Phytoliths of sago palms (
Metroxylon sagu Rottb.) in three soil profiles (94 cm depth) that were collected in Pangasugan (coastal area, western part of Leyte), Julita (slightly interior lowland area, eastern part of Leyte), and Dulag (coastal area, eastern part of Leyte) in the Philippines in 2019 were used as indicators for reconstructing plant communities and evaluating sago palm cultivation. All three soils were classified as Eutropepts, which are dominant in colored minerals such as augite, hypersthene, hornblende, and iron compounds. Arecaceae phytoliths were categorized into five groups; spheroid echinate (including
M. sagu phytoliths), globular echinate, hat-shaped to conical, ellipsoid echinate, and others. Spheroid echinate phytoliths in soils at the three sites accounted for 6-76 % of the whole, and their content was especially high at depths of 0-16.5 cm in the Pangasugan profile (57 %), 16.5-32 cm in the Julita profile (58 %), and 32-63 cm in the Dulag profile (76%). In the Dulag soil profile, the frequency percentage of spheroid echinate phytoliths was high throughout the layers, except at depths of 63-78.5 cm and 78.5-94 cm. The dominant sizes of spheroid echinate phytoliths were 5-10 μm (47.0%) for Pangasugan, 5-10 μm (24.7%) and 10-15 μm (30.9%) for Julita, and <15 μm (25.4-27.0%) for Dulag. Based on the gathering of the small spheroid echinate phytoliths in the surface layer in the Pangasugan soil profile and that of the large spheroid echinate phytoliths in the subsurface layers in the Julita and Dulag soil profiles, it was concluded that sago palm cultivation started in recent years in western Leyte, whereas it has continued for a long period in eastern Leyte.
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