Bioprecipitation is the concept of rain-making bacteria and was proposed by David Sands from Montana State University in the 1970s.[1] This is precipitation that is beneficial for microbial and plant growth, it is a feedback cycle beginning with land plants generating small air-borne particles called aerosols that contain microorganisms that influence the formation of clouds by their ice nucleation properties. [2] The formation of ice in clouds is required for snow and most rainfall. Dust and soot particles can serve as ice nuclei, but biological ice nuclei are capable of catalyzing freezing at much warmer temperatures.[3] The ice-nucleating bacteria currently known are mostly plant pathogens. Recent research suggests that bacteria may be present in clouds as part of an evolved process of dispersal.[4]
^Morris, Cindy E., et al. “Bioprecipitation: A feedback cycle linking Earth history, ecosystem dynamics and land use through biological ice nucleators in the atmosphere.” Global Change Biology, vol. 20, no. 2, 2013, pp. 341–351, doi:10.1111/gcb.12447.
^Cilliers, C., Neveling, O., Tichapondwa, S. M., Chirwa, E. M. N., & Brink, H. G. (2022). “Microbial pb(ii)-bioprecipitation: Characterising Responsible Biotransformation Mechanisms.” Journal of Cleaner Production, 374, 133973. doi:10.1016/j.jclepro.2022.133973