Shelf morphology as an indicator of sedimentary regimes: a synthesis from a mixed siliciclastic-carbonate shelf on the eastern Brazilian margin

Modern shelf morphology is the result of the interplay between short and long term sedimentary processes. The relation between rates of sediment supply/carbonate growth and accommodation space creation will not only control coastal transgression and regression, but will also define the shelf sedimentary regimes acting to shape the seabed. Herein, shelf morphology and sedimentology are investigated in order to discuss how these characteristics can be representative of distinct sedimentary regimes. The study area is the eastern Brazilian shelf where coastal transgression and regression coexist with the most important coral reef system of the South Atlantic. A compilation of existing published and unpublished data was carried out in order to produce morphological and faciological maps and compare the mapped features with high-resolution seismic and sonographic data. The results show three major regions or morphological compartments: Abrolhos Shelf, Doce River Shelf and the Paleovalleys Shelf. In terms of shelf sedimentary domain, rhodolith beds predominate over the outer shelf along the entire area, coralline reefs are present along the northern Abrolhos inner shelf and a significant terrigenous mud deposit is observed associated to the Doce River adjacent inner shelf beds. The rest of the shelf is composed by bioclastic or terrigenous mud sand and gravel. Terrigenous sedimentation is always restricted to the shoreface or inner shelf shallower areas and carbonate sands and gravels are predominant elsewhere. The Abrolhos shelf shows two distinct sectors; the northern area is a typical mixed sediment environment that has a supply regime along the coast/shoreface, mainly due to longshore transport and a carbonate regime along the inner and outer shelf. The southern shelf morphology and sedimentation are controlled by the antecedent topography and is typically a accommodation regime shelf with associated rhodolith beds. The Doce river shelf is a supply regime environment with the formation of a 5 to 8m thick regressive deposit with downlapping clinoforms. Southward from the Doce river shelf, a significant shift in sedimentary regime is observed as the morphology becomes very irregular with associated hardbottoms and unfilled paleovalleys. This sector of the shelf (Paleovalley shelf) is characterized by an accommodation regime. The interpretation shows that the entire study area can be defined as a mixed sedimentation shelf, showing supply and accommodation regimes. Shelf morphology worked as an indicator of these changes. Carbonate/terrigenous deposition during a highstand/regressive phase coeval along the eastern Brazilian shelf, either laterally and across shelf. This lateral/along coast variation in sediment supply and carbonate production leads to distinct lateral facies and geometry. These spatial changes in morphology and facies, with coexistence of carbonate and siliciclastic sedimentation, are very important for the correlation and interpretation of the geological record, especially stratigraphic surfaces and sequence units

Pharmacological Study Of Edema And Myonecrosis In Mice Induced By Venom Of The Bushmaster Snake (lachesis Muta Muta) And Its Basic Asp49 Phospholipase A(2) (lmtx-i).

Previous in vitro studies show that Lachesis muta venom and its purified Asp49 phospholipase A(2), named as LmTX-I, display potent neurotoxic and myotoxic activities. Here, an in vivo study was conducted to investigate some pharmacological effects of the venom or its LmTX-I toxin, after intra-muscular injection in tibialis anterior (TA) and following subplantar injection in hind paws of mice. Findings showed that LmTX-I increased plasma creatine kinase activity and produced strong myonecrosis and inflammatory reactions in TA muscle. In addition to these effects, the venom also induced intense local hemorrhage. Pre-treatment of the venom with EDTA (5 mM) significantly inhibited the edema and hemorrhage. Histological examination showed that L. muta venom caused inner dermal layer thickening in the pad hind paw. In addition, there was marked inflammatory cell infiltration, particularly of neutrophils, and hemorrhage. LmTX-I also demonstrated edema-forming activity, which was inhibited by pretreatment with indomethacin.27384-9