Comparison of thermal properties of bovine spectrin and fodrin

Thermal properties of bovine brain fodrin have been studied by circular dichroism and electron spin resonance and compared to those of bovine erythrocyte spectrin. Protein unfolding was induced either by urea or by a combination of heat and urea. The denaturation profiles of the two proteins, as measured by the changes in ellipticity at 222 nm as a function of temperature, were very similar but fodrin denaturation occurred at both higher temperatures and higher urea concentrations. In the absence of urea the thermal transition of spectrin was centered at 51 degrees C and that of fodrin at 54.5 degrees C. Proteins were also labeled with a maleimide analog spin probe. Spin-labeled fodrin showed a thermal transition similar to that of spectrin but centered at 46 degrees C instead of 42 degrees C. These findings indicated a close structural similarity of the two proteins but a slightly higher conformational stability of fodrin to both heat and urea.     

Microbial Transport, Survival, and Succession in a Sequence of Buried Sediments

Abstract Two chronosequences of unsaturated, buried loess sediments, ranging in age from <10,000 years to >1 million years, were investigated to reconstruct patterns of microbial ecological succession that have occurred since sediment burial. The relative importance of microbial transport and survival to succession was inferred from sediment ages, porewater ages, patterns of abundance (measured by direct counts, counts of culturable cells, and total phospholipid fatty acids), activities (measured by radiotracer and enzyme assays), and community composition (measured by phospholipid fatty acid patterns and Biolog substrate usage). Core samples were collected at two sites 40 km apart in the Palouse region of eastern Washington State, near the towns of Washtucna and Winona. The Washtucna site was flooded multiple times during the Pleistocene by glacial outburst floods; the Winona site elevation is above flood stage. Sediments at the Washtucna site were collected from near surface to 14.9 m depth, where the sediment age was approximately 250 ka and the porewater age was 3700 years; sample intervals at the Winona site ranged from near surface to 38 m (sediment age: approximately 1 Ma; porewater age: 1200 years). Microbial abundance and activities declined with depth at both sites; however, even the deepest, oldest sediments showed evidence of viable microorganisms. Same-age sediments had equal quantities of microorganisms, but different community types. Differences in community makeup between the two sites can be attributed to differences in groundwater recharge and paleoflooding. Estimates of the microbial community age can be constrained by porewater and sediment ages. In the shallower sediments (<9 m at Washtucna, <12 m at Winona), the microbial communities are likely similar in age to the groundwater; thus, microbial succession has been influenced by recent transport of microorganisms from the surface. In the deeper sediments, the populations may be considerably older than the porewater ages, since microbial transport is severely restricted in unsaturated sediments. This is particularly true at the Winona site, which was never flooded.     

Purification and properties ofα-amylase from chicken (Gallus Gallus L.) pancreas

Summary Amylase from chicken pancreas was purified by an affinity method involving filtering a crude extract from pancreas through a Sepharose-wheat albumin column and eluting the retained enzyme with maltose. The purified amylase showed two active bands upon polyacrylamide electrophoresis in an alkaline buffer system and only one band in an acidic buffer system. The enzyme is a Ca²⁺—glycoprotein which behaves as a typical-amylase. It consists of a single polypeptide chain with molecular weight 53,000 and contains 5.3 moles of reducing sugars per mole of protein. Optimal conditions of pH and temperature for the enzymic activity are 7.5 and 37°C. The enzyme is irreversibly inactivated by removal of Ca²⁺ by exhaustive dialysis and is activated by the presence in the assay mixture of Cl^–; other halides are less effective than Cl^– in activating the enzyme.     

Caveolin-3 directly interacts with the C-terminal tail of beta -dystroglycan. Identification of a central WW-like domain within caveolin family members

Caveolin-3, the most recently recognized member of the caveolin gene family, is muscle-specific and is found in both cardiac and skeletal muscle, as well as smooth muscle cells. Several independent lines of evidence indicate that caveolin-3 is localized to the sarcolemma, where it associates with the dystrophin-glycoprotein complex. However, it remains unknown which component of the dystrophin complex interacts with caveolin-3. Here, we demonstrate that caveolin-3 directly interacts with beta-dystroglycan, an integral membrane component of the dystrophin complex. Our results indicate that caveolin-3 co-localizes, co-fractionates, and co-immunoprecipitates with a fusion protein containing the cytoplasmic tail of beta-dystroglycan. In addition, we show that a novel WW-like domain within caveolin-3 directly recognizes the extreme C terminus of beta-dystroglycan that contains a PPXY motif. As the WW domain of dystrophin recognizes the same site within beta-dystroglycan, we also demonstrate that caveolin-3 can effectively block the interaction of dystrophin with beta-dystroglycan. In this regard, interaction of caveolin-3 with beta-dystroglycan may competitively regulate the recruitment of dystrophin to the sarcolemma. We discuss the possible implications of our findings in the context of Duchenne muscular dystrophy.     

Androecium development in the bromeliad Dyckia pseudococcinea L.B.Sm. (Pitcairnioideae-Bromeliaceae), an endangered species endemic to Brazil: implications for conservation

Dyckia pseudococcinea L.B.Sm. is endemic to the restingas of Maricá, State of Rio de Janeiro, in southeastern Brazil. However, since this area is under intense ecological stress, D. pseudococcinea is considered an endangered plant species. An important step toward the conservation of this species is establishing the developmental stage most favorable to in vitro propagation. Accordingly, the present study analyzed the androecium to establish the developmental stages of anthers, emphasizing anther wall development, androsporogenesis and androgametogenesis. The relationships between the size of flowers and anthers were also studied. Anther wall development follows the basic-type, while the tapetum, which is originated from the subepidermal layer (inner secondary parietal layer 2 and archesporial initials), follows the secretory-type. Androsporogenesis is successive and originates isobilateral and decussate tetrads. The oblate and monosulcate pollen grains exhibit microreticulate exine and are dispersed at the bicellular stage. At the vacuolated stage, the androspore (microspore) is still proliferating and not yet completely differentiated. Therefore, since the androspore has not yet lost its embryonic capacity, we suggest the preferential use of this developmental stage, which is present in flower buds 6.4–7.1 mm in length, in conservation protocols focused on the androgenesis of D. pseudococcinea.