“…Temporal and spatial fluctuations in chemical conditions in shallow waters mainly result from the interaction between biological activity and hydrodynamic forcing (Cyronak et al, 2018; Kapsenberg & Hofmann, 2016; Saderne et al, 2013; Wahl et al, 2018). Biological activity is the main driver of chemical variations in highly productive systems that are dominated by ‘engineer species’ (see Box 1) such as seagrass meadows, kelp forests, coral reefs or mollusc beds (Falkenberg et al, 2021). At high population densities, engineer species have the capacity to strongly modulate the chemical and physical conditions of their surrounding waters (Gutiérrez et al, 2003, 2011; Hurd et al, 2014; Kregting et al, 2013; Pujol et al, 2019; Turk et al, 2015; Unsworth et al, 2012).…”