Cenozoic planktonic foraminiferal palaeoecology inferred from isotopic and trace element geochemical signals
Rehemat Bhatia1,2, Daniela N Schmidt3, Bridget Wade4, Christina J Manning5, David Mattey5, Wolfgang Muller6, John Spratt7, Marci M Robinson8, David Evans9, David Thornalley10 and Andy Ridgwell3,11, (1)University of Bristol, School of Earth Sciences, Bristol, BS8, United Kingdom, (2)University College London, Dept of Earth Sciences, London, United Kingdom, (3)University of Bristol, School of Earth Sciences, Bristol, United Kingdom, (4)University College London, Department of Earth Sciences, London, United Kingdom, (5)Royal Holloway University of London, Dept of Earth Sciences, Egham, United Kingdom, (6)Goethe University Frankfurt, Institute of Geosciences, Frankfurt am Main, Germany, (7)Natural History Museum, Core Research Laboratories, London, United Kingdom, (8)USGS, Florence Bascom Geoscience Center, Reston, United States, (9)University of St Andrews, Earth & Environmental Sciences, St Andrews, United Kingdom, (10)University College London, Department of Geography, London, United Kingdom, (11)University of California, Riverside, Department of Earth Sciences, Riverside, United States
