Variability in dissolved organic matter optical properties in surface waters in the Amerasian Basin

Surface absorption and fluorescence measurements of Dissolved Organic Matter (DOM) were conducted along with hydrographic parameters in the Canada and Makarov Basins. Parallel factor analysis of DOM fluorescence identified four humic-like and one protein-like component in all 107 surface samples. Ba...

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Main Authors: Celine eGueguen, Motoyo eItoh, Takashi eKikuchi, Jane eEert, William J. Williams
Format: Article
Language:English
Published: Frontiers Media S.A. 2015-10-01
Series:Frontiers in Marine Science
Subjects:
Online Access:http://journal.frontiersin.org/Journal/10.3389/fmars.2015.00078/full
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spelling doaj-f66c835514b14b03b4ea97781eff0c772020-11-24T22:25:30ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452015-10-01210.3389/fmars.2015.00078159770Variability in dissolved organic matter optical properties in surface waters in the Amerasian BasinCeline eGueguen0Motoyo eItoh1Takashi eKikuchi2Jane eEert3William J. Williams4Trent UniversityJapan Agency for Marine-Earth Science and TechnologyJapan Agency for Marine-Earth Science and TechnologyDepartment of Fisheries and OceanDepartment of Fisheries and OceanSurface absorption and fluorescence measurements of Dissolved Organic Matter (DOM) were conducted along with hydrographic parameters in the Canada and Makarov Basins. Parallel factor analysis of DOM fluorescence identified four humic-like and one protein-like component in all 107 surface samples. Based on strong negative trends observed between the spectral slope in the 275-295 nm range and absorption at 370 nm, and four humic-like components C1-C4, the DOM character was found to be basin-dependent. The Makarov basin surface DOM was largely dominated by high molecular weight and humic-rich material whereas the Canada Basin surface DOM was more heterogeneous with a marked influence of in situ production. This study highlights that absorbing and fluorescing measurements can be used successfully to trace and differentiate DOM from diverse sources and across frontal zones, and as such can be convenient and complementary tools for the better understanding of marine biogeochemical cycling of carbon.http://journal.frontiersin.org/Journal/10.3389/fmars.2015.00078/fullIce CoverCanada BasinCDOMMakarov BasinFDOMfrontal zone
collection DOAJ
language English
format Article
sources DOAJ
author Celine eGueguen
Motoyo eItoh
Takashi eKikuchi
Jane eEert
William J. Williams
spellingShingle Celine eGueguen
Motoyo eItoh
Takashi eKikuchi
Jane eEert
William J. Williams
Variability in dissolved organic matter optical properties in surface waters in the Amerasian Basin
Frontiers in Marine Science
Ice Cover
Canada Basin
CDOM
Makarov Basin
FDOM
frontal zone
author_facet Celine eGueguen
Motoyo eItoh
Takashi eKikuchi
Jane eEert
William J. Williams
author_sort Celine eGueguen
title Variability in dissolved organic matter optical properties in surface waters in the Amerasian Basin
title_short Variability in dissolved organic matter optical properties in surface waters in the Amerasian Basin
title_full Variability in dissolved organic matter optical properties in surface waters in the Amerasian Basin
title_fullStr Variability in dissolved organic matter optical properties in surface waters in the Amerasian Basin
title_full_unstemmed Variability in dissolved organic matter optical properties in surface waters in the Amerasian Basin
title_sort variability in dissolved organic matter optical properties in surface waters in the amerasian basin
publisher Frontiers Media S.A.
series Frontiers in Marine Science
issn 2296-7745
publishDate 2015-10-01
description Surface absorption and fluorescence measurements of Dissolved Organic Matter (DOM) were conducted along with hydrographic parameters in the Canada and Makarov Basins. Parallel factor analysis of DOM fluorescence identified four humic-like and one protein-like component in all 107 surface samples. Based on strong negative trends observed between the spectral slope in the 275-295 nm range and absorption at 370 nm, and four humic-like components C1-C4, the DOM character was found to be basin-dependent. The Makarov basin surface DOM was largely dominated by high molecular weight and humic-rich material whereas the Canada Basin surface DOM was more heterogeneous with a marked influence of in situ production. This study highlights that absorbing and fluorescing measurements can be used successfully to trace and differentiate DOM from diverse sources and across frontal zones, and as such can be convenient and complementary tools for the better understanding of marine biogeochemical cycling of carbon.
topic Ice Cover
Canada Basin
CDOM
Makarov Basin
FDOM
frontal zone
url http://journal.frontiersin.org/Journal/10.3389/fmars.2015.00078/full
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AT takashiekikuchi variabilityindissolvedorganicmatteropticalpropertiesinsurfacewatersintheamerasianbasin
AT janeeeert variabilityindissolvedorganicmatteropticalpropertiesinsurfacewatersintheamerasianbasin
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