首页> 外文期刊>Proceedings of the Indian Academy of Sciences. Earth and Planetary Sciences >Amino sugars in suspended particulate matter from the Bay of Bengal during the summer monsoon of 2001
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Amino sugars in suspended particulate matter from the Bay of Bengal during the summer monsoon of 2001

机译:2001年夏季风期间孟加拉湾悬浮颗粒物中的氨基糖

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Amino sugars (AS) are important constituents of organic matter. However, very little is known about their cycling in marine waters. In this research, we assessed the distribution and cycling of these compounds in waters of the Bay of Bengal. For this purpose, samples of suspended particulate matter (SPM) were collected from 8 depths (surface to 1000 m) at 6 locations during the 166th cruise of the ORV Sagar Kanya in the Bay of Bengal in July/August 2001. The SPM samples were analysed for particulate organic carbon (POC), particulate nitrogen (PN) and AS concentrations and composition. The AS varied between 0.4 and 17.5 nmol/l. Concentrations were high in the surface waters and generally decreased with increasing depth. AS concentration decreased from the south to north. AS accounted for 0.01 to 0.71% and 0.05 to 2.37% of POC and PN, respectively. Rapid decrease in AS-C% and AS-N% with depth indicates that these compounds were preferentially degraded relative to bulk POC and PN. The composition of AS suggests that glucosamine (GLU-N) and galactosamine (GAL-N) were present in the surface SPM samples, and their abundance decreased from surface downwards. Relatively, low values of GLU-N/GAL-N ratio indicate that the organic matter was mostly derived from the detritus of micro-organisms. Our data suggest that chitin, a polymer of the glucosamine produced by many marine organisms was not the major source of AS in the Bay. Rapid cycling of these compounds indicates their importance in the cycling of nitrogen in marine waters.
机译:氨基糖(AS)是有机物的重要成分。然而,关于它们在海水中的循环知之甚少。在这项研究中,我们评估了这些化合物在孟加拉湾水域中的分布和循环。为此,在2001年7月/ 8月在孟加拉湾进行的第166次ORV Sagar Kanya航行期间,从6个位置的8个深度(表面至1000 m)收集了悬浮颗粒物(SPM)样品。分析颗粒有机碳(POC),颗粒氮(PN)和AS的浓度和组成。 AS在0.4和17.5nmol / l之间变化。地表水中的浓度很高,并且通常随着深度的增加而降低。 AS浓度从南到北下降。 AS分别占POC和PN的0.01至0.71%和0.05至2.37%。 AS-C%和AS-N%随深度迅速降低表明,相对于大量POC和PN,这些化合物优先降解。 AS的组成表明,表面SPM样品中存在氨基葡萄糖(GLU-N)和半乳糖胺(GAL-N),并且它们的丰度从表面向下降低。相对而言,GLU-N / GAL-N比值低表明有机物主要来自微生物的碎屑。我们的数据表明,几丁质是许多海洋生物产生的葡糖胺的聚合物,并不是海湾地区AS的主要来源。这些化合物的快速循环表明它们在海水中氮循环中的重要性。

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