葛洲坝下游中华鲟(Acipenser sinensis)产卵场地形分析

根据1981年葛洲坝截流至1998年对葛洲坝坝下河床研究的历史资料,结合1999~2006年间获得的中华鲟产卵场所在江段河床的5次地形数据,采用ArcGIS9.0软件,对中华鲟产卵场河床的高程、坡度、坡向等地形因子进行了详细分析。结果表明:葛洲坝至磨基山江段中华鲟产卵场与历史产卵场相比具有极其相似的特征,临江溪至虎牙滩江段中华鲟自然繁殖频率不高可能主要是因为地形不符合要求,从而造成相关的水文因子也不能满足需要。中华鲟自然繁殖前期的迁徙分布和产卵后受精卵的散播与河床地形都有一定的关系,葛洲坝水利枢纽下游河势调整工程较大地改变了葛洲坝至庙咀江段河床的地形,地形复杂度的增加可能对中华鲟自然繁殖前期的栖息有利,而河床坡度、底质的改变则可能会对中华鲟受精卵的散播和发育产生不利影响。有必要结合中华鲟历史产卵场精确的地形数据,对"中华鲟产卵场功能分区模型假说"进行验证,并针对产卵场地形对中华鲟自然繁殖的影响,做出进一步探讨。     

葛洲坝下游江段中华鲟产卵场食卵鱼类资源量估算

为定量评估食卵鱼类对中华鲟资源的危害,1997－2001年间,对中华鲟产卵场所在的葛洲坝水利枢纽坝址至下游庙嘴之间长约5km的江段,进行了渔业捕捞样本抽样和解剖检测,运用体长股分析方法并结合淦获物中不同种类的相对数量比例估算出食卵鱼类资源量,研究结果表明,吞食中华鲟卵的主要有圆口铜鱼,铜鱼,瓦氏黄颡鱼等11种鱼类,其年度资源量为197487－744487尾,多年平均444822尾。     

葛洲坝下游中华鲟（Acipenser sinensis）产卵场地形分析

根据1981年葛洲坝截流至1998年对葛洲坝坝下河床研究的历史资料,结合1999～2006年间获得的中华鲟产卵场所在江段河床的5次地形数据,采用ArcGIS 9.0软件,对中华鲟产卵场河床的高程、坡度、坡向等地形因子进行了详细分析。结果表明：葛洲坝至磨基山江段中华鲟产卵场与历史产卵场相比具有极其相似的特征,临江溪至虎牙滩江段中华鲟自然繁殖频率不高可能主要是因为地形不符合要求,从而造成相关的水文因子也不能满足需要。中华鲟自然繁殖前期的迁徙分布和产卵后受精卵的散播与河床地形都有一定的关系,葛洲坝水利枢纽下游河势调整工程较大地改变了葛洲坝至庙咀江段河床的地形,地形复杂度的增加可能对中华鲟自然繁殖前期的栖息有利,而河床坡度、底质的改变则可能会对中华鲟受精卵的散播和发育产生不利影响。有必要结合中华鲟历史产卵场精确的地形数据,对“中华鲟产卵场功能分区模型假说”进行验证,并针对产卵场地形对中华鲟自然繁殖的影响,做出进一步探讨。     

葛洲坝下中华鲟繁殖生物学特性及其人工繁殖效果

以1998—2004年(除2002年外)间从葛洲坝下产卵场捕获的57尾(雌36尾,雄21尾)中华鲟人工繁殖群体为材料,研究了中华鲟人工繁殖群体的繁殖生物学特性.结果表明:1998—2004年间中华鲟雌鲟体长240～320cm,体质量140～432kg,年龄15～30龄;雄鲟体长153～284cm,体质量70～244kg,年龄12～26龄.雌鲟催产率93·1%,雄鲟催产率100%.卵子可明显分为7种颜色;绝对怀卵量为20～59万粒,平均35·8万粒;相对怀卵量820～3020粒·kg-1,平均1590粒·kg-1.精液明显分为4种颜色;绝对采精量1000～5952ml,平均2597·8ml;相对采精量1·25～31·24ml·kg-1,平均13·3ml·kg-1.多年人工催产受精率平均达到63·7%,孵化率达到48·1%,6年共孵化出苗476·2万尾,保证了人工繁殖放流的实施.资料对比显示,中华鲟繁殖群体自然繁殖力大幅下降.     

三峡蓄水以来葛洲坝下中华鲟产卵场河床质特征变化

中华鲟是国家一级保护水生动物,是产底层产粘性卵鱼类。河床质构成了中华鲟受精卵和早期胚胎发育的物理环境,其变化可能直接影响中华鲟自然繁殖的规模和效果。基于水声学和水下视频技术对葛洲坝下现存唯一已知中华鲟自然产卵场的河床质特征进行了连续观测,对三峡水库蓄水以来中华鲟自然产卵场的河床质特征变化进行了研究。水声学分析结果显示,2004-2012年间,中华鲟产卵场区域内河床硬度未有明显变化,但粗糙度显著增加 (P < 0.05)。对产卵位点的河床质特征分析表明,下产卵区的硬度增加(2012年显著高于2008和2004年 (P < 0.05)),上产卵区硬度呈明显下降趋势(2004年显著高于2008和2012年(P < 0.05));上产卵区的河床粗糙度均呈不显著上升趋势(P > 0.05);下产卵场区的河床粗糙度呈显著上升趋势(P < 0.05)。水下视频观测结果显示,三峡蓄水导致的水体含沙量明显减少,对河床的冲刷日益明显,表现在产卵场江段沉积细砂和粗砂区域面积显著减少,河床卵石缝隙充塞度明显下降 (P < 0.05)。下产卵区在2007-2012年视频观察过程中发现河床卵石缝隙充分暴露,几乎没有任何细砂或粗砂填充,与上产卵区河床卵石缝隙充塞度特征明显不同。长期观测表明,2004-2012年期间中华鲟自然产卵位点发生了明显的改变,2004-2007年均发生在下产卵区,而2008-2012年均发生在上产卵区,自然繁殖规模和效果也明显下降。综合分析显示,中华鲟产卵场河床质特征的变化可能是导致中华鲟自然产卵位点的改变和迁移的原因,进而影响中华鲟自然产卵场的繁殖适合度,影响中华鲟自然繁殖的规模和效果。对三峡蓄水清水下泄的生态影响评估以及中华鲟自然产卵场的改良或修复有重要借鉴意义。     

中华鲟产卵场平面平均涡量计算与分析

采用Delft3D-Flow模型对葛洲坝下游中华鲟产卵场河段进行流场模拟,用实测资料对模型进行验证和参数率定,模拟结果和实测资料基本吻合.在此基础上,阐述了平面平均涡量计算方法,利用模拟所得流速场,通过计算得到中华鲟产卵场河段区域平面平均涡量强度分布.计算结果表明,鱼卵密集区的平面平均涡量为1.38×10-3～1.64×10-3s-1,说明中华鲟产卵对区域平面涡量强度有偏好选择,这种选择具有生物学意义.可为今后保护中华鲟产卵场水力学环境提供理论支持和参考.     

中华鲟物种保护的历史与前景

中华鲟是在我国和朝鲜近海生长,在长江上游或珠江中游繁殖的大型溯河洄游鱼类,长江中华鲟种群的繁殖季节在10月中旬至11月上旬1、2,珠江的在3初至4月初3,二者属于不同的生态类群,但也有学者认为二者是不同的种4,60年代末,国家决定在长江中下游交界处宜昌修建葛洲坝水利枢纽(以下简称葛洲坝),由于该枢纽将阻隔中华鲟的生殖洄游通道,有关其对中华鲟资源影响的程度,以及如何采取相应的保护措施等问题,曾引起广泛的争论。       

长江葛洲坝枢纽坝下江段中华鲟成鱼性腺的观察

1981年1月,葛洲坝水利枢纽截流,中华鲟被大坝所阻而滞留在宜昌以下的江段。1981年秋季在葛洲坝枢纽的坝下江段采集到中华鲟的Ⅲ、Ⅳ、Ⅵ期卵巢和Ⅲ、Ⅳ、Ⅴ期精巢,1982年秋季又采集到中华鲟产出的卵和早期鱼苗。研究结果表明,中华鲟在坝下江段不仅能发育成熟,而且能自然产卵。为了保护和增殖中华鲟,人工繁殖放流的方法是切实可行的。同时,必须严禁滥捕,以保护中华鲟资源。     

基于中华鲟繁殖群体数量的长江中、下游生态环境考核指标

繁殖群体数量是中华鲟能否成功繁殖的重要影响因子, 建议作为长江生态考核的重要评价指标。根据重要种群参数和历史数据, 基于稳态转换理论和方法, 确定中华鲟繁殖群体数量指标的评估基准值和等级, 670尾以上为“优”、400—670尾为“良”、200—400尾为“中”、50—200尾为“差”、50尾以下为“极差”。水声学探测结果显示, 1998—2001年中华鲟繁殖群体数量指标评级为“良”; 2004—2012年三峡工程蓄水后至向家坝蓄水前评级为“中”; 2013—2020年评级为“极差”。为了复壮中华鲟野生种群, 建议修复葛洲坝下中华鲟产卵场功能, 大规模放流性成熟亲鱼和大规格个体, 建立国家级中华鲟保育中心。     

长江中华鲟繁殖群体资源现状的初步研究

根据1994—1998年获得的246尾标本,对中华鲟繁殖群体的性比、性腺发育成熟个体比例、年龄结构、体长和体重特征等进行了研究。并结合历史资料,对其种群资源现状进行评价,提出了相应的资源保护措施建议。     

Hydrological Status of the spawning ground of Acipenser sinensis underneath the Gezhouba Dam and its relationship with the spawning runs

The spawning runs of Chinese Sturgeon (CS; Acipenser sinensis) were observed 37 times below Gezhouba Dam of Yangtze River between 1983 and 2004. Five hydrological factors (water temperature, water level, flow discharge, silt content and current velocity) were monitored on a daily basis at the spawning ground between October and November for 22 consecutive years (1983–2004). The effect of current velocity on the spawning ground at the bottom layer of the river, where CS was spawning for four years, was measured (1996–1999). The authors of this study analyzed the relationship between the five hydrological factors and the respective spawning runs. Twenty-two years of continuous observations indicated that the daily mean values of all the five hydrological factors fluctuated within a certain range when CS was spawning. It was concluded that the optimal values for the hydrological factors during the spawning runs are 18.0–20.0°C for temperature, 14100 m³/s for discharge volume, 42.0–45.0 m for water level above the sea level, and 0.2–0.3 kg/m³ for silt content in the water, wherein the current velocity above the bottom layer to stimulate the fish to spawn should be between 1.0–1.7 m/s. The optimal water temperature might provide an essential precondition for other factors to trigger spawning. As water temperature reaches the optimal values and most of the other parameters are at the brink of deviation from their optimal range of values (water level, current velocity and silt content in the water), CS would begin to spawn. By 2009, when the Yangtze Three Gorges Project, which is located 45 km upstream of the Gezhouba Dam, is completed and begins to operate normally, changes in the downstream water temperature are expected to occur, which may have a negative effect on the development of gonad and the stimulation of spawning of CS; however, the anticipated decrease of the silt content in the water may be considered favorable for the performance of the spawning site.     

Hydrological Status of the spawning ground of Acipenser sinensis underneath the Gezhouba Dam and its relationship with the spawning runs

The spawning runs of Chinese Sturgeon (CS; Acipenser sinensis) were observed 37 times below Gezhouba Dam of Yangtze River between 1983 and 2004. Five hydrological factors (water temperature, water level, flow discharge, silt content and current velocity) were monitored on a daily basis at the spawning ground between October and November for 22 consecutive years (1983–2004). The effect of current velocity on the spawning ground at the bottom layer of the river, where CS was spawning for four years, was measured (1996–1999). The authors of this study analyzed the relationship between the five hydrological factors and the respective spawning runs. Twenty-two years of continuous observations indicated that the daily mean values of all the five hydrological factors fluctuated within a certain range when CS was spawning. It was concluded that the optimal values for the hydrological factors during the spawning runs are 18.0–20.0°C for temperature, 14100 m³/s for discharge volume, 42.0–45.0 m for water level above the sea level, and 0.2–0.3 kg/m³ for silt content in the water, wherein the current velocity above the bottom layer to stimulate the fish to spawn should be between 1.0–1.7 m/s. The optimal water temperature might provide an essential precondition for other factors to trigger spawning. As water temperature reaches the optimal values and most of the other parameters are at the brink of deviation from their optimal range of values (water level, current velocity and silt content in the water), CS would begin to spawn. By 2009, when the Yangtze Three Gorges Project, which is located 45 km upstream of the Gezhouba Dam, is completed and begins to operate normally, changes in the downstream water temperature are expected to occur, which may have a negative effect on the development of gonad and the stimulation of spawning of CS; however, the anticipated decrease of the silt content in the water may be considered favorable for the performance of the spawning site.     

Impacts of variability of habitat factors on species composition of ichthyoplankton and distribution of fish spawning ground in the Changjiang River estuary and its adjacent waters

During June, August and October 2006, there were three multi-disciplinary surveys carried out in the Changjiang River estuary and its adjacent waters (122°00′–125°00′E, 27°50′–34°00′N) by R/V Beidou to study the species composition and abundance of ichthyoplankton (including fish eggs, larvae and juveniles), the spatial distribution of fish spawning ground and their relationship with habitat factors. There were 29, 29 and 25 grid stations sampled in the three cruises, respectively. The ichthyoplankton samples were collected by horizontally towing with a macro-plankton net (mouth diameter 80 cm, length 270 cm, mesh size 0.50 mm) at the sea surface, and the towing speed was 3.0 n mile/h at each sampling station. The towing lasted for 10 min. After hauling for each station, habitat factors including temperature and salinity were measured by Sea Bird-25 CTD. Samples were preserved in 5% formaldehyde solution immediately after sampling for analysis in laboratory. Since the trawl speed could not be accurately evaluated due to the effects of ocean currents and wind-induced wave, the amount of ichthyoplankton was evaluated by actual number of the sampling haul in each station. Ichthyoplankton collected were divided into three categories: dominant species, important species and main species by the index of relative importance (IRI). There are 71 species (including 1200 fish eggs and 2575 fish larvae and juveniles) collected during 3 cruises and 59 species have been correctly identified to species level, which belongs to 50 genera, 37 families and 9 orders; while 5 species can only be identified to genera level, 1 species only identified to family level and 6 species identified to order level. These 59 species identified to species level and 5 species identified to genera level are divided into three ecological patterns, i.e., brackish water species, neritic water species and coastal water species. Warm water species have 34 species in those 59 species identified to species level, accounting for 57.63%, warm temperature species have 25 species, accounting for 42.37%. According to the analysis of IRI, the dominant species are Engraulis japonicus (in June and August, that is important species in October), Scomber japonicus (in August), and Johnius grypotus (in October) during the survey; important species are Cynoglossus joyneri (in June and August), Trichiurus lepturus (in June, August and October), Gonorhynchus abbreviatus (in August), Stolephorus commersonii (in October), Saurida undosquamis (in October) and Saurida elongate (in October), and main species have 12 species in June, 9 species in August and 10 species in October, respectively. The amount of fish eggs and larvae of the dominant species, important species and main species (28 species) are 97.50% and 97.13% of the total amount of fish eggs and larvae, respectively, which are the important composition of fish eggs and larvae in the Changjiang River estuary and its adjacent waters.
In June and August of 2006, if compared with that in corresponding months in 1986, there are great changes in the habitat factors especially for temperature and salinity in the investigating areas: high salinity water from off-shelf is much closer to the coastal areas which results in the dramatic increase of sea surface salinity during all three surveys. Sea surface temperature, on the other hand, decreases distinctively in June, but significantly increases in August. The run-off of the Changjiang River greatly reduced due to the long-term drought in summer 2006, which is responsible for the great changes of habitat factors in the Changjiang River estuary and its adjacent waters. The habitat of the Changjiang River estuary is greatly changed, which consequently has significant influences on the spawning, breeding and the spatial distribution of spawning ground of neritic water species, such as Sardinella zunasi, Thryssa kammalensis, Thryssa mystax, Setipinna taty and S. commersonii ect, and coastal water species, such as Ilisha elongate and Konosirus punctatus ect.     

Impacts of variability of habitat factors on species composition of ichthyoplankton and distribution of fish spawning ground in the Changjiang River estuary and its adjacent waters

During June, August and October 2006, there were three multi-disciplinary surveys carried out in the Changjiang River estuary and its adjacent waters (122°00′–125°00′E, 27°50′–34°00′N) by R/V Beidou to study the species composition and abundance of ichthyoplankton (including fish eggs, larvae and juveniles), the spatial distribution of fish spawning ground and their relationship with habitat factors. There were 29, 29 and 25 grid stations sampled in the three cruises, respectively. The ichthyoplankton samples were collected by horizontally towing with a macro-plankton net (mouth diameter 80 cm, length 270 cm, mesh size 0.50 mm) at the sea surface, and the towing speed was 3.0 n mile/h at each sampling station. The towing lasted for 10 min. After hauling for each station, habitat factors including temperature and salinity were measured by Sea Bird-25 CTD. Samples were preserved in 5% formaldehyde solution immediately after sampling for analysis in laboratory. Since the trawl speed could not be accurately evaluated due to the effects of ocean currents and wind-induced wave, the amount of ichthyoplankton was evaluated by actual number of the sampling haul in each station. Ichthyoplankton collected were divided into three categories: dominant species, important species and main species by the index of relative importance (IRI). There are 71 species (including 1200 fish eggs and 2575 fish larvae and juveniles) collected during 3 cruises and 59 species have been correctly identified to species level, which belongs to 50 genera, 37 families and 9 orders; while 5 species can only be identified to genera level, 1 species only identified to family level and 6 species identified to order level. These 59 species identified to species level and 5 species identified to genera level are divided into three ecological patterns, i.e., brackish water species, neritic water species and coastal water species. Warm water species have 34 species in those 59 species identified to species level, accounting for 57.63%, warm temperature species have 25 species, accounting for 42.37%. According to the analysis of IRI, the dominant species are Engraulis japonicus (in June and August, that is important species in October), Scomber japonicus (in August), and Johnius grypotus (in October) during the survey; important species are Cynoglossus joyneri (in June and August), Trichiurus lepturus (in June, August and October), Gonorhynchus abbreviatus (in August), Stolephorus commersonii (in October), Saurida undosquamis (in October) and Saurida elongate (in October), and main species have 12 species in June, 9 species in August and 10 species in October, respectively. The amount of fish eggs and larvae of the dominant species, important species and main species (28 species) are 97.50% and 97.13% of the total amount of fish eggs and larvae, respectively, which are the important composition of fish eggs and larvae in the Changjiang River estuary and its adjacent waters.
In June and August of 2006, if compared with that in corresponding months in 1986, there are great changes in the habitat factors especially for temperature and salinity in the investigating areas: high salinity water from off-shelf is much closer to the coastal areas which results in the dramatic increase of sea surface salinity during all three surveys. Sea surface temperature, on the other hand, decreases distinctively in June, but significantly increases in August. The run-off of the Changjiang River greatly reduced due to the long-term drought in summer 2006, which is responsible for the great changes of habitat factors in the Changjiang River estuary and its adjacent waters. The habitat of the Changjiang River estuary is greatly changed, which consequently has significant influences on the spawning, breeding and the spatial distribution of spawning ground of neritic water species, such as Sardinella zunasi, Thryssa kammalensis, Thryssa mystax, Setipinna taty and S. commersonii ect, and coastal water species, such as Ilisha elongate and Konosirus punctatus ect.     

Evaluating the effects of controlled flows on historical spawning site access,reproduction and recruitment of lake sturgeon Acipenser fulvescens

Lake sturgeon Acipenser fulvescens spawn at the base of Kakabeka Falls, a 39 m waterfall on the Kaministiquia River, a tributary to Lake Superior. Access to this historical spawning site can be restricted or delayed due to hydroelectric flow fluctuations that coincide with the A. fulvescens spawning season. The objectives of this study were to determine (a) the necessary flow conditions that facilitate spawning site access; (b) quantity and duration of flow required for successful spawning and dispersal of larvae; and (c) evaluate recruitment of juvenile A. fulvescens in relation to flow. A. fulvescens spawning migrations were tracked using a stationary telemetry receiver that logged the movements of 166 A. fulvescens fitted with radio-transmitters. Unrestricted access to the spawning site was facilitated when spawning flow was controlled at 23 m³ s⁻¹ in 2004 and 17 m³ s⁻¹ in 2006. Fluctuating (0.5–8.5 m³ s⁻¹) and delayed spawning flows resulted in restricted and delayed access to the spawning site. Flow duration for successful egg incubation, hatch and larval dispersal was determined by sampling larvae using drift nets and quantified using cumulative temperature units (CTU). Over 10 years, 10,083 larvae were captured between 31 May and 20 July with 97% of the drift occurring prior to 30 June. From the date of first spawning to the end of larval dispersal took an average of 38.6 days, and the mean CTU value was 398.6. In general, a minimum flow of approximately 14.5 m³ s⁻¹ from the date of initial spawning to the accumulation of c. 400 CTU ensured successful hatch and larval dispersal. During the timeframe of this study, recruitment was variable. This study described the complex and variable reproductive life history of A. fulvescens and defined spawning flow requirements ecologically, which can be used to develop operational provisions at hydropower facilities to ensure successful reproduction.     

小浪底水库运行对黄河鲤鱼栖息地的影响

通过历史文献和实地生态调查,了解黄河鲤鱼生态习性及与径流组分响应关系,在此基础上,通过分析水库对径流组分影响,建立栖息地模拟模型,研究小浪底水库运行对黄河鲤鱼生存繁衍的影响。研究表明:(1)径流的流量组分与黄河鲤鱼的生态习性有密切的相关关系,小浪底水库的运行显著改变了流量脉冲、小洪水及大洪水,流量脉冲消失或减少使得黄河鲤鱼产卵缺乏足够的产卵栖息地;小洪水减少使黄河鲤鱼的食物来源和栖息地减少;漫滩洪水减少和消失使黄河鲤鱼失去从河滩地获得食物和栖息地机会。(2)通过建立River2D模型,得到了不同流量下黄河鲤鱼在不同生命阶段栖息地面积的变化情况,研究表明,建库后大于1400m3/s流量的显著减少,影响了黄河鲤鱼的产卵;建库后花园口低限流量变化不明显,建库对成鱼和幼鱼生存的影响不大。