Variation in nitrogen-15 natural abundance and nitrogen uptake traits among co-occurring alpine species: do species partition by nitrogen form?

In the N-limited alpine tundra, plants may utilize a diversity of N sources (organic and inorganic N) in order to meet their nutritional requirements. To characterize species-level differences in traits related to N acquisition, we analyzed foliar '¹⁵N, nitrate reductase activity (NRA) and mycorrhizal infection in co-occurring alpine species during the first half of the growing season and compared these traits to patterns of N uptake using a ¹⁵N (¹⁵N-NH₄⁺, ¹⁵N-NO₃^-) or ¹³C,¹⁵N ([1]-¹³C-¹⁵N-glycine) tracer addition in the greenhouse. ¹³C enrichment in belowground tissue indicated that all species were capable of taking up labeled glycine, although only one species showed uptake of glycine potentially exceeding that of inorganic N. Species showing the most depleted foliar '¹⁵N and elevated NRA in the field also tended to show relatively high rates of NO₃^- uptake in the greenhouse. Likewise, species showing the most enriched foliar '¹⁵N also showed high rates of NH₄⁺ uptake. The ratio of NO₃^-:NH₄⁺ uptake rates and growth rate explained 64% and 72% of the variance in foliar '¹⁵N, respectively, suggesting that species differ in the ability to take up NO₃^- and NH₄⁺ in the field and that such differences may enable species to partition soil N on the basis of N form.     

Future eating and country keeping: what role has environmental history in the management of biodiversity?

In order to understand and moderate the effects of the accelerating rate of global environmental change land managers and ecologists must not only think beyond their local environment but also put their problems into a historical context. It is intuitively obvious that historians should be natural allies of ecologists and land managers as they struggle to maintain biodiversity and landscape health. Indeed, ‘environmental history’ is an emerging field where the previously disparate intellectual traditions of ecology and history intersect to create a new and fundamentally interdisciplinary field of inquiry. Environmental history is rapidly becoming an important field displacing many older environmentally focused academic disciplines as well as capturing the public imagination. By drawing on Australian experience I explore the role of ‘environmental history’ in managing biodiversity. First I consider some of the similarities and differences of the ecological and historical approaches to the history of the environment. Then I review two central questions in Australian environment history: landscape‐scale changes in woody vegetation cover since European settlement and the extinction of the marsupials in both historical and pre‐historical time. These case studies demonstrate that environmental historians can reach conflicting interpretations despite using essentially the same data. The popular success of some environmental histories hinges on the fact that they narrate a compelling story concerning human relationships and human value judgements about landscape change. Ecologists must learn to harness the power of environmental history narratives to bolster land management practices designed to conserve biological heritage. They can do this by using various currently popular environmental histories as a point of departure for future research, for instance by testing the veracity of competing interpretations of landscape‐scale change in woody vegetation cover. They also need to learn how to write parables that communicate their research findings to land managers and the general public. However, no matter how sociologically or psychologically satisfying a particular environmental historical narrative might be, it must be willing to be superseded with new stories that incorporate the latest research discoveries and that reflects changing social values of nature. It is contrary to a rational and publicly acceptable approach to land management to read a particular story as revealing the absolute truth.     

Transmembrane potential changes during phagocytosis in rat alveolar macrophages

Studies were carried out to measure changes in the transmembrane potential of rat alveolar macrophages during exposure of the cells to zymosan particles or to the membrane perturbant, phorbol-12-myristate-13-acetate (PMA), and to determine if changes in membrane potential are related to superoxide anion release. Exposure of the cells to either zymosan or PMA leads to membrane depolarization, which precedes superoxide anion release. Furthermore, the magnitude of the depolarization is dependent upon the concentration of either zymosan or PMA. During exposure of the alveolar macrophages to increasing levels of zymosan, there is an increase in the amount of superoxide released as well as an increase in the magnitude of the depolarization. Incubation of the cells in medium containing 150 mM K+, a medium which causes membrane depolarization, leads to superoxide release from resting cells and a decrease in the amount of superoxide released from cells exposed to zymosan. These results indicate that release of superoxide anion from rat alveolar macrophages is related to membrane depolarization and suggest that the transmembrane potential change may act as a signal to initiate the phagocytotic responses of the cells.     

Effect of sexual stimulation on concentrations of 5α-androstenone and testosterone in the peripheral plasma of boars reared individually

Six Yorkshire boars were reared from 107 days of age in individual pens. No female pigs were housed in the same building. When the boars were 200 days old, sows in oestrus were introduced to the pens of five boars and remained with the boars for 2 days. No oestrous sow was introduced to the pen with the sixth boar. Plasma 5α-androstenone and testosterone concentrations were low between 107 and 200 days of age in all boars. The maximum mean concentrations of these two steroids during this period were 6.18 ± 0.72 and 3.04 ± 1.02 ng/ml, respectively. Plasma 5α-androstenone concentrations increased with advancing age (P < 0.01). A similar trend was not seen for plasma testosterone concentrations. Plasma concentrations of 5α-androstenone and testosterone increased by 247 ± 27% (P < 0.02) and 1212 ± 204% (P < 0.001), respectively, in the samples drawn 24 h after the introduction of the sexually receptive sows. The maximal mean concentrations recorded following sexual stimulation were 12.90 ± 1.80 and 17.51 ± 1.96 ng/ml for 5α-androstenone and testosterone, respectively. The control boar also showed increases in plasma 5α-androstenone (221%) and testosterone (751%) concentrations in the same period, probably in response to auditory and olfactory stimuli originating in the pens nearby with introduced oestrous sows.     

Hospital training for general practice: views of trainees in the North Western region.

Vocational trainees in the North Western region who were in their general practice year completed a questionnaire concerning the hospital component of their training. Replies were received from 125 trainees, providing information about 451 hospital posts. In a total of 372 posts (85%) less than two hours of formal teaching a week was provided. Trainees stated that they received no informal teaching in nearly one third of posts. The orientation of teaching towards general practice was reported as greatest in the posts that were not part of a vocational training scheme. Study leave was applied for by doctors in only 163 (37%) posts, usually to prepare for or to sit an examination. There seem to be serious educational deficiencies in hospital posts that are used to train both general practitioners and other specialists. Improvements in both the quantity and quality of in service teaching are therefore needed urgently.     

Effects of lead on luteal function in rhesus monkeys

Exposure to lead in the workplace or home environment has been implicated as a cause of decreased fertility in women. In a previous study, as part of our effort to determine effects of lead in primates, female rhesus monkeys were exposed to lead acetate in drinking water (n = 10) or provided water with no added lead (n = 7) for 33 mo. Lead was administered at levels between 2 and 8 mg/kg/day, with doses adjusted to keep blood lead values near a target of 70 micrograms/dl (observed mean +/- SEM = 68.9 +/- 6.54 micrograms/dl). Blood lead concentrations in control animals were less than 10 micrograms/dl. No significant differences were detected between control and experimental animals in body weight, hematocrit, or general health. Female monkeys receiving lead exhibited longer and more variable menstrual cycles and shorter menstrual flow. In the present study, circulating amounts of progesterone (P4) were determined to evaluate luteal function during the final 7 mo of treatment with lead. Several characteristics were altered as a result of lead treatment: circulating amounts of P4 were reduced as indicated by relative units of area under the concentration-time curve, maximal amounts of P4 were reduced, and P4 levels were greater than 1 ng/ml on fewer days. There were no significant differences between groups in mean percent of anovulatory cycles. Therefore, although chronic treatment with the levels of lead used in this study did not prevent ovulation, luteal function was suppressed. These results extend previous observations of adverse effects of lead on ovarian activity and fertility in monkeys.     

Green land: Multiple perspectives on green algal evolution and the earliest land plants

Green plants, broadly defined as green algae and the land plants (together, Viridiplantae), constitute the primary eukaryotic lineage that successfully colonized Earth's emergent landscape. Members of various clades of green plants have independently made the transition from fully aquatic to subaerial habitats many times throughout Earth's history. The transition, from unicells or simple filaments to complex multicellular plant bodies with functionally differentiated tissues and organs, was accompanied by innovations built upon a genetic and phenotypic toolkit that have served aquatic green phototrophs successfully for at least a billion years. These innovations opened an enormous array of new, drier places to live on the planet and resulted in a huge diversity of land plants that have dominated terrestrial ecosystems over the past 500 million years. This review examines the greening of the land from several perspectives, from paleontology to phylogenomics, to water stress responses and the genetic toolkit shared by green algae and plants, to the genomic evolution of the sporophyte generation. We summarize advances on disparate fronts in elucidating this important event in the evolution of the biosphere and the lacunae in our understanding of it. We present the process not as a step-by-step advancement from primitive green cells to an inevitable success of embryophytes, but rather as a process of adaptations and exaptations that allowed multiple clades of green plants, with various combinations of morphological and physiological terrestrialized traits, to become diverse and successful inhabitants of the land habitats of Earth.