Silvia Sigismondi

Planktic foraminifera-bound nitrogen isotopes across the Middle Eocene Climatic Optimum (MECO, ~40 Ma): implications for photosymbiosis and community change in the Atlantic Ocean

Impact of the Late Lutetian Thermal Maximum (41.52 Ma) on plankticforaminiferal assemblages (Site 1263, Atlantic Ocean)

Evaluating planktic foraminiferal resilience during the Middle Eocene Climatic Optimum (MECO) in the Atlantic Ocean

Impact of the Middle Eocene Climatic Optimum on Planktic Foraminiferal Resilience in the Atlantic Ocean

Impact of EECO Hyperthermals on Planktic Foraminiferal Communities

Investigating warm climatic conditions through bulk and clay mineralogy in the AlanoSection (Neo-Tethys) during the Middle Eocene Climatic Optimum (MECO, ~40 Ma)

Global Coiling Shifts in Morozovella and Ecological Resilience of Acarinina during the EECO

Planktic foraminiferal changes and the Early Eocene Climatic Optimum (EECO, ~ 53-49 Ma): crisis or resilience strategy to global warming?

The Middle Eocene Climatic Optimum (MECO) impact on Southern Atlantic planktic foraminifera (Site 702)