Abstract
Several protein stability tests have been proposed, but as their results are not always consistent, wine-makers may hesitate when determining a bentonite dose. The chemical composition of the naturally occurring protein precipitate of a Sauvignon blanc wine was compared with the precipitates obtained after using different protein stability tests. Chemical composition, molecular exclusion profiles, and electrophoresis profiles of stability test precipitates were compared with naturally occurring precipitate. All forced precipitates presented different chemical compositions than the naturally occurring precipitate. None of the tests is a perfect reproduction of the natural phenomenon. The slow heat test does not precipitate thaumatin-like proteins and the ethanol test precipitates a large quantity of polysaccharide, making neither test suitable. Results indicate the fast heat test is most similar to the natural precipitate in terms of its chemical composition and therefore is likely the most appropriate stability test. The results offer a thorough comparison of the chemical composition of a natural protein precipitate and precipitates obtained after applying different stability tests.
The appearance of protein haze is one of the major problems in bottled wines (Bayly and Berg 1967, Hsu and Heatherbell 1987b, Waters et al. 1991). Some of the proteins in white and rosé wines can be denatured, which leads to the appearance of a haze or in some cases a precipitate. However, protein instability does not correlate well with total protein concentration because individual proteins behave differently (Bayly and Berg 1967, Hsu and Heatherbell 1987b). Some authors have suggested that other factors may also play an important role in protein precipitation (Waters et al. 1995, Siebert 1999), including sulfate (Pocock et al. 2007).
Several studies into the chemical nature of unstable proteins have been conducted. Bayly and Berg (1967) stated that the proteins with the lowest isoelectric points (pI) were the most unstable during the slow heat test. These data were confirmed by Hsu and Heatherbell (1987b), who reported that unstable proteins have a low pI (4.1–5.8) and a low relative molecular mass (13–30 kDa). Some years later, pathogenesis-related proteins, thaumatin-like proteins, and chitinases were identified as causes of haze (Waters et al. 1991, 1996, 1998). More recently, our research group has identified the presence of thaumatin-like proteins (VvTL1), β-(1–3)-glucanase, and the ripening-related protein Grip22 precursor in natural precipitates using MALDI-TOF/TOF (Esteruelas et al. 2009). These proteins all have a molecular weight between 20 and 45 kDa. Therefore, unstable proteins are present mainly within this range of molecular weight.
Since protein haze represents a major problem, wine-makers frequently treat white and rosé wines with bentonite in order to remove unstable proteins (Hsu and Heatherbell 1987a). Bentonite interacts electrostatically with proteins, which produces flocculation (Hsu and Heatherbell 1987a, Hsu et al. 1987). However, it has been demonstrated that bentonite treatment negatively affects the flavor (Lubbers et al. 1996) and texture (Guillou et al. 1998) of wine. Moreover, bentonite treatment is especially detrimental to sparkling wines because it drastically affects the quality and persistence of its foam (Martinez-Rodriguez and Polo 2003, Vanrell et al. 2007). Consequently, alternative treatments such as ultrafiltration (Hsu et al. 1987), chitin (Vincenzi et al. 2005), and zirconium oxide (Salazar et al. 2006) have been suggested, although their use is still experimental.
Selecting the correct dosage of bentonite for stabilizing wines is essential to its correct application. However, there are many different methods for estimating the protein stability of white wines (Berg and Akiyoshi 1961, Mesrob et al. 1983, Dubourdieu et al. 1988, Toland et al. 1996, Sarmento et al. 2000, Borrot and Gresser 2000), and they differ in their results. Consequently, the calculated dose of bentonite necessary for stabilizing a wine may vary depending on the method used, representing a major challenge for enologists because there is always a certain degree of uncertainty when determining the minimum dose of bentonite to ensure the protein stability of a given wine.
The different protein stability tests can be classified according to their mechanisms of action (Boulton 1980, Mesrob et al. 1983, Dawes et al. 1994, Sarmento et al. 2000). The Bentotest and trichloroacetic acid (TCA) tests precipitate all the proteins in the sample and these methods have been reported to overestimate the amount of bentonite needed (Berg and Akiyoshi 1961, Dubourdieu et al. 1988, Dawes et al. 1994, Toland et al. 1996). Heat tests are probably the most commonly used method by the wine industry. However, different procedures have been described in the literature, which has led to some confusion and has caused reproducibility problems at different wineries (Dubourdieu et al. 1988, Toland et al. 1996, Sarmento et al. 2000). All versions of the heat test are based on the accelerated oxidation, condensation, and precipitation of phenolic compounds with proteins at high temperatures (Sarmento et al. 2000). Heat tests usually select a lower dose of bentonite to stabilize wine than other tests (Dubourdieu et al. 1988, Sarmento et al. 2000).
The ethanol test is based on decreasing the dielectric constant of the solution, which reduces protein solubility (Lehninger 1981). The ammonium sulfate test precipitates proteins using a high salt concentration (salting out), but the precipitatation is incomplete (Stryer 1975). The tannin precipitation test is based on the assumption that proteins precipitate in wine during storage by binding to phenolic compounds, such as tannins. This test provides information on the ability of some wine proteins to be precipitated by polyphenolic compounds. The tannin test is influenced by many intrinsic factors of wine: pH, total protein, and concentrations of iron, potassium, and copper. Hence, it is not a good indicator of the optimum dose of bentonite (Sarmento et al. 2000). Finally, the Prostab stability test kit (Borrot and Gresser 2000) has been recently introduced on the market, but no information is available on its mechanism of action.
The aim of this work was to compare the chemical composition of a naturally occurring protein precipitate of a Sauvignon blanc wine with the precipitates obtained after applying the different protein stability tests in order to identify which tests are the most similar. The following eight stability tests were examined: fast heat, slow heat, tannin, ethanol, trichloroacetic acid (TCA), ammonium sulfate, Bentotest, and Prostab.
Materials and Methods
Chemicals.
All products were of high purity and suitable for fast protein liquid chromatography (FPLC). All solutions were previously filtered through 0.22 μm acetate cellulose filters (Millipore GSE) and degassed using an ultrasonic water bath.
Wine samples.
Research was carried out in 2006 at the experimental winery of the Faculty of Oenology in Tarragona (Rovira i Virgili University) in Constanti, A.O.C. Tarragona, Spain. Two thousand kg of Sauvignon blanc grapes were harvested at a sugar concentration of 210 g/L and with a titratable acidity of 6.9 g/L (expressed as tartaric acid). Grapes were pressed with a yield of 65% grape juice and 60 mg/L sulfur dioxide was added to protect the must against oxidation and microbiological spoilage. After cold settling (16°C), the must was inoculated with 20 g/L dry active yeasts (EC1118; Lallemand, Montreal, Canada). Once the alcoholic fermentation was complete, the wine was racked, sulfited (40 mg/L), and stored at 4°C for one month. Wine was centrifuged (10 min at 12,000 g), filtered (0.45 μm), and used for the stability tests. Simultaneously, 40-mL samples of wine were bottled and stored at room temperature (20–25°C) until natural precipitation occurred. Analytical parameters of the wine were 12.8% v/v ethanol, 6.2 g/L titratable acidity (expressed as tartaric acid), and pH 3.10.
Stability tests.
All stability tests were performed in triplicate. All samples were equilibrated at room temperature (25°C) before measuring their turbidity.
Fast heat:
40 mL wine was subjected to a temperature of 90°C for 1 hr in a thermostatic water bath, followed by a temperature of 4°C for 6 hr in a refrigerator (Sarmento et al. 2000).
Slow heat:
40 mL wine was stored at a temperature of 60°C for 4 days, and then maintained at 4°C for 6 hr (Sarmento et al. 2000).
Bentotest:
This reagent is a commercial solution of phosphomolybdic acid in hydrochloric acid. 4 mL Bentotest solution (Richard Wagner, Alzey, Germany) was added to 40 mL wine. The solution was then inverted three times and maintained for 20 min at room temperature (Toland et al. 1996).
Tannin:
1.0 g enological wood tannin (Proenol, Gaia, Portugal) was dissolved in 10 mL distilled water at 70°C. When the tannin was well dissolved, 50 mL distilled water was then added and ethanol was added to make a total volume of 100 mL. 3.2 mL tannin solution was added to 40 mL wine. The solution was mixed, maintained at room temperature for 15 min, and then placed in a boiling water bath for 3 min (Mesrob et al. 1983).
Ammonium sulfate:
2.1 mL saturated solution of ammonium sulfate was added to 40 mL wine. The solution was then heated for 7 hr at 55°C (Toland et al. 1996).
Trichloroacetic acid (TCA):
4 mL trichloroacetic acid solution (55% w/v) was added to 40 mL wine. The solution was then heated in boiling water for 2 min (Berg and Akiyoshi 1961).
Ethanol:
40 mL pure ethanol was added to an equal volume of wine and maintained in closed tubs at room temperature for 2 hr (Sarmento et al. 2000).
Prostab:
A Prostab Kit (Martin Vialatte Œnologie, Epernay, France) was used. According to the manufacturer’s instructions, 4 mL of reagent 1 was added to 40 mL wine. The mixture was homogenized and then 4 mL of reagent 2 was added. After homogenization, the solution was maintained at room temperature for 20 min.
Measure of turbidity.
Samples were well stirred before reading to prevent sedimentation. Developed turbidity was measured against a blank using a Hach 2100N Turbidimeter (Hach Company, Loveland, CO). All stability tests were performed in triplicate.
Selection of bentonite dose for wine stabilization.
A total of 2 g natural sodic bentonite in powder form (Volclay, Laffort, Renteria, Spain) was carefully hydrated with 100 mL deionized water. This mixture was maintained at room temperature for 24 hr before use. 1-L wine samples were added to enough bentonite solution to arrive at final concentrations of 0, 100, 200, 300, 400, 500, 600, 700, 800, 900, and 1000 mg/L (corresponding to industrial doses 0, 10, 20, 30, 40, 50, 60, 70, 80, 90, and 100 g/hL). After stirring, the samples were kept at room temperature for 2 hr. Aliquots of the supernatant were centrifuged and used for estimating protein stability with the different tests. In all cases, the wine was considered stable when the increase of turbidity in relation to the blank was lower than 2 NTU (Moine-Ledoux and Dubourdieu 1999).
Precipitate manipulation.
The resulting wines after natural precipitation and after the application of the different stability tests were centrifuged and the supernatant was discarded. All precipitates were dissolved in 2.6 mL 50 mM disodium phosphate with 0.2% SDS and then maintained at a temperature of 80°C for 5 min to achieve total dissolution. A total of 0.4 mL dissolved precipitate was lyophilized and stored at −20°C for subsequent gel filtration analysis.
Chemical analysis of precipitate.
The dissolved precipitates were assayed for protein using the Bradford dye-binding microassay method (Bradford 1976), polysaccharides using the phenol-sulfuric acid assay method (Segarra et al. 1995), and phenolic compounds using the Folin-Ciocalteu microassay method (Singleton et al. 1999).
Gel filtration chromatography on FPLC.
The lyophilized precipitates were dissolved in 150 μL 0.3 M ammonium acetate solution. The samples were centrifuged (5 min at 12,000 g, 4°C) and the supernatant was used directly for FPLC analysis (Canals et al. 1998). Analyses were conducted with a Superdex 75 PC 3.2/30 column on a fast protein liquid chromatography (FPLC) system (Smart System, Pharmacia, Uppsala, Sweden). The samples (50 μL) were injected and eluted with a 0.3 M ammonium acetate solution at a flow of 40 μL/min. The column eluents were continuously monitored at 280 and 320 nm using a μPeak Monitor (Pharmacia, Uppsala, Sweden).
SDS-PAGE.
Sodium dodecyl sulfate (SDS) polyacrylamide gel electrophoresis (PAGE) was performed using a precast discontinuous gel buffer system (Laemmli 1970). Phast- Gel Homogeneous 20 (Pharmacia) was used to adequately separate the proteins. Exclusion molecular fractions F1+F2 and F3, obtained from FPLC, were mixed, lyophilized, and resuspended in a buffer containing 62.5 mM Tris-HC1 (pH 6.8), 2% SDS, 5% β-mercaptoethanol, 10% glycerol, and 0.002% bromophenol blue, thus ensuring an SDS/protein ratio greater than three. The buffer volume was selected to obtain a protein concentration of 30 ng/μL for silver stain and 500 ng/μL for periodic acid-Schiff (PAS) stain. The samples were boiled for 5 min and subjected to electrophoresis.
Two molecular weight standards calibration kits for SDS-PAGE were used to determine the molecular weights (ref. 161-0304 and 161-0326; Bio-Rad, Hercules, CA). The low range molecular weight standards calibration kit was made up of phosphorylase b (97400 Da), serum albumin (66200 Da), ovalbumin (45000 Da), carbonic anhydrase (31000 Da), trypsin inhibitor (21500 Da) and lysozyme (14400 Da). The polypeptide molecular weight standards kit was made up of triosephosphate isomerase (26625 Da), myoglobin (16950 Da), α-lactalbumin (14437 Da), aprotinin (6512 Da), insulin b chain oxidized (3496 Da), and bacitracin (1423 Da). Electrophoresis was performed using a PhastSystem apparatus (Pharmacia LKB, Uppsala, Sweden) and PhastSystem Separation Technique File No.111 (Pharmacia 1990).
Stains.
The protocols for silver staining are described in Amersham Biosciences Automated Staining of Polyacrylamide Gels with Processor Plus (Pharmacia 1990). The reagents used for the silver stain were prepared according to Plus One Silver Stain Kit Protein Instructions (Pharmacia 1990). Periodic acid-Schiff (PAS) stain was carried out using a Glycoprotein Detection Kit (Sigma-Aldrich, Saint Louis, MO).
Statistical analysis.
All numeric data are expressed as the arithmetic average ± standard deviation from three replicates. Statistical comparisons between means were established with a Student t test using StatView (software for Macintosh).
Results and Discussion
The increase of turbidity after applying the different stability tests to the Sauvignon blanc wine under different bentonite doses is shown (Table 1⇓). The Bentotest and tannin test produced the highest turbidity in the unfined wine, whereas the other tests produced comparable levels. All tests indicated that the unfined wine was very unstable, in that in all cases the increase of turbidity was greater than 2 NTU. Considering this value as the threshold of protein stability (Moine-Ledoux and Dubourdieu 1999), the different tests indicate different doses of bentonite to achieve wine protein stability. Specifically, the fast heat, slow heat, TCA, tannin, and Prostab tests indicated that the wine was stable after a treatment with 60 g/hL bentonite. However, the ammonium sulfate test indicated stability with 50 g/hL bentonite, the Bentotest indicated 80 g/hL bentonite, and the ethanol test indicated that the wine remained unstable even after treatment with 100 g/hL bentonite. According to these results, the dose of bentonite needed for stabilizing wine differs depending on the test used. This discrepancy raises concerns about the accuracy of the tests and could cause winemakers to overtreat wines to ensure their absolute protein stability.
The chemical compositions of the natural precipitate and the precipitates obtained after applying the different stability tests is shown (Table 2⇓). In all cases, the application of the stability test generated more precipitate than natural precipitate: slow heat, three times more; fast heat and ammonium sulfate, four times more; Bentotest, TCA, and ethanol approximately six times more; tannin eight times more; and Prostab almost 11 times more. In addition, all forced precipitates resulted in different chemical compositions.
All the forced precipitates contained more protein, polyphenols, and polysaccharides than the natural precipitate. For proteins, the ethanol test precipitate contained twice as much protein than natural precipitate; slow heat, three times; fast heat, five times; ammonium sulfate, seven times; Bentotest, TCA, and tannin, approximately nine times; and Prostab, 16 times. For polyphenols, the ethanol and ammonium sulfate tests produced almost twice as many polyphenols as the natural precipitate; the fast and slow heat tests, Bentotest, and TCA, approximately three times; the Prostab, almost four times; and the tannin, eight times. The tannin test precipitated the most polyphenols, probably because the test uses tannin as a denaturing agent. With regard to polysaccharides, the ammonium sulfate and TCA tests precipitated approximately twice as many polysaccharides as the natural precipitate; fast heat, slow heat, and tannin test, five times; Bentotest, six times; Prostab, 10 times; and ethanol, 23 times. Therefore, none of the stability tests produced a precipitate with exactly the same chemical composition as the natural precipitate.
In a previous study (Canals et al. 1998), we proposed a method that used FPLC to separate white wine proteins into different fractions. In all the studied wines, three or four fractions were obtained by molecular exclusion chromatography: F1 with a molecular weight (MW) >100 kDa, F2 with a MW of 60 kDa, F3 with a MW between 20 and 40 kDa, and F4 with a MW <20 kDa. Depending on the wine protein concentration, F1 and F2 were either two single peaks or one overlapped peak. This method was used to study the precipitate obtained by natural precipitation and by the application of the different stability tests.
The molecular exclusion chromatograms of natural precipitate differ from those of the different precipitates, especially in their absorbance at 280 and 320 nm (Figure 1⇓). Absorbance at 280 nm is characteristic of all compounds with aromatic rings such as proteins and polyphenols, while absorbance at 320 nm is more characteristic of hydroxycinnamic acids and derivatives (Somers and Ziemelis 1985, Gómez-Alonso et al. 2007). The molecular exclusion chromatogram of the natural precipitate at 280 nm presented four major peaks corresponding to fractions F1+F2, F3, F4, and F5. The contribution of fraction F2 was relatively low and did not separate from fraction F1. However, a new fraction of very low molecular weight (F5) was identified. This fraction had been overlaid with fraction F4 in previous studies (Canals et al. 1998, Esteruelas et al. 2009), but here it was clearly separated. In contrast, the molecular exclusion chromatogram of the natural precipitate obtained at 320 nm showed only three peaks (F1+F2, F4, and F5), with lower peaks than those obtained at 280 nm. At this wavelength, F3 was not present.
Since the molecular weight of unstable proteins has been reported to range from 20 to 40 kDa (Hsu and Heatherbell 1987b, Waters et al. 1991, Esteruelas et al. 2009), haze proteins must be present in fraction F3. Therefore, the presence of the other fractions (F1+F2, F4, and F5) in the natural precipitate may be attributed to other compounds such as polyphenols, polysaccharides, and peptides. The fact that natural precipitate contains significant amounts of these compounds (Table 2⇑) coincides with this possibility. On the other hand, the chromatogram of the natural precipitate obtained at 320 nm seems to confirm the presence of hydroxycinnamic acids (or their derivatives), especially in fractions of lower molecular weight (F4 and F5).
The molecular exclusion chromatograms of natural and fast heat test precipitates presented similar profiles at 280 and 320 nm (Figure 1A⇑). However, the fractions F1+F2 and F3 of the fast heat precipitate overlap at both wavelengths, likely because the area of the peak corresponding to these fractions is much greater than in the natural precipitate. The fractions F4 and F5 were very similar to the fractions of the natural precipitate at both wavelengths. The slow heat precipitate (Figure 1B⇑) produced similar exclusion molecular fractions to the fast heat, but F4 and F5 presented slightly higher peaks and eluted somewhat earlier than similar fractions of the natural precipitate.
The molecular exclusion chromatograms of the natural and Bentotest precipitates presented the same fractions at 280 nm, but there are clear differences in their areas (Figure 1C⇑). Specifically, the Bentotest precipitate presented more of the fractions F1+F2, F3, and F4 and less of F5. At 320 nm, all the Bentotest precipitate fractions presented smaller peak areas than the natural ones.
Molecular exclusion chromatograms showed that the ammonium sulfate test generated a precipitate with the same fractions as natural precipitate (Figure 1D⇑), but with clear size differences between their peaks. At 280 nm, fractions F1+F2 and F3 overlapped and presented a larger area, whereas fractions F4 and F5 presented smaller areas. At 320 nm both profiles were more similar, although the areas of the low molecular fractions (F4 and F5) of ammonium sulfate precipitate were lower.
In the chromatograms of the natural and TCA precipitates, the fractions F1+F2 and F3 of the TCA precipitate were overlapped at 280 nm and presented a much larger area than similar fractions of natural precipitate (Figure 1E⇑). Furthermore, fractions F4 and F5 of the TCA precipitate presented slightly smaller areas and eluted somewhat earlier. At 320 nm, the area of the fractions F1+F2 were slightly larger, while the areas of fractions F4 and F5 were slightly smaller and eluted somewhat earlier.
The tannin test resulted in a precipitate with a completely different profile than the natural precipitate, probably because of the presence of added tannins (Figure 1F⇑). At 280 nm, all fractions presented much larger areas than the natural precipitate fractions and they were grouped in two major peaks, one overlapping the fractions F1+F2 and F3 and the other overlapping fractions F4 and F5. At 320 nm, fractions F1+F2 of both precipitates were very similar, but a large peak overlapping fractions F4 and F5 was present in the tannin precipitate.
Chromatograms of the natural and ethanol test precipitates gave completely different profiles, inasmuch as the ethanol precipitate generated only one major fraction of a high molecular weight (F1+F2) at both wavelengths (Figure 1G⇑). Lastly, the chromatographic profile of the Prostab test precipitate at 280 nm differed greatly from the profile of the natural precipitate (Figure 1F⇑). Although all fractions were present, all were more abundant, especially fractions F4 and F5. At 320 nm, the fractions F1+F2 were very similar, whereas fractions F4 and F5 also presented a larger area. These results suggest that some of the components of Prostab reagent are likely present in peaks F4 and F5.
It therefore appears that none of the commonly used stability tests generates a precipitate with a chromatographic profile similar to that of natural precipitate. These results are in line with data previously presented (Table 2⇑), which indicate that the chemical composition of the precipitates of all eight stability tests differ from the natural precipitate.
As noted previously, unstable proteins must be present in fraction F3. The chromatograms of precipitates of all the stability tests indicate that all the tests, with the sole exception of ethanol, present fraction F3 with an area similar to or higher than the natural precipitate. The ethanol test, however, generated a fraction F3 with a smaller area than the natural precipitate. According to these data, all eight stability tests targeted the fraction containing unstable proteins. However, all tests also generated greater areas in the other fractions compared with the natural precipitate, which would confirm that these tests also precipitate other compounds apart from unstable proteins.
As the measurement of absorbance at 280 nm is not quite specific for protein estimation, no additional information can be extracted from molecular exclusion chromatograms. As SDS-PAGE with silver stain is more specific for protein analysis, electrophoresis was conducted for the purpose of comparing natural precipitates with those obtained from the different tests. In a previous study (Esteruelas et al. 2009), we verified that direct SDS-PAGE of natural wine protein precipitate produced a large smear without good band definition. In contrast, the SDS-PAGE of the fractions obtained by molecular exclusion FPLC presented more clearly defined bands, probably because of the elimination of some interference, such as phenolic compounds (Charmont et al. 2005).
Since the unstable proteins of the natural precipitate are mainly in fraction F3 (Hsu and Heatherbell 1987b, Waters et al. 1991, Esteruelas et al. 2009), only this fraction should be analyzed. However, all stability tests produced precipitate containing more protein, polysaccharides, and phenolic compounds than the natural precipitate. Moreover, most of the stability tests generated an overlapped fraction including F1+F2 and F3. For that reason, the ensemble of fractions F1+F2+F3 of the natural and test precipitates was collected and used for SDS-PAGE analysis to determine which stability test would generate a protein precipitate most similar to the natural one.
The SDS-PAGE of fractions F1+F2+F3 of the natural and test precipitates dyed with silver stain is shown (Figure 2⇓). The natural precipitate presented a major band at 18–22 kDa and another five minor bands at 10, 11, 48, 59, and 67 kDa. Some researchers have shown that unstable proteins are mainly thaumatin-like proteins with a molecular weight of 21 kDa and chitinases with a molecular weight of 25–26 kDa (Waters et al. 1998, Pocock et al. 2000, Hayasaka et al. 2001). Our results are generally in agreement with these findings, inasmuch as the major electrophoretic band is within a molecular weight interval in the vicinity of this value. Moreover, in a previous work (Esteruelas et al. 2009), we identified the presence of a thaumatin-like protein (VVTL1) in this band using MALDI-TOF/TOF. However, chitinase was not identified in any band of the natural precipitate.
All stability test precipitates generated different bands from those generated by natural precipitate (Table 3⇓). In general terms, nearly all tests produced more bands and these bands were more intense than those of the natural precipitate (Table 3⇓, Figure 2⇑). The fast heat test precipitate presented well-defined bands, although a smear throughout the entire electrophoretic band was clearly present. Specifically, a major band at 18–25 kDa and seven other minor bands at 9, 10, 11, 37, 51, 59 and 67 kDa were detected. Two bands can be distinguished within the major band, one in the interval between 18 and 21 kDa and the other between 22 and 25 kDa. In contrast, the slow heat test presented a more intense smear and more poorly defined bands, and only five bands at 9, 10, 11, 22–25, and 67 kDa were detected. Comparison with natural precipitate indicates that neither heat test precipitates exactly the same proteins.
The fast heat test produced bands at 9, 22–25, 37, and 51 kDa that were not present in the natural precipitate. Moreover, the band at 18–21 kDa, detected in the natural precipitate, lengthened to 25 kDa in the fast heat precipitate, and it was possible to distinguish, as mentioned, two bands within this broad interval. The band at 48 kDa, present in the natural precipitate, was not detected in the fast heat precipitate.
The slow heat test produced a band at 9 kDa that was not present in the natural precipitate and did not produce bands at 48 and 59 kDa, which were present in the natural precipitate. The broad band at 18–25 kDa, observed in the fast heat test, was shortened to 22–25 kDa in the slow heat test.
All the other stability tests generated similar results. All presented a very intense band at 18–25 kDa and four other bands at 10, 11, 33, and 67 kDa. All the tests, with the exception of ammonium sulfate, also presented bands at 12 and 37 kDa. The Bentotest and Prostab presented a supplementary band at 40 and 59 kDa, respectively. The bands at 10, 11, 18–25, and 67 kDa, detected in all tests, were also present in the natural precipitate. The major band detected at 18–25 kDa in all tests was more intense and had a greater range than the natural precipitate (18–21 kDa). On the other hand, the band at 33 kDa detected in all eight tests, the bands at 12 and 37 kDa detected in the Bentotest, TCA, tannin, ethanol, and Prostab tests, and the band at 40 kDa detected only in the Bentotest were not present in the natural precipitate. The natural precipitate also presented two bands at 48 and 59 kDa; the former was not precipitated by any of the tests and the latter was only present in the fast heat and Prostab tests.
It is interesting that in this broad interval (18–25 kDa), in which mainly unstable proteins are present, natural precipitate only contains a band within 18–21 kDa, the slow heat test only contains a band at 22–25 kDa, and all other tests present both bands. As noted previously, thaumatin-like proteins have a molecular weight of 21 kDa and chitinases of 25–26 kDa (Waters et al. 1998, Pocock et al. 2000, Hayasaka et al. 2001). According to this data, it is logical to presume that the band at 18–21 kDa corresponds to thaumatin-like proteins and the band at 22–25 kDa corresponds to chitinases. Both proteins have been shown as present in this SDS-PAGE major band (Waters et al. 1996). Assuming this hypothesis, our results would indicate that natural precipitate contains thaumatin-like protein but not chitinases, the slow heat test precipitates chitinases but not thaumatin-like proteins, and all the other tests precipitate both proteins. This assumption may explain why, in a previous study using MALDI-TOF/TOF, it was possible to identify thaumatin-like proteins but not chitinases in a natural precipitate from a Sauvignon blanc wine, whereas other studies, which have worked with forced precipitates, have found both proteins (Waters et al. 1991, 1996, 1998, Pocock et al. 2000).
In SDS-PAGE of fractions F1+F2+F3 of natural and the stability test precipitates dyed with periodic acid-Schiff (PAS) stain, natural precipitate does not present any bands, whereas all the tests presented a band at the beginning of the lane (Figure 3⇓). This band was especially intense in the ethanol precipitate. These results agree with data in Table 2⇑ inasmuch as the stability tests, which precipitated a large quantity of polysaccharide, produced the most intense bands. As the natural precipitate contained very little polysaccharide, its presence was not detected in the gel. Meanwhile, all the other stability tests precipitated more polysaccharide and thus produced bands of a greater or lesser intensity. This data confirms that the ethanol test precipitated a large quantity of polysaccharide, which would explain why its use causes an overestimate of the bentonite dose needed to stabilize wine (Table 1⇑).
Conclusions
Results showed that all eight stability tests produced higher amounts of precipitate with chemical compositions different than that of the natural precipitate. All tests precipitated more protein, more polyphenols, and more polysaccharides. All tests targeted the molecular weight interval containing unstable proteins, with the sole exception of the slow heat test, which does not precipitate the 18–21 kDa range, which probably contains thaumatin-like proteins, and should therefore be abandoned. All other stability tests also precipitated other proteins that are not present in the natural precipitate. This is especially significant in the area of molecular weight between 22 and 25 kDa, which probably contains chitinases. Of all the stability tests, the fast heat test precipitates the least protein in this area and is therefore the most similar to the natural precipitate. The ethanol test precipitates a large quantity of polysaccharide, and thus likely overestimates the dose of bentonite necessary for wine stabilization. It should therefore also be abandoned. All other tests—Bentotest, ammonium sulfate, TCA, tannin, and Prostab—generated very similar results with regard to the protein composition of the precipitate. All these tests seem to precipitate nearly all the protein present in wine.
In short, all the stability tests generated precipitates very different than the natural precipitate and therefore none should be considered a perfect reproduction of the natural phenomenon. The fast heat test appears to be the most similar to the natural precipitate in terms of chemical composition, and therefore may be the most appropriate stability test.
Footnotes
Acknowledgments: The authors thank CICYT (AGL2007-66338 and AGL2004- 02309) and CDTI (Project CENIT Demeter) for financial support.
- Received November 2008.
- Revision received February 2009.
- Accepted February 2009.
- Published online September 2009
- Copyright © 2009 by the American Society for Enology and Viticulture
Literature Cited
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