLA(2) induce hypotension and bradycardia while simultaneously blocking electrical conduction in the heart. Moreover, the decrease in glomerular filtration rate, urinary flow and electrolyte transport demonstrates physiological changes to the renal system. (C) 2009 Elsevier Ltd. All rights reserved.

Cartografias da educação na Amazônia rural ribeirinha: estudo do currículo, imagens, saberes e identidade em uma escola do município de Breves/Pará

Esta dissertação resulta de uma pesquisa realizada em Breves, localizado ao sul da ilha de Marajó, no Estado do Pará - Brasil. Ela investiga o planejamento curricular da escola rural ribeirinha da vila de madeireira "Ivo Mainardi" da rede municipal de Breves/PA, na perspectiva das identidades e dos saberes da população ribeirinha marajoara de Breves. No percurso metodológico investigativo foi utilizado a análise documental, a entrevista semiestruturada e a fotografia, com a perspectiva de possibilitar ao leitor uma melhor compreensão sobre a Amazônia rural ribeirinha. A história de Breves tem início no Período Colonial, com a chegada dos portugueses ao local, sua população é constituída de ribeirinhos, muitos desses residem em pequenas comunidades, povoados e vilas de madeireiras. Muitos ribeirinhos são atraídos às vilas de madeireiras pela oferta do emprego na empresa madeireira e pela escola. Apesar do ribeirinho viver em um contexto em que a produção material está relacionada à exploração da madeira os currículos escolares não tratam desta questão, distanciando-se do que preconizam as Diretrizes Operacionais para a Educação Básica nas Escolas do Campo, que estabelece como princípio de qualidade do currículo a ecologia e a sustentabilidade. O planejamento curricular das escolas do meio rural é elaborado com a participaçã dos educadores rurais ribeirinhos, mas ainda não expressa os saberes, a cultura, e a identidade dos ribeirinhos marajoaras da Vila Mainardi. Assim, o desafio colocado aos gestores, os sujeitos sociais e os educadores é de vislumbrar o compromisso com uma educação que construa e cultive identidades, valores, memória coletiva e sinalize para a valorização e respeito dos povos que vivem na Amazônia marajoara, rural e ribeirinha de Breves.

Intoxicação por Ipomoea asarifolia em ovinos e bovinos na Ilha de Marajó

Para estudar as intoxicações por plantas que ocorrem na Ilha de Marajó foram visitadas 7 fazendas. Em todas as fazendas visitadas as pastagens eram constituídas de campo nativo, tinham pouco ou nenhuma disponibilidade de forragem e estavam severamente invadidas por Ipomoea asarifolia. Nas 5 propriedades foi relatada a ocorrência da intoxicação por esta planta em ovinos. Animais jovens são mais afetados do que adultos. Em duas dessas propriedades foram observados ovinos com sinais clínicos. Em 4 fazendas, os proprietários relataram a ocorrência da intoxicação por I. asarifolia em bovinos e, em uma dessas, foram observados bovinos com sinais clínicos em duas visitas realizadas, uma no período seco e outra no início do período chuvoso. Em bovinos as mortes ocorrem principalmente quando são afetados bezerros. A doença é observada todos os anos, com morbidade variável e baixa mortalidade. Os sinais clínicos foram característicos de uma doença tremogênica. Um bovino e um ovino, que apresentavam sinais clínicos acentuados e foram eutanasiados e necropsiados, não apresentavam alterações macroscópicas nem histológicas de significação. Em todas as fazendas visitadas eram criados bubalinos juntamente com bovinos e/ou ovinos e em 3 propriedades eram criados caprinos, mas nenhum proprietário relatou a ocorrência da intoxicação nestas duas espécies.

Níveis de fósforo, cobre, cobalto e zinco em bubalinos (Bubalus bubalis) na Ilha de Marajó, Estado do Pará

Foram estudados 104 bubalinos, adultos, sem distinção de raça e sexo, criados extensivamente, sem suplementação, em pastagens nativas de baixa qualidade nutricional, dos municípios de Breves, Cachoeira do Arari, Salvaterra e Soure, Ilha de Marajó, Pará. Realizou-se coleta de amostras de fígado, osso e sangue de 26 animais do município de Salvaterra, 38 animais do município de Soure, 20 animais do município de Breves e 20 animais do município de Cachoeira do Arari. Foram realizadas determinações dos teores de fósforo, no soro sanguíneo e no osso, do percentual de cinzas e da densidade específica no tecido ósseo, e de cobalto, cobre e zinco no tecido hepático. Observou-se que a média das concentrações de fósforo no soro sanguíneo (6,26mg/dl) e no osso (10,77%), a percentagem de cinzas (60,87%) e a densidade específica (1,59g/ml) do osso foram inferiores aos níveis críticos estabelecidos para bovinos, caracterizando deficiência de fósforo. As concentrações médias de cobre (5,57ppm), e zinco (27,05ppm) foram consideradas baixas quando comparadas com valores de referência, caracterizando deficiência para estes elementos. No caso do cobalto, quando se considerou os valores detectáveis e não detectáveis pela metodologia observou-se que 51,92% dos animais apresentaram níveis inferiores aos de referência, demonstrando a ocorrência da deficiência de cobalto nesses animais. Ressalta-se que as deficiências de cobre e zinco demonstraram uma maior gravidade já que todos os animais estudados apresentaram níveis deficientes nesses elementos.

Filogeografia em lagartos no baixo Tocantins, Ilha do Marajó e Sul do Amapá

Estudos filogeográficos têm ajudado a esclarecer o contexto espacial e temporal da diversificação de organismos amazônicos, o que pode ser diretamente comparado com cenários geológicos específicos. O presente estudo visa fornecer informações que possam auxiliar na reconstituição da história recente do baixo Tocantins/Ilha do Marajó a partir e uma análise filogeográfica de Gonatodes humeralis e Kentropyx calcarata. Adicionalmente, a utilidade do gene citocromo oxidase I como marcador para estudos populacionais de lagartos foi avaliada. Dados de 49 exemplares de G. humeralis e 32 de K. calcarata de 14 localidades ao sul do Amapá, baixo Tocantins, Ilha do Marajó e de uma externa à área focal do estudo foram analisados. Alem das medidas de diversidade e diferenciação genética, foram possíveis eventos de expansão demográfica recente nestas populações foram avaliados com uso da estatística R₂. As relações filogenéticas entre as populações foram avaliadas pela construção de árvores não enraizadas usando-se os métodos de máxima parcimônia (MP) e máxima verossimilhança (MV). Os resultados obtidos demonstram que embora o COI tenha sido raramente utilizado para esta finalidade, a variação observada entre seqüências de populações de G. humeralis e K. calcarata indicam que ele é um marcador útil para análises filogeográficas. As cinco populações de ambas as espécies aqui estudadas, são geneticamente estruturadas. Isso indica um baixo ou mais provavelmente inexistente fluxo gênico entre elas. As relações filogeográficas observadas, embora mais seguramente para G. humeralis que para K. calcarata indicam que ocorreram mudanças significativas em tempos relativamente recentes no sistema de drenagem na região do baixo rio Tocantins e Ilha do Marajó. Isto porque, há neste estudo, fortes indícios de que em tempos pretéritos recentes houve maior movimentação, ativa ou passiva, das espécies entre as regiões do Marajó e oeste do rio Tocantins que teriam sido as mais diretamente afetadas por estas mudanças.

Intoxicação por Ipomoea carnea subsp. fistulosa (Convolvulaceae) em caprinos na Ilha do Marajó, Pará

Ipomoea carnea subsp. fistulosa é uma planta que contém swainsonina causando doença de depósito lisossomal em ruminantes, principalmente em caprinos na região Nordeste do Brasil. Para o estudo das plantas tóxicas da Ilha de Marajó, foram visitadas sete propriedades rurais na Ilha de Marajó, seis localizadas no município de Cachoeira do Arari e uma no município de Soure. Em todas as propriedades visitadas as pastagens eram constituídas de campo nativo, tinham pouca disponibilidade de forragem e I. carnea subsp. fistulosa encontrava-se em grande quantidade. Nas três propriedades onde eram criados caprinos foram observados animais com sinais nervosos, incluindo tremores de intenção, aumento da base de sustentação quando em estação, ataxia, hipermetria, nistagmo, paresia espástica ou debilidade, alterações posturais, perda de equilíbrio e quedas. Em duas fazendas a prevalência foi de 32% (23/71) e 100% (32/32) e em outra havia um animal com sinais acentuados e o resto do rebanho, de 19 caprinos, não foi examinado clinicamente. Bovinos, ovinos e bubalinos não foram afetados. Foram eutanasiados e necropsiados seis caprinos que apresentavam sinais clínicos acentuados. Macroscopicamente não foram observadas alterações. Na histologia observou-se vacuolização do pericário de neurônios e do citoplasma de células epiteliais da tireóide, rim, fígado, pâncreas e macrófagos de diversos órgãos. No sistema nervoso central a vacuolização era mais grave nos neurônios de Purkinje do cerebelo e nos neurônios dos núcleos cerebelares e do tronco encefálico. Observaram-se também degeneração walleriana dos axônios e gliose. A alta freqüência da intoxicação nas três fazendas que criavam caprinos sugere que a intoxicação por I. carnea subsp. fistulosa é muito importante para caprinos na Ilha de Marajó, onde há abundante quantidade da planta, que permanece verde durante todo o período seco.