River damming has been practised for millennia, with the first dams built before 2000 BCE in the Egyptian empire 1. The number of dams increased steadily prior to the Second World War, but expanded rapidly thereafter, peaking in the 1960s and 1970s, with most construction in North America and Western Europe 2. A second surge in dam construction began in the early 2000s, with over 3,700 hydroelectric dams either planned or under construction worldwide during this construction boom 3 , each with a generating capacity of >1 megawatt (MW). Many of the new dams are being constructed in South America, Asia and the Balkans, largely driven by the need to expand energy production in growing economies 3,4. Indeed, by 2015, dammed reservoirs supplied around 30-40% of irrigation water globally 5,6 , and 16.6% of the world's electricity was generated by hydropower 7. Almost two-thirds of the world's long rivers (that is, those >1,000 km) are no longer free-flowing 8 and the current surge in dam construction-motivated by the 2016 Paris Agreement and the need for greater renewable energy generation-is expected to double river fragmentation by 2030 (ref. 9). Accordingly, freshwater ecosystems have been referred to as the 'biggest losers' of the Paris Agreement 10. Nutrients, such as carbon (C), nitrogen (N), phosphorus (P) and silicon (Si), are transported and transformed along the land-ocean aquatic continuum (LOAC), forming the basis for freshwater and, ultimately, marine food webs.