Studies on British chytrids XXVIII. Rhizophydium nobile sp. nov., parasitic on the resting spore of Ceratium hirundinella O.F.Müll. from the plankton

The life history of a new species of the Chytridiales Rhizophydium nobile is described. It occurs in the autumn on resting spores of the alga Ceratium hirundinella O.F.M. in Blelham Tarn, Windermere and Esthwaite Water, lakes in the English Lake District. The sporangium develops from the zoospore and possesses a branched rhizoidal system. The zoospores are fully formed in the sporangium. On dehiscence part of the sporangium content flows out surrounded by a vesicle which eventually bursts and liberates the zoospores. Only a few resting spores were seen associated with the sporangial stage. They were small spherical thick-walled bodies containing several globules. Further observations need to be made upon this stage.     

Population dynamics of Ceratium spp. in three English lakes, 1945–1985

Changes in the annual population densities of Ceratium spp. in three adjacent English lakes, Windermere, Esthwaite Water and Blelham Tarn, are summarised over the 41 year period 1945–1985. In these lakes the genus is represented by two species, C. hirundinella (O.F. Müll) Bergh. and C. furcoides (Levander) Langhans. Although the species have not been distinguished over the entire study period, they have been shown by examination of preserved samples to undergo marked changes of relative abundance in Esthwaite Water. Both long-term (years) and short-term (within year) changes of populations densities of Ceratium spp. are considered in relation to possible controlling factors including recruitment of the inoculum, nutrient enrichment, physical stability and fungal epidemics. Given an early inoculum, the relative success of Ceratium populations in these lakes decreases along gradients of increasing mixed depths, increasing turbulence and decreasing retention times. The potential for good population growth is regulated by energy inputs, lake bathymetry and hydraulic characteristics. The realisation of such growth is governed by nutrient availability and microbial grazing. The significance of large between-year differences of populations of Ceratium spp. for general lake metabolism is illustrated for summers of contrasting production in Esthwaite Water.     

Modelling the effects on phytoplankton communities of changing mixed depth and background extinction coefficient on three contrasting lakes in the English Lake District

1. The process‐based phytoplankton community model, PROTECH, was used to model the response of algal biomass to a range of mixed layer depths and extinction coefficients for three contrasting lakes: Blelham Tarn (eutrophic), Bassenthwaite Lake (mesotrophic) and Ullswater (oligotrophic). 2. As expected, in most cases biomass and diversity decreased with decreasing light availability caused by increasing the mixed depth and background extinction coefficient. The communities were generally dominated by phytoplankton tolerant of low light. Further, more novel, factors were identified, however. 3. In Blelham Tarn in the second half of the year, biomass and diversity did not generally decline with deeper mixing and the community was dominated by nitrogen‐fixing phytoplankton because that nutrient was limiting to growth. 4. In Bassenthwaite Lake, changing mixed depth influenced the retention time so that, as the mixed depth declined, the flushing rate in the mixed layer increased to the point that only fast‐growing phytoplankton could dominate. 5. In the oligotrophic Ullswater, changing the mixed depth had a greater effect through nutrient supply rather than light availability. This effect was observed when the mixed layer was relatively shallow (<5.5 m) and the driver for this was that the inflowing nutrients were added to a smaller volume of water, thus increasing nutrient concentrations and algal growth. 6. Therefore, whilst changes in mixed depth generally affect the phytoplankton via commonly recognized factors (light availability, sedimentation rate), it also affected phytoplankton growth and community composition through other important factors such as retention time and nutrient supply.     

Interaction of acetogens and methanogens in anaerobic freshwater sediments.

Anaerobic decomposition processes in the profundal sediments of Blelham Tarn (English Lake District) are often limited during late summer by the input of organic carbon. The concentration of acetate in the interstitial water fell from about 100 microM (immediately after sedimentation of the spring diatom bloom) to a relatively constant value of about 20 microM in late summer, during which acetate utilization appeared to be balanced by production. Addition of chloroform and molybdate caused an accumulation of cold acetate in large sediment cores and of [14C]acetate in small cores to which [14C]bicarbonate had been added. In both cases chloroform caused the greater accumulation, implying that acetoclastic methanogens were the more active consumers. The conversion of 14CO2 to [14C]acetate was inversely related, with depth, to its conversion to 14CH4. Methanogenesis from CO2 decreased during late summer, whereas acetogenesis and acetoclastic methanogenesis increased over the same time period. The production of acetate from CO2 was generally equivalent to less than 10% of the acetate carbon utilized but could be as high as 25% of that value. Hydrogen consumption by acetogens could be as high as 50% of that utilized in methanogenesis. The role of acetogenic bacteria in anaerobic processes may therefore be of greater significance in lakes such as Blelham Tarn than in more eutrophic systems.     

The importance of Protozoa in controlling the abundance of planktonic algae in lakes

Apart from ciliates, there are other protozoans which can form an important element in the herbivorous zooplankton of lakes.
The protozoans discussed in this paper feed on colonial algae. They can greatly reduce the numbers of certain Chlorophyta in Windermere, Esthwaite Water and Blelham Tarn, lakes in the English Lake District.
A very short period, often 7–14 days, can suffice for the destruction of more than 99% of an algal population.
Experiments with a species of Pseudospora showed that it would only ingest one out of six green algal species, although, in nature, Pseudosporae which are morphologically similar to this species have been observed in all these algae.
The importance of such protozoans, and of parasitic fungi, has been underrated or neglected in studies of the quantitative relationships between primary and secondary production in the plankton.     

Aulacoseira subarctica: taxonomy,physiology, ecology and palaeoecology

Knowledge of the morphology, taxonomy, physiology, ecology and palaeoecology of the filamentous freshwater diatom Aulacoseira subarctica (O. Müller) Haworth is reviewed from the literature. The species is widely distributed across Northern Europe, Scandinavia and North America, Japan, China, Australia and New Zealand, in the last usually as fo. subborealis. The species is rare in the Tropics and positive identifications are lacking for Africa. The importance of correct identification is stressed because literature reports of its occurrence often need revision. A comparison is made between two sites with detailed records of its seasonal cycle. Blelham Tarn, England, is a clear-water seasonally stratified lake; Lough Neagh, Northern Ireland, is a very large turbid and unstratified lake. In spite of their contrasting characters, Aulacoseira subarctica succeeds in both lakes. In Blelham Tarn, there is a strong seasonal cycle of growth, dormancy on the sediment and further growth on re-suspension. In Lough Neagh, there is a large deposition of cells at the end of the spring bloom but few of these cells survive grazing by benthic animals. Fossil occurrences are summarized from the species’ initial appearance in the Pliocene and its later occurrence during the last inter-glacial (Eemian) deposits in NW Europe, where it is an important ecological indicator. Palaeolimnological studies are reviewed to describe the contemporary distribution and ecological preference of this widespread diatom. Aulacoseira subarctica usually appears in response to moderate increases in nutrients but is disadvantaged by further enrichment. In Blelham Tarn the species only became abundant during the twentieth century, reaching a peak between 1930 and 1960. With nutrient enrichment, abundance has declined. In Lough Neagh, it has been present for much of the post-glacial period and still thrives today in spite of the highly enriched state of the lake. The species has disappeared from many eutrophic lakes and its sustained existence in Lough Neagh is anomalous. Lough Neagh may continue to offer a favourable habitat in spite of the poor light climate because the water depth, lack of stratification and long water retention time reduce losses to a sustainable level.     

Interaction of acetogens and methanogens in anaerobic freshwater sediments

Anaerobic decomposition processes in the profundal sediments of Blelham Tarn (English Lake District) are often limited during late summer by the input of organic carbon. The concentration of acetate in the interstitial water fell from about 100 microM (immediately after sedimentation of the spring diatom bloom) to a relatively constant value of about 20 microM in late summer, during which acetate utilization appeared to be balanced by production. Addition of chloroform and molybdate caused an accumulation of cold acetate in large sediment cores and of [14C]acetate in small cores to which [14C]bicarbonate had been added. In both cases chloroform caused the greater accumulation, implying that acetoclastic methanogens were the more active consumers. The conversion of 14CO2 to [14C]acetate was inversely related, with depth, to its conversion to 14CH4. Methanogenesis from CO2 decreased during late summer, whereas acetogenesis and acetoclastic methanogenesis increased over the same time period. The production of acetate from CO2 was generally equivalent to less than 10% of the acetate carbon utilized but could be as high as 25% of that value. Hydrogen consumption by acetogens could be as high as 50% of that utilized in methanogenesis. The role of acetogenic bacteria in anaerobic processes may therefore be of greater significance in lakes such as Blelham Tarn than in more eutrophic systems.     

Factors influencing the temporal coherence of five lakes in the English Lake District

1. The lakes in the Windermere catchment are all deep, glacial lakes but they differ in size, shape and general productivity. Here, we examine the extent to which year‐to‐year variations in the physical, chemical and biological characteristics of these lakes varied synchronously over a 30–40‐year period. 2. Coherence was estimated by correlating time‐series of the spring, summer, autumn and winter characteristics of five lakes: Esthwaite Water, Blelham Tarn, Grasmere and the North and South Basins of Windermere. Three physical, four chemical and two biological time‐series were analysed and related to year‐to‐year variations in a number of key driving variables. 3. The highest levels of coherence were recorded for the physical and chemical variables where the average coherence was 0.81. The average coherence for the biological variables was 0.11 and there were a number of significant negative relationships. The average coherence between all possible lake pairs was 0.59 and average values ranged from 0.50 to 0.74. A graphical analysis of these results demonstrated that the coherence between individual lake pairs was influenced by the relative size of the basins as well as their trophic status. 4. A series of examples is presented to demonstrate how a small number of driving variables influenced the observed levels of coherence. These range from a simple example where the winter temperature of the lakes was correlated with the climatic index known as the North Atlantic Oscillation, to a more complex example where the summer abundance of zooplankton was correlated with wind‐mixing. 5. The implications of these findings are discussed and a conceptual model developed to illustrate the principal factors influencing temporal coherence in lake systems. The model suggests that our ability to detect temporal coherence depends on the relative magnitude of three factors: (a) the amplitude of the year‐to‐year variations; (b) the spatial heterogeneity of the driving variables and (c) the error terms associated with any particular measurement.     

The distribution of some freshwater planktonic bacteria in two stratified eutrophic lakes

SUMMARY. Changes in bacterial populations and certain physical and chemical variables in Esthwaite Water between June and September 1975 were studied and compared with results obtained from 1972 to 1974 in the hypolimnia of Blelham Tarn and the Lund tubes. The counts of total bacteria ranged between 1 and 7 × 10⁶ml⁻¹ and were highest in the anoxic hypolimnion. The bacterial genera examined in more detail constituted only a small percentage of this count and included Ochrobium (10⁴ml⁻¹), Naumanniella (10³ml⁻¹), Leptothrix (10²ml⁻¹), Planctomyces (10³ml⁻¹), and Metallogenium (10²ml⁻¹). The iron bacteria appear to grow best in the oxycline where there was not only sufficient oxygen for aerobic growth but also a plentiful supply of reduced iron. Planctomyces numbers increased as the thermocline became depressed in September. The results from Blelham Tarn might be interpreted as further evidence of growth by iron bacteria in the absence of dissolved oxygen, but other explanations are possible. Examination of the results by multiple regression analysis showed that it was possible to explain a significant proportion of the bacterial variation (with the notable exception of the Planctomyces counts) in spite of considerable intercorrelation of the regressor variables.     

Growth-rate responses of Volvox aureus Ehrenb. (Chlorophyta,Volvocales) to variability in the physical environment

An analysis of the dynamic responses of a population of Volvox aureus to artificially-imposed alternations in mixing and stratification in a large limnetic enclosure (“Lund Tube” C, Blelham Tarn) is presented. The rates of population increase are shown to be regulated largely through the propagation of daughter colonies that are subsequently released into the medium. The efficiency of propagation is measured in terms of the numbers of developing daughter colonies in parent colonies at any time and the time required for their maturation prior to release. Efficiency of propagation increased when the vegetative population was unmixed and decreased when it was mixed through an optically-deeper water column. Self-regulation of vertical position in the depth profile also influences propagation and, hence, the rate of population increase.     

The annual cycle of growth rate and biomass change in Planktothrix spp. in Blelham Tarn, English Lake District

SUMMARY 1. The changes in the vertical distributions of red coloured Planktothrix rubescens and green P. agardhii filaments in Blelham Tarn, English Lake District, were related to vertical profiles of temperature and light attenuation and to continuous records of the surface irradiance and windspeed, from August 1999 to October 2000. 2. The potential growth rate of each organism was calculated from the irradiance and temperature at 0.5 m depths and hourly intervals throughout the year, using algorithms determined from growth rates in culture. The analyses indicated that there was sufficient irradiance for growth, integrated over the 24‐h cycle, at depths down to the metalimnion where the Planktothrix populations stratified in summer. The compensation depth for growth by P. rubescens reached a maximum of 9.3 m in spring and midsummer, and fell to a minimum of 1.6 m in midwinter; the corresponding values for P. agardhii were 7.9 and 0.5 m. 3. The mixed depth (z_m) exceeded the critical depth for growth (z_b) by P. rubescens (the condition preventing population increase) on only 3 days of the year; for P. agardhii, however, z_m exceeded z_b on 31 days, contributing to its faster decline. The stratified population of P. rubescens was the major cause of light attenuation during the summer of 2000, and resulted in competitive exclusion of P. agardhii. 4. The calculated growth rates integrated over the depth of the water column in Blelham Tarn equalled, or exceeded, the measured changes of the populations during periods when they were increasing, during summer and autumn. Close agreement between the two values was found for much of the year when allowance was made for dilution of the lake population by rainfall over the watershed. During periods of rapid decline, of P. agardhii in September 1999, P. rubescens in December 1999 and both in July–August 2000, additional losses (e.g. by chytrid parasitism and grazing) are invoked.     

Further observations on limnetic zooplankton in a small lake and two enclosures containing fish

SUMMARY. In a small lake (Blelham Tarn, English Lake District) two plastic cylinders, each of which extends from the lake surface to the bottom sediments and encloses 18 000 m³ of water, were used to investigate effects of enclosure on the zooplankton. This paper describes observations from March 1973 to October 1974 and is the second part of a report on a project spanning 4 years.
Seasonal population densities of the more abundant species were essentially similar to those observed in the first part of the project, despite large changes in algal and predator populations. In the enclosures, fish (mostly Perca fluviatilis ) populations are known from observations by divers to have been large in the period under consideration and small in the first part of the project. Populations of Chaoborus larvae in the enclosures were small at all seasons from March 1973 to October 1974.     

The impact of regional-scale changes in the weather on the long-term dynamics of Eudiaptomus and Daphnia in Esthwaite Water, Cumbria

1. Year‐to‐year changes in the weather have a profound effect on the seasonal dynamics of zooplankton in lakes. Here, I analyse some zooplankton data from Esthwaite Water in Cumbria and demonstrate that much of the recorded inter‐annual variation can be related to regional‐scale changes in the weather.
2. The first data set analysed shows the effect of changes in the water temperature on the winter abundance of the calanoid copepod Eudiaptomus gracilis. The highest numbers of Eudiaptomus were recorded when the winters were mild and the lowest when the winters were cold.
3. Winter temperatures in northern and western Europe are now known to be influenced by the atmospheric feature known as the North Atlantic Oscillation (NAO). Positive values of the NAO are associated with mild winters and westerly winds and there was a significant positive correlation between the winter abundance of Eudiaptomus in Esthwaite Water and this empirical index of change.
4. The second data set analysed shows the effect of wind‐induced mixing on the summer abundance of Daphnia. The highest numbers of Daphnia were recorded in years when the early summer thermocline was deep and the lowest number in years when the thermocline was shallow.
5. One of the most important factors influencing the depth of the early summer thermocline in the English lakes is the position of the north‐wall of the Gulf Stream. Southerly movements of the Gulf Stream are typically associated with higher winds, whilst northerly movements are associated with stable conditions. In Esthwaite Water, a significant positive correlation was recorded between the abundance of Daphnia and the depth of the early summer thermocline and significant negative correlations between the same variables and the position of the Gulf Stream.
6. A detailed analysis of the seasonal variations recorded in one calm and one windy year suggest that the main factor responsible for these correlations was the entrainment of nutrients which then stimulated the growth of edible algae. Daphnia numbers were low in 1968 (a ‘north’ Gulf Stream year which was relatively calm) and high in 1972 (a ‘south’ Gulf Stream year with intense wind‐mixing).     

<Emphasis Type="Italic">Diaphanosoma mongolianum</Emphasis> Ueno, 1938 (Cladocera: Sididae) in Lakes of Yaroslavl Oblast (Russia)

Findings of the cladoceran Diaphanosoma mongolianum have been recorded in lakes Pleshcheevo (since 2004) and Nero (since 2007) in Yaroslavl oblast at the northern boundary of its range. Similar species D. brachyurum, previously described in both lakes, is found in insignificant numbers. In 2004–2015, the seasonal abundance, spatial distribution, and diel vertical migration of D. mongolianum were studied in deep mesotrophic Lake Pleshcheevo. The species was found in the plankton from early June until October, with the maximum abundance in July–August. The late appearance of males and gamogenetic females (September) is characteristic of its population. D. mongolianum was the most abundant in the epilimnion of the pelagic zone, where it performed diel vertical migrations, concentrating in the surface layer (0–2 m) at night and at a depth of 2–6 m during the day.     

Contrasting effects of nutrients and climate on algal communities in two lakes in the Windermere catchment since the late 19th century

相似文献   

Some observations on the location of sites of fungal activity at Blelham Tarn

Summary Using a previously described method to enumerate viable propagules of Saprolegniales, an attempt has been made to locate major sites of activity of this group of fungi at Blelham Tarn (English Lake District). There was evidence of high activity in periodically inundated soils at the lake margin, but not in bottom muds from the lake itself.

---

Zusammenfassung Mittels einer früher beschriebenen Methode die vermehrungsfähigen Teile der Saprolegniales festzustellen, wurden die wichtigsten Zonen ihrer Wirkungskreise bei Blelham Tarn (Englisches Seegebiet) gefunden. Es wurde gezeigt, dass sie am meisten im Boden am Seerand, welcher öfters überschwemmt ist, vorkommen, aber nicht im Schlamm des Sees selbst.

     

The distribution of bacteria and fungal spores in Blelham Tarn with particular reference to an experimental overturn

Summary During an experimental overturn at Blelham Tarn, surface water bacteria and fungal spore contents (determined by plating) ranged from 600–6,000 and from 0.3–30 per ml respectively. Following heavy rainfall however, bacterial numbers rose to over 10,000 and fungal spore numbers to over 100 per ml. These high concentrations normally extended down to the thermocline but not below it. The evidence was that particulate matter washed in by rain, and presumably carrying an attached bacterial and fungal flora, was largely lost to the lake through the outflow stream and did not sediment through to the hypolimnion.     

Environmental conditions and phosphorus removal in Florida lakes and wetlands inhabited by Hydrilla verticillata (Royle): implications for invasive species management

Hydrilla verticillata is considered the most problematic aquatic plant in the United States. In south Florida, Hydrilla dominance has also been documented in treatment wetlands. This paper characterizes (1) environmental conditions which favor Hydrilla growth and (2) understand its nutrient removal capability. Despite its occurrence over a wide range of environmental conditions, Hydrilla abundance increased with increasing pH, alkalinity, total P and total N, and decreased with water depth in selected Florida lakes. No relationship was found between color, Secchi depth and Hydrilla abundance. In several Hydrilla-dominated lakes, mean total P concentration (126 μg/l) at inflow was reduced to 106 μg/l at outflow. The maximum inflow total P concentration in a lake with positive nutrient reduction was 148 μg/l. Total P removal efficiency by Hydrilla-dominated lakes and wetlands was comparable to or higher than systems dominated by emergent and other submerged plants. Mean total P settling rates for lakes and a constructed wetland dominated by Hydrilla were estimated at 19 and 34 m/year, respectively, which were higher than or comparable to similar systems dominated by other aquatic plants. Results from this study suggest that reduction of Hydrilla from constructed wetlands will not likely improve nutrient removal performance.     

The biology of the burrowing goby Croilia mossambica Smith (Teleostei,Gobiidae)

Synopsis Croilia mossambica, a burrowing goby endemic to the coastal lakes of south east Africa occurs from L. Poelela (salinity 8%.) to L. Sibaya (freshwater). Since these lakes are isolated from one another its distribution is discontinuous. It is not found in estuaries or the sea. In L. Sibaya C. mossambica is present on sheltered sides from a depth of 1 m to about 16 m. On exposed shores it is not found at less than 3.5 m depth. It is restricted to sandy, quiet water areas and is unable to form burrows where the substrate is disturbed by water movement, is muddy or consists of sand with a particle diameter greater than 0.5 mm. The maximum depth at which it lives is probably determined by light penetration since it is dependent on sight for prey capture. The food consists of slow moving benthic invertebrates such as chironomid larvae, gastropods, bivalves and amphipods. The relative importance of each depends upon its abundance. C. mossambica is a summer breeder with a protracted spawning season. The sticky eggs measure 0.7–0.8 mm when laid. Tolerance experiments show that it is euryhaline and can survive in seawater of 35%. and that its upper temperature limit is between 32 and 35°C. Temperatures in shallow waters of lakes and estuaries of the region frequently exceed 35°C. Thus its local distribution may be limited by temperature. Its lack of tolerance to high temperatures, to marked water movements and its ability to live in seawater indicates that C. mossambica is suited to life in the sea rather than in estuaries. It is suggested that it was present in quiet areas of the sea, such as lagoons, and that it invaded the coastal lakes which were formed as the estuaries and river valleys were inundated during the Pleistocene marine transgression. C. mossambica cannot tolerate estuarine conditions and with the present absence of quiet water in the sea off the south east African coast the species is now confined to deep coastal lakes.Note