Expansion and diversification of high-latitude radiolarian assemblages in the late Eocene linked to a cooling event in the southwest Pacific

• Published in: Climate of the Past
• Main Authors: Pascher, K. M., Hollis, C. J., Bohaty, S. M., Cortese, G., McKay, R. M., Seebeck, H., Suzuki, N., Chiba, K.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2015
• Subjects: article; Verlagsveröffentlichung; Antarctic; Campbell Plateau; Pacific; The Antarctic; Antarc*
• Online Access: https://doi.org/10.5194/cp-11-1599-2015; https://noa.gwlb.de/receive/cop_mods_00014602; https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00014557/cp-11-1599-2015.pdf; https://cp.copernicus.org/articles/11/1599/2015/cp-11-1599-2015.pdf

The long-term cooling trend from middle to late Eocene was punctuated by several large-scale climate perturbations that culminated in a shift to "icehouse" climates at the Eocene–Oligocene transition. We present radiolarian micro-fossil assemblage and foraminiferal oxygen and carbon stable...