8 research outputs found

    Accumulation, persistence and effects of indospicine residues in camels fed Indigofera plant

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    Indospicine (L-2-amino-6-amidinohexanoic acid) is a natural hepatotoxin found in all parts of some Indigofera plants such as I. linnaei and I. spicata. Several studies have documented a susceptibility to this hepatotoxin in different species of animals, including cattle, sheep, dogs and rats, which are associated with mild to severe liver disease after prolonged ingestion. However, there is little published data on the effects of this hepatotoxin in camels, even though Indigofera plants are known to be palatable to camels in central Australia. The secondary poisoning of dogs after prolonged dietary exposure to residual indospicine in camel muscle has raised additional food safety concerns. In this study, a feeding experiment was conducted to investigate the in vivo accumulation, excretion, distribution and histopathological effects of dietary indospicine on camels. Six young camels (2 – 4 year old), weighing 270 − 390 kg were fed daily a roughage diet consisting of Rhodes grass hay and lucerne chaff, supplemented with Indigofera and steam flaked barley. Indigofera (I. spicata) was offered at 597 mg DM/kg body weight (bw)/day designed to deliver 337 ”g indospicine/kg bw/day, and fed for a period of 32 days. Blood and muscle biopsies were collected over the period of the study. Concentrations of indospicine in the plasma and muscle biopsy samples were quantitated by validated ultra-performance liquid chromatography−tandem mass spectrometry (UPLC−MS/MS). The highest concentrations in plasma (1.01 mg/L) and muscle (2.63 mg/kg fresh weight (fw)) were found at necropsy (day 33). Other tissues were also collected at necropsy and analysis showed ubiquitous distribution of indospicine, with the highest indospicine accumulation detected in the pancreas (4.86 ± 0.56 mg/kg fw) and liver (3.60 ± 1.34 mg/kg fw); followed by the muscle, heart and kidney. Histopathological examination of liver tissue showed multiple small foci of predominantly mononuclear inflammatory cells. After cessation of Indigofera intake, indospicine present in plasma in the remaining 3 camels had a longer terminal elimination half-life (18.6 days) than muscle (15.9 days), and both demonstrated mono-exponential decreases

    Corrigendum to ""Alcohol production from sterilized and non-sterilized molasses by Saccharomyces cerevisiae immobilized on brewer's spent grains in two types of continuous bioreactor systems"" [Biomass Bioenerg, 45 (2012) 87-94] (DOI:10.1016/j.biombioe.2012.05.015)

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    Livestock industries have maintained a keen interest in pasture legumes because of the high protein content and nutritive value. Leguminous Indigofera plant species have been considered as having high feeding values to be utilized as pasture, but the occurrence of the toxic constituent indospicine in some species has restricted this utility. Indospicine has caused both primary and secondary hepatotoxicosis and also reproductive losses, but has only previously been determined in a small number of Indigofera species. This paper validates a high-throughput ultraperformance liquid chromatography-tandem mass spectrometry (UPLC-MS/MS) method to determine the indospicine content of various Indigofera species found in Australian pasture. Twelve species of Indigofera together with Indigastrum parviflorum plants were collected and analyzed. Of the 84 samples analyzed, ∗I. spicata (the asterisk indicates a naturalized species) contained the highest indospicine level (1003 ± 328 mg/kg DM, n = 4) followed by I. linnaei (755 ± 490 mg/kg DM, n = 51). Indospicine was not detected in 9 of the remaining 11 species and at only low levels

    Mesozoic dinosaurs from Brazil and their biogeographic implications

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    The record of dinosaur body-fossils in the Brazilian Mesozoic is restricted to the Triassic of Rio Grande do Sul and Cretaceous of various parts of the country. This includes 21 named species, two of which were regarded as nomina dubia, and 19 consensually assigned to Dinosauria. Additional eight supraspecific taxa have been identified based on fragmentary specimens and numerous dinosaur footprints known in Brazil. In fact, most Brazilian specimens related to dinosaurs are composed of isolated teeth and vertebrae. Despite the increase of fieldwork during the last decade, there are still no dinosaur body-fossils of Jurassic age and the evidence of ornithischians in Brazil is very limited. Dinosaur faunas from this country are generally correlated with those from other parts of Gondwana throughout the Mesozoic. During the Late Triassic, there is a close correspondence to Argentina and other south-Pangaea areas. Mid-Cretaceous faunas of northeastern Brazil resemble those of coeval deposits of North Africa and Argentina. Southern hemisphere spinosaurids are restricted to Africa and Brazil, whereas abelisaurids are still unknown in the Early Cretaceous of the latter. Late Cretaceous dinosaur assemblages of south-central Brazil are endemic only to genus or, more conspicuously, to species level, sharing closely related taxa with Argentina, Madagascar, Indo-Pakistan and, to a lesser degree, continental Africa.<br>O registro osteolĂłgico de dinossauros no MesozĂłico brasileiro estĂĄ restrito a rochas triĂĄssicas do Rio Grande do Sul e estratos cretĂĄceos de vĂĄrias partes do paĂ­s. Isto inclui 21 espĂ©cies nominais, sendo duas referidas como nomina dubia, e 19 consensualmente classificadas como dinossauros. Oito tĂĄxons supraespecĂ­ficos adicionais baseados em material fragmentado e diversas pegadas sĂŁo conhecidos no Brasil. De fato, a maior parte dos espĂ©cimes Ă© composta de dentes isolados e vĂ©rtebras. Apesar do aumento em trabalhos de campo na Ășltima dĂ©cada, nĂŁo hĂĄ exemplar esqueletal de dinossauro no JurĂĄssico brasileiro, e Ă© escassa a evidĂȘncia de Ornithischia. Faunas dinossaurianas aqui registradas sĂŁo em geral correlatas com aquelas da PangĂ©ia durante o MesozĂłico. No TriĂĄssico Superior, hĂĄ uma correspondĂȘncia prĂłxima com a Argentina e outras regiĂ”es sul-gondwĂąnicas. Faunas do CretĂĄceo mĂ©dio do nordeste brasileiro sĂŁo semelhantes Ă s dos depĂłsitos coevos do norte da África e Argentina. Registros de espinossaurĂ­deos no hemisfĂ©rio sul estĂŁo restritos Ă  África e Brasil, enquanto abelissaurĂ­deos nĂŁo sĂŁo conhecidos no CretĂĄceo Inferior deste Ășltimo. Assembleias de dinossauros da regiĂŁo sul e central do Brasil sĂŁo endĂȘmicas apenas em nĂ­vel de gĂȘnero e, mais conspicuamente, espĂ©cie, compartilhando tĂĄxons proximamente relacionados com assembleias da Argentina, Indo-PaquistĂŁo, e, num menor grau, África continental
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