Airborne minerals and related aerosol particles: Effects on climate and the environment

Aerosol particles are ubiquitous in the troposphere and exert an important influence on global climate and the environment. They affect climate through scattering, transmission, and absorption of radiation as well as by acting as nuclei for cloud formation. A significant fraction of the aerosol particle burden consists of minerals, and most of the remainder— whether natural or anthropogenic—consists of materials that can be studied by the same methods as are used for fine-grained minerals. Our emphasis is on the study and character of the individual particles. Sulfate particles are the main cooling agents among aerosols; we found that in the remote oceanic atmosphere a significant fraction is aggregated with soot, a material that can diminish the cooling effect of sulfate. Our results suggest oxidization of SO2 may have occurred on soot surfaces, implying that even in the remote marine troposphere soot provided nuclei for heterogeneous sulfate formation. Sea salt is the dominant aerosol species (by mass) above the oceans. In addition to being important light scatterers and contributors to cloud condensation nuclei, sea-salt particles also provide large surface areas for heterogeneous atmospheric reactions. Minerals comprise the dominant mass fraction of the atmospheric aerosol burden. As all geologists know, they are a highly heterogeneous mixture. However, among atmospheric scientists they are commonly treated as a fairly uniform group, and one whose interaction with radiation is widely assumed to be unpredictable. Given their abundances, large total surface areas, and reactivities, their role in influencing climate will require increased attention as climate models are refined.

Detecting the conformational change of transmembrane signaling in a bacterial chemoreceptor by measuring effects on disulfide cross-linking in vivo.

Transmembrane signaling by bacterial chemoreceptors is thought to involve relative movement among the four transmembrane helices of the homodimer. We assayed that movement by measuring effects of ligand occupancy on rates of oxidative cross-linking between cysteines introduced into neighboring helices of the transmembrane domain of chemoreceptor Trg from Escherichia coli. Measurements were done on chemoreceptors in their native environment, intact cells that were motile and chemotactically responsive. Receptor occupancy did not appear to cause drastic rearrangement of the four-helix structure since, among 67 cysteine pairs tested, the same 19 exhibited oxidative cross-linking in the presence or absence of saturating chemoattractant. However, occupancy did cause subtle changes that were detected as effects on rates of cross-linking. Among the seven disulfides appropriate for measurements of initial rates of formation, ligand occupancy had significant and different effects on all three cross-links that connected the two helices within a subunit but had minimal effects on the four that spanned the packing interface between subunits. This constitutes direct evidence that the conformational change of transmembrane signaling involves significant movement within a subunit and minimal movement between subunits, a pattern deduced from several previous studies and now documented directly. Among possible modes of movement between the two helices of a subunit, axial sliding of one helix relative to the other was the conformational change that best accounted for the observed effects on cross-linking.