Control of phyllotaxy by the cytokinin-inducible response regulator homologue ABPHYL1

Phyllotaxy describes the geometric pattern of leaves and flowers, and has intrigued botanists and mathematicians for centuries. How these patterns are initiated is poorly understood, and this is partly due to the paucity of mutants. Signalling by the plant hormone auxin appears to determine the site of leaf initiation; however, this observation does not explain how distinct patterns of phyllotaxy are initiated. abphyl1 (abph1) mutants of maize initiate leaves in a decussate pattern (that is, paired at 180 degrees), in contrast to the alternating or distichous phyllotaxy observed in wild-type maize and other grasses. Here we show that ABPH1 is homologous to two-component response regulators and is induced by the plant hormone cytokinin. ABPH1 is expressed in the embryonic shoot apical meristem, and its spatial expression pattern changes rapidly with cytokinin treatment. We propose that ABPH1 controls phyllotactic patterning by negatively regulating the cytokinin-induced expansion of the shoot meristem, thereby limiting the space available for primordium initiation at the apex.     

Contrasting origins of the upper mantle revealed by hafnium and lead isotopes from the Southeast Indian Ridge

The origin of the isotopic signature of Indian mid-ocean ridge basalts has remained enigmatic, because the geochemical composition of these basalts is consistent either with pollution from recycled, ancient altered oceanic crust and sediments, or with ancient continental crust or lithosphere. The radiogenic isotopic signature may therefore be the result of contamination of the upper mantle by plumes containing recycled altered ancient oceanic crust and sediments, detachment and dispersal of continental material into the shallow mantle during rifting and breakup of Gondwana, or contamination of the upper mantle by ancient subduction processes. The identification of a process operating on a scale large enough to affect major portions of the Indian mid-ocean ridge basalt source region has been a long-standing problem. Here we present hafnium and lead isotope data from across the Indian-Pacific mantle boundary at the Australian-Antarctic discordance region of the Southeast Indian Ridge, which demonstrate that the Pacific and Indian upper mantle basalt source domains were each affected by different mechanisms. We infer that the Indian upper-mantle isotope signature in this region is affected mainly by lower continental crust entrained during Gondwana rifting, whereas the isotope signature of the Pacific upper mantle is influenced predominantly by ocean floor subduction-related processes.     

Identification of autonomous IAP LTR retrotransposons mobile in mammalian cells

Mammalian genomes contain two main classes of retrotransposons, the well-characterized long and short interspersed nuclear elements, which account for approximately 30% of the genome, and the long terminal repeat (LTR) retrotransposons, which resemble the proviral integrated form of retroviruses, except for the absence of an envelope gene in some cases. Genetic studies confirmed mobility of the latter class of elements in mice, with a high proportion of phenotypic mutations consequent to transposition of the intracisternal A particle (IAP) family of LTR retrotransposons. Using the mouse genome sequence and an efficient ex vivo retrotransposition assay, we identified functional, master IAP copies that encode all the enzymatic and structural proteins necessary for their autonomous transposition in heterologous cells. By introducing mutations, we found that the three genes gag, prt and pol are all required for retrotransposition and identified the IAP gene products by electron microscopy in the form of intracellular A-type particles in the transfected cells. These prototypic elements, devoid of an envelope gene, are the first LTR retrotransposons autonomous for transposition to be identified in mammals. Their high rates of retrotransposition indicate that they are potent insertional mutagens that could serve as safe (noninfectious) genetic tools in a large panel of cells.     

Spectroscopic study of the disulfide bond in oxidized glutathione

Summary Raman and circular dichroism spectra are used for obtaining structural information on the disulfide bridge in oxidized glutathione. Quantitative estimates of dihedral angles and bond angles are proposed.     

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.     

Coulomb blockade and the Kondo effect in single-atom transistors

Using molecules as electronic components is a powerful new direction in the science and technology of nanometre-scale systems. Experiments to date have examined a multitude of molecules conducting in parallel, or, in some cases, transport through single molecules. The latter includes molecules probed in a two-terminal geometry using mechanically controlled break junctions or scanning probes as well as three-terminal single-molecule transistors made from carbon nanotubes, C(60) molecules, and conjugated molecules diluted in a less-conducting molecular layer. The ultimate limit would be a device where electrons hop on to, and off from, a single atom between two contacts. Here we describe transistors incorporating a transition-metal complex designed so that electron transport occurs through well-defined charge states of a single atom. We examine two related molecules containing a Co ion bonded to polypyridyl ligands, attached to insulating tethers of different lengths. Changing the length of the insulating tether alters the coupling of the ion to the electrodes, enabling the fabrication of devices that exhibit either single-electron phenomena, such as Coulomb blockade, or the Kondo effect.     

Paxillin binds schwannomin and regulates its density-dependent localization and effect on cell morphology

Neurofibromatosis type 2 is an autosomal dominant disorder characterized by tumors, predominantly schwannomas, in the nervous system. It is caused by mutations in the gene NF2, encoding the growth regulator schwannomin (also known as merlin). Mutations occur throughout the 17-exon gene, with most resulting in protein truncation and undetectable amounts of schwannomin protein. Pathogenic mutations that result in production of defective schwannomin include in-frame deletions of exon 2 and three independent missense mutations within this same exon. Mice with conditional deletion of exon 2 in Schwann cells develop schwannomas, which confirms the crucial nature of exon 2 for growth control. Here we report that the molecular adaptor paxillin binds directly to schwannomin at residues 50-70, which are encoded by exon 2. This interaction mediates the membrane localization of schwannomin to the plasma membrane, where it associates with beta 1 integrin and erbB2. It defines a pathogenic mechanism for the development of NF2 in humans with mutations in exon 2 of NF2.     

Mantle thermal pulses below the Mid-Atlantic Ridge and temporal variations in the formation of oceanic lithosphere

A 20-Myr record of creation of oceanic lithosphere is exposed along a segment of the central Mid-Atlantic Ridge on an uplifted sliver of lithosphere. The degree of melting of the mantle that is upwelling below the ridge, estimated from the chemistry of the exposed mantle rocks, as well as crustal thickness inferred from gravity measurements, show oscillations of approximately 3-4 Myr superimposed on a longer-term steady increase with time. The time lag between oscillations of mantle melting and crustal thickness indicates that the mantle is upwelling at an average rate of approximately 25 mm x yr(-1), but this appears to vary through time. Slow-spreading lithosphere seems to form through dynamic pulses of mantle upwelling and melting, leading not only to along-axis segmentation but also to across-axis structural variability. Also, the central Mid-Atlantic Ridge appears to have become steadily hotter over the past 20 Myr, possibly owing to north-south mantle flow.