Determination
of the molecular structures of petroporphyrins has
been crucial to understand the diagenetic pathways and maturation
of petroleum. However, these studies have been hampered by their structural
complexity and the challenges associated with their isolation. In
comparison to the skeletal macrocyclic structures, much less is known
about the substitutions, which are more sensitive to the maturation
and diagenesis pathways. While these isolated vanadyl petroporphyrins
largely consist of etioporphyrin and deoxophylloerythroetioporphyrin
as expected, surprisingly, we find evidence that one or a few β
hydrogens are present in petroporphyrins of low carbon numbers using
a combination of ultraviolet–visible spectroscopy, Fourier
transform ion cyclotron resonance mass spectrometry, and non-contact
atomic force microscopy. Petroporphyrins with β hydrogens were
not anticipated on the basis of their biological precursors. The data
support dealkylation under catagenesis but not transalkylation or
random alkylation of the β and meso positions, despite the fact
that more complex porphyrin structures are formed.