Rising concentrations of atmospheric CO2 have increased growth in natural stands of quaking aspen (Populus tremuloides)

As atmospheric CO₂ levels rise, temperate and boreal forests in the Northern Hemisphere are gaining importance as carbon sinks. Quantification of that role, however, has been difficult due to the confounding effects of climate change. Recent large‐scale experiments with quaking aspen (Populus tremuloides), a dominant species in many northern forest ecosystems, indicate that elevated CO₂ levels can enhance net primary production. Field studies also reveal that droughts contribute to extensive aspen mortality. To complement this work, we analyzed how the growth of wild aspen clones in Wisconsin has responded to historical shifts in CO₂ and climate, accounting for age, genotype (microsatellite heterozygosity), and other factors. Aspen growth has increased an average of 53% over the past five decades, primarily in response to the 19.2% rise in ambient CO₂ levels. CO₂‐induced growth is particularly enhanced during periods of high moisture availability. The analysis accounts for the highly nonlinear changes in growth rate with age, and is unaffected by sex or location sampled. Growth also increases with individual heterozygosity, but this heterozygote advantage has not changed with rising levels of CO₂ or moisture. Thus, increases in future growth predicted from previous large‐scale, common‐garden work are already evident in this abundant and ecologically important tree species. Owing to aspen's role as a foundation species in many North American forest ecosystems, CO₂‐stimulated growth is likely to have repercussions for numerous associated species and ecosystem processes.     

Limnochemical and phytoplankton studies on Nyumba ya Mungu reservoir, Tanzania

This publication reports on the chemical and phytoplankton aspects of a three month biological survey of Nyumba ya Mungu reservoir, Tanzania.
The lake had a total salt concentration of about 8 meq dm^-3 and specific conductivity of 900 μS cm^-1. The main salt in solution was sodium bicarbonate, and when the lake level fell it sometimes formed a crust on the exposed shore. The concentrations of major nutrient ions were probably not limiting to algal growth and good nutrient replenishment was provided by the two inflow rivers.
Nyumba ya Mungu supports a rich phytoplanton dominated by Melosira and blue-green algae. Acetone extractions gave chlorophyll 'a' concentrations ranging from 20–40 mgm^-3 in the vertical profiles, and light and dark bottle experiments indicated a maximum gross photosynthesis of about 800 mg O₂ m^-3h^-1. There was evidence of chemical stratification in the open water and diurnal stratification in the sheltered bays, but discontinuities were short-lived and the Trade Winds ensured regular mixing of the water. The lake appeared to have a higher primary production than the larger Rift Valley lakes and it was considered that this level of production would continue.     

Congruence between larval ventromental plate ultrastructure and immature morphology in Yama Sublette & Martin and some Oceanian species of Chironomus Meigen (Diptera: Chironomidae)

The morphology of the larval ventromental plates of Y. tahitiensis Sublette & Martin and four Oceanian species of Chironomus Meigen, C. hawaiiensis Grimshaw, C. javanus Kieffer, C. magnivalva Kieffer and C. samoensis Edwards, has been studied by scanning electron micrography. Data on ventromental plate ultrastructure are used in phenetic and cladistic analyses of the relationships of T. tahitiensis and the Oceanian Chironomus to other species in Chironomus and additional genera. The results of these analyses support the current generic status of T. tahitiensis but indicate that Yama is less closely related to Chironomus than previously supposed, a finding that is supported by a reexamination of ‘traditional’ morphological features.     

Bias in studies of heterozygosity and mate choice

A key question for molecular and behavioural ecologists who study mating systems is to understand why, in many species, females choose to mate with extra-pair males. Recently a possible explanation, 'genetic compatibility', has gained increasing empirical support (for a comprehensive review, see Kempenaers 2007 ). Genetic compatibility hypotheses assume that females seek extra-pair mates with alleles that complement their own. Typically, this will be achieved by mating with a male of a different genotype than her own, in order to maximise the heterozygosity of her offspring. Because numerous studies have indicated positive associations between heterozygosity and fitness (see Coltman & Slate 2003 ), it follows that mating with 'compatible' males will result in heterozygous, and therefore fit, offspring. Most empirical support for genetic compatibility has been obtained with microsatellite markers that have first been used to assess parentage and then to estimate relatedness and/or individual heterozygosity. A problem with this approach is a possible bias that favours the detection of extra-pair paternity when the extra-pair male has a genotype different from that of the female and her social mate. This in turn could lead to the erroneous conclusion that extra-pair males are less related to the female than within-pair males. In this issue of Molecular Ecology , Wetzel & Westneat 2009 (hereafter W&W), use simulation studies to assess the extent of this bias, using parameter estimates obtained from recent empirical data. They identify two forms of bias that may affect tests of the genetic compatibility hypothesis, and provide guidelines on how these biases may be avoided.     

The use of eddy covariance to infer the net carbon dioxide uptake of Brazilian rain forest

• 1 Eddy covariance measurements of CO₂ flux, based on four and six week campaigns in Rondôdnia, Brazil, have been used in conjunction with a model to scale up data to a whole year, and thus estimate the carbon balance of the tropical forest ecosystem, and the changes in carbon balance expected from small interannual variations in climatological conditions.
• 2 One possible source of error in this estimation arises from the difficulty in measuring fluxes under stably stratified meteorological conditions, such as occur frequently at night. Flux may be ‘lost’ because of low velocity advection, caused by nocturnal radiative cooling at sites on raised ground. Such effects may be detected by plotting the net ecosystem flux of CO₂, F_eco is a function of wind speed. If flux is ‘lost’ then F_eco is expected to decline with wind speed. In the present data set, this did not occur, and F_eco was similar to the nocturnal flux estimated independently from chamber measurements.
• 3 The model suggests that in 1992/3, the Gross Primary Productivity (GPP) was 203.3 mol C m^?2 y^?1 and ecosystem respiration was 194.8 mol C m^?2 y^?1, giving an ecosystem carbon balance of 8.5 mol C m^?2 y^?1, equivalent to a sink of 1.0 ton C ha^?1 y^?1. However, the sign and magnitude of this figure is very sensitive to temperature, because of the strong influence of temperature on respiration.
• 4 The model also suggests that the effect of temperature on the net carbon balance is strongly dependent on the partial pressure of CO₂.

     

Evidence for mate‐encounter Allee effect in an invasive longhorn beetle (Coleoptera: Cerambycidae)

1. Limited empirical support is available for mate‐encounter Allee effects in invasive insects due to the logistical challenges of studying demographic trends in low‐density populations. 2. Traps baited with pheromone and spruce volatiles were used to monitor the abundance of female Tetropium fuscum F. (Coleoptera: Cerambycidae) at multiple sites in Nova Scotia in 2011 and 2012. Each female was dissected to determine the presence or absence of sperm in its spermatheca (mated or virgin female, respectively). 3. Both male and total T. fuscum abundance declined with increasing distance to the focal point of T. fuscum's invasion. Female mating probability declined with male abundance and with distance from the invasion focus, and mating probabilities were very low at the most peripheral sites. Difficulty in encountering mates may thus contribute to limiting the spread of T. fuscum. 4. The approach outlined here could be integrated into existing surveys of wood borers using traps baited with semiochemicals to improve our understanding of the role of the mate‐encounter Allee effect in invasion dynamics.     

Mathematical determination of coiled shell volumes and surface areas

Mathematical models of shells enable researchers to estimate the maximum possible sizes of organisms that once occupied fossil shells. In this study, a whorl-by-whorl method of determining coiled shell volumes and surface areas is introduced. The whorl-by-whorl analysis yielded results that were more accurate than those obtained from a model that assumes isometric growth, when both were used to calculate volumes of gastropod shells. The whorl-by-whorl method is more laborious, but it is better suited for the analysis of shells exhibiting allometric variation than are methods that use models of isometric growth.     

Ventilatory Mechanism and Control in Grasshoppers

SYNOPSIS. Grasshoppers exhibit a diversity of ventilatory patternsdepending on activity status. For each pattern, the mechanismand control of gas exchange is analyzed in terms of a two-stepmodel, consisting of tracheolar and trans-spiracular steps inseries. During the intermittent gas exchange that characterizesthe most quiescent grasshoppers, spiracles open and close inresponse to changing carbon dioxide, and trans-spiracular resistancecontrols gas exchange. In resting but alert grasshoppers, abdominalpumping occurs, and gas exchange is controlled equally by tracheolarand trans-spiracular resistances; tracheal oxygen and carbondioxide are regulated by variation in abdominal pumping andspiracular opening. During hopping, abdominal pumping does notoccur, and bulk gas flow is driven by cuticular deformationsassociated with locomotion. Increased cellular oxygen consumptiondepends on use of internal oxygen stores and increased partialpressure gradients. After hopping ceases, abdominal pumpingincreases dramatically and restores tracheal gas composition;however, the rise in abdominal pumping after hopping is notaffected by tracheal gas levels. During flight, bulk flow tothe flight muscles is driven by tidal thoracic auto-ventilation,while the remainder of the body is ventilated by abdominal pumping.During both hopping and flight, the greatest resistances togas transport exist in the tracheolar rather than the trans-spiracularstep.