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SOIL CARBON AND MICROBIAL COMMUNITIES AT MITIGATED AND LATE SUCCESSIONAL BOTTOMLAND FOREST WETLANDS
The practice of wetland mitigation has come into question during the past decade because the relative capacity of the mitigated wetlands to perform normal wetland functions is mostly unknown. In this study, we wanted to determine whether soil microbial communities were significantly different in ear...
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| Published in: | Wetlands (Wilmington, N.C.) N.C.), 2005-03, Vol.25 (1), p.162-175 |
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| container_title | Wetlands (Wilmington, N.C.) |
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| creator | D'Angelo, Elisa M. Karathanasis, Anastasios D. Sparks, Earl J. Ritchey, Sloane A. Wehr-McChesney, Stephanie A. |
| description | The practice of wetland mitigation has come into question during the past decade because the relative capacity of the mitigated wetlands to perform normal wetland functions is mostly unknown. In this study, we wanted to determine whether soil microbial communities were significantly different in early successional mitigated wetlands ( |
| doi_str_mv | 10.1672/0277-5212(2005)025[0162:SCAMCA]2.0.CO;2 |
| format | article |
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In this study, we wanted to determine whether soil microbial communities were significantly different in early successional mitigated wetlands (<10 years) (ES) compared to late successional bottomland hardwood forest wetlands (LS) due to differences in soil properties, such as carbon quality and storage and water-holding capacity. Carbon storage in litter and soil was 1.5 times greater in LS wetlands than ES wetlands. Soil water-holding capacity was significantly greater in LS wetlands and was related to soil organic C content (r2=0.87, p-value=0.0007). Gravimetric water content was a moderately strong predictor of microbial respiration (r2=0.55–0.61, p-value=0.001–0.0004) and microbial biomass (r2=0.70, p-value=0.0019). Anaerobic microbial groups were enriched in soils from LS wetlands in both the dry and wet seasons, which suggested that LS soils were wetter for longer periods of the year than ES soils. The capacity of these wetlands to support anaerobic microbial processes depends on soil water retention characteristics, which were dictated by organic matter content. 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The capacity of these wetlands to support anaerobic microbial processes depends on soil water retention characteristics, which were dictated by organic matter content. As an integrator of microbial growth conditions in soils, determination of microbial community composition by phospholipid fatty acid (PLFA) analysis may be an important new tool for monitoring successional development of compensatory mitigation wetlands.</description><subject>Anaerobic microorganisms</subject><subject>Anaerobic processes</subject><subject>Bottomland</subject><subject>Carbon</subject><subject>carbon quality</subject><subject>Carbon sequestration</subject><subject>Community composition</subject><subject>fatty acids</subject><subject>Growth conditions</subject><subject>Hardwoods</subject><subject>lowland forests</subject><subject>Microbial activity</subject><subject>microbial respiration</subject><subject>microbial resuscitation</subject><subject>Microbiomes</subject><subject>Microorganisms</subject><subject>Moisture content</subject><subject>Organic matter</subject><subject>Organic soils</subject><subject>phospholipid fatty acids</subject><subject>Phospholipids</subject><subject>Rainy season</subject><subject>soil microorganisms</subject><subject>Soil properties</subject><subject>Soil water</subject><subject>soil water retention</subject><subject>Soil water storage</subject><subject>soil water-holding capacity</subject><subject>Water content</subject><subject>wetland conservation</subject><subject>wetland functions</subject><subject>wetland succession</subject><subject>Wetlands</subject><issn>0277-5212</issn><issn>1943-6246</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2005</creationdate><recordtype>article</recordtype><recordid>eNqdkN1OgzAUgBujifPnGSTxRi_YTltKQa9Yh5MEaLJ28cKYBhiYGZUJ88K3t4jxAbxo2tPznZ98CM0wTLHPyQwI5y4jmFwRAHYNhD0C9smNElEmoicyhamQt-QATXDoUdcnnn-IJn9Vx-ik719gKCF4giolk9QR0WoucyfKF06WiJWcJ5H9lFm2zhOdxMqJtE3oZBnpePGDpfblqLUQsVKJzC0-l1rLLB2Sd3IVK-08xHoI1Rk6aorXvj7_vU_R-i7W4t5N5TIRUeqWHtC9S1lFA-D1xsdhxUsoNk3JNiWzezLOPNoUZVVVFIcAAaMh9-qg9nCDK16UYelt6Cm6HPvuuvbjs-735qX97N7tSENCK4MHPg8stRypqmv7vqsbs-u2b0X3ZTCYwbAZXJnBlRkM29Aeq8uMho0FjJCG2E4XY6emaE3x3G17s1YEMAUMQEPGLRGPRLlt2_f635O-AflPhgg</recordid><startdate>20050301</startdate><enddate>20050301</enddate><creator>D'Angelo, Elisa M.</creator><creator>Karathanasis, Anastasios D.</creator><creator>Sparks, Earl J.</creator><creator>Ritchey, Sloane A.</creator><creator>Wehr-McChesney, Stephanie A.</creator><general>Springer Nature B.V</general><scope>FBQ</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7X2</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>LK8</scope><scope>M0K</scope><scope>M7P</scope><scope>PATMY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PYCSY</scope></search><sort><creationdate>20050301</creationdate><title>SOIL CARBON AND MICROBIAL COMMUNITIES AT MITIGATED AND LATE SUCCESSIONAL BOTTOMLAND FOREST WETLANDS</title><author>D'Angelo, Elisa M. ; Karathanasis, Anastasios D. ; Sparks, Earl J. ; Ritchey, Sloane A. ; Wehr-McChesney, Stephanie A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-b403t-35c3807ed619c7b0adfb5db522157543fabccc31900853974e8e41f1c7ab9b4d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2005</creationdate><topic>Anaerobic microorganisms</topic><topic>Anaerobic processes</topic><topic>Bottomland</topic><topic>Carbon</topic><topic>carbon quality</topic><topic>Carbon sequestration</topic><topic>Community composition</topic><topic>fatty acids</topic><topic>Growth conditions</topic><topic>Hardwoods</topic><topic>lowland forests</topic><topic>Microbial activity</topic><topic>microbial respiration</topic><topic>microbial resuscitation</topic><topic>Microbiomes</topic><topic>Microorganisms</topic><topic>Moisture content</topic><topic>Organic matter</topic><topic>Organic soils</topic><topic>phospholipid fatty acids</topic><topic>Phospholipids</topic><topic>Rainy season</topic><topic>soil microorganisms</topic><topic>Soil properties</topic><topic>Soil water</topic><topic>soil water retention</topic><topic>Soil water storage</topic><topic>soil water-holding capacity</topic><topic>Water content</topic><topic>wetland conservation</topic><topic>wetland functions</topic><topic>wetland succession</topic><topic>Wetlands</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>D'Angelo, Elisa M.</creatorcontrib><creatorcontrib>Karathanasis, Anastasios D.</creatorcontrib><creatorcontrib>Sparks, Earl J.</creatorcontrib><creatorcontrib>Ritchey, Sloane A.</creatorcontrib><creatorcontrib>Wehr-McChesney, Stephanie A.</creatorcontrib><collection>AGRIS</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Agricultural Science Collection</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>ProQuest Central</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Biological Science Collection</collection><collection>Agriculture Science Database</collection><collection>Biological Science Database</collection><collection>Environmental Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Environmental Science Collection</collection><jtitle>Wetlands (Wilmington, N.C.)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>D'Angelo, Elisa M.</au><au>Karathanasis, Anastasios D.</au><au>Sparks, Earl J.</au><au>Ritchey, Sloane A.</au><au>Wehr-McChesney, Stephanie A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>SOIL CARBON AND MICROBIAL COMMUNITIES AT MITIGATED AND LATE SUCCESSIONAL BOTTOMLAND FOREST WETLANDS</atitle><jtitle>Wetlands (Wilmington, N.C.)</jtitle><date>2005-03-01</date><risdate>2005</risdate><volume>25</volume><issue>1</issue><spage>162</spage><epage>175</epage><pages>162-175</pages><issn>0277-5212</issn><eissn>1943-6246</eissn><abstract>The practice of wetland mitigation has come into question during the past decade because the relative capacity of the mitigated wetlands to perform normal wetland functions is mostly unknown. In this study, we wanted to determine whether soil microbial communities were significantly different in early successional mitigated wetlands (<10 years) (ES) compared to late successional bottomland hardwood forest wetlands (LS) due to differences in soil properties, such as carbon quality and storage and water-holding capacity. Carbon storage in litter and soil was 1.5 times greater in LS wetlands than ES wetlands. Soil water-holding capacity was significantly greater in LS wetlands and was related to soil organic C content (r2=0.87, p-value=0.0007). Gravimetric water content was a moderately strong predictor of microbial respiration (r2=0.55–0.61, p-value=0.001–0.0004) and microbial biomass (r2=0.70, p-value=0.0019). Anaerobic microbial groups were enriched in soils from LS wetlands in both the dry and wet seasons, which suggested that LS soils were wetter for longer periods of the year than ES soils. The capacity of these wetlands to support anaerobic microbial processes depends on soil water retention characteristics, which were dictated by organic matter content. As an integrator of microbial growth conditions in soils, determination of microbial community composition by phospholipid fatty acid (PLFA) analysis may be an important new tool for monitoring successional development of compensatory mitigation wetlands.</abstract><cop>Dordrecht</cop><pub>Springer Nature B.V</pub><doi>10.1672/0277-5212(2005)025[0162:SCAMCA]2.0.CO;2</doi><tpages>14</tpages></addata></record> |
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| identifier | ISSN: 0277-5212 |
| ispartof | Wetlands (Wilmington, N.C.), 2005-03, Vol.25 (1), p.162-175 |
| issn | 0277-5212 1943-6246 |
| language | eng |
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| source | Springer Nature |
| subjects | Anaerobic microorganisms Anaerobic processes Bottomland Carbon carbon quality Carbon sequestration Community composition fatty acids Growth conditions Hardwoods lowland forests Microbial activity microbial respiration microbial resuscitation Microbiomes Microorganisms Moisture content Organic matter Organic soils phospholipid fatty acids Phospholipids Rainy season soil microorganisms Soil properties Soil water soil water retention Soil water storage soil water-holding capacity Water content wetland conservation wetland functions wetland succession Wetlands |
| title | SOIL CARBON AND MICROBIAL COMMUNITIES AT MITIGATED AND LATE SUCCESSIONAL BOTTOMLAND FOREST WETLANDS |
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