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Fatty acid biomarkers of organic matter sources and early diagenetic signatures in sediments from a coastal upwelling area (south-eastern Brazil)

机译:沿海上升流区(巴西东南部)沉积物中有机物源的脂肪酸生物标志物和早期成岩特征

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Sediment bulk parameters and fatty acid biomarkers were used to investigate the relative contribution of major sources of particulate organic matter during upwelling and non-upwelling conditions, at organic enriched sites on the south-eastern Brazilian coast. The degradation state of the organic material and its implications for benthic food webs were also evaluated. Temperature and salinity values indicate the intrusion of the South Atlantic Central Water in spring with a strong influence at station 4S. C:N ratios and fatty acid biomarkers suggest that sedimentary particulate organic matter is mainly autochthonous and originated from phytoplankton, zooplankton and bacteria, with a minor terrestrial contribution. Short-chain saturated fatty acids predominated, indicating the prevalence of partially degraded detritus. An exception was station 4S, where polyunsaturated fatty acids dominated, indicating the input of labile organic matter linked to upwelling of the South Atlantic Central Water. Fatty acid concentrations and the organic carbon content of the sediments suggest that food quantity is not a limiting factor for benthic fauna. Despite the high organic background of the sediments, the sporadic inputs of labile organic matter associated with South Atlantic Central Water intrusions may produce an important impact on benthic fauna and on the biogeochemistry of the sediments.View full textDownload full textKeywordscoastal sediments, particulate organic matter, fatty acids, sources, diagenetic status, food qualityRelated var addthis_config = { ui_cobrand: "Taylor & Francis Online", services_compact: "citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more", pubid: "ra-4dff56cd6bb1830b" }; Add to shortlist Link Permalink http://dx.doi.org/10.1080/02757540.2011.644537
机译:在巴西东南沿海的有机物富集点,使用沉积物体积参数和脂肪酸生物标记物研究上升和非上升条件下颗粒有机物主要来源的相对贡献。还评估了有机材料的降解状态及其对底栖食物网的影响。温度和盐度值指示春季南大西洋中央水域的入侵,对4S站产生了重大影响。 C:N比值​​和脂肪酸生物标志物表明,沉积颗粒有机物主要是自生的,起源于浮游植物,浮游动物和细菌,对陆地的贡献较小。短链饱和脂肪酸占主导地位,表明部分降解的碎屑普遍存在。 4S站是个例外,其中多不饱和脂肪酸占主导地位,这表明与南大西洋中央水流上升有关的不稳定有机物的输入。沉积物中的脂肪酸浓度和有机碳含量表明,食物数量不是底栖动物的限制因素。尽管沉积物的有机背景很高,但与南大西洋中央水入侵相关的零星不稳定有机物输入可能会对底栖动物群和沉积物的生物地球化学产生重要影响。查看全文下载全文关键词脂肪酸,来源,成岩状态,食品质量:“ ra-4dff56cd6bb1830b”};添加到候选列表链接永久链接http://dx.doi.org/10.1080/02757540.2011.644537

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