Bioaccumulation of methylmercury within the marine food web of the outer Bay of Fundy, Gulf of Maine.

Mercury and methylmercury were measured in seawater and biota collected from the outer Bay of Fundy to better document mercury bioaccumulation in a temperate marine food web. The size of an organism, together with δ13 C and δ15 N isotopes, were measured to interpret mercury levels in biota ranging i...

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Published in:PLOS ONE
Main Authors: Gareth Harding, John Dalziel, Peter Vass
Format: Article in Journal/Newspaper
Language:English
Published: Public Library of Science (PLoS) 2018
Subjects:
R
Q
Online Access:https://doi.org/10.1371/journal.pone.0197220
https://doaj.org/article/c079823b99e640c8bc7aa1145bbbf403
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spelling ftdoajarticles:oai:doaj.org/article:c079823b99e640c8bc7aa1145bbbf403 2023-05-15T15:13:42+02:00 Bioaccumulation of methylmercury within the marine food web of the outer Bay of Fundy, Gulf of Maine. Gareth Harding John Dalziel Peter Vass 2018-01-01T00:00:00Z https://doi.org/10.1371/journal.pone.0197220 https://doaj.org/article/c079823b99e640c8bc7aa1145bbbf403 EN eng Public Library of Science (PLoS) http://europepmc.org/articles/PMC6047777?pdf=render https://doaj.org/toc/1932-6203 1932-6203 doi:10.1371/journal.pone.0197220 https://doaj.org/article/c079823b99e640c8bc7aa1145bbbf403 PLoS ONE, Vol 13, Iss 7, p e0197220 (2018) Medicine R Science Q article 2018 ftdoajarticles https://doi.org/10.1371/journal.pone.0197220 2022-12-31T12:23:48Z Mercury and methylmercury were measured in seawater and biota collected from the outer Bay of Fundy to better document mercury bioaccumulation in a temperate marine food web. The size of an organism, together with δ13 C and δ15 N isotopes, were measured to interpret mercury levels in biota ranging in size from microplankton (25μm) to swordfish, dolphins and whales. Levels of mercury in seawater were no different with depth and not elevated relative to upstream sources. The δ13 C values of primary producers were found to be inadequate to specify the original energy source of various faunas, however, there was no reason to separate the food web into benthic, demersal and pelagic food chains because phytoplankton has been documented to almost exclusively fuel the ecosystem. The apparent abrupt increase in mercury content from "seawater" to phytoplankton, on a wet weight basis, can be explained from an environmental volume basis by the exponential increase in surface area of smaller particles included in "seawater" determinations. This physical sorption process may be important up to the macroplankton size category dominated by copepods according to the calculated biomagnification factors (BMF). The rapid increase in methylmercury concentration, relative to the total mercury, between the predominantly phytoplankton (<125μm) and the zooplankton categories is likely augmented by gut microbe methylation. Further up the food chain, trophic transfer of methylmercury dominates resulting in biomagnification factors greater than 10 in swordfish, Atlantic bluefin tuna, harbour porpoise, Atlantic white-sided dolphin and common thresher shark. The biomagnification power of the northern Gulf of Maine ecosystem is remarkably similar to that measured in tropical, subtropical, other temperate and arctic oceanic ecozones. Article in Journal/Newspaper Arctic Harbour porpoise Phytoplankton Zooplankton Copepods Directory of Open Access Journals: DOAJ Articles Arctic PLOS ONE 13 7 e0197220
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Gareth Harding
John Dalziel
Peter Vass
Bioaccumulation of methylmercury within the marine food web of the outer Bay of Fundy, Gulf of Maine.
topic_facet Medicine
R
Science
Q
description Mercury and methylmercury were measured in seawater and biota collected from the outer Bay of Fundy to better document mercury bioaccumulation in a temperate marine food web. The size of an organism, together with δ13 C and δ15 N isotopes, were measured to interpret mercury levels in biota ranging in size from microplankton (25μm) to swordfish, dolphins and whales. Levels of mercury in seawater were no different with depth and not elevated relative to upstream sources. The δ13 C values of primary producers were found to be inadequate to specify the original energy source of various faunas, however, there was no reason to separate the food web into benthic, demersal and pelagic food chains because phytoplankton has been documented to almost exclusively fuel the ecosystem. The apparent abrupt increase in mercury content from "seawater" to phytoplankton, on a wet weight basis, can be explained from an environmental volume basis by the exponential increase in surface area of smaller particles included in "seawater" determinations. This physical sorption process may be important up to the macroplankton size category dominated by copepods according to the calculated biomagnification factors (BMF). The rapid increase in methylmercury concentration, relative to the total mercury, between the predominantly phytoplankton (<125μm) and the zooplankton categories is likely augmented by gut microbe methylation. Further up the food chain, trophic transfer of methylmercury dominates resulting in biomagnification factors greater than 10 in swordfish, Atlantic bluefin tuna, harbour porpoise, Atlantic white-sided dolphin and common thresher shark. The biomagnification power of the northern Gulf of Maine ecosystem is remarkably similar to that measured in tropical, subtropical, other temperate and arctic oceanic ecozones.
format Article in Journal/Newspaper
author Gareth Harding
John Dalziel
Peter Vass
author_facet Gareth Harding
John Dalziel
Peter Vass
author_sort Gareth Harding
title Bioaccumulation of methylmercury within the marine food web of the outer Bay of Fundy, Gulf of Maine.
title_short Bioaccumulation of methylmercury within the marine food web of the outer Bay of Fundy, Gulf of Maine.
title_full Bioaccumulation of methylmercury within the marine food web of the outer Bay of Fundy, Gulf of Maine.
title_fullStr Bioaccumulation of methylmercury within the marine food web of the outer Bay of Fundy, Gulf of Maine.
title_full_unstemmed Bioaccumulation of methylmercury within the marine food web of the outer Bay of Fundy, Gulf of Maine.
title_sort bioaccumulation of methylmercury within the marine food web of the outer bay of fundy, gulf of maine.
publisher Public Library of Science (PLoS)
publishDate 2018
url https://doi.org/10.1371/journal.pone.0197220
https://doaj.org/article/c079823b99e640c8bc7aa1145bbbf403
geographic Arctic
geographic_facet Arctic
genre Arctic
Harbour porpoise
Phytoplankton
Zooplankton
Copepods
genre_facet Arctic
Harbour porpoise
Phytoplankton
Zooplankton
Copepods
op_source PLoS ONE, Vol 13, Iss 7, p e0197220 (2018)
op_relation http://europepmc.org/articles/PMC6047777?pdf=render
https://doaj.org/toc/1932-6203
1932-6203
doi:10.1371/journal.pone.0197220
https://doaj.org/article/c079823b99e640c8bc7aa1145bbbf403
op_doi https://doi.org/10.1371/journal.pone.0197220
container_title PLOS ONE
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