Transuranic elements are highly reactive and form multiple oxidation states and complex species that can co‐exist, which underlies their fascinating inorganic, bioinorganic, and environmental chemistry. Because they are ubiquitous, microorganisms through their natural processes can interact with transuranic elements to change their speciation through both direct microbe‐transuranics interactions and indirect change of physical and chemical conditions in their environment. Understanding how microbial processes affect transuranic elements broadens our knowledge of fundamental transuranic chemistry, increases our understanding of the impact of biological and environmental receptors and metals on each other, and enables the development of applications in separation, remediation technologies, mammalian decorporation strategies, and nuclear repository design. Microorganisms and biogeochemical processes transform metals via numerous and varied chemical, biological, and geological processes, many of which have yet to be characterized in detail even for main group elements. The focus of this article is a brief overview of transuranic species that form in the environment and the biogeochemical processes that transform them. The primary processes that have been well studied for transuranic species are as follows: (i) complexation with inorganic/bioinorganic ligands within, and produced by, bacteria; (ii) complexation by organic ligands, including microbial metabolites, and transuranic bio‐associations; and (iii) biomineralization to form transuranic materials and mineral analogs.