Analysis of mutations in $\beta$-tubulin genes affecting tubulin stability and assembly

Cmd4 is a colcemid-sensitive CHO cell line that is temperature sensitive for growth and expresses an altered $\beta$-tubulin, $\beta\sb1$. One revertant of this cell line, D2, exhibits a further alteration in $\beta\sb1$ resulting in an acidic shift in its isoelectric point and a decrease in its molecular weight to 40 kD, as measured by two dimensional gel electrophoresis. This $\beta$-tubulin variant has been shown to be assembly-defective and unstable. Characterization of the mutant $\beta\sb1$ in D2 by high pressure liquid chromatography (HPLC) revealed the loss of methionine containing tryptic peptides 7,8,9, and 10. Southern analysis of the genomic DNA digested with several different restriction enzymes resulted in the appearance of new restriction fragments 250 base pairs shorter than the corresponding fragments from the wild-type $\beta\sb1$-tubulin gene. Northern analysis on mRNA from D2 revealed two new message products that also differed by 250 bases from the corresponding wild type $\beta$-tubulin transcripts. To precisely define the region of the alteration, cloning and sequencing of the mutant and wild type genomic $\beta$-tubulin genes were conducted. A size-selected EcoRI genomic library was prepared using the Stratagene lambda Zap II phage cloning system. Using subclones of CHO $\beta$-tubulin cDNA as probes, a 2.5 kb wild type clone and a 2.3 kb mutant clone were identified from this library. Each of these was shown to contain a portion of the gene extending from intron 3 through the end of the coding sequence in exon 4 and into the 3$\sp\prime$ untranslated region on the basis of alignment with the published human $\beta$-tubulin sequence. Sequencing of the mutant 2.3 kb clone revealed that the mutation is due to a 246 base pair internal deletion in exon 4 (base pair 756-1001) that encodes amino acids 253-334. This deletion results in the loss of a putative binding site for GTP which could potentially explain the phenotype of this mutant $\beta$-tubulin. Also sequence comparison of the 3$\sp\prime$ untranslated region between different species revealed the conservation of 200 base pairs with 78% homology. It is proposed that this region could play an important role in the regulation of $\beta$-tubulin gene expression. ^

(John L. Stoddard's) lectures; illustrated and embellished with views of the world's famous places and people ...

v. 1. Norway. Switzerland. Athens. Venice.--v. 2. Constantinople. Jerusalem. Egypt.--v. 3. Japan (two lectures) China.--v. 4. India (two lectures) The passion play.--v. 5. Paris. La belle France. Spain.--v. 6. Berlin. Vienna. St. Petersburg. Moscow.--v. 7. The Rhine. Belgium. Holland. Mexico.--v. 8. Florence. Naples. Rome.--v. 9. Scotland. England. London.--v. 10. Southern California. Grand Cañon of the Colorado river. Yellowstone national park.

Vascular plant diversity and climate change in the alpine zone of the Lefka Ori, Crete

The aim of this study is to analyse the vascular flora and the local climate along an altitudinal gradient in the Lefka Ori massif Crete and to evaluate the potential effects of climate change on the plant diversity of the sub-alpine and alpine zones. It provides a quantitative/qualitative analysis of vegetation-environment relationships for four summits along an altitude gradient on the Lefka Ori massif Crete (1664-2339 m). The GLORIA multi-summit approach was used to provide vegetation and floristic data together with temperature records for every summit. Species richness and species turnover was calculated together with floristic similarity between the summits. 70 species were recorded, 20 of which were endemic, belonging to 23 different families. Cretan endemics dominate at these high altitudes. Species richness and turnover decreased with altitude. The two highest summits showed greater floristic similarity. Only 20% of the total flora recorded reaches the highest summit while 10% is common among summits. Overall there was a 4.96 degrees C decrease in temperature along the 675 m gradient. Given a scenario of temperature increase the ecotone between the sub-alpine and alpine zone would be likely to have the greatest species turnover. Southern exposures are likely to be invaded first by thermophilous species while northern exposures are likely to be more resistant to changes. Species distribution shifts will also depend on habitat availability. Many, already threatened, local endemic species will be affected first.

Sedimentary environments and climate change: a case study (late Miocene, central Crete)

In this study, conditions of deposition and stratigraphical architecture of Neogene (Tortonian, 11-6,7Ma) sediments of southern central Crete were analysed. In order to improve resolution of paleoclimatic data, new methods were applied to quantify environmental parameters and to increase the chronostratigraphic resolution in shallow water sediments. A relationship between paleoenvironmental change observed on Crete and global processes was established and a depositional model was developed. Based on a detailed analysis of the distribution of non geniculate coralline red algae, index values for water temperature and water depth were established and tested with the distribution patterns of benthic foraminifera and symbiont-bearing corals. Calcite shelled bivalves were sampled from the Algarve coast (southern Portugal) and central Crete and then 87Sr/86Sr was measured. A high resolution chronostratigraphy was developed based on the correlation between fluctuations in Sr ratios in the measured sections and in a late Miocene global seawater Sr isotope reference curve. Applying this method, a time frame was established to compare paleoenvironmental data from southern central Crete with global information on climate change reflected in oxygen isotope data. The comparison between paleotemperature data based on red algae and global oxygen isotope data showed that the employed index values reflect global change in temperature. Data indicate a warm interval during earliest Tortonian, a second short warm interval between 10 and 9,5Ma, a longer climatic optimum between 9 and 8Ma and an interval of increasing temperatures in the latest Tortonian. The distribution of coral reefs and carpets shows that during the warm intervals, the depositional environment became tropical while temperate climates prevailed during the cold interval. Since relative tectonic movements after initial half-graben formation in the early Tortonian were low in southern central Crete, sedimentary successions strongly respond to global sea-level fluctuation. A characteristic sedimentary succession formed during a 3rd order sea-level cycle: It comprises mixed siliciclastic-limestone deposited during sea-level fall and lowstand, homogenous red algal deposits formed during sea-level rise and coral carpets formed during late rise and highstand. Individual beds in the succession reflect glacioeustatic fluctuations that are most prominent in the mixed siliciclastic-limestone interval. These results confirm the fact that sedimentary successions deposited at the critical threshold between temperate and tropical environments develop characteristic changes in depositional systems and biotic associations that can be used to assemble paleoclimatic datasets.