Re-evaluating the general dynamic theory of oceanic island biogeography

  • Steinbauer M
  • Dolos K
  • Field R
  • et al.
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Abstract

The general dynamic model of oceanic island biogeography integrates temporal changes in ecological circumstances with diversification processes, and has stimulated current research in island biogeography. In the original publication, a set of testable hypotheses was analysed using regression models: specifically, whether island data for four diversity indices are consistent with the ‘B~ATT²’ model, in which B is a diversity index, A is log(area) and T is time. The four indices were species richness, the number and percentage of single-island endemic species, and a diversification index. Whether the relationships between these indices and time are unimodal (i.e., ‘hump-shaped’) was a key focus, based on the characteristic ontogeny of a volcanic oceanic island. However, the significance testing uninten- tionally used zero, rather than the mean of the diversity index, as the null hypothesis, greatly inflating F- values and reducing P-values compared with the standard regression approach. Here we first re-analyze the data used to evaluate the general dynamic model in the seminal paper, using the standard null hy- pothesis, to provide an important qualification of its empirical results. This supports the significance of about half the original tests, the rest becoming non-significant but mostly suggestive of the hypothe- sized relationship. Then we expand the original analysis by testing additional, theoretically derived func- tional relationships between the diversity indices, island area and time, within the framework of the ATT² model and using a mixed-effects modelling approach. This shows that species richness peaks ear- lier in island life-cycles than endemism. Area has a greater effect on species richness and the number of single-island endemics than on the proportion of single-island endemics and the diversification index, and was always better fit as a log–log relationship than as a semi-log one. Finally, the richness–time rela- tionship is positively skewed, the initial rise happening much more quickly than the later decline.

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Steinbauer, M. J., Dolos, K., Field, R., Reineking, B., & Beierkuhnlein, C. (2013). Re-evaluating the general dynamic theory of oceanic island biogeography. Frontiers of Biogeography, 5(3). https://doi.org/10.21425/f5fbg19669

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