Fukushima 137Cs at the base of planktonic food webs off Japan

dc.contributor.author Baumann, Zofia
dc.contributor.author Fisher, Nicholas S.
dc.contributor.author Gobler, Christopher J.
dc.contributor.author Buesseler, Ken O.
dc.contributor.author George, J. A.
dc.contributor.author Breier, Crystaline F.
dc.contributor.author Nishikawa, Jun
dc.date.accessioned 2016-01-14T16:05:45Z
dc.date.available 2016-09-25T08:38:29Z
dc.date.issued 2015-09-18
dc.description © The Author(s), 2015. This is the author's version of the work and is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Deep Sea Research Part I: Oceanographic Research Papers 106 (2015): 9-16, doi:10.1016/j.dsr.2015.09.006. en_US
dc.description.abstract The potential bioaccumulation of 137Cs in marine food webs off Japan became a concern following the release of radioactive contaminants from the damaged Fukushima nuclear power plant into the coastal ocean. Previous studies suggest that 137Cs activities increase with trophic level in pelagic food webs, however, the bioaccumulation of 137Cs from seawater to primary producers, to zooplankton has not been evaluated in the field. Since phytoplankton are frequently the largest component of SPM (suspended particulate matter) we used SPM concentrations and particle-associated 137Cs to understand bioaccumulation of 137Cs in through trophic pathways in the field. We determined particle-associated 137Cs for samples collected at 20 m depth from six stations off Japan three months after the initial release from the Fukushima nuclear power plant. At 20 m SPM ranged from 0.65 to 1.60 mg L-1 and rapidly declined with depth. The ratios of particulate organic carbon to chlorophyll a suggested that phytoplankton comprised much of the SPM in these samples. 137Cs activities on particles accounted for on average 0.04% of the total 137Cs in seawater samples, and measured concentration factors of 137Cs on small suspended particles were comparatively low (~102). However, when 137Cs in crustacean zooplankton was derived based only on modeling dietary 137Cs uptake, we found predicted and measured 137Cs concentrations in good agreement. We therefore postulate the possibility that the dietary route of 137Cs bioaccumulation (i.e., phytoplankton ingestion) could be largely responsible for the measured levels in the copepod-dominated (%) zooplankton assemblages in Japanese coastal waters. Finally, our data did not support the notion that zooplankton grazing on phytoplankton results in a biomagnification of 137Cs. en_US
dc.description.embargo 2016-09-25 en_US
dc.description.sponsorship This project was funded by the Gordon and Betty Moore Foundation through Grants GBMF3007 and GBMF 3423, and JSPS KAKENHI Grant-in-Aid for Scientific Research on Innovative Areas Grant Number 24110005. en_US
dc.format.mimetype application/pdf
dc.identifier.uri https://hdl.handle.net/1912/7728
dc.language.iso en_US en_US
dc.relation.uri https://doi.org/10.1016/j.dsr.2015.09.006
dc.rights Attribution-NonCommercial-NoDerivs 3.0 United States *
dc.rights.uri http://creativecommons.org/licenses/by-nc-nd/3.0/us/ *
dc.subject Fukushima en_US
dc.subject Cesium en_US
dc.subject Trophic transfer en_US
dc.subject Phytoplankton en_US
dc.subject Zooplankton en_US
dc.title Fukushima 137Cs at the base of planktonic food webs off Japan en_US
dc.type Preprint en_US
dspace.entity.type Publication
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