Assembling and alerting scents produced by the bedbugCimex lectularius L.

Zusammenfassung Es wird gezeigt, dass die Aggregation der Bettwanzen (Cimex lectularius) durch einen von beiden Geschlechtern abgegebenen Versammlungsduft eingeleitet wird. Letzterer ist in Methylalkohol, aber nicht in Diäthyläther löslich, verdampft bei 32°C und lockt unbegattete sowie begattete Wanzen beider Geschlechter an. Die Lockreaktion ist von der Duftmenge abhängig und bleibt bei antennenlosen Wanzen aus. Die Stinkdrüsen gereizter, respektive verletzter Bettwanzen sondern Hex-2-en-1-al und Oct-2-en-1-al als Alarmduft ab, der die Zerstreuung der Wanzengruppen hervorruft.     

Histone hydrolase in tadpole liver

Résumé Le cytoplasme du foie de têtard contient une enzyme qui hydrolyse spécifiquement les protéines basiques telle que la polylysine, la protamine et les histones. L'addition d'autres protéines telles que l'albumine, la globuline et l'acide polyglutamique inhibe l'activité de cette enzyme. Les résultats obtenus montrent que cette hydrolysase extraite du foie de têtard diffère des cathépsines ou de l'histone-hydrolase du rein de rat.

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This work was supported by research grants from the National Institute of Arthritis and Metabolic Diseases No. AM 09602, National Science Foundation No. GB-22663 and from the National Cancer Institute No. CA 07174.     

Re-Os isotopic evidence for long-lived heterogeneity and equilibration processes in the Earth's upper mantle

The geochemical composition of the Earth's upper mantle is thought to reflect 4.5 billion years of melt extraction, as well as the recycling of crustal materials. The fractionation of rhenium and osmium during partial melting in the upper mantle makes the Re-Os isotopic system well suited for tracing the extraction of melt and recycling of the resulting mid-ocean-ridge basalt. Here we report osmium isotope compositions of more than 700 osmium-rich platinum-group element alloys derived from the upper mantle. The osmium isotopic data form a wide, essentially gaussian distribution, demonstrating that, with respect to Re-Os isotope systematics, the upper mantle is extremely heterogeneous. As depleted and enriched domains can apparently remain unequilibrated on a timescale of billions of years, effective equilibration seems to require high degrees of partial melting, such as occur under mid-ocean ridges or in back-arc settings, where percolating melts enhance the mobility of both osmium and rhenium. We infer that the gaussian shape of the osmium isotope distribution is the signature of a random mixing process between depleted and enriched domains, resulting from a 'plum pudding' distribution in the upper mantle, rather than from individual melt depletion events.