Climate change has a massive impact on the global water cycle. Subsurface ecosystems, the earth largest reservoir of liquid freshwater, currently experience a significant increase in temperature and serious consequences from extreme hydrological events. Extended droughts as well as heavy rains and floods have measurable impacts on groundwater quality and availability. In addition, the growing water demand puts increasing pressure on the already vulnerable groundwater ecosystems. Global change induces undesired dynamics in the typically nutrient and energy poor aquifers that are home to a diverse and specialized microbiome and fauna. Current and future changes in subsurface environmental conditions, without doubt, alter the composition of communities, as well as important ecosystem functions, for instance the cycling of elements such as carbon and nitrogen. A key role is played by the microbes. Understanding the interplay of biotic and abiotic drivers in subterranean ecosystems is required to anticipate future effects of climate change on groundwater resources and habitats. This review summarizes potential threats to groundwater ecosystems with emphasis on climate change and the microbial world down below our feet in the water saturated subsurface. caister.com/cimb 509 Curr. Issues Mol. Biol. Vol. 41 Climate Change and Groundwater Microbes Retter et al. use (e.g. cooling agent), as well as for production of potable water. Worth mentioning, in Europe, around 50 -70 % of all drinking water stems from groundwater (Zektser and Everett, 2004). Groundwater constitutes a major component of the hydrological cycle and sustains streams, lakes, and wetlands, many of which would not be perennial without the direct connection to an aquifer. Groundwater ecosystems are typically covered by vegetated soil and vadose sediment layers of varying thickness.Where the protective layers are thin and perforated (e.g. in mountainous areas and karstic rock) or even absent, and where groundwater reaches land surface (e.g.wetlands and springs), the down below systems are highly vulnerable to disturbance from above. Moreover, due to the comparably long residence time of groundwater in the subsurface (Danielopol et al., 2003), its response time to external impacts can be delayed and sometimes masked by complex hydrologically patterns (Alley et al., 2002;Kløve et al., 2014). The subsurface is a naturally light deprived and nutrient limited environment, hence the energy required for sustaining groundwater ecosystems is largely derived from the surface. In fact, the groundwater ecosystems balance is susceptible to several external influences. It is on one hand largely dependent on energy import from the surface, but on the other hand responding sensitively to increased input of organics and nutrients as well as various types of contaminants including heavy metals and heat. While in the past, groundwater pollution mainly resulted from source contaminations with deposited or spilled petroleum hydrocarbons and halogenated solvents as well as leaking...