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claudia-bouman
Team TFS
Team TFS
Penultimate deglacial warming across the Mediterranean Sea revealed by clumped isotopes in foraminifera
L. Rodríguez-Sanz (1), S. M. Bernasconi (2), G. Marino (1,3), D. Heslop (1), I. A. Müller (2), A. Fernandez (2), K. M. Grant (1), E. J. Rohling (1,4)
1) Research School of Earth Sciences, The Australian National University, Canberra, Australia; 2) Geological Institute, ETH Zürich, Switzerland; 3) University
of Vigo, Spain; 4) Ocean and Earth Science, University of Southampton, National Oceanography Centre, Southampton, UK
Scientific Reports (2017), V7: 16572, DOI: 10.1038/s41598-017-16528-6
Here we advance the understanding of Mediterranean hydrographic variability through the penultimate glacial termination (TII) and last interglacial, by applying the clumped isotope (Δ47) paleothermometer to
planktic foraminifera with a novel data-processing approach.
  • IRMS
  • 253Plus
  • Kiel IV
  • Clumped Isotopes
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