Hui Wang, Fernando T. Maestre, Nan Lü, Guang Zhao, Y Zhang, Sergio Asensio, De Shorn E. Bramble, Weiliang Chen, Michaela A. Dippold, David J. Eldridge, Juan J. Gaitán, Miguel García‐Gómez, Beatriz Gozalo, Nicolas Gross, Emilio Guirado, Yoann Le Bagousse‐Pinguet, Jaime Martínez‐Valderrama, Betty Mendoza, Victoria Ochoa, César Plaza, Hugo Sáiz, Marion Schrumpf, Carlos A. Sierra, Andrés Tangarife‐Escobar, Enrique Valencia, Sophie F. von Fromm, Cong Wang, Kai Wang, Yunqiang Wang, Sönke Zaehle, Bojie Fu, Susan Trumbore, Jianbei Huang
Abstract Reliable predictions of dryland carbon fluxes require understanding the persistence and turnover of soil organic carbon (SOC). We measure radiocarbon to quantify the age of SOC and CO 2 released from soil respiration at 97 dryland sites across six continents. Here we show that bulk SOC contains little C fixed in the past 60 years, while respired CO 2 originates from both bomb-derived recent C and millennia-old C, challenging the idea that old C is chemically or physically protected. Radiocarbon suggests mean ages of ~2100 years for bulk SOC and ~520 years for respired CO 2 , the latter far older than machine-learning (<50 years) or Earth system models predict. Aridity, net primary productivity, and SOC content are dominant predictors for radiocarbon signatures, with abrupt shifts to older C beyond an aridity threshold of ~0.87. Our findings underscore the need to incorporate the vulnerability of older carbon into models and land management strategies.