1 Early Jurassic climate and atmospheric CO2 concentration in the 2 Sichuan paleobasin, Southwest China 3 1 1 2 1 1 1 4 Xianghui Li , Jingyu Wang , Troy Rasbury , Min Zhou , Zhen Wei , Chaokai Zhang 5 1State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, 6 Nanjing 210023 China. 7 2Department of Geosciences, Stony Brook University, Stony Brook, NY 11794-2100, USA 8 Correpondence to: Xiangui Li (
[email protected]) 9 1 10 Abstract: Climatic oscillations had been developed through the (Early) Jurassic from marine sedimentary archives, but 11 remain unclear from terrestrial records. This work presents investigation of climate-sensitive sediments and carbon and 12 oxygen isotope analyses of lacustrine and pedogenic carbonates for the Early Jurassic Ziliujing Formation from the grand 13 Sichuan paleobasin (GSB), Southwest China. Sedimentary and stable isotope proxies manifest that an overall secular (semi-) 14 arid climate dominated the GSB during the Early Jurassic except for the Hettangian. This climate pattern is similar to the 15 arid climate in the Colorado Plateau region, western North America, but distinct from the relatively warm-humid climate in 16 North China and high latitude in Southern Hemisphere. The estimated atmospheric CO2 concentration (pCO2) from carbon 17 isotopes of pedogenic carbonates shows a range of 980-2610 ppmV (~ 3.5-10 times the pre-industrial value) with a mean of 18 1660 ppmV. Three phases of pCO2 (the Sinemurian 1500-2000 ppmV, the Pliensbachian 1000-1500 ppmV, and the early 19 Toarcian 1094-2610 ppmV) and two events of rapid falling pCO2 by ~1000-1300 ppmV are observed, illustrating the pCO2 20 perturbation in the Early Jurassic.