Dynamic manganese cycling in the northern Gulf of Mexico

IF 3 3区 地球科学 Q2 CHEMISTRY, MULTIDISCIPLINARY Marine Chemistry Pub Date : 2024-11-01 DOI:10.1016/j.marchem.2024.104466
Jessalyn E. Davis , Rebecca S. Robinson , Emily R. Estes , Veronique E. Oldham , Evan A. Solomon , Roger P. Kelly , Katherine E. Bell , Joseph A. Resing , Randelle M. Bundy
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Abstract

Transport processes along the river-ocean continuum influence delivery of nutrients, carbon and trace metals from terrestrial systems to the marine environment, impacting coastal primary productivity and water quality. Although trace metal transformations have been studied extensively in the Mississippi River Delta region of the Northern Gulf of Mexico, investigations of manganese (Mn) and the presence of ligand-stabilized, dissolved manganese (Mn(III)-L) and its role in the transformation of trace elements and organic matter during riverine transport and estuarine mixing have not been considered. This study examined the chemical speciation of dissolved and particulate Mn in the water column and sediment porewaters in the Mississippi River and Northern Gulf of Mexico in March of 2021 to explore transformations in Mn speciation along the river-ocean continuum and the impact of different processes on the distribution of Mn. Total dissolved Mn concentrations were highest in the Mississippi River and decreased offshore, while Mn(III)-L contributed most to the dissolved Mn pool in near-shore waters. Porewater profiles indicated that ligand stabilization prevented dissolved Mn(III) reduction below the depth of oxygen penetration and in the presence of equimolar dissolved iron(II). Dissolved Mn(III)-L was enriched in bottom waters at all Northern Gulf of Mexico stations, and diffusive flux modelling of porewater dissolved Mn suggested that reducing sediments were a source of dissolved Mn to the overlying water column in the form of both reduced Mn(II) and Mn(III)-L. A simple box model of the Mn cycle in the Northern Gulf of Mexico indicates that Mn(III)-L is required to balance the Mn budget in this region and is an integral, and previously unconsidered, piece of the Mn cycle in the Northern Gulf of Mexico. The presence of Mn(III)-L in this system likely has an outsized impact on trace element scavenging rates, oxidative capacity, and the carbon cycle that have not been previously appreciated.
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墨西哥湾北部的动态锰循环
河流-海洋连续流的传输过程影响着营养物质、碳和痕量金属从陆地系统向海洋环境 的传输,从而影响沿岸的初级生产力和水质。虽然对墨西哥湾北部密西西比河三角洲地区的痕量金属转化过程进行了广泛研究,但对锰(Mn)和配体稳定的溶解锰(Mn(III)-L)的存在及其在河流传输和河口混合过程中痕量元素和有机物转化过程中的作用还没有进行过研究。这项研究考察了 2021 年 3 月密西西比河和墨西哥湾北部水体和沉积物孔隙水中溶解锰和颗粒锰的化学形态,以探索锰形态在河流-海洋连续过程中的转变以及不同过程对锰分布的影响。密西西比河的溶解锰总浓度最高,近海则有所下降,而 Mn(III)-L 在近海水域的溶解锰池中占比最大。孔隙水剖面显示,配体稳定化阻止了溶解锰(III)在氧气渗透深度以下和等摩尔溶解铁(II)存在时的还原。墨西哥湾北部所有站点的底层水都富含溶解锰(III)-L,孔隙水溶解锰的扩散通量模型表明,还原沉积物是以还原锰(II)和锰(III)-L 两种形式向上层水体提供溶解锰的来源。墨西哥湾北部锰循环的一个简单箱式模型表明,Mn(III)-L 是平衡该地区锰预算所必需的,也是墨西哥湾北部锰循环中不可或缺的、以前未被考虑的一部分。该系统中 Mn(III)-L 的存在很可能对微量元素清除率、氧化能力和碳循环产生了巨大影响,而这一点以前尚未得到重视。
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来源期刊
Marine Chemistry
Marine Chemistry 化学-海洋学
CiteScore
6.00
自引率
3.30%
发文量
70
审稿时长
4.5 months
期刊介绍: Marine Chemistry is an international medium for the publication of original studies and occasional reviews in the field of chemistry in the marine environment, with emphasis on the dynamic approach. The journal endeavours to cover all aspects, from chemical processes to theoretical and experimental work, and, by providing a central channel of communication, to speed the flow of information in this relatively new and rapidly expanding discipline.
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