Habitat scale and biodiversity: influence of catchment, stream reach and bedform scales on local invertebrate diversity

Although many studies have investigated the influence of environmental patterns on local stream invertebrate diversity, there has been little consistency in reported relationships between diversity and particular environmental variables. Here we test the hypothesis that local stream invertebrate diversity is determined by a combination of factors occurring at multiple spatial scales. We developed predictive models relating invertebrate diversity (species richness and equitability) to environmental variables collected at various spatial scales (bedform, reach and catchment, respectively) using data from 97 sampling sites dispersed throughout the Taieri River drainage in New Zealand. Models based on an individual scale of perception (bedform, reach or catchment) were not able to match predictions to observations (r < 0.26, P > 0.01, between observed and predicted equitability and species richness). In contrast, models incorporating all three scales simultaneously were highly significant (P < 0.01; r = 0.55 and 0.64, between observed and predicted equitability and species richness, respectively). The most influential variables for both richness and equitability were median particle size at the bedform scale, adjacent land use at the reach scale, and relief ratio at the catchment scale. Our findings suggest that patterns observed in local assemblages are not determined solely by local mechanisms acting within assemblages, but also result from processes operating at larger spatial scales. The integration of different spatial scales may be the key to increasing model predictability and our understanding of the factors that determine local biodiversity.     

岷江上游流域种子植物区系研究

岷江上游流域在地理位置上位于青藏高原、四川盆地两个自然地理区域的过渡地带;其在植被分区上属于泛北极植物区中国—喜马拉雅森林植物亚区横断山脉地区的一部分。区内共有种子植物169科,726属,2162种。其中大科、大属在区系组成中起着非常重要的作用。该区种子植物区系包含有15种分布区类型及其14个变型,其中泛热带分布、北温带分布、旧世界温带分布、东亚分布等成分占有重要地位。其种子植物区系的主要特征为：地理过渡特征明显,区系成分新老并存;区系地理成分复杂,以北温带成分为主;沿海拔梯度植物区系地理成分差异显著。在该区未来的生态建设中,应充分利用其植物区系的基本特征,保护现有物种,并充分利用当地具有特殊抗性的珍贵物种资源和遗传资源。     

Patchiness of River–Groundwater Interactions within Two Floodplain Landscapes and Diversity of Aquatic Invertebrate Communities

In fluvial systems, the interactions between rivers and groundwater significantly affect various ecological structures (for example, riparian vegetation) and functions. To examine the effects of hydrological exchange between groundwater and surface water on the distribution of aquatic invertebrates within a riverine landscape, we investigated the main stem, tributaries, and various surface and subsurface waters of two floodplains of a southern Alpine river (Brenno, Switzerland) in terms of their physicochemical, hydraulic, substratum, and faunal characteristics. The origins of the water were investigated by analyzing geomorphic settings and physicochemical variables. The two floodplains had different hydrological regimes. The middle floodplain was dominated by lateral inputs and exfiltration of hillslope groundwater from two different subcatchments. Bank filtration of river water sustained subsurface water only close to the channel. The aquatic habitats of the middle floodplain formed a rather homogeneous group with high taxon richness and intrahabitat diversities. These aquatic habitats resembled mountain springbrooks in their physicochemical characteristics and faunal compositions. In the lower floodplain, the exchange between river water and groundwater was more extensive. The aquatic floodplain habitats of the lower floodplain were fed mainly by deep and shallow alluvial groundwater, hyporheic exfiltration, and partly by surface water. In contrast to aquatic habitats of the middle floodplain, habitats of the lower floodplain showed a low intrahabitat and a high interhabitat diversity in terms of both substrate characteristics and faunal compositions. For both floodplains, ordination analyses showed a high concordance between the structure of the invertebrate community and the characteristics of the environmental habitat, including chemical, geomorphic, and hydraulic variables. Ordinations grouped aquatic habitats according to the origins of the waters. Taxon richness was related to local structural diversity, but species turnover was related to differential vertical and lateral connectivity. Exfiltration of groundwaters provided aquatic floodplain habitats for several specialized species. The results of this study show the significance of the river–groundwater connectivity for the creation of the habitat mosaic that sustains biodiversity in floodplains and thus have important implications for managing the ecological integrity of floodplains.     

New penis characters to distinguish between two American Artemia species

Biofilms are an ensemble of autotrophs and heterotrophs, which are highly efficient in removing inorganic and organic compounds, as well as other chemicals, from river water. They are, therefore, key elements in the self-purification processes which occur in rivers. Biofilm function is related to several environmental factors that govern river ecosystems: physical (light, temperature, water current), chemical (nutrient availability, toxicant effects), but also biological. Among the biological factors, community composition (algae, bacteria and fungi), biofilm structure (layer arrangement and biomass accumulation), and the presence of grazers determine variations in the efficiency of the self-depuration function of biofilms in rivers. Algae and bacteria show specific abilities for nutrients and other organic and inorganic compounds, but biofilm thickness may affect these abilities, both through a decrease in diffusion and by enhancing recycling within the biofilm. Nutrient uptake and consequently the capacity of biofilm to ameliorate water quality decreases with biomass. Moreover, biofilm thickness determines the effect of toxicants, since biomass prevents their diffusion through the biofilm. Grazing interferes in the relative efficiency of biofilms, by simplifying the composition of the biofilm community and by decreasing the amount of sorption and uptake of the biofilm. Closer attention should be paid to these aspects, since they unambiguously interfere with the performance of biofilms in the amelioration of the quality of river water.     

Spatial and temporal dynamics of phytoplankton communities along a regulated river system, the Nakdong River, Korea

The longitudinal distribution and seasonal fluctuation of phytoplankton communities was studied along the middle to lower part of a regulated river system (Nakdong River, Korea). Phytoplankton biomass decreased sharply in the middle part of the river (182 km upward the estuary dam), and then increased downstream reaching a maximum at the last sampling station (27 km upward the estuary dam). In contrast, there was little downstream fluctuation in species composition, irrespective of pronounced differences in nutrient concentrations (TN, TP, NO₃, NH₄, PO₄) as well as in algal biomass. In the main river channel, small centric diatoms (Stephanodiscus hantzschii, Cyclotella meneghiniana) and pennate diatoms (Synedra, Fragilaria, Nitzschia) were dominant from winter to early spring (November–April). A mixed community of cryptomonads, centric and pennate diatoms, and coenobial greens (Pediastrum, Scenedesmus) was dominant in late spring (May–June). Blue-green algae (Anabaena, Microcystis, Oscillatoria) were dominant in the summer (July–September). A mid-summer Microcystis bloom occurred at all study sites during the dry season, when discharge was low, though the nutrient concentration varied in each study site. Nutrients appeared everywhere to be in excess of algal requirement and apparently did not influence markedly the downstream and seasonal phytoplankton compositional differences in this river.     

Effects of dredge material placement on benthic macroinvertebrates of the Illinois River

Since the 1930s, dredge material has been removed from the Illinois River and placed along the main channel border in shallow depths to maintain a 2.7 m deep main channel for commercial navigation. Placement of this material changes the sediment composition from primarily silt/clay to primarily sand, and it buries pre-existing benthic invertebrates. During 1997 and 1998, the benthos of an 125 km reach of the middle Illinois River (La Grange Reach) was studied by extracting 1065 Ponar samples from randomly-selected sites which had never received dredge material, received dredge material one year previous, or received dredge material during the current year. Although total numbers of macroinvertebrates collected was lower in 1998 than in 1997, relative abundances of eight targeted taxa were highly similar between years. Chironimidae were most abundant and comprised >66% of all macroinvertebrates collected both years. Differences in densities of Chironomidae, Ephemeroptera, Sphaeriidae, Corbicula fluminea (Muller, 1774), Dreissena polymorpha (Pallas, 1771), Odonata, and Gastropoda among the three classes of dredge material placement were all significant (P< 0.05). For all taxa, densities were highest at sites that had never received dredge material; and, for all taxa except Chironimidae, densities were lowest at sites that received dredge material during the current year. No significant recovery by macroinvertebrates was noticed on dredge areas of this reach after one year (P>0.05). Future operations to maintain a channel for navigation should consider preexisting densities of macroinvertebrate taxa. Because benthic macroinvertebrates are an important component of the food web and shifting sand does not support diverse macroinvertebrate communities, strategic placement of dredge material by avoiding islands or other areas of high macroinvertebrate diversity could improve overall system productivity and biotic integrity of large river-floodplains.     

Nutrient limitation of plant growth on the floodplain of the Narran River, Australia: growth experiments and a pilot soil survey

Water resource development has altered the hydrological regime on the Lower Balonne River in Queensland, Australia. Concerns have been raised about possible impacts to floodplain plant communities, which support a pastoral industry and a range of native fauna. Water and nutrients commonly limit plant growth in south central Queensland, where the climate is semi-arid and the soils are infertile. Floodplain plant productivity is boosted by inundation with water, but the role of flooding in nutrient provision is not known. Growth experiments and a pilot soil survey were conducted to help determine if soil nutrient deficiencies exist and if regular flooding is required to maintain floodplain soil fertility. Soils were sampled from areas representing three flood frequency classes: high, moderate, and low. Chemical extractions were performed as a surrogate for `bioavailable' nutrients. Soil nitrogen (N) but not phosphorus (P) limited the growth of seedlings of wheat (Triticum aestivum L. Gardia) based on responses to nutrient additions: plants supplied with N had greater shoot length and total biomass than plants without N. Clear evidence of an effect of flood frequency on fertility was not revealed. Neither soil P, soil N, nor plant growth varied significantly with flood frequency. However, this analysis had low statistical power. There were trends for greater biomass of seedlings grown on moderately flooded soils and thinner roots for seedlings grown on frequently flooded soils, but neither of these growth responses was clearly linked to nutrient limitation. Nevertheless, the possibility that flooding provides a nutrient subsidy to plants cannot be ruled out because of a number of factors, including the statistical power of this analysis and the possibility that short-term nutrient subsidies occur with floods.     

Distribution patterns of nutrients and symptoms of eutrophication in the Rio de la Plata River Estuary System

In this paper we discuss nutrient dynamics and the effects of eutrophication in the Rio de la Plata River Estuary System since 1980. The tidal river was characterized by high suspended particulate matter (SPM), nutrients, and N:P ratio (>25), moderate chlorophyll a values, an inverse relationship between SPM and phosphate, and cianobacteria blooms. Seaward of the salinity front, where both SPM and nutrient concentrations are lower and chlorophyll a values greater, the net ecosystem metabolism is positive. Permanent stratification controls nutrient, organic matter and oxygen dynamics leading to biological stress and hypoxia below the halocline. Non conservative behavior of nitrogen in the estuary leads to a low N:P ratio (<3) because of both phytoplankton assimilation of nitrogen and denitrification, and benthic flux of phosphate. Periodic nuisance and toxic blooms occur at high salinities along the Uruguayan coast (Canal Oriental). Over the recent decades, changes in freshwater inflow, point and non-point nutrient load, and stratification, triggered by ENSO events, seem to have controlled the ecosystem metabolism, nutrient-oxygen dynamics, and the development of harmful blooms. The assessment of the regional and overall ranking of eutrophic conditions determines that the system is moderately eutrophied. Nevertheless, increasing trends in quantity of freshwater and nutrient loads, and the low potential to dilute and flush nutrients, suggest that the Rio de la Plata, in particular the Canal Oriental is prone to worsening eutrophication conditions like oxygen stress and harmful blooms.     

Applicability of a generic index for diatom assemblages to monitor pollution in the tropical River Tsanwun, Taiwan

A generic index (GI) utilizing epilithic diatom assemblages as abioindicator of water pollution in subtropical rivers in Taiwan was applied toastudy of a tropical river. Seven sites on the River Tsanwun were sampledseasonally from August 1995 to June 1998. Although there is a marked differencein water chemistry between tropical and subtropical rivers in Taiwan, thedominant genera of their diatom assemblages are quite similar. The six generaused for the calculation of GI in the subtropical rivers were also the maincomponents of diatom assemblages in the River Tsanwun. The calculated valuesdisplayed a close correlation with water quality, evaluated on the basis ofphysical and chemical variables. A strong correlation was found between this GIand other diatom-based indices of water quality.     

Geochemical and petrographic evidence of meteoric diagenesis in tufa deposits in Northern Dalmatia (Zrmanja and Krupa Rivers, Croatia)

Summary Holocene tufa deposits in the Northern Dalmatia region of Croatia occur along the banks and at present sites of waterfalls of the Zrmanja river and its tributary the Krupa river. Petrographic, geochemical and statistical analyses have been used to relate textural features and trace element composition to the degree of meteoric diagenesis. Trace metal concentrations associated with carbonate phase were determined by sequential extraction procedure. The insoluble residue (I.R.) is predominantly of primary origin and its amount ranges from 3% to 29%, averaging 13.75%, thus permitting variable water/rock ratios of the stabilazing meteoric system. All the evidence points to a scarcity of post-depositional recrystallization and cementation, but where present these features are accompanied by I.R., Mg, Sr and Zn depletion and Fe enrichment.