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1.
Studies on the occurrence of aquatic hyphomycetes were carried out in Panekal sulfur spring in the Western Ghats, India by incubation of leaf litter and analysis of natural foam and of induced foam. Sampling was done once every three months over a period of two years from September 1989 to June 1991. The temperature, pH, dissolved oxygen, and sulfide content of water were also measured. No fungi were observed within the spring, whereas 16 species belonging to 13 genera were isolated from two outflow sites of the stream. The percent frequency of Triscelophorus monosporus was high (24.0%). The temperature of water in the spring ranged between 30.0 and 38.5°C and the sulfide content between 3.2 and 4.3 mg 1–1. Studies showed that sulfide water (4.0 mg 1–1). from the spring inhibited the growth of the colonies of Dactylella aquatica, Phalangispora constricta, Tetracladium setigerum, Vermispora cauveriana, and Wiesneriomyces laurinus. When the leaves colonized by aquatic hyphomycetes were incubated at different temperatures in sulfur-spring water and stream water separately, sporulation was not observed in any of the fungi at and above 35°C except Phalangispora constricta, which could sporulate at 35°C. At lower temperatures (15–30°C) relatively fewer species were found to sporulate in sulfur-spring water than in stream water. Correspondence to: K.M. Kaveriappa  相似文献   

2.
We examined the effects of hot spring water (35–45 °C) on the ecology of a small, intermittant swamp-stream in Nova Scotia, Canada. Temperatures diminished quickly with distance downstream from the hot spring because of abundant inflow of cold ground water (<10 °C), but elevated temperature effects were detectable 130 m downstream. The brook below the hot spring supported a dense mat of the cyanobacterium Oscillatoria (10 m) followed by the green alga Vaucheria taylorii (40 m). Herbaceous vegetation below the algal zones was also altered by the hot water inflow, even where the temperature increase was slight. The structure of the sparse community of benthic invertebrates was sharply different at sites of different stream temperature: only oligochaete worms, ostracods, chironomids, and a single species of snail thrived at the warmest sites; cold downstream sites supported a typical headwater stream community. Mass loss from decomposing leaves of speckled alder was fast at all sites and strongly correlated with water temperature. The changes in community composition and decomposition rate in response to added heat persisted even where the temperature increase was small, indicating a tight coupling of ecosystem structure and function with the physical environment.  相似文献   

3.
Rajashekhar  M.  Kaveriappa  K.M. 《Hydrobiologia》2000,441(1):149-153
Nine isolates of the aquatic hyphomycetes Dactylella aquatica, Flagellospora penicillioides, Flagellospora saccata, Helicomyces sp., Lunulospora curvula, Phalangispora constricta, Tetracladium setigerum, Vermispora cauveriana and Wiesneriomyces laurinus were incubated at different temperatures (5–35 °C) to study their growth on MEA medium. Maximum growth was observed between 20 and 30 °C. Growth rate was highest in Vermispora cauveriana and lowest in Tetracladium setigerum. Colonies on submerged leaves showed maximum spore production at 25 °C. Light was confirmed as a stimulus to sporulation.  相似文献   

4.
We investigated how fungal decomposer (aquatic hyphomycetes) communities colonizing alder and eucalyptus leaf litter respond to changes in habitat characteristics (transplantation experiment). We examined the breakdown of leaf materials and the associated fungal communities at two contrasting sites, a headwater stream (H) and a midreach (M). Agroforestry increased from headwater to midreach. One month after the start of experiments at both sites, some leaf samples from the midreach site were transplanted to the headwater site (M–H treatment). Although both sites showed similar dissolved inorganic nutrient concentrations, eucalyptus leaves initially incubated at the midreach site (M, M–H) increased their breakdown rate compared to those incubated along the experiment at the headwater site (H). Alder breakdown rate was not enhanced, suggesting that their consumption was not limited by nutrient availability. Sporulation rates clearly differed between leaf types (alder > eucalyptus) and streams (H > M), but no transplantation effect was detected. When comparing conidial assemblages after transplantation, an inoculum effect (persistence of early colonizing species) was clear in both leaf species. Substrate preference and shifts in the relative importance of some fungal species along the process were also observed. Overall, our results support the determining role of the initial conditioning phase on the whole litter breakdown process, highlighting the importance of intrinsic leaf characteristics and those of the incubation habitat.  相似文献   

5.
Ferreira V  Gulis V  Graça MA 《Oecologia》2006,149(4):718-729
We assessed the effect of whole-stream nitrate enrichment on decomposition of three substrates differing in nutrient quality (alder and oak leaves and balsa veneers) and associated fungi and invertebrates. During the 3-month nitrate enrichment of a headwater stream in central Portugal, litter was incubated in the reference site (mean NO3-N 82 μg l−1) and four enriched sites along the nitrate gradient (214–983 μg NO3-N l−1). A similar decomposition experiment was also carried out in the same sites at ambient nutrient conditions the following year (33–104 μg NO3-N l−1). Decomposition rates and sporulation of aquatic hyphomycetes associated with litter were determined in both experiments, whereas N and P content of litter, associated fungal biomass and invertebrates were followed only during the nitrate addition experiment. Nitrate enrichment stimulated decomposition of oak leaves and balsa veneers, fungal biomass accrual on alder leaves and balsa veneers and sporulation of aquatic hyphomycetes on all substrates. Nitrate concentration in stream water showed a strong asymptotic relationship (Michaelis–Menten-type saturation model) with temperature-adjusted decomposition rates and percentage initial litter mass converted into aquatic hyphomycete conidia for all substrates. Fungal communities did not differ significantly among sites but some species showed substrate preferences. Nevertheless, certain species were sensitive to nitrogen concentration in water by increasing or decreasing their sporulation rate accordingly. N and P content of litter and abundances or richness of litter-associated invertebrates were not affected by nitrate addition. It appears that microbial nitrogen demands can be met at relatively low levels of dissolved nitrate, suggesting that even minor increases in nitrogen in streams due to, e.g., anthropogenic eutrophication may lead to significant shifts in microbial dynamics and ecosystem functioning. Electronic Supplementary Material Supplementary material is available to authorised users in the online version of this article at .  相似文献   

6.
The contribution of fungi and bacteria to the decomposition of alder leaves was examined at two reference and two polluted sites in the Ave River (northwestern Portugal). Leaf mass loss, microbial production from incorporation rates of radiolabeled compounds into biomolecules, fungal biomass from ergosterol concentration, sporulation rates, and diversity of aquatic hyphomycetes associated with decomposing leaves were determined. The concentrations of organic nutrients and of inorganic nitrogen and phosphorus in the stream water was elevated and increased at downstream sites. Leaf decomposition rates were high (0.013 day−1 < k < 0.042 day−1), and the highest value was estimated at the most downstream polluted site, where maximum values of microbial production and fungal biomass and sporulation were found. The slowest decomposition occurred at the other polluted site, where, along with the nutrient enrichment, the lowest current velocity and dissolved-oxygen concentration in water were observed. At this site, fungal production, biomass, and sporulation were depressed, suggesting that stimulation of fungal activity by increased nutrient concentrations might be offset by other factors. Although bacterial production was higher at polluted sites, fungi accounted for more than 94% of the total microbial net production. Fungal yield coefficients varied from 10.2 to 13.6%, while those of bacteria were less than 1%. The contribution of fungi to overall leaf carbon loss (29.0 to 38.8%) greatly exceeded that of bacteria (4.2 to 13.9%).  相似文献   

7.
Chironomid pupal exuviae were collected over an eight-week period from a delta-swamp which receives thermal effluent from a nuclear reactor on the Savannah River Plant, South Carolina, USA. Two sites were sampled using box-type emergence traps. Site 1 was directly in a major thermal plume channel, and site 2 was outside the plume in a stand of stressed bald cypress trees. Sixteen chironomid taxa were collected, of these, species of Chironomus (42%) and Tanytarsus (35%) dominated the warmer site (site 1, maximum temperature 46 °C), whereas Tanypus neopunctipennis comprised > 84 % at site 2 (maximum temperature 43 °C). Emergence substantially increased at both sites after the reactor was shut down and water temperatures returned to ambient (27–28 °C). Tanytarsus sp. 1 and T. neopunctipennis were capable of successfully emerging during water temperature periods of 40–46 °C. The deep organic sediment, characteristic of the delta-swamp apparently served as a refugium for these and other species of midges during high temperature periods. It is suggested that the ability of some taxa to tolerate these elevated temperatures may be a combination of several factors: behavioral and ecological adaptations to utilize available refugia; and physiological adaptations to withstand higher temperatures and low dissolved oxygen concentrations.  相似文献   

8.
Summary Transects were cut from alder leaves incubated in a freshwater stream and plated as quadrats so that fungal isolates could be mapped by reconstruction of each transect. Initially there was fewer than one aquatic hyphomycete colonist per quadrat, but the mode increased to 6–7 then progressively decreased to <1. Numbers of species of aquatic hyphomycetes per quadrat rose and fell similarly with a maximum mode of 3–4, as did species per transect with a maximum of 11 and a diversity of 16, comprising 6 dominant species and about 10 occasional species. The latter showed no pattern of appearance but the dominant group was established early and persisted in a dynamic equilibrium. Aquatic hyphomycetes were initially randomly distributed but developed progressively into clumped consortia which persisted after peak colonization, declining as leaf degradation became total. Colonies of the most persistent aquatic hyphomycete species were initially discrete,developing into a complex network of overlapping colonies and species, no two of which showed positive association. These complexes broke down to large colonies of a few species and finally to 1–2 small colonies. The pattern of isolates of the 18 genera of other fungi was the reverse of that for aquatic hyphomycetes. Only Cladosporium, Epicoccum and Fusarium were important colonizers. The first two appear to be inhibited by aquatic hyphomycetes, but were found to degrade substrates representative of cell-wall polymers vigorously whereas aquatic hyphomycetes showed varied degradative ability. Leaf transects were examined by S.E.M. and epifluorescent microscopy so that hyphal colonization could be followed at progressive stages of leaf degradation. Bacteria on transects were patchily distributed, the temporal pattern indicating inhibition by aquatic hyphomycetes and colonization of senescent hyphae.  相似文献   

9.
Summary The daily movements of two co-occurring tiger beetle species were monitored in conjunction with changes in microclimate along streams in Northeast Arizona. Cicindela oregona and C. tranquebarica temporarily segregated across areas of beach exhibiting different microclimates. C. oregona progressively moved from the dry upper beach to the wet stream edge as beach temperatures increased and humidity decreased. The actively foraged throughout the day in this moist habitat at air temperatures between 25 and 38°C. C. tranquebarica remained on the dry, upper portions of the beach and shuttled between sun and shade at air temperatures above 35°C. Only when stream edge temperatures exceeded 30°C was tranquebarica found in this subhabitat. Both species exhibited physiological tolerances in the laboratory that were consistent with their microhabitat preferences in the field. Although both species had similar high lethal temperatures (47–48°C) in saturated air, oregona died at lower temperatures (39–43°C) than tranquebarica (46–47°C) under dry (0% RH) conditions. C. oregona was considerably more active than tranquebarica at body temperatures below 30°C and exhibited higher levels of active metabolism between 25 and 40°C. In addition, C. tranquebarica exhibited significantly lower water loss rates than oregona at 30, 35 and 40°C.  相似文献   

10.
Nitrate depletion in the riparian zone of a small woodland stream   总被引:1,自引:0,他引:1  
Field enrichments with nitrate in two spring-fed drainage lines within the riparian zone of a small woodland stream near Toronto, Ontario showed an absence of nitrate depletion. Laboratory experiments with riparian substrates overlain with nitrate enriched solutions revealed a loss of only 5–8% of the nitrate during 48 h incubation at 12°C. However, 22–24% of the initial nitrate was depleted between 24 and 48 h when a second set of substrate cores was incubated at 20°C. Short-term (3 h) incubations of fresh substrates amended with acetylene were used to estimate in situ denitrification potentials which varied from 0.05–3.19 g N g–1 d–1 for organic and sandy sediments. Denitrification potentials were highly correlated with initial nitrate content of substrate samples implying that low nitrate levels in ground water and riparian substrates may be an important factor in controlling denitrification rates. The efficiency of nitrate removal in spring-fed drainage lines is also limited by short water residence times of < 1 h within the riparian zone. These data suggest that routes of ground water movement and substrate characteristics are important in determining nitrate depletion within stream riparian areas.  相似文献   

11.
The effects of temperature on rates of mineralization of [14C]lignocellulose were investigated in water and sediment from a thermally impacted stream and from a nearby unimpacted swamp at the Savannah River Plant, South Carolina. The temperature optimum for lignocellulose mineralization remained near 35°C at the unimpacted site throughout the sampling period from November 1986 to May 1987. The temperature optimum for lignocellulose mineralization in the thermally impacted stream was near 45°C when thermal effluents from a nuclear reactor were released to the stream, and was near 35°C when the reactor was not operating. Microbial populations capable of rapidly degrading lignocellulose at higher temperatures (45–55°C) developed between 9 and 27 days under conditions of thermal stress, indicating that under favorable conditions thermophilic microorganisms became dominant components of the microbiota. Removal of thermal stress for periods of 75 days or less resulted in a collapse of the thermophilic degrading population.  相似文献   

12.
Population dynamics and production of C. luctuosa were compared in two reaches of the Agüera stream (northern Spain). This species showed univoltine winter life history in both sites. However, the start of the recruitment period, and the cohort production interval differed in 1 month between reaches. Secondary production of C. luctuosa ranged from 76 mg m–2 year–1 (upper site) to 93 mg m–2 year–1 (lower site). Although annual production seemed to be mainly influenced by the biomass found at each site, changes in life history may have also been important. The need to have accurate information about life history of the analysed species at the study sites when assessing secondary production is highlighted.  相似文献   

13.
The annual temperature regime of a small stream in New Zealand   总被引:2,自引:1,他引:1  
C. L. Hopkins 《Hydrobiologia》1971,37(3-4):397-408
Summary An electrically operated strip-chart recorder was installed in the Hinau Stream, a small hill stream in the North Island of New Zealand. With this instrument the temperatures of the stream, air, and a small spring were monitored for 2 years. Mercury-in-glass maximum/minimum thermometers were installed at two other points in the stream system, one 500 m below the site sampled by the recorder probes and the other in another stream which joined the first.The annual temperature in the stream at the site of the continuous recorder ranged from 6°C to 18.5°C. Annual range in the spring water was much less, 10–14°C. The greatest daily range in temperature in both air and water was found during summer and the smallest in winter. Data taken 500 m down stream of the continuously recorded site showed that summer maxima were 3–4° higher than in the upper reaches, though the minima were about the same at the two sites. During winter there was little difference between the two sites. Data from certain other waters with wider annual temperature ranges showed summer maxima to be higher than in the Hinau, but winter minima to be about the same.Maximum temperature in the Hutt River where it flowed through thickly forested country was much less than in the same river in cleared land down stream and also much less than in two other rivers in open country for which data exist.Comparison of quantitative samples of benthic invertebrates taken from different parts of the Hinau Stream showed that several species of Trichoptera were more abundant in the recorder-monitored headwater than elsewhere in the stream. This may have been partly due to the less extreme temperature conditions in the headwater.
Résumé Un enregistreur électrique sur bande de papier a été installé dans Hinau Stream, un petit ruisseau qui coule dans des collines dans l'Ile du Nord de la Nouvelle Zélande. Les températures du ruisseau, de l'air, et d'une petite source furent enregistrées par cet appareil pendant une période couvrant deux années. Des thermomèters maximum/minimum à mercure furent placés en deux autres points du système hydrologique du ruisseau, l'un à 500 m en aval du site où opérait la sonde de l'enregistreur et l'autre dans un autre ruisseau qui rejoignait le premier.La température annuelle dans le ruisseau à l'emplacement de l'enregistreur permanent variait entre 6°C et 18.5°C. Les variations annuelles de l'eau de la source étaient biens moindres, 10–14°C. La plus importante variation journalière de température de l'air et de l'eau se produisait pendant l'été et la plus faible pendant l'hiver. Des mesures faites 500 m en aval du site où l'enregistrement était permanent montrèrent que les maxima pendant l'été étaient de 3 à 4° plus grands que dans l'amont, bien que les minima soient approximativement les mêmes dans les deux sites. Pendant l'hiver il y avait peu de différence entre les deux sites. Des mesures faites dans certains autres cours d'eau avec des plages de variation de températures annuelles beaucoup plus larges montrèrent que leurs maxima de l'été étaient plus grands que dans l'Hinau mais que leurs minima pendant l'hiver étaient à peu près les mêmes. La température maximum dans la Hutt River quand elle coulait à travers une région couverte de forêts épaisses était bien moindre que lorsque cette même rivière passait dans une région déboisée en aval, et elle était aussi bien moindre que dans deux autres cours d'eau coulant en pays non boisé pour lesquels il existe des mesures.Des comparaisons entre des échantillons quantitatifs d'invertébrés benthiques pris dans différentes parties d'Hinau Stream montrèrent que plusieurs espèces de Trichoptera étaient plus abondantes dans le cours supérieur du ruisseau où se trouvait l'enregistreur qu'autre part dans le ruisseau. Ceci est peut-être dû à des conditions de températures moins extrêmes dans la partie supérieure du ruisseau.
  相似文献   

14.
Jost Borcherding 《Oecologia》1991,87(2):208-218
Summary The annual development of the gonads of Dreissena polymorpha was studied at three sampling sites in two lakes over 3 and 1 1/2 years, respectively. A resting stage occurred after the last spawning in summer/autumn. Oogenesis (accompanied by multiplying segmentation of the oogonia and early growth processes of its oocytes) restarted in specimens at least 1 year old at low temperatures (below 10° C) during winter and early spring. At one location (Fühlinger See) the onset of the spawning season was correlated with an increase of water temperatures above 12° C. At 2 m depth, two main spawning periods in May and August were normally recognized, the first at temperatures of 12–16° C, the second at 16–21° C. It was clearly demonstrated for the first time in Dreissena polymorpha that the oocytes became mature in successive cohorts within one gonad. A female mussel may spawn several times during the reproductive season. At 9 m depth, the onset of spawning also started at about 12° C; this occurred in late summer, with two spawning periods within 1 month at a temperature range of 12–16° C. At another location (Heider Bergsee) the size of the gonads and the oocytes was reduced during April of both years studied, when food supply was low simultaneously with rapidly rising water temperatures in this shallow lake. There was no spawning period during spring. The major spawning period was delayed until July (temperatures 19–22°C). This shows (1) the synchronizing influence of low winter temperatures on the annual reproductive cycle and (2) a temperature threshold of at least 12° C for the start of the spawning processes. The results are discussed with regard to the geographical limits of further spread of Dreissena polymorpha.  相似文献   

15.
Seasonal variation of methane emissions from a temperate swamp   总被引:6,自引:4,他引:2  
Methane flux measurements were made at four sites in a freshwater temperate swamp over the 13 month period of April 1985 through May 1986. Emissions were highly variable both between sites and over time at any one site. Ebullition from sediments was an important component of methane release. Although release of methane through bubbling occurred in only 19% of the measurements made between April and June 1985, when instrumentation allowed us to separate diffusive and bubble fluxes, ebullition accounted for 34% of the total flux during this period. Methane release rates showed a strong seasonal variation, with highest emission rates observed in early spring and again in late summer, which was associated with changes in plant growth and physiology. Emission rates were partially correlated with sediment temperature, but the relationship was not straightforward, and resembled a step function. Emissions responded strongly to temperature change through the range of 10–16°C. At winter sediment temperatures between 4–9°C, CH4 flux continued at low rates (0–28 mg CH4 m–2d–1; average = 7.9 mg CH4m–2d–1) and appeared insensitive to changes in sediment temperature. Annual methane emission from three constantly flooded sites (mean water depth = 35 cm) was 43.7 +/- 7.8 gm–2 (standard error); annual flux from a bank site was 41.4 +/- 20.5 gm–2. A comparison of flux measurements from fresh and saline wetlands in the immediate area of Newport News Swamp emphasizes the importance of edaphic factors in controlling flux.  相似文献   

16.
Linda May 《Hydrobiologia》1987,147(1):335-338
Sediment samples from Loch Leven, Scotland, were incubated at 5°C, 10°C and 15°C to induce hatching of rotifer resting eggs. The emergent animals were identified and counted. The temperature which induced hatching varied among the nine species studied. These results are discussed in relation to seasonality and temperature preferences previously recorded for the most abundant species. Resting egg densities of 2.2–13.9 eggs cm–3 were recorded in the upper 5 cm of sediment.  相似文献   

17.
Chapman  B. R.  Ferry  B. W.  Ford  T. W. 《Hydrobiologia》1997,353(1-3):161-170
The species richness and the dynamics of the ciliatecommunitieswere studied at three stations along a streamlet formed bywaterdischarged from a geothermal sulphur spring. Altogether, 73specieswere identified. Ciliate coenoses were composed primarily offreshwater forms, but they were numerically dominated byeuryhalinespecies. The great fluctuation in both number of species andindividuals observed along the streamlet were due to vigorouschemical changes in the physico-chemical characteristics ofthewater. These changes were caused mainly by the sulphide andsaltgradient observed along the water course. The maximum value ofsulphide was observed in August with 391 µM l–1, andthehighest conductivity value was observed in April with 18 mScm–1. The most characteristic and abundant species weresmall-sized bacterivorous scuticociliates which have a rapidecological adaptability and whose tolerance limits toenvironmentalchanges are wide. Bacterivorous scuticociliates such as Cyclidium citrullus, C. glaucoma, Cinetochilummargaritaceum, and Uronema nigricans were numericallydominant when the thermal water contained the highestconcentrationof sulphide. The diversity index values changed sharply intimeboth inside and among sampling stations, indicating unstablecommunities which depended on highly fluctuatingconditions.  相似文献   

18.
Structural, functional, and biochemical characteristics of the photosynthetic apparatus of a nemoral herbaceous perennial plant Ajuga reptansL. inhabiting the middle taiga subzone were investigated. Plant leaves were characterized by a high content of green (3.1 mg/dm2) and yellow (0.64 mg/dm2) pigments and contained moderate-sized chloroplasts with grana consisting of ten thylakoids or more. The maximum rate of photosynthesis in summergreen leaves (5–8 mg CO2/(dm2h)) was observed at 14–16°C under a saturating photosynthetically active radiation of 50 W/m2. At 6–7°C, the rate of CO2assimilation was reduced to 60–80% of the maximum one. The temperature optimum of photosynthesis was not constant and shifted by 2–6°C depending on the changes in the ambient temperature. Wintergreen leaves were capable of photosynthesis in late autumn after heavy freezes and in early spring after a long winter. The accumulation of soluble carbohydrates and free amino acids in leaves helps to maintain the functional activity of the photosynthetic apparatus.  相似文献   

19.
Göran Bengtsson 《Oecologia》1992,89(4):542-549
Summary Immigration and colonization of isolates of naturally occurring stream bacteria and hyphomycetes on beech leaves were studied in a laboratory stream microcosm. Fungal spores were more successful immigrants, especially on new leaves, than bacteria, which were more repelled than attracted by the substrate. Fewer bacteria immigrated to older leaves than to new, and bacteria multiplied faster in water than on leaves. Fungi and bacteria showed synergistic relationships so that each group grew significantly faster in presence of the other group. If one considers, differences in immigration, colonization and synergism patterns, fungal mycelia doubled about 10 times faster than bacterial cells which might explain the dominance of fungi usually found on leaves in early decay. The individual fungal species could be assigned to one of three colonization groups; one of fugitive species, preceding a second group of species that grew from rarity to dominance, and a third group of very slow colonizers. The leachate was fractionated in different molecular size classes by gel chromatography, and the fraction around 2500D in the new leaf leachate was associated with a high concentration of polyphenols. High-pressure liquid chromatography (HPLC) and gas chromatography-mass spectrometry (GC-MS) revealed the presence of 16 phenolic acids in the new leaf leachate at concentrations ranging from < 1 to 640 g l–1. All fungi except the species with the slowest growth rate grew faster on leachate with the fraction around 2500D removed, and the density of bacteria was significantly reduced when pure stream water was supplemented with compounds from the same fraction.  相似文献   

20.
Synopsis Two groups of coho salmon,Oncorhynchus kisutch, were raised under identical regimes to test the hypothesis that the group from a stream with lower and less variable temperatures would have a lower and less variable preferred temperature than would the group from a stream with warmer and more variable temperatures. The preferred (modal) temperatures in an electronic shuttlebox of coho salmon young from a relatively cool, groundwater-fed stream were slightly lower and less variable than those of young from a warmer and more heterothermal stream (mean = 9.6° C, range: 6–16° C vs. mean = 11.6° C, range: 7–21° C). However, there was a great deal of variation within and among individual fish. While some genetic variation in thermal preference may exist, the species seems best characterized as tolerant of relatively large temperature fluctuations.  相似文献   

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