Decomposition of mangrove leaf litter with different quality and its effects on the organic carbon components and sources in sediments

IF 2.6 3区 地球科学 Q1 MARINE & FRESHWATER BIOLOGY
Jianxiang Feng , Lixia You , Long Wei , Yilai You , Zhengzheng Sun , Zhenxiong Yang
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Abstract

Litter decomposition is the process through which organic matter produced by mangroves is transferred to the sediment, with the stabilization of leaf litter carbon in sediment organic matter being crucial for mitigating climate change. This study analyzed the dynamics of carbon and nutrient release during litter decomposition through indoor ex situ controlled experiments and further traced the flow of litter carbon using carbon isotope labeling to quantify the proportion of litter carbon contributing to sediment carbon. Sediment organic carbon (SOC) content exhibited no significant change following short-term litter decomposition, indicating that respiration loss and water dissolution accompanied decomposition, and high-quality leaf litter input may balance sediment carbon loss. During short-term decomposition, 49.8 %–83.5 % of leaf litter carbon was decomposed, with 7.4 %–27.8 % of litter carbon fixed in sediment organic matter as mineral-associated organic carbon (MAOC), and 6.4 %–54.0 % as particulate organic carbon (POC), influenced by litter quality. High-quality leaf litter resulted in greater accumulation of both POC and MAOC, with higher MAOC transfer efficiency. Litter input promoted the production of ‘new carbon’ but did not significantly affect the total sediment MAOC, suggesting that new carbon formation may be accompanied by the loss of native carbon. The results provide important data on the key destinations of mangrove leaf litter carbon, highlight the importance of quantifying litter-derived carbon stabilization in mangrove sediments. Future research should prioritize quantifying lateral carbon exports (e.g., particulate and dissolved forms) and respiratory losses to fully understand mangrove blue carbon budgets.
不同质量红树林凋落叶的分解及其对沉积物中有机碳组分和来源的影响
凋落物分解是红树林产生的有机物向沉积物转移的过程,而稳定凋落物中沉积物有机质中的碳对减缓气候变化至关重要。本研究通过室内非原位控制实验分析凋落物分解过程中碳和养分释放的动态,并利用碳同位素标记进一步追踪凋落物碳的流动,量化凋落物碳对沉积物碳的贡献比例。短期凋落叶分解后沉积物有机碳(SOC)含量变化不显著,说明分解过程中伴随着呼吸损失和水分溶解,而优质凋落叶的输入可以平衡沉积物碳损失。在短期分解过程中,凋落叶碳被分解的比例为49.8% ~ 83.5%,其中7.4% ~ 27.8%的凋落叶碳以矿物伴生有机碳(MAOC)形式固定在沉积物有机质中,6.4% ~ 54.0%的凋落叶碳以颗粒有机碳(POC)形式固定在沉积物有机质中。高质量凋落叶对POC和MAOC的积累都有较大的影响,MAOC的转移效率也较高。凋落物输入促进了“新碳”的产生,但对沉积物总MAOC的影响不显著,表明新碳的形成可能伴随着原生碳的损失。研究结果为红树林凋落叶碳的主要目的地提供了重要数据,强调了红树林沉积物中凋落叶碳稳定量化的重要性。未来的研究应优先量化横向碳输出(如颗粒和溶解形式)和呼吸损失,以充分了解红树林蓝碳预算。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
5.60
自引率
7.10%
发文量
374
审稿时长
9 months
期刊介绍: Estuarine, Coastal and Shelf Science is an international multidisciplinary journal devoted to the analysis of saline water phenomena ranging from the outer edge of the continental shelf to the upper limits of the tidal zone. The journal provides a unique forum, unifying the multidisciplinary approaches to the study of the oceanography of estuaries, coastal zones, and continental shelf seas. It features original research papers, review papers and short communications treating such disciplines as zoology, botany, geology, sedimentology, physical oceanography.
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