Abstract

The world's southernmost tree has been documented along with the condition and growth pattern of the world's southernmost forest on Isla Hornos, Chile. The distribution of trees at broad scales is strongly influenced by the abiotic environment and determining the position and condition of tree limits around the world is an important way to monitor global change. This offers an ideal way to test the relationship between the biogeography of individual species and the effects of climate/climate change. The limits of trees, as all ecotones, are also useful communication points – easily understood signposts of ecosystems and their change through time. The southernmost trees in the world exist at soil temperatures that correspond to the low range of global treeline temperatures, with a climate analogous to equatorial treeline despite the high latitude (56° S). However, their fine‐scale distribution is strongly influenced by wind exposure rather than simply aspect and/or elevation, as one would expect if temperature were limiting the range. Recent establishment further south was found from core forest areas, however significant dieback along wind‐exposed edges of the contiguous forest was also noted. In contrast to the wide extension of land where boreal or subarctic forests grow in the Northern Hemisphere, in the Southern Hemisphere Isla Hornos represents a single point embedded in the ocean under much milder climatic conditions. Documented shifts in wind intensity and direction as result of larger‐scale climate change will likely continue to strongly shape the condition of these unique forests.

Highlights

  • Climate change, warming, should drive the migration of plants to higher latitudes

  • While general expectations are for expansion, both well described and less well described constraints may limit the expansion of trees around the world

  • The overarching purpose was to document the worlds’ southernmost individual tree and evaluate the world’s southernmost forest. To examine if this latitudinal extreme distribution correspond climatically to patterns identified for highaltitude treelines in other regions, to assess if the tree limits in the south appear to be climatic or some other factor, and assess if climate change is impacting health and distribution of the world’s southernmost trees

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Summary

Introduction

Warming, should drive the migration of plants to higher latitudes. Plant migration plays a significant role in global climate modelling via changes to albedo, carbon cycling and water balance. Plants are excellent bioindicators of climate change at high latitudes (Smith 1994), with trees useful. The limits of tree-form life are assumed to be temperature driven, and idea with strong global evidence (Körner and Paulsen 2004, Paulsen and Körner 2014) and as such anticipated to generally be expanding as climate warms. While general expectations are for expansion, both well described (e.g. competition with shrubs) and less well described (e.g. changes in wind patterns driven by climate change) constraints may limit the expansion of trees around the world

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