Blue carbon sink capacity of mangroves determined by leaves and their associated microbiome

Glob Chang Biol. 2024 Jan;30(1):e17007. doi: 10.1111/gcb.17007. Epub 2023 Nov 2.

Abstract

Mangroves play a globally significant role in carbon capture and storage, known as blue carbon ecosystems. Yet, there are fundamental biogeochemical processes of mangrove blue carbon formation that are inadequately understood, such as the mechanisms by which mangrove afforestation regulates the microbial-driven transfer of carbon from leaf to below-ground blue carbon pool. In this study, we addressed this knowledge gap by investigating: (1) the mangrove leaf characteristics using state-of-the-art FT-ICR-MS; (2) the microbial biomass and their transformation patterns of assimilated plant-carbon; and (3) the degradation potentials of plant-derived carbon in soils of an introduced (Sonneratia apetala) and a native mangrove (Kandelia obovata). We found that biogeochemical cycling took entirely different pathways for S. apetala and K. obovata. Blue carbon accumulation and the proportion of plant-carbon for native mangroves were high, with microbes (dominated by K-strategists) allocating the assimilated-carbon to starch and sucrose metabolism. Conversely, microbes with S. apetala adopted an r-strategy and increased protein- and nucleotide-biosynthetic potentials. These divergent biogeochemical pathways were related to leaf characteristics, with S. apetala leaves characterized by lower molecular-weight, C:N ratio, and lignin content than K. obovata. Moreover, anaerobic-degradation potentials for lignin were high in old-aged soils, but the overall degradation potentials of plant carbon were age-independent, explaining that S. apetala age had no significant influences on the contribution of plant-carbon to blue carbon. We propose that for introduced mangroves, newly fallen leaves release nutrient-rich organic matter that favors growth of r-strategists, which rapidly consume carbon to fuel growth, increasing the proportion of microbial-carbon to blue carbon. In contrast, lignin-rich native mangrove leaves shape K-strategist-dominated microbial communities, which grow slowly and store assimilated-carbon in cells, ultimately promoting the contribution of plant-carbon to the remarkable accumulation of blue carbon. Our study provides new insights into the molecular mechanisms of microbial community responses during reforestation in mangrove ecosystems.

红树林在碳捕获和储存方面发挥着全球性的重要作用,是海岸带地区重要的蓝碳,也是关键的碳汇。然而,这些红树林蓝碳形成的基本生物地球化学过程尚未得到充分了解,例如红树林造林活动如何通过凋落物DOM调节植物源碳向地下碳库转移的微生物机制。在这项研究中,本研究通过野外试验解决了这一知识差距:(1)使用先进的FT-ICR-MS技术解析红树林叶片碳组分特征;(2)阐述土壤微生物生物量和同化碳的分配模式;(3)对比引入树种无瓣海桑(Sonneratia apetala)和土著树种秋茄(Kandelia obovate)来源叶片碳在沉积物表面的降解潜力。结果发现,无瓣海桑S. apetala和秋茄K. obovate采用完全不同的生物地球化学循环途径:秋茄K. obovate的土壤有机碳库更大且植物源碳对其的贡献更高,其微生物群落(K-策略者占优)将同化碳分配给淀粉及蔗糖合成途径;相反,无瓣海桑S. apetala的土壤微生物群落以r-策略者主导,将同化碳主要分配至蛋白质及核苷酸合成途径。这些不同的生物化学循环途径可归因为两个树种的叶片碳特征。与秋茄K. obovate叶片相比,无瓣海桑S. apetala的叶片分子量、碳氮比及木质素含量相对较低。另外,研究还发现了,无瓣海桑的种植年龄不影响土壤对植物源碳的总体降解能力,但是显著影响木质素的厌氧降解过程。综上所述,我们认为,对于引进的无瓣海桑,新鲜叶片凋落后,迅速被微生物降解,释放出大量有利于r-策略者增殖的营养丰富的有机物(碳氮比较低),r-策略者消耗同化的碳以支持自身的快速增殖,进而提高了微生物残体碳对土壤有机碳库的贡献。相比之下,富含木质素的秋茄使得土壤微生物群落以K-策略者占优,它们生长较为缓慢且主要讲同化的碳储存于细胞中,最终促进植物碳对土壤有机碳库的贡献。我们的研究为红树林生态系统重新植树造林期间微生物群落驱动的土壤有机碳库形成的分子机制提供了新的见解。.

Keywords: FT-ICR-MS; biogeochemistry; blue carbon; carbon cycling; coastal ecosystem; functional potential; mangrove restoration; metagenome sequencing; microbial biomass; microbiome.

MeSH terms

  • Carbon
  • Carbon Sequestration*
  • Ecosystem*
  • Lignin
  • Plant Leaves
  • Soil
  • Wetlands

Substances

  • Lignin
  • Carbon
  • Soil