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闽江口秋茄红树林凋落物产量及分解动态
引用本文:张雨雪,胡伟芳,罗敏,仝川,赵斓林,陈坤龙,黄佳芳.闽江口秋茄红树林凋落物产量及分解动态[J].环境科学学报,2019,39(4):1312-1323.
作者姓名:张雨雪  胡伟芳  罗敏  仝川  赵斓林  陈坤龙  黄佳芳
作者单位:福建师范大学湿润亚热带生态地理过程教育部重点实验室,福州350007;福建师范大学地理科学学院,福州350007;福建师范大学亚热带湿地研究中心,福州350007;福建师范大学湿润亚热带生态地理过程教育部重点实验室,福州350007;福建师范大学地理研究所,福州350007;福建师范大学亚热带湿地研究中心,福州350007;福建师范大学亚热带湿地研究中心,福州350007;福州大学环境与资源学院,福州350007;国家林业和草原局福建闽江河口湿地生态系统定位观测研究站,福州350007;福建师范大学湿润亚热带生态地理过程教育部重点实验室,福州350007;福建师范大学地理研究所,福州350007;福建师范大学地理科学学院,福州350007;福建师范大学亚热带湿地研究中心,福州350007;国家林业和草原局福建闽江河口湿地生态系统定位观测研究站,福州350007
基金项目:国家自然科学基金青年项目(No.41601102);福建省科技厅省属公益类科研专项(No.2015R1101029-7);福建师范大学校级创新团队项目(No.IRTL1205)
摘    要:于2017年以闽江口粗芦岛秋茄(Kandelia obovata)红树林为研究对象,分别采用凋落物收集框和分解袋法,研究秋茄凋落物产量及其碳(C)、氮(N)、磷(P)含量月动态及凋落叶分解过程中C、N、P含量与水解酶活性.结果表明:①秋茄凋落物年产量为618.79 g·m~(-2)·a~(-1),其中,叶占61.2%,果、枝和花分别占23.7%、10.5%和4.6%.②凋落叶总氮(TN)含量8月显著高于其他月份(p0.05),而TP含量在1—3月显著高于其他月份;C/N在8月显著低于其他月份(p0.05),而C/P及N/P在9月显著升高(p0.05).③在凋落叶分解过程中,C、N、P含量及其化学计量比随时间存在明显差异(p0.01),并且地上组TC、TN、C/N和C/P明显不同于地下组(p0.05).④在分解过程中,4种水解酶随时间存在明显差异(p0.01).⑤凋落叶酸性磷酸酶活性与土壤温度、电导率和凋落叶TP含量存在显著相关关系(p0.01).这些结果说明,秋茄凋落物产量及元素含量随季节变化存在明显差异;沉积作用对凋落叶分解过程中元素含量有显著影响,水解酶活性主要受凋落叶元素含量和土壤环境因子的控制.

关 键 词:凋落物量  凋落叶分解  元素含量  水解酶活性  秋茄  闽江口
收稿时间:2018/9/26 0:00:00
修稿时间:2018/12/12 0:00:00

Litter production and decomposition dynamics of Kandelia obovata from a mangrove swamp in Min River estuary
ZHANG Yuxue,HU Weifang,LUO Min,TONG Chuan,ZHAO Lanlin,CHEN Kunlong and HUANG Jiafang.Litter production and decomposition dynamics of Kandelia obovata from a mangrove swamp in Min River estuary[J].Acta Scientiae Circumstantiae,2019,39(4):1312-1323.
Authors:ZHANG Yuxue  HU Weifang  LUO Min  TONG Chuan  ZHAO Lanlin  CHEN Kunlong and HUANG Jiafang
Institution:1. Key Laboratory of Humid Sub-tropical Eco-geographical Process of Ministry of Education, Fujian Normal University, Fuzhou 350007;2. School of Geographical Sciences, Fujian Normal University, Fuzhou 350007;3. Research Centre of Wetlands in Subtropical Region, Fujian Normal University, Fuzhou 350007,1. Key Laboratory of Humid Sub-tropical Eco-geographical Process of Ministry of Education, Fujian Normal University, Fuzhou 350007;2. Institute of Geography, Fujian Normal University, Fuzhou 350007;3. Research Centre of Wetlands in Subtropical Region, Fujian Normal University, Fuzhou 350007,1. Research Centre of Wetlands in Subtropical Region, Fujian Normal University, Fuzhou 350007;2. College of Environment and Resources, Fuzhou University, Fuzhou 350007;3. Wetland Ecosystem Research Station of Minjiang River Estuary, State Administration of Forestry and Grassland, Fuzhou 350007,1. Key Laboratory of Humid Sub-tropical Eco-geographical Process of Ministry of Education, Fujian Normal University, Fuzhou 350007;2. Institute of Geography, Fujian Normal University, Fuzhou 350007;3. School of Geographical Sciences, Fujian Normal University, Fuzhou 350007;4. Research Centre of Wetlands in Subtropical Region, Fujian Normal University, Fuzhou 350007;5. Wetland Ecosystem Research Station of Minjiang River Estuary, State Administration of Forestry and Grassland, Fuzhou 350007,1. Key Laboratory of Humid Sub-tropical Eco-geographical Process of Ministry of Education, Fujian Normal University, Fuzhou 350007;2. School of Geographical Sciences, Fujian Normal University, Fuzhou 350007;3. Research Centre of Wetlands in Subtropical Region, Fujian Normal University, Fuzhou 350007,1. Key Laboratory of Humid Sub-tropical Eco-geographical Process of Ministry of Education, Fujian Normal University, Fuzhou 350007;2. School of Geographical Sciences, Fujian Normal University, Fuzhou 350007;3. Research Centre of Wetlands in Subtropical Region, Fujian Normal University, Fuzhou 350007 and 1. Key Laboratory of Humid Sub-tropical Eco-geographical Process of Ministry of Education, Fujian Normal University, Fuzhou 350007;2. Institute of Geography, Fujian Normal University, Fuzhou 350007;3. School of Geographical Sciences, Fujian Normal University, Fuzhou 350007;4. Research Centre of Wetlands in Subtropical Region, Fujian Normal University, Fuzhou 350007;5. Wetland Ecosystem Research Station of Minjiang River Estuary, State Administration of Forestry and Grassland, Fuzhou 350007
Abstract:Using litter collection box and litter bag techniques, the production and decomposition dynamics of Kandelia obovata from an estuarine mangrove swamp in Min River estuary were measured in 2017. The results showed that the annual litter production of K. obovata was 618.79 g·m-2·a-1, of which the leaf was the most abundant, accounting for an average of 61.2% of all production, followed by fruit, branch and flower, with contributions of 23.7%, 10.5%, and 4.6%, respectively. The total nitrogen (TN) content of litter was highest in August 2017, while the total phosphorus (TP) content was significantly higher in January-March than in other months. The litter carbon/nitrogen (C/N) ratios were lowest in August, while the carbon/phosphorus (C/P) ratios and nitrogen/phosphorus (N/P) ratios were significantly higher in September than in other months. During the decomposition of leaf litter, the C, N, P contents and its stoichiometric ratios showed significant differences with time. The TC, TN, C/N and C/P of the aboveground groups were significantly different from those of the underground groups. The acid phosphatase activity was significantly correlated with soil temperature, soil electric conductivity and litter TP content. These results indicated that the production and elemental content of K. obovata litter were significantly different with seasons; sedimentation significantly affected the element content during leaf litter decomposition, and soil environment factors and litter element content were important factors controlling hydrolase activity.
Keywords:litter fall production  leaf litter decomposition  element content  hydrolytic activity  Kandelia obovata  Min River estuary
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