Line 125: |
Line 125: |
| | | |
| ==Biodegradation limitations== | | ==Biodegradation limitations== |
| + | |
| + | [[file:oiloil-and-oilsource-rock-correlations_fig8-20.png|thumb|{{figure number|8-16}}From Curiale et al.;<ref name=ch08r12>Curiale, J., A., 1994, Correlation of oils and source rocks—a conceptual and historical perspective, in Magoon, L., B., Dow, W., G., eds., The [[Petroleum system]]—From Source to Trap: AAPG Memoir 60, p. 251–260.</ref> and Curiale<ref name=ch08r9>Curiale, J., A., 1991, The petroleum geochemistry of Canadian Beaufort Tertiary “non-marine” oils: Chemical Geology, vol. 93, p. 21–45., 10., 1016/0009-2541(91)90062-V</ref> reprinted with permission from Elsevier.]] |
| + | |
| Biodegradation can severely alter gas chromatograms. In the earliest stages of biodegradation, ''n''-alkanes are removed selectively, leading to significant loss of information. | | Biodegradation can severely alter gas chromatograms. In the earliest stages of biodegradation, ''n''-alkanes are removed selectively, leading to significant loss of information. |
| | | |
| ===Examples of biodegradation=== | | ===Examples of biodegradation=== |
− | The figure below (left) shows gas chromatograms of three oils from a common source in central Myanmar. A waxy oil (top) is sequentially converted into an extremely biodegraded remnant oil (bottom). The API gravity of the oil decreases and sulfur content increases substantially with increasing biodegradation.
| + | [[:file:oiloil-and-oilsource-rock-correlations_fig8-20.png|Figure 16]] (left) shows gas chromatograms of three oils from a common source in central Myanmar. A waxy oil (top) is sequentially converted into an extremely biodegraded remnant oil (bottom). The API gravity of the oil decreases and sulfur content increases substantially with increasing biodegradation. |
| | | |
| Pristane–phytane ratios may also be affected slightly at low stages of biodegradation. At moderate levels these compounds are removed completely (left figure). The right figure below shows whole-oil gas chromatograms of three oils from the offshore Mackenzie Delta, northwestern Canada, showing a modest decrease in the pristane–phytane ratio, apparently as the result of minor biodegradation. | | Pristane–phytane ratios may also be affected slightly at low stages of biodegradation. At moderate levels these compounds are removed completely (left figure). The right figure below shows whole-oil gas chromatograms of three oils from the offshore Mackenzie Delta, northwestern Canada, showing a modest decrease in the pristane–phytane ratio, apparently as the result of minor biodegradation. |
− |
| |
− | [[file:oiloil-and-oilsource-rock-correlations_fig8-20.png|thumb|{{figure number|8-20}}From Curiale et al.;<ref name=ch08r12>Curiale, J., A., 1994, Correlation of oils and source rocks—a conceptual and historical perspective, in Magoon, L., B., Dow, W., G., eds., The [[Petroleum system]]—From Source to Trap: AAPG Memoir 60, p. 251–260.</ref> and Curiale<ref name=ch08r9>Curiale, J., A., 1991, The petroleum geochemistry of Canadian Beaufort Tertiary “non-marine” oils: Chemical Geology, vol. 93, p. 21–45., 10., 1016/0009-2541(91)90062-V</ref> reprinted with permission from Elsevier.]]
| |
| | | |
| ==See also== | | ==See also== |