Kumar Manoj, van Elsas Jan Dirk, Nissinen Riitta
Department of Biological and Environmental Science, University of Jyväskylä, Jyväskylä, Finland.
Department of Microbial Ecology, University of Groningen, Groningen, Netherlands.
Front Microbiol. 2017 Oct 13;8:1972. doi: 10.3389/fmicb.2017.01972. eCollection 2017.
Arctic and alpine biomes are most often strongly nitrogen-limited, and hence biological nitrogen fixation is a strong driver of these ecosystems. Both biomes are characterized by low temperatures and short growing seasons, but they differ in seasonality of solar radiation and in soil water balance due to underlying permafrost in the Arctic. Arcto-alpine plant species are well-adapted to the low temperatures that prevail in their habitats, and plant growth is mainly limited by the availability of nutrients, in particular nitrogen, due to slow mineralization. Nitrogen fixing bacteria are likely important for plant growth in these habitats, but very little is known of these bacteria or forces shaping their communities. In this study, we characterized the potential nitrogen fixing bacterial (PNFB) communities associated with two arcto-alpine pioneer plant species, (mountain sorrel) and (blue saxifrage), in three climate regions. Both of these plants readily colonize low nutrient mineral soils. Our goal was to investigate how climate (region) and, on the other hand, host plant and plant species shape these communities. To our knowledge, this is the first comprehensive study describing PNFB communities associated with pioneer plants in different arcto-alpine biomes. Replicate samples were taken from two arctic regions, Kilpisjärvi and Ny-Ålesund, and one alpine region, Mayrhofen. In these, the PNFB communities in the bulk and rhizosphere soils and the plant endospheres were characterized by -targeted PCR and massive parallel sequencing. The data revealed strong effects of climatic region on the dominating nitrogen fixers. Specifically, sequences related to (δ-) were present in high relative abundances in the nitrogen-fixing communities in the Mayrhofen and Kilpisjärvi regions, while members of the prevailed in the Kilpisjärvi and Ny-Ålesund regions. The bulk and rhizosphere soil as well as the endosphere communities in the Mayrhofen region were all characterized by high relative abundances of sequences related to . In contrast, the endosphere and soil (bulk or rhizosphere soil) communities in the High Arctic were highly divergent: endosphere communities in the arctic regions were shaped by spp., while sequences representing δ-, β- (in Ny-Ålesund), and (in Kilpisjärvi) dominated the soil communities. Interestingly, the major PNFB genera identified in this study have been previously identified as members of conserved core microbiomes in the endospheres and seeds of these plants by 16S rRNA gene based analyses combined with bacterial isolation, suggesting a very tight interaction between diazotrophic bacteria and these arctic pioneer plants. Overall, anaerobic bacterial taxa dominated the PNFB communities of the endospheres and rhizospheres of the two plant species in all study sites. This could indicate anoxic conditions in and around plant roots at the time of sampling (early growth season), created by melting snow and underlying permafrost.
北极和高山生物群落通常受到强烈的氮限制,因此生物固氮是这些生态系统的一个重要驱动因素。这两个生物群落的特点都是低温和生长季节短,但由于北极地区存在永久冻土,它们在太阳辐射的季节性和土壤水分平衡方面存在差异。北极-高山植物物种很好地适应了其栖息地普遍存在的低温,由于矿化缓慢,植物生长主要受到养分尤其是氮的可用性的限制。固氮细菌可能对这些栖息地的植物生长很重要,但对这些细菌或塑造其群落的力量了解甚少。在本研究中,我们对与两种北极-高山先锋植物物种(山地酢浆草)和(高山虎耳草)相关的潜在固氮细菌(PNFB)群落在三个气候区域进行了特征分析。这两种植物都很容易在低养分的矿质土壤中定殖。我们的目标是研究气候(区域)以及宿主植物和植物物种如何塑造这些群落。据我们所知,这是第一项全面描述不同北极-高山生物群落中与先锋植物相关的PNFB群落的研究。从两个北极地区基尔皮斯耶尔维和新奥尔松以及一个高山地区迈尔霍芬采集了重复样本。在这些样本中,通过靶向PCR和大规模平行测序对土壤和根际土壤以及植物内圈中的PNFB群落进行了特征分析。数据揭示了气候区域对主要固氮菌的强烈影响。具体而言,与(δ-)相关的序列在迈尔霍芬和基尔皮斯耶尔维地区的固氮群落中相对丰度较高,而在基尔皮斯耶尔维和新奥尔松地区则以的成员为主。迈尔霍芬地区的土壤和根际土壤以及内圈群落都以与相关的序列相对丰度高为特征。相比之下,高北极地区的内圈和土壤(土壤或根际土壤)群落差异很大:北极地区的内圈群落由 spp. 塑造,而代表δ-、β-(在新奥尔松)和(在基尔皮斯耶尔维)的序列主导土壤群落。有趣的是,本研究中鉴定出的主要PNFB属先前已通过基于16S rRNA基因的分析结合细菌分离被鉴定为这些植物内圈和种子中保守核心微生物群的成员,这表明固氮细菌与这些北极先锋植物之间存在非常紧密的相互作用。总体而言,在所有研究地点,厌氧细菌类群主导了这两种植物物种内圈和根际的PNFB群落。这可能表明在采样时(生长季节早期)植物根内和根周围存在缺氧条件,这是由融雪和下面的永久冻土造成的。