Variability and Export Timescales of Upper Ocean Particulate Trace Metals in the North Pacific Subtropical Gyre

IF 5.5 2区 地球科学 Q1 ENVIRONMENTAL SCIENCES
Eleanor S. Bates, Angelicque E. White, Nicholas J. Hawco
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Abstract

The transport of trace metals (TMs) in and out of the upper ocean is largely controlled by particulate phases, but the seasonal variability and residence time of these particles are not well known. Over three years and 21 cruises, we measured upper ocean particulate trace metal concentrations and export fluxes at 150 m at Station ALOHA in the North Pacific Subtropical Gyre. Vertical profiles for most metals were highest near the surface, but Al, Fe, Ni, and Cu also showed evidence of scavenging below the mixed layer. In contrast, labile particulate Mn and Cd had unique subsurface maxima driven by the photoinhibition of Mn-oxides in the euphotic zone and uptake of Cd near the base of the euphotic zone. Our sampling period captured pulses of lithogenic dust input, evident in high export fluxes of particulate Al, Ti, and Fe, which were exported on a timescale of ∼10 days. The mean export-based residence time for labile particulate Fe was 36 days, three times longer than that for recalcitrant Fe, indicating that labile particulate Fe is recycled several times before export. Particulate Cu and Co had mean residence times of 6 months, similar to particulate C, N, and P, suggesting that their export is controlled by the export of biomass. Labile particulate Mn, Ni, and Cd appear to be exported more efficiently with mean residence times of 1.8–3 months. The range of TM residence times underlines the differences in the recycling, biotic utilization, and scavenging of these metals in the upper ocean.

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北太平洋副热带环流上层海洋微粒微量金属的变率和输出时间尺度
海洋上层微量金属(TMs)的进出在很大程度上受颗粒相控制,但这些颗粒的季节变化和停留时间尚不清楚。在三年和21次巡航中,我们在北太平洋副热带环流ALOHA站测量了上层海洋颗粒微量金属浓度和150米出口通量。大多数金属的垂直剖面在地表附近最高,但Al, Fe, Ni和Cu在混合层以下也显示出清除的证据。相比之下,活性颗粒Mn和Cd具有独特的亚表面最大值,这是由光抑制区Mn-氧化物的光抑制和光区底部附近Cd的吸收驱动的。我们的采样周期捕获了岩质粉尘输入的脉冲,这在颗粒Al、Ti和Fe的高输出通量中是显而易见的,它们在约10天的时间尺度上输出。易失稳颗粒铁的平均出口停留时间为36天,是难失稳颗粒铁的3倍,说明易失稳颗粒铁在出口前经过多次回收。颗粒Cu和Co的平均停留时间为6个月,与颗粒C、N和P相似,表明它们的出口受到生物质出口的控制。在1.8 ~ 3个月的平均停留时间内,Mn、Ni、Cd等不稳定颗粒的输出效率更高。TM停留时间的范围强调了这些金属在上层海洋的回收、生物利用和清除方面的差异。
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来源期刊
Global Biogeochemical Cycles
Global Biogeochemical Cycles 环境科学-地球科学综合
CiteScore
8.90
自引率
7.70%
发文量
141
审稿时长
8-16 weeks
期刊介绍: Global Biogeochemical Cycles (GBC) features research on regional to global biogeochemical interactions, as well as more local studies that demonstrate fundamental implications for biogeochemical processing at regional or global scales. Published papers draw on a wide array of methods and knowledge and extend in time from the deep geologic past to recent historical and potential future interactions. This broad scope includes studies that elucidate human activities as interactive components of biogeochemical cycles and physical Earth Systems including climate. Authors are required to make their work accessible to a broad interdisciplinary range of scientists.
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