Structure, floristics and diversity of tropical montane rain forests over ultramafic soils on Mount Kinabalu (Borneo) compared with those on non-ultramafic soils
Shin-ichiro Aiba A F , Yoshimi Sawada A , Masaaki Takyu B , Tatsuyuki Seino C , Kanehiro Kitayama D and Rimi Repin E
+ Author Affiliations
- Author Affiliations
A Graduate School of Science and Engineering, Kagoshima University, Kagoshima 890-0065, Japan.
B Faculty of Regional Environmental Science, Tokyo University of Agriculture, Sakuragaoka 1-1-1, Setagaya-ku, Tokyo 156-8502, Japan.
C Faculty of Life and Environmental Sciences, University of Tsukuba, Tsukuba 305-8572, Japan.
D Graduate School of Agriculture, Kyoto University, Kyoto 606-8502, Japan.
E Sabah Parks, PO Box 10626, 88806 Kota Kinabalu, Sabah, Malaysia.
F Corresponding author. Email: aiba@sci.kagoshima-u.ac.jp
Australian Journal of Botany 63(4) 191-203 https://doi.org/10.1071/BT14238
Submitted: 12 September 2014 Accepted: 13 February 2015 Published: 23 April 2015
Abstract
We describe here the structure, floristics and diversity of tropical montane rain forests over ultramafic soils on Mount Kinabalu, Borneo, and compared them with those on non-ultramafic soils. We used 14 sample plots from 1580 to 3080 m elevation, six on ultramafic soils and eight on non-ultramafic soils, and identified all trees ≥4.8 cm diameter. The plot area ranged from 0.1 to 1 ha, the majority (nine plots) being 0.25 ha. Forests on ultramafic soils showed more stunted structure, especially at higher altitudes, than those on non-ultramafic soils and on ridges than on slopes. Species of Coniferae (Araucariaceae and Podocarpaceae) and Myrtaceae strongly dominated on ultramafic soils occupying 61–96% of basal area in each plot, compared with 22–63% on non-ultramafic soils. Among 287 species found in the 14 plots, only nine species (including four species endemic to Mount Kinabalu) were strictly restricted to ultramafic soils. Nonmetric multidimensional scaling demonstrated that elevational change in species composition was accelerated on ultramafic soils and on ridges. Tree species diversity was generally lower on ultramafic soils than on non-ultramafic soils at the comparative altitudes. Multiple regression analysis suggested that soil nutrients (phosphorus and nitrogen) could be the cause of vegetation differentiation between ultramafic and non-ultramafic soils, although the data on soil metals are lacking. Comparison of our results with those from other mountains with ultramafic soils in South-east Asia demonstrated the uniqueness of the montane rain forests over ultramafic soils on Mount Kinabalu.
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