Size distribution of particulate trace elements in the U.S. GEOTRACES Eastern Pacific Zonal Transect (GP16)

Particles play an important role in the cycling of many trace elements in the ocean by transporting them to the deep sea. As a particle's settling speed and rates of interaction with dissolved species and other particles depend partly on its size, it is essential to understand the distribution...

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Bibliographic Details
Published in:Marine chemistry 2018-04, Vol.201, p.108-123
Main Authors: Lee, Jong-Mi, Heller, Maija I., Lam, Phoebe J.
Format: Article
Language:English
Subjects:
GEOTRACES
Hydrothermal
Nepheloid layers
OMZ
Particle dynamics
Particles
Sciences of the Universe
Size distribution
Trace elements
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Summary:Particles play an important role in the cycling of many trace elements in the ocean by transporting them to the deep sea. As a particle's settling speed and rates of interaction with dissolved species and other particles depend partly on its size, it is essential to understand the distribution of trace elements in small (suspended) vs. large (sinking) particles and its controlling factors. Here we present the size-distribution of ten particulate trace elements (pTEs; Al, Cd, Co, Cu, Fe, Mn, Ni, P, Ti, and V) from the Eastern Tropical South Pacific collected during the U.S. GEOTRACES GP16 cruise. The surface waters at all stations (surface), subsurface waters west of 100°W (subsurface), oxygen minimum zone (OMZ) off Peru, hydrothermal plume from the East Pacific Rise (HT), and benthic nepheloid layer (BNL) show distinct pTE concentrations. In these regions, certain elements are found more in the large size fraction (LSF, >51μm): V within the surface, Al, Ti, and Fe in the subsurface, and most elements in the OMZ, HT, and BNL, whereas pTEs are >80% partitioned to the small size fraction (SSF, 0.8–51μm) in the rest of the section. The higher partitioning of pTEs to the LSF in these regions is likely a result of higher V quota of large-size particles (e.g., diatom) (surface) and enhanced particle aggregation relative to disaggregation in these regions caused by the cycling of organic particles (subsurface), increased particle density (OMZ, BNL, HT) or lack of zooplankton-mediated disaggregation (OMZ). Several groups of elements appear to have similar concentration distribution and size partitioning depending on the particle phase (lithogenic, biogenic, Fe oxyhydroxides, and Mn oxides) that each element is mainly associated with. This result implies that the elements occurring in the same particle phase not only have similar sources and sinks, but also are affected by similar particle cycling processes within the ocean. •Full water column section of size-fractionated pTE concentrations•pTEs are highly partitioned to large particles in the OMZ, BNL, and hydrothermal plume.•Particle dynamics causes subsurface minima for small lithogenic particles in the gyre.•Vanadium is highly partitioned to large particles in the surface mixed layer.•Similar size-partitioning of pTEs for the elements associated with the same type of particles
ISSN:0304-4203
1872-7581
DOI:10.1016/j.marchem.2017.09.006