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微生物群落对裙带菜释放的溶解性有机碳降解的长期响应

Long-term response of the microbial community to the degradation of DOC released from Undaria pinnatifida.

作者信息

Xie Yuyang, Su Jie, Shao Kuishuang, Hu Tian, Ming Hongxia, Shi Tingting, Wang Wenjing, Fan Jingfeng

机构信息

College of Marine Ecology and Environment, Shanghai Ocean University, Shanghai, 201306, China.

State Environmental Protection Key Laboratory of Coastal Ecosystem, National Marine Environmental Monitoring Center, Dalian, 116023, Liaoning, China.

出版信息

Mar Environ Res. 2024 Feb;194:106313. doi: 10.1016/j.marenvres.2023.106313. Epub 2023 Dec 25.

Abstract

With the aim to study the mechanism underlying the macroalgal carbon sequestration driven by microbes, we investigated the microbial community using metagenomics methods and its long-term degradation of dissolved organic carbon (DOC) derived from Undaria pinnatifida. It was observed that after removing U. pinnatifida, the concentration of the DOC decreased significantly (p < 0.05) within 4 days. Over a period of 120 days of degradation, the concentration of remaining DOC (26%) remained stable. The succession of microbial community corresponded to the three stages of DOC concentration variation. Moreover, the structure of microbes community and its metabolic function exhibited evident patterns of succession. The concentration of DOC was correlated negatively with the abundances of Planctomycetaceae (p < 0.01), and was correlated positively with the abundances of Roseobacteraceae and Rhodobacteraceae (p < 0.01). In addition, the metabolic pathways related to "Glycolysis/Gluconeogenesis", "Alanine, aspartate, and glutamate metabolism", "Citrate cycle (TCA cycle)" and "Tryptophan metabolism" was significantly correlated with the variations in DOC concentration (p < 0.05). These findings indicate that the variation in the DOC concentration was closely linked to the succession of Planctomycetaceae, Roseobacteraceae, Rhodobacteraceae, and the degradation of DOC derived from U. pinnatifida appeared to be influenced by metabolic functions.

摘要

为了研究微生物驱动大型藻类碳固存的潜在机制,我们采用宏基因组学方法研究了微生物群落及其对裙带菜衍生的溶解有机碳(DOC)的长期降解情况。观察到去除裙带菜后,DOC浓度在4天内显著下降(p<0.05)。在120天的降解期内,剩余DOC的浓度(26%)保持稳定。微生物群落的演替与DOC浓度变化的三个阶段相对应。此外,微生物群落结构及其代谢功能呈现出明显的演替模式。DOC浓度与浮霉菌科的丰度呈负相关(p<0.01),与红杆菌科和红螺菌科的丰度呈正相关(p<0.01)。此外,与“糖酵解/糖异生”、“丙氨酸、天冬氨酸和谷氨酸代谢”、“柠檬酸循环(TCA循环)”和“色氨酸代谢”相关的代谢途径与DOC浓度变化显著相关(p<0.05)。这些发现表明,DOC浓度的变化与浮霉菌科、红杆菌科、红螺菌科的演替密切相关,裙带菜衍生的DOC降解似乎受代谢功能影响。

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