The Distribution of Sudoriferous Glands in the Hairy Skin of Reindeer (Rangifer tarandus L.)

Skin samples were taken from forest reindeer (Rangifer tarandus L.) in order to study the distribution of apocrine tubular glands. Glands with well-developed secretory epithelium were restricted to certain areas of the body, namely the foreleg pit, a narrow strip on the belly, the groin and on the legs. Well-developed glands were also found in the oral angle and in the rump patch. The greatest amount was found in the ventral interdigital skin of both fore and hindfeet. In other parts of the body could only the excretory duct and a thin walled extension but no developed secretory epithelium be seen.     

Biometry and biology of Constempellina brevicosta (Chironomidae) in a subarctic lake

Grimås, U. and Wiederholm, T. 1979. Biometry and biology of Constempellina brevicosta (Chironomidae) in a subarctic lake. – Holarct. Ecol. 2: 119-124. Constempellina brevicosta Edw. made up about 50% of the chironomids emerging from the littoral of Lake Blåsjön. The lake is impounded for hydroelectrical purposes. Constempellina was less abundant at an earlier, smaller amplitude of water level fluctuations in the same lake and much less abundant in a nearby natural lake. The species is able to survive in a frozen substratum on ice-covered bottoms. Records of early life stages and emergence data indicated a one-year life cycle with peak emergence from the littoral zone occurring in mid July. Statistical comparisons were made of size characteristics with respect to time and site of emergence and swarming. Swarming individuals were found to be significantly larger than emerging ones as measured in length of body, wing, tibia, and tarsi. Individuals swarming from mid July to August were successively smaller in all characters except basal antennal segments. Individuals swarming in June were smaller than those occurring somewhat later. The changes in size seem to reflect differences in larval habitat, with early summer material emanating from areas exposed to winter freezing. Males swarming at different sites at the same date were similar in all respects except for body size. Individuals emerging from different depths within the littoral zone at a single date were different in most respects, those from more shallow areas being smaller. Linear regression of swarm material from different dates showed a positive correlation for most characters. The correlations were particularly strong, and applied to all characters, when the early summer material was excluded. Mean AR values were successively lower throughout the season and positively correlated with size. Mean LR values were slightly higher in early summer than later. The LR values varied independantly of size. AR and LR values in swarm material varied between extremes for single individuals which were usually within 20% of the arithmetic mean, or 0.92–1.36 for AR and 0.78–1.06 for LR. Confidence limits for population estimates were within 0.04 units of the means.     

Purification of Pregnancy Zone Protein and Its Receptor Binding Domain from Human Plasma

A new significantly improved method for purification of pregnancy zone protein (PZP), α₂-macroglobulin (α₂M), and the C-terminal PZP receptor binding domain is presented. Several steps in an earlier procedure have been deleted, and modifications in the gradients in the DEAE step leave most of the contaminants bound to a DEAE-Sephacel gel. This procedure makes possible the rapid, simultaneous purification of both of these closely related unstable proteins in native form from human plasma, with no thiolester cleavage or formation of tetrameric PZP. The final preparations of both α₂M and PZP are pure as determined by nonreducing and reducing polyacrylamide gel electrophoresis following silver staining and no cross-contamination can be observed. The yield has been significantly improved and typically more than 500 mg PZP can be obtained from 1 liter pregnancy plasma. Furthermore, the stability of PZP at different temperatures on storage was studied. In liquid nitrogen PZP can be maintained in native dimeric form with intact thiolester for many years. The storage of native PZP with intact functional properties during and after purification is an obligatory prerequisite to elucidate the biological role of PZP. The receptor binding domain of PZP can be cleaved from the PZP–methylamine complex by papain and isolated from the other peptides by S-200 gel filtration. The cleavage site was determined and the C-terminal fragment was identified with several site-specific monoclonal antibodies against PZP.     

A living environment. Objectives and measures in the Swedish Government Bill on environmental policy 1990/91, pertaining to waters and the seas

Increased international cooperation to limit transboundary and global environmental problems, increased sectoral responsibility and decentralization, and improved information and statistics on the state of the environment are the main lines for the development of future environmental policy. For lakes, watercourses, and the seas the overall objective is to maintain viable, balanced populations of naturally occurring species. Pollution is not to limit the use of water for fishing, recreation, or water supply. Foreign species or organisms subjected to genetic mutation are only to be introduced with great restriction. Measures are suggested that will reduce environmental disturbances from agriculture and forestry, traffic, energy production, industry, goods, chemical products, and waste.Paper presented at Seminar on Ecosystems Approach to To Water Management (Oslo, Norway, 27–31 May 1991).     

Genomics in a changing arctic: critical questions await the molecular ecologist

Molecular ecology is poised to tackle a host of interesting questions in the coming years. The Arctic provides a unique and rapidly changing environment with a suite of emerging research needs that can be addressed through genetics and genomics. Here we highlight recent research on boreal and tundra ecosystems and put forth a series of questions related to plant and microbial responses to climate change that can benefit from technologies and analytical approaches contained within the molecular ecologist's toolbox. These questions include understanding (i) the mechanisms of plant acquisition and uptake of N in cold soils, (ii) how these processes are mediated by root traits, (iii) the role played by the plant microbiome in cycling C and nutrients within high‐latitude ecosystems and (iv) plant adaptation to extreme Arctic climates. We highlight how contributions can be made in these areas through studies that target model and nonmodel organisms and emphasize that the sequencing of the Populus and Salix genomes provides a valuable resource for scientific discoveries related to the plant microbiome and plant adaptation in the Arctic. Moreover, there exists an exciting role to play in model development, including incorporating genetic and evolutionary knowledge into ecosystem and Earth System Models. In this regard, the molecular ecologist provides a valuable perspective on plant genetics as a driver for community biodiversity, and how ecological and evolutionary forces govern community dynamics in a rapidly changing climate.     

Nitrogen availability affects saprotrophic basidiomycetes decomposing pine needles in a long term laboratory study

Fungi, especially basidiomycetous litter decomposers, are pivotal to the turnover of soil organic matter in forest soils. Many litter decomposing fungi have a well-developed capacity to translocate resources in their mycelia, a feature that may significantly affect carbon (C) and nitrogen (N) dynamics in decomposing litter. In an eight-month long laboratory study we investigated how the external availability of N affected the decomposition of Scots pine needles, fungal biomass production, N retention and N-mineralization by two litter decomposing fungi – Marasmius androsaceus and Mycena epipterygia. Glycine additions had a general, positive effect on fungal biomass production and increased accumulated needle mass loss after 8 months, suggesting that low N availability may limit fungal growth and activity in decomposing pine litter. Changes in the needle N pool reflected the dynamics of the fungal mycelium. During late decomposition stages, redistribution of mycelium and N out from the decomposed needles was observed for M. epipterygia, suggesting autophagous self degradation.     

Compensatory growth for free? A field experiment on brown trout,Salmo trutta

Laboratory studies suggest that animals may be capable of compensatory growth after periods of food shortage. There is, however, a lack of field experiments investigating the incidence and consequences of compensatory growth in the wild, and the relevance of compensatory responses in natural populations has recently been questioned. Here we addressed the hypotheses that (1) food restriction during critical growth periods can induce compensatory growth, and (2) that compensatory growth is associated with delayed costs in natural populations. These hypotheses were addressed by (1) manipulating the food intake of brown trout in spring, (2) measuring growth rate responses over the first month following release, and (3) measuring growth and mortality (i.e. recapture rate) over the subsequent fall and winter. We found that brown trout restored lost body weight and condition within a month, providing the first experimental demonstration of compensatory growth in the wild. However, no delayed costs of the compensatory response could be detected within the timespan of the experiment. We suggest that wild brown trout have an adapted "buffer capacity" to withstand fluctuations in food supply, allowing restoration of lost lipid reserves when feeding conditions improve. However, when prolonged food deprivation affect structural components, compensation may not be possible without compromising long-term performance.     

The return of an experimentally N-saturated boreal forest to an N-limited state: observations on the soil microbial community structure,biotic N retention capacity and gross N mineralisation

Background and aims

To find out how N-saturated forests can return to an N-limited state, we examined the recovery of biotic N sinks under decreasing N supply.

Methods

. We studied a 40-year-old experiment in Pinus sylvestris forest, with control plots, N0, three N treatments, N1-N3, of which N3 was stopped after 20 years, allowing observation of recovery.

Results

In N3, the N concentration in foliage was still slightly elevated, but the N uptake capacity of ectomycorrhizal (ECM) roots in N3 was no longer lower than in N0. Per area the amount of a biomarker for fungi, here mainly attributed ECM, was higher in N3 and N0 than in N1 and N2. Retention of labeled ¹⁵NH₄ ⁺ by the soil was greater in the control (99 %) and N3 (86 %), than in N1 (45 %) and N2 (29 %); we ascribe these differences to biotic retention because cation exchange capacity did not vary. Gross N mineralisation and retention of N correlated, negatively and positively, respectively, with abundance of ECM fungal biomarker.

Conclusions

. The results suggest a key role for ECM fungi in regulating the N cycle. We propose, in accordance with plant C allocation theory, that recovery is driven by increased tree below-ground C allocation to ECM roots and fungi.     

Temperature responses of photosynthetic capacity parameters were not affected by foliar nitrogen content in mature Pinus sylvestris

A key weakness in current Earth System Models is the representation of thermal acclimation of photosynthesis in response to changes in growth temperatures. Previous studies in boreal and temperate ecosystems have shown leaf‐scale photosynthetic capacity parameters, the maximum rates of carboxylation (V_cmax) and electron transport (J_max), to be positively correlated with foliar nitrogen (N) content at a given reference temperature. It is also known that V_cmax and J_max exhibit temperature optima that are affected by various environmental factors and, further, that N partitioning among the foliar photosynthetic pools is affected by N availability. However, despite the strong recent anthropogenic influence on atmospheric temperatures and N deposition to forests, little is known about the role of foliar N contents in controlling the photosynthetic temperature responses. In this study, we investigated the temperature dependencies of V_cmax and J_max in 1‐year‐old needles of mature boreal Pinus sylvestris (Scots pine) trees growing under low and high N availabilities in northern Sweden. We found that needle N status did not significantly affect the temperature responses of V_cmax or J_max when the responses were fitted to a peaked function. If such N insensitivity is a common tree trait it will simplify the interpretation of the results from gradient and multi‐species studies, which commonly use sites with differing N availabilities, on temperature acclimation of photosynthetic capacity. Moreover, it will simplify modeling efforts aimed at understanding future carbon uptake by precluding the need to adjust the shape of the temperature response curves to variation in N availability.