Chen Quan, Zhao Qian, Li Jing, Jian Shuguang, Ren Hai
Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650, P. R. China.
University of Chinese Academy of Sciences, Beijing 100049, P. R. China.
Sci Rep. 2016 Jun 6;6:27468. doi: 10.1038/srep27468.
Sediment microorganisms help create and maintain mangrove ecosystems. Although the changes in vegetation during mangrove forest succession have been well studied, the changes in the sediment microbial community during mangrove succession are poorly understood. To investigate the changes in the sediment microbial community during succession of mangroves at Zhanjiang, South China, we used phospholipid fatty acid (PLFA) analysis and the following chronosequence from primary to climax community: unvegetated shoal; Avicennia marina community; Aegiceras corniculatum community; and Bruguiera gymnorrhiza + Rhizophora stylosa community. The PLFA concentrations of all sediment microbial groups (total microorganisms, fungi, gram-positive bacteria, gram-negative bacteria, and actinomycetes) increased significantly with each stage of mangrove succession. Microbial PLFA concentrations in the sediment were significantly lower in the wet season than in the dry season. Regression and ordination analyses indicated that the changes in the microbial community with mangrove succession were mainly associated with properties of the aboveground vegetation (mainly plant height) and the sediment (mainly sediment organic matter and total nitrogen). The changes in the sediment microbial community can probably be explained by increases in nutrients and microhabitat heterogeneity during mangrove succession.
沉积物微生物有助于创建和维持红树林生态系统。尽管红树林演替过程中植被的变化已得到充分研究,但对于红树林演替过程中沉积物微生物群落的变化却知之甚少。为了研究中国南方湛江红树林演替过程中沉积物微生物群落的变化,我们采用磷脂脂肪酸(PLFA)分析方法,并选取了从初级群落到成熟群落的以下时间序列:无植被浅滩;白骨壤群落;桐花树群落;以及木榄+红海榄群落。随着红树林演替的每个阶段,所有沉积物微生物类群(总微生物、真菌、革兰氏阳性菌、革兰氏阴性菌和放线菌)的PLFA浓度均显著增加。沉积物中微生物PLFA浓度在雨季显著低于旱季。回归分析和排序分析表明,微生物群落随红树林演替的变化主要与地上植被(主要是株高)和沉积物(主要是沉积物有机质和总氮)的性质有关。沉积物微生物群落的变化可能可以通过红树林演替过程中养分增加和微生境异质性增加来解释。