从沼泽到海洋:利用氢同位素比率量化热带陆架海中的陆地溶解有机碳

IF 2.6 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
A’an Johan Wahyudi , Nikita Kaushal , Cristian Gudasz , Patrick Martin
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引用次数: 0

摘要

溶解有机碳(DOC)是沿岸生物地球化学循环的一个重要组成部分,但其组成和反 应能力取决于自生水生 DOC 和异生陆生 DOC(tDOC)的相对贡献。在复杂的沿岸水域,tDOC 通常是用大体积 DOC 稳定碳同位素比值(δ13CDOC)来量化的。然而,δ13CDOC 在海洋生态系统中的应用受到一些限制,例如:(1)自生和异生内含物之间的分隔范围较窄,而且经常重叠;(2)tDOC 矿化为溶解的无机碳会产生储层效应,使自生 DOC 获得类似于原生 DOC 的δ13CDOC。DOC 中不可交换氢的稳定同位素比值(δ2Hn)作为一种新工具,有可能克服这些局限性:(1)δ2Hn 在水生和陆生内含物之间有很大的分隔(50‰);(2)它不受 tDOC 矿化造成的储层效应的影响。在此,我们评估了从固相萃取溶解有机物(SPE-DOM)中获得的δ2Hn的潜力,并将其与δ13CDOC和色度DOM(CDOM)的光学性质进行了比较。我们在东南亚巽他陆架的一个地点采集了样本,该地点的 tDOC 输入量季节性变化很大,主要受季风引起的泥炭地 tDOC 物理平流的影响。在为期一年的月度时间序列中,使用 SPE-DOM 的 δ2Hn 和大体积 DOC 的 δ13CDOC 测定的 DOC 的陆生部分(fterr)具有良好的相关性(r2 = 0.42),两种同位素系统之间的 fterr 没有显著差异。事实上,与δ13CDOC相比,δ2Hn与盐度和CDOM光学特性的相关性稍强。我们的研究结果表明,SPE-DOM 的 δ2Hn 能有效地量化沿岸梯度的 tDOC,可能比 δ13CDOC 具有更高的灵敏度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
From swamp to sea: Quantifying terrestrial dissolved organic carbon in a tropical shelf sea using hydrogen isotope ratios

Dissolved organic carbon (DOC) is a key component of coastal biogeochemical cycles, but its composition and reactivity depend on the relative contribution of autochthonous aquatic versus allochthonous terrigenous DOC (tDOC). In complex coastal waters, tDOC is commonly quantified using the bulk DOC stable carbon isotope ratio (δ13CDOC). However, several limitations can hamper the use of δ13CDOC in marine ecosystems, such as (1) the narrow and often overlapping separation of the autochthonous and allochthonous endmembers, and (2) mineralization of tDOC to dissolved inorganic carbon creates a reservoir effect such that autochthonous DOC can acquire a terrigenous-like δ13CDOC. The stable isotope ratio of non-exchangeable hydrogen in the DOC (δ2Hn) has emerged as a new tool that can potentially overcome these limitations: (1) δ2Hn has a large separation between aquatic and terrigenous endmembers (>50‰) and (2) it is not subject to reservoir effects caused by tDOC mineralization. Here, we evaluate the potential of δ2Hn obtained from solid phase-extracted dissolved organic matter (SPE-DOM), by comparing it to δ13CDOC and chromophoric DOM (CDOM) optical properties. We collected samples at a site in Southeast Asia’s Sunda Shelf that experiences substantial seasonal variation in tDOC input, driven primarily by the monsoon-induced physical advection of peatland-derived tDOC. Over a 1-year monthly time series, the terrigenous fraction of DOC (fterr) determined using δ2Hn of SPE-DOM and δ13CDOC of bulk DOC was well correlated (r2 = 0.42), and there was no significant difference in fterr between the two isotope systems. In fact, δ2Hn displayed slightly stronger correlations with salinity and CDOM optical properties compared to δ13CDOC. Our results indicate that δ2Hn of SPE-DOM is effective for quantifying tDOC across coastal gradients, potentially offering greater sensitivity than δ13CDOC, and is a viable alternative in settings where δ13CDOC is inadequate.

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来源期刊
Organic Geochemistry
Organic Geochemistry 地学-地球化学与地球物理
CiteScore
5.50
自引率
6.70%
发文量
100
审稿时长
61 days
期刊介绍: Organic Geochemistry serves as the only dedicated medium for the publication of peer-reviewed research on all phases of geochemistry in which organic compounds play a major role. The Editors welcome contributions covering a wide spectrum of subjects in the geosciences broadly based on organic chemistry (including molecular and isotopic geochemistry), and involving geology, biogeochemistry, environmental geochemistry, chemical oceanography and hydrology. The scope of the journal includes research involving petroleum (including natural gas), coal, organic matter in the aqueous environment and recent sediments, organic-rich rocks and soils and the role of organics in the geochemical cycling of the elements. Sedimentological, paleontological and organic petrographic studies will also be considered for publication, provided that they are geochemically oriented. Papers cover the full range of research activities in organic geochemistry, and include comprehensive review articles, technical communications, discussion/reply correspondence and short technical notes. Peer-reviews organised through three Chief Editors and a staff of Associate Editors, are conducted by well known, respected scientists from academia, government and industry. The journal also publishes reviews of books, announcements of important conferences and meetings and other matters of direct interest to the organic geochemical community.
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