Yeh Tz-Ching, Krennmayr Kathrin, Liao Chien-Sen, Ejarque Elisabet, Schomakers Jasmin, Huang Jr-Chuan, Zehetner Franz, Hein Thomas
Institute of Hydrobiology and Aquatic Ecosystem Management University of Natural Resources and Life Sciences (BOKU) Vienna Austria.
WasserCluster Lunz (WCL) Biological Station Lunz am See Austria.
Freshw Biol. 2020 Nov;65(11):1973-1988. doi: 10.1111/fwb.13593. Epub 2020 Jul 13.
Bamboo, as a pioneer vegetation, often forms forests on bare lands after catastrophic landslides. Compared to evergreen forest soil, bamboo forest soil is much more labile, with a higher percentage of microbially derived organic carbon (OC), lower molecular weight, and lower humic acid content. We hypothesised that different terrigenous organic matter (tOM) sources with varying lability and phosphorus (P) availability select for bacterioplankton with distinct metabolic pathways.We incubated natural bacterioplankton assemblages with tOM leached from bamboo forest soil (BOM) and evergreen forest soil (EOM) and compared these to a lake water control. To test if microbial metabolism would be limited by OC or P availability of each tOM treatment, we used acetate as an extra labile OC source and phosphate as an inorganic P source. Bacterial metabolism was measured by analysing respiration via O consumption and production via tritiated thymidine (TdR) assimilation.Bacterioplankton metabolism is limited by the availability of P in BOM substrates. When using BOM, bacteria had higher enzymatic activities for phosphatase. The nutrients required for bacterial biomass seemed to be derived from organic matter. Under BOM treatment, bacterial production (BP) (0.92 ± 0.13 μg C L hr) and cell specific TdR assimilation rates (0.015 ± 0.002 10 M TdR cell hr) were low. Adding P enhanced BP (BOM 1.52 ± 0.31 and BOM 2.25 ± 0.37 μg C L hr) while acetate addition had no significant effect on BOM treatment.This indicated that the bacteria switched to using added inorganic P to respire a P-limited BOM substrate, which increased total BP and abundance, resulting in even more active respiration and lower growth efficiency. We also found higher activities for chitin-degrading enzyme β-N-acetylglucosaminidase, which is associated with N mining from aminosaccharides.Microbes using EOM, however, did not change metabolic strategies with additional acetate or/and inorganic P. This is due to higher concentrations of organic P in EOM substrates and the presence of inorganic N in the EOM leachates an alternative nutrient source. Bacteria produced β-glucosidase and leucyl-aminopeptidase in order to utilise the humic substances, which sustained greater bacterial abundance, higher BP (2.64 ± 0.39 μg C L hr), and lower cell-specific respiration. This yielded a much higher bacterial growth efficiency (15 ± 9.2%) than the lake water control.Our study demonstrated the aquatic metabolic discrepancy between tOM of different forest types. Bacterioplankton in BOM and EOM exhibit distinct metabolic responses. Bacterial metabolic strategy when using BOM implied that the supposedly stabilised biomass OM might be efficiently used by aquatic bacterioplankton. As the labile and nutrient-deficient BOM is more susceptible to the influence of additional nutrients, fertiliser residues in bamboo forest catchments might have a stronger effect on aquatic bacterial metabolic pathways. Thus, it is important to take tOM differences into consideration when building models to estimate soil carbon turnover rates along a terrestrial-aquatic continuum.
竹子作为先锋植被,常在灾难性山体滑坡后的裸地上形成森林。与常绿林土壤相比,竹林土壤更不稳定,微生物衍生有机碳(OC)的百分比更高,分子量更低,腐殖酸含量更低。我们假设,具有不同稳定性和磷(P)有效性的不同陆源有机物质(tOM)来源会选择具有不同代谢途径的浮游细菌。我们将天然浮游细菌群落与从竹林土壤(BOM)和常绿林土壤(EOM)中浸出的tOM一起培养,并将其与湖水对照进行比较。为了测试微生物代谢是否会受到每种tOM处理的OC或P有效性的限制,我们使用乙酸盐作为额外的不稳定OC源,磷酸盐作为无机P源。通过分析氧消耗来测量呼吸作用,并通过氚化胸腺嘧啶核苷(TdR)同化来测量生产,以此来测定细菌代谢。浮游细菌代谢受到BOM底物中P有效性的限制。使用BOM时,细菌的磷酸酶活性更高。细菌生物量所需的养分似乎来自有机物质。在BOM处理下,细菌产量(BP)(0.92±0.13μg C L⁻¹ hr⁻¹)和细胞特异性TdR同化率(0.015±0.002×10⁻⁶ M TdR cell⁻¹ hr⁻¹)较低。添加P提高了BP(BOM添加P后为1.52±0.31和2.25±0.37μg C L⁻¹ hr⁻¹),而添加乙酸盐对BOM处理没有显著影响。这表明细菌转而使用添加的无机P来呼吸P受限的BOM底物,这增加了总BP和丰度,导致呼吸作用更活跃且生长效率更低。我们还发现几丁质降解酶β-N-乙酰氨基葡萄糖苷酶的活性更高,这与从氨基糖中获取氮有关。然而,使用EOM的微生物在添加额外的乙酸盐或/和无机P时并未改变代谢策略。这是由于EOM底物中有机P浓度较高,且EOM浸出液中存在无机氮作为替代养分源。细菌产生β-葡萄糖苷酶和亮氨酰氨基肽酶以利用腐殖物质,这维持了更高的细菌丰度、更高的BP(2.64±0.39μg C L⁻¹ hr⁻¹)和更低的细胞特异性呼吸。这产生了比湖水对照高得多的细菌生长效率(15±9.2%)。我们的研究证明了不同森林类型的tOM之间的水生代谢差异。BOM和EOM中的浮游细菌表现出不同的代谢反应。使用BOM时的细菌代谢策略表明,原本稳定的生物质OM可能会被水生浮游细菌有效利用。由于不稳定且营养缺乏的BOM更容易受到额外养分的影响,竹林集水区中的肥料残留可能对水生细菌代谢途径有更强的影响。因此,在构建模型以估计陆地-水生连续体沿线的土壤碳周转速率时,考虑tOM差异很重要。