A high-pressure form of sulfuric acid monohydrate as determined by X-ray and neutron diffraction

Two high-pressure polymorphs of sulfuric acid monohydrate (oxonium hydrogensulfate) have been obtained at ambient temperature by crystallisation at high pressure from the liquid at 1.3 GPa (form III) and by direct compression of the ambient-pressure form I first to 1.26 GPa (form II) and then to 1.72 GPa (form III). The structure of form III was solved by single crystal X-ray diffraction and this structure was used as the basis for the refinement of hydrogen positions using high-pressure neutron powder diffraction data. Form III crystallises in the orthorhombic crystal system at 1.97 GPa, and features parallel chains of hydrogensulfate ions linked by oxonium ions to form a three-dimensional hydrogen-bonded network. On further compression to 3.05 GPa, the direction of maximum compressibility is found to be along the a-axis and is associated with the shortening of a hydrogen bond between a hydrogensulfate ion and an oxonium ion. The structure of form II remains elusive although at ambient temperature it is stable (or metastable) at pressures as low as 0.42 GPa, perhaps indicating that it could be recoverable to ambient-pressure at low temperature.     

The fossil record and estimating divergence times between lineages: Maximum divergene times and the importance of reliable phylogenies

Summary Bounded estimates on divergence times between lineaes are crucial to the calculation of absolute rates of molecular evolution. Upper (minimum) bounds on divergence times are easily estimated based on earliest fossil finds. Lower (maximum) bounds are more difficult to estimate; the age of putative ancestors may be used, though in practice it is virtually impossible to distinguish ancestors from primitive sister groups, which do not, of logical necessit, consitute lower bounds on divergence times. Two relatively new approaches to estimating lower bounds directly assess the incompleteness of the fossil record. The first uses taphonomic control groups to distinguish real absences from nonpreservation, while the second, and probably more powerful, uses the quality of the fossil recored to estimate confidence intervals on the bases of stratigraphic ranges. For some groups, especially vertebrates, the inclusion or exclusion of problematic fossils can dramaticaly affect estimated lower bounds on divergence times, often swamping the uncertainties due to the incompleteness of the fossil record and/or corelation and dating errors. When datable paleogeographic events reflect ancient divisions of faunas, a lower bound on the divergence time of speices within a fauna can be established based on the geologic, rather than fossil, record. The fossil records of hominids, eutherianmammals, echinoids, and geese are used as examples.This article was presented at the C.S.E.O.L. Conferrence on DNA-DNA Hybridization and Evolution, Lake Arrowhead, California, May 11–14, 1989     

Monoclonal anti-β1-adrenergic receptor antibodies activate G protein signaling in the absence of β-arrestin recruitment

Thermostabilized G protein-coupled receptors used as antigens for in vivo immunization have resulted in the generation of functional agonistic anti-β₁-adrenergic (β₁AR) receptor monoclonal antibodies (mAbs). The focus of this study was to examine the pharmacology of these antibodies to evaluate their mechanistic activity at β₁AR. Immunization with the β₁AR stabilized receptor yielded five stable hybridoma clones, four of which expressed functional IgG, as determined in cell-based assays used to evaluate cAMP stimulation. The antibodies bind diverse epitopes associated with low nanomolar agonist activity at β₁AR, and they appeared to show some degree of biased signaling as they were inactive in an assay measuring signaling through β-arrestin. In vitro characterization also verified different antibody-receptor interactions reflecting the different epitopes on the extracellular surface of β₁AR to which the mAbs bind. The anti-β₁AR mAbs only demonstrated agonist activity when in dimeric antibody format, but not as the monomeric Fab format, suggesting that agonist activation may be mediated through promoting receptor dimerization. Finally, we have also shown that at least one of these antibodies exhibits in vivo functional activity at a therapeutically-relevant dose producing an increase in heart rate consistent with β₁AR agonism.     

The effects of ouabain on the cell mitotic cycle of mouse lymphoblasts

The inhibition of cell proliferation by ouabain has been analyzed with respect to the cell cycle. Three lines of evidence indicate that growth rate is modified by altering to different degrees the rate of progress through stages of the cell cycle: (1) a three hour lag occurs between the time of ouabain addition and the inhibition of proliferation; (2) ouabain must be present at least two to four hours prior to the mitotic burst of synchronized cells for inhibition of mitosis to occur; (3) parasynchrony is observed when cells are resuspended in ouabain-free medium after 12 hours of exposure to ouabain. Analysis of the distribution of cells in each of the stages of the cell cycle at various times during ouabain treatment reveals a progressive increase in the fraction of cells in S with a concomitant decrease in the percent of cells in each of the other stages. These results indicate that the prolongation of the cell cycle time in the presence of ouabain is due primarily to an S stage block.