Hofmann Katrin, Lamprecht Andrea, Pauli Harald, Illmer Paul
Institute of Microbiology, University of Innsbruck, Innsbruck, Austria.
GLORIA coordination, Institute for Interdisciplinary Mountain Research, Austrian Academy of Sciences and Center for Global Change and Sustainability, University of Natural Resources and Life Sciences, Vienna, Austria.
Microb Ecol. 2016 Oct;72(3):704-16. doi: 10.1007/s00248-016-0803-z. Epub 2016 Jul 11.
Studies of the altitudinal distributions of soil microorganisms are rare or have led to contradictory results. Therefore, we studied archaeal and bacterial abundance and microbial-mediated activities across an altitudinal gradient (2700 to 3500 m) on the southwestern slope of Mt. Schrankogel (Central Alps, Austria). Sampling sites distributed over the alpine (2700 to 2900 m), the alpine-nival (3000 to 3100 m), and the nival altitudinal belts (3200 to 3500 m), which are populated by characteristic plant assemblages. Bacterial and archaeal abundances were measured via quantitative real-time PCR (qPCR). Moreover, microbial biomass C, microbial activity (dehydrogenase), and enzymes involved in carbon (CM-cellulase), nitrogen (protease), phosphorus (alkaline phosphatase), and sulfur (arylsulfatase) cycling were determined. Abundances, microbial biomass C, and activities almost linearly decreased along the gradient. Archaeal abundance experienced a sharper decrease, thus pointing to pronounced sensitivity toward environmental harshness. Additionally, abundance and activities were significantly higher in soils of the alpine belt compared with those of the nival belt, whereas the alpine-nival ecotone represented a transitional area with intermediate values, thus highlighting the importance of vegetation. Archaeal abundance along the gradient was significantly related to soil temperature only, whereas bacterial abundance was significantly related to temperature and dissolved organic carbon (DOC). Soil carbon and nitrogen concentrations explained most of the variance in enzyme activities involved in the cycling of C, N, P, and S. Increasing temperature could therefore increase the abundances and activities of microorganisms either directly or indirectly via expansion of alpine vegetation to higher altitudes and increased plant cover.
关于土壤微生物垂直分布的研究很少,或者得出了相互矛盾的结果。因此,我们研究了施兰科格尔山(奥地利中部阿尔卑斯山)西南坡海拔梯度(2700至3500米)上古菌和细菌的丰度以及微生物介导的活动。采样点分布在高山带(2700至2900米)、高山-雪缘带(3000至3100米)和雪缘带(3200至3500米),这些地带生长着具有特色的植物群落。通过定量实时PCR(qPCR)测定细菌和古菌的丰度。此外,还测定了微生物生物量碳、微生物活性(脱氢酶)以及参与碳(CM-纤维素酶)、氮(蛋白酶)、磷(碱性磷酸酶)和硫(芳基硫酸酯酶)循环的酶。丰度、微生物生物量碳和活性几乎沿梯度呈线性下降。古菌丰度下降更为明显,表明对环境恶劣程度具有显著敏感性。此外,与雪缘带土壤相比,高山带土壤中的丰度和活性显著更高,而高山-雪缘交错带代表了一个具有中间值的过渡区域,从而突出了植被的重要性。沿梯度的古菌丰度仅与土壤温度显著相关,而细菌丰度与温度和溶解有机碳(DOC)显著相关。土壤碳和氮浓度解释了参与碳、氮、磷和硫循环的酶活性的大部分变异。因此,温度升高可能直接或间接通过高山植被向更高海拔扩展和植物覆盖增加来提高微生物的丰度和活性。