Effect of Crab Burrows on CO₂ Flux from the Sediment Surface to the Atmosphere in a Subtropical Mangrove Forest on Ishigaki Island, Southwestern Japan
To clarify the effects of crab burrows on variation in sediment CO₂ flux in mangrove forest, we measured the traits of crab burrows (density and entrance area size) and the CO₂ flux rate from sediment surfaces, in areas with and without burrows, in a subtropical mangrove forest on Ishigaki Island, s...
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description | To clarify the effects of crab burrows on variation in sediment CO₂ flux in mangrove forest, we measured the traits of crab burrows (density and entrance area size) and the CO₂ flux rate from sediment surfaces, in areas with and without burrows, in a subtropical mangrove forest on Ishigaki Island, southwestern Japan. Burrow density and entrance area showed significant differences among seasons (warm, middle, and cool) and mangrove zones (upper-, middle-, and downstream), which may have depended on crab phenology, life cycle, and species composition. The sediment CO₂ flux rate was significantly higher at plots with crab burrows (B+) than at those without burrows (B-) in each zone and season. However, standardized sediment CO₂ flux rate by burrow surface area at B+ plots did not differ significantly from that at B- plots. In addition, there were no significant differences in sediment temperature and sediment water content between the two types of plots. Moreover, the level of microbial respiration differed significantly between sediments collected from the deep part and those collected from either the ground surface part or burrow walls. These results suggest that crab burrows increase sediment CO₂ flux from the mangrove forest floor by increasing the sediment–atmosphere interface area, thereby inducing a change to aerobic conditions in the sediments around burrows. Therefore, the seasonal and spatial effect of crab burrows on the forest floor should be considered when evaluating sediment CO₂ flux and examining the role of the mangrove ecosystem as a carbon sink. |
doi_str_mv | 10.1007/s12237-019-00667-2 |
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Burrow density and entrance area showed significant differences among seasons (warm, middle, and cool) and mangrove zones (upper-, middle-, and downstream), which may have depended on crab phenology, life cycle, and species composition. The sediment CO₂ flux rate was significantly higher at plots with crab burrows (B+) than at those without burrows (B-) in each zone and season. However, standardized sediment CO₂ flux rate by burrow surface area at B+ plots did not differ significantly from that at B- plots. In addition, there were no significant differences in sediment temperature and sediment water content between the two types of plots. Moreover, the level of microbial respiration differed significantly between sediments collected from the deep part and those collected from either the ground surface part or burrow walls. These results suggest that crab burrows increase sediment CO₂ flux from the mangrove forest floor by increasing the sediment–atmosphere interface area, thereby inducing a change to aerobic conditions in the sediments around burrows. Therefore, the seasonal and spatial effect of crab burrows on the forest floor should be considered when evaluating sediment CO₂ flux and examining the role of the mangrove ecosystem as a carbon sink.</description><identifier>ISSN: 1559-2723</identifier><identifier>EISSN: 1559-2731</identifier><identifier>DOI: 10.1007/s12237-019-00667-2</identifier><language>eng</language><publisher>New York: Springer Science + Business Media</publisher><subject>Aerobic conditions ; Area ; Atmosphere ; Burrowing organisms ; Burrows ; Carbon dioxide ; Carbon sinks ; Coastal Sciences ; Density ; Earth and Environmental Science ; Ecology ; Environment ; Environmental Management ; Floors ; Fluctuations ; Flux ; Forest floor ; Freshwater & Marine Ecology ; Life cycle ; Life cycles ; Mangrove swamps ; Mangroves ; Marine crustaceans ; Microorganisms ; Moisture content ; ORIGINAL PAPERS ; Oxic conditions ; Seasons ; Sediment ; Sediment temperature ; Sediments ; Species composition ; Water and Health ; Water content ; Zoobenthos</subject><ispartof>Estuaries and coasts, 2020-01, Vol.43 (1), p.102-110</ispartof><rights>Coastal and Estuarine Research Federation 2019</rights><rights>Estuaries and Coasts is a copyright of Springer, (2019). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c407t-8c7195c6edc27f8917800a0e1cb175d608dee6504d3a48ded56439abbef634fa3</citedby><cites>FETCH-LOGICAL-c407t-8c7195c6edc27f8917800a0e1cb175d608dee6504d3a48ded56439abbef634fa3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/48728483$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/48728483$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,27923,27924,41487,42556,51318,58016,58249</link.rule.ids></links><search><creatorcontrib>Tomotsune, Mitsutoshi</creatorcontrib><creatorcontrib>Arai, Hideshi</creatorcontrib><creatorcontrib>Yoshitake, Shinpei</creatorcontrib><creatorcontrib>Kida, Morimaru</creatorcontrib><creatorcontrib>Fujitake, Nobuhide</creatorcontrib><creatorcontrib>Kinjo, Kazutoshi</creatorcontrib><creatorcontrib>Ohtsuka, Toshiyuki</creatorcontrib><title>Effect of Crab Burrows on CO₂ Flux from the Sediment Surface to the Atmosphere in a Subtropical Mangrove Forest on Ishigaki Island, Southwestern Japan</title><title>Estuaries and coasts</title><addtitle>Estuaries and Coasts</addtitle><description>To clarify the effects of crab burrows on variation in sediment CO₂ flux in mangrove forest, we measured the traits of crab burrows (density and entrance area size) and the CO₂ flux rate from sediment surfaces, in areas with and without burrows, in a subtropical mangrove forest on Ishigaki Island, southwestern Japan. Burrow density and entrance area showed significant differences among seasons (warm, middle, and cool) and mangrove zones (upper-, middle-, and downstream), which may have depended on crab phenology, life cycle, and species composition. The sediment CO₂ flux rate was significantly higher at plots with crab burrows (B+) than at those without burrows (B-) in each zone and season. However, standardized sediment CO₂ flux rate by burrow surface area at B+ plots did not differ significantly from that at B- plots. In addition, there were no significant differences in sediment temperature and sediment water content between the two types of plots. Moreover, the level of microbial respiration differed significantly between sediments collected from the deep part and those collected from either the ground surface part or burrow walls. These results suggest that crab burrows increase sediment CO₂ flux from the mangrove forest floor by increasing the sediment–atmosphere interface area, thereby inducing a change to aerobic conditions in the sediments around burrows. Therefore, the seasonal and spatial effect of crab burrows on the forest floor should be considered when evaluating sediment CO₂ flux and examining the role of the mangrove ecosystem as a carbon sink.</description><subject>Aerobic conditions</subject><subject>Area</subject><subject>Atmosphere</subject><subject>Burrowing organisms</subject><subject>Burrows</subject><subject>Carbon dioxide</subject><subject>Carbon sinks</subject><subject>Coastal Sciences</subject><subject>Density</subject><subject>Earth and Environmental Science</subject><subject>Ecology</subject><subject>Environment</subject><subject>Environmental Management</subject><subject>Floors</subject><subject>Fluctuations</subject><subject>Flux</subject><subject>Forest floor</subject><subject>Freshwater & Marine Ecology</subject><subject>Life cycle</subject><subject>Life cycles</subject><subject>Mangrove swamps</subject><subject>Mangroves</subject><subject>Marine crustaceans</subject><subject>Microorganisms</subject><subject>Moisture content</subject><subject>ORIGINAL PAPERS</subject><subject>Oxic conditions</subject><subject>Seasons</subject><subject>Sediment</subject><subject>Sediment temperature</subject><subject>Sediments</subject><subject>Species composition</subject><subject>Water and Health</subject><subject>Water 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Coasts</stitle><date>2020-01-01</date><risdate>2020</risdate><volume>43</volume><issue>1</issue><spage>102</spage><epage>110</epage><pages>102-110</pages><issn>1559-2723</issn><eissn>1559-2731</eissn><abstract>To clarify the effects of crab burrows on variation in sediment CO₂ flux in mangrove forest, we measured the traits of crab burrows (density and entrance area size) and the CO₂ flux rate from sediment surfaces, in areas with and without burrows, in a subtropical mangrove forest on Ishigaki Island, southwestern Japan. Burrow density and entrance area showed significant differences among seasons (warm, middle, and cool) and mangrove zones (upper-, middle-, and downstream), which may have depended on crab phenology, life cycle, and species composition. The sediment CO₂ flux rate was significantly higher at plots with crab burrows (B+) than at those without burrows (B-) in each zone and season. However, standardized sediment CO₂ flux rate by burrow surface area at B+ plots did not differ significantly from that at B- plots. In addition, there were no significant differences in sediment temperature and sediment water content between the two types of plots. Moreover, the level of microbial respiration differed significantly between sediments collected from the deep part and those collected from either the ground surface part or burrow walls. These results suggest that crab burrows increase sediment CO₂ flux from the mangrove forest floor by increasing the sediment–atmosphere interface area, thereby inducing a change to aerobic conditions in the sediments around burrows. Therefore, the seasonal and spatial effect of crab burrows on the forest floor should be considered when evaluating sediment CO₂ flux and examining the role of the mangrove ecosystem as a carbon sink.</abstract><cop>New York</cop><pub>Springer Science + Business Media</pub><doi>10.1007/s12237-019-00667-2</doi><tpages>9</tpages></addata></record> |
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subjects | Aerobic conditions Area Atmosphere Burrowing organisms Burrows Carbon dioxide Carbon sinks Coastal Sciences Density Earth and Environmental Science Ecology Environment Environmental Management Floors Fluctuations Flux Forest floor Freshwater & Marine Ecology Life cycle Life cycles Mangrove swamps Mangroves Marine crustaceans Microorganisms Moisture content ORIGINAL PAPERS Oxic conditions Seasons Sediment Sediment temperature Sediments Species composition Water and Health Water content Zoobenthos |
title | Effect of Crab Burrows on CO₂ Flux from the Sediment Surface to the Atmosphere in a Subtropical Mangrove Forest on Ishigaki Island, Southwestern Japan |
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