A GFP-MAP4 reporter gene for visualizing cortical microtubule rearrangements in living epidermal cells

Microtubules influence morphogenesis by forming distinct geometrical arrays in the cell cortex, which in turn affect the deposition of cellulose microfibrils. Although many chemical and physical factors affect microtubule orientation, it is unclear how cortical microtubules in elongating cells maintain their ordered transverse arrays and how they reorganize into new geometries. To visualize these reorientations in living cells, we constructed a microtubule reporter gene by fusing the microtubule binding domain of the mammalian microtubule-associated protein 4 (MAP4) gene with the green fluorescent protein (GFP) gene, and transient expression of the recombinant protein in epidermal cells of fava bean was induced. The reporter protein decorates microtubules in vivo and binds to microtubules in vitro. Confocal microscopy and time-course analysis of labeled cortical arrays along the outer epidermal wall revealed the lengthening, shortening, and movement of microtubules; localized microtubule reorientations; and global microtubule reorganizations. The global microtubule orientation in some cells fluctuates about the transverse axis and may be a result of a cyclic self-correcting mechanism to maintain a net transverse orientation during cellular elongation.     

Synthesis of eicosa-2-trans-8,11,14-all cis-tetraenoic acid-3-14C and DL-3-hydroxy eicosa-8,11,14-all cis-trienoic acid-3-14C

A general procedure for the synthesis of 2-trans polyenoic fatty acids and of dl-3-hydroxypolyenoic acids is described. The 2-trans acids are prepared by LiAlH(4) reduction of a suitable polyenoic fatty acid ester to the alcohol, formation of the tosylate, oxidation to the aldehyde, and Doebner condensation of the latter with malonic acid. The 3-hydroxy acids are obtained by reaction of the acyl chloride of a suitable polyenoic acid with the sodium enolate of methyl acetoacetate and sodium methoxide to give the 3-keto ester, the keto group of which is reduced with sodium borohydride to the alcohol. These procedures were applied to the synthesis of eicosa-2-trans-8, 11, 14-all cis-tetraenoic acid-3-(14)C and DL-3-hydroxy eicosa-8, 11, 14-trienoic acid-3-(14)C.     

Synthesis, transport, and processing of apolipoproteins of high density lipoproteins

Cell biology methods have greatly influenced the elucidation of the biosynthetic pathways of apolipoproteins. In vitro and tissue culture systems allow the study, to a large extent, of the process of synthesis, intracellular processing, secretion, and extracellular processing of the major high density lipoprotein apoproteins apoA-I and A-II and also of a minor component, apoA-IV. Whereas the latter apoprotein is equipped only with a signal sequence, the primary translation products of apoA-I and apoA-II carry N-terminal extensions of preprosequence of 24 amino acids for apoA-I and 23 amino acid residues for apoA-II. The pro-form of apoA-I characterized by a hexapeptide extension is completely stable intracellularly and is secreted as such. The pro-form is further processed by a serum protease specific for an unusual -Gln-Gln-Asp-Glu-sequence site. Pro-apoA-II, a pentapeptide sequence, is partially processed intracellularly to its mature form and secreted together with the residual pro-form. The cleavage site of pro-apoA-II is characterized by two basic amino acid residues Arg-Arg, present also in other known pro-proteins. The biological function of the N-terminal pro-sequences and details of their final processing by the serum protease(s) have yet to be established.     

Debris-flow activity along a torrent in the Swiss Alps: Minimum frequency of events and implications for forest dynamics

This study reports on a tree-ring-based reconstruction of geomorphic activity and illustrates impacts of such processes on tree germination along a debris-flow torrent in the Swiss Alps. Analysis included the identification of growth disturbances and the assessment of germination dates for 28 trees along the channel of the Geisstriftbach torrent (Valais, Swiss Alps). Provided that recolonizing trees indicate the minimum time elapsed since the last deposition, germination dates suggest that a devastating debris-flow event in the 1880s had cleared the surface and scoured the currently active channel. This interpretation is supported by two topographic maps showing a dislocation of the channel. Analyzing the age structure of trees along the channel in more detail, we observe higher tree ages with increasing distance from the cone apex. In addition, dendrogeomorphic methods allowed for the reconstruction of 13 debris-flow events between AD 1913 and 2006. In combination with geomorphic mapping, the spatial distribution of trees affected by individual events was assessed and a minimum frequency of previous debris-flow events reconstructed. Although the present study was based on a limited set of tree-ring records, it illustrates that tree-ring analysis in combination with cartographic methods holds much promise for dating minimum ages of surfaces cleared by destructive events as well as for determining the spatio-temporal impacts of past debris-flow activity.