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应用生态学报 ›› 2010, Vol. 21 ›› Issue (08): 2140-2147.

• 研究报告 • 上一篇    下一篇

2008年浒苔大暴发末期黄海小型底栖动物现存量及空间分布

吴秀芹1,2,徐奎栋2**,于子山1,于婷婷2,孟昭翠2,代仁海2,类彦立2   

  1. 1中国海洋大学海洋生命学院,山东青岛 266003;2中国科学院海洋研究所,山东青岛 266071
  • 出版日期:2010-08-18 发布日期:2010-08-18

Standing crop and spatial distribution of meiofauna in Yellow Sea at late stage of Enteromorpha prolifera bloom in 2008.

WU Xiu-qin1, XU Kui-dong2, YU Zi-shan1, YU Ting-ting2, MENG Zhao-cui2, DAI -hai2, LEI Yan-li2
  

  1. 1College of Marine Life Sciences, Ocean University of China, Qingdao 266003, Shandong, China|2Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, Shandong, China
  • Online:2010-08-18 Published:2010-08-18

摘要: 在2008年夏季浒苔暴发末期,对黄海33个站位(其中冷水团中22个,浒苔暴发区域9个)进行了小型底栖动物现存量、分布及沉积环境研究.结果表明:在浒苔灾害严重的南黄海区域,沉积物中的粉砂粘土含量较往年(2007年)有明显增加;沉积物中叶绿素a和脱镁叶绿素a含量在大多区域较2007年变化不大,但在苏南至长江口近岸海域的含量有明显降低.所获的16个小型底栖动物类群的垂直分布及各类群对现存量的贡献较往年未见明显差异.小型底栖动物平均丰度为(1375 ± 793) ind·10 cm-2,生物量为(1203 ± 707) μg·10 cm-2.黄海小型底栖动物总体现存量较2007年低约1/3,并在浒苔暴发区域下降尤为明显,而南黄海冷水团海域则略有上升,由此导致南黄海的小型底栖动物现存量分布呈现从中央冷水区向外围减小的反常现象;相较于此,在浒苔灾害影响较小的北黄海则呈从冷水区向外围增加的趋势.统计分析显示,浒苔暴发区域的小型底栖动物丰度与盐度呈正相关,与叶绿素a含量不相关.浒苔的暴发对近岸的小型底栖生物现存量产生了明显的抑制,但导致小型底栖动物现存量降低的主要因素并非缘于饵料匮乏,而更可能是浒苔暴发后的沉积与降解过程产生的影响所致.

关键词: 小型底栖动物, 丰度, 生物量, 绿潮, 黄海冷水团, 长期施肥, 红壤性水稻土, 土壤有机碳含量, 土壤有机碳储量

Abstract: An investigation was made on the standing crop, spatial distribution, sediment environment of meiofauna at 33 stations (including 22 stations in cold water mass area and 9 stations in Enteromorpha prolifera bloom area) in the Yellow Sea at the late stage of E. prolifera bloom in summer 2008. In this southern Yellow Sea area which was seriously impacted by the green algal bloom, the silt and clay contents in the sediments in 2008 had an obvious increase, compared with those in 2007, and the sediment chlorophyll a and phaeophytin a contents in 2008 did not show obvious changes in cold water mass area but distinctly decreased in southern Jiangsu inshore area and Yangtze River estuary. Within the total 16 meiofaunal groups sorted, no marked variation was observed in their vertical distribution and in the contribution of each group to the total meiofauna. In 2008, the average abundance of meiofauna was (1375 ± 793) ind·10 cm-2, and the biomass was (1203 ± 707) μg·10 cm-2, both of which were decreased by about 1/3, compared with those in 2007. The meiofaunal standing crop was decreased more obviously in the stations heavily affected by the E. prolifera bloom, while that in the Yellow Sea cold water mass area was slightly increased, resulting in an unusual trend of meiofaunal standing crop decreasing from the central area of cold water mass to the inshore area in the southern Yellow Sea. By contrast, and as usual, the meiofaunal standing crop was increased from the cold water mass area to the inshore area in the northern Yellow Sea. Statistical analyses suggested that only the meiofaunal abundance had positive correlation with the salinity in the stations heavily affected by the green algal bloom. Our study indicated that macroalgal bloom obviously inhibited the standing crop of meiofauna in the inshore area. The decrease was not due to the deficiency of food concentration, but likely caused by the deposition and degradation of the E. prolifera bloom.

Key words: meiofauna, abundance, biomass, green algal bloom, Yellow Sea cold water mass, long-term fertilization, red paddy soil, SOC content, SOC storage.