Biomimetic properties of simulated protomembranes

Origins of Life and Evolution of Biospheres -     

At least two nuclear gene products are specifically required for translation of a single yeast mitochondrial mRNA.

Mitochondrial translation of the oxi2 mRNA, encoding yeast cytochrome c oxidase subunit III (coxIII), has previously been shown to specifically require the mitochondrially located protein product of the nuclear gene PET494. We show here that this specific translational activation involves at least one other newly identified gene termed PET54. Mutations in PET54 cause an absence of the coxIII protein despite the presence of normal levels of its mRNA. pet494 mutations are known to be suppressible by mitochondrial gene rearrangements that replace the normal 5'-untranslated leader of the oxi2 mRNA with the leaders of other mitochondrial mRNAs. In this study we show that pet54, pet494 double mutants are suppressed by the same mitochondrial gene rearrangements, showing that the PET54 product is specifically required, in addition to the PET494 protein, for translation of the oxi2 mRNA. Since, as we show here, PET54 is not an activator of PET494 gene expression, our results suggest that the products of both of these genes may act together to stimulate coxIII translation.     

Structural forms, stabilities and transitions in double-helical poly(dG-dC) as a function of hydration and NaCl content. An infrared spectroscopic study.

The poly(dG-dC) helical duplex forms a modified, B-family structure (B*) at very high hydration and a normal B structure at slightly lower hydration. The B* structure is slightly different in sugar-phosphate and base-stacking conformations than the B structure. Increasing the hydration or decreasing the NaCl content stabilizes B* with respect to B. Poly(dG-dC) forms the Z structure at low NaCl contents when the hydration is sufficiently reduced. At moderate NaCl content, the B to Z transition is sharp and cooperative for hydration with D2O. Hydration with H2O broadens the transition which occurs at lower hydration. This suggests that hydrogen bonding is stronger in the Z structure and helps stabilize Z over B. IR spectra may be used to quantitatively estimate the fractions of B and Z structures present in a sample. Some new indicator bands are described.     

Stepwise mass extinctions and impact events: Late Eocene to early Oligocene

Species ranges and relative abundances of dominant planktonic foraminifers of eight late Eocene to early Oligocene deep-sea sections are discussed to determine the nature and magnitude of extinctions and to investigate a possible cause-effect relationship between impact events and mass extinctions.Late Eocene extinctions are neither catastrophic nor mass extinctions, but occur stepwise over a period of about 1–2 million years. Four stepwise extinctions are identified at the middle/late Eocene boundary, the upperGlobigerapsis semiinvoluta zone, theG. semiinvoluta/Globorotalia cerroazulensis zone boundary and at the Eocene/Oligocene boundary. Each stepwise extinction event represents a time of accelerated faunal turnover characterized by generally less than 15% species extinct and in itself is not a significant extinction event. Relative species abundance changes at each stepwise extinction event, however, indicate a turnover involving > 60% of the population implying major environmental changes.There microtektite horizons are present in late Eocene sediments; one in the upperG. semiinvoluta zone (38.2 Ma) and two closely spaced layers only a few thousand years apart in the lower part of theGloborotalia cerroazulensis zone (37.2 Ma). Each of the three impact events appears to have had some effect on microplankton communities. However, the overriding factor that led to the stepwise mass extinctions may have been the result of multiple causes as there is no evidence of impacts associated with the step preceding, or the step following the deposition of the presently known microtektite horizons.     

Surface tension gradients: feasible model for gliding motility of Myxococcus xanthus.

We propose that surface tension is the driving force for the gliding motility of Myxococcus xanthus. Our model requires that the cell be able to excrete surfactant in a polar and reversible fashion. We present calculations that (i) estimate the surface tension difference across a cell necessary to move the cell at the observed rate, which is less than 10(-5) dyn/cm, an extremely small value; (ii) estimate the rate of surfactant excretion necessary to produce the required surface tension difference, a rate that we conclude to be metabolically reasonable; (iii) predict the behavior of cells moving in close apposition to each other, and show that the model is consistent with observed behavior; and (iv) predict the behavior of cells moving in dense swarms. In an accompanying paper we present experimental evidence to support the surface tension model.