1. Climate Effects on Belowground Tea Litter Decomposition Depend on Ecosystem and Organic Matter Types in Global Wetlands.
- Author
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Trevathan-Tackett SM, Kepfer-Rojas S, Malerba M, Macreadie PI, Djukic I, Zhao J, Young EB, York PH, Yeh SC, Xiong Y, Winters G, Whitlock D, Weaver CA, Watson A, Visby I, Tylkowski J, Trethowan A, Tiegs S, Taylor B, Szpikowski J, Szpikowska G, Strickland VL, Stivrins N, Sousa AI, Sinutok S, Scheffel WA, Santos R, Sanderman J, Sánchez-Carrillo S, Sanchez-Cabeza JA, Rymer KG, Ruiz-Fernandez AC, Robroek BJM, Roberts T, Ricart AM, Reynolds LK, Rachlewicz G, Prathep A, Pinsonneault AJ, Pendall E, Payne R, Ozola I, Onufrock C, Ola A, Oberbauer SF, Numbere AO, Novak AB, Norkko J, Norkko A, Mozdzer TJ, Morgan P, Montemayor DI, Martin CW, Malone SL, Major M, Majewski M, Lundquist CJ, Lovelock CE, Liu S, Lin HJ, Lillebo A, Li J, Kominoski JS, Khuroo AA, Kelleway JJ, Jinks KI, Jerónimo D, Janousek C, Jackson EL, Iribarne O, Hanley T, Hamid M, Gupta A, Guariento RD, Grudzinska I, da Rocha Gripp A, González Sagrario MA, Garrison LM, Gagnon K, Gacia E, Fusi M, Farrington L, Farmer J, de Assis Esteves F, Escapa M, Domańska M, Dias ATC, de Los Santos CB, Daffonchio D, Czyryca PM, Connolly RM, Cobb A, Chudzińska M, Christiaen B, Chifflard P, Castelar S, Carneiro LS, Cardoso-Mohedano JG, Camden M, Caliman A, Bulmer RH, Bowen J, Boström C, Bernal S, Berges JA, Benavides JC, Barry SC, Alatalo JM, Al-Haj AN, and Adame MF
- Subjects
- Tea, Climate, Ecosystem, Carbon, Temperature, Wetlands
- Abstract
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.
- Published
- 2024
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