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Microbial Response to Organic Matter Enrichment in the Oligotrophic Levantine Basin (Eastern Mediterranean)

机译:贫营养性黎凡特盆地(东部地中海)对有机质富集的微生物响应

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The response of a deep-water benthic microbial community to organic matter (OM) enrichment was studied in the unexplored region of the SW Cretan margin (E. Mediterranean). A food pulse of 0.5 g C m−2 was simulated by adding 13C-labelled diatoms to sediment cores retrieved from 1079 m depth. The diatom addition resulted in a significant increase in the sediment community oxygen consumption (SCOC). After 6 days, 50 mg C m−2 of the added material was processed by the microbial community. The major carbon sink was respiration, which accounted for 96% of the total processed material. The carbon uptake rate (12 mg C m−2 d−1) was considerably lower than previously published values in the E. Mediterranean at similar depths. The microbial community in our study site is distinct, as revealed by the unusually high presence of branched phospholipid fatty acids (PLFA). Previous studies have revealed that the slope under investigation may act as a conduit of OM from the shallow shelf to the deep basins, resulting in the prevalence of relatively refractory OM at mid-slope depths. We postulate that sedimentary processes affect the amount of bioavailable sedimentary OM and consequently the structure and physiological state of bacterial community in our study site. The distinct microbial community composition at our station compared to more stable adjacent slopes could explain the limited response of the microbial community to the addition of labile OM. Supplemental materials are available for this article. Go to the publisher's online edition of Geomicrobiology Journal to view the free supplemental file.View full textDownload full textKeywordsstable isotope labelling, Eastern Mediterranean, organic matter mineralization, deep-sea bacteria, δ13C, PLFARelated 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/10.1080/01490451.2011.605822
机译:在西南克里特岛边缘(地中海地区)的未开发区域研究了深水底栖微生物群落对有机质(OM)富集的响应。通过将 13 C标记的硅藻添加到从1079 m深度取回的沉积物中,模拟了0.5 g C m up2 的食物脉冲。硅藻的添加导致沉积物群落耗氧量(SCOC)显着增加。 6天后,微生物群落处理了50 mg C m 的添加材料。主要的碳汇是呼吸,其占总加工材料的96%。碳吸收率(12 mg C m →2 d →1 )大大低于以前在地中海地区类似深度发布的值。我们的研究站点中的微生物群落与众不同,这是由支链磷脂脂肪酸(PLFA)异常高的存在所揭示的。先前的研究表明,所研究的斜坡可能是从浅层陆架到深盆的OM的管道,导致在中坡深度存在相对难熔的OM。我们假设沉积过程会影响生物可利用沉积OM的数量,从而影响我们研究地点细菌群落的结构和生理状态。与更稳定的相邻斜坡相比,我们站点的微生物群落组成独特,这可以解释微生物群落对不稳定的OM的有限响应。补充材料可用于本文。转到出版商的《地球微生物学期刊》在线版本,以查看免费的补充文件。弗朗西斯在线”,services_compact:“ citeulike,netvibes,twitter,technorati,美味,linkedin,facebook,stumbleupon,digg,google,更多”,发布号:“ ra-4dff56cd6bb1830b”};添加到候选列表链接永久链接http://dx.doi.org/10.1080/01490451.2011.605822

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