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Contribution of the polychaete,Neanthes japonica (Izuka), to the oxygen uptake and carbon dioxide production of an intertidal mud-flat of the Nanakita River estuary,Japan
Institution:1. Biological Institute, Graduate School of Science, Tohoku University, Aramaki-Aoba, Aoba-ku, Sendai 980-8578, Japan;2. National Institute for Environmental Studies, 16-2 Onogawa, Tsukuba 305-8506, Japan;3. Emeritus Professor, Tohoku Gakuin University, Japan;4. EEC, Miyagi University of Education, 149 Aramaki-Aoba, Sendai 980-0845, Japan;1. Key Laboratory for Humid Subtropical Eco-geographical Processes of the Ministry of Education, Fujian Normal University, Fuzhou 350007, China;2. School of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China;3. Key Laboratory of Geographic Information Science of the Ministry of Education, School of Geographic Sciences, East China Normal University, Shanghai, 200241, China;4. State Key Laboratory of Estuarine and Costal Research, East China Normal University, Shanghai, 200062, China
Abstract:The benthic oxygen consumption and carbon dioxide production of undisturbed and sieved sediment cores with various values for the biomass of polychaetes collected from the intertidal mud-flat of Nanakita River estuary of Japan were measured simultaneously. The benthic oxygen consumption and carbon dioxide production increased in proportion to the biomass of a dominant polychaete species Neanthes japonica (Izuka). This increase was not explained by the respiration of the animals alone. The residual increase in benthic O2 and CO2 fluxes may be due to mineralization processes in the burrow wall and enhanced diffusion caused by the pumping activity of the worms. From the average biomass of polychaetes at the study site, total benthic O2 and CO2 fluxes were estimated to be 5.2 mmol·m−2·h−1 and 7.3 mmol·m−2·h−1, respectively, at 20 ° C. The worms were responsible for 79% of the total O2 flux and 73% of the total CO2 flux but the respiration of the worms accounted for only 53% of the total O2 flux and 36% of the total CO2 flux. The residual enhanced fluxes were 26% and 37% for the total O2 and CO2 fluxes, respectively.
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