Amniotes through major biological crises: faunal turnover among Parareptiles and the end‐Permian mass extinction

Abstract: The Parareptilia are a small but ecologically and morphologically diverse clade of Permian and Triassic crown amniotes generally considered to be phylogenetically more proximal to eureptiles (diapsids and their kin) than to synapsids (mammals and their kin). A recent supertree provides impetus for an analysis of parareptile diversity through time and for examining the influence of the end‐Permian mass extinction on the clade’s origination and extinction rates. Phylogeny‐corrected measures of diversity have a significant impact on both rates and the distribution of origination and extinction intensities. Time calibration generally results in a closer correspondence between origination and extinction rate values than in the case of no time correction. Near the end‐Permian event, extinction levels are not significantly higher than origination levels, particularly when time calibration is introduced. Finally, regardless of time calibration and/or phylogenetic correction, the distribution of rates does not differ significantly from unimodal. The curves of rate values are discussed in the light of the numbers and distributions of both range extensions and ghost lineages. The disjoint time distributions of major parareptile clades (e.g. procolophonoids and nycteroleterids‐pareiasaurs) are mostly responsible for the occurrence of long‐range extensions throughout the Permian. Available data are not consistent with a model of sudden decline at the end‐Permian but rather suggest a rapid alternation of originations and extinctions in a number of parareptile groups, both before and after the Permian/Triassic boundary.     

The blackflies (Diptera: Simuliidae) of Bioko (Republic of Equatorial Guinea) and the Gulf of Guinea with a description of the larvae of the 'Pomeroy' form of Simulium cervicornutum

Abstract.  Like many other organisms, Simuliidae often show a high degree of endemism on oceanic islands, and the Gulf of Guinea, including its islands, is a region of general biogeographical interest in view of the uniqueness of its flora and fauna. This paper presents a comprehensive review of the Simuliidae in the region, and is the first faunistic record of blackflies from Bioko. Simuliidae (larvae, pupae and neonate adults) were collected from Bioko and from around Mount Cameroon and compared with previous findings from Mount Cameroon, Príncipe and São Tomé. Twenty-seven species are known from the region. Twenty-five species have been recorded around Mount Cameroon, eight species on Bioko, three species on São Tomé and one species on Príncipe. Two taxonomic 'forms' (one on Bioko alone, and one on both Bioko and around Mount Cameroon) and one species (found only on São Tomé) are endemic to the region. A study of the variation in the morphology of Simulium cervicornutum revealed two morphotypes, one from Bioko and around Mount Cameroon and the other from the rest of Africa. The speciation and biogeography of the Simuliidae in the Gulf of Guinea are discussed.     

GENETIC STRUCTURE OF THE WESTERN NORTH AMERICAN AQUATIC GASTROPOD GENUS TAYLORCONCHA AND DESCRIPTION OF A SECOND SPECIES

The Bliss Rapids Snail (Taylorconcha serpenticola) is a threatenedspecies that ranges along a short reach of the middle SnakeRiver in southern Idaho. Additional Taylorconcha populationsof uncertain taxonomic status have recently been discoveredin other portions of the Snake River basin (Owyhee River, lowerSnake River). We investigated the phylogenetic relationshipsand population structure of these snails, together with twooutgroups, using cytochrome c oxidase subunit I (COI) of mitochondrialDNA and the first internal transcribed spacer region betweenthe 18S and 5.8S ribosomal DNA. These data show no sharing ofhaplotypes or genotypes among T. serpenticola and the Owyhee-LowerSnake populations, with both depicted as monophyletic unitswithin the Taylorconcha clade. Both of these datasets and morphologicalevidence suggest that the Owyhee-Lower Snake populations area distinct species, which we describe herein (T. insperata newspecies). Application of an available COI molecular clock suggeststhat Taylorconcha arose in the late Miocene, when ancestralSnake River drainage was impounded in an extensive lacustrinesystem (‘Lake Idaho’) in western Idaho. The shallowpopulation structuring of T. insperata suggests that the lowerSnake River was only recently colonized subsequent to incisionof Hells Canyon, draining of Lake Idaho, and development ofa through-going river in the late Neogene. The absence of significantgenetic structure in T. serpenticola, which is attributed tothe unstable course and flow regime of the middle Snake Riverduring the Quaternary, suggests that this species can be treatedas a single management unit. (Received 14 July 2005; accepted 23 September 2005)     

Frequency of fault bars in feathers of birds and susceptibility to predation

Fault bars are transparent bands in the feathers of birds produced under stressful and adverse conditions. The frequency of feathers with fault bars is highly heterogeneous among species. We predicted that prey had a higher frequency of fault bars than individuals from the general population, and that a high susceptibility to predation would be associated with a low frequency of fault bars among species of birds because such species would suffer particularly high costs of producing fault bars. The frequency of fault bars in prey was almost three-fold higher than in the general population, based on a database on the frequency of fault bars and susceptibility to predation by the goshawk Accipiter gentilis L., implying intense natural selection against fault bars. A high susceptibility to predation by the sparrowhawk Accipiter nisus L. and the goshawk, relative to what would be expected from their abundance, was associated with a low frequency of fault bars across species, with long distance migration also being negatively associated with frequency of fault bars. Feathers with fault bars were more likely to break than feathers without fault bars, thereby potentially affecting the flight ability of individuals. These findings are consistent with the hypothesis that susceptibility to factors that cause production of fault bars can be modified by natural selection, as illustrated by the impact of predation on the frequency of fault bars.  © 2009 The Linnean Society of London, Biological Journal of the Linnean Society , 2009, 97 , 334–345.     

Fate of soil‐applied black carbon: downward migration,leaching and soil respiration

Black carbon (BC) is an important pool of the global C cycle, because it cycles much more slowly than others and may even be managed for C sequestration. Using stable isotope techniques, we investigated the fate of BC applied to a savanna Oxisol in Colombia at rates of 0, 11.6, 23.2 and 116.1 t BC ha^?1, as well as its effect on non‐BC soil organic C. During the rainy seasons of 2005 and 2006, soil respiration was measured using soda lime traps, particulate and dissolved organic C (POC and DOC) moving by saturated flow was sampled continuously at 0.15 and 0.3 m, and soil was sampled to 2.0 m. Black C was found below the application depth of 0–0.1 m in the 0.15–0.3 m depth interval, with migration rates of 52.4±14.5, 51.8±18.5 and 378.7±196.9 kg C ha^?1 yr^?1 (±SE) where 11.6, 23.2 and 116.1 t BC ha^?1, respectively, had been applied. Over 2 years after application, 2.2% of BC applied at 23.2 t BC ha^?1 was lost by respiration, and an even smaller fraction of 1% was mobilized by percolating water. Carbon from BC moved to a greater extent as DOC than POC. The largest flux of BC from the field (20–53% of applied BC) was not accounted for by our measurements and is assumed to have occurred by surface runoff during intense rain events. Black C caused a 189% increase in aboveground biomass production measured 5 months after application (2.4–4.5 t additional dry biomass ha^?1 where BC was applied), and this resulted in greater amounts of non‐BC being respired, leached and found in soil for the duration of the experiment. These increases can be quantitatively explained by estimates of greater belowground net primary productivity with BC addition.     

Induction of Group-specific Interspecies Antibody in a Cat by Immunization with Disrupted Feline Leukaemia Virus

“ALL mice, cats and virtually all chickens seem to be completely refractory to developing antibody to the group-specific, gs, antigens characteristic of the RNA tumour viruses of their own species.”¹ This is explained on the basis of an immune tolerance induced in early embryonic life by the expression of these antigens before the development of immune competence. Avian group-specific (gs) antibody has been demonstrated in the sera of immunized chickens by the immunodiffusion (Ouchterlony)² and complement fixation inhibition³ tests. This report is to record the production of gs antibody in a cat which had been immunized with gs antigen from disrupted feline leukaemia virus (FeLV).