Lignocellulolytic and plastolytic potential of groundwater and sediment bacteria from the serpentinization-driven hyperalkaline springs

IF 2 3区 环境科学与生态学 Q3 ENVIRONMENTAL SCIENCES
Vladimir Šaraba, Tatjana Trtić-Petrović, Violeta Gajić, Predrag Dabić, Tanja Petrović Pantić, Ivana Jovanić, Jasmina Nikodinovic-Runic, Milica Ciric
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Abstract

Four serpentinization-driven hyperalkaline springs (HAS) in the Jurassic ophiolites of western Serbia, with pH values between 11.1 and 11.7, were selected to assess the lignocellulose- and plastic-degrading potential of cultivable bacteria found in both the groundwaters and sediments of the zone of emergence of the investigated occurrences. Also, the physico-chemical properties of the groundwaters and petrological and mineralogical composition of sediments were examined. The HAS investigated are cold (temperature: 14.7–19.4 °C) and low in minerals (total dissolved solids: 104.1–450.4 mg/L) and belong to the Ca2+–OH and Ca2+, Na+–OH genetic type. Ca2+ was the most abundant cation (39.7–132.7 mg/L), followed by Na+ (2.0–82.5 mg/L) in three and Mg (6.6 mg/L) in one HAS, respectively. OH was the most abundant anion (24.6–123.2 mg/L), followed by CO32− (18.0–36.2 mg/L) and Cl (12.4–71.0 mg/L) in all tested groundwaters. Binocular examination revealed that gravelly spring sediments consist predominantly of peridotite, serpentinite, carbonate and quartzite clasts, while the powder X-ray diffraction experiments identified calcite and lizardite as the main mineral phases in the silt fraction. In total, 210 groundwater and sediment isolates were screened on lignocellulose and plastic substrates, and 33.8% of all screened HAS isolates (9.1% from groundwaters and 38.4% from sediments) degraded carboxymethyl cellulose. Selected bacterial isolates were identified by partial 16S ribosomal DNA sequencing to belong to the genera Bacillus, Peribacillus, Paenibacillus and Lysinibacillus; these could have potential applications in various commercial sectors requiring cellulose degradation. All identified isolates demonstrated growth on the plastic substrates Impranil® DLN-SD (SD) and Impranil® DL 2077 (DL), while three isolates, belonging to genera Bacillus, Peribacillus and Paenibacillus, respectively, demonstrated growth on all four tested plastic substrates (SD, DL, polycaprolactone diol and bis(2-hydroxyethyl) terephthalate). These isolates should be further explored as potential candidates for bioremediation treatments of plastic-polluted groundwaters and sediments.

Abstract Image

蛇纹石化驱动的高碱性泉水中地下水和沉积物细菌的木质纤维素分解和塑性分解潜力
在塞尔维亚西部侏罗纪蛇绿岩中,选取了四个pH值在11.1至11.7之间的蛇纹岩驱动的高碱性泉(HAS),以评估在研究发生区域的地下水和沉积物中发现的可培养细菌的木质纤维素和塑料降解潜力。研究了地下水的物理化学性质和沉积物的岩石矿物组成。所研究的HAS是冷(温度:14.7-19.4°C)和低矿物质(总溶解固体:104.1-450.4 mg/L),属于Ca2+ -OH -和Ca2+, Na+ -OH -遗传型。Ca2+含量最高(39.7 ~ 132.7 mg/L),其次是Na+ (2.0 ~ 82.5 mg/L)和mg (6.6 mg/L)。所有地下水阴离子中OH−含量最多(24.6 ~ 123.2 mg/L),其次是CO32−(18.0 ~ 36.2 mg/L)和Cl−(12.4 ~ 71.0 mg/L)。结果表明,砂质春季沉积物主要由橄榄岩、蛇纹岩、碳酸盐和石英岩碎屑组成,粉末x射线衍射实验表明,粉砂组分中主要矿物相为方解石和蜥蜴石。在木质纤维素和塑料基质上共筛选到210株地下水和沉积物分离株,其中33.8%(9.1%来自地下水,38.4%来自沉积物)能降解羧甲基纤维素。经部分16S核糖体DNA测序鉴定,分离菌株属芽孢杆菌属、芽孢杆菌属、Paenibacillus属和赖氨酸芽孢杆菌属;这些可能在需要纤维素降解的各种商业部门中有潜在的应用。所有鉴定的分离株均可在塑料底物Impranil®DLN-SD (SD)和Impranil®DL 2077 (DL)上生长,而分别属于芽孢杆菌属、芽孢杆菌属和芽孢杆菌属的3株分离株可在所有4种塑料底物(SD、DL、聚己内酯二醇和双(2-羟乙基)对苯二甲酸酯)上生长。这些分离物应进一步作为塑料污染地下水和沉积物生物修复处理的潜在候选者进行探索。
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来源期刊
Aquatic Sciences
Aquatic Sciences 环境科学-海洋与淡水生物学
CiteScore
3.90
自引率
4.20%
发文量
60
审稿时长
1 months
期刊介绍: Aquatic Sciences – Research Across Boundaries publishes original research, overviews, and reviews dealing with aquatic systems (both freshwater and marine systems) and their boundaries, including the impact of human activities on these systems. The coverage ranges from molecular-level mechanistic studies to investigations at the whole ecosystem scale. Aquatic Sciences publishes articles presenting research across disciplinary and environmental boundaries, including studies examining interactions among geological, microbial, biological, chemical, physical, hydrological, and societal processes, as well as studies assessing land-water, air-water, benthic-pelagic, river-ocean, lentic-lotic, and groundwater-surface water interactions.
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