“…In addition to the structural changes described here, it is highly likely that ocean warming has affected key processes, including rates of primary productivity (Pessarrodona et al, 2019), the capture and export of carbon to adjacent habitats , resilience to physical disturbance (Wernberg et al, 2010), and habitat provision (Teagle & Smale, 2018 Moreover, several kelp deforestation events have been attributed to non-climatic stressors, such as overgrazing by sea urchins (Ling et al, 2015) or decreased water quality in coastal habitats (Connell et al, 2008). While range edge populations are likely to be particularly vulnerable to warming, recent evidence suggests that local thermal adaptation in kelps and other marine macrophytes may be commonplace (King et al, 2019). Typically, equatorward trailing range edge populations are more likely to undergo local extinctions and range contractions, whereas poleward leading-edge populations are more likely to proliferate and extend their range.…”