4.3 Article

Horizontal distribution of particulate matter and its characterization using phosphorus as an indicator in surface coastal water, Harima-Nada, the Seto Inland Sea, Japan

Journal

JOURNAL OF OCEANOGRAPHY
Volume 70, Issue 3, Pages 277-287

Publisher

SPRINGER
DOI: 10.1007/s10872-014-0230-z

Keywords

Particulate phosphorus (PP); Particulate inorganic phosphorus (PIP); Phytoplankton; Vertical mixing; Seto Inland Sea; Harima-Nada

Categories

Funding

  1. JSPS [2331007]

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To study the horizontal distribution and characterization of suspended particulate matter (SPM) in the coastal environment, the distribution and seasonal variation of particulate phosphorus (PP), divided as organic (POP) and inorganic (PIP) fractions with POC, PON, and Chl.a, in 4 seasons throughout Harima-Nada of the Seto Inland Sea, Japan, were investigated. A high concentration of PIP was observed not only in the northern coastal area, which received much freshwater discharge, but also in the channel parts. In winter, when Delta sigma t was low, the difference between surface and bottom sigma t, resuspension of sinking particles or/and surface sediment which has a high PIP/PP ratio seems to have occurred, and then a high concentration of PIP in surface water was observed. In spring and summer, PIP/PP ratios (0.24) of surface waters were close to those of phytoplankton (0.1-0.2). On the other hand, PIP/PP ratios in autumn and winter, when Delta sigma t was low, were similar to those of surface sediment in Harima-Nada (0.32-0.39). SPM in Harima-Nada showed higher PP contents than other coastal environments, and its mean value of 9.10 mg P/g was close to the phytoplankton P content of 9.75 mg P/g. This suggests that SPM in Harima-Nada was strongly affected by phytoplankton. The C/N ratio in Harima-Nada in spring was high (11), although high Chl.a and low PIP/PP were observed, possibly resulting from preferential decomposition of nitrogen in comparison with carbon. We consider that the PIP/PP ratio is a good indicator to characterize SPM and to predict its origin as well as the C/N.

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