Marine organic matter

Marine organic matterMarine organic matter
  1. The regional differentiation of the δ 13C values of suspended particulate matter reflect the source of terrestrial and marine organic matter input in the distribution along the growth and decline . 3 .

    悬浮颗粒物的δ13C值的地区分异就反映出陆源和海源有机质输入量在沿岸分布上的消长变化。

  2. The oils had heavy carbon isotopic ratios ( - 26 ‰~ - 24 ‰) and flat curves of individual n-alkane isotope profile , showing similar isotopic characteristics of marine organic matter .

    其全油碳同位素偏重(-26‰~-24‰);正构烷烃系列单体烃碳同位素分布曲线呈水平状,表现出类同于海相有机质的碳同位素组成特征。

  3. Measurement of riverine and marine dissolved organic matter by fluorescence excitation-emission spectra

    河流与海洋溶解有机物荧光激发-发射矩阵光谱的测定

  4. Summary of Processes and Significance of Clay Minerals in Marine Sedimentary Organic Matter Preservation and in Global Carbon Cycle

    粘土矿物保存海洋沉积有机质研究进展及其碳循环意义

  5. Research has shown that , high paraffin content crude oil is not continental facies , and marine facies organic matter can also generate crude oil with high paraffin content .

    研究表明,高蜡原油并非来源于陆相,海相有机质也可以生成含蜡量较高的原油。

  6. Study of marine sedimentary organic matter is mainly focused on the composition , distribution , biological sources and diagenesis in the early stages of bio-geochemical conversion of organic matter in marine sediments .

    海洋沉积有机质主要是研究海洋沉积物中有机质组成、分布特征、生物来源以及有机质在早期成岩作用阶段的生物地球化学转换。

  7. An Overview of Marine Fluorescent Dissolved Organic Matter

    海洋荧光溶解有机物研究进展

  8. Paleoproduction could be obtained from the carbon stable isotopic records of marine carbonates and organic matter , and nitrogen isotopic ratios in the marine organic matter .

    海相碳酸盐和有机质的碳同位素记录,海相有机物的氮同位素比值也用以再造古生产率等古海洋学参数;

  9. Carbohydrates are ubiquitous in marine environments , including marine organisms , dissolved organic matter , colloids , sediments , and sinking and suspended particles .

    碳水化合物普遍存在于海洋环境中,包括海洋生物、溶解有机物、胶体、沉积物及悬浮颗粒物。

  10. Here we use an expanded marine sedimentary section from Spitsbergen to reconstruct the carbon isotope excursion as recorded in marine organic matter .

    本研究使用来自挪威属地斯匹茨卑尔根的海相沉积岩样品,该剖面沉积连续而且沉积速率较高。