Monovalent cations regulate expression and activity of the Hak1 potassium transporter in Debaryomyces hansenii.

Debaryomyces hansenii was able to grow in a medium containing residual amounts of K(+), indicating the activity of high affinity K(+) transporters. Transcriptional regulation analysis of the genes encoding the two potassium uptake systems in D. hansenii revealed that while DhTRK1 is not regulated at transcriptional level, expression of DhHAK1 required starvation in the absence of K(+) and Na(+) and was not affected by changes in membrane potential. Rb(+) transport in cells expressing DhHAK1 was activated by external Na(+) or acidic pH and inhibited by high pH. We propose a K(+)-H(+) symporter that, under certain conditions may work as a K(+)-Na(+) transporter, as the mechanism driving K(+) influx mediated by DhHak1p.

Mechanisms underlying the halotolerant way of Debaryomyces hansenii.

The yeast Debaryomyces hansenii is usually found in salty environments such as the sea and salted food. It is capable of accumulating sodium without being intoxicated even when potassium is present at low concentration in the environment. In addition, sodium improves growth and protects D. hansenii in the presence of additional stress factors such as high temperature and extreme pH. An array of advantageous factors, as compared with Saccharomyces cerevisiae, is putatively involved in the increased halotolerance of D. hansenii: glycerol, the main compatible solute, is kept inside the cell by an active glycerol-Na+ symporter; potassium uptake is not inhibited by sodium; sodium protein targets in D. hansenii seem to be more resistant. The whole genome of D. hansenii has been sequenced and is now available at http://cbi.labri.fr/Genolevures/ and, so far, no genes specifically responsible for the halotolerant behaviour of D. hansenii have been found.

Monovalent cation fluxes and physiological changes of Debaryomyces hansenii grown at high concentrations of KCl and NaCl.

Debaryomyces hansenii showed an increased growth in the presence of either 1 M, KCl or 1 M NaCl and a low acidification of the medium, higher for the cells grown in the presence of NaCl. These cells accumulated high concentrations of the cations, and showed a very fast capacity to exchange either Na+ or K+ for the opposite cation. They showed a rapid uptake of 86Rb+ and 22Na+. 86Rb+ transport was saturable, with K(m) and Vmax values higher for cells grown in 1 M NaCl. 22Na+ uptake showed a diffusion component, also higher for the cells grown with NaCl. Changes depended on growth conditions, and not on further incubation, which changed the internal ion concentration. K+ stimulated proton pumping produced a rapid extrusion of protons, and also a decrease of the membrane potential. Cells grown in 1 M KCl showed a higher fermentation rate, but significantly lower respiratory capacity. ATP levels were higher in cells grown in the presence of NaCl; upon incubation with glucose, those grown in the presence of KCl reached values similar to the ones grown in the presence of NaCl. In both, the addition of KCl produced a transient decrease of the ATP levels. As to ion transport mechanisms, D. hansenii appears to have (a) an ATPase functioning as a proton pump, generating a membrane potential difference which drives K+ through a uniporter; (b) a K+/H+ exchange system; and (c) a rapid cation/cation exchange system. Most interesting is that cells grown in different ionic environments change their studied capacities, which are not dependent on the cation content, but on differences in their genetic expression during growth.

Physiological basis for the high salt tolerance of Debaryomyces hansenii.

The effects of KCl, NaCl, and LiCl on the growth of Debaryomyces hansenii, usually considered a halotolerant yeast, and Saccharomyces cerevisiae were compared. KCl and NaCl had similar effects on D. hansenii, indicating that NaCl created only osmotic stress, while LiCl had a specific inhibitory effect, although relatively weaker than in S. cerevisiae. In media with low K+, Na+ was able to substitute for K+, restoring the specific growth rate and the final biomass of the culture. The intracellular concentration of Na+ reached values up to 800 mM, suggesting that metabolism is not affected by rather high concentrations of salt. The ability of D. hansenii to extrude Na+ and Li+ was similar to that described for S. cerevisiae, suggesting that this mechanism is not responsible for the increased halotolerance. Also, the kinetic parameters of Rb+ uptake in D. hansenii (Vmax, 4.2 nmol mg [dry weight]-1 min-1; K(m), 7.4 mM) indicate that the transport system was not more efficient than in S. cerevisiae. Sodium (50 mM) activated the transport of Rb+ by increasing the affinity for the substrate in D. hansenii, while the effect was opposite in S. cerevisiae. Lithium inhibited Rb+ uptake in D. hansenii. We propose that the metabolism of D. hansenii is less sensitive to intracellular Na+ than is that of S. cerevisiae, that Na+ substitutes for K+ when K+ is scarce, and that the transport of K+ is favored by the presence of Na+. In low K+ environments, D. hansenii behaved as a halophilic yeast.

Reversible oligonucleosome self-association: dependence on divalent cations and core histone tail domains.

Regularly spaced nucleosomal arrays equilibrate between unfolded and highly folded conformations in <2 mM MgCl2, and self-associate above 2 mM MgCl2 [Schwarz, P. M., & Hansen, J. C. (1994) J. Biol. Chem. 269, 16284-16289]. Here we use analytical and differential sedimentation techniques to characterize the molecular mechanism and determinants of oligonucleosome self-association. Divalent cations induce self-association of intact nucleosomal arrays by binding to oligonucleosomal DNA and neutralizing its negative charge. Neither linker histones nor H2A/H2B dimers are required for Mg2+ - dependent self-association. However, divalent cations are unable to induce self-association of trypsinized nucleosomal arrays lacking their N- and C-terminal core histone tail domains. This suggests that the H3/H4 tail domains directly mediate oligonucleosome self-association through a non-Coulombic-based mechanism. Self-association occurs independently of whether the oligonucleosome monomers are folded or unfolded. The first step in the self-association pathway is strongly cooperative and produces a soluble association intermediate that sediments approximately 10 times faster than the oligonucleosome monomers. The size of the oligonucleosome polymers increases rapidly as a consequence of small increases in the divalent cation concentration, eventually producing polymeric species that sediment at >> 10 000 S. Importantly, all steps in the self-association pathway are freely reversible upon removal of the divalent cations. Taken together, these data indicate that short oligonucleosome fragments composed of only core histone octamers and DNA possess all of the structural features required to achieve chromosome-level DNA compaction. These findings provide a molecular basis for explaining many of the recently uncovered structural features of interphase and metaphase chromosomal fibers.