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25th International Meeting on Organic Geochemistry IMOG 2011

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P-069<br />

The age and palaeoenvir<strong>on</strong>mental c<strong>on</strong>diti<strong>on</strong>s spanning the<br />

Permian/Triassic boundary in the northern <strong>on</strong>shore Perth Basin<br />

by using biomarker distributi<strong>on</strong>s and stable isotopes (C, H)<br />

Mojgan Ladjavardi 1 , Kliti Grice 1 , Chris Boreham 2 , Dianne Edwards 2 , Ian Metcalfe 3 , Roger<br />

Summ<strong>on</strong>s 4<br />

1 WA <strong>Organic</strong> and Isotope geochemistry centre, Department of Chemistry, Curtin University of Technology,<br />

Perth, WA, Australia, 2 Geoscience Australia, GPO BOX 378, Canberra, Australia, 3 Schools of envir<strong>on</strong>mental<br />

and Rural science, University of New England, NSW, Australia, 4 Massachussetts Institue of Technology,<br />

Earth and Planetary Sciences, Cambridge, United States of America<br />

The Perth Basin petroleum system has been<br />

intermittently explored for the last few decades,<br />

resulting in the producti<strong>on</strong> of gas and oil from several<br />

<strong>on</strong>shore fields (e.g. Summ<strong>on</strong>s et al., 1995). The<br />

effective source rock for petroleum in the Perth Basin<br />

is the marine Kockatea Shale, with the hydrogenrichest<br />

interval being the Sapropelic Unit of the Hovea<br />

Member (Thomas et al., 2004). The Perth Basin in<br />

southwest Western Australia (WA) is a deep, north to<br />

south trending basin, extending over 1,000 km from<br />

Geraldt<strong>on</strong> to the north of Perth. The Perth Basin<br />

sediments comprise of rocks of Permian−Early<br />

Cretaceous in age. The current percepti<strong>on</strong> is that the<br />

area is gas pr<strong>on</strong>e and has been challenged with the<br />

recent discovery of the near-shore Cliff Head oil field.<br />

The D<strong>on</strong>gara gas field in the <strong>on</strong>shore Perth Basin<br />

c<strong>on</strong>tains more than half the oil and gas reserves. The<br />

Perth Basin sediments used in this study are from the<br />

Senecio-1 core which is located approximately 15.5<br />

km from the north of D<strong>on</strong>gara. Stable carb<strong>on</strong> and<br />

hydrogen isotopic compositi<strong>on</strong> of biomarkers<br />

measured by compound specific isotopic analysis<br />

(CSIA) has been shown to be an effective tool for<br />

establishing biogeochemical changes across the<br />

Permian/Triassic boundary (e.g. Nabbefeld et al.,<br />

2010). In the present study bulk geochemical,<br />

biomarker and CSIA of biomarkers are used to<br />

restrain the age and palaeoenvir<strong>on</strong>mental c<strong>on</strong>diti<strong>on</strong>s<br />

spanning the Permian/Triassic in the northern<br />

<strong>on</strong>shore Perth Basin and to compare these results<br />

with the Hovea-3 drill core ‗type-secti<strong>on</strong>‘ (Grice et al.,<br />

2005a). For this purpose 31 samples from the<br />

Senecio-1 cored including Permian/Triassic interval at<br />

1 m spacing were selected. The ages of the samples<br />

have been determined by c<strong>on</strong>od<strong>on</strong>t biostratigraphy.<br />

Rock-Eval & TOC analyses have been performed to<br />

identify the type and maturity of organic matter and to<br />

evaluate the petroleum potential of these samples.<br />

The samples were analysed following the<br />

methodology of Grice et al. (2005b). Each sample<br />

was ground to a fine powder and extracted using an<br />

Accelerated solvent extractor. The extracts were<br />

separated into 6 fracti<strong>on</strong>s by liquid chromatography.<br />

Saturate and aromatic hydrocarb<strong>on</strong> fracti<strong>on</strong>s were<br />

characterised by GC-MS. The saturated hydrocarb<strong>on</strong><br />

fracti<strong>on</strong>s were separated from branched and cyclic<br />

hydrocarb<strong>on</strong>s by treating with 5A molecular sieves<br />

and CSIA of biomarkers was performed for these<br />

fracti<strong>on</strong>s. Bulk stable isotopic compositi<strong>on</strong>s were<br />

measured <strong>on</strong> the kerogens isolated from the extracted<br />

powders. The data is c<strong>on</strong>sistent with Hovea-3 for both<br />

Rock-Eval and kerogen type. � 13 C of the bulk organic<br />

matter is c<strong>on</strong>sistent with the Permian interval of the<br />

core being mainly land plant derived, whereas the<br />

Triassic interval is mainly phytoplankt<strong>on</strong>ic, the change<br />

in stable isotopes is not as abrupt as shown in Hovea-<br />

3.<br />

References<br />

Grice, K., Cao C., Love G.D., Bottcher M.E., Twitchett R.,<br />

Grosiean E., Summ<strong>on</strong>s R., Turge<strong>on</strong> S., Dunning W. J., Jin<br />

Y., 2005a. Photoc Z<strong>on</strong>e Euxinia during the Permian-Triassic<br />

Superanoxic Event. Science 307,706-709.<br />

Grice, K., Summ<strong>on</strong>s, R.E., Grosjean, E., Twitchett, R.J.,<br />

Dunning, W., E., Wang, S.X., Boettcher, M.E., 2005b.<br />

Depositi<strong>on</strong>al c<strong>on</strong>diti<strong>on</strong>s of the northern <strong>on</strong>shore Perth Basin<br />

(Basal Triassic). Australian Petroleum Producti<strong>on</strong> and<br />

Explorati<strong>on</strong> Associati<strong>on</strong> Journal 45, 263-273.<br />

Nabbefeld, B., Grice, K., Twitchett, R.J., Summ<strong>on</strong>s, R.E.,<br />

Hays, L., Boettcher, M.E., Asif, M., 2010. An integrated<br />

biomarker, isotopic and palaeoenvir<strong>on</strong>mental study through<br />

the late Permian event at Lusitaniadalen, Spitsbergen. Earth<br />

and Planetary Science Letters 291, 84-96.<br />

Summ<strong>on</strong>s R.E., Boreham, C.J., Foster, C.B., Murray, A.P.,<br />

Gorter, J.D., 1995. Chemostratigraphy and the compositi<strong>on</strong><br />

of oils in the Perth Basin, Western Australia. Australian<br />

Petroleum Explorati<strong>on</strong> Associati<strong>on</strong> Journal 35, 613-632.<br />

Thomas, B.M., Willink, R.J., Grice, K., Twitchett, R.J.,<br />

Purcell, R.R., Archbold, N.W., George, A.D., Tye, S.,<br />

Alexander, R., Foster, C.B., Barber, C.J., 2004. Unique<br />

marine Permian-Triassic boundary secti<strong>on</strong> from Western<br />

Australia. Australian Journal of Earth Sciences 51(3), 423-<br />

430.<br />

214

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