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

被引:28
作者
Ouyang, Xiaoguang [1 ,2 ,3 ,4 ]
Kristensen, Erik [5 ]
Zimmer, Martin [6 ]
Thornber, Carol [7 ]
Yang, Zhifeng [1 ,2 ]
Lee, Shing Yip [3 ,4 ]
机构
[1] Southern Marine Sci & Engn Guangdong Lab Guangzhou, Res Ctr Ecol & Environm Coastal Area & Deep Sea, Guangzhou 511458, Peoples R China
[2] Guangdong Univ Technol, Sch Ecol Environm & Resources, Guangdong Prov Key Lab Water Qual Improvement & Ec, Guangzhou 510006, Peoples R China
[3] Chinese Univ Hong Kong, Simon FS Li Marine Sci Lab, Shatin, Hong Kong, Peoples R China
[4] Chinese Univ Hong Kong, Sch Life Sci, Shatin, Hong Kong, Peoples R China
[5] Univ Southern Denmark, Dept Biol, DK-5230 Odense, Denmark
[6] Leibniz Ctr Trop Marine Res, D-28359 Bremen, Germany
[7] Univ Rhode Isl, Dept Nat Resources Sci, Kingston, RI 02881 USA
基金
中国国家自然科学基金;
关键词
blue carbon ecosystems; carbon sinks; climate change; litter decomposition; mangroves; tidal marshes; seagrasses; and macroalgae; warming; TEMPERATURE SENSITIVITY; CO2; EFFLUX; PLANT-COMMUNITIES; MANGROVE FORESTS; NITROGEN; CONSEQUENCES; PHOSPHORUS; ENRICHMENT; EMISSIONS; DYNAMICS;
D O I
10.1111/gcb.16693
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
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 x 10(-2) day(-1) for macroalgae were higher than for seagrasses (1.7 +/- 0.2 x 10(-2) day-1), mangroves (1.6 +/- 0.1 x 10(-2) day(-1)) and tidal marshes (5.9 +/- 0.5 x 10(-3) day(-1)). 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 similar to 25 degrees C and similar to 20 degrees 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 degrees C) and high-warming conditions (4 degrees 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.
引用
收藏
页码:3806 / 3820
页数:15
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