Experimental investigations of diel vertical movements by lotic mayflies over substrate surfaces

SUMMARY. 1. The vertical distribution within the substrate of three lotic mayflies (Rhithrogena sp., Paraleptophlebia sp. and Baetis tricaudalus Dodds) was examined in laboratory streams to determine if diel patterns of vertical movement across substrate surfaces existed and whether light intensity, temperature, substrate composition or food availability influenced the observed movement patterns.
2. Rhithrogena sp. and B. tricaudatus exhibited significant diel movement from lower substrate surfaces during the day to upper surfaces at night, although >64% of B. tricaudalus occupied the upper surfaces throughout the 24 h period. In contrast, Parakplophlebia sp. larvae did not change their vertical distribution over the 24 h period.
3. The proportion of mayflies occupying substrate surfaces was influenced by the amount of upper and lower surface area available in the substrate and, possibly, crevice sizes associated with lower surfaces.
4. The movement of Rhiihrogena sp. from lower surfaces during the day to the upper surfaces during the night was influenced by changes in light intensity, but not by changes in food availability or water temperature.
5. The diel patterns of vertical movement exhibited by lotic mayflies in this investigation raise the possibility that at least some biotic interactions may vary over a diel cycle. These could include competitive interactions or temporal cycling of prey availability to predators.     

Novel Scavenger Removal Trials Increase Wind Turbine—Caused Avian Fatality Estimates

ABSTRACT For comparing impacts of bird and bat collisions with wind turbines, investigators estimate fatalities/megawatt (MW) of rated capacity/year, based on periodic carcass searches and trials used to estimate carcasses not found due to scavenger removal and searcher error. However, scavenger trials typically place ≥10 carcasses at once within small areas already supplying scavengers with carcasses deposited by wind turbines, so scavengers may be unable to process and remove all placed carcasses. To avoid scavenger swamping, which might bias fatality estimates low, we placed only 1–5 bird carcasses at a time amongst 52 wind turbines in our 249.7-ha study area, each carcass monitored by a motion-activated camera. Scavengers removed 50 of 63 carcasses, averaging 4.45 days to the first scavenging event. By 15 days, which corresponded with most of our search intervals, scavengers removed 0% and 67% of large-bodied raptors placed in winter and summer, respectively, and 15% and 71% of small birds placed in winter and summer, respectively. By 15 days, scavengers removed 42% of large raptors as compared to 15% removed in conventional trials, and scavengers removed 62% of small birds as compared to 52% removed in conventional trials. Based on our methodology, we estimated mean annual fatalities caused by 21.9 MW of wind turbines in Vasco Caves Regional Preserve (within Altamont Pass Wind Resource Area, California, USA) were 13 red-tailed hawks (Buteo jamaicensis), 12 barn owls (Tyto alba), 18 burrowing owls (Athene cunicularia), 48 total raptors, and 99 total birds. Compared to fatality rates estimated from conventional scavenger trials, our estimates were nearly 3 times higher for red-tailed hawk and barn owl, 68% higher for all raptors, and 67% higher for all birds. We also found that deaths/gigawatt-hour of power generation declined quickly with increasing capacity factor among wind turbines, indicating collision hazard increased with greater intermittency in turbine operations. Fatality monitoring at wind turbines might improve by using scavenger removal trials free of scavenger swamping and by relating fatality rates to power output data in addition to rated capacity (i.e., turbine size). The resulting greater precision in mortality estimates will assist wildlife managers to assess wind farm impacts and to more accurately measure the effects of mitigation measures implemented to lessen those impacts.     

Immediate and long-term nitrogen oxide emissions from tropical forest soils exposed to elevated nitrogen input

Tropical nitrogen (N) deposition is projected to increase substantially within the coming decades. Increases in soil emissions of the climate‐relevant trace gases NO and N₂O are expected, but few studies address this possibility. We used N addition experiments to achieve N‐enriched conditions in contrasting montane and lowland forests and assessed changes in the timing and magnitude of soil N‐oxide emissions. We evaluated transitory effects, which occurred immediately after N addition, and long‐term effects measured at least 6 weeks after N addition. In the montane forest where stem growth was N limited, the first‐time N additions caused rapid increases in soil N‐oxide emissions. During the first 2 years of N addition, annual N‐oxide emissions were five times (transitory effect) and two times (long‐term effect) larger than controls. This contradicts the current assumption that N‐limited tropical montane forests will respond to N additions with only small and delayed increases in soil N‐oxide emissions. We attribute this fast and large response of soil N‐oxide emissions to the presence of an organic layer (a characteristic feature of this forest type) in which nitrification increased substantially following N addition. In the lowland forest where stem growth was neither N nor phosphorus (P) limited, the first‐time N additions caused only gradual and minimal increases in soil N‐oxide emissions. These first N additions were completed at the beginning of the wet season, and low soil water content may have limited nitrification. In contrast, the 9‐ and 10‐year N‐addition plots displayed instantaneous and large soil N‐oxide emissions. Annual N‐oxide emissions under chronic N addition were seven times (transitory effect) and four times (long‐term effect) larger than controls. Seasonal changes in soil water content also caused seasonal changes in soil N‐oxide emissions from the 9‐ and 10‐year N‐addition plots. This suggests that climate change scenarios, where rainfall quantity and seasonality change, will alter the relative importance of soil NO and N₂O emissions from tropical forests exposed to elevated N deposition.     

Aluminium Toxicity in Roots: An Investigation of Spatial Sensitivity and the Role of the Root Cap

The primary symptom of aluminium (Al) toxicity in higher plantsis inhibition of root growth. In this study, we investigatedthe spatial sensitivity of maize (Zea mays L.) roots to Al.A divided-chamber technique indicated that only exposure ofthe terminal 10 to 15 mm of the root to Al resulted in inhibitionof growth. Application of Al to all but this apical region ofthe root had little or no effect on growth for 24 h and causedminimal damage to the root tissue. Small agar blocks infusedwith Al were then applied to discrete areas of the apex of maizeroots to determine which section (root cap, meristem or elongationzone) was more important to Al-induced inhibition of growth.The terminal 20 to 30 mm of root (root cap and meristem) mustbe exposed to Al for inhibition. Application of Al to the 30mm of root proximal to this terminal zone (elongation zone)resulted in damage to the root tissue but no significant inhibitionof growth. Therefore, the visible injuries incurred by rootsduring Al-stress are not associated directly with the inhibitionof root growth. Furthermore, removal of the root cap had noeffect on the Al-induced inhibition of root growth in solutionexperiments and argues against the root cap providing protectionfrom Al stress or serving an essential role in the mechanismof toxicity. We suggest that the meristem is the primary siteof Al-toxicity. Key words: Aluminium, toxicity, root growth, root cap     

Unravelling causal components of the Ordovician Radiation: the Builth Inlier (central Wales) as a case study

Hypotheses about the causes of biodiversification during the Ordovician have been focused in three main areas: tectonic activity and nutrient supply, palaeogeography, and ecological escalation. There is as yet no consensus on mechanisms, and it is unclear whether it is better to study the patterns at local or regional scales. By applying ecological knowledge to the available palaeontological information, it can be shown that neither tectonic nor palaeogeographic effects could account for the permanence of the diversity rise, in the absence of elements of ecological escalation. However, it may be possible to identify trigger mechanisms resulting in enhanced speciation or reduced extinction. Areas of local diversity increase should be distinguished from speciation centres. An ongoing study of the Middle Ordovician Builth-Llandrindod Inlier of central Wales, conducted over 10 years, has identified elements of all three of the above categories of causal mechanisms affecting local diversity. This implies that the patterns of causal relationship and diversification are complex even at very local scales, and at this stage we should not anticipate a clear correlation of global diversity with any single factor. More data are needed from small-scale but intensive studies before we can generalize about the causal mechanisms of the Ordovician Radiation.     

Pigment Cell Refugia in Homeotherms—The Unique Evolutionary Position of the Iris

Homeotherms are generally considered to lack classical active dermal pigment cells (chromatophores) in their integument, attributable to the development of an outer covering coat of hair or feathers. However, bright colored dermal pigment cells, comparable to chromatophores of lower vertebrates, are found in the irides of many birds. We propose that, because of its exposed location, the iris is an area in which color from pigment cells has sustained a selective advantage and appears to have evolved independently of the general integument. In birds, the iris appears to have retained the potential for the complete expression of all dermal chromatophore types. Differences in cell morphology and the presence of unusual pigments in birds are suggested to be the result of evolutionary changes that followed the divergence of birds from reptiles. By comparison, mammals appear to have lost the potential for producing iridophores, xanthophores, or erythrophores comparable to those of lower vertebrates, even though some species possess brightly colored irides. It is proposed that at least one species of mammal (the domestic cat) has recruited a novel iridial reflecting pigment organelle originally developed in the choroidal tapetum lucidum. The potential presence of classical chromatophores in mammals remains open, as few species with bright irides have been examined.     

Chemorepellents in Paramecium and Tetrahymena

Although Paramecium has been widely used as a model sensory cell to study the cellular responses to thermal, mechanical and chemoattractant stimuli, little is known about their responses to chemorepellents. We have used a convenient capillary tube repellent bioassay to describe 4 different compounds that are chemorepellents for Paramecium and compared their response with those of Tetrahymena. The classical Paramecium t-maze chemokinesis test was also used to verify that this is a reliable chemorepellent assay. The first two compounds, GTP and the oxidant NBT, are known to be depolarizing chemorepellents in Paramecium but this is the first report of them as repellents in Tetrahymena. The second two compounds, the secretagogue alcian blue and the dye cibacron blue, have not previously been described as chemorepellents in either of these ciliates. Two other compounds, the secretagogue AED and the oxidant cytochrome c, were found to be repellents to Paramecium but not to Tetrahymena. The repellent nature of each of these compounds is not related to toxicity because cells are completely viable in all of them. More importantly, all of these repellents are effective at micromolar to nanomolar concentrations, providing an opportunity to use them as excitatory ligands in future works concerning their membrane receptors and possible receptor operated ion channels.     

Identification of CO2 Chemoreceptors in Helix pomatia

SYNOPSIS. Gas exchange in pulmonate snails of the family Helicidaeoccurs through a highly vascularized diffusion lung known asthe mantle. The extent of ventilation of the mantle dependsupon the duration and size of opening of an occlusible poreknown as the pneumostome. In Helix aspersa and Helix pomatia,pneumostomal size and frequency of opening are exquisitely sensitiveto CO₂. Respiratory CO₂ chemosensitivity resides in a discreteregion of the subesophageal ganglia. The discharge pattern ofmany neurons in the chemoreceptor area changes during stimulationwith CO₂. However, the electrophysiological response to CO,stimulation alone does not discriminate between CO₂ chemoreceptorcells and CO₂-insensitive neurons active in the pneumostomalresponse to CO₂. We identified a subset of CO₂-sensitive neuronsfrom the larger population of neurons active during CO₂ stimulation.The action potential discharge frequency of CO₂ chemosensoryneurons increased in response to CO₂ stimulation. An increaseddischarge frequency of CO₂-sensitive neurons was associatedwith increased pneumostomal opening, and both the size and thefrequency of pneumostomal opening increased during CO₂ stimulation.Injecting depolarizing current into individual chemosensoryneurons elicited opening of the pneumostome in the absence ofCO₂. Action potential generation in response to CO₂ was independentof synaptic transmission. Removal of individual CO₂-sensitivecells or inhibition of action potential generation in CO₂-sensitivecells reduced or eliminated pneumostomal responses to CO₂. CO₂sensitivity in chemoreceptor cells required extracellular calcium,but not sodium. Substituting barium for calcium supported chemoreceptoractivity. In summary, we have identified respiratory related,chemosensory neurons that are CO₂ sensitive in the absence ofsynaptic input.     

Endocrinology of the Amphibian Pineal

McCord and Allen (1917) found that extracts of mammalian pinealglands contain a potent contracting agent of larval amphibianmelanophores. Lerner and his co-workers determined the chemicalstructure of this principle and named it melatonin. This agentcontracts dermal melanophores at a concentration as low as 10^–10g/ml. Both intact and eyeless larval amphibians blanch whenplaced in the dark, and the melanophore contraction which causesthis lightening response is abolished by pinealectomy. The amphibianpineal contains photoreceptive elements similar to those foundin the vertebrate lateral eyes, and these elements are inhibitedby light but are stimulated in its absence. There is evidencefor the presence of both HIOMT and melatonin the amphibian pineal.It has been proposed that the body-blanching response resultsfrom a direct stimulation of the pineal under conditions ofdarkness leading to a release of melatonin into the generalcirculation which is then responsible for a direct contractingeffect on dermal melanophores. The cytophysiological effectsof melatonin mimic those that take place in the body-blanchingresponse. Since no other hormone or pharmacological agent duplicatesthis response, this is strong evidence that melatonin is a hormonethat normally regulates body blanching. Other evidence for thesupport of this hypothesis is presented. Cytological features of both normal and melatonin-induced lighteningindicate that the effects of melatonin are at the effector celllevel rather than at either the hypothalamus or the pituitary.An inhibition of MSH-release by melatonin is not involved. Melatoninplays a normal role in young larvae to regulate the lighteningresponse that takes place in darkness (the primary chromaticresponse). Neither melatonin nor the pineal play a role in thelater (secondary stage) adaptive background responses of amphibians.As McCord and Allen first noted, the pineal may contain othersubstances which may have other physiological roles in amphibiansas well as other vertebrates. These have been little studied.