Md Hafijur Rahaman Khan is a Research Associate at the South China Sea Institute of Oceanology, Chinese Academy of Sciences (CAS), specializing in marine geology. His research focuses on marine sedimentology, mineralogy, and elemental and organic geochemistry, with an emphasis on sediment provenance, paleoenvironmental reconstruction, and biogeochemical cycling in marine and riverine systems. By employing high-resolution geochemical and mineralogical analyses, he investigates sediment dynamics, organic carbon sequestration, and heavy metal contamination, particularly in the Bengal Basin and the northern Bay of Bengal. His key contributions include reconstructing depositional environments and sedimentary processes in the northeastern Indian Ocean to understand past climate variability, sediment source dynamics, and long-term carbon cycling, as well as tracing sediment sources, transport pathways, and geochemical characteristics in the Ganges-Brahmaputra-Meghna River system and the northern Bay of Bengal to assess their implications for weathering processes, carbon storage, and sedimentary material fluxes. His work enhances the understanding of Earth's climatic and sedimentary processes, offering valuable insights into past and present environmental changes and contributing to broader discussions on Earth system science and marine geochemistry.
Md Hafijur Rahaman Khan is a Research Associate at the South China Sea Institute of Oceanology, Chinese Academy of Sciences (CAS), specializing in marine geology. His research focuses on marine sedimentology, mineralogy, and elemental and organic geochemistry, with an emphasis on sediment provenance, paleoenvironmental reconstruction, and biogeochemical cycling in marine and riverine systems. By employing high-resolution geochemical and mineralogical analyses, he investigates sediment dynamics, organic carbon sequestration, and heavy metal contamination, particularly in the Bengal Basin and the northern Bay of Bengal. His key contributions include reconstructing depositional environments and sedimentary processes in the northeastern Indian Ocean to understand past climate variability, sediment source dynamics, and long-term carbon cycling, as well as tracing sediment sources, transport pathways, and geochemical characteristics in the Ganges-Brahmaputra-Meghna River system and the northern Bay of Bengal to assess their implications for weathering processes, carbon storage, and sedimentary material fluxes. His work enhances the understanding of Earth's climatic and sedimentary processes, offering valuable insights into past and present environmental changes and contributing to broader discussions on Earth system science and marine geochemistry.