
Postdoctoral Researcher
Dr. Zekun Meng
I am interested in Precambrian paleoenvironmental evolution and marine iron cycling. My research examines how iron was transformed, stabilized, and buried in ancient oceans, with a focus on the Proterozoic Eon and the Snowball Earth intervals. I combine sedimentary geochemistry, laboratory experiments, and numerical modeling to explore the links between marine iron cycling and Earth surface environmental change.
I am particularly interested in the processes that controlled iron precipitation, biological iron oxidation, and the distribution of different iron species and components in ancient seawater. These processes are central to understanding how iron was transported, transformed, stabilized, and ultimately buried in marine sediments, and how such mechanisms influenced the formation, decline, and reappearance of Banded Iron Formations (BIFs) through Earth history.
In addition, I study the evolution of Neoproterozoic Snowball Earth glaciations and their implications for marine iron cycling, particularly how extreme climate states may have altered ocean chemistry, iron supply, redox structure, and iron burial. By integrating geochemical records, experimental observations, and numerical models, my work aims to connect the mechanistic behavior of iron in seawater with large-scale geological patterns preserved in Precambrian sedimentary archives.
2025 Ph.D. in Geology and Geobiology, Northwest University, China
2021 M.S. in Geobiology, Northwest University, China
2018 B.S. in Geology, Northwest University, China


