“…For headwater environments (e.g., 1st and 2nd order streams), low flow responses can also include widespread hypoxic conditions and accumulation of reduced inorganic solutes 6 , which likely have first-order influences on aquatic organisms and community structure 40 . By comparison, for streams, rivers, and lakes embedded further down in the aquatic network, summer DOC declines are likely to have more direct ecological and biogeochemical impacts, given the role of DOC as an energy source to aquatic heterotrophs 41 , as a contributor to watercolor that restricts aquatic photosynthesis 10 and mediator of the nutritional quality of algal resources to consumers 42 . Indeed, average summer DOC concentrations for the largest stream (C16) varied by nearly three-fold over the 17 years (5.2−14.6 mg L −1 ), a range comparable to that which is thought to shape aquatic metabolic patterns across broad regional gradients in the northern hemisphere 43 .…”