植物生态学报

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川西高寒窄叶鲜卑花灌丛凋落枝和凋落叶生产与分解研究

陈诚智,高钰森,罗力嘉,王东   

  1. 西华师范大学
  • 收稿日期:2024-09-11 修回日期:2024-12-19 出版日期:2025-01-27 发布日期:2025-01-27

Twig and leaf litter production and decomposition in an alpline Sibiraea angustata shrubland of western Sichuan

Cheng-Zhi CHEN,Yu-Sen GAO,Li-Jia Luo,Dong Wang   

  1. 西华师范大学
  • Received:2024-09-11 Revised:2024-12-19 Online:2025-01-27

摘要: 高寒灌丛因其较高的土壤碳储量及对全球变化的敏感性,已成为全球碳循环研究的热点区域。凋落枝和凋落叶在陆地生态系统物质循环中起着重要作用,但有关二者生产与分解的对比研究还十分缺乏,难以准确评估其对土壤碳和养分循环的影响差异。基于此,本研究以青藏高原东部的优势灌丛——窄叶鲜卑花 (Sibiraea angustata)为研究对象,连续四年监测了凋落枝和凋落叶的生产与分解,并量化其碳氮残留量。结果表明:(1)凋落叶的年均生产量为凋落枝的4.41倍,分别为138.94 g·m?2·a?1和31.48 g·m?2·a?1,使凋落叶具有较高的碳氮归还量;(2)凋落枝的分解速率显著低于凋落叶,其分解常数分别为0.356 a-1和0.522 a-1,且凋落枝分解的最终残留比例为凋落叶的4.86倍,分别为0.287和0.059;(3)在四年的分解过程中,凋落叶中的氮动态表现为净释放模式,而凋落枝则为“富集—稳定—释放”模式;(4)凋落枝和凋落叶的年均碳残留量较为接近(3.85 g?m-2?a-1和3.72 g?m-2?a-1),但凋落叶的氮残留量更高(0.06 g?m-2?a-1和0.11 g?m-2?a-1)。该研究明确了凋落枝慢速分解在高寒灌丛碳储量累积中的关键作用,以及凋落叶高效氮归还对缓解土壤氮限制的重要性,为准确评估凋落枝和凋落叶对土壤碳氮循环的贡献提供了重要依据。

关键词: 凋落物生产, 凋落物分解, 碳氮归还, 青藏高原, 高寒灌丛

Abstract: Aims Alpine shrublands are crucial for global carbon cycle due to their substantial soil carbon storage and sensitivity to global changes. Twig and leaf litter play a crucial role in terrestrial ecosystem carbon and nutrient cycling; however, comparative studies on their production and decomposition remain limited. This knowledge gap hinders accurate assessments of their contributions to soil carbon and nutrient cycling. Methods This study investigated the annual production, decomposition rates, and carbon and nitrogen retention of twig and leaf litter in an alpine shrubland ecosystem on the eastern margin of the Qinghai–Tibetan Plateau of China over a four-year period. Important findings Results found that: (1) Leaf litter production (138.94 g·m?2·a?1) was 4.41 times higher than twig litter production (31.48 g·m?2·a?1). Thus, leaf litter had a higher annual carbon and nitrogen inputs than twig litter. (2) Decomposition rate of twig litter (K = 0.356 a-1) was significantly slower than that of leaf litter (K = 0.522 a-1). The proportion of recalcitrant fraction of twig litter during decomposition was 4.86 times higher than that of leaf litter (0.287 vs. 0.059, respectively). (3) Nitrogen release patterns differed between twig and leaf litter: leaf litter exhibited a net nitrogen release, while twig litter followed a pattern of “enrichment—stabilization—release”. (4) After four years of decomposition, the estimated annual carbon retention of twig and leaf litter was similar (3.85 g?m-2?a-1 for twig litter and 3.72 g?m-2?a-1 for leaf litter). However, leaf litter retained significantly more nitrogen than twig litter (0.11 g?m-2?a-1 vs. 0.06 g?m-2?a-1). This study highlights the complementary roles of twig litter in promoting carbon accumulation in alpine shrubland due to its slower decomposition. In contrast, leaf litter plays a more crucial role in alleviating soil nitrogen limitation due to its faster nitrogen release and higher nitrogen return. Our results provide valuable foundation for accurately assessing the contributions of twig and leaf litter to soil carbon and nitrogen cycling.

Key words: Litterfall production, litter decomposition, carbon and nitrogen inputs, Tibetan Plateau, alpine shrubland