TEXT

Top Abstract Text References

Choline is a major component of membranes and a structural component of some microbial cell wall polymers (12, 16, 20). In some bacteria and higher plants, choline is a precursor of the osmolyte glycine betaine (GB) (2, 3, 15). In Penicillium fellutanum cultured in a medium containing 3 M NaCl, 46 and 70 mM concentrations of the osmolytes choline-O-sulfate (COS) and GB, respectively, accumulated (14). Choline stimulates hyphal extension, inhibits initiation of branching (19, 22), and is an essential nutrient for growth of choline auxotrophs of Neurospora crassa (6) and Aspergillus nidulans (9, 10).

COS is a known sulfate storage molecule in fungi (4, 5, 7), and it is also a known endogenous reserve source of choline that stimulates growth in choline-requiring auxotrophs of A. nidulans cultured in insufficient choline (11). However, Markham et al. (11) suggested that A. nidulans carrying mutations blocked in sulfate metabolism did not synthesize COS and that residual growth must have resulted from an unknown endogenous storage precursor of choline.

We previously reported that, as phosphate in the nutrient medium becomes limiting, choline phosphodiesters of P. fellutanum extracellular glycopeptide (peptidophosphogalactomannan) provide phosphate and choline, and excess choline accumulates as cytoplasmic GB and COS (13, 14). This finding was exploited to determine the relationship between COS, GB, and choline in P. fellutanum under sulfate-limiting conditions. We assume that COS is a storage form of both sulfate and choline in filamentous fungi (11). This study was focused on determining if an alternative intracellular soluble precursor of choline or COS accumulates in P. fellutanum cultured in limiting sulfate or if the concentration of choline increases in the cytoplasm.

Influence of phosphate concentration in the nutrient medium on accumulation of COS and GB. The sources of P. fellutanum, nutrients, and L-[methyl-¹³C]methionine, preparation of mycelial extracts, and ¹³C nuclear magnetic resonance (NMR) spectroscopy analysis have been described recently (14). The ¹³C-methyl signals of COS (56.77 ppm) and GB (56.23 ppm) in extracts of mycelium from 200 ml of 8-day cultures in low-phosphate standard growth (LPSG) (2 mM P_i) or standard growth (SG) (20 mM P_i) medium containing L-[methyl-¹³C]methionine were integrated, and their magnitudes were compared with that of the 0.22% TSP [(trimethylsilane)-1-propanesulfonate] (0.00 ppm) signal, all as described previously (13, 14). COS in extracts of day-5 mycelium from LPSG and SG medium was 9.3 and 6.3 mg (dry weight) per g, respectively (14). No significant GB was found in extracts of SG mycelium. The increases in COS and GB in mycelium from LPSG medium may result from decreases in the requirements for choline and ethanolamine. No detectable soluble choline occurred in mycelium from LPSG medium. This suggests that COS and GB are the primary choline precursors or storage products.

Age-dependent accumulation of COS and GB. Mycelium from day-5 LPSG medium enriched with L-[methyl-¹³C]methionine accumulated [methyl-¹³C]COS with a major signal (COS1, 56.77 ppm) and two unidentified signals at 54.94 and 48.75 ppm (Fig. 1A). These signals were confirmed as ¹³C-methyl signals by comparison with those in an extract of mycelium of a culture supplemented with L-methionine not enriched with ¹³C (data not shown).

View larger version (10K): [in this window] [in a new window]   FIG. 1.   Time-dependent accumulation of choline derivatives in mycelium. Mycelial extracts were obtained from P. fellutanum cultured in 50 mg of L-[methyl-13C]methionine in 200 ml of LPSG medium. NMR spectra from day-5 (A) and day-8 (B) cultures are shown. Peak symbol abbreviations are defined in the text.

Effects of sulfate limitation in the culture medium on accumulation of COS and GB. Because COS is a sulfate and choline storage molecule in filamentous fungi (11), it was reasoned that a significant level of choline might accumulate in mycelium cultured in limiting sulfate and low phosphate concentrations. Mycelium was prelabeled for 5 days with ¹³C by addition of 50 mg of L-[methyl-¹³C]methionine to LPSG cultures. The ¹³C spectrum of an extract from the enriched mycelium is shown in Fig. 2A. The remainder of the culture was harvested aseptically from separate flasks and transferred either to fresh LPSG medium without added L-[methyl-¹³C]methionine, as a control, or to fresh LPSG low-sulfate unenriched medium containing 1.53 µM Cr₂(SO₄)₃ · 12H₂O and 6.41 µM CuSO₄ · 5H₂O with FeCl₂ · 2H₂O substituted for FeSO₄ · 7H₂O. These ¹³C-labeled P. fellutanum cells were cultured for an additional 8 days; the mycelial extract from each culture was then subjected to ¹³C NMR analysis with 0.51% TSP as a reference. Mycelium which was transferred to fresh LPSG medium (control) (Fig. 2B) shows a slightly decreased level of cytosolic COS (carbons are designated COS1, COS2, and COS3) and the appearance of a [methyl-¹³C]GB signal at 56.23 ppm. In contrast, the extract of mycelium transferred to and cultured in LPSG low-sulfate medium (Fig. 2C) shows a significant decrease in COS and an increase in the GB level to that of COS shown in Fig. 2A. No choline signals are present in these spectra. These results clearly indicate that COS is a sulfate storage molecule in P. fellutanum as well as other filamentous fungi. The precipitous decrease in [methyl-¹³C]COS, and the large increase in [methyl-¹³C]GB, in the extracts of mycelium cultured in LPSG low-sulfate medium (Fig. 2C) suggests that (i) COS was converted to GB or (ii) any excess [methyl-¹³C]choline synthesized was converted to GB.

View larger version (17K): [in this window] [in a new window]   FIG. 2.   Influence of the concentration of sulfate in the culture medium on accumulation of intracellular COS and GB. The cytoplasmic solutes of mycelium cultured for 5 days in 200 ml of LPSG medium that was enriched with 50 mg of L-[methyl-13C]methionine are shown (A). On day 5, 13C-labeled mycelium was transferred to fresh LPSG medium and cultured for an additional 8 days (B) or transferred to fresh LPSG low-sulfate medium and cultured for 8 days (C).

Effects of adding sulfate to cultures in LPSG low-sulfate medium. ¹³C-methyl-labeled mycelium from LPSG low-sulfate (8 µM SO₄) medium (Fig. 2C) was transferred to an LPSG-5 mM sulfate medium (Fig. 3A) or to fresh LPSG low-sulfate medium as a control (Fig. 3B) and cultured for 5 days. This experiment was performed to determine whether the levels of GB and COS in the mycelium are influenced by addition of sulfate to the culture medium. The [methyl-¹³C]COS signal increased significantly with a concomitant decrease of [methyl-¹³C]GB in mycelium cultured in LPSG high-sulfate medium (Fig. 3A). The high ratio of GB1 to COS1 signal intensities remained relatively unchanged in control mycelium (Fig. 3B). No detectable quantity of choline was observed in extracts of mycelium obtained from either set of nutritional conditions. These results suggest that COS and GB are metabolically closely related and that they are interconvertible depending upon the concentrations of sulfate and phosphate in the culture medium. However, the intensities of signals from the primary and secondary hydroxyl groups of erythritol and glycerol at 65.5 and 75.1 ppm, respectively, as well as other minor signals, were severalfold larger than those noted in Fig. 1 and 2. This effect may have resulted from the synthesis of polyhydroxy alcohols after the mycelium was transferred to fresh media.

View larger version (15K): [in this window] [in a new window]   FIG. 3.   Influence of sulfate on the accumulation of intracellular COS and GB. 13C-methyl-labeled mycelium cultured for 5 days in LPSG low-sulfate medium (shown in Fig. 2C) was transferred to fresh LPSG medium containing 5 mM Na2SO4 (A) or to fresh LPSG low-sulfate medium (B) as a control. The region of 72.50 to 56.80 ppm is shown with twofold enlargement in signal height in the insets. "x" placed at 58.59 and 70.22 ppm indicates the absence of signals representing the choline hydroxymethyl and N-methylene carbons, respectively.

GB as a potential intracellular alternative reserve of choline. COS accumulation is common among filamentous fungi (8, 17, 18), and Markham et al. (11) concluded that the role of COS in fungal physiology is as a storage source of sulfur, based on the observation (9) that choline-requiring auxotrophs of A. nidulans continued growth in the absence of added choline. However, Arst (1) argued against COS being the endogenous source of choline because, under choline-deficient conditions, A. nidulans double mutants, carrying the choA1 mutation and a mutation that makes the organism unable to either synthesize or utilize COS, showed growth equivalent to that of the choA1 mutant. It was suggested that such residual growth is due to choline supplied from sources other than membrane phospholipids or endogenously stored choline (11). We reported previously that a phosphocholine-containing P. fellutanum peptidophosphogalactomannan is a precursor of intracellular COS and GB (13) when the organism is cultured in LPSG medium. Based on the observation that a detectable level of soluble choline does not accumulate in the mycelium in a sulfate-deficient medium and that a loss of cytoplasmic COS and an increase of GB results, we now conclude that GB is another endogenous storage precursor of choline in P. fellutanum and is likely the unknown precursor of choline that Markham et al. predicted (11). This conclusion was strengthened by the demonstration that adjusting the culture's concentration of sulfate to 5 mM resulted in the near depletion of GB and the return of cytoplasmic COS as the major storage form of choline.

View larger version (20K): [in this window] [in a new window]   FIG. 4.   Metabolic relationships of choline and three of its derivatives in biological systems. The known reactions (solid lines) and the proposed conversion of GB to betaine aldehyde (broken lines) are shown. The latter two reactions depict the activation of the GB carboxyl group to form [X], followed by the reductive cleavage of [X] to betaine aldehyde and an unknown activating acidic agent (not shown). `SO4,' activated SO4.