Eleanor S. Bates, Angelicque E. White, Nicholas J. Hawco
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引用次数: 0
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.
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.