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Nature|March 19, 2004
A 'snowball Earth' climate triggered by continental break-up through changes in runoffYannick Donnadieu, Yves Goddéris, Gilles Ramstein, et al.Nature Communications|October 29, 2021
Assessing the importance of thermogenic degassing from the Karoo Large Igneous Province (LIP) in driving Toarcian carbon cycle perturbationsThea H Heimdal, Yves Goddéris, Morgan T Jones, et al.Science (New York, N.Y.)|August 8, 2024
Biogeographic climate sensitivity controls Earth system response to large igneous province carbon degassingJulian Rogger, Emily J Judd, Benjamin J W Mills, et al.Proceedings of the National Academy of Sciences of the United States of America|September 25, 2020
Emergence of the Southeast Asian islands as a driver for Neogene coolingYuem Park, Pierre Maffre, Yves Goddéris, et al.Science Advances|February 14, 2025
Phanerozoic icehouse climates as the result of multiple solid-Earth cooling mechanismsAndrew S Merdith, Thomas M Gernon, Pierre Maffre, et al.Nature Communications|August 4, 2022
Climate windows of opportunity for plant expansion during the PhanerozoicKhushboo Gurung, Katie J Field, Sarah A Batterman, et al.Nature Communications|July 2, 2025
Early Triassic super-greenhouse climate driven by vegetation collapseZhen Xu, Jianxin Yu, Hongfu Yin, et al.Science (New York, N.Y.)|November 6, 2020
Past climates inform our futureJessica E Tierney, Christopher J Poulsen, Isabel P Montañez, et al.Pageof 1