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Meet our Executive Committee

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CNRS, Lab. EPOC, University of Bordeaux (France)

Dr. Marion Peral

Marion is a researcher in palaeoclimatology and geochemistry. She works in particular on marine and continental carbonates at different time scales (mainly during the Neogene and the Quaternary).

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Geological Survey of Canada (Canada)

Dr. Benjamin Fosu

Benjamin's interests broadly encompass the application of stable isotope geochemistry to petrology, marine, environmental, and ore geology, focusing on carbonate archives. He's currently working on the palaeothermometry of dolomite and siderite. 

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University of Miami (USA)

Dr. Chaojin Lu

Chaojin's research focuses on the comparative carbonate sedimentology and diagenesis spanning the Precambrian to Modern using dual clumped isotopes.

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IMAU, Utrecht University (The Netherlands)

Dr. Bibhasvata Dasgupta

Bibhas's research uses traditional, compound-specific and clumped isotopologues of carbon, oxygen, hydrogen, nitrogen and lithium in naturally occurring samples of water, soil organic matter and plants lipids and more recently atmospheric greenhouse gasses, to infer hydroclimate, plant biogeochemistry and atmospheric processes. He has worked extensively on the Himalayan mountains, which combines two of his main interests: mountaineering and climatology.

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Trent University (Canada)

Dr. Minger Guo

Minger's research generates paleoclimatic reconstructions using triple oxygen isotope values of phytoliths. She also identifies how climatic parameters, such as relative humidity, affect the triple oxygen isotope values of phytoliths. 

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Goethe-Universität Frankfurt (Germany)

Dr. Philip Staudigel

Philip's research focuses on mechanistically understanding the physical and chemical processes which occur in sediments after their deposition. His current academic method applies clumped isotopes towards studying the formation and re-crystallization of carbonate minerals as sediments and cements.

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Past Members

Vrije Universiteit Brussel (Belgium)

Dr. Rebecca Doyle

Rebecca's research uses traditional stable isotope analysis, compound-specific isotope analysis and clumped isotope analysis to reconstruct paleoenvironmental conditions during the Quaternary (2.6 mya to present). Her research primarily focuses on lake sediment archives, but recently she has started analyzing speleothem and marine records. 

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