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全球蓝碳生态系统大型植物凋落物分解对气候变化的响应。

Response of macrophyte litter decomposition in global blue carbon ecosystems to climate change.

机构信息

Research Centre of Ecology & Environment for Coastal Area and Deep Sea, Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, 511458, China.

Guangdong Provincial Key Laboratory of Water Quality Improvement and Ecological Restoration for Watersheds, School of Ecology, Environment and Resources, Guangdong University of Technology, Guangzhou, 510006, China.

出版信息

Glob Chang Biol. 2023 Jul;29(13):3806-3820. doi: 10.1111/gcb.16693. Epub 2023 Apr 20.

Abstract

Blue carbon ecosystems (BCEs) are important nature-based solutions for climate change-mitigation. However, current debates question the reliability and contribution of BCEs under future climatic-scenarios. The answer to this question depends on ecosystem processes driving carbon-sequestration and -storage, such as primary production and decomposition, and their future rates. We performed a global meta-analysis on litter decomposition rate constants (k) in BCEs and predicted changes in carbon release from 309 studies. The relationships between k and climatic factors were examined by extracting remote-sensing data on air temperature, sea-surface temperature, and precipitation aligning to the decomposition time of each experiment. We constructed global numerical models of litter decomposition to forecast k and carbon release under different scenarios. The current k averages at 27 ± 3 × 10  day for macroalgae were higher than for seagrasses (1.7 ± 0.2 × 10  day ), mangroves (1.6 ± 0.1 × 10  day ) and tidal marshes (5.9 ± 0.5 × 10  day ). Macrophyte k increased with both air temperature and precipitation in intertidal BCEs and with sea surface temperature for subtidal seagrasses. Above a temperature threshold for vascular plant litter at ~25°C and ~20°C for macroalgae, k drastically increased with increasing temperature. However, the direct effect of high temperatures on k are obscured by other factors in field experiments compared with laboratory experiments. We defined "fundamental" and "realized" temperature response to explain this effect. Based on relationships for realized temperature response, we predict that proportions of decomposed litter will increase by 0.9%-5% and 4.7%-28.8% by 2100 under low- (2°C) and high-warming conditions (4°C) compared to 2020, respectively. Net litter carbon sinks in BCEs will increase due to higher increase in litter C production than in decomposition by 2100 compared to 2020 under RCP 8.5. We highlight that BCEs will play an increasingly important role in future climate change-mitigation. Our findings can be leveraged for blue carbon accounting under future climate change scenarios.

摘要

蓝碳生态系统(BCEs)是应对气候变化的重要自然解决方案。然而,目前的争论质疑 BCEs 在未来气候情景下的可靠性和贡献。这个问题的答案取决于驱动碳固存和存储的生态系统过程,例如初级生产和分解,以及它们未来的速率。我们对 BCEs 中的凋落物分解率常数(k)进行了全球荟萃分析,并预测了 309 项研究中碳释放的变化。通过提取与每个实验分解时间相对应的空气温度、海表温度和降水的遥感数据,研究了 k 与气候因子之间的关系。我们构建了凋落物分解的全球数值模型,以预测不同情景下的 k 和碳释放。目前,宏观藻类的平均 k 值为 27±3×10 天,高于海草(1.7±0.2×10 天)、红树林(1.6±0.1×10 天)和潮汐沼泽(5.9±0.5×10 天)。在潮间带 BCEs 中,大型藻类的 k 值随着空气温度和降水的增加而增加,而在亚潮带海草中,k 值随着海表温度的增加而增加。在约 25°C 左右的维管束植物凋落物和约 20°C 左右的宏观藻类的温度阈值之上,k 值随温度的升高而急剧增加。然而,与实验室实验相比,野外实验中高温对 k 的直接影响被其他因素所掩盖。我们定义了“基本”和“实际”温度响应来解释这种效应。基于实际温度响应的关系,我们预测与 2020 年相比,在低(2°C)和高(4°C)变暖条件下,2100 年分解的凋落物比例将分别增加 0.9%-5%和 4.7%-28.8%。与 2020 年相比,在 RCP8.5 下,2100 年 BCEs 中凋落物碳汇将因凋落物 C 生产的增加高于分解而增加。我们强调,BCEs 将在未来应对气候变化的过程中发挥越来越重要的作用。我们的研究结果可用于未来气候变化情景下的蓝碳核算。

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