معرفی
Dr. Maximilian Hansen is a researcher at the Institute of Geosciences, Johannes Gutenberg University Mainz, specializing in speleothem research and isotope geochemistry. His work focuses on quantifying isotope fractionation processes (δ¹³C and δ¹⁸O) in speleothems through controlled laboratory experiments, aiming to improve climate proxy interpretations. Key projects include investigating kinetic isotope effects, clumped isotope thermometry, and trace element partitioning in cave carbonates.
His research integrates experimental approaches with modeling to address uncertainties in paleoclimate reconstructions. He collaborates on projects like the 'Isotope fractionation processes in stalagmite formation,' which explores atmospheric, soil, and solution-layer influences on isotopic signals. Hansen’s contributions include advancing understanding of prior calcite precipitation (PCP) biases and carbonate formation dynamics.
Publications span high-impact journals like Geochimica et Cosmochimica Acta and Nature Communications, reflecting expertise in isotope systems, geochemical modeling, and cave environment studies. His work bridges laboratory experiments and field observations to refine climate and environmental records derived from speleothems.
