Key Laboratory of Algal Biology, Institute of Hydrobiology, Chinese Academy of Sciences, Wuhan, 430072, China.
Department of Geography and Earth Sciences, Aberystwyth University, Aberystwyth, SY23 3DB, UK.
Environ Microbiol Rep. 2021 Dec;13(6):884-898. doi: 10.1111/1758-2229.13011. Epub 2021 Sep 17.
Cyanobacteria, as key biocrust components, provide a variety of ecosystem functions in drylands. In this study, to identify whether a cyanobacterial community shift is involved in biocrust succession and whether this is linked to altered ecological functions, we investigated cyanobacterial composition, total carbon and nitrogen contents of biocrusts in the Gurbantunggut Desert. Our findings showed that the biocrust cyanobacteria in the Gurbantunggut desert were mostly filamentous, coexisting with abundant unicellular colonial Chroococcidiopsis. Heterocystous Nostoc, Scytonema and Tolypothrix always represented the majority of biocrust nitrogen-fixing organisms, comprising an average of 92% of the nifH gene reads. Community analysis showed a clear shift in prokaryotic community composition associated with biocrust succession from cyanobacteria- to lichen- and moss-dominated biocrusts, and filamentous non-nitrogen-fixing cyanobacteria-dominated communities were gradually replaced by nitrogen-fixing and unicellular colonial communities. Along the succession, there were concomitant reductions in cyanobacterial relative abundance, whereas Chl-a, total carbon and nitrogen contents increased. Concurrently, distinct carbon and nitrogen stores shifts occurred, implying that the main ecological contribution of cyanobacteria in biocrusts changes from carbon- to nitrogen-fixation along with the succession. Our results suggest that any activity that reverses biocrust succession will influence cyanobacterial community composition and eventually lead to large reductions in soil carbon and nitrogen stores.
蓝藻作为关键的生物结皮组成部分,在干旱地区提供了多种生态系统功能。在这项研究中,为了确定蓝藻群落的变化是否参与生物结皮演替,以及这是否与生态功能的改变有关,我们调查了古尔班通古特沙漠中生物结皮的蓝藻组成、总碳和氮含量。我们的研究结果表明,古尔班通古特沙漠的生物结皮蓝藻主要是丝状的,与丰富的单细胞群体 Chroococcidiopsis 共存。固氮蓝藻 Nostoc、Scytonema 和 Tolypothrix 总是代表生物结皮固氮生物的大部分,平均占 nifH 基因读数的 92%。群落分析显示,与生物结皮演替相关的原核生物群落组成发生了明显变化,从蓝藻到地衣和苔藓占主导地位的生物结皮,而丝状非固氮蓝藻占主导地位的群落逐渐被固氮和单细胞群体群落所取代。随着演替的进行,蓝藻的相对丰度相应减少,而 Chl-a、总碳和氮含量增加。同时,也发生了明显的碳氮储量转移,这意味着蓝藻在生物结皮中的主要生态贡献从碳固定到氮固定随着演替而发生变化。我们的研究结果表明,任何逆转生物结皮演替的活动都将影响蓝藻群落的组成,并最终导致土壤碳氮储量的大幅减少。