Comparison of alternative methods of contact tracing in a syphilis control program

The purpose of this study was to compare the relative effectiveness of alternative methods of tracing named contacts of syphilis patients. A total of 236 contacts, identified by patients in two City of Houston Department of Health and Human Services clinics during the period April 1 through July 31, 1987, were studied. After contacts were grouped by sex and age, the proportion brought to examination by each of three methods, and by a combination of methods, was determined for each subgroup.^ The study found that 78.4% of all the 236 named sex contacts reported were located and brought to examination by the various methods of contact tracing and that 21.6% were missed. Of the 185 contacts examined, a combination of methods identified 47.7% of the cases, telephone contact, 28.6%, field contact, 16.9%, and patient referral, 11.8%.^ Of the 236 contacts reported, males made up 56.8% and females 43.2%. Contact tracing was more successful among females, with 81.4% of the 102 named female contacts, as compared to 76.1% of the 134 named male contacts being brought to examination. It is not known whether equal efforts were exerted in the follow-up of both male and female contacts. In both female and male subgroups, a combination of methods brought over 40% of sex contacts to examination. Telephone contact among females yielded 27.7% of the cases and field contact 18.1%, whereas in males, telephone contact identified 29.4% of the cases and field contact 15.7%. Patient referral was the least productive method in both sex groups, locating 12.8% in males as compared to 10.8% in females.^ On an age specific basis, a combination of methods was the most effective method in the 15-39 age group, whereas telephone contact was most effective in the 40-44 age group, and field contact in the 50-54 age group. Of all the methods of contact tracing, patient referral was the least productive in most age groups.^ Future studies of contact tracing should incorporate several important variables which were not examined in this study. ^

Major and trace element composition of melts from the Gorely volcanic center, southern Kamchatka

Melt inclusions in olivine and plagioclase phenocrysts from rocks (magnesian basalt, basaltic andesite, andesite, ignimbrite, and dacite) of various age from the Gorely volcanic center, southern Kamchatka, were studied by means of their homogenization and by analyzing the glasses in 100 melt inclusions on an electron microprobe and 24 inclusions on an ion probe. The SiO2 concentrations of the melts vary within a broad range of 45-74 wt%, as also are the concentrations of other major components. According to their SiO2, Na2O, K2O, TiO2, and P2O5 concentrations, the melts are classified into seven groups. The mafic melts (45-53 wt% SiO2) comprise the following varieties: potassic (on average 4.2 wt% K2O, 1.7 wt% Na2O, 1.0 wt% TiO2, and 0.20 wt% P2O5), sodic (3.2% Na2O, 1.1% K2O, 1.1% TiO2, and 0.40% P2O5), and titaniferous with high P2O5 concentrations (2.2% TiO2, 1.1% P2O5, 3.8% Na2O, and 3.0% K2O). The melts of intermediate composition (53-64% SiO2) also include potassic (5.6% K2O, 3.4% Na2O, 1.0% TiO2, and 0.4% P2O5) and sodic (4.3% Na2O, 2.8% K2O, 1.3% TiO2, and 0.4% P2O5) varieties. The acid melts (64-74% SiO2) are either potassic (4.5% K2O, 3.6% Na2O, 0.7% TiO2, and 0.15% P2O5) or sodic (4.5% Na2O, 3.1% K2O, 0.7% TiO2, and 0.13% P2O5). A distinctive feature of the Gorely volcanic center is the pervasive occurrence of K-rich compositions throughout the whole compositional range (silicity) of the melts. Melt inclusions of various types were sometimes found not only in a single sample but also in the same phenocrysts. The sodic and potassic types of the melts contain different Cl and F concentrations: the sodic melts are richer in Cl, whereas the potassic melts are enriched in F. We are the first to discover potassic melts with very high F concentrations (up to 2.7 wt%, 1.19 wt% on average, 17 analyses) in the Kuriles and Kamchatka. The average F concentration in the sodic melts is 0.16 wt% (37 analyses). The melts are distinguished for their richness in various groups of trace elements: LILE, REE (particularly HREE), and HFSE (except Nb). All of the melts share certain geochemical features. The concentrations of elements systematically increase from the mafic to acid melts (except only for the Sr and Eu concentrations, because of active plagioclase fractionation, and Ti, an element contained in ore minerals). The paper presents a review of literature data on volcanic rocks in the Kurile-Kamchatka area in which melt inclusions with high K2O concentrations (K2O/Na2O > 1) were found. K-rich melts are proved to be extremely widespread in the area and were found on such volcanoes as Avachinskii, Bezymyannyi, Bol'shoi Semyachek, Dikii Greben', Karymskii, Kekuknaiskii, Kudryavyi, and Shiveluch and in the Valaginskii and Tumrok Ranges.

Mapping the σ70 subunit contact sites on Escherichia coli RNA polymerase with a σ70-conjugated chemical protease

The core enzyme of Escherichia coli RNA polymerase acquires essential promoter recognition and transcription initiation activities by binding one of several σ subunits. To characterize the proximity between σ70, the major σ for transcription of the growth-related genes, and the core enzyme subunits (α2ββ′), we analyzed the protein-cutting patterns produced by a set of covalently tethered FeEDTA probes [FeBABE: Fe (S)-1-(p-bromoacetamidobenzyl)EDTA]. The probes were positioned in or near conserved regions of σ70 by using seven mutants, each carrying a single cysteine residue at position 132, 376, 396, 422, 496, 517, or 581. Each FeBABE-conjugated σ70 was bound to the core enzyme, which led to cleavage of nearby sites on the β and β′ subunits (but not α). Unlike the results of random cleavage [Greiner, D. P., Hughes, K. A., Gunasekera, A. H. & Meares, C. F. (1996) Proc. Natl. Acad. Sci. USA 93, 71–75], the cut sites from different probe-modified σ70 proteins are clustered in distinct regions of the subunits. On the β subunit, cleavage is observed in two regions, one between residues 383 and 554, including the conserved C and Rif regions; and the other between 854 and 1022, including conserved region G, regions of ppGpp sensitivity, and one of the segments forming the catalytic center of RNA polymerase. On the β′ subunit, the cleavage was identified within the sequence 228–461, including β′ conserved regions C and D (which comprise part of the catalytic center).

Protein-RNA interactions in the active center of transcription elongation complex.

By using a crosslinkable probe incorporated into the 3' terminus of nascent transcript, three sites were mapped in Escherichia coli RNA polymerase that are contacted by the RNA in the productive elongation complex. Two of these sites are in the beta subunit and one is in the beta' subunit. During elongation, the transcription complex occasionally undergoes an arrest whereby it can neither extend nor release the RNA transcript. It is demonstrated that in an arrested complex, the three contacts of RNA 3' terminus are lost, while a new beta' subunit contact becomes prominent. Thus, elongation arrest appears to involve the disengagement of the bulk of the active center from the 3' terminus of RNA and the transfer of the terminus into a new protein environment.

Center of Diagonal

Stamp on verso: Ivory Photo

Fountain. In the center of the circular driveway between the Michigan Union and the Administration Bldg.

Gift of Clas of 1956

Survey Research Center National Elections Study

l-r Philip Converse, asst. study director, Warren E. Miller research associate, Angus Campbell, dir.

Survey Research Center National Elections Study

1-r Philip Converse, asst. study director, Warren E. Miller research associate, Angus Campbell, dir.

Survey Research Center National Elections Study

l-r: Philip Converse, asst. study director, Warren E. Miller research associate, Angus Campbell, dir.

Survey Research Center National Elections Study

l-r; Philip Converse, asst. study director, Warren E. Miller research associate, Angus Campbell, dir.