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Abstract The evolution of modern academic practices, analogous to the evolution of biological systems, reflects the influence of both contingency and determinism. From a theoretical perspective, how then could academic practices differ from those that were inherited? Would any alternative outcomes be more just, equitable, diverse, or inclusive? Here we present 14 alternative academic practices that might be attained upon replaying the tape of academia and evaluate their benefits and drawbacks. Oriented primarily around the physical sciences within the United States, these alternative practices reconsider common activities within the broad categories of the graduate student experience, faculty careers, evaluation methods, peer review and publication, and conference norms. Consideration of these alternative practices can guide within‐system change and large‐scale restructuring of academia to address the myriad challenges facing researchers and students. Conversely, alternative practices may introduce new issues or exacerbate existing problems. These alternative practices are meant to be imaginative, not prescriptive, and we hope their underlying ideas spur reflection and conversation on the existing practices embedded within academic culture. Readers are encouraged to complete a brief survey regarding their impressions of the alternative practices, available at the following link:rebrand.ly/AlternativePractices2024. 

Biogeochemical reactions modulate the chemical composition of the oceans and atmosphere, providing feedbacks that sustain planetary habitability over geological time. Here, we mathematically evaluate a suite of biogeochemical processes to identify combinations of reactions that stabilize atmospheric carbon dioxide by balancing fluxes of chemical species among the ocean, atmosphere, and geosphere. Unlike prior modeling efforts, this approach does not prescribe functional relationships between the rates of biogeochemical processes and environmental conditions. Our agnostic framework generates three types of stable reaction combinations: closed sets, where sources and sinks mutually cancel for all chemical reservoirs; exchange sets, where constant ocean–atmosphere conditions are maintained through the growth or destruction of crustal reservoirs; and open sets, where balance in alkalinity and carbon fluxes is accommodated by changes in other chemical components of seawater or the atmosphere. These three modes of operation have different characteristic timescales and may leave distinct evidence in the rock record. To provide a practical example of this theoretical framework, we applied the model to recast existing hypotheses for Cenozoic climate change based on feedbacks or shared forcing mechanisms. Overall, this work provides a systematic and simplified conceptual framework for understanding the function and evolution of global biogeochemical cycles.