How will global warming affect sub-Antarctic vegetation? To answer this question, it is necessary to understand the thermal environment of dominant plant species and how variation in resources affects photosynthetic responses to temperature. Our study focussed on vegetation on
Results/Conclusions
Average daytime temperature decreased by 0.7ºC per 100m altitude. However, the daily range in leaf temperatures was greater in the large-leaved megaherb, with lower minima and higher maxima. Warmer leaf temperatures and higher photosynthetic temperature optima gave Stilbocarpa similar assimilation rates to Poa when modelled for their average daytime leaf temperatures. In both species, photosynthetic temperature optima were lower at the cooler, higher altitudes. Leaf nitrogen content decreased with increasing altitude with no concurrent changes in specific leaf area. Photosynthetic capacity followed gradients in leaf nitrogen such that assimilation rates were highest near the coast and declined with altitude. The tussock grass had similar leaf nitrogen content to the megaherb, but invested more nitrogen in photosynthetic capacity. Higher photosynthetic capacity enabled Poa to function with a higher assimilation rate at lower stomatal conductance, and hence also greater water use efficiency and higher δ13C than Stilbocarpa. Stomatal closure increasingly limited assimilation rates when leaf temperatures increased above 12ºC, particularly in Stilbocarpa, implying that water deficit may limit response to warming or to increased exposure to sunny periods when leaf temperatures can exceed 12ºC. These results suggest that Poa may benefit more from warming than Stilbocarpa.