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25th International Meeting on Organic Geochemistry IMOG 2011

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P-079<br />

<strong>Geochemistry</strong> of ―just generated‖ oils from Uz<strong>on</strong> volcano<br />

caldera(Kamchatka) in comparis<strong>on</strong> with oldest pre-Cambrian<br />

oils<br />

Enver Ablya, Irina Slivko<br />

Moscow State University, Moscow, Russian Federati<strong>on</strong> (corresp<strong>on</strong>ding author:eablya@yandex.ru)<br />

Uz<strong>on</strong> volcanic caldera is the largest geothermal<br />

field located in the eastern part of Kamchatka,<br />

Russia. Some hot springs and lakes are notable,<br />

because some are highly acidic and are locati<strong>on</strong><br />

of the occurrence of specific algae and<br />

extremophile. But it is also amazing place of the<br />

generati<strong>on</strong> and occurrence of ―youngest‖ oils. This<br />

oils appear as stains <strong>on</strong> soluti<strong>on</strong>s surface and<br />

quickly evanesce, some oils saturates sediments<br />

around geothermal fields. We studied different oil<br />

samples collected periodically at the same place –<br />

near highly acidic and hot lake. Oils have different<br />

phase from diesel type to very waxy . Oils have<br />

different HC distributi<strong>on</strong> - some as marine type with<br />

prevalence of normal alkanes and Pr/Ph ratio<br />

around 1, and some with prevalence of iso-alkanes<br />

with unusual Pr/Ph ratios less then 0.5-0.3.<br />

Surprisingly that some oils have unusual HC‘s as-<br />

12-and13-methylalkanes. The distributi<strong>on</strong> of<br />

terpanes are characterised by different<br />

c<strong>on</strong>centrati<strong>on</strong>s of tri- and tetracyclic - some oils with<br />

low but some – with sharp high value of the C19/C23<br />

ratios; all oils with predominance of the C30hopane<br />

over the C29-norhopane. In some oils<br />

prevalence of C 32 and C 35 homo-hopanes<br />

Saturate and aromatic fracti<strong>on</strong>s of Uz<strong>on</strong> oils are<br />

characterized by polar �13C values from –27‰ to<br />

–34‰. Based <strong>on</strong> biomarker parameters (steranes,<br />

Ts/Tm, 4-MDBT/1 MDBT, the thermal maturity of<br />

Uz<strong>on</strong> oils is assessed as low or n<strong>on</strong>-mature ( Fig.<br />

1-2, GC-MS -m/z 217). Oils have relatively low<br />

c<strong>on</strong>centrati<strong>on</strong>s of C26 tri and C27 m<strong>on</strong>oaromatic HC<br />

and abundant dibenzotiophen. Distributi<strong>on</strong> of<br />

steranes are also unusual with a significant<br />

predominance of C29 , less C28 and very low C27<br />

steranes (Fig 1-2) . Very interesting that Uz<strong>on</strong> oils<br />

not c<strong>on</strong>tent trace elements excluding a hundred<br />

ppm c<strong>on</strong>tent of As am<strong>on</strong>g studied tens usual oils.<br />

We discovered that some Proterozoic (PR) sourced<br />

oils in East Siberia have geochemical fingerprints<br />

similar to those found in some Uz<strong>on</strong> oils. These PR<br />

oils are characterised by a dominance of C29<br />

steranes ( fig.3), and the occurrence of 12- and 13methylalkanes.<br />

PR oils are characterized by �13C<br />

values around – 33 ‰. . It must be note that some<br />

oldest pre-Cambrian oils from East Siberia and<br />

Paleozoic oils from West Siberia also shows<br />

c<strong>on</strong>siderable c<strong>on</strong>tent of As.<br />

So it believes that this Uz<strong>on</strong> oils ―just‖<br />

generated by high plant fossils, algae with ―help‖ of<br />

bacteria in boiling toxic geothermal soluti<strong>on</strong>s.<br />

Extremophiles are believed to have been some of<br />

the earliest lifeforms <strong>on</strong> earth, since such early<br />

organisms would have to be adapted to harsh<br />

c<strong>on</strong>diti<strong>on</strong>s, for example, Picrophilus torridus, an<br />

extreme archaean acidophile, thrives at pH of<br />

essentially zero, equivalent to a 1.2 molar<br />

c<strong>on</strong>centrati<strong>on</strong> of sulfuric acid. Some of ―oldest‖ oils<br />

generated in same c<strong>on</strong>diti<strong>on</strong>s ?<br />

Fig.1<br />

Fig.2<br />

Fig.3<br />

222

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