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A short mechanism for iso-octane applied previously to flame propagation was found to be inadequate to describe the hydrocarbon evolution after quenching.
Findings of rapid evolution and positive selection of such genes [ 60, 61] suggest that hydrocarbon evolution may exert strong, direct effects on phenotypic changes that mediate speciation.
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Because of differences in tectonic activities, the extent of hydrocarbon generation evolution varies by basin.
We next wanted to develop insights into the processes that shape hydrocarbon profile evolution among sexual Timema species.
Using the phylogeny of these species, we also evaluated the tempo and mode of hydrocarbon profile evolution to develop insights into the processes underlying divergence between species for this trait.
Inference of the tempo and mode of hydrocarbon profile evolution provides evidence generally consistent with the hypothesis that change in this set of characters does not occur gradually during phyletic evolution, but relatively rapidly, in proportion to the number of speciation events.
Generally speaking, petroleum inclusions formed in the low mature phase of hydrocarbon source rock evolution had a high density, with a high content of heavy hydrocarbon and asphaltene.
The effect of mechanical compaction is one of several factors influencing hydrocarbon formation and evolution, with other factors including erosion effects, tectonic activity, diagenesis, and abnormal pressure.
In this paper, the author presented a novel general model of hydrocarbon generation and evolution with soluble and insoluble organic matter both contributing to hydrocarbon generation.
Evidence for cuticular hydrocarbons mediating the evolution of reproductive isolation has thus far centered mainly on associations between variation in hydrocarbon profiles and variation in propensities to mate [ 47].
The generation of hydrocarbons from thermal evolution of organic matter not only needs heat but also hydrogen.
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