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Conservation of dissolved organic matter molecular composition during mixing of the deep water masses of the northeast Atlantic Ocean

机译:大西洋东北部深水团混合过程中溶解有机物分子组成的守恒

摘要

Characterizing the composition ofmarine dissolved organicmatter (DOM) is important for gaining insight into itsrole in oceanic biogeochemical cycles. Using Fourier transform ion cyclotron resonance mass spectrometry, weanalyzed the molecular composition of solid phase extracted (SPE) DOM from the northeast Atlantic to investigatethe specificity of the DOMpool of the individualmajor watermasses of the North Atlantic. All 272 measuredsamples from depths ranging from 87 to 5609 m and latitudes from 24°N to 68°N shared 96% similarity (on aBray–Curtis scale) in their DOM composition. Small variations between subsurface and deep samples andamong latitudinal groupings were identified, but overall, water mass specific SPE-DOM composition was notapparent. A strong correlation between a calculated degradation index and water mass age indicates variabilityin portions of the DOM pool, and ocean-scale differences were observed between the North Atlantic and deepNorth Pacific. However, within the deep northeast Atlantic, conservative mixing primarily drives the molecularcomposition of SPE-DOM.
机译:表征海洋溶解有机物(DOM)的组成对于深入了解海洋生物地球化学循环中的甲壳素至关重要。使用傅里叶变换离子回旋共振质谱,分析了东北大西洋固相萃取(SPE)DOM的分子组成,以研究北大西洋各个主要水质DOMpool的特异性。所有272个从87到5609 m的深度和24°N到68°N的纬度的测量样品在DOM组成上具有96%的相似度(在aBray–Curtis尺度上)。在地下样品和深层样品之间以及在纬度分组之间都发现了微小的变化,但是总体上,水质比值的SPE-DOM组成并不明显。计算出的降解指数与水质年龄之间的强相关性表明DOM池的各个部分存在变化,并且在北大西洋和北太平洋深海之间观察到了海洋尺度差异。但是,在大西洋东北部深部,保守混合主要驱动SPE-DOM的分子组成。

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