Reef-building corals harbour an astonishing diversity of microorganisms, including endosymbiotic microalgae, bacteria, archaea, and fungi. The metabolic interactions within this symbiotic consortium are fundamental to the ecological success of corals and the unique productivity of coral reef ecosystems. Over the last two decades, scientific efforts have been primarily channelled into dissecting the symbioses occurring in coral tissues. Although easily accessible, this compartment is only 2-3 mm thick, whereas the underlying calcium carbonate skeleton occupies the vast internal volume of corals. Far from being devoid of life, the skeleton harbours a wide array of algae, endolithic fungi, heterotrophic bacteria, and other boring eukaryotes, often forming distinct bands visible to the bare eye. Some of the critical functions of these endolithic microorganisms in coral health, such as nutrient cycling and metabolite transfer, which could enable the survival of corals during thermal stress, have long been demonstrated. In addition, some of these microorganisms can dissolve calcium carbonate, weakening the coral skeleton and therefore may play a major role in reef erosion. Yet, experimental data are wanting due to methodological limitations. Recent technological and conceptual advances now allow us to tease apart the complex physical, ecological, and chemical interactions at the heart of coral endolithic microbial communities. These new capabilities have resulted in an excellent body of research and provide an exciting outlook to further address the functional microbial ecology of the "overlooked" coral skeleton.
Looking below the surface: abundance and diversity of endolithic communitiesEndolithic environments-the pore spaces within solid substrates-are ubiquitous habitats for microbial life on Earth [1]. In terrestrial systems, these microenvironments typically provide protection from intense solar radiation and desiccation, as well as sources of nutrients, moisture, and substrates derived from minerals [2,3]. In marine systems, endolithic communities similarly exploit the rocky seafloors, but also dwell into limestone and mineralised skeleton of a broad range of marine animals [4,5]. A wide spectrum of boring microorganisms was already described in the late 1880s, with several species of cyanobacteria, fungi, and eukaryotic green algae known to penetrate coastal carbonate rocks and the shells of molluscs [6]. Coral endolithic microorganisms forming distinct and visible bands in the skeleton were first characterized not long after, in 1902 [7], a mere 19 years after the description of the unicellular symbiotic algae in coral tissues [8]. While the past 120 years have seen a vast improvement in our understanding of the ecology, physiology, metabolism, diversity, and genetics of Symbiodiniaceae [9], the photosynthetic microalgal symbionts inhabiting the tissue of corals, less effort was channelled into the characterization of endolithic microorganisms. Their ecological significance