Geographic Variation of Particle Size Distribution in the Kuroshio Region: Possible Causes in the Upper Water Column

Particle size distribution (PSD) in the ocean is a fundamental property that influences carbon export and food webs; however, PSD variation and its causes in oligotrophic oceans are not entirely clear. Here, we used Laser In-Situ Scattering and Transmissometry to investigate PSD (size range 5.2–119...

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Autores principales: Yosuke Yamada, Hideki Fukuda, Yu Umezawa, Toshi Nagata
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Publicado: Frontiers Media S.A. 2021
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spelling oai:doaj.org-article:491f33721fbb4ac997f53c822d53eeda2021-11-16T04:49:51ZGeographic Variation of Particle Size Distribution in the Kuroshio Region: Possible Causes in the Upper Water Column2296-774510.3389/fmars.2021.768766https://doaj.org/article/491f33721fbb4ac997f53c822d53eeda2021-11-01T00:00:00Zhttps://www.frontiersin.org/articles/10.3389/fmars.2021.768766/fullhttps://doaj.org/toc/2296-7745Particle size distribution (PSD) in the ocean is a fundamental property that influences carbon export and food webs; however, PSD variation and its causes in oligotrophic oceans are not entirely clear. Here, we used Laser In-Situ Scattering and Transmissometry to investigate PSD (size range 5.2–119 μm) and related variables at 11 stations in the surface layer (0–20 m) of the Kuroshio region of the western North Pacific, where strong current causes dynamic hydrographic and ecological conditions. PSD slopes (range –3.2 to –4.2), derived from the power law model, were steeper at onshore stations and flatter at oligotrophic stations located offshore and at lower latitudes. Notably, slopes tended to become steeper with increasing chlorophyll a concentration, opposing the generally observed relationship between the two variables, whereas they became flatter with increasing transparent exopolymer particle (TEP) concentration. Possible explanations of the above results are localized occurrence of nanophytoplankton and TEP facilitation of particle aggregation. The results support the hypothesis that PSD slopes are controlled by a multitude of factors, including phytoplankton community dynamics and aggregation processes. To determine whether TEP-induced particle aggregation enhances or suppresses carbon export, we need a better understanding of the nature (porosity, density, and sinking velocity) of aggregates in oligotrophic oceans.Yosuke YamadaHideki FukudaYu UmezawaToshi NagataFrontiers Media S.A.articleslope of particle size distributionchlorophyll atransparent exopolymer particles (TEP)Kuroshionanophytoplanktonparticle aggregationScienceQGeneral. Including nature conservation, geographical distributionQH1-199.5ENFrontiers in Marine Science, Vol 8 (2021)
institution DOAJ
collection DOAJ
language EN
topic slope of particle size distribution
chlorophyll a
transparent exopolymer particles (TEP)
Kuroshio
nanophytoplankton
particle aggregation
Science
Q
General. Including nature conservation, geographical distribution
QH1-199.5
spellingShingle slope of particle size distribution
chlorophyll a
transparent exopolymer particles (TEP)
Kuroshio
nanophytoplankton
particle aggregation
Science
Q
General. Including nature conservation, geographical distribution
QH1-199.5
Yosuke Yamada
Hideki Fukuda
Yu Umezawa
Toshi Nagata
Geographic Variation of Particle Size Distribution in the Kuroshio Region: Possible Causes in the Upper Water Column
description Particle size distribution (PSD) in the ocean is a fundamental property that influences carbon export and food webs; however, PSD variation and its causes in oligotrophic oceans are not entirely clear. Here, we used Laser In-Situ Scattering and Transmissometry to investigate PSD (size range 5.2–119 μm) and related variables at 11 stations in the surface layer (0–20 m) of the Kuroshio region of the western North Pacific, where strong current causes dynamic hydrographic and ecological conditions. PSD slopes (range –3.2 to –4.2), derived from the power law model, were steeper at onshore stations and flatter at oligotrophic stations located offshore and at lower latitudes. Notably, slopes tended to become steeper with increasing chlorophyll a concentration, opposing the generally observed relationship between the two variables, whereas they became flatter with increasing transparent exopolymer particle (TEP) concentration. Possible explanations of the above results are localized occurrence of nanophytoplankton and TEP facilitation of particle aggregation. The results support the hypothesis that PSD slopes are controlled by a multitude of factors, including phytoplankton community dynamics and aggregation processes. To determine whether TEP-induced particle aggregation enhances or suppresses carbon export, we need a better understanding of the nature (porosity, density, and sinking velocity) of aggregates in oligotrophic oceans.
format article
author Yosuke Yamada
Hideki Fukuda
Yu Umezawa
Toshi Nagata
author_facet Yosuke Yamada
Hideki Fukuda
Yu Umezawa
Toshi Nagata
author_sort Yosuke Yamada
title Geographic Variation of Particle Size Distribution in the Kuroshio Region: Possible Causes in the Upper Water Column
title_short Geographic Variation of Particle Size Distribution in the Kuroshio Region: Possible Causes in the Upper Water Column
title_full Geographic Variation of Particle Size Distribution in the Kuroshio Region: Possible Causes in the Upper Water Column
title_fullStr Geographic Variation of Particle Size Distribution in the Kuroshio Region: Possible Causes in the Upper Water Column
title_full_unstemmed Geographic Variation of Particle Size Distribution in the Kuroshio Region: Possible Causes in the Upper Water Column
title_sort geographic variation of particle size distribution in the kuroshio region: possible causes in the upper water column
publisher Frontiers Media S.A.
publishDate 2021
url https://doaj.org/article/491f33721fbb4ac997f53c822d53eeda
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