LotaV3, PascalFrancis, Curation, bibRecord, 000116

Low and Declining Mercury in Arctic Russian Rivers

Identifieur interne : 000116 ( PascalFrancis/Curation ); précédent : 000115; suivant : 000117

Low and Declining Mercury in Arctic Russian Rivers

Auteurs : Leandro Castello [États-Unis] ; Alexander V. Zhulidov [Russie] ; Tatiana Yu. Gurtovaya [Russie] ; Richard D. Robarts [Canada] ; Robert M. Holmes [États-Unis] ; Daniel A. Zhulidov [Russie] ; Vladimir S. Lysenko [Russie] ; Robert G. M. Spencer [États-Unis]

Source :

Environmental science & technology [ 0013-936X ] ; 2014.

RBID : Pascal:15-0009283

Descripteurs français

Pascal (Inist)
- Mercure, Arctique Russie, Cours eau, Rivière, Lota lota, Eau surface.
Wicri :
- topic : Mercure.

English descriptors

KwdEn :
- Lota lota, Mercury, Rivers, Russian Arctic, Stream, Surface water.

Abstract

Mercury (Hg) dynamics in the Arctic is receiving increasing attention, but further understanding is limited by a lack of studies in Russia, which encompasses the majority of the pan-Arctic watershed. This study reports Hg concentrations and trends in burbot (Lota lota) from the Lena and Mezen Rivers in the Russian Arctic, and assesses the extent to which they differ from those found in burbot in arctic rivers elsewhere. Mercury concentrations in burbot in the Lena and Mezen Rivers were found to be generally lower than in 23 other locations, most of which are in the Mackenzie River Basin (Canada). Mercury concentrations in burbot in the Lena and Mezen Rivers also were found to have been declining at an annual rate of 2.3% while they have been increasing in the Mackenzie River Basin at annual rates between 2.2 and 5.1% during roughly the same time period. These contrasting patterns in Hg in burbot across the pan-Arctic may be explained by geographic heterogeneity in controlling processes, including riverine particulate material loads, historically changing atmospheric inputs, postdepositional processes, and climate change impacts.

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A11	`01`	`1`		`@1 CASTELLO (Leandro)`
A11	`02`	`1`		`@1 ZHULIDOV (Alexander V.)`
A11	`03`	`1`		`@1 GURTOVAYA (Tatiana Yu.)`
A11	`04`	`1`		`@1 ROBARTS (Richard D.)`
A11	`05`	`1`		`@1 HOLMES (Robert M.)`
A11	`06`	`1`		`@1 ZHULIDOV (Daniel A.)`
A11	`07`	`1`		`@1 LYSENKO (Vladimir S.)`
A11	`08`	`1`		`@1 SPENCER (Robert G. M.)`
A14	`01`			`@1 Virginia Polytechnic Institute and State University @2 Blacksburg, Virginia 24061 @3 USA @Z 1 aut.`
A14	`02`			`@1 South Russian Centre for Preparation and Implementation of International Projects @2 Rostov-on-Don @3 RUS @Z 2 aut. @Z 3 aut. @Z 6 aut.`
A14	`03`			`@1 World Water and Climate Foundation @2 Saskatoon, Saskatchewan @3 CAN @Z 4 aut.`
A14	`04`			`@1 Woods Hole Research Center @2 Falmouth, Massachusetts 02540 @3 USA @Z 5 aut. @Z 8 aut.`
A14	`05`			`@1 South Federal University, Institute of Biology @2 Rostov-on-Don @3 RUS @Z 7 aut.`
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C01	`01`		`ENG`	@0 Mercury (Hg) dynamics in the Arctic is receiving increasing attention, but further understanding is limited by a lack of studies in Russia, which encompasses the majority of the pan-Arctic watershed. This study reports Hg concentrations and trends in burbot (Lota lota) from the Lena and Mezen Rivers in the Russian Arctic, and assesses the extent to which they differ from those found in burbot in arctic rivers elsewhere. Mercury concentrations in burbot in the Lena and Mezen Rivers were found to be generally lower than in 23 other locations, most of which are in the Mackenzie River Basin (Canada). Mercury concentrations in burbot in the Lena and Mezen Rivers also were found to have been declining at an annual rate of 2.3% while they have been increasing in the Mackenzie River Basin at annual rates between 2.2 and 5.1% during roughly the same time period. These contrasting patterns in Hg in burbot across the pan-Arctic may be explained by geographic heterogeneity in controlling processes, including riverine particulate material loads, historically changing atmospheric inputs, postdepositional processes, and climate change impacts.
C02	`01`	`X`		`@0 002A14D05H1`
C03	`01`	`X`	`FRE`	`@0 Mercure @2 NC @2 FX @5 02`
C03	`01`	`X`	`ENG`	`@0 Mercury @2 NC @2 FX @5 02`
C03	`01`	`X`	`SPA`	`@0 Mercurio @2 NC @2 FX @5 02`
C03	`02`	`X`	`FRE`	`@0 Arctique Russie @2 NG @5 03`
C03	`02`	`X`	`ENG`	`@0 Russian Arctic @2 NG @5 03`
C03	`02`	`X`	`SPA`	`@0 Ártico Rusia @2 NG @5 03`
C03	`03`	`X`	`FRE`	`@0 Cours eau @5 05`
C03	`03`	`X`	`ENG`	`@0 Stream @5 05`
C03	`03`	`X`	`SPA`	`@0 Curso agua @5 05`
C03	`04`	`X`	`FRE`	`@0 Rivière @5 06`
C03	`04`	`X`	`ENG`	`@0 Rivers @5 06`
C03	`04`	`X`	`SPA`	`@0 Río @5 06`
C03	`05`	`X`	`FRE`	`@0 Lota lota @2 NS @5 08`
C03	`05`	`X`	`ENG`	`@0 Lota lota @2 NS @5 08`
C03	`05`	`X`	`SPA`	`@0 Lota lota @2 NS @5 08`
C03	`06`	`X`	`FRE`	`@0 Eau surface @5 09`
C03	`06`	`X`	`ENG`	`@0 Surface water @5 09`
C03	`06`	`X`	`SPA`	`@0 Agua superficie @5 09`
C07	`01`	`X`	`FRE`	`@0 Russie @2 NG`
C07	`01`	`X`	`ENG`	`@0 Russian Federation @2 NG`
C07	`01`	`X`	`SPA`	`@0 Federación de Rusia @2 NG`
C07	`02`	`X`	`FRE`	`@0 Eurasie @2 NG`
C07	`02`	`X`	`ENG`	`@0 Eurasia @2 NG`
C07	`02`	`X`	`SPA`	`@0 Eurasia @2 NG`
C07	`03`	`X`	`FRE`	`@0 Pisces @2 NS`
C07	`03`	`X`	`ENG`	`@0 Pisces @2 NS`
C07	`03`	`X`	`SPA`	`@0 Pisces @2 NS`
C07	`04`	`X`	`FRE`	`@0 Vertebrata @2 NS`
C07	`04`	`X`	`ENG`	`@0 Vertebrata @2 NS`
C07	`04`	`X`	`SPA`	`@0 Vertebrata @2 NS`
C07	`05`	`X`	`FRE`	`@0 Métal lourd @5 61`
C07	`05`	`X`	`ENG`	`@0 Heavy metal @5 61`
C07	`05`	`X`	`SPA`	`@0 Metal pesado @5 61`
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C07	`06`	`X`	`SPA`	`@0 Elemento traza @5 62`
N21				`@1 005`

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Pascal:15-0009283

Le document en format XML

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<sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Low and Declining Mercury in Arctic Russian Rivers</title>
<author><name sortKey="Castello, Leandro" sort="Castello, Leandro" uniqKey="Castello L" first="Leandro" last="Castello">Leandro Castello</name>
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<author><name sortKey="Gurtovaya, Tatiana Yu" sort="Gurtovaya, Tatiana Yu" uniqKey="Gurtovaya T" first="Tatiana Yu." last="Gurtovaya">Tatiana Yu. Gurtovaya</name>
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<author><name sortKey="Holmes, Robert M" sort="Holmes, Robert M" uniqKey="Holmes R" first="Robert M." last="Holmes">Robert M. Holmes</name>
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<author><name sortKey="Zhulidov, Daniel A" sort="Zhulidov, Daniel A" uniqKey="Zhulidov D" first="Daniel A." last="Zhulidov">Daniel A. Zhulidov</name>
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<front><div type="abstract" xml:lang="en">Mercury (Hg) dynamics in the Arctic is receiving increasing attention, but further understanding is limited by a lack of studies in Russia, which encompasses the majority of the pan-Arctic watershed. This study reports Hg concentrations and trends in burbot (Lota lota) from the Lena and Mezen Rivers in the Russian Arctic, and assesses the extent to which they differ from those found in burbot in arctic rivers elsewhere. Mercury concentrations in burbot in the Lena and Mezen Rivers were found to be generally lower than in 23 other locations, most of which are in the Mackenzie River Basin (Canada). Mercury concentrations in burbot in the Lena and Mezen Rivers also were found to have been declining at an annual rate of 2.3% while they have been increasing in the Mackenzie River Basin at annual rates between 2.2 and 5.1% during roughly the same time period. These contrasting patterns in Hg in burbot across the pan-Arctic may be explained by geographic heterogeneity in controlling processes, including riverine particulate material loads, historically changing atmospheric inputs, postdepositional processes, and climate change impacts.</div>
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<fC01 i1="01" l="ENG"><s0>Mercury (Hg) dynamics in the Arctic is receiving increasing attention, but further understanding is limited by a lack of studies in Russia, which encompasses the majority of the pan-Arctic watershed. This study reports Hg concentrations and trends in burbot (Lota lota) from the Lena and Mezen Rivers in the Russian Arctic, and assesses the extent to which they differ from those found in burbot in arctic rivers elsewhere. Mercury concentrations in burbot in the Lena and Mezen Rivers were found to be generally lower than in 23 other locations, most of which are in the Mackenzie River Basin (Canada). Mercury concentrations in burbot in the Lena and Mezen Rivers also were found to have been declining at an annual rate of 2.3% while they have been increasing in the Mackenzie River Basin at annual rates between 2.2 and 5.1% during roughly the same time period. These contrasting patterns in Hg in burbot across the pan-Arctic may be explained by geographic heterogeneity in controlling processes, including riverine particulate material loads, historically changing atmospheric inputs, postdepositional processes, and climate change impacts.</s0>
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<s2>NC</s2>
<s2>FX</s2>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="FRE"><s0>Arctique Russie</s0>
<s2>NG</s2>
<s5>03</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG"><s0>Russian Arctic</s0>
<s2>NG</s2>
<s5>03</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA"><s0>Ártico Rusia</s0>
<s2>NG</s2>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE"><s0>Cours eau</s0>
<s5>05</s5>
</fC03>
<fC03 i1="03" i2="X" l="ENG"><s0>Stream</s0>
<s5>05</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA"><s0>Curso agua</s0>
<s5>05</s5>
</fC03>
<fC03 i1="04" i2="X" l="FRE"><s0>Rivière</s0>
<s5>06</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG"><s0>Rivers</s0>
<s5>06</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA"><s0>Río</s0>
<s5>06</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE"><s0>Lota lota</s0>
<s2>NS</s2>
<s5>08</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG"><s0>Lota lota</s0>
<s2>NS</s2>
<s5>08</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA"><s0>Lota lota</s0>
<s2>NS</s2>
<s5>08</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE"><s0>Eau surface</s0>
<s5>09</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG"><s0>Surface water</s0>
<s5>09</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA"><s0>Agua superficie</s0>
<s5>09</s5>
</fC03>
<fC07 i1="01" i2="X" l="FRE"><s0>Russie</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="X" l="ENG"><s0>Russian Federation</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="X" l="SPA"><s0>Federación de Rusia</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="X" l="FRE"><s0>Eurasie</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="X" l="ENG"><s0>Eurasia</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="X" l="SPA"><s0>Eurasia</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="03" i2="X" l="FRE"><s0>Pisces</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="03" i2="X" l="ENG"><s0>Pisces</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="03" i2="X" l="SPA"><s0>Pisces</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="04" i2="X" l="FRE"><s0>Vertebrata</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="04" i2="X" l="ENG"><s0>Vertebrata</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="04" i2="X" l="SPA"><s0>Vertebrata</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="05" i2="X" l="FRE"><s0>Métal lourd</s0>
<s5>61</s5>
</fC07>
<fC07 i1="05" i2="X" l="ENG"><s0>Heavy metal</s0>
<s5>61</s5>
</fC07>
<fC07 i1="05" i2="X" l="SPA"><s0>Metal pesado</s0>
<s5>61</s5>
</fC07>
<fC07 i1="06" i2="X" l="FRE"><s0>Elément trace</s0>
<s5>62</s5>
</fC07>
<fC07 i1="06" i2="X" l="ENG"><s0>Trace element</s0>
<s5>62</s5>
</fC07>
<fC07 i1="06" i2="X" l="SPA"><s0>Elemento traza</s0>
<s5>62</s5>
</fC07>
<fN21><s1>005</s1>
</fN21>
</pA>
</standard>
</inist>
</record>

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   |wiki=    Eau
   |area=    LotaV3
   |flux=    PascalFrancis
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   |clé=     Pascal:15-0009283
   |texte=   Low and Declining Mercury in Arctic Russian Rivers
}}

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Data generation: Fri May 20 09:58:26 2022. Site generation: Fri May 20 10:24:07 2022

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Serveur d'exploration Lota lota

Low and Declining Mercury in Arctic Russian Rivers

Low and Declining Mercury in Arctic Russian Rivers

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Descripteurs français

English descriptors

Abstract

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