Darwin Center programs and projects2023: Reconstruction of ocean temperature and carbonate chemistry during astronomical-paced early Eocene hyperthermal events
Darwin Center publicationsStap, H.L., Sluijs, A., Thomas, E., Lourens, L.J.
(2009). Patterns and magnitude of deep sea carbonate dissolution during Eocene Thermal Maximum 2 and H2, Walvis Ridge, southeastern Atlantic Ocean
. Paleoceanography24: 1-13.
Darwin Center authors: Lourens L. J., Sluijs A., Stap L.Stap, H.L., Lourens, L.J., Thomas, E., Sluijs, A., Bohaty, S., Zachos, J.C. (2010). High-resolution deep-sea carbon and oxygen isotope records of Eocene Thermal Maximum 2 and H2. Geology38: 607- 610.
Darwin Center authors: Lourens L. J., Sluijs A., Stap L.Lucy Stap (2010). Palaeoceanographic and biotic response during early Eocene extreme global warming events.
Darwin Center authors: Stap L.Stap, H.L., Lourens, L.J., Van Dijk, A., Schouten, S., Thomas, E. (2010). Coherent pattern and timing of the carbon isotope excursion and warming during Eocene Thermal
Maximum 2 as recorded in planktic and benthic foraminifera. Geochem. Geophys. Geosyst.11, Q11011:
Darwin Center authors: Lourens L. J., Schouten S., Stap L.