One
of the important paradigms of fundamental petroleum geochemistry
has been (and still is) that native asphaltenes in present day crude
oils originated in the respective source rocks and are representative
of the molecular composition in ancient organic deposits. The survival
of “prehistoric” molecular species is enabled by shielding
them in complex macromolecular structures of asphaltene nanocolloidal
particles. In addition, the maturity of petroleum expelled from the
source may define the structures of asphaltene colloidal aggregates,
as indicated by recent advances in colloid science. On the other hand,
in applied asphaltene research, the above paradigm is most often ignored,
while its revitalization may improve our understanding of asphaltene
behavior in native crude oils and, in particular, may provide a new
criterion for potential instability of some crude oils with respect
to asphaltene precipitation and deposition.