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崇明东滩大型底栖动物食源的稳定同位素示踪
引用本文:余婕,刘敏,侯立军,许世远,欧冬妮,程书波.崇明东滩大型底栖动物食源的稳定同位素示踪[J].自然资源学报,2008,23(2):319-326.
作者姓名:余婕  刘敏  侯立军  许世远  欧冬妮  程书波
作者单位:1. 华东师范大学 地理学系,教育部地理信息科学重点实验室,上海 200062;
2. 华东师范大学 河口海岸科学研究院,上海 200062
基金项目:国家自然科学基金 , 华东师范大学校科研和教改项目
摘    要:利用稳定同位素示踪技术,对崇明东滩盐沼湿地夏季不同生境大型底栖动物的食物来源和营养结构进行了初步研究。结果显示,表层沉积有机质稳定碳、氮同位素组成分别在-21.3‰~-24.2‰、4.6‰~5.6‰,不同生境下存在一定差异。植物体各组织的同位素值存在差异,在判别食物来源时需要注意,不能简单地以植物叶片值来代替整个植株。大型底栖动物的δ13C值为-14.7‰~-23.6‰,表现出食物来源的差异。总体上说,湿地优势植物的活植物体不是大型底栖动物的主要食物来源,沉积有机质是大部分底栖消费者的食物基础。底栖动物的氮同位素能较好地反映其食性和营养级,计算出崇明东滩大型底栖动物营养级在2.0~3.7,为一级消费者和二级消费者。

关 键 词:海洋生物学  底栖动物  食源  营养级  碳同位素  氮同位素  崇明东滩  
文章编号:1000-3037(2008)02-0319-08
收稿时间:3/9/2007 12:00:00 AM
修稿时间:2007-12-10

Food Sources of Macrofaunal in East Chongming Salt Marsh as Traced by Stable Isotopes
YU Jie,LIU Min,HOU Li-jun,XU Shi-yuan,OU Dong-ni,CHENG Shu-bo.Food Sources of Macrofaunal in East Chongming Salt Marsh as Traced by Stable Isotopes[J].Journal of Natural Resources,2008,23(2):319-326.
Authors:YU Jie  LIU Min  HOU Li-jun  XU Shi-yuan  OU Dong-ni  CHENG Shu-bo
Institution:1. Key Laboratory of Geo-information Science of Ministry of Education, Department of Geography, East China Normal University, Shanghai 200062;
2. State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China
Abstract:East Chongming salt marsh,located in the east of Changjiang Estuary, is a large wetland, which exhibits a variety of macrobenthos. Understanding the food sources and trophic level of macrofauna is a foundation to study the material and energy flux in the ecosystem. In this paper, stable carbon and nitrogen isotope ratios of organic matter sources and consumers were investigated in the summer of 2005 in the differents living environments of East Chongming salt marsh. It is found that the δ13C and δ15N values of surface sediments vary in different tidal levels, with δ13C from-21.3‰ to-24.2‰ and δ15N from 4.6‰ to 5.6‰. These stable isotope values suggest that sediments not only contain the extraneous materials but also are influenced by the autochthonous organic matter. Our data displays that the dominant macrophytes Scirpus mariqueter and Phragmites australis are the main allochthonous sources of sedimentary organic matter and the extraneous source is suspended particulate organic matter. The dominant macrophytes Scirpus mariqueter and Phragmites australis are C3 plants, and Spartina alterniflora is C4 plant. The stable isotopes are variable among different tissues of plants, especially of Phragmites australis, which suggests that care must be taken and the isotope value of leaves may not be used as that of the whole plant when estimating the food sources. The macrofauna shows a wide range of δ13C, with overall δ13C values between -23.6‰ and -14.7‰, which suggests significant difference of food sources. As a whole, sedimentary organic matter seems to be food base for macrofauna, while the dominant macrophytes of salt marsh appears to play a negligible trophic role. The nitrogen isotope can reflect the trophic level of macrobenthos. It is calculated that trophic level of macrofauna in East Chongming salt marsh is between 2.0 and 3.7, and thus the invertebrates are primary and secondary consumers.
Keywords:marine biology  macrobenthos  food source  trophic level  carbon isotope  nitrogen isotope  East Chongming salt marsh
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