Late Cenozoic atmospheric CO2 reconstruction
Understanding the role of CO2 in major climate transitions.
Understanding the role of CO2 in major climate transitions.
It is imperative to understand what is recorded by those geochemical signals before applying them for paleoenvironmental reconstructions.
The spatiotemporal heterogeneity of Neogene C4 expansion over East Asia resulted from changes in seasonal rainfall distributions paced by the latitudinal migration of the westerly jet.
Testing the possibility of discriminating abiotic and biogenic methyl groups via clumped isotologues