Functional diversity of the phosphoglucomutase superfamily: structural implications.

Three-dimensional structural models of three members of the phosphoglucomutase (PGM) superfamily, parafusin, phosphoglucomutase-related protein and sarcoplasmic reticulum phosphoglucomutase, were constructed by homology modeling based on the known crystal structure of rabbit muscle phosphoglucomutase. Parafusin, phosphoglucomutase-related protein and sarcoplasmic reticulum phosphoglucomutase each have 50% or more identity with rabbit muscle phosphoglucomutase at the amino acid level and all are reported to exhibit no or minor phosphoglucomutase activity. There are four major insertions and two deletions in the parafusin sequence relative to PGM, all of which are located in surface-exposed loops connecting secondary structural elements. The remaining amino acid substitutions are distributed throughout the sequence and are not predicted to alter the polypeptide fold. Parafusin contains a putative protein kinase C site located on a surface loop in domain II that is not present in the homologs. Although the general domain structure and the active site of rabbit muscle phosphoglucomutase are preserved in the model of phosphoglucomutase-related protein, a major structural difference is likely to occur in domain 1 due to the absence of 55 amino acid residues in PGM-RP. This deletion predicts the loss of three alpha-helices and one beta-strand from an anti-parallel beta-sheet in this domain as compared with the rabbit muscle phosphoglucomutase.     

Nonsurgical repair of perinasal skin defects

Immediate reconstruction of full-thickness skin defects after cancer surgery is a commonly accepted surgical principle used to preserve function and minimize cosmetic deformity. Healing by secondary intention, however, offers the advantages of optimal cancer surveillance, simplified wound management, and avoidance of reconstructive procedures with their associated costs and potential complications. Accurate prediction of the course of wound healing, and thereby the final functional and cosmetic result, would allow a rational approach to selection of patients for surgical or nonsurgical repair. We observed 282 patients with full-thickness perinasal (glabella, medial canthus, dorsum, sidewall, tip, ala, philtrum, alar base, and nasolabial fold) skin defects after Mohs' surgery and documented a variety of parameters affecting wound healing, including location, depth, and size of the wound. Patients were examined at intervals, and a final determination regarding cosmesis and function was made at 6 months or later. We conclude that the most important considerations in predicting the final functional and cosmetic result include location by subunit, followed by size and depth of the wound.     

Carbon and oxygen isotope geochemistry of live (stained) benthic foraminifera from the Aleutian Margin and the Southern Australian Margin

Comparisons of ambient bottom-water geochemistry and stable isotopic values of the tests of living (stained) calcareous benthic foraminifera from the North Pacific (on the Aleutian Margin, water depth 1988 m) and Murray Canyons group in the Southern Indian Ocean (Australian Margin, water depths 2476 m and 1634 m) provide modern environmental analogs to calibrate paleoenvironmental assessments. Consistent with the hypothesis that microhabitat preferences influence foraminiferal isotopic values, benthic foraminifera from both margins were depleted in ¹³C with respect to bottom-water dissolved inorganic carbon (DIC). The carbon isotope values of deep infaunal foraminifera (Chilostomella oolina, Globobulimina pacifica) showed greater differences from estimates of those of DIC than shallow benthic foraminifera (Bulimina mexicana, Bolivinita quadrilatera, Pullenia bulloides). This study provides new isotopic and ecological information for B. quadrilatera. The mean Δδ¹³C value, defined as foraminiferal δ¹³C values minus estimated ambient δ¹³C values from the Aleutian Margin, is 0.97‰ higher for G. pacifica than the mean from the Murray Canyon. This difference may result either from genetic or biological differences between the populations or from differences in environmental isotopic influences (such as pore water differences) that were not accounted for in the equilibrium calculations. These analyses provide calibration information for the evaluation of bottom water conditions and circulation patterns of ancient oceans based on fossil foraminiferal geochemistry.