AN INTEGRATING RECORDER FOR PHOTOSYNTHETICALLY ACTIVE RADIANT ENERGY WITH IMPROVED RESOLUTION

A device counting fixed amount of parcels of radiant energyefficient in photosynthesis (wavelength region 400 to 720 mµand recording their total as a digital reading on a counteris described. Radiant energy is transformed by means of a phototubeto electrical current which becomes divided into individualparcels by cycles of charging .and discharge of a condenserbetween two fixed values of potential, and the number of thesecycles is counted. From instruments of similar design published earlier the onepresented here is distinguished mainly (1) by improved linearityof response in the integrating circuit down to slow countingrates and (2) by the design of a nonselective detector (in thelimited range of wavelengths indicated) based on a vacuum emissionphototube, which may be combined with the simple integratingcircuit used. Thus totals of irradiance (throughout the rangeof intensities of solar radiation) may be obtained directlyin units of energy or in the number of quanta. A very reliable and stable receiver with energy proportionalresponse in the region of wavelength 400–720 mµ(with possible extension up to 1,000 mµ) was realizedusing a vacuum emission photocell with photosensitive surfaceof the double-peak emission type (covering the range from nearUV to near IR) and precisely counterbalancing its spectral sensitivitycurve by selective absorption glass filters. The RENTSCHLER's type integrating circuit with a cold cathodedischarge tube was improved by increasing the maximum countingrate on one side (damping germanium diodes across the coilsof relay and counter) and by minimization of leakage in parallelto spare condenser (the contact which shortcircuits the condensersimultaneously with ignition of the discharge tube). ¹ Dedicated to Prof. H. TAMIYA on his 60th birthday. (Received November 24, 1962; )     

Aspects of the biology of Hyolitha (Mollusca)

Hyolitha constitute an extinct group of class rank assigned to Molhsca. Two orders, Ortho-thecida and Hyolithida, are well established and most knowledge of morphologic detail is derived from the latter. Both orders had an operculum not hinged to the conch. Hyolithida also had paired, curved, whiskerlike appendages, requiring complex musculature to move them and the operculum. The Hyolithida were probably deposit feeders living in shallow water, and accordingly were tentaculate. A reconstruction of the soft parts of this sedentary organism is given — a shallow mantle cavity on the dorsal side, anterior tentacles, a long intestine, and a reduced ventral foot. Except for the more complex musculature associated with an elaborate operculum, Orthothecida are judged to have had a similar anatomy.     

Identification of net‐winged beetle larvae (Coleoptera: Lycidae) using three mtDNA fragments: a comparison of their utility

Abstract We investigated the effectiveness of short mitochondrial DNA fragments for the identification of lycid larvae. The rrnL, cox1 and nad5 mtDNA sequences from 17 specimens of immature stages of Lycidae and Lampyridae were combined with a previously published dataset of homologous fragments representing all major lineages of Lycidae and outgroups. Their relationships were analysed under parsimony criteria. We demonstrate that high‐density profiles are necessary for accurate identification of unknown samples to generic and tribal levels and that a multilocus approach is critical for obtaining reliable results. Although widely used, the cox1 mtDNA fragment showed the worst performance for identification at genus level when the query species was not present in the library. Stronger support for deeper branches came from rrnL mtDNA. The neotenic female larvae and male adult stages of Platerodrilus sp. and Macrolibnetis depressus Pic, 1938 were associated by mtDNA fragments. Based on the present identification, larvae of Dictyopterini (Dictyopterini gen. sp., Dictyoptera aurora Herbst, 1784), Sulabanus sp., Leptotrichalus sp. (Metriorrhynchini) and Macrolibnetis depressus Pic, 1938 (Platerodrilini) are described for the first time. Further species of Platycis Thomson, 1859, Plateros Bourgeois, 1979, Macrolycus Waterhouse, 1878, Cautires Waterhouse, 1879 and Lyponia Waterhouse, 1878 are identified by morphology and molecular markers. The data on larval morphology and their usefulness for classification are discussed.     

Patterns of allozyme variation in western Eurasian Fagus

Fagus sylvatica L. is one of the most widespread broad‐leaved trees in the temperate forests of the northern hemisphere. In addition to two subspecies, F. sylvatica ssp. sylvatica in Europe and F. sylvatica ssp. orientalis in south‐western Asia, two further taxa were described: F. moesiaca (Maly) Czeczott in the south‐western Balkans and F. taurica Popl. in Crimea. The opinions about the number and ranks of taxa within this complex are highly controversial. To assess the degree of genetic differentiation among them, and to reveal geographical patterns of genetic diversity and their relationships to history and biogeography of beech populations, genetic variation at 12 allozyme loci was studied in 279 populations in western Eurasia. A Bayesian analysis of population structure revealed the existence of two clusters, which fairly well coincided with F. sylvatica ssp. sylvatica and F. sylvatica ssp. orientalis, whereby the populations from the south‐western Balkans and Crimea contained a mixture of these two gene pools. On the other hand, a neighbour‐joining tree based on pairwise F_ST failed to separate the subspecies into well‐defined distinct clades. Populations of F. sylvatica ssp. orientalis proved to be incomparably more differentiated than ssp. sylvatica (F_ST = 0.157 and 0.032, respectively). Asian populations also showed higher levels of allelic richness both on population and taxon levels than the European ones (the number of alleles after rarefaction was 3.40 and 4.27 in F. sylvatica ssp. sylvatica and ssp. orientalis, respectively). This indicates that the gene pool of F. sylvatica ssp. orientalis has not been depleted by reduced population sizes during the Pleistocene glaciations, as is the case of F. sylvatica ssp. sylvatica. Genetic similarities between isolated regional populations are explained by shared ancestral polymorphisms and/or range overlaps with subsequent hybridization in the past. © 2007 The Linnean Society of London, Botanical Journal of the Linnean Society, 2007, 154 , 165–174.     

Longitudinal zonation of macroinvertebrates in an Ecuadorian glacier‐fed stream: do tropical glacial systems fit the temperate model?

1. The ecology of glacier‐fed streams at temperate latitudes has been intensely studied in recent years, leading to the development of a well‐validated conceptual model on the longitudinal distribution of macroinvertebrate communities downstream of the glacier margin (Freshwater Biology, 2001a; 46 , 1833). However, to our knowledge, the ecology of tropical glacier‐fed streams has not yet been studied. 2. We sampled benthic macroinvertebrates and measured environmental variables at nine sites between 4730 and 4225 m altitude along a 4.3 km stretch of a glacier‐fed stream 40 km south of the equator in the Ecuadorian Andes. Our goal was to study the longitudinal distribution of the fauna in relation to environmental factors and to compare this with the conceptual model based on temperate–arctic glacier‐fed streams. 3. Total density of invertebrates differed considerably at the two highest altitude sites; 4600 m^?2 at a pro‐glacial lake outlet and only 4 m^?2 at a site originating directly from the glacier snout. Otherwise, there was a downstream decrease in density to about 825 m^?2 at the three lowest sites. Taxon richness increased with distance from the glacier, very similar to the pattern predicted. A total of 28 taxa were collected; two at the glacier snout, seven at the nearby pro‐glacial lake outlet, 13 at site 2 (<400 m from the glacier) and 20 at the lowest sites. 4. The numerical percentage of Chironomidae (Diptera) decreased downstream from 100 to 44%. The subfamily Podonominae was numerous at the highest sites but became much less important further downstream. The Orthocladiinae were important both in numbers and species at all sites, while Diamesinae were numerous only in the middle of the reach studied and were completely absent from the upper three sites. The limited importance of the Diamesinae, and its replacement by Podonominae, is different from the pattern typically observed in north‐temperate glacier‐fed streams. This could be because of the fact that the genus Diamesa is missing from the Neotropics. 5. Stream temperature and channel stability explained most of the variability in faunal composition and richness, supporting the model. Stability increased systematically downstream while temperature did not. Surprisingly, no classical kryal zone (T_max < 4 °C) was found, as even the site closest to the glacier snout (50 m) had a T_max of 15 °C and no site had T_max < 8 °C. We propose that this might be a general feature of equatorial glacial streams.     

Spatial variability in macroinvertebrate assemblages along and among neighbouring equatorial glacier‐fed streams

1. During the past two decades, understanding of the structure and function of glacier‐fed stream ecosystems at temperate latitudes has increased substantially. In contrast, information on their tropical counterparts is very limited. We studied three neighbouring glacier‐fed streams in the tropical Andes of Ecuador. Our main goals were (i) to determine overall longitudinal patterns in density, taxon richness and the composition of macroinvertebrate assemblages and driving factors in equatorial glacial streams and (ii) to examine variability among replicate streams in faunal metrics and assemblages, and stream‐specific effects of supposed environmental key factors. 2. We measured four geographical and 17 environmental factors and collected five Surber samples (500 cm²) of macroinvertebrates at each of nine sites, three sites along three streams. The streams were located 1–5 km apart. In each stream, the three sites were placed at comparable distances from the glacier and were grouped as ‘upper’ (50–200 m), ‘middle’ (1.5 km) and ‘lower’ sites (3.5–5.6 km). 3. In total, 2200 individuals (64% chironomids) were collected and 47 taxa (30 dipterans, 18 of these Chironomidae) identified. Density ranged from 176 to 372 ind. m^?2, and the number of taxa ranged from 2 to 6 at the upper sites and 868–3044 ind. m^?2 and 21–27 taxa at the lower sites. Density, number of taxa, rarefied richness and axis‐1 coordinates from a MDS ordination increased logarithmically with distance from the glacier. These faunal metrics were equally related to altitude and glacier per cent of catchment and correlated with maximum conductivity, mean temperature, mean daily maximum temperature and a channel stability index. As expected, the mean difference in distance decay in similarity was higher at the upper (47% km^?1) than at the lower reaches (20% km^?1) of the streams. 4. The number of taxa varied among sites within the upper and middle groups, but not among the lower sites. In contrast, but in accordance with our expectation, assemblage composition did not differ among upper sites but did so at middle and lower sites, following a supposed decrease in environmental harshness along the streams. Relationships between faunal metrics and the four environmental variables mean temperature, the stability index, chlorophyll a and coarse particulate organic matter also varied among the three streams. Generalised linear model analyses revealed that temperature interacted with stream on macroinvertebrate density, while chlorophyll a had a significant effect on the number of taxa in interaction with stream and stability. 5. The basic predictions of the Milner et al. (2001a) , model regarding longitudinal faunal patterns and temperature and stability as main driving factors were met by our three replicate equatorial glacial streams. Qualitative departures from the model were mainly because of zoogeographical differences. We demonstrated that variability in assemblages between comparable sites in closely situated streams was considerable, and the effect of key environmental factors varied among streams and interacted with other factors. Quantifying spatial variation in benthic assemblages may help us foresee possible consequences for biodiversity as a result of glacial retreat.