Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, China; Xainza Alpine Steppe and Wetland Ecosystem Observation Station, Xainza 853100, China.
Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, China.
Sci Total Environ. 2021 Jan 1;750:142306. doi: 10.1016/j.scitotenv.2020.142306. Epub 2020 Sep 12.
The decomposition of plant litter is a key link in global C budgets and provides strong feedback to changes in climate and biogeochemical cycles. However, the combined effects of global warming and plant litter quality on the rate of plant litter decomposition and nutrient dynamics in alpine ecosystems are still poorly understood. We conducted a warming experiment to investigate the effects of litter quality and temperature on decomposition rates and variations in nutrients of four common herbaceous plants (low-quality litter species Stipa purpurea and Carex moorcroftii and high-quality litter species Astragalus confertus and Leontopodium nanum) during 2011-2016. During the initial stages of decomposition, warming had no significant effect on the mass loss of plant litter for low-quality litter species, but in the later stages of decomposition, it had a negative effect on the mass loss across all species (P < 0.05). Litter quality was the best predictor of N and P release/immobilisation during the decomposition of aboveground plant litter. Low-quality litter had the highest immobilisation of N at about 80% of the initial remaining mass; nutrients were then released in the following stages of decomposition. However, the fraction of initial P decreased with the mass remaining during the initial and later phases of decomposition, but a short period of P immobilisation occurred in the middle phase of decomposition. For high-quality litter, the fraction of initial N and P decreased with the mass remaining during the whole decomposition process. Warming had a marginal influence on the N and P dynamics throughout the decomposition process. Our study showed that the decay of plant litter was strongly suppressed by warming climate and that the N and P dynamics on the investigated Tibetan grassland were mainly regulated by litter quality, providing valuable insights into the biogeochemical cycles of nutrients in alpine ecosystems.
植物凋落物的分解是全球碳预算中的一个关键环节,它为气候变化和生物地球化学循环的变化提供了有力的反馈。然而,全球变暖与植物凋落物质量对高山生态系统中植物凋落物分解速率和养分动态的综合影响仍知之甚少。我们进行了一项增温实验,以研究凋落物质量和温度对四种常见草本植物(低质量凋落物物种紫花针茅和毛果苔草以及高质量凋落物物种麻花艽和绵头雪兔子)凋落物分解速率和养分变化的影响,实验时间为 2011-2016 年。在分解的初始阶段,增温对低质量凋落物物种的凋落物质量损失没有显著影响,但在分解的后期,它对所有物种的质量损失都有负面影响(P < 0.05)。凋落物质量是预测地上植物凋落物分解过程中氮和磷释放/固定的最佳指标。低质量凋落物对氮的固定最高,约为初始剩余质量的 80%;然后在分解的后续阶段释放养分。然而,在分解的初始和后期阶段,初始磷的比例随着剩余质量的减少而减少,但在分解的中期会出现短时间的磷固定。对于高质量凋落物,初始氮和磷的比例随着整个分解过程中剩余质量的减少而减少。增温对整个分解过程中的氮和磷动态有轻微影响。我们的研究表明,气候变暖强烈抑制了植物凋落物的衰减,而研究藏草地的氮和磷动态主要受凋落物质量调控,为高山生态系统中养分的生物地球化学循环提供了有价值的见解。