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- W2092814661 abstract "Significance The vertical supply of dissolved Fe (iron) is insufficient compared with the physiological needs of marine phytoplankton in vast swathes of the open ocean. However, the relative importance of the main sources of “new” Fe to the ocean—continental mineral dust, hydrothermal exhalations, and sediment dissolution—and their temporal evolution are poorly constrained. By analyzing the isotopic composition of Fe in marine sediments, we find that much of the dissolved Fe in the central Pacific Ocean originated from hydrothermal and sedimentary sources thousands of meters below the sea surface. As such, these data underscore the vital role of the oceans’ physical mixing in determining if any deeply sourced Fe ever reaches the Fe-starved surface-dwelling biota." @default.
- W2092814661 created "2016-06-24" @default.
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- W2092814661 date "2015-01-20" @default.
- W2092814661 modified "2023-10-17" @default.
- W2092814661 title "Persistence of deeply sourced iron in the Pacific Ocean" @default.
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- W2092814661 doi "https://doi.org/10.1073/pnas.1420188112" @default.
- W2092814661 hasPubMedCentralId "https://www.ncbi.nlm.nih.gov/pmc/articles/4321247" @default.
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