Nanoparticles in the environment can form by natural processes or be released due to human activities 1 . Owing to limited analytical methods, the behaviour of nanoparticles in the natural environment is poorly understood and until now they have only been described by the variations in the nanoparticle size or the concentration of the element of interest. Here we show that by using inductively coupled plasma mass spectrometry to measure silver (Ag) isotope ratios it is possible to understand the transformation processes of silver nanoparticles (AgNPs) in the environment. We found that the formation and dissolution of AgNPs under natural conditions caused significant variations in the ratio of natural Ag isotopes ( 107 Ag and 109 Ag) with an isotopic enrichment factor (ε) up to 0.86‰. Furthermore, we show that engineered AgNPs have distinctly different isotope fractionation effects to their naturally formed counterparts. Further studies will be needed to understand whether isotope analysis can be used to reveal the sources of AgNPs in the environment.AgNPs are the most widely used nanomaterial due to their broad spectrum in antimicrobial activities 2 . An exponential increase in the environmental levels of AgNPs is predicted due to their rising usage and disposal levels 3,4 . As the natural abundance of Ag in the Earth's crust is extremely low (∼0.07 mg kg -1 ; ref. 5), the release of even a small mass of Ag to the environment from anthropogenic activities may lead to proportionally large deviations from natural conditions 6 . AgNPs present in the environment are normally thought to originate from human activities. However, recent studies reveal that AgNPs can also form naturally via the reduction of Ag + in natural waters mediated by dissolved organic matter (DOM) 7,8 and sunlight 9 , which implies that the level of AgNPs in the environment may be underestimated. There is evidence that AgNPs are potentially harmful for organisms and human health 1 and that AgNP loading can significantly influence important ecosystem processes 10,11 . However, little is known about the natural processes and fate of AgNPs due to the lack of proper methods to detect or trace AgNPs in environmental media.Here, we studied the variations in the stable Ag isotope ratio in the natural transformation process of AgNPs. Ag isotopes have previously been applied as chronometers for early-stage planetary differentiation 12,13 and as tracers in archaeometry 14,15 , whereas other applications are rare in the literature. Naturally occurring Ag is composed of 107 Ag and 109 Ag with approximately equal natural abundances (51.8% versus 48.2%) and subtle variations in 107 Ag/ 109 Ag ratio were observed in various terrestrial samples 16,17 . We hypothesized that variations in the natural stable isotope ratio may provide a new means to study the environmental processes of NPs. To test this hypothesis, we studied two reversible processes of AgNPs in natural waters (Fig. 1): the formation of AgNPs via the reduction of Ag + in the presence of DOM and the...