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Carbon cycling in a continental margin sediment: contrasts between organic matter characteristics and remineralization rates and pathways

机译:大陆边缘沉积物中的碳循环:有机质特征与再矿化率和途径之间的对比

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Although particulate organic carbon (POC) in sediments is derived from diverse sources, characteristics of bulk POC are frequently used as indicators of the 'quality' of organic matter potentially available to sedimentary microbial communities. In order to investigate the extent to which characteristics of POC relate to sedimentary metabolism, the rates of the initial and terminal steps of organic carbon remineralization (extracellular enzymatic hydrolysis, and sulfate, iron, and manganese reduction, respectively) were compared at three sites in Skagerrak dominated by different terminal remineralization processes. In parallel, dissolved organic carbon (DOC) inventories and bulk POC characteristics were assessed. At all three sites, bulk characteristics of POC were similar, with C/N close to 12, low sedimentary amino acid content, and moderate concentrations of total hydrolyzable carbohydrates. On average, just 12% of POC was characterizable as carbohydrates or amino acids. These characteristics are frequently considered typical of unreactive or 'low quality' organic matter. At all three sites, however, organic carbon remineralization (measured as CO_2 production and sediment O_2 uptake) was quite high relative to other locations with similar bulk characteristics. A comparison of DOC inventories with rates of terminal remineralization demonstrated that at the three sites, on average 27, 8, and 31% of the sedimentary DOC pool must be turned over on a daily basis in order to support terminal respiration. Extracellular enzymatic activity, calculated as potential carbon turnover, was sufficient to support these rates. At these sites, standard chemical characterization of bulk POC does not reflect the reactivity and availability of substrates to the sedimentary microbial community. Carbon remineralization is likely fueled by a small fraction of POC, not distinguishable by measurement of bulk parameters, which is rapidly cycled through the DOC pool.
机译:尽管沉积物中的颗粒有机碳(POC)来自多种来源,但散装POC的特性经常被用作沉积微生物群落可能利用的有机物“质量”的指标。为了研究POC特性与沉积代谢的相关程度,在以下三个地点比较了有机碳再矿化的初始和最终步骤的速率(分别为细胞外酶水解以及硫酸盐,铁和锰的还原)。斯卡格拉克(Skagerrak)由不同的终端再矿化过程主导。同时,评估了溶解有机碳(DOC)的库存和总体POC特性。在这三个位置上,POC的体积特征均相似,C / N接近12,较低的沉积氨基酸含量,且总水解碳水化合物的浓度适中。平均而言,只有12%的POC可表征为碳水化合物或氨基酸。这些特性通常被认为是非反应性或“低质量”有机物的典型特征。然而,在所有三个地点,相对于其他具有类似体积特征的地点,有机碳再矿化(以CO_2的产生和沉积物O_2的吸收来衡量)都很高。 DOC存量与最终再矿化率的比较表明,在这三个地点,平均每天必须沉积27%,8%和31%的DOC沉积池,以支持最终呼吸。以潜在的碳周转率计算的细胞外酶活性足以支持这些速率。在这些站点上,散装POC的标准化学特征并未反映底物对沉积微生物群落的反应性和可用性。碳的再矿化可能是由一小部分的POC推动的,而这不能通过测量大量参数来区分,该参数在DOC池中快速循环。

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