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Amino acid biogeochemistry and bacterial contribution to sediment organic matter along the western margin of the Bay of Bengal

机译:孟加拉湾西缘的氨基酸生物地球化学和细菌对沉积物有机质的贡献

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摘要

Six sediment cores collected from various water depths and sampling locations along the western margin of the Bay of Bengal (BOB) were investigated for the total hydrolysable amino acids (THAA) and D-amino acids (D-AA) to understand their distribution, digenetic alteration and bacterial contribution to organic matter (OM). Irrespective of their location, THAA concentrations and yields generally decreased and mol% glycine increased with increasing water depth indicating that OM was degraded during its transit through the water column. Amino acid based degradation index (DI) indicated that OM of the surface sediments of shallow stations, BOB-1 to BOB-3 was relatively fresher than that of deeper stations, BOB-4, BOB-5 and BOB-6. The concentrations and mol% of the d-AA varied from 0.04 to 0.76 μmol gdw~(-1) and 0.3 to 8.5 mol%, respectively. Contribution of bacterial peptidoglycan amino acids to THAA (% THAApep/ THAA) ranged between 4.0% and 55.0%. Both % THAA_(pep)/THAA and mol% d-Aas were significantly (p < 0.01) higher in the surface sediments and decreased with sediment core depth. Based on the d-AA yields, bacterial OM accounted for 1.5-15.6% of TOC, and 3.7-50.0% of TN of the sediments of BOB.
机译:研究了从孟加拉湾西缘(BOB)的不同水深和采样位置收集的六个沉积物核心的总可水解氨基酸(THAA)和D-氨基酸(D-AA),以了解它们的分布,双基因改变和细菌对有机物(OM)的贡献。无论它们位于何处,THAA的浓度和产率通常随着水深的增加而降低,而甘氨酸的摩尔%会随着水深的增加而增加,这表明OM在通过水柱的过程中被降解了。基于氨基酸的降解指数(DI)表明,浅站BOB-1至BOB-3的表层沉积物OM比较深站BOB-4,BOB-5和BOB-6的表层沉积物相对新鲜。 d-AA的浓度和mol%分别从0.04至0.76μmolgdw·(-1)和0.3至8.5mol%变化。细菌肽聚糖氨基酸对THAA的贡献(%THAApep / THAA)在4.0%至55.0%之间。 THAA_(pep)/ THAA的%和d-Aas的摩尔%均显着(p <0.01)在表层沉积物中较高,并且随沉积物芯深而降低。根据d-AA的产量,细菌OM占BOB沉积物的TOC的1.5-15.6%和TN的3.7-50.0%。

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