
TY  - JOUR
A1  - Foster, C.B. 
A1  - Logan, G.A. 
A1  - Summons, R.E. 
A1  - Gorter, J.D. 
A1  - Edwards, D.S. 
T1  - CARBON ISOTOPES, KEROGEN TYPES AND THE PERMIAN-TRIASSIC BOUNDARY IN AUSTRALIA: IMPLICATIONS FOR EXPLORATION
JF  - The APPEA Journal
JO  - The APPEA Journal
Y1  - 1997
VL  - 37
IS  - 1
SP  - 472
EP  - 489
KW  - 
UR  - https://doi.org/10.1071/AJ96028 
N2  - A global stratotype section for the boundary between the Permian and Triassic Systems is yet to be agreed internationally. However, in many parts of the world, there is evidence of massive extinction of marine fauna at or near the P-T boundary. In the absence of marine fauna, as is the case in most of Australia, changes in plant microfossils, in carbon isotopic signatures, and radiometric dates using SHRIMP, have been used to mark the boundary. The leading questions which arise from this are whether these events are synchronous and how they affect exploration.In eastern Australia, the top of the coal measures has been used as the top of the Permian, although presently only plant microfossils can be used to determine if the youngest seam is present. This has important economic consequences for determination of volumes of effective source rock and for estimates of coal-bed methane. It has been suggested that changes in the carbon isotopic signatures (&#x3b4;13C) of either organic matter (&#x3b4;13Corg) or carbonates (&#x3b4;13Ccarb) can be used to delimit the P-T boundary. From studies of (&#x3b4;13Ccarb data, Scholle (1995) concluded that &apos;the establishment of a secular variation curve which has enough detail and reliability to be used as a chemostratigraphic tool still lies in the future&apos;. We concur, and demonstrate for organic carbon that, while there is evidence for secular change, the 13C signature is complicated and overprinted by contributions from different parent plant types; wood-dominated organics are typically &#x2212;24 %o, while non-woody matter is significantly lighter (&#x2212;30 %o). There is no simple relationship of &#x3b4;13Corg to geological age. The consistency of our data, from both the east and west of Australia, allows us to construct a model to predict probable depositional and organic facies using either carbon isotopes (from kerogen or oil) or quantitative estimates of organic matter from standard palynlogical slides. This offers a novel and usefl predictive tool for hydrocarbon exploration. 
ER  -

