Lumbricid macrofauna alter atrazine mineralization and sorption in a silt loam soil
Identifieur interne : 000487 ( PascalFrancis/Checkpoint ); précédent : 000486; suivant : 000488Lumbricid macrofauna alter atrazine mineralization and sorption in a silt loam soil
Auteurs : Francoise Binet [France] ; Anne Kersante [France] ; Colette Munier-Lamy [France] ; Renée-Claire Le Bayon [Suisse] ; Marie-José Belgy [France] ; Martin J. Shipitalo [États-Unis]Source :
- Soil biology & biochemistry [ 0038-0717 ] ; 2006.
Descripteurs français
- Pascal (Inist)
- Wicri :
- topic : Herbicide.
English descriptors
- KwdEn :
Abstract
Atrazine is a widely used herbicide and is often a contaminant in terrestrial and freshwater ecosystems. It is uncertain, however, how the activity of soil macrofauna affects atrazine fate and transport. Therefore, we investigated whether earthworms enhance atrazine biodegradation by stimulating herbicide degrading soil microflora, or if they increase atrazine persistence by facilitating herbicide sorption. Short (43 d) and medium term (86 d) effects of the earthworms Lumbricus terrestris and Aporrectodea caliginosa on mineralization, distribution, and sorption of U-ring-14C atrazine and on soil C mineralization was quantified in packed-soil microcosms using silt loam soil. A priming effect (stimulation of soil C mineralization) caused by atrazine supply was shown that likely lowered the earthworm net effect on soil C mineralization in atrazine-treated soil microcosms. Although earthworms significantly increased soil microbial activity, they reduced atrazine mineralization to 14CO2-C from 15.2 to 11.7% at 86 d. Earthworms facilitated formation of non-extractable atrazine residues within C-rich soil microsites that they created by burrowing and ingesting soil and organic matter. Atrazine sorption was highest in their gut contents and higher in casts than in burrow linings. Also, gut contents exhibited the highest formation of bound atrazine residues (non-extractable atrazine). Earthworms also promoted a deeper and patchier distribution of atrazine in the soil. This contributed to greater leaching losses of atrazine in microcosms amended with earthworms (3%) than in earthworm-free microcosms (0.003%), although these differences were not significant due to high variability in transport from earthworm-amended microcosms. Our results indicated that earthworms, mainly by casting activity, facilitated atrazine sorption, which increased atrazine persistence. As a consequence, this effect overrode any increase in atrazine biodegradation due to stimulation of microbial activity by earthworms. It is concluded that the affect of earthworms of atrazine mineralization is time-dependent, mineralization being slightly enhanced in the short term and subsequently reduced in the medium term.
Affiliations:
- France, Suisse, États-Unis
- Canton de Neuchâtel, Grand Est, Lorraine (région), Ohio, Région Bretagne
- Nancy, Neuchâtel, Rennes
- Université Henri Poincaré, Université de Neuchâtel
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Shipitalo</name><affiliation wicri:level="2"><inist:fA14 i1="05"><s1>USDA-Agricultural Research Service, North Appalachian Expérimental Watershed, P.O. 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Shipitalo</name><affiliation wicri:level="2"><inist:fA14 i1="05"><s1>USDA-Agricultural Research Service, North Appalachian Expérimental Watershed, P.O. Box 488</s1><s2>Coshocton, OH 43812-0488</s2><s3>USA</s3><sZ>6 aut.</sZ></inist:fA14><country>États-Unis</country><placeName><region type="state">Ohio</region></placeName></affiliation></author></analytic><series><title level="j" type="main">Soil biology & biochemistry</title><title level="j" type="abbreviated">Soil biol. biochem.</title><idno type="ISSN">0038-0717</idno><imprint><date when="2006">2006</date></imprint></series></biblStruct></sourceDesc><seriesStmt><title level="j" type="main">Soil biology & biochemistry</title><title level="j" type="abbreviated">Soil biol. biochem.</title><idno type="ISSN">0038-0717</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Atrazine</term><term>Degradation</term><term>Earthworm</term><term>Herbicide</term><term>Macrofauna</term><term>Mineralization</term><term>Silt loam soil</term><term>Soil science</term><term>Sorption</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Macrofaune</term><term>Minéralisation</term><term>Sorption</term><term>Dégradation</term><term>Science du sol</term><term>Ver de terre</term><term>Atrazine</term><term>Herbicide</term><term>Sol limoneux fin</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Herbicide</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Atrazine is a widely used herbicide and is often a contaminant in terrestrial and freshwater ecosystems. It is uncertain, however, how the activity of soil macrofauna affects atrazine fate and transport. Therefore, we investigated whether earthworms enhance atrazine biodegradation by stimulating herbicide degrading soil microflora, or if they increase atrazine persistence by facilitating herbicide sorption. Short (43 d) and medium term (86 d) effects of the earthworms Lumbricus terrestris and Aporrectodea caliginosa on mineralization, distribution, and sorption of U-ring-<sup>14</sup>C atrazine and on soil C mineralization was quantified in packed-soil microcosms using silt loam soil. A priming effect (stimulation of soil C mineralization) caused by atrazine supply was shown that likely lowered the earthworm net effect on soil C mineralization in atrazine-treated soil microcosms. Although earthworms significantly increased soil microbial activity, they reduced atrazine mineralization to <sup>14</sup>CO<sub>2</sub>-C from 15.2 to 11.7% at 86 d. Earthworms facilitated formation of non-extractable atrazine residues within C-rich soil microsites that they created by burrowing and ingesting soil and organic matter. Atrazine sorption was highest in their gut contents and higher in casts than in burrow linings. Also, gut contents exhibited the highest formation of bound atrazine residues (non-extractable atrazine). Earthworms also promoted a deeper and patchier distribution of atrazine in the soil. This contributed to greater leaching losses of atrazine in microcosms amended with earthworms (3%) than in earthworm-free microcosms (0.003%), although these differences were not significant due to high variability in transport from earthworm-amended microcosms. Our results indicated that earthworms, mainly by casting activity, facilitated atrazine sorption, which increased atrazine persistence. As a consequence, this effect overrode any increase in atrazine biodegradation due to stimulation of microbial activity by earthworms. It is concluded that the affect of earthworms of atrazine mineralization is time-dependent, mineralization being slightly enhanced in the short term and subsequently reduced in the medium term.</div></front></TEI><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0038-0717</s0></fA01><fA02 i1="01"><s0>SBIOAH</s0></fA02><fA03 i2="1"><s0>Soil biol. biochem.</s0></fA03><fA05><s2>38</s2></fA05><fA06><s2>6</s2></fA06><fA08 i1="01" i2="1" l="ENG"><s1>Lumbricid macrofauna alter atrazine mineralization and sorption in a silt loam soil</s1></fA08><fA11 i1="01" i2="1"><s1>BINET (Francoise)</s1></fA11><fA11 i1="02" i2="1"><s1>KERSANTE (Anne)</s1></fA11><fA11 i1="03" i2="1"><s1>MUNIER-LAMY (Colette)</s1></fA11><fA11 i1="04" i2="1"><s1>LE BAYON (Renée-Claire)</s1></fA11><fA11 i1="05" i2="1"><s1>BELGY (Marie-José)</s1></fA11><fA11 i1="06" i2="1"><s1>SHIPITALO (Martin J.)</s1></fA11><fA14 i1="01"><s1>CNRS/Université de Rennes1,UMR 6553 ECOBIO-IFR CAREN, Bat 14B, Avenue du Général Leclerc</s1><s2>35042 Rennes</s2><s3>FRA</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ></fA14><fA14 i1="02"><s1>CNRS/Université Henri Poincaré, UMR 7137 LIMOS, Faculté des Sciences, Boulevard des Aiguillettes, BP 239</s1><s2>54 506 Vandoeuvre-les-Nancy</s2><s3>FRA</s3><sZ>3 aut.</sZ></fA14><fA14 i1="03"><s1>Université de Neuchâtel, Institut de Botanique, LEVP, Rue Emile Argan, 11</s1><s2>20007, Neuchâtel</s2><s3>CHE</s3><sZ>4 aut.</sZ></fA14><fA14 i1="04"><s1>CNRS/ENSIC-INPL, UMR 7630, Département de chimie physique des réactions, 1 rue Granville, BP451</s1><s2>54001 Nancy</s2><s3>FRA</s3><sZ>5 aut.</sZ></fA14><fA14 i1="05"><s1>USDA-Agricultural Research Service, North Appalachian Expérimental Watershed, P.O. Box 488</s1><s2>Coshocton, OH 43812-0488</s2><s3>USA</s3><sZ>6 aut.</sZ></fA14><fA20><s1>1255-1263</s1></fA20><fA21><s1>2006</s1></fA21><fA23 i1="01"><s0>ENG</s0></fA23><fA43 i1="01"><s1>INIST</s1><s2>14360</s2><s5>354000142586860100</s5></fA43><fA44><s0>0000</s0><s1>© 2006 INIST-CNRS. All rights reserved.</s1></fA44><fA45><s0>1 p.1/4</s0></fA45><fA47 i1="01" i2="1"><s0>06-0285209</s0></fA47><fA60><s1>P</s1></fA60><fA61><s0>A</s0></fA61><fA64 i1="01" i2="1"><s0>Soil biology & biochemistry</s0></fA64><fA66 i1="01"><s0>GBR</s0></fA66><fC01 i1="01" l="ENG"><s0>Atrazine is a widely used herbicide and is often a contaminant in terrestrial and freshwater ecosystems. It is uncertain, however, how the activity of soil macrofauna affects atrazine fate and transport. Therefore, we investigated whether earthworms enhance atrazine biodegradation by stimulating herbicide degrading soil microflora, or if they increase atrazine persistence by facilitating herbicide sorption. Short (43 d) and medium term (86 d) effects of the earthworms Lumbricus terrestris and Aporrectodea caliginosa on mineralization, distribution, and sorption of U-ring-<sup>14</sup>C atrazine and on soil C mineralization was quantified in packed-soil microcosms using silt loam soil. A priming effect (stimulation of soil C mineralization) caused by atrazine supply was shown that likely lowered the earthworm net effect on soil C mineralization in atrazine-treated soil microcosms. Although earthworms significantly increased soil microbial activity, they reduced atrazine mineralization to <sup>14</sup>CO<sub>2</sub>-C from 15.2 to 11.7% at 86 d. Earthworms facilitated formation of non-extractable atrazine residues within C-rich soil microsites that they created by burrowing and ingesting soil and organic matter. Atrazine sorption was highest in their gut contents and higher in casts than in burrow linings. Also, gut contents exhibited the highest formation of bound atrazine residues (non-extractable atrazine). Earthworms also promoted a deeper and patchier distribution of atrazine in the soil. This contributed to greater leaching losses of atrazine in microcosms amended with earthworms (3%) than in earthworm-free microcosms (0.003%), although these differences were not significant due to high variability in transport from earthworm-amended microcosms. Our results indicated that earthworms, mainly by casting activity, facilitated atrazine sorption, which increased atrazine persistence. As a consequence, this effect overrode any increase in atrazine biodegradation due to stimulation of microbial activity by earthworms. It is concluded that the affect of earthworms of atrazine mineralization is time-dependent, mineralization being slightly enhanced in the short term and subsequently reduced in the medium term.</s0></fC01><fC02 i1="01" i2="X"><s0>002A32B03B4D</s0></fC02><fC03 i1="01" i2="X" l="FRE"><s0>Macrofaune</s0><s5>01</s5></fC03><fC03 i1="01" i2="X" l="ENG"><s0>Macrofauna</s0><s5>01</s5></fC03><fC03 i1="01" i2="X" l="SPA"><s0>Macrofauna</s0><s5>01</s5></fC03><fC03 i1="02" i2="X" l="FRE"><s0>Minéralisation</s0><s5>02</s5></fC03><fC03 i1="02" i2="X" l="ENG"><s0>Mineralization</s0><s5>02</s5></fC03><fC03 i1="02" i2="X" l="SPA"><s0>Mineralización</s0><s5>02</s5></fC03><fC03 i1="03" i2="X" l="FRE"><s0>Sorption</s0><s5>03</s5></fC03><fC03 i1="03" i2="X" l="ENG"><s0>Sorption</s0><s5>03</s5></fC03><fC03 i1="03" i2="X" l="SPA"><s0>Sorción</s0><s5>03</s5></fC03><fC03 i1="04" i2="X" l="FRE"><s0>Dégradation</s0><s5>04</s5></fC03><fC03 i1="04" i2="X" l="ENG"><s0>Degradation</s0><s5>04</s5></fC03><fC03 i1="04" i2="X" l="SPA"><s0>Degradación</s0><s5>04</s5></fC03><fC03 i1="05" i2="X" l="FRE"><s0>Science du sol</s0><s5>05</s5></fC03><fC03 i1="05" i2="X" l="ENG"><s0>Soil science</s0><s5>05</s5></fC03><fC03 i1="05" i2="X" l="SPA"><s0>Ciencia del suelo</s0><s5>05</s5></fC03><fC03 i1="06" i2="X" l="FRE"><s0>Ver de terre</s0><s5>10</s5></fC03><fC03 i1="06" i2="X" l="ENG"><s0>Earthworm</s0><s5>10</s5></fC03><fC03 i1="06" i2="X" l="SPA"><s0>Lombriz de tierra</s0><s5>10</s5></fC03><fC03 i1="07" i2="X" l="FRE"><s0>Atrazine</s0><s2>NK</s2><s2>FF</s2><s5>15</s5></fC03><fC03 i1="07" i2="X" l="ENG"><s0>Atrazine</s0><s2>NK</s2><s2>FF</s2><s5>15</s5></fC03><fC03 i1="07" i2="X" l="SPA"><s0>Atrazina</s0><s2>NK</s2><s2>FF</s2><s5>15</s5></fC03><fC03 i1="08" i2="X" l="FRE"><s0>Herbicide</s0><s5>16</s5></fC03><fC03 i1="08" i2="X" l="ENG"><s0>Herbicide</s0><s5>16</s5></fC03><fC03 i1="08" i2="X" l="SPA"><s0>Herbicida</s0><s5>16</s5></fC03><fC03 i1="09" i2="X" l="FRE"><s0>Sol limoneux fin</s0><s2>NT</s2><s5>24</s5></fC03><fC03 i1="09" i2="X" l="ENG"><s0>Silt loam soil</s0><s2>NT</s2><s5>24</s5></fC03><fC03 i1="09" i2="X" l="SPA"><s0>Suelo franco limoso</s0><s2>NT</s2><s5>24</s5></fC03><fC07 i1="01" i2="X" l="FRE"><s0>Faune</s0></fC07><fC07 i1="01" i2="X" l="ENG"><s0>Fauna</s0></fC07><fC07 i1="01" i2="X" l="SPA"><s0>Fauna</s0></fC07><fC07 i1="02" i2="X" l="FRE"><s0>Oligochaeta</s0><s2>NS</s2></fC07><fC07 i1="02" i2="X" l="ENG"><s0>Oligochaeta</s0><s2>NS</s2></fC07><fC07 i1="02" i2="X" l="SPA"><s0>Oligochaeta</s0><s2>NS</s2></fC07><fC07 i1="03" i2="X" l="FRE"><s0>Annelida</s0><s2>NS</s2></fC07><fC07 i1="03" i2="X" l="ENG"><s0>Annelida</s0><s2>NS</s2></fC07><fC07 i1="03" i2="X" l="SPA"><s0>Annelida</s0><s2>NS</s2></fC07><fC07 i1="04" i2="X" l="FRE"><s0>Invertebrata</s0><s2>NS</s2></fC07><fC07 i1="04" i2="X" l="ENG"><s0>Invertebrata</s0><s2>NS</s2></fC07><fC07 i1="04" i2="X" l="SPA"><s0>Invertebrata</s0><s2>NS</s2></fC07><fC07 i1="05" i2="X" l="FRE"><s0>Pesticide</s0></fC07><fC07 i1="05" i2="X" l="ENG"><s0>Pesticides</s0></fC07><fC07 i1="05" i2="X" l="SPA"><s0>Plaguicida</s0></fC07><fC07 i1="06" i2="X" l="FRE"><s0>Triazine dérivé</s0><s2>FR</s2><s5>50</s5></fC07><fC07 i1="06" i2="X" l="ENG"><s0>Triazine derivatives</s0><s2>FR</s2><s5>50</s5></fC07><fC07 i1="06" i2="X" l="SPA"><s0>Triazina derivado</s0><s2>FR</s2><s5>50</s5></fC07><fN21><s1>184</s1></fN21><fN44 i1="01"><s1>OTO</s1></fN44><fN82><s1>OTO</s1></fN82></pA></standard></inist><affiliations><list><country><li>France</li><li>Suisse</li><li>États-Unis</li></country><region><li>Canton de Neuchâtel</li><li>Grand Est</li><li>Lorraine (région)</li><li>Ohio</li><li>Région Bretagne</li></region><settlement><li>Nancy</li><li>Neuchâtel</li><li>Rennes</li></settlement><orgName><li>Université Henri Poincaré</li><li>Université de Neuchâtel</li></orgName></list><tree><country name="France"><region name="Région Bretagne"><name sortKey="Binet, Francoise" sort="Binet, Francoise" uniqKey="Binet F" first="Francoise" last="Binet">Francoise Binet</name></region><name sortKey="Belgy, Marie Jose" sort="Belgy, Marie Jose" uniqKey="Belgy M" first="Marie-José" last="Belgy">Marie-José Belgy</name><name sortKey="Kersante, Anne" sort="Kersante, Anne" uniqKey="Kersante A" first="Anne" last="Kersante">Anne Kersante</name><name sortKey="Munier Lamy, Colette" sort="Munier Lamy, Colette" uniqKey="Munier Lamy C" first="Colette" last="Munier-Lamy">Colette Munier-Lamy</name></country><country name="Suisse"><region name="Canton de Neuchâtel"><name sortKey="Le Bayon, Renee Claire" sort="Le Bayon, Renee Claire" uniqKey="Le Bayon R" first="Renée-Claire" last="Le Bayon">Renée-Claire Le Bayon</name></region></country><country name="États-Unis"><region name="Ohio"><name sortKey="Shipitalo, Martin J" sort="Shipitalo, Martin J" uniqKey="Shipitalo M" first="Martin J." last="Shipitalo">Martin J. 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