Postdoctoral Researcher
Department of Earth and Planetary Sciences
Weizmann Institute of Science
I am an isotope geochemist working on stable isotope fractionation in carbonate minerals using density functional theory (DFT), ab initio molecular dynamics (AIMD), and geochemical archive datasets. My research focuses on stable Mg, S, Ca, O, C and clumped isotope systems, carbonate-associated sulfate, impurity effects in minerals, and the geochemical applications of isotope proxies in environmental and sedimentary systems.
Natural carbonate minerals rarely form as chemically pure phases. This project investigates how magnesium, sulfate and other lattice impurities modify the local bonding environment of calcite and aragonite and alter equilibrium isotope fractionation factors. Using density functional theory and lattice-dynamics calculations, I quantify the influence of impurity concentration on Mg, S, Ca, O, C and clumped isotope systematics in carbonate minerals.
This research develops theoretical frameworks for calculating equilibrium isotope fractionation factors using density functional theory, vibrational spectroscopy and reduced partition function ratios. Applications include carbonate minerals, aqueous species, sulfates, silicates and mineral-fluid systems relevant to environmental and geological processes.
Carbonate-associated sulfate preserves valuable information about the sulfur cycle, seawater chemistry and diagenetic alteration. My work explores the structural incorporation of sulfate into carbonate minerals and the controls on sulfur and oxygen isotope fractionation between CAS and aqueous sulfate through a combination of quantum mechanical calculations and geochemical modeling.
Magnesium and calcium isotopes provide important constraints on carbonate precipitation, recrystallization, dolomitization and fluid–rock interaction. This project investigates equilibrium and kinetic controls on Mg and Ca isotope fractionation and their applications to reconstructing seawater chemistry, sedimentary diagenesis and global biogeochemical cycles.
Clumped-isotope signatures in carbonates are widely used as temperature proxies, but they can be modified during burial and diagenesis. My research combines first-principles calculations, reaction-pathway modeling and isotope thermodynamics to understand the mechanisms and rates of clumped-isotope reordering and their implications for paleoclimate reconstructions.
View complete publication list on Google Scholar
Email: chirantan.pramanik@weizmann.ac.il, chirantanp88@gmail.com