Bioactive hydroxyphenylpyrrole-dicarboxylic acids from a new marine Halomonas sp.: Production and structure elucidation.

The new marine Halomonas sp. strain GWS-BW-H8hM (DSM 17996) was found to produce 3-(4'-hydroxyphenyl)-4-phenylpyrrole-2,5-dicarboxylic acid (HPPD-1) and 3,4-bis(4'-hydroxy- phenyl)pyrrole-2,5-dicarboxylic acid (HPPD-2). In initial cultivations using marine broth, only low contents of these compounds have been isolated. Improving the conditions and growing the strain on artificial seawater supplemented with tryptone 10 g l(-1), yeast extract 5 g l(-1), L-tyrosine 0.6 g l(-1), glycine 1 g l(-1), and glucose 6 g l(-1), the growth-associated HPPD-1 and HPPD-2 production of a 40-l batch cultivation reached the amounts of 47 mg l(-1) and 116 mg l(-1), respectively, after 65 h. Both compounds showed potent anti-tumor-promoting activities.

Recovery of cell volume and electrolytes of A6 cells after re-establishing isotonicity following hypotonic stress.

Cellular element concentrations and dry weight contents in A6 cells were determined using electron microprobe analysis to establish whether these cells exhibit a regulatory volume increase (post-RVD-RVI) when re-establishing isotonicity following a hypotonically induced regulatory volume decrease (RVD). Hypotonic stress was induced by reducing basolateral [NaCl], and hence, osmolarity fell from 260 to 140 mosmol/l. The alterations in cell volume after re-establishing isotonicity, calculated from the cellular dry weight changes, indicate within the first 2 min cell shrinkage from 120 to 76% of control, compatible with almost ideal osmometric behaviour of A6 cells, and thereafter a post-RVD-RVI to 94%. The cellular uptake of osmolytes necessary to explain the post-RVD-RVI could be accounted for solely by a gain in cellular K and Cl. The involvement of a Na-K-2Cl cotransporter in most of the KCl uptake seems plausible since basolateral bumetanide blocked KCl uptake and post-RVD-RVI. The net uptake of cations (K uptake of 185.2, Na loss of 8.2 mmol/kg dry wt) during the isotonic period exceeded the Cl uptake by 38.2 mmol/kg dry wt, suggesting the uptake of another anion and/or the alteration of cellular buffer capacity. The relatively low Na concentration maintained during the isotonic period (13.3 vs. 20.4 mmol/kg wet wt under control conditions) might favour electrolyte uptake via the Na-K-2Cl cotransporter.

Changes in element composition of A6 cells following hypotonic stress.

Cellular element concentrations and dry weight contents were determined in A6 epithelia using electron microprobe analysis. This was done to assess the quantitative contributions of Na, K and Cl to the regulatory volume decrease (RVD) and isovolumetric regulation (IVR) after decreasing the basolateral osmolality from 260 to 140 mosmol/kg in a stepwise or gradual way. Two minutes after inducing acute hypotonic stress the cells behaved almost like ideal osmometers, as indicated by a pronounced increase in cell height and decreases in the cellular dry weight and concentrations of all measured elements by about the same degree. Sixty minutes after inducing acute hypotonic stress the dry weight and concentrations of the impermeant elements P, Mg and Ca had returned approximately to control values, indicating normalized cell volume. Na, K and Cl concentrations, however, remained greatly reduced. The cellular amounts of Na, K and Cl diminished during RVD by approximately 31%, 24% and 46%, respectively. The dry weights and element concentrations measured 60 min after inducing acute hypotonic stress were similar to those obtained after a continuous reduction of basolateral osmolality. The cellular loss of Na and K following hypotonic stress exceeded that of Cl by about 40 mmol/kg wet wt., suggesting the exit of an other anion and/or the titration of fixed negative charges. The contribution of Na, K and Cl to total cellular osmolality increased from about 75% under control conditions to about 85% during RVD and IVR. Since only approximately 70% of the loss of cellular osmolytes necessary for the observed RVD and IVR is accounted for by the cellular exit of Na, K and Cl, other osmolytes, possibly amino acids, must leave the cells following hypotonic stress.