Benthic macrofaunal communities in intermittent estuaries during a drought: Comparisons with permanently open estuaries

Drought conditions have prevailed in many areas of NSW since 2002. On the mid-north coast, below-average rainfall resulted in reduced riverine flows and the extended closure of intermittent estuaries within the Solitary Islands Marine Park. Patterns of structure of benthic infaunal communities were evaluated at the height of the drought to determine if they differed between closed, intermittent estuaries and permanently open estuaries within the region. Replicate van Veen grab samples were taken in the upper, mid- and lower reaches of six intermittent and three permanently open estuaries and sieved to retain the macrofauna. A range of physico-chemical measures was also taken at each sampling time. Multivariate analyses of assemblage data revealed a significant difference between the structure of the two estuary types and also among estuaries within each type. Differences between estuary types were attributable to small differences in the abundance of a number of taxa but also to the absence of the amphipod Urohaustorius metungi from most of the intermittent estuaries. In contrast, these small amphipods dominated communities in the lower reaches of the permanently open estuaries. Physico-chemical variables were highly variable among estuaries and were not strongly correlated with assemblage patterns. Correlations with catchment size were the strongest and, as most of the intermittent estuaries in the region are smaller than the permanently open estuaries, this confounds the interpretation of assemblage patterns in this preliminary study. In order to differentiate between the effects of catchment size and entrance status, the same estuaries need to be resurveyed during periods when at least some of the intermittent estuaries are open.     

High temporal resolution of ion fluxes in semi-natural ecosystems – gain of information or waste of resources?

Monitoring programs of ion concentrations and fluxes in semi-natural ecosystems are confronted with the task to gain as much information as possible with simultaneously minimizing costs and efforts. The aim of this study was (i) to assess how much of the heterogeneity of solution concentrations is lost because of temporal integration of measurements and (ii) to estimate the error in ion fluxes due to temporal integration. High resolution measurements (daily interval) of ion concentrations (sulfate, nitrate, chloride, pH and EC) in throughfall, soil solutions and runoff at the catchment Lehstenbach (Fichtelgebirge, Northeast Bavaria, Germany) were compared over a two year period with the reference monitoring program (biweekly measurement interval). Evaluation of the maximum temporal heterogeneity of ion concentrations in throughfall, soil solution and runoff (expressed as minimum, maximum, median and 25–75% percentile) did not result in an overall higher heterogeneity of the high resolution measurements compared to the reference program. The calculation of runoff fluxes from the reference data (biweekly concentration) resulted in significant errors of up to 25% for time periods < 1 year (high resolution data was considered the "true" value and set as 100%). However, errors became minor (< 10%) if longer time periods were considered. The suitability of different interpolation methods to up-scale biweekly concentration data for the calculation of runoff fluxes was evaluated in this study. We concluded for the monitoring programs at the Lehstenbach catchment that a biweekly measurement interval seemed to be suitable to capture the heterogeneity of ion concentrations and fluxes (and thus temporal trends). In comparison, high resolution measurements with a daily measurement interval were higher in cost, work and time resources and had a relatively low information gain. While the introduced methods are applicable in all monitoring programs, conclusions on temporal resolution of measurements are most likely not valid for systems where ion concentrations have a low autocorrelation length (e.g., agricultural or urban systems with nitrate or pesticide treatment; tropical systems with extreme temperature or hydrological events).     

Chlorine transport in a small catchment in southeast Sweden during two years

Previous studies have revealed that chlorine participates in a complex biogeochemical cycle in soil, which suggests that the transport of chloride through catchments may also be influenced. The present study is based on field observations of organic carbon, chloride (Cl_in), and chlorinated organic carbon (Cl_org) in precipitation, soil, and runoff over a 2-year period from a small, forested catchment in southeast Sweden. The study reveals that (1) the soil pool is dominated by Cl_org, (2) the input via wet deposition and output of Cl_in via runoff is 30 times smaller than the total storage of chlorine (Cl_in + Cl_org) in soil, and (3) the transport is dominated by Cl_in. The organic matter that entered the outlet of the catchment was more chlorinated in the autumn than during the rest of the year, and rain events taking place in low-flow periods had a greater influence on TOC, Cl_org, and Cl_in than did rain events taking place in high-flow periods. The seasonal pattern in combination with the low-flow versus high-flow pattern and previous findings of increasing chlorine-to-carbon ratios with soil depth suggests that the chlorine-to-carbon ratio variation in the leached organic matter is due that water preferentially comes from deeper layers in low-flow conditions. This study provides well-founded estimates of Cl_org and Cl_in storage and fluxes for the studied catchment; however, the processes underlying the observed seasonal Cl_org variations and transportation processes need further study.     

The hydrogeology of a catchment area and an artificially divided dystrophic lake — consequences for the limnology of Lake Fuchskuhle

The hydrogeology between the catchment area and the divided dystrophic Lake Fuchskuhle with respect to the genesis and the land-water interactions were investigated. Water levels at numerous locations in the catchment area were measured in order to characterize the hydrology. The water balance of the area was calculated based on long term climatic investigations. The geology of the peat was documented at 25 sampling points by cores collected with a peat drill. Chemical parameters including pH, total phosphorus and total nitrogen concentrations, DOC concentration, colour (SAK 436 m^–1) and the UV₂₅₄/DOC ratio in the catchment area and in two compartments (NE and SW compartment) were determined. The chemical fluxes of DOC, nitrogen and phosphorus from the catchment area into one compartment (SW compartment) were determined. During the genesis of the Lake Fuchskuhle area two aquifer systems (local peat aquifer, regional sandy main aquifer) developed. Both aquifers are largely independently with almost no lateral interactions. Two compartments are supplied with water from the local peat aquifer. From the other two compartments, however, water is flowing out into the peat body. During high groundwater inflow into the SW compartment higher concentration of DOC, nitrogen and phosphorus in the SW compartment were detected. The fen can be divided in two parts: in the meso — to eutrophic fen northwest and the mainly meso — to oligotrophic — acid fen in the southeast. The significant differences in parameters such as pH, conductivity and DOC concentration gave a clear picture of the heterogeneity of the two compartments and their dependence on the catchment area with the two aquifers.     

Relationships between lake macrophyte cover and lake and landscape features

We examined the ability of lake and landscape features to predict a variety of macrophyte cover metrics using 54 north temperate lakes. We quantified submersed cover, emergent cover, floating leaf cover, Eurasian watermilfoil cover and total macrophyte cover. Measured lake features included lake physio-chemical and morphometric variables and landscape features included hydrologic, catchment and land use/cover variables. Univariate regression analyses demonstrated that these macrophyte cover metrics are predicted by a wide range of predictor variables, most commonly by: Secchi disk depth, maximum or mean depth, catchment morphometry, road density and the proportion of urban or agricultural land use/cover in the riparian zone or catchment (r² = 0.06–0.46). Using a combination of lake and landscape features in multiple regressions, we were able to explain 29–55% of the variation in macrophyte cover metrics. Total macrophyte cover and submersed cover were related to Secchi disk depth and mean depth, whereas the remaining metrics were best predicted by including at least one land use/cover variable (road density, proportion local catchment agriculture land use/cover, proportion cumulative catchment urban land use/cover, or proportion riparian agriculture land use/cover). The two main conclusions from our research are: (1) that different macrophyte growth forms and species are predicted by a different suite of variables and thus should be examined separately, and (2) that anthropogenic landscape features may override patterns in natural landscape or local features and are important in predicting present-day macrophytes in lakes.     

CO2-fluxes in different plant communities of a high-Arctic tundra watershed (Western Spitsbergen)

Abstract. There is little information on (1) whether the net carbon balance is positive or negative in different habitats in high Arctic ecosystems such as Spitsbergen today, and (2) what effect a cloudier, cooler summer could have on carbon balance. To provide data on this subject CO₂-flux measurements in different plant communities were made in the high-Arctic coastal tundra of Spitsbergen, using a mobile macro-cuvette system based on infrared gas analysis. The study area was situated on the exposed west coast, where westerly winds produce precipitation daily in the form of rain, drizzle and fog. During the cold and cloudy measurement period in 1996, light and surface temperatures were limiting for primary producers, resulting in low size and low physiological activity of the plants. Net CO₂-flux measurements showed carbon fluxes from soil to atmosphere in most of the communities even during the brightest hours of the day, when mean photon flux density was 325 mmol m^-2 s^-1. Calculations based on spatial distribution of the plant communities and soils in the watershed combined with C-flux measurements revealed information on daily carbon loss. For instance, the Drepanocladus community, covering 21 % of the catchment area, was responsible for 42.6 % of the catchment carbon loss. Only two of nine investigated plant communities, the Racomitrium and a Salix-Saxifraga community on debris, both adapted to frequent fog situations, were able to compensate for respiratory CO₂-losses under the prevailing low light conditions during daytime. Since there were no significant sunny periods in this area in the summer of 1996, the habitats of the investigated coastal tundra finished the season with a marked carbon loss due to increased cloudiness.     

香溪河流域一条一级支流河岸林凋落物季节动态

对神农架南坡的一条一级支流河岸林的凋落物进行了一年的连续收集研究。结果表明：凋落物干重年输入量为438．72g／m^2,其中树叶凋落物是凋落物的主要成分,占整个凋落物年产量的84％。凋落物的输入明显存在季节性的时间格局。凋落物在秋季的产量占全年产量的75％,春季占6．2％,夏季占13．6％,冬季为5．5％。凋落物组成中,树叶和花果的产量显示出季节变化的趋势;枝条的产量并未显示出明显的季节趋势。在秋季,树叶的产量占全年树叶总量的83％;枝条最高值出现于秋季,产量占全年总员的29％;花果在整个凋落物中所占比重分小,最高值出现在夏季,占年产量的63％。着生藻类的密度月际间的变化较大,存在着显著的差异。最大值与最小值的出现月份与凋落物最大、最低值的出现月份相同。通过统计分析表明,着生藻类的密度变化与凋落物和树叶凋落物的动态具有明显的相关性。     

Relationships between morphometry,geographic location and water quality parameters of European lakes

I addressed the question how lake and catchment morphometry influences water chemistry and water quality over a large scale of European lakes, and developed the regression equations between most closely related morphometric and water quality indices. I analysed the data of 1,337 lakes included in the European Environment Agency (EEA) database, carrying out separate analyses for three basic lake types: large lakes (area ≥100 km², 138 lakes), shallow lakes (mean depth ≤3 m, 153 lakes) and large and shallow lakes (area ≥100 km² and mean depth ≤8 m, 35 lakes). The study revealed that in Europe, the lakes towards North are larger but shallower and have smaller catchment areas than the southern lakes; lakes at higher altitudes are deeper and smaller and have smaller catchment areas than the lowland lakes. Larger lakes have generally larger catchment areas and bigger volumes, and they are deeper than smaller lakes, but the relative depth decreases with increasing surface area. The lakes at higher latitudes have lower alkalinity, pH and conductivity, and also lower concentrations of nitrogen and phosphorus while the concentration of organic matter is higher. In the lakes at higher altitudes, the concentration of organic matter and nutrient contents are lower and water is more transparent than in lowland lakes. In larger lakes with larger catchment area, the alkalinity, pH, conductivity and the concentrations of nutrients and organic matter are generally higher than in smaller lakes with smaller catchments. If the lake is deep and/or its residence time is long, the water is more transparent and the concentrations of chlorophyll a, organic matter and nutrients are lower than in shallower lakes with shorter residence times. The larger the catchment area is with respect to lake depth, area and volume, the lower is the water transparency and the higher are the concentrations of the nutrients, organic matter and chlorophyll as well as pH, alkalinity and conductivity. The links between lake water quality and morphometry become stronger towards large and shallow lakes. Along the decreasing gradients of latitude, altitude and relative depth, the present phosphorus concentration and its deviation from the reference concentration increases.     

Identification of zoonotic Cryptosporidium and Giardia genotypes infecting animals in Sydney's water catchments

To identify the animal sources for Cryptosporidium and Giardia contamination, we genotyped Cryptosporidium and Giardia spp. in wildlife from Sydney’s water catchments using sequence analysis at the 18S rRNA locus for Cryptosporidium and 18S rRNA and glutamate dehydrogenase (gdh) for Giardia. A total of 564 faecal samples from 16 different host species were analysed. Cryptosporidium was identified in 8.5% (48/564) samples from eight host species and Giardia was identified in 13.8% (78/564) from seven host species. Eight species/genotypes of Cryptosporidium were identified. Five G. duodenalis assemblages were detected including the zoonotic assemblages A and B.     

Dissolved load transported by rivers as an indicator of landscape sustainability

Investigation of the Stör River catchment in Germany shows very high annual matter losses (about 1050 kg total mineral salts per ha; excluding NaCl). Loss of base cations (e.g. Ca 263 kg ha⁻¹ year⁻¹), which are essential elements, was an important focus of this research. Compared to the stock of base cations to those minerals added by fertilising, topsoils are being depleted continuously. If this loss is not stopped, a complete breakdown of vegetation growth is expected. Strong impacts on the water cycle and a land management that is spatially and temporally unadapted leads to insufficient energy dissipation in both physical (evapotranspiration, condensation) and biological cyclic processes (photosynthesis, respiration). The resultant increased thermal and chemical potentials cause changes by way of feedback loops on the water cycle and cause matter losses. Some suggestions are presented to manage land sustainably — minimising matter losses with the help of managed wetlands and using much more perennial vegetation biomass.