TY - JOUR
T1 - Drought-induced peatland carbon loss exacerbated by elevated CO2 and warming
AU - Quan, Quan
AU - Zhou, Jian
AU - Hanson, Paul
AU - Ricciuto, Daniel
AU - Sebestyen, Stephen D.
AU - Weston, David J.
AU - Chanton, Jeffrey P.
AU - Wilson, Rachel M.
AU - Kostka, Joel E.
AU - Zhou, Yu
AU - Wei, Ning
AU - Jiang, Lifen
AU - Mayes, Melanie A.
AU - Stelling, Jonathan M.
AU - Richardson, Andrew D.
AU - Dusenge, Mirindi Eric
AU - Way, Danielle
AU - Warren, Jeffrey M.
AU - Luo, Yiqi
N1 - Publisher Copyright:
Copyright © 2025 the authors, some rights reserved
PY - 2025/10/23
Y1 - 2025/10/23
N2 - extreme drought events are predicted to increase with climate change, yet their impacts on ecosystem carbon dynamics under warming and elevated carbon dioxide (ecO2) remain unclear. In a peatland experiment with five warming treatments each under ambient carbon dioxide (acO2) and ecO2 (+500 parts per million), a 2-month extreme drought in 2021 reduced net ecosystem productivity by 444.0 ± 65.8 and 736.6 ± 57.8 grams of carbon per square meter at +9°c under acO2 and ecO2, respectively—228.6 ± 56.8% and 381.9 ± 83.4% of the reduction at +0°c under acO2. this exacerbation was driven by warming-induced water table decline, prolonged low water tables, and cO2-enhanced substrate availability through increased plant carbon inputs. Findings indicate that future climate will greatly amplify carbon loss during extreme drought, reinforcing positive carbon-climate feedbacks.
AB - extreme drought events are predicted to increase with climate change, yet their impacts on ecosystem carbon dynamics under warming and elevated carbon dioxide (ecO2) remain unclear. In a peatland experiment with five warming treatments each under ambient carbon dioxide (acO2) and ecO2 (+500 parts per million), a 2-month extreme drought in 2021 reduced net ecosystem productivity by 444.0 ± 65.8 and 736.6 ± 57.8 grams of carbon per square meter at +9°c under acO2 and ecO2, respectively—228.6 ± 56.8% and 381.9 ± 83.4% of the reduction at +0°c under acO2. this exacerbation was driven by warming-induced water table decline, prolonged low water tables, and cO2-enhanced substrate availability through increased plant carbon inputs. Findings indicate that future climate will greatly amplify carbon loss during extreme drought, reinforcing positive carbon-climate feedbacks.
UR - https://www.scopus.com/pages/publications/105019822634
UR - https://www.scopus.com/pages/publications/105019822634#tab=citedBy
U2 - 10.1126/science.adv7104
DO - 10.1126/science.adv7104
M3 - Article
C2 - 41129626
AN - SCOPUS:105019822634
SN - 0036-8075
VL - 390
SP - 367
EP - 370
JO - Science
JF - Science
IS - 6771
ER -