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Why tree lines are lower on islands—Climatic and biogeographic effects hold the answer
Author(s) -
Karger Dirk Nikolaus,
Kessler Michael,
Conrad Olaf,
Weigelt Patrick,
Kreft Holger,
König Christian,
Zimmermann Niklaus E.
Publication year - 2019
Publication title -
global ecology and biogeography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 3.164
H-Index - 152
eISSN - 1466-8238
pISSN - 1466-822X
DOI - 10.1111/geb.12897
Subject(s) - tree line , ecology , climate change , environmental science , precipitation , tree (set theory) , climatology , geography , physical geography , geology , biology , meteorology , mathematical analysis , mathematics
Aim To determine the global position of tree line isotherms, compare it with observed local tree limits on islands and mainlands, and disentangle the potential drivers of a difference between tree line and local tree limit. Location Global. Time period 1979–2013. Major taxa studied Trees. Methods We modelled the potential climatic tree line based on monthly temperatures and precipitation for the period 1979–2013. We then compared the potential tree line based on climate to observed tree limits at 26 oceanic islands, 55 continental islands and 382 mainland locations. The differences between potential tree line and observed tree limits was then analysed by regression with the islands’ maximum elevation, age, isolation, and area. Additionally, we estimated growing season temperature niches for 16,041 species known to occur in the vicinity of the studied tree lines, and compared them across mainlands, and islands of continental and oceanic origin. Results Observed local tree limits differ up to 2,066 m from the potential tree line at the mainland on oceanic islands. Climatic effects are responsible for a difference of up to 1,296 m between tree lines of mainland regions and oceanic islands (but only for 756 m for continental islands). On oceanic islands, a remaining difference of up to 829 m correlates with the isolation and the maximum elevation of an island. Floras of oceanic islands are however depauperate with respect to potential tree line species and species show an affinity to higher growing season temperatures. Main conclusions Climate can explain about half of the differences between observed local tree limits and potential tree lines between the mainland and continental and oceanic islands. The remaining difference can be attributed to the higher isolation of oceanic islands, especially in the tropics, and as a consequence, a more depauperate flora and a lack of tree species that are able to grow at the tree line.