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| 1 | 中国近海生态系统碳循环与生物固碳显示文摘本文系统总结了近几年来中国近海海-气界面碳通量及控制因素、近海碳循环的关键过程以及近海生物固碳强度的研究进展,提出了中国近海渔业碳汇过程研究应关注的主要科学问题。近海海一气界面碳通量过程、生物泵过程、颗粒物沉降与释放以及捕捞/养殖碳转移过程是中国近海生态系统碳循环的主要控制过程。中国近海在总体上是大气二氧化碳的汇,年吸收3000万~5000万t碳,但在部分浅海海域如胶州湾、长江口等是大气二氧化碳的源;中国近海浮游植物的年固碳量可达6.39亿t,春季和夏季浮游植物固碳占全年的65.3%。南海浮游植物固碳达4.16亿t,为渤海、黄海和东海的2倍。渔业捕捞与海水养殖可明显增加海洋碳汇,仅就近几年大型藻养殖而言,每年可多固定40万t碳,如果每年的养殖量增加5%,到2020年大型藻养殖可固定碳93万t/年,所以,为增加渔业捕捞与海水养殖碳汇,必须加强揭示渔业碳汇海域生态环境、建立渔业碳增汇强度评估方法以及明确渔业资源利用碳再生循环周期等研究。 | 宋金明 | 2011 | 中国水产科学2011，18，3： | 32 |
| 2 | 三种主养草鱼池塘沉积物-水界面碳通量的研究显示文摘为了探讨环境因子和底栖配养生物对碳通量的影响,采用实验室培养方法,测定并比较了不同混养模式下沉积物-水界面各形态碳的通量,监测了8月沉积物-水界面上覆水中各形态碳含量的昼夜变化。3种主养草鱼池塘的养殖模式为草鱼、鲢和鳙混养(GSB),草鱼、鲢、鳙和凡纳滨对虾混养(GSBL),草鱼、鲢、鳙和鲤混养(GSBC)。主要实验结果如下:(1)在养殖周期内,3种混养模式沉积物-水界面可溶性无机碳(DIC)通量范围为0.65~16.90 mg/(m^2·d),可溶性有机碳(DOC)通量范围为0.16~13.49 mg/(m^2·d),颗粒性有机碳(POC)通量范围为-2.29~3.32 mg/(m^2·d);GSB和GSBC模式各形态碳通量均以8月最高,GSBL模式则以7月最高。(2)在养殖周期内,3种混养模式沉积物对DIC和DOC均表现为释放,而对POC在4-6月以吸收为主,其余时间表现为释放。(3)在养殖的中后期,3种混养模式的DIC、DOC和POC通量存在一定差异。其中,GSBL和GSBC模式中各形态碳通量值显著高于GSB模式(P〈0.05)。(4)8月上覆水中DIC和DOC的含量在4:00达到最大值,POC含量则表现为GSBL模式在4:00达到最大值,12:00达到最小值,而GSBC模式在4:00达到最小值,12:00达到最大值。(5)各形态碳通量的变化与上覆水中的DO、p H呈显著负相关关系,而与水温呈显著正相关关系。 | 熊莹槐 王芳 陈燕 董双林 刘峰 | 2015 | 水产学报2015，39，7： | 5 |
| 3 | Zooplankton spatial and diurnal variations in the Changjiang River estuary before operation of the Three Gorges Dam显示文摘Estuarine plankton communities can serve as indicators of ecosystem modification in response to anthropogenic influences. The main objectives of this study were to describe the spatial distribution and diurnal variability in zooplankton abundance and biomass over almost entire salinity gradient of the Changjiang (Yangtze) River estuary and to provide a background reference for future studies. To accomplish this, data were collected from 29 stations in the estuary from May 19 to 26, 2003, including two anchor stations. The spatial and diurnal variations in zooplankton characteristics, i.e. abundance, biomass, and gross taxonomic composition, were examined. Generally, both the abundance and biomass gradually increased seaward and presented distinct spatial variations. In addition, the spatial data revealed a significant correlation between abundance and biomass; however, there was no significant correlation between abundance and biomass for the diurnal data. Although the zooplankton composition indicated distinct spatial differences in terms of dominant groups, copepods accounted for >50% of the total zooplankton abundance in most regions and times. Three zooplankton assemblages were recognized through hierarchical cluster analysis. These assemblages existed along the salinity gradient from fresh water to seawater, and their positions coincided with those of the three principal water masses in the estuary. The assemblages were classified as: (1) true estuarine, (2) estuarine and marine, and (3) euryhaline marine, which were characterized by the copepods Sinocalanus dorrii, Labidocera euchaeta, and Calanus sinicus, respectively. Both spatial and diurnal data indicated that there was no significant correlation between zooplankton abundance/biomass and depth-integrated phytoplankton abundance. | 高学鲁 宋金明 李学刚 | 2011 | Chinese Journal of Oceanology and Limnology2011，29，3： | 3 |
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