Skip to main content
Log in

Geochemical characteristics of a tropical lowland peat dome in the Kota Samarahan-Asajaya area, West Sarawak, Malaysia

  • Original Article
  • Published:
Environmental Earth Sciences Aims and scope Submit manuscript

Abstract

Augered tropical lowland peat samples (KS.TP.02 to 10) were characterized, classified (von post) and subjected to source rock analyses and biomarker gas chromatography mass spectrometry analyses. Lateral variations in the organic matter types within the top 0–0.5 m layer were found to occur from the margin to the mid-section to the center/near-center (i.e., thicker areas) of the studied peat dome. The organic matter types of these three regions correspond to kerogen types II, III, and II, respectively. The lateral vegetation succession, phasic community zonation and organic matter types (II and III kerogen) are most likely associated with tropical lowland peat domes. The Pr/n-C17 and Ph/n-C18 ratios for the peat samples from the same locations are low and indicate anoxic to suboxic and reducing depositional environmental conditions for the wet tropical lowland peats. The S/(S+R) ratios are relatively low, indicating the immaturity of the peats in terms of hydrocarbon production. The dominant biomarker hopane compounds have 13–39 carbon atoms, with dominant peaks exhibiting an odd over even carbon number predominance, indicating the terrestrial depositional environment of the peats. The Pr/Ph ratios most likely indicate anoxic (the marginal, relatively wet “moat area”) to suboxic (the mid-section and the basin center) depositional environmental conditions. The ββ hopanes biomarkers that indicate immaturity include ββ C30 hopane (17β, 21β (H)-Hopane) and ββ C31 hopane (17β, 21β (H)-Homohopane). Other common hopanes present are C29 hopane (Norhopane), 22Sαβ C31 hopane (17α, 21β (H)-Homohopane) and 22Rαβ C31 hopane (17α, 21β (H)-Homohopane).

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11

Similar content being viewed by others

References

  • Anderson JAR (1961) The ecology and forest types of the peat swamp forests of Sarawak and Brunei in relation to their siviculture. Dissertation, Univ. of Edinburgh, UK

  • Anderson JAR (1963) The flora of the peat swamp forests of Sarawak and Brunei, including a catalogue of all recorded species of flowering plants, ferns and fern allies. Gard Bull 20:131–228

    Google Scholar 

  • Anderson JAR (1964) The structure and development of the peat swamps of Sarawak and Brunei. J Trop Geogr 18:7–16

    Google Scholar 

  • Anderson JAR (1974) Observations on the ecology of five peat swamp forests in Sumatra and Kalimantan. Peat and podsolic soils and their potential for agriculture in Indonesia. Soil Research Institute, Bogor, pp 45–55

    Google Scholar 

  • Anderson JAR (1983) The tropical peat swamps of western Malesia. In: Gore AJP (ed) Ecosystems of the world, vol 4B., Mires: swamp, bog, fen and moorElsevier Scientific Pub. Co, Amsterdam, pp 181–199

    Google Scholar 

  • Anderson JAR, Muller J (1975) Palynological study of a holocene peat and miocene coal deposit from NW Borneo. Rev Palaeobot Palynol 19:291–351

    Article  Google Scholar 

  • Andriesse JP (1988) Nature and management of tropical peat soils, 1st edn. FAO, Rome

    Google Scholar 

  • Brooks JD, Gould K, Smith J (1969) Isoprenoid hydrocarbons in coal and petroleum. Nature 222:257–259

    Article  Google Scholar 

  • Bujang BH (2004) Organic and peat soil engineering Kuala Lumpur. University Putra Malaysia, Serdang

    Google Scholar 

  • Buwalda P (1940) Bosverkenning in de Indragirische Bovenlanden. Rep. For. Res. Sta, Bogor, Indonesia (unpub.) (Quoted by Polak, 1975)

  • Cameron CC, Esterle JS, Palmer CA (1989) The geology, botany and chemistry of selected peat-forming environments from temperate and tropical latitudes. Int J Coal Geol 12:105–156

    Article  Google Scholar 

  • Dehmer J (1993) Petrology and organic geochemistry of peat samples from a raised bog in Kalimantan (Borneo). Org Geochem 20:349–362

    Article  Google Scholar 

  • Dehmer J (1995) Petrological and organic geochemical investigation of recent peats with known environments of deposition. Int J Coal Geol 28:111–138

    Article  Google Scholar 

  • Engineering Geology Working Group (2007) Guideline for engineering geological investigation in peat and soft soils. In: Minerals and Geoscience Department of Malaysia

  • Espitalie J, Madec M, Tissot BP, Mennig JJ, Leplat P (1977) Source rock characterization method for petroleum exploration. In: Offshore technology conference, Houston, Texas

  • Esterle JS, Ferm JC (1994) Spatial variability in modern tropical peat deposits from Sarawak, Malaysia and Sumatera, Indonesia: analogues for coal. Int J Coal Geol 26:1–41

    Article  Google Scholar 

  • Farhaduzzaman Md, Wan Hasiah A, Islam MA (2012) Depositional environment and hydrocarbon source potential of the Permian Gondwana coals from the Barapukuria Basin, Northwest Bangladesh. Int J Coal Geol 90–91:162–179

    Article  Google Scholar 

  • Fitzpatrick RW, Merry RH, Williams J, White I, Bowman G, Taylor G (1998) Acid sulfate soil assessment: coastal, inland and minesite conditions. In: National land and water resources audit methods paper

  • Hakimi MH, Wan Hasiah A, Shalaby MR (2010) Source rock characterization and oil generating potential of the Jurassic Madbi Formation, onshore East Shabowah oil fields, Republic of Yemen. Org Geochem 41:513–521

    Article  Google Scholar 

  • Huat BBK (2004) Organic and peat soils engineering. Universiti Putra Malaysia Press, Serdang

    Google Scholar 

  • Jaafar MZ (1998) Kajian petrografi dan geokimia gambut di kawasan Tanjung Duabelas, Kuala Langat, Selangor. B.Sc. Thesis, University of Malaya, Kuala Lumpur

  • Jarrett PM (1995) Geoguide 6. Site investigations for organic soils and peat. In: JKR Document 20709-0341-95. Institut Kerja Raya, Malaysia

  • Khorasani GK (1987) Oil-prone coals of the Waloon Coal Measures, Surat Basin, Australia. In: Scott AC (ed) Coal and coal-bearing strata: recent advances. Published for the Geological Society by Blackwell Scientific Publications, Oxford, pp 303–310

    Google Scholar 

  • Lam SK (1989) Quaternary geology of the Kota Samarahan Area, Sarawak. In: Geological Survey Department of Malaysia

  • Mohamad Tarmizi MZ, Ng TF, Wan Hasiah A, Kuna Raj J, Paramananthan S, Hashim R, Ashraf MA (2013) Distribution, classification, petrological and related geochemical (SRA) characteristics of a tropical lowland peat dome in the Kota samarahan-Asajaya area, West Sarawak, Malaysia. Cent Eur J Geosci 5:285–314

    Article  Google Scholar 

  • Murtedza M, Padmanabhan E, Mei BLH, Siong WB (2002) The peat soils of Sarawak. In: Individual partner report in: STRAPEAT (strategies for implementing sustainable management of peatlands in Borneo) status report. University Malaysia Sarawak, Sarawak, Malaysia

  • Ourisson G, Rohmer M, Poralla K (1987) Prokaryotic hopanoids and other polyterpenoid sterol surrogates. Annu Rev Microbiol 41:301–333

    Article  Google Scholar 

  • Paramananthan S (2011) Keys to the identification of Malaysian soils according to parent materials (Mimeo). In: Param agricultural soil surveys (M) Sdn. Bhd., Petaling Jaya, Selangor, Malaysia

  • Peters KE, Moldowan JM (1991) Effects of source, thermal maturity, and biodegradation on the distribution and isomerization of homohopanes in petroleum. Organ Geochem 17:47–61

    Article  Google Scholar 

  • Peters KE, Walters CC, Moldowan JM (2005) The biomarker guide, 2nd edn. Cambridge University Press, Cambridge

    Google Scholar 

  • Philp RP (1985) Fossil fuel biomarkers: applications and spectra. Elsevier Science Pub. Co, Amsterdam

    Google Scholar 

  • Powell T, McKirdy DM (1973) Relationship between ratio of pristane to phytane, crude oil composition and geological environments in Australia. Nature 243:37–39

    Google Scholar 

  • Quirk MM, Wardroper AMK, Wheatley RE, Maxwell JR (1984) Extended hopanoids in peat environments. Chem Geol 42:25–43

    Article  Google Scholar 

  • Stach E, Mackowsky MTh, Teichmuller M, Taylor GH, Chandra D, Teichmuller R (1982) Stach’s textbook of coal petrology, 3rd edn. Gebruder Borntraeger, Berlin

    Google Scholar 

  • Stout SA, Spackman W (1987) A microscopic investigation of woody tissues in peats: some processes active in the peatification of Ligno-cellulosic cell walls. Int J Coal Geol 8:55–68

    Article  Google Scholar 

  • Talbot HM, Coolen MJL, Damste JSS (2008) An unusual 17a, 21b(H)-bacteriohopanetetrol in holocene sediments from Ace Lake (Antarctica). Org Geochem 39:1029–1032

    Article  Google Scholar 

  • Teichmuller M (1989) The genesis of coal from the viewpoint of coal petrology. Int J Coal Geol 12:1–87

    Article  Google Scholar 

  • Thiel V, Blumenberg M, Pape T, Seifert R, Michaelis W (2003) Unexpected occurrence of hopanoids at gas seeps in the Black Sea. Org Geochem 34:81–87

    Article  Google Scholar 

  • Thompson S, Cooper B, Morely RJ, Barnard PC (1985) Oil generating coals. In: Thomas BM et al (eds) Petroleum geochemistry in exploration of the Norwegian Shelf. Graham & Trotman, London, pp 59–73

    Chapter  Google Scholar 

  • Tie YL (1990) Studies of peat swamps in Sarawak with particular reference to soil-forest relationships and development of domed shaped structures. Dissertation, Univ. of Reading, England

  • van Dorsselaer A, Albrecht P, Ourisson G (1977) Identification of novel (17αH)-hopanes in shales, coals, lignites, sediments and petroleum. Bull Soc Chim Fr 1–2:165–170

    Google Scholar 

  • Wan Hasiah A (1999) Oil-generating potential of tertiary coals and other organic-rich sediments of the Nyalau Formation, onshore Sarawak. J Asian Earth Sci 17:255–267

    Article  Google Scholar 

  • Wan Hasiah A, Abolins P (1998) Organic petrological and organic geochemical characterization of the tertiary coal-bearing sequence of Batu Arang, Selangor, Malaysia. J Asian Earth Sci 16:351–367

    Article  Google Scholar 

  • Waples DW, Machihara T (1991) Biomarkers for geologists: a practical guide to the application of steranes and triterpanes in petroleum geology. In: AAPG methods in exploration series, no. 9. the American Association of Petroleum Geologists, Tulsa, OK

  • Wilford GE (1959) Radiocarbon age determinations of quaternary sediments in Brunei and northeast Sarawak. In: British borneo geological Survey Annual Report

  • Yogeswaran M (1995) Geological considerations in the development of Kuching area dialogue session. In: Geological and geotechnical considerations in civil works. Geological Survey of Malaysia, Kuala Lumpur

Download references

Acknowledgments

The authors are grateful to Dr. Michael Pearson and the anonymous reviewers, who have contributed constructive comments to improve this manuscript considerably. The authors also acknowledge the Institute of Research Management and Consultancy (IPPP) grant PV018-2011A for financial support from the University of Malaya.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Muhammad Aqeel Ashraf.

Electronic supplementary material

Below is the link to the electronic supplementary material.

Supplementary material 1 (PDF 1947 kb)

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Zulkifley, M.T.M., Ng, T.F., Abdullah, W.H. et al. Geochemical characteristics of a tropical lowland peat dome in the Kota Samarahan-Asajaya area, West Sarawak, Malaysia. Environ Earth Sci 73, 1443–1458 (2015). https://doi.org/10.1007/s12665-014-3504-2

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s12665-014-3504-2

Keywords

Navigation