Luo Ling, Meng Han, Wu Ruo-Nan, Gu Ji-Dong
College of Environmental Sciences, Sichuan Agricultural University, Huimin Road, Chengdu, 611130, People's Republic of China; Laboratory of Environmental Microbiology and Toxicology, School of Biological Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong Special Administrative Region.
Laboratory of Environmental Microbiology and Toxicology, School of Biological Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong Special Administrative Region.
Chemosphere. 2017 Jun;177:275-283. doi: 10.1016/j.chemosphere.2017.03.027. Epub 2017 Mar 8.
This study applied different concentration of NaNO solution to simulate the effect of inorganic nitrogen (N) deposition/pollution on carbon (C) storage in coastal mangrove sediment through observing the changes of enzyme activity and microbial abundance. Sediment collected from mangrove forest (MG) and intertidal zone (IZ) were incubated with different N rates (0 (control), 5 (low-N) and 20 (high-N) μg N g dry sediment, respectively). After incubation, the activities of phenol oxidase (PHO) and acid phosphatase (ACP) were enhanced, but β-glucosidase (GLU) and N-β-acetyl-glucosaminidase (NAG) activities were reduced by N addition. The altered enzymatic stoichiometries by N input implied that microbial phosphorus (P) limitation was increased, whereas C and N limitation were alleviated. Besides, N input decreased the bacterial abundance but increased fungal abundance in both types of sediment. The increased pH and soluble phenolics along with the exacerbated P limitation by N addition might explain these changes. Furthermore, sediment with N addition (except high-N treated MG sediment) showed a trend of C sequestration, which might be largely caused by the decrease of bacterial abundance and GLU activity. However, MG sediment with high-N suggested a trend of C loss, and the possible reason for this discrepancy might be the relatively higher increase of PHO and ACP activity. To better understand the influence of N deposition/pollution on C cycling, the long-term N effect on microorganisms, enzymes, and thus C storage should be paid more attention in the future.
本研究通过观察酶活性和微生物丰度的变化,应用不同浓度的硝酸钠溶液来模拟无机氮(N)沉降/污染对沿海红树林沉积物中碳(C)储存的影响。从红树林(MG)和潮间带(IZ)采集的沉积物分别以不同的氮添加量(0(对照)、5(低氮)和20(高氮)μg N g干沉积物)进行培养。培养后,酚氧化酶(PHO)和酸性磷酸酶(ACP)的活性增强,但添加氮后β-葡萄糖苷酶(GLU)和N-β-乙酰氨基葡萄糖苷酶(NAG)的活性降低。氮输入导致的酶化学计量比变化表明,微生物对磷(P)的限制增加,而对碳和氮的限制得到缓解。此外,氮输入降低了两种沉积物中的细菌丰度,但增加了真菌丰度。氮添加导致的pH值和可溶性酚类物质增加以及磷限制加剧可能解释了这些变化。此外,添加氮的沉积物(除高氮处理的MG沉积物外)呈现出碳固存的趋势,这可能主要是由于细菌丰度和GLU活性的降低。然而,高氮处理的MG沉积物呈现出碳损失的趋势,这种差异的可能原因可能是PHO和ACP活性相对较高的增加。为了更好地理解氮沉降/污染对碳循环的影响,未来应更加关注氮对微生物、酶以及碳储存的长期影响。