Short-term effects of a large dam decommissioning on biofilm structure and functioning

Aging dams and the rising efforts to restore stream ecosystems are increasing the number of dam decommissioning programs. Although dam decommissioning aims at improving in-stream habitat, biodiversity, and ecosystem functioning in the long term, it might also cause ecological impacts in the short term due to the mobilization of the sediment accumulated in the reservoir. Benthic biofilm in particular can be impaired by episodes of high turbidity and scouring. We conducted a multiple before-after/control-impact experiment to assess the effects of the drawdown of a large dam (42 m tall), a first step to its decommissioning, on biofilm structure (biomass and chlorophyll-a) and functioning (metabolism, nutrient uptake, and organic matter breakdown). Our results show that the reservoir drawdown reduced the autotrophic biofilm biomass (chlorophyll-a) downstream from the dam, which in turn lowered metabolism. However, nitrogen and phosphorus uptake by the biofilm was not affected. Organic matter breakdown was slower below the dam than in nearby undammed reaches before and during drawdown. All drawdown effects quickly disappeared and reaches downstream from the dam approached values found in nearby undammed reaches. Thus, our results indicate that the effects of reservoir drawdown on stream biofilms exist but may be small and disappear rapidly.     

Une etude sur clarias senegalensis val. dans la region du lac kossou (cote d'ivoire)

A study on Clarias senegalensis Val. in the region of Lake Kossou (Ivory Coast). Clarias senegalensis is the dominant silurid of the man-made lake Kossou and some smaller impoundments in the same region. Comparison of data spread over a five year period starting from 1970, some months before the dam was completed, reveals that the density of C. senegalensis dropped to the original level that existed in the river after reaching a peak in the years following the damming. This phenomenon which coincides with the impoverishment of the lake waters, is explained by the fact that C. senegalensis has its optimal habitat in poorly oxygenated waters, rich in organic matter. It is able to colonize this kind of productive waters thanks to the suprabranchial organ. In these optimal conditions it mainly feeds on aquatic insects and plankton.The fecundity of C. senegalensis may reach 20o ooo ripening eggs per female. Reproduction occurs during the rainy season in flooded savannas. Growth rates are very high and the age determinations show that, in the region of Kossou, C. senegalensis reaches an average standard length of 620 mm (2.7 kg) within three years.Our results are compared to literature data on other related species of the genus Clarias and the position of C. senegalensis within this generic complex is discussed.

     

Patterns of change in zooplankton community structures and the selective feeding of Bleak, Alburnus alburnus (L.) in the Serre Ponçon dam between 1980 and 1996

The Serre Ponçon reservoir, in the southern French alps, filled when the dam was completed in 1960. It has meso-eutrophic characteristics. Two hydrobiological studies carried out in 1980 and in 1996 showed interspecific variation in zooplankton and fish communities. A strong development of B. longirostris, D. brachyurum and C. pulchella, characteristic of eutrophic environments, was apparent in 1996, while the population of Daphnia longispina, which was dominant in 1980, had declined. At the same time, strong growth of the bleak Alburnus alburnus, was observed. Research into prey selection over several seasons showed that prey size and density were often a determining factor for capture, e.g., in C. pulchella, D. longispina and C.v. vicinus. However, some small sized rare species such as B. longirostris were also much sought after.     

Are we underestimating the genetic variances of dimorphic traits?

Populations often contain discrete classes or morphs (e.g., sexual dimorphisms, wing dimorphisms, trophic dimorphisms) characterized by distinct patterns of trait expression. In quantitative genetic analyses, the different morphs can be considered as different environments within which traits are expressed. Genetic variances and covariances can then be estimated independently for each morph or in a combined analysis. In the latter case, morphs can be considered as separate environments in a bivariate analysis or entered as fixed effects in a univariate analysis. Although a common approach, we demonstrate that the latter produces downwardly biased estimates of additive genetic variance and heritability unless the quantitative genetic architecture of the traits concerned is perfectly correlated between the morphs. This result is derived for four widely used quantitative genetic variance partitioning methods. Given that theory predicts the evolution of genotype‐by‐environment (morph) interactions as a consequence of selection favoring different trait combinations in each morph, we argue that perfect correlations between the genetic architectures of the different morphs are unlikely. A sampling of the recent literature indicates that the majority of researchers studying traits expressed in different morphs recognize this and do estimate morph‐specific quantitative genetic architecture. However, ca. 16% of the studies in our sample utilized only univariate, fixed‐effects models. We caution against this approach and recommend that it be used only if supported by evidence that the genetic architectures of the different morphs do not differ.     

Shifts of food habit and jaw position of white-spotted charr after damming

Stomach fullness of white-spotted charr, Salvelinus leucomaenis did not differ significantly between above-dam (allopatric with masu salmon) and below-dam (sympatric with masu salmon) areas, but stomach contents did. Juveniles (1+) below the dam consumed relatively more aquatic insects (benthic prey), and those above the dam consumed relatively more terrestrial insects (drifting prey), but there was no difference in the diet of >2+ fish between areas. The mouths of juveniles above the dam were more terminal than those of fish below the dam. The adaptive significance of these differences is discussed in relation to differences in fish assemblages. 1999 The Fisheries Society of the British Isles     

Unexpected CH4 emission from the Three Gorges Reservoir and its implications

Until the end of last century, scientists began to show their concern about greenhouse gas emission from reservoirs and questioned the “green credential” of hydroelectric dams since then. Through measurements along the channel of the TGR, an unexpectedly low CH₄ emission rate was recently observed from the surface of the TGR, much lower than our assumed estimate before. Moreover, the rate from the TGR is lower than that from many hydroelectric reservoirs. One possible reason for such a low emission rate is that lack of substrates supplied by decomposed vegetation limits the CH₄ production in the sediment of the TGR because of vegetation clearance since 2002 before impounding, whose primary purpose is to conserve the water quality. These results indicated that TGR is not a hotspot of CH₄ emission. On a broader sense, it also indicated that removal of flooded vegetation would help to decrease CH₄ emission from dam reservoirs before impounding, especially in the drawdown area.     

Unexpected CH4 emission from the Three Gorges Reservoir and its implications

Until the end of last century, scientists began to show their concern about greenhouse gas emission from reservoirs and questioned the “green credential” of hydroelectric dams since then. Through measurements along the channel of the TGR, an unexpectedly low CH₄ emission rate was recently observed from the surface of the TGR, much lower than our assumed estimate before. Moreover, the rate from the TGR is lower than that from many hydroelectric reservoirs. One possible reason for such a low emission rate is that lack of substrates supplied by decomposed vegetation limits the CH₄ production in the sediment of the TGR because of vegetation clearance since 2002 before impounding, whose primary purpose is to conserve the water quality. These results indicated that TGR is not a hotspot of CH₄ emission. On a broader sense, it also indicated that removal of flooded vegetation would help to decrease CH₄ emission from dam reservoirs before impounding, especially in the drawdown area.     

Invertebrate community and stream substrate responses to woody debris removal from an ice storm-impacted stream system, NY USA

We assessed the influence of ice-storm-derived debris dams on aquatic macroinvertebrates and stream substrates in a high-gradient watershed in the eastern Adirondack Mountains of New York State. Using a modification of electrofishing techniques, invertebrates were collected once before (June 2000) and once after (June 2001) wood removal from the downstream reach in each of six pairs of reaches (second and third-order streams). Stream substrates were also mapped in 2000 and 2001 to evaluate shifts in dominant substrates within a reach following wood removal. The following metrics were used to compare the invertebrate communities before and after wood removal: genera similarity, Shannon–Weiner equitability, taxa richness, dominant taxon, percent dominance and functional feeding group relative abundance. The changes in removal reaches were evaluated relative to changes in upstream reference reaches using a Before-After Control-Impact (BACI) design and analysis. Stream substrates did not change significantly in response to wood removal, although a trend toward coarser substrates was observed following removal. Following wood removal, the relative proportion of grazers increased upstream and downstream from removed dams in all streams; however, comparisons of other metrics indicated no significant response to removal. Invertebrate responses to wood removal were lower than expected, perhaps due to the presence of abundant boulder-formed pools in this high gradient system. Electronic supplementary material Electronic supplementary material is available for this article at and accessible for authorised users.     

Physical and chemical post-dam alterations in the Jamari River, a hydroelectric-developed river of the Brazilian Amazon

The regulation of the Jamari River advanced peak floods by 1–2 months and increased dry-season discharges from 60 to 200 m³ s^–1, resulting in water levels approximately 1 m above those recorded before regulation. Daily variation in water level associated with fluctuations in electricity production by the dam propagated to the lower reaches of the tributary Candeias River. Dissolved oxygen (DO), temperature, pH, and conductivity measured over 1.5 years on three locations along the regulated and two free-flowing rivers indicated important alterations in the case of oxygen concentrations. DO levels shifted from saturated (7–8 mg l^–1) during the flood season (when the spillways were open releasing epilimnetic water) to hypoxic (1.5–3 mg l^–1) during the dry season (when the floodgates were closed and only hypolimnetic water used to run the turbines was feeding the river). Fluctuations in water level and variation in dissolved oxygen tended to be greater at the site closest to the dam, gradually attenuating downstream. Mitigation of the downstream effects of river regulation would require modifications in the operation of the dam.     

长江胭脂鱼的洄游问题及水利工程对其资源的影响

胭脂鱼为我国特有鱼类,自然分布地仅在长江和闽江。长江上游为胭脂鱼的主要分布区,孵化出的部分幼鱼可能会随水流漂至长江中下游及其附属水体生长发育,至性成熟前返回上游参加繁殖,其后留在上游生活。目前长江上游和葛洲坝以下江段已存在自然繁殖的不同的胭脂鱼种群;葛洲坝和三峡水利枢纽的建设不会直接威胁胭脂鱼物种的生存和繁衍。