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Organic sulfur: A spatially variable and understudied component of marine organic matter

机译:有机硫:海洋有机物的空间可变和升级成分

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Sulfur (S) is a major heteroatom in organic matter. This project evaluated spatial variability in the concentration and molecular‐level composition of organic sulfur along gradients of depth and latitude. We measured the concentration of total organic sulfur (TOS) directly from whole seawater. Our data reveal high variability in organic sulfur, relative to established variability in total organic carbon or nitrogen. The deep ocean contained significant amounts of organic sulfur, and the concentration of TOS in North Atlantic Deep Water (NADW) decreased with increasing age while total organic carbon remained stable. Analysis of dissolved organic matter extracts by ultrahigh resolution mass spectrometry revealed that 6% of elemental formulas contained sulfur. The sulfur‐containing compounds were structurally diverse, and showed higher numbers of sulfur‐containing elemental formulas as NADW moved southward. These measurements of organic sulfur in seawater provide the foundation needed to define the factors controlling organic sulfur in the global ocean.
机译:硫(s)是有机物质中的主要杂原子。该项目评估了沿着深度和纬度梯度的有机硫的浓度和分子水平组成的空间变异性。我们将总有机硫(TOS)的浓度直接从整个海水中测量。我们的数据揭示了有机硫的高变异性,相对于总有机碳或氮的既定变异性。深海含有大量的有机硫,北大西洋深水(NADW)的TO浓度随着年龄的增加而降低,而总有机碳保持稳定。超高分辨率质谱法分析溶解有机物提取物,显示出6%的元素公式含有硫。含硫化合物在结构上是多样的,并且显示出较高数量的含硫元素公式,因为纳氏升起向南移动。这些海水中有机硫的测量提供了定义控制全球海洋有机硫的因素所需的基础。

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