552 publications from this institution
Summary The mechanistic basis of feather moss–cyanobacteria associations, a main driver of nitrogen ( N ) input into boreal forests, remains unknown. Here, we studied colonization by N ostoc sp. on two feather mosses that form these associations ( P leurozium schreberi and H ylocomium splendens ) and two acrocarpous mosses that do not ( D icranum polysetum and P olytrichum commune ). We also determined how N availability and moss reproductive stage affects colonization, and measured N transfer from cyanobacteria to mosses. The ability of mosses to induce differentiation of cyanobacterial hormogonia, and of hormogonia to then colonize mosses and re‐establish a functional symbiosis was determined through microcosm experiments, microscopy and acetylene reduction assays. Nitrogen transfer between cyanobacteria and Pleurozium schreberi was monitored by secondary ion mass spectrometry ( SIMS ). All mosses induced hormogonia differentiation but only feather mosses were subsequently colonized. Colonization on P leurozium schreberi was enhanced during the moss reproductive phase but impaired by elevated N . Transfer of N from cyanobacteria to their host moss was observed. Our results reveal that feather mosses likely secrete species‐specific chemo‐attractants when N ‐limited, which guide cyanobacteria towards them and from which they gain N . We conclude that this signalling is regulated by N demands of mosses, and serves as a control of N input into boreal forests.
There is currently much interest in understanding how biodiversity loss affects the functioning of ecosystems, but few studies have evaluated how ecosystem processes change in response to one another following biodiversity loss. We focused on a well‐described gradient of 30 forested lake islands in northern Sweden, where island size determines the occurrence of lightning‐ignited wildfire, which in turn determines successional stage, plant species composition, and productivity. We investigated the effect of biodiversity loss on biological nitrogen fixation by feathermosses through an experiment consisting of factorial removals of three understory shrub species ( Vaccinium myrtillis , Vaccinium vitis‐idaea , and Empetrum hermaphroditum ) and two plant functional groups (shrubs and tree roots). We tested the hypothesis that, following vascular plant species loss, N fixation rates would be impaired by changes in pools or processes that increase extractable soil N, because changes in the supply rate of N to feathermosses should influence their demand for newly fixed N. Further, we hypothesized that the effects of removals on N fixation would depend on environmental context (i.e., island size), because it has been previously demonstrated that the effect of vascular plant species removal on N recycling pools and processes was strongest on productive islands. The data demonstrated that removal of two shrub species ( V. vitis‐idaea and E. hermaphroditum ) negatively affected the N fixation of Hylocomium splendens , but positively affected Pleurozium schreberi , resulting in unchanged areal N fixation rates. In the functional removal experiment, tree root removal resulted in a significant negative effect on N fixation. The effects of shrub and root removals on N fixation occurred only on small islands and thus were context dependent. This pattern did not correspond to the effect of shrub and root removal treatments on N‐recycling pools or processes, which only occurred in response to specific vascular plant removals on large or medium islands. The data thus did not support our hypothesis that N fixation was directly responsive to changes in N‐recycling pools or processes caused by vascular plant species removals, but instead highlighted the importance of species‐specific interactions and environmental context in determining the manner in which biodiversity loss alters ecosystem processes.
Nitrogen (N) and carbon (C) isotopic signatures (δ15N and δ13C) serve as powerful tools for understanding temporal changes in ecosystem processes
Many insects are drawn to the heat, ash, and smoke produced by forest fires and arrive in large numbers at recent burns, often while the fire is still active. Some of these insects are pyrophilic and reproduce exclusively in the immediate aftermath of fire but are rarely, if ever, collected from unburnt habitats. Numerous observations made at active fires note an apparent preference among some pyrophilic insects to oviposit exclusively in the burnt portions of trees, raising broader questions about the adaptive benefits of reproduction in the post‐burn environment. Here, we tested whether the reproductive output of pyrophilic ground beetles (i.e., Sericoda spp.) increased in heat‐sterilized soils. In the first experiment, the eggs of Sericoda quadripunctata were reared in three types of soil collected from burnt forests: recently burnt soil (collected 1–2 weeks after the fire), soil collected 1 year after burn, and soil from an unburnt patch of forest adjacent to the fire. Daily monitoring through a dissecting microscope documented extensive predation of eggs by soil microarthropods (mites, springtails, and nematodes), especially in 1‐year‐old and unburnt soil treatments. This led to a second experiment that included the same three treatments and an additional fourth soil treatment: recently, burnt soil reheated to 100°C for 2 h (i.e., reheated soil). In this experiment, male and female pairs ( n = 100) of Sericoda obsoleta were reared for 14 days in jars containing 90 g of soil corresponding to each of the four soil treatments. Reproductive output, measured as the number of larvae produced by each breeding pair, was significantly higher in the reheated soil, suggesting that heat sterilization and removal of soil‐dwelling predators improved egg survival. Our findings suggest that pyrophily in insects may have evolved as a means of increasing reproductive output in the post‐burn environment through access to heat‐sterilized ovipositing substrates. Furthermore, the abrupt disappearance of Sericoda and other pyrophilic insects following fire may be explained by suboptimal reproductive conditions as the burn is colonized by other organisms and by local emigration in favor of other recent burns on the landscape.
Despite the likely importance of inter-year dynamics of plant production and consumer biota for driving community- and ecosystem-level processes, very few studies have explored how and why these dynamics vary across contrasting ecosystems. We utilized a well-characterized system of 30 lake islands in the boreal forest zone of northern Sweden across which soil fertility and productivity vary considerably, with larger islands being more fertile and productive than smaller ones. In this system we assessed the inter-year dynamics of several measures of plant production and the soil microbial community (primary consumers in the decomposer food web) for each of nine years, and soil microfaunal groups (secondary and tertiary consumers) for each of six of those years. We found that, for measures of plant production and each of the three consumer trophic levels, inter-year dynamics were strongly affected by island size. Further, many variables were strongly affected by island size (and thus bottom-up regulation by soil fertility and resources) in some years, but not in other years, most likely due to inter-year variation in climatic conditions. For each of the plant and microbial variables for which we had nine years of data, we also determined the inter-year coefficient of variation (CV), an inverse measure of stability. We found that CVs of some measures of plant productivity were greater on large islands, whereas those of other measures were greater on smaller islands; CVs of microbial variables were unresponsive to island size. We also found that the effects of island size on the temporal dynamics of some variables were related to inter-year variability of macroclimatic variables. As such, our results show that the inter-year dynamics of both plant productivity and decomposer biota across each of three trophic levels, as well as the inter-year stability of plant productivity, differ greatly across contrasting ecosystems, with potentially important but largely overlooked implications for community and ecosystem processes.
The soil microbial biomass and microbial metabolic quotient (respiration: biomass ratio) was measured in 16 forest and scrubland ecosystems throughout New Zealand, on materials representing successional stages of plant litter and its subsequent incorporation into the F-H and mineral soil layers. Microbial biomass usually peaked in the L 1 layer and then declined. The microbial carbon:organic carbon ratio decreased sharply between the F-H layer and the underlying mineral layer, indicating that a stress factor (possibly pH) reduced the proportion of organic matter immobilized in the microbial biomass at this stage. The microbial respiration: biomass ratio declined between the L 1 and F-H stages
We agree with Winter and Schweiger that it is important to differentiate between gradually changing and abruptly changing systems. Transformation of tropical regions by land-use change will inevitably have abrupt and profound effects on ecosystem properties, which will be driven both by changes in abiotic factors and by the replacement of one suite of species with another. As such, we maintain that in these cases the species trait concept remains relevant. Even when most or all species are lost, changes in the ecosystem will be driven most strongly by the loss of those species whose traits had the strongest effects on ecosystem processes before the loss occurred.
The influence of capitulum maturity on achene germination was investigated for Senecio jacobaea L. and Carduus nutans L. Germination of achenes from capitula in full flower was negligible for both species but as the floral tissues began to senesce the germination percentage rose to at least 50% for all populations investigated. S. jacobaea achenes with floral parts abscised or absent were generally more viable than achenes with floral parts attached, and seedlings from such achenes exhibited higher growth rates. C. nutans did not exhibit any consistent trends.
We hypothesised that plant species composition and richness would affect soil chemical and microbial community properties, and that these in turn would aff
While most studies focusing on the effects of agricultural intensification on soil biota are inherently short-term in nature, long-term (multiyear) studies are essential in assessing long-term temporal responses of soil biota to agronomic practices. We investigated the effects of three components of agricultural intensification, i.e. cultivation (disturbance), herbicide addition (modification of floristic composition) and mulching (resource addition) on soil-associated arthropods in an annual (maize) and a perennial (asparagus) cropping system over a 7 yr period. An additional treatment (hand-hoeing of weeds during the crop growing season) was used to represent minimal intensification. Many taxa of arthropods responded positively to mulching and to treatments which allowed high weed biomass in the non crop-production period, e.g. the hand-hoeing and cultivation treatments in the perennial crop. Herbicide treatments also facilitated high numbers of many taxa in the annual crop when this coincided with plot invasion by herbicide-tolerant weeds. Generally, arthropod taxa were positively correlated with weed biomass and negatively with crop plant biomass, probably because of the superior resource (litter) quality produced by the former. Ordination analyses indicated that arthropod community structure was often correlated with weed community structure. Mulching and allowing high weed biomass also promoted a high species richness of soil-associated Coleoptera, but coleopteran diversity was not related to weed species diversity. Analyses of temporal variability (inversely related to stability) of arthropod taxa across years revealed few treatment effects in the annual crop, but showed destabilising effects of weed reduction in the perennial crop. In the perennial crop, temporal variability was also positively correlated with crop biomass and negatively with weed biomass across plots. Our study shows that agricultural intensification is not consistently harmful to the soil fauna, that soil-associated arthropods are most responsive to management practices which affect the nature and quality of resource input, and that long-term experiments are essential for answering questions about how agricultural practices affect soil organisms against the natural backdrop of temporal variation.