Sponges are the oldest extant Metazoans, with fossils dating back to the Precambrian (Li et al., 2014) and recent work supporting sponges as sister to all other animals (Feuda et al., 2017). They form an abundant and diverse component of benthic communities, with 8,866 formally described species (20,000 estimated species), that occupy both marine and freshwater habitats from the poles to the tropics (Van Soest et al., 2017). Sponges also play integral roles in ecosystem processes such as bioerosion and consolidation, benthic-pelagic coupling through their immense filtering capabilities, as well as nutrient cycling through their complex symbiosis with microorganisms (Bell, 2008; de Goeij et al., 2013; Diaz & Rüetzler, 2001). Sponges undertake this nutrient cycling using exceptionally diverse microbial communities, with over 40 microbial phyla (including candidate phyla) known to associate with sponges (Thomas et al., 2016). Nutrient levels in coastal areas have been increasing due to inputs from both point (e.g., sewage effluent) and nonpoint (e.g., agricultural and urban runoff) sources (Carpenter et al., 1998), and this has contributed to the degradation of reef ecosystems worldwide (D'Angelo & Wiedenmann, 2014; Fabricius et al., 2011). Various aspects of coral physiology (e.g., reproductive success, calcification rates and growth) are negatively impacted by elevated nutrients