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Distribution And Sources Of Organic Carbon, Nitrogen And Their Isotopic Signatures In Sediments From The Ayeyarwady (irrawaddy) Continental Shelf, Northern Andaman Sea

机译:安达曼北部海伊洛瓦底(陆风)大陆架沉积物中沉积物中有机碳,氮及其同位素特征的分布和来源

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Total organic carbon (TOC), total nitrogen (TN) and their δ~(13)C and δ~(15)N values were determined from 110 sediment samples from the Ayeyarwady (Irrawaddy) continental shelf, northern Andaman Sea to decipher the concentration and source of organic matter. Comparatively higher TOC and TN concentrations are found in the inner-shelf mud belt, and on the continental slope sediments, whereas the outer-shelf sediments, composed mostly of relict sands, are low in TOC. The TOC contents are positively correlated with the abundance of fine-grained sediments. The TOC:TN ratios and δ~(13)C and δ~(15)N values show low variability within the modern inner-shelf mud belt and Gulf of Martaban, indicating similar source. The TOC:TN ratios are mostly between 6 and 8 in the inner-shelf mud belt and these values are similar to the suspended sediments in the Ayeyarwady and Salween rivers. The δ~(13)C values of organic matter increase from -25‰ in the Gulf of Martaban to about -22‰ in the slope regions indicating decreasing terrestrial input away from the coast. The δ~(15)N values on the Ayeyarwady shelf are rather low (+3.3 to +4.8‰), especially off the mouths of the Ayeyarwady River mouths, reflecting greater influence of freshwater and terrigenous sediment discharge. A simple two end-member carbon mixing model applied to the Ayeyarwady shelf region indicates that terrigenous sources contribute more than 70% of the organic carbon in the modern mud belt in the inner shelf and Gulf of Martaban. Terrigenous organic carbon percentages reduce gradually offshore, reducing to less than 60% near the continental shelf edge. A strong terrigenous signal is preserved in the inner shelf and Gulf of Martaban sediments probably because organic matter from the source region is not subject to intensive processing and replacement in the floodplains and deltaic regions as well as rapid burial at sea.
机译:从安达曼海北部伊洛瓦底江陆架的110个沉积物样品中确定了总有机碳(TOC),总氮(TN)以及它们的δ〜(13)C和δ〜(15)N值,以解释其浓度和有机物的来源。在内层泥质带和大陆斜坡沉积物中发现较高的TOC和TN浓度,而TOC中主要由残留砂组成的外层沉积物含量较低。 TOC含量与细颗粒沉积物的含量呈正相关。 TOC:TN比值和δ〜(13)C和δ〜(15)N值在现代内架泥质带和Martaban海湾内显示出较低的变异性,表明来源相似。内层泥质带的TOC:TN比大部分在6到8之间,这些值类似于Ayeyarwady河和Salween河中的悬浮沉积物。有机质的δ〜(13)C值从Martaban湾的-25‰增加到斜坡地区的-22‰,表明远离海岸的地面输入减少。伊洛瓦底陆架的δ〜(15)N值较低(+3.3至+ 4.8‰),特别是在伊洛瓦底河入海口附近,反映了淡水和陆源沉积物排放的更大影响。在伊洛瓦底陆架地区应用的一个简单的两个末端碳混合模型表明,陆源在内陆架和马塔班湾的现代泥质带中贡献了70%以上的有机碳。陆上的陆源有机碳百分比逐渐减少,在大陆架边缘附近减少到不足60%。在陆架和马塔班湾的沉积物中保留了强大的陆源信号,这可能是因为源区的有机物在洪泛区和三角洲地区没有经过密集的处理和替换以及在海上快速埋葬。

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