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Nature Communications|July 21, 2022
Subsurface ocean warming preceded Heinrich EventsLars Max, Dirk Nürnberg, Cristiano M Chiessi, et al.Nature Communications|June 4, 2016
North Atlantic Deep Water Production during the Last Glacial MaximumJacob N W Howe, Alexander M Piotrowski, Taryn L Noble, et al.Scientific Reports|December 22, 2021
Coupled changes in western South Atlantic carbon sequestration and particle reactive element cycling during millennial-scale Holocene climate variabilityBruna B Dias, Alexander M Piotrowski, Cátia F Barbosa, et al.Scientific Reports|May 4, 2021
Meridional changes in the South Atlantic Subtropical Gyre during Heinrich StadialsTainã M L Pinho, Cristiano M Chiessi, Rodrigo C Portilho-Ramos, et al.Nature Communications|July 22, 2025
Low variability of the Atlantic Meridional Overturning Circulation throughout the HoloceneLukas Gerber, Jörg Lippold, Finn Süfke, et al.Scientific Reports|October 26, 2016
Equatorial Pacific forcing of western Amazonian precipitation during Heinrich Stadial 1Yancheng Zhang, Xu Zhang, Cristiano M Chiessi, et al.Scientific Reports|June 22, 2022
South American precipitation dipole forced by interhemispheric temperature gradientMarília C Campos, Cristiano M Chiessi, Valdir F Novello, et al.Scientific Reports|December 1, 2019
Brazilian montane rainforest expansion induced by Heinrich Stadial 1 eventJorge L D Pinaya, Francisco W Cruz, Gregório C T Ceccantini, et al.Pageof 1