水库渔业营养类型划分标准研究──1.指标层次的确定

依据１９８０－１９９２年全国２０个省５５座水库渔业资源调查数据,运用Ｒ型聚类分析和主成分分析方法对４８项指标间的层次性进行分析,水库渔业营养类型划分标准的指导层次体系可确定为：第一层次包括地理,气候,水深,面积和体积,土壤,水文等６个小层次;     

政府补助对海洋渔业上市公司经营绩效的影响

海洋渔业在我国农业发展中发挥着重要作用,政府对海洋渔业上市公司实施了一系列扶持补助政策。文章对我国海洋渔业上市公司2012—2018年连续的财务数据进行实证研究,运用面板数据回归模型分析政府补助是否能够有效地促进海洋渔业上市公司经营绩效,并进一步以产权性质作为分组变量进行研究。通过实证研究发现：政府补助对海洋渔业上市公司的经营绩效有显著正向影响,且国有上市公司的政府补助效果优于民营上市公司。基于研究结论,提出以下建议：政府实施补助政策应坚持市场导向,并建立评估追踪机制,海洋渔业上市公司要建立科学的公示制度,明确补助资金的流向及用处。     

长江口大型工程对河口生境破碎化影响的初步研究

通过对工程海域26个站位的调查采样,研究分析了长江口深水航道治理一期工程对河口生境破碎化的影响。结果表明,工程已对长江河口区局部海域水体和底栖生境破碎化产生了明显影响,而对工程海域小尺度海洋水团、底栖生境和渔业资源生境的破碎化影响最大,造成局部小尺度海洋水团改变,部分渔业资源种类洄游通道、产卵场、肥育场、渔场生境破碎化。建议建立长江口生态特别保护区,加强对河口大型工程综合影响研究与生态修复,加强河口生态系统管理与执法力度,为长江口沿岸城市社会经济的可持续健康发展提供良好的海洋生态环境基础。     

海洋及相关产业分类研究

在研究分析海洋经济构成的基础上,以国民经济行业分类标准为依据,结合海洋经济统计工作实际,对我国海洋及相关产业的分类进行了探索研究,提出了核心层、支持层和外围层三个层次的海洋经济构成和海洋及相关产业的其分类方法。     

天津团泊洼水库水体生物生产力与渔业开发利用

天津市团泊洼水库属华北平原滨海盐碱性水库。1989年多学科综合调查的结果表明:该水体中营养盐类含量氮高磷低,挺水植物藨草、芦苇为主要初级生产者,浮游生物种类贫乏,现存量不高,周丛生物丰富。结果还表明,该水体仍有较大渔产潜力。应从调整鱼类种群结构着手,充分而合理地利用水体中的可更新资源,使渔业、环境协调发展。     

Standardizing CPUE of <Emphasis Type="Italic">Ommastrephes bartramii</Emphasis> for Chinese squid-jigging fishery in Northwest Pacific Ocean

Generalized linear models (GLM) and generalized additive models (GAM) were used to standardize catch per unit fishing effort (CPUE) of Ommastrephes bartramii for Chinese squid-jigging fishery in Northwest Pacific Ocean. Three groups of variables were considered in the standardization: spatial variables (longitude and latitude), temporal variables (year and month) and environmental variables, including sea surface temperature (SST), sea surface salinity (SSS) and sea level height (SLH). CPUE was treated as the dependent variable and its error distribution was assumed to be log-normal in each model. The model selections of GLM and GAM were based on the finite sample-corrected Akaike information criterion (AICC) and pseudo-coefficient (Pcf) combined P-value, respectively. Both GAM and GLM analysis showed that the month was the most important variable affecting CPUE and could explain 21.3% of variability in CPUE while other variables only explained 8.66%. The interaction of spatial and temporal variables weakly influenced the CPUE. Moreover, spatio-temporal factors may be more important in influencing the CPUE of this squid than environmental variables. The standardized and nominal CPUEs were similar and had the same trends in spatio-temporal distribution, but the standardized CPUE values tended to be smaller than the nominal CPUE. The CPUE tended to have much higher monthly variation than annual variations and their values increased with month. The CPUE became higher with increasing latitude-high CPUE usually occurred in 145°E–148°E and 149°E–162°E. The CPUE was higher when SST was 14–21°C and the SLH from −22 cm to −18 cm. In this study, GAM tended to be more suitable than GLM in analysis of CPUE.     

有效微生物菌群对养虾水体细菌生态和水质的影响

研究有效微生物菌群(EM)对养虾水体中异养细菌、弧菌、光合细菌、放线菌的数量以及水体水质的影响。结果表明,在养殖池中添加EM,对水体中的异养细菌、弧菌、光合细菌及放线菌的数量均有显著影响:实验组异养细菌数量比传统对照池减少40.0%,弧菌数量减少7.8%,光合细菌数量增加98.2%,放线菌数量增加99.2%。EM能改良水质条件,与对照组相比,实验组溶解氧提高11.0%,COD降低8.0%,氨氮含量降低20.7%,亚硝酸氮含量降低10.0%。另外,实验组对虾成活率比对照组提高23.08%,饵料系数下降9.4%,利润提高了16.11%。     

厦门杏林虾池夏冬季微型浮游动物对浮游植物的摄食压力

20 0 0年 8月和 2 0 0 1年 2月 ,在杏林虾池用稀释法研究了微型浮游动物对浮游植物的摄食压力 .结果表明 :砂壳纤毛虫、甲壳类无节幼体是微型浮游动物的优势种 ;浮游植物生长率夏季为 0 .40～ 1 .0 1 /d、冬季为 0 .1 8～ 0 .96/d ;浮游动物的摄食率夏季为 0 .578～ 1 .3 2 4/d、冬季为 0 .2 0 4～ 0 .2 55/d ;日摄食率 (以C计 )夏季为 1 9.1 7～89.51mg/(m3·d)、冬季为 3 .3 2～ 7.2 3mg/(m3·d) ,各占浮游植物现存量的 43 .90 %～ 73 .40 %、1 8.43 %～ 2 2 .51 %;对初级生产力的摄食压力夏季为 1 1 5.2 3 %～1 93 .52 %、冬季为 3 7.47%～ 1 1 1 .3 1 %.     

厦门潘涂对虾养殖垦区浮游植物的生态特征

1995年6月至1996年5月对厦门市潘涂对虾养殖垦区的浮游植物进行了调查，鉴定虾池浮游植物82属300种。其中，硅藻229种（底栖种类为主），甲藻30种，绿藻30种，蓝藻5种，隐藻和裸藻各3种。发现虾池浮游植物数量上以硅藻、绿藻和甲藻为主，并且多属于微型和超微型种类、调查虾池浮游植物的生态特征与邻近海区有较大的差别。文中还对浮游植物生态特征及其与保持虾池水质环境稳定性关系方面作了初步探讨。     

The Pacific Decadal Oscillation

The Pacific Decadal Oscillation (PDO) has been described by some as a long-lived El Niño-like pattern of Pacific climate variability, and by others as a blend of two sometimes independent modes having distinct spatial and temporal characteristics of North Pacific sea surface temperature (SST) variability. A growing body of evidence highlights a strong tendency for PDO impacts in the Southern Hemisphere, with important surface climate anomalies over the mid-latitude South Pacific Ocean, Australia and South America. Several independent studies find evidence for just two full PDO cycles in the past century: “cool” PDO regimes prevailed from 1890–1924 and again from 1947–1976, while “warm” PDO regimes dominated from 1925–1946 and from 1977 through (at least) the mid-1990's. Interdecadal changes in Pacific climate have widespread impacts on natural systems, including water resources in the Americas and many marine fisheries in the North Pacific. Tree-ring and Pacific coral based climate reconstructions suggest that PDO variations—at a range of varying time scales—can be traced back to at least 1600, although there are important differences between different proxy reconstructions. While 20th Century PDO fluctuations were most energetic in two general periodicities—one from 15-to-25 years, and the other from 50-to-70 years—the mechanisms causing PDO variability remain unclear. To date, there is little in the way of observational evidence to support a mid-latitude coupled air-sea interaction for PDO, though there are several well-understood mechanisms that promote multi-year persistence in North Pacific upper ocean temperature anomalies.