Izumi, KentaroKemp, David BItamiya, ShomaInui, Mutsuko2018-11-052018-11-052018-01-01Izumi, K, Kemp, D B, Itamiya, S & Inui, M 2018, 'Sedimentary evidence for enhanced hydrological cycling in response to rapid carbon release during the early Toarcian oceanic anoxic event', Earth and Planetary Science Letters, vol. 481, pp. 162-170. https://doi.org/10.1016/j.epsl.2017.10.0300012-821Xhttp://hdl.handle.net/2164/11392Part of this work was financially supported by JSPS KAKENHI 12J08818 and 15J08821 to KI. DBK acknowledges recipe of NERC Fellowship NE/I02089X/1 and grants from the Sasakawa Foundation of Great Britain, grant number 4883, and Daiwa Anglo-Japanese Foundation, grant number 10960/12369. This study contributes to IGCP 655. We thank M. Ikeda, T. Ohta, K. Suzuki, N. Nishida and K. Kawano for assistance in the field and/or helpful discussion. Fieldwork was carried out with full permission and support from its landowners. S. Nicoara and S. Kurokawa are thanked for analytical assistance. The comments of the Editor (D. Vance) and three reviewers (G. Suan, S. Bodin, and an anonymous reviewer) greatly improved the manuscript.93205436engSDG 14 - Life Below WaterToarciancarbon isotopehydrological cyclingsedimentologyatmospheric warmingQE GeologyNatural Environment Research Council (NERC)NE/I02089X/1QEJournal item10.1016/j.epsl.2017.10.030481