A limnological investigation of the tarn Syslaktjønn, W Norway

An investigation covering hydrography, chemistry, vascular and cryptogamic plants, nitrogen fixation, phytoplankton biomass and production, and zooplankton was carried out from April to November 1976 in tarn in W Norway, The volume of the tarn was 18000 m³ and the turnover time about 30 d. Temperature ranged between 3.6 and 23.4°C and pH between 4.8 and 5.5. Nuphar luteum and Carex rostrata were the two dominating vasculars-with biomasses of 117 and 97 g m⁻², respectively The biomass of the bryophytes ( Sphagnum spp.) was about 510 g m⁻² and the production of the order 0.2–2.1 μg (mg d.w.)⁻¹h⁻¹. Nitrogen fixation in association with Sphagnum spp. was estimated at 25 g yr⁻¹ for the whole tarn. Phytoplankton was dominated by diatoms, green algae and chrysophyceans. The chlorophyll a content ranged from 2 to 20 mg m⁻³ and the carbon assimilation rates from 0.03 to 20 mg C m⁻³h⁻¹ at 0–4 m depths. Production in the period was of the magnitude 22 g C m⁻². The copepod Eudiaptomus gracilis was the most common netzooplankter. Large numbers of rotationrians were found during summer.     

Photosynthetic capacity in relation to nitrogen content and its partitioning in lichens with different photobionts

We tested the hypothesis that lichen species with a photosynthetic CO₂-concentrating mechanism (CCM) use nitrogen more efficiently in photosynthesis than species without this mechanism. Total ribulose bisphosphate carboxylase-oxygenase (Rubisco; EC 4.1.1.39) and chitin (the nitrogenous component of fungal cell walls), were quantified and related to photosynthetic capacity in eight lichens. The species represented three modes of CO₂ acquisition and two modes of nitrogen acquisition, and included one cyanobacterial ( Nostoc ) lichen with a CCM and N₂ fixation, four green algal ( Trebouxia ) lichens with a CCM but without N₂ fixation and three lichens with green algal primary photobionts ( Coccomyxa or Dictyochloropsis ) lacking a CCM. The latter have N₂-fixing Nostoc in cephalodia. When related to thallus dry weight, total thallus nitrogen varied 20-fold, chitin 40-fold, Chl a 5-fold and Rubisco 4-fold among the species. Total nitrogen was lowest in three of the four Trebouxia lichens and highest in the bipartite cyanobacterial lichen. Lichens with the lowest nitrogen invested a larger proportion of this into photosynthetic components, while the species with high nitrogen made relatively more chitin. As a result, the potential photosynthetic nitrogen use efficiency was negatively correlated to total thallus nitrogen for this range of species. The cyanobacterial lichen had a higher photosynthetic capacity in relation to both Chl a and Rubisco compared with the green algal lichens. For the range of green algal lichens both Chl a and Rubisco contents were linearly related to photosynthetic capacity, so the data did not support the hypothesis of an enhanced photosynthetic nitrogen use efficiency in green-algal lichens with a CCM.     

Changes in forest soils and vegetation in Søgne, southern Norway, during a 20 year period

An investigation of the edaphic conditions and the vegetation of 21 fixed plots in Søgne municipality, Vest-Agder, South Norway was carried out in 1967-69 and 1987. Loss on ignition, pH, total nitrogen, total exchangeable bases, base saturation, exchangeable hydrogen, sodium, potassium, magnesium, calcium and manganese was analysed. The species composition of vascular plants was investigated. The total cover of the bottom layer was scored.
The soil pH had decreased in the more basic soils but had increased in the more acidic soils. The organic content had increased and base saturation had decreased in most samples. Na⁺ had increased in more than half of the plots, Ca²⁺ and Mg²⁺ had not changed, and K⁺ and Mn²⁺ had decreased in most plots. Salt depositions from the neighbouring North Sea and leaching from the soil accounted for these changes. In many of the parameters opposite changes were found in the poorer soils compared to the richer soils. In the field layer Deschampsia flexuosa, Convallaria majalis had increased, and Oxalis acetocella, Galium odoratum had decreased. The cover of cryptogams had decreased in most of the plots.     

Denitrification and nitrate-reducing bacterial populations in abandoned and reclaimed minesoils

Abstract Microbial populations, nitrogen mineralization potentials, and denitrification enzyme activities were examined in two abandoned carbolithic minesoils. Numbers and activities of bacteria and fungi were lower in nonamended than in lime and/or fly ash amended sites. Rates of aerobic NO₃⁻ production (3 to 38 μg-N kg⁻¹ h⁻¹) and anaerobic NO₃⁻ reduction to N₂O (5 to 68 μg-N kg⁻¹ h⁻¹) were measured. Organisms capable of N₂O production under anaerobic soil conditions were present in low numbers, and their activity was restricted in part by low soil pH. Nondenitrifying nitrate-reducing bacteria were more diverse and in greater numbers than respiratory denitrifiers and may have been responsible for N₂O production in assays measuring denitrification enzyme activity.     

Near-zero recent carbon accumulation in a bog with high nitrogen deposition in SW Sweden

We present data on the accumulation of carbon and nitrogen into an open oceanic ombrotrophic bog, SW Sweden, with high levels of anthropogenic nitrogen deposition. The aim was to investigate if this peatland currently acts as a sink for atmospheric carbon. Peat cores were sampled from the top peat layer in five different vegetation types. Small pines were used to date the cores. The cores bulk density and carbon and nitrogen content were determined. A vegetation-classified satellite image was used to estimate the areal extent of the vegetation types and to scale up these results to bog level. The rate of current carbon input into the upper oxic acrotelm was 290 g m⁻² yr⁻¹, and there were no significant differences in accumulation rates among the vegetation types. This organic matter input to the acrotelm was almost completely decomposed before it was deposited for storage in the deeper peat layers (the catotelm) and only a small fraction (≪1%) or 0.012 g m⁻² yr⁻¹ of the carbon would be left, assuming a residence time of 100 years in the acrotelm. Nitrogen accumulation rates differed between the vegetation classes, and the average input via primary production varied from 5.33 to 16.8 g m⁻² yr⁻¹. Current nitrogen input rates into the catotelm are much lower, 0–0.059 g m⁻² yr⁻¹, with the highest accumulation rates in lawn-dominated communities. We suggest that one of the main causes of the low carbon input rates is the high level of nitrogen deposition, which enhances decomposition and changes the vegetation from peat-forming Sphagnum -dominance to dominance by dwarf shrubs and graminoids.     

Phytoplankton ecology in an Antarctic lake

SUMMARY. The ecology of the phytoplankton of Heywood Lake, Signy Island, South Orkney Islands, Antarctica was investigated during 1969–72. The lake, which is ice-covered for 8–10 months per year, is moderately eutrophic due to enrichment by seal excreta.
The annual cycle of the phytoplankton is described. During the winter (approximately May-September), very few algal cells could be detected in the water column and ¹⁴C fixation was below measurable limits. In spring (October-November), a rapidly-growing population of algae caused a large increase in the chlorophyll- a concentration (maximum value 170 mg m⁻²) but carbon fixation remained low, with values <500 mg C m⁻² day⁻¹. The algae contributing to this peak were mainly small chlorophytes and chrysophytes. The summer open-water period (December-March) was characterized by a different phytoplankton population dominated by cryptophytes. Chlorophyll levels were lower ( c . 40 mg m⁻²) but ¹⁴C fixation rates >3 g C m⁻² day⁻¹ were measured on bright days. Values for Assimilation Number were very high (maximum value 10.5 mg C h⁻¹ mg⁻¹ (chlorophyll- a ) in January (1971) though temperatures never exceeded 8°C. In autumn, the phytoplankton regressed to winter levels. Both spring and summer algal populations probably overwinter as resting stages.     

The Placopsis trachyderma – Raoulia – community, a special type of biological soil crusts in the braided rivers of southern New Zealand

The braided rivers with their ever-changing water channels are recognized as one of New Zealand's most distinctive and important ecosystem. We made a survey of the vegetation on the shingle plains in the upper reaches of the braided rivers of South Island. A well-defined colonizing vegetation type was recognized. It consists of lichens, mosses, low herbs, low cushion plants and tufted grasses, and mat-forming plants. Because of the close mechanical connection between the thalli of the lichens of the genus Placopsis (Agyraceae: Ascomycota) with moss cushions and spreading mats of vascular plants, we see this Placopsis trachyderma – Raoulia – community as a special type of biological soil crusts.     

Methanogenesis and methanotrophy within a Sphagnum peatland

Abstract: Methane production and consumption activities were examined in a Massachusetts peatland. Peat from depths of 5–35 cm incubated under anaerobic conditions, produced an average of 2 nmol CH₄ g⁻¹ h⁻¹ with highest rates for peat fractions between 25–30 cm depth. Extracted microbial nucleic acids showed the strongest relative hybridization with a 16S rRNA oligonucleotide probe specific for Archaea with samples from the 25–30 cm depth. In aerobic laboratory incubations, the peat consumed methane with a maximum velocity of 67 nmol CH₄ g⁻¹ h⁻¹ and a K _s of 1.6 μM. Methane consumption activity was concentrated 4–9 cm below the peat surface, which corresponds to the aerobic, partially decomposed region in this peatland. Phospholipid fatty acid analysis of peat fractions demonstrated an abundance of methanotrophic bacteria within the region of methane consumption activity. Increases in temperature up to 30°C produced an increase in methane consumption rates for shallow samples, but not for samples taken from depths greater than 9 cm. Nitrogen fixation experiments were carried out using ¹⁵N₂ uptake in order to avoid problems associated with inhibition of methanotrophy. These experiments demonstrated that methane in peat samples did not stimulate nitrogen fixation activity, nor could activity be correlated with the presence of methanotrophic bacteria in peat fractions.     

The effect of nitrogen and phosphorus on starch accumulation and net photosynthesis in two variants of Panicum maximum Jacq.

Abstract. Two anatomical variants of Panicum maximum Jacq. were observed to accumulate an unusually large number of starch grains in the bundle sheath chloroplasts when grown under controlled environmental conditions in a nutrient medium containing a low level of nitrate nitrogen (20 mg N dm⁻³ as KNO₃). When these plants were placed under dark conditions the chloroplasts were destarched, but exhibited a marked distortion of the thylakoid membranes. Under a higher level of nitrate nitrogen supply (200 mg N dm⁻³ as KNO₃) the number of starch grains was markedly reduced compared to that observed above in both plant variants. When the nitrogen was supplied as ammonium nitrogen (200 mg N dm⁻³ as NH₄Cl) there was again a high level of starch in the bundle sheath chloroplasts, the level being only slightly lower than that observed at the low KNO₃ supply. An unusually large number of starch grains accumulated in the bundle sheath chloroplasts in the absence of added phosphorus in the nutrient medium, in the presence of the higher nitrate nitrogen level. It is suggested that the increased starch accumulation results from a reduced trans-location of Calvin cycle intermediates out of the chloroplasts into the cytoplasm and that both nitrate nitrogen and phosphorus may play an important role in this process. A good correlation between high net photosynthetic activity and low bundle sheath starch content was observed. Nutrient medium requirements favouring low starch content in chloroplasts also favoured high net photosynthetic rates.     

模拟氮沉降对华西雨屏区天然常绿阔叶林土壤微生物生物量碳和氮的影响

为理解模拟氮沉降对华西雨屏区天然常绿阔叶林土壤微生物生物量碳(MBC)和氮(MBN)的影响,通过一年野外模拟氮(NH₄NO₃)沉降试验,氮沉降水平分别为对照(CK, 0 g N·m^-2·a^-1)、低氮沉降(L, 5 g N·m^-2·a^-1)、中氮沉降(M, 15 g N·m^-2·a^-1)和高氮沉降(H, 30 g N·m^-2·a^-1),研究了氮沉降对天然常绿阔叶林土壤MBC和MBN的影响.结果表明: 氮沉降显著降低了0～10 cm土层MBC和MBN,且随氮沉降量的增加,下降幅度增大;L和M处理对10～20 cm土层MBC和MBN无显著影响,H处理显著降低了10～20 cm土层土壤MBC和MBN;氮沉降对MBC和MBN的影响随土壤深度的增加而减弱.MBC和MBN具有明显的季节变化,在0～10和10～20 cm土层均表现为秋季最高,夏季最低.0～10和10～20 cm土层土壤微生物生物量C/N分别介于10.58～11.19和9.62～12.20,表明在华西雨屏区天然常绿阔叶林土壤微生物群落中真菌占据优势.     

Effects of soil frost on nitrogen net mineralization, soil solution chemistry and seepage losses in a temperate forest soil

Freezing and thawing may alter element turnover and solute fluxes in soils by changing physical and biological soil properties. We simulated soil frost in replicated snow removal plots in a mountainous Norway spruce stand in the Fichtelgebirge area, Germany, and investigated N net mineralization, solute concentrations and fluxes of dissolved organic carbon (DOC) and of mineral ions (NH₄⁺, NO₃⁻, Na⁺, K⁺, Ca²⁺, Mg²⁺). At the snow removal plots the minimum soil temperature was −5 °C at 5 cm depth, while the control plots were covered by snow and experienced no soil frost. The soil frost lasted for about 3 months and penetrated the soil to about 15 cm depth. In the 3 months after thawing, the in situ N net mineralization in the forest floor and upper mineral soil was not affected by soil frost. In late summer, NO₃⁻ concentrations increased in forest floor percolates and soil solutions at 20 cm soil depth in the snow removal plots relative to the control. The increase lasted for about 2–4 months at a time of low seepage water fluxes. Soil frost did not affect DOC concentrations and radiocarbon signatures of DOC. No specific frost effect was observed for K⁺, Ca²⁺ and Mg²⁺ in soil solutions, however, the Na⁺ concentrations in the upper mineral soil increased. In the 12 months following snowmelt, the solute fluxes of N, DOC, and mineral ions were not influenced by the previous soil frost at any depth. Our experiment did not support the hypothesis that moderate soil frost triggers solute losses of N, DOC, and mineral ions from temperate forest soils.     

Growth of reindeer lichens and effects of reindeer grazing on ground cover vegetation in a Scots pine forest and a subarctic heathland in Finnish Lapland

Reindeer lichens are an important component of northern ecosystems. The aim of this study was to measure the growth rate of terricolous lichens as it is a key parameter involved in productivity of these ecosystems and an important part of lichen tolerance to reindeer grazing. Furthermore, the natural succession and the long-term effects of reindeer grazing on lichen community characteristics in two contrasting habitats were investigated as well as the interactions between lichen cover and mosses and vascular plants. Biomass and coverage measurements were conducted in a lichen woodland and in a subarctic heath with grazed and ungrazed areas in northern Finland. Measurements spanning over 13 yr of undisturbed development show that the growth rate of Cladina stellaris can be as high as >0.17 g g⁻¹ produced annually, although in average growth rates were much lower. During the succession of ground vegetation, C. stellaris , C. rangiferina , C. mitis and Cetraria nivalis increased in biomass in fenced areas and were reduced most in biomass by reindeer in unprotected areas. Reindeer grazing and trampling seem to change the vegetation towards a type that is dominated by small dwarf shrubs, bare soil and minute-cup lichens ( Cladonia spp.). Removing the lichen layer by reindeer may reduce natural regeneration of pine trees as implied by increasing numbers of pine seedlings with increasing lichen cover.     

Effects of glyphosate on nitrogen fixation of free-living heterotrophic bacteria

The effect of the herbicide glyphosate ( N -(phosphonomethyl)glycine) on the growth, respiration and nitrogen fixation of Azotobacter chroococcum and A. vinelandii was studied. Azotobacter vinelandii was more sensitive to glyphosate toxicity than A. chroococcum. Recommended dosages of glyphosate did not affect growth rates. More than 4 kg ha^-1 is needed to find some inhibitory effect. Specific respiration rates were 19.17 mmol O₂ h^-1 g^-1 dry weight for A. chroococcum and 12.09 mmol h^-1 g^-1 for A. vinelandii. When 20 kg ha^-1 was used with A. vinelandii , respiration rates were inhibited 60%, the similar percentage inhibition A. chroococcum showed at 28 kg ha^-1. Nitrogen fixation dropped drastically 80% with 20 kg ha^-1 in A. vinelandii and 98% with 28 kg ha^-1 in A. chroococcum. Cell size as determined by electron microscopy decreased in the presence of glyphosate, probably because glyphosate induces amino acid depletion and reduces or stops protein synthesis.     

An Ecological Study of Marked Rhizobium trifolii Strains on the Host Plant Trifolium repens var. Huai in an Acidic Peat and a Neutral Mineral Soil

An ecological study of the nodulation of Trifolium repens var. grassland Huai by genetically marked Rhizobium trifolii was carried out in two Irish soils, a neutral mineral and an acidic peat. An indigenous population of 2 x 10⁴ R. trifolii /g was found in the mineral soil. In the peat soil, 4 x 10¹ R. trifolii /g was found in the uninoculated peat. This number increased to 4.5 x 10⁵ R. trifolii /g, however, eight weeks after the peat soil was neutralized, supplemented with nutrients and sown with uninoculated clover seed. Indigenous R. trifolii strains from the mineral soil were effective whereas strains from the peat soil were ineffective on the host plant T. repens under plant room conditions. The introduced strains were inoculated on to clover seed at the rate of 1 x 10⁵ R. trifolii /seed. In the mineral soil, the introduced inoculum failed to establish at any period during the growing season. In the peat soil, the percentage establishment of the introduced inoculum varied from 40-50% of nodules selected eight weeks after sowing to 70-90% of nodules selected at the end of the growing season.     

Nitrogen use efficiency. 3. Nitrogen fixation: genes and costs

The nitrogen use efficiencies (NUE) of N₂ fixation, primary NH ₄⁺ assimilation and NO ₃⁻ assimilation are compared. The photon and water costs of the various biochemical and transport processes involved in plant growth, N-assimilation, pH regulation and osmolarity generation, per unit N assimilated are respectively likely to be around 5 and 7% greater for N₂ fixation than for a combination of NH ₄⁺ and root and shoot NO ₃⁻ assimilation as occurs with most crops. Studies on plant and rhizobial genes involved in nodulation and N₂ fixation may lead to more rapid nodulation, production of more stress-tolerant N₂ fixing systems and transfer of the hydrogenase system to rhizobium/legume symbioses which currently do not have this ability. The activity of an uptake hydrogenase is predicted to decrease the photon cost of diazotrophic plant growth by about 1%.     

Interactions between elevated CO2 concentration, nitrogen and water: effects on growth and water use of six perennial plant species

Two experiments are described in which plants of six species were grown for one full season in greenhouse compartments with 350 or 560 μ mol mol^–1 CO₂. In the first experiment two levels of nitrogen supply were applied to study the interaction between CO₂ and nitrogen. In the second experiment two levels of water supply were added to the experimental set-up to investigate the three-way interaction between CO₂, nitrogen and water. Biomass and biomass distribution were determined at harvests, while water use and soil moisture were monitored throughout the experiments. In both experiments a positive effect of CO₂ on growth was found at high nitrogen concentrations but not at low nitrogen concentrations. However, plants used much less water in the presence of low nitrogen concentrations. Drought stress increased the relative effect of elevated CO₂ on growth. Available soil moisture was used more slowly at high CO₂ during drought or at high nitrogen concentrations, while at low nitrogen concentrations decreased water use resulted in an increase in soil moisture. The response to the treatments was similar in all the species used. Although potentially faster growing species appeared to respond better to high CO₂ when supplied with a high level of nitrogen, inherently slow-growing species were more successful at low nitrogen concentrations.     

三江平原小叶章湿地温室气体排放及其对模拟氮沉降的响应

利用黑龙江省科学院自然与生态研究所三江平原湿地生态定位研究站内的长期模拟氮沉降试验平台,采用静态箱-气相色谱法,设置低氮(40 kg N·hm^-2·a^-1)和高氮(80 kg N·hm^-2·a^-1)处理,以及对照(0 kg N·hm^-2·a^-1),测定小叶章湿地温室气体排放通量及其相关环境因子,研究三江平原小叶章湿地温室气体排放对氮沉降的响应.结果表明: 低氮和高氮输入均显著增加了温室气体的排放通量,低氮和高氮处理使CO₂排放通量增加47.5%和47.9%,CH₄排放通量增加76.8%和110.1%,N₂O排放通量增加42.4%和10.6%.低氮输入改变了N₂O排放的季节动态,但对CO₂和CH₄排放的季节动态没有显著影响,高氮处理对3种气体排放的季节动态均未造成影响.CO₂排放通量和CH₄排放通量均与土壤温度呈显著正相关,而影响N₂O排放的因素较为复杂,未与土壤温度出现显著的相关关系.     

Increased soil nitrogen associated with dinitrogen-fixing, terricolous lichens of the genus Peltigera in northern Minnesota

Dinitrogen (N₂)-fixing lichens (cyanolichens) have long been recognized as a source of exogenous N in various ecosystems, yet the effects of nitrogen inputs from these lichens have been little studied. Cyanolichens of the genus Peltigera Willd. are often the dominant members of the earth-dwelling (terricolous) cyanolichen community. They occur in diverse habitats around the globe, but no studies of their influence on soil N have been reported.
We conducted field and laboratory investigations with the primary objective of determining whether soil N availability is increased near healthy thalli of terricolous dinitrogen-fixing lichens. We measured available soil N in situ with ion-exchange resin bags, potentially mineralizable N with laboratory incubations, total soil N, and soil temperature. Measurements were taken along transects that extended away from thalli of Peltigera, perpendicular to and parallel to topographic contours. Studies were conducted in ten types of forest across northern Minnesota, including two contrasting sites that represent extremes of habitat for Peltigera.
Soil N availability, potentially mineralizable N, and soil %N increased significantly with proximity to healthy thalli of Peltigera (P-values<0.05). Moreover, potential N mineralization was highly correlated with soil %N (R²=0.765). Our results suggest a potential zone of influence that extends 1.5 m from thalli of Peltigera. The data indicate that soil temperature is not a primary factor in these associations.     

Fine Root Distribution in a Lower Montane Rain Forest of Panama

In a Panamanian lower montane rain forest we: (1) analyzed the vertical and horizontal distribution of fine roots; and (2) assessed the relationship of fine root mass to thickness of the soil organic layer, soil pH, and soil-extractable nitrogen. The soil in the study area has developed on volcanic ash deposits and was classified as Hapludand. In randomly distributed samples, the median fine root mass (biomass and necromass, diam ≤ 2 mm) to a depth of 100 cm mineral soil was 544 g/m², 41 percent of which was found in the organic layer. Fine root mass was approximately twice as high in the vicinity of stems of the tree species Oreomunnea mexicana (1069 g/m²) and the palm species Colpothrinax aphanopetala (1169 g/m²) and was associated with thick organic layers. The median thickness of the soil organic layer in a larger random sample ( N = 64) was 8 cm with a considerable variation (interquartile range: 7 cm). In these samples, the density of fine root biomass was correlated with the concentration of extractable nitrogen ( r = 0.33, P = 0.011), and on an areal basis, fine root biomass in the organic layer increased with increasing thickness of the organic layer ( r = 0.63, P < 0.001) and decreasing pH_KCl ( r =−0.33, P < 0.01). Fine root biomass in the upper mineral soil did not show significant correlations with any of the studied parameters.     

Nitrogen Fixation and Leaching of Biological Soil Crust Communities in Mesic Temperate Soils

Biological soil crust is composed of lichens, cyanobacteria, green algae, mosses, and fungi. Although crusts are a dominant source of nitrogen (N) in arid ecosystems, this study is among the first to demonstrate their contribution to N availability in xeric temperate habitats. The study site is located in Lucas County of Northwest Ohio. Using an acetylene reduction technique, we demonstrated potential N fixation for these crusts covering sandy, acidic, low N soil. Similar fixation rates were observed for crust whether dominated by moss, lichen, or bare soil. N inputs from biological crusts in northwestern Ohio are comparable to those in arid regions, but contribute substantially less N than by atmospheric deposition. Nitrate and ammonium leaching from the crust layer were quantified using ion exchange resin bags inserted within intact soil cores at 4 cm depth. Leaching of ammonium was greater and nitrate less in lichen than moss crusts or bare soil, and was less than that deposited from atmospheric sources. Therefore, biological crusts in these mesic, temperate soils may be immobilizing excess ammonium and nitrate that would otherwise be leached through the sandy soil. Moreover, automated monitoring of microclimate in the surface 7 cm of soil suggests that moisture and temperature fluctuations in soil are moderated under crust compared to bare soil without crust. We conclude that biological crusts in northwestern Ohio contribute potential N fixation, reduce N leaching, and moderate soil microclimate.