This session aims to bring together interdisciplinary scientists to discuss the evolution of early life, environments, biogeochemical cycles, climate, and ecology throughout Earth’s history.
The Archean to Proterozoic saw a transition from ‘prebiotic chemistry’ to a world with life, nutrient cycling, and the co-evolution of early life and environment. The Jurassic-early Cretaceous period was marked by tectonic events, volcanism, variations in paleoclimate, and the reconfiguration of paleoceanographic patterns that led to critical changes in ocean redox conditions across many basins. Among many important transitions, the Cenozoic witnessed global cooling and a long-term decline in atmospheric pCO2, shifts in the isotopic and elemental ratios of major ions in seawater, the diversification and expansion of mammalian taxa, changing fluxes from silicate weathering and sulfide oxidation, and a global deepening of the carbonate compensation depth.
This session invites contributions in early Earth to Cenozoic biogeochemistry, covering topics such as prebiotic geochemistry, nutrient element supply and cycling, the origin and early evolution of life, and the interplay between life, tectonics and the Earth's surface in the development and governance of nutrient cycles. We welcome submissions across a broad range of spatial scales (microscopic to global), approaches (isotopic, genomic, theoretical, numerical), samples (rocks, fossils, modern and ancient sediment), and disciplines (geology, surface processes, atmospheric chemistry, biological/chemical/physical oceanography, marine/terrestrial ecology, geobiology). We especially welcome submissions from early-career researchers, under-represented scientists, and any collaborative studies and discussions between scientists in academia and industry.