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25th International Meeting on Organic Geochemistry IMOG 2011

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P-474<br />

Paleosalinity significance of the occurrence and distributi<strong>on</strong> of<br />

MTTCs in the Nenjiang Formati<strong>on</strong> of Upper Cretaceous in<br />

S<strong>on</strong>gliao Basin, China<br />

Li Wang 1,2 , Zhiguang S<strong>on</strong>g 1 , Qin Yin 1,2 , Jiangtao Guo 1,2<br />

1 Guangzhou Institute of <strong>Geochemistry</strong>, Chinese Academy of Sciences,, Guangzhou, China, 2 Graduate<br />

School of Chinese Academy of Sciences, Beijing, China (corresp<strong>on</strong>ding author:zs<strong>on</strong>g@gig.ac.cn)<br />

A group of methylated-2methyltrimethyltridecylchromans<br />

(MTTCs) is identified<br />

in the core samples of Member 1 (K2n 1 ) and Member<br />

2 (K2n 2 ) of Nenjiang Formati<strong>on</strong> of Upper Cretaceous<br />

from SK-l drilling borehole of S<strong>on</strong>gliao Basin. This is<br />

the first time that these compounds are reported from<br />

the sediments older than Tertiary in China. Their<br />

compositi<strong>on</strong> and distributi<strong>on</strong> are mainly indicative of<br />

the redox and salinity c<strong>on</strong>diti<strong>on</strong>s of depositi<strong>on</strong>al<br />

envir<strong>on</strong>ments. Am<strong>on</strong>g these MTTCs, δ-MTTC is found<br />

in relative abundant in enhanced salinity and reduced<br />

envir<strong>on</strong>ment, but absent in oxic and much less salinity<br />

envir<strong>on</strong>ment, while α-MTTC appears to be a n<strong>on</strong>salinity<br />

dependent compound and presents in all<br />

envir<strong>on</strong>ments. It is also found that α-MTTC/γ-MTTC<br />

(α/γ) ratio has similar salinity indicati<strong>on</strong> as that of α/δ<br />

ratio but is more widely applicable. The combinati<strong>on</strong><br />

of all related index and biomarkers suggest that the<br />

massive lacustrine petroleum-pr<strong>on</strong>e source rocks<br />

within K2n 1 member were likely developed under a<br />

stratified water column envir<strong>on</strong>ment with the reduced<br />

and enhanced salinity of bottom water layer, which<br />

was associated with a much less salinity top layer of<br />

water(fresh to brackish). Finally, this study suggests<br />

that the MTTC compounds were formed abiotically<br />

from the precursors that originated from various<br />

species of algae under a broad range of redox and<br />

salinity depositi<strong>on</strong>al c<strong>on</strong>diti<strong>on</strong>s.<br />

Key words: MTTCs; depositi<strong>on</strong>al envir<strong>on</strong>ment;<br />

paleosalinity; Nenjiang formati<strong>on</strong>; S<strong>on</strong>gliao Basin<br />

Acknowledge: This research was supported by<br />

NSFC project of 40973033 and State ―973‖ Project<br />

(2006CB701404)<br />

599

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