Beta-globin chain hemoglobin polymorphism and hemoglobin stability in black rhinoceroses (Diceros bicornis)

To evaluate the syndrome of acute intravascular hemolytic anemia in black rhinoceroses (Diceros bicornis), the hemoglobin of this species was evaluated by use of isopropanol- and heat-stability tests and was further characterized by electrophoretic studies. Samples were obtained from 22 apparently healthy captive North American black rhinoceroses, though 3 of the study animals had survived previous hemolytic events, and 3 others were parents of 3 offspring that had suffered hemolysis. The eastern African (Diceros bicornis michaeli) and the southern African subspecies (D b minor) were represented. Comparative samples were also obtained from 2 white (Ceratotherium simum) and 1 Indian (Rhinoceros unicornis) rhinoceroses. The hemoglobin of all 3 species appeared stable when tested by use of the heat and isopropanol methods. Thus, an unstable hemoglobin does not appear to be involved in the hemolytic crises of captive black rhinoceroses. Black rhinoceros hemoglobin had a striking polymorphism. Thirteen of the samples from black rhinoceroses had a single hemoglobin band, based on results of alkaline electrophoresis. Nine had, in addition to this major band, a slow (more cathodic) minor band that comprised about 10% of the total hemoglobin. Further studies indicated that the major band and the slower minor band may contain globin chains analogous to human beta- and delta-chains respectively; these bands have been tentatively designated B and C. Phenotypes B and BC are common, in a ratio of 4:3. A genetic mechanism is proposed that assumes beta b and beta c gene loci and that beta c-locus-expressed (beta c+) and beta c-locus-inhibited (beta c degrees) are common alleles for the beta c-locus.(ABSTRACT TRUNCATED AT 250 WORDS)     

Electrophoretic Characterization of Quinoa Seed Proteins

Quinoa (Chenopodium quinoa Willd) is an important domesticated food crop of the Andean highlands with potential as an alternative crop elsewhere. Among its most attractive characteristics are the quantity and favorable amino acid balance of the seed proteins. The objective of this study was to characterize quinoa seed proteins by electrophoretic mobility, solubility fractionation, and genetic variability from a wide genetic base. Electrophoretic profiles of denatured albumin, globulin, prolamin, and glutelin solubility fractions demonstrated that quinoa seed polypeptides could be classified as either albumin or globulin with most predominant polypeptides in the globulin fraction. Insignificant amounts of protein were present in the prolamin fraction and all polypeptides in the glutelin fraction had identical electrophoretic mobilities to albumins and globulins. Three globulin polypeptides of 34.3, 35.6, and 36.2 kilodaltons in size were highly variable within and among the accessions examined and appear to be coded by at least two loci. Two-dimensional peptide mapping revealed that these three polypeptides were homologous. These highly variable markers could be used for identification and classification of germplasm and elucidation of systematics and genetic variability within the quinoa germplasm pool. All other major polypeptides were electrophoretically invariant among the accessions examined.     

Enhancement of RAPD Analysis by Restriction-endonuclease Digestion of Template DNA in Wheat

Random amplified polymorphic DNA (RAPD) analysis has proven to be an effective procedure for molecular marker applications in plant breeding, although non-specific amplification may limit its utility in some species. The objective of this study was to determine the effectiveness of restriction-endonuclease digestion of template DNA for elimination of non-specific amplification and generation of heritable RAPD markers. Restriction endonucleases digested wheat DNA to completion in amplification buffer, suggesting that the restriction endonuclease can be added directly to the reaction mixture prior to amplification. A 1-h 37°C step was programmed into the thermal cycler for restriction-endonuclease digestion which was followed immediately by amplification. Non-specific amplification was reduced and DNA marker patterns were altered in digested samples when compared to undigested samples. Genetic segregation of two polymorphic markers tested in F₅ inbred progeny fit expected 1:1 ratios. These results suggest that heritable DNA markers may be generated with reduction in non-specific amplification when restriction-endonuclease digestion of template DNA is conducted as part of the RAPD procedure.     

Oxygen isotopes in biogenic silica: global changes in ocean temperature and isotopic composition

A record of oxygen isotopes in biogenic silica from a deep-sea sediment core from the Southern Ocean reveals that marine diatoms retain their primary isotopic composition after burial. As a result, the marine diatom record can be combined with data on coexisting planktonic foraminifera to monitor past surface temperature and isotopic composition of seawater. The coupling of these two records allows the solution of two paleotemperature equations for each core interval. Data from a South Atlantic core show that the average delta(18)O during the glacial period at this site was higher by about 1.3 per mil than average Holocene values, and that average glacial-age temperatures were not significantly different from average Holocene values.     

Recent variability in the southern oscillation: isotopic results from a tarawa atoll coral

In the western tropical Pacific, the interannual migration of the Indonesian Low convective system causes changes in rainfall that dominate the regional signature of the El Ni?o-Southern Oscillation (ENSO) system. A 96-year oxygen isotope record from a Tarawa Atoll coral (1 degrees N, 172 degrees E) reflects regional convective activity through rainfall-induced salinity changes. This monthly resolution record spans twice the length of the local climatological record and provides a history of ENSO variability comparable in quality with those derived from instrumental climate data. Comparison of this coral record with a historical chronology of EI Ni?o events indicates that climate anomalies in coastal South America are occasionally decoupled from Pacific-wide ENSO extremes. Spectral analysis suggests that the distribution of variance in this record has shifted among annual to interannual periods during the present century, concurrent with observed changes in the strength of the Southern Oscillation.     

Vertical distribution and isotopic composition of living planktonic foraminifera in the Western north atlantic

Thirteen species of planktonic foraminifera collected with vertically stratified zooplankton tows in the slope water, Gulf Stream cold core ring, and northern Sargasso Sea show significant differences in their vertical distributions in the upper 200 meters of these different hydrographic regimes. Gulf Stream cold core rings may be responsible for a southern displacement of the faunal boundary associated with the Gulf Stream when reconstructed from the deep-sea sediment record. Oxygen isotope analyses of seven species reveal that nonspinose species (algal symbiont-barren) apparently calcify in oxygen isotope equilibrium, whereas spinose species usually calcify out of oxygen isotope equilibrium by approximately -0.3 to -0.4 per mil in delta(18)O values. The isotope data indicate that foraminifera shells calcify in depth zones that are significantly narrower than the overall vertical distribution of a species would imply.