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Transcript
Potential geographic distribution of Rhizophora apiculata Blume under
different future climate change and sea level rise scenarios
S. Record1, N.D. Charney2, M.Z. Rozainah3 & A.M. Ellison1
1
Harvard Forest, Harvard University, 324 North Main Street, Petersham, U.S.A. 01366. E-mail:
[email protected]
2
Department of Biology, University of Massachusetts, 611 North Pleasant Street, Amherst, MA 01006.
3
Institute of Biological Sciences, University of Malaya, Kuala Lumpur, Malaysia 50603.
Abstract
Species distribution models (SDMs) are a common tool used to link occurrence data and
environmental predictors to project species' potential geographic distributions in response to
climate change. While SDMs have been applied to many taxa, there are few examples of
SDMs for mangroves. We present one of the first examples of a mangrove SDM for
Rhizophora apiculata Blume. Occurrence data from the online Mangrove Reference
Database and Herbarium were used to fit the models. We chose a suite of predictor variables
that were relevant to the biology of the species and were not correlated: minimum annual air
temperature, mean annual precipitation, horizontal tide, distance from coast, and river
discharge. Models were fitted to 70% of the occurrence data using MaxEnt software and
current climate data from the Worldclim database. The remaining 30% of the occurrence data
were set aside as a holdout dataset for model validation. We projected R. apiculata's future
potential distribution in 2080 under different future climate and sea-level rise (0, 1, 3, and 6
m) scenarios.
The model exhibited excellent predictive performance with an Area Under the Operating
Curve value of 0.917 ± 0.03. An analysis estimating the relative contributions of each
predictor to the model showed that the first and second most important predictors were
distance to coast and minimum annual air temperature, respectively. Under all future climate
and sea level rise scenarios, the projected percentage of coastal R. apiculata occurrences
increased by 5-9%. These areas of increased occurrences were primarily along the western
coasts of India and northern Australia. These projections may be optimistic because the
models do not account for dispersal limitation or localities projected to be inundated with sea
level rise that have unsuitable substrate (e.g., developed urban areas).
Keywords
climate envelope, southeast Asia, Australia
154