SUMMARY OF GREEN PLANT PHYLOGENY AND CLASSIFICATION

Abstract— A cladogram of green plants involving all major extant groups of green algae, bryophytes, pteridophytes, and seed plants is presented. It is partly based on contributions by B. Mishler and S. Churchill, H. Wagner, and P. Crane. The relationships of green plants to other green organisms ( Prochloron , euglenophytes) are discussed. The characters and subclades of the cladogram are briefly discussed, with an attempt to indicate weak points. The possibility of including some major extinct groups is considered. A cladistic classification consistent with the cladogram is presented. Grades are abandoned as taxa and major clades like the division Chlorophyta (green algae excluding micro-monadophytes and charophytes sensu Mattox and Stewart), the division Streptophyta (charophytes + embryophytes), the subdivision Embryophytina (land plants or embryophytes), the superclass Tracheidatae (tracheophytes), and the class Spermatopsida (seed plants) are recognized.     

Raman spectra of a solid antifreeze glycoprotein and its liquid and frozen aqueous solutions.

Raman spectroscopy was used to study the anomalous decrease in the freezing temperature of water produced by an antifreeze glycoprotein obtained from the sera of an Antarctic fish. An active fraction of this glycoprotein has a molecular weight of approximately 18,000 by equilibrium sedimentation compared to an apparent weight of 20 by freezing temperature depression. The Raman spectra of water present in a 1% antifreeze glycoprotein solution and of ice frozen from this solution were indistinguishable from the spectra of pure water and ice, respectively. These results indicate that the bulk properties of water and ice are unaffected by the presence of the antifreeze glycoprotein. Raman measurements on ice grown slowly, using as seed an oriented single crystal of ice in contact with 1% glycoprotein solutions, showed that the active glycoprotein was not excluded from the ice phase. On the other hand, we found that a smaller, inactive glycoprotein was excluded. Comparison of the Raman spectra of active and inactive glycoprotein components as solids, in 5% solutions, and rapidly frozen 5% solutions, showed that the two components differ in conformation and possibly in the environment of their carbohydrate hydroxyls. These observations suggest that hydrogen bonding of the carbohydrate hydroxyls of the active glycoprotein at the ice-solution interface may physically prevent growth of the ice lattice.     

A novel method of preparing totally alpha-deuterated amino acids for selective incorporation into proteins. Application to assignment of 1H resonances of valine residues in dihydrofolate reductase

The pyridoxal/2H2O exchange reaction of the alpha-CH of amino acids is known to be accompanied by racemisation: Thus by using a D-amino acid as the starting material any L-amino acid formed in the reaction will be essentially fully deuterated at its alpha-position. We have used this method to prepare alpha-deuterated L-valine and incorporated this biosynthetically into L. casei dihydrofolate reductase. A comparison of the alpha CH-NH fingerprint regions of COSY spectra of deuterated and normal DHFR complexes allows one to identify cross-peaks from 15 of the 16 valine residues.     

Fish community changes after minimum flow increase: testing quantitative predictions in the Rhône River at Pierre-Bénite, France

1. Many aspects of the flow regime influence the structure of stream communities, among which the minimum discharge left in rivers has received particular attention. However, instream habitat models predicting the ecological impacts of discharge management often lack biological validation and spatial generality, particularly for large rivers with many fish species. 2. The minimum flow at Pierre‐Bénite, a reach of the Rhône river bypassed by artificial channels, was increased from 10 to 100 m³ s^?1 in August 2000 (natural mean discharge 1030 m³ s^?1), resulting in a fivefold increase in average velocity at minimum flow. Fish were electrofished in several habitat units on 12 surveys between 1995 and 2004. 3. Principal components analysis revealed a significant change in the relative abundance of fish species. The relative abundance of species preferring fast‐flowing and/or deep microhabitats increased from two‐ to fourfold after minimum flow increase. A change in community structure confirmed independent quantitative predictions of an instream habitat model. This change was significantly linked to minimum flow increase, but not to any other environmental variables describing high flows or temperature at key periods of fish life cycle. The rapidity of the fish response compared with the lifespan of individual species can be explained by a differential response of specific size classes. 4. The fish community at Pierre‐Bénite is in a transitional stage and only continued monitoring will indicate if the observed shift in community structure is perennial. We expect that our case study will be compared with other predictive tests of the impacts of flow restoration in large rivers, in the Rhône catchment and elsewhere.