Rapid sediment accumulation and microbial mineralization in forests of the mangrove Kandelia candel in the Jiulongjiang Estuary, China

被引:199
|
作者
Alongi, DM [1 ]
Pfitzner, J [1 ]
Trott, LA [1 ]
Tirendi, F [1 ]
Dixon, P [1 ]
Klumpp, DW [1 ]
机构
[1] Australian Inst Marine Sci, Townsville, Qld 4810, Australia
关键词
sedimentation rates; diagenesis; carbon cycle; nitrogen cycle; organic matter; mangrove; sediment; China;
D O I
10.1016/j.ecss.2005.01.004
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
Rates of sediment accumulation and microbial mineralization were examined at three Kandelia candel forests spanning the intertidal zone along the south coastline of the heavily urbanized Jiulongljiang Estuary, Fujian Province, China. Mass sediment accumulation rates were rapid (range: 10-62 kg m(-2) y(-1)) but decreased from the low- to the high-intertidal zone. High levels of radionuclides suggest that these sediments originate from erosion of agricultural soils within the catchment. Mineralization of sediment carbon and nitrogen was correspondingly rapid, with total rate of mineralization ranging from 135 to 191 mol C m(-2) y(-1) and 9 to 11 mol N m(-2)y(-1); rates were faster in summer than in autumn/winter. Rates of mineralization efficiency (70-93% for C; 69-92% for N) increased, as burial efficiency (7-30% for C; 8-31% for N) decreased, from the low-to the high-intertidal mangroves. Sulphate reduction was the dominant metabolic pathway to a depth of I m, with rates (19-281 nmol S m(-2) d(-1)) exceeding those measured in other intertidal deposits. There is some evidence that Fe and Mn reduction-oxidation cycles are coupled to the activities of live roots within the 0-40 cm depth horizon. Oxic respiration accounted for 5-12% of total carbon mineralization. Methane flux was slow and highly variable when detectable (range: 5-66 pmol CH4 m(-2) d(-1)). Nitrous oxide flux was also highly variable, but within the range (1.6-106.5 mu mol N2O m(-2) d-1) measured in other intertidal sediments. Rates of denitrification were rapid, ranging from 1106 to 3780 mu mol N-2 m(-2) d(-1), and equating to 11-20% of total sediment nitrogen inputs. Denitrification was supported by rapid NH4 release within surface deposits (range: 3.6-6.1 mmol m(-2) d(-1)). Our results support the notion that mangrove forests are net accumulation sites for sediment and associated elements within estuaries, especially Kandelia candel forests receiving significant inputs as a direct result of intense human activity along the south China coast. (c) 2005 Elsevier Ltd. All rights reserved.
引用
收藏
页码:605 / 618
页数:14
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