Limnology and Oceanography, Vol. 62, No. 5 (September 2017), pp. 2004-2022 (19 pages) It is well known that phytoplankton growth is broadly limited by iron (Fe) availability in the subarctic Pacific.
Iron isotope fractionation has emerged as a critical tracer for deciphering the complex biogeochemical cycling of iron in soils. This process, whereby natural variations in the relative abundance of ...
Sean M. McAllister, Joshua M. Barnett, James W. Heiss, Alyssa J. Findlay, Daniel J. MacDonald, Charles L. Dow, George W. Luther III, Holly A. Michael, Clara S. Chan, Dynamic hydrologic and ...
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