Characterisation and palaeoenvironmental significance of amber from the Tukau Formation, NW Sarawak, Malaysia

Cover-1
Author : Yi Ning Fong*, Dominique Dodge-Wan, Prasanna Mohan Viswanathan
Publication : Warta Geologi
Page : 20-28
Volume Number : 52
Year : 2026
DOI : https://doi.org/10.7186/wg521202603

Warta Geologi, Vol. 52, No. 1, April 2026, pp. 20-28

Characterisation and palaeoenvironmental significance of amber from the Tukau Formation, NW Sarawak, Malaysia

Yi Ning Fong*, Dominique Dodge-Wan, Prasanna Mohan Viswanathan

Department of Applied Sciences, Faculty of Engineering and Science, Curtin University Malaysia,

CDT 250, 98009 Miri, Sarawak, Malaysia

*Corresponding author email address: yining.fong@postgrad.curtin.edu.my

Abstract: Amber fragments recovered in situ from the Tukau Formation (Middle Miocene to Pliocene) in northwest Sarawak were analysed to assess their physical and chemical characteristics. Amber samples were collected from ten different localities and underwent diagnostic tests to evaluate hardness, solvent solubility, buoyancy, UV fluorescence, and burning reaction. The samples display melting points above 160 °C, hardness between 3-4 on the Mohs scale, non-reactivity to acetone, and a characteristic resinous odour upon heating, properties consistent with fossil amber. Fourier Transform Infrared (FTIR) spectra reveal consistent absorption bands at approximately 2920, 2863, 1694, 1454, 1374, 1042, and 887 cm-1, and display absorption patterns comparable to fossil dipterocarp (Class II) resins and distinct from succinite. When considered together with the diagnostic physical properties and the Neogene age of the host sediments, these observations support classification of the material as fossil amber rather than weakly polymerised resin. The spectral profile closely corresponds to that of resins from Dipterocarpaceae trees, suggesting a tropical lowland forest origin. The preservation of amber within fluvio-deltaic to shallow marine deposits indicates burial under conditions favourable for the preservation of organic matter. Tukau amber is thus comparable to Neogene dipterocarp-derived amber elsewhere in Borneo, providing insights into Miocene palaeoenvironments and vegetation in the region.

Keywords: Borneo amber, Tukau Formation, palaeoenvironment, Miocene, Dipterocarpaceae

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Manuscript received 26 November 2025;
Received in revised form 6 January 2026;
Accepted 11 February 2026
Available online 30 April 2026

DOI: https://doi.org/10.7186/wg521202603

0126-5539; 2682-7549 / Published by the Geological Society of Malaysia.
© 2026 by the Author(s). This is an open access article distributed under the terms of the Creative Commons Attribution (CC-BY) License 4.0