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. 2018 Jan 30;8:1851. doi: 10.1038/s41598-018-20009-9

Figure 1.

Figure 1

Geographic context and population characteristics for 12 Australian kelp forests. (a) The coastline of southwestern Australia is swept by the poleward flow of the warm Leeuwin Current, which creates a uniform gradient in ocean temperature of 2–3 °C across latitudes from 27°S to 35°S (annual daily mean 21.9 to 19.5 °C, respectively) (Wernberg & Smale, 2009, see also Fig. S1). Prior to the 2011 marine heat wave, kelp forests had their equatorward limit in Kalbarri (27.7°S). (b) Genetic diversity (data range: He 0.269–0.375, Na 12–21)19, (c) physiological versatility (data range: α 2.8–12.4%, ETRmax 2.3–22.2%) and (d) ecological resilience (data range: 1.2–11.1 kelps m−2)14 of kelp forests measured prior to the heat wave. (e) Ecosystem impact (data range: −86–26% change in kelp forest cover) of the 2011-extreme heat wave measured two years after the event. Latitude is shown on the y-axis for all panels and scaled population characteristics on the x-axis for panels (b–e). Lines represent linear regressions (dashed) with associated 95% confidence limits (dotted). Regression coefficients are given in Table S1. The map (Fig. 1a) was generated in Google Earth version 7.1.8.3036 (https://www.google.com/earth/; © CNES/SpotImage, Data SIO, NOAA, US Navy, NGA, GEBCO) and modified using GIMP version 2.8.14 (https://www.gimp.org/). This included drawing and adding the insert map of Australia.