Trevathan-Tackett Stacey M, Kepfer-Rojas Sebastian, Malerba Martino, Macreadie Peter I, Djukic Ika, Zhao Junbin, Young Erica B, York Paul H, Yeh Shin-Cheng, Xiong Yanmei, Winters Gidon, Whitlock Danielle, Weaver Carolyn A, Watson Anne, Visby Inger, Tylkowski Jacek, Trethowan Allison, Tiegs Scott, Taylor Ben, Szpikowski Jozef, Szpikowska Grażyna, Strickland Victoria L, Stivrins Normunds, Sousa Ana I, Sinutok Sutinee, Scheffel Whitney A, Santos Rui, Sanderman Jonathan, Sánchez-Carrillo Salvador, Sanchez-Cabeza Joan-Albert, Rymer Krzysztof G, Ruiz-Fernandez Ana Carolina, Robroek Bjorn J M, Roberts Tessa, Ricart Aurora M, Reynolds Laura K, Rachlewicz Grzegorz, Prathep Anchana, Pinsonneault Andrew J, Pendall Elise, Payne Richard, Ozola Ilze, Onufrock Cody, Ola Anne, Oberbauer Steven F, Numbere Aroloye O, Novak Alyssa B, Norkko Joanna, Norkko Alf, Mozdzer Thomas J, Morgan Pam, Montemayor Diana I, Martin Charles W, Malone Sparkle L, Major Maciej, Majewski Mikołaj, Lundquist Carolyn J, Lovelock Catherine E, Liu Songlin, Lin Hsing-Juh, Lillebo Ana, Li Jinquan, Kominoski John S, Khuroo Anzar Ahmad, Kelleway Jeffrey J, Jinks Kristin I, Jerónimo Daniel, Janousek Christopher, Jackson Emma L, Iribarne Oscar, Hanley Torrance, Hamid Maroof, Gupta Arjun, Guariento Rafael D, Grudzinska Ieva, da Rocha Gripp Anderson, González Sagrario María A, Garrison Laura M, Gagnon Karine, Gacia Esperança, Fusi Marco, Farrington Lachlan, Farmer Jenny, de Assis Esteves Francisco, Escapa Mauricio, Domańska Monika, Dias André T C, de Los Santos Carmen B, Daffonchio Daniele, Czyryca Paweł M, Connolly Rod M, Cobb Alexander, Chudzińska Maria, Christiaen Bart, Chifflard Peter, Castelar Sara, Carneiro Luciana S, Cardoso-Mohedano José Gilberto, Camden Megan, Caliman Adriano, Bulmer Richard H, Bowen Jennifer, Boström Christoffer, Bernal Susana, Berges John A, Benavides Juan C, Barry Savanna C, Alatalo Juha M, Al-Haj Alia N, Adame Maria Fernanda
Deakin Marine Research and Innovation Centre, School of Life and Environmental Sciences, Deakin University, Melbourne, Victoria 3125, Australia.
Centre for Nature Positive Solutions, Biosciences and Food Technology Discipline, RMIT University, Melbourne, Victoria 3001, Australia.
Environ Sci Technol. 2024 Dec 10;58(49):21589-21603. doi: 10.1021/acs.est.4c02116. Epub 2024 Nov 25.
Patchy global data on belowground litter decomposition dynamics limit our capacity to discern the drivers of carbon preservation and storage across inland and coastal wetlands. We performed a global, multiyear study in over 180 wetlands across 28 countries and 8 macroclimates using standardized litter as measures of "recalcitrant" (rooibos tea) and "labile" (green tea) organic matter (OM) decomposition. Freshwater wetlands and tidal marshes had the highest tea mass remaining, indicating a greater potential for carbon preservation in these ecosystems. Recalcitrant OM decomposition increased with elevated temperatures throughout the decay period, e.g., increase from 10 to 20 °C corresponded to a 1.46-fold increase in the recalcitrant OM decay rate constant. The effect of elevated temperature on labile OM breakdown was ecosystem-dependent, with tidally influenced wetlands showing limited effects of temperature compared with freshwater wetlands. Based on climatic projections, by 2050 wetland decay constants will increase by 1.8% for labile and 3.1% for recalcitrant OM. Our study highlights the potential for reduction in belowground OM in coastal and inland wetlands under increased warming, but the extent and direction of this effect at a large scale is dependent on ecosystem and OM characteristics. Understanding local versus global drivers is necessary to resolve ecosystem influences on carbon preservation in wetlands.
关于地下凋落物分解动态的零散全球数据限制了我们识别内陆和沿海湿地碳保存与储存驱动因素的能力。我们在28个国家和8种大气候区的180多个湿地开展了一项全球多年研究,使用标准化凋落物来衡量“难分解”(路易波士茶)和“易分解”(绿茶)有机物质(OM)的分解情况。淡水湿地和潮汐沼泽中剩余的茶质量最高,表明这些生态系统中碳保存的潜力更大。在整个腐烂期,难分解OM的分解随着温度升高而增加,例如,温度从10℃升高到20℃,难分解OM分解速率常数增加了1.46倍。温度升高对易分解OM分解的影响取决于生态系统,与淡水湿地相比,受潮汐影响的湿地温度影响有限。根据气候预测,到2050年,湿地中易分解OM的分解常数将增加1.8%,难分解OM的分解常数将增加3.1%。我们的研究强调了在气候变暖加剧的情况下,沿海和内陆湿地地下OM减少的可能性,但这种影响在大规模上的程度和方向取决于生态系统和OM特征。了解局部和全球驱动因素对于解决生态系统对湿地碳保存的影响至关重要。