The team documented a sequence of mineral barriers that acted as a natural "geological vault" . First, fluorapatite (a calcium phosphate) formed rapidly within and around the bone, stabilizing fine structural features. Next, successive layers of calcite gradually filled the bone cavity. Critically, the calcite is depleted in carbon-13, indicating it originated from the decay of the pterosaur's own fatty tissues and lipids
. The multi-layered mineral coat shielded organic compounds—including steroid biomarkers and microscopic structures resembling collagen fibers—from chemical degradation over 113 million years
.
The study documents a complex, multi-staged mineralization process driven by local redox (oxidation-reduction) shifts during early diagenesis . Sulfur-oxidizing bacteria (SOB)—identified by the minerals barite and celestite they left behind—were key players
. These microbes broke down soft tissues and fats, releasing carbon that fed calcite precipitation. At the same time, their activity created the chemical conditions that sealed the bone in protective minerals before delicate structures could be lost
.
Conventional thinking held that oxygen and microbial oxidation are destructive—that decay microbes consume and erase soft tissues and biomolecules, and that exceptional preservation requires anoxic conditions to suppress microbial activity. This study overturns that assumption in two ways :
As Grice stated, "Rather than being destroyed by oxygen, some fossils are preserved because of it, through oxidative processes carried out by ancient microbiomes" . The team proposes this as a new global Lagerstätten mechanism—a common pathway for exceptional fossil preservation that is now being identified at other fossil sites
.
The Curtin-led study is the first to recover steroid biomarkers from a pterosaur, revealing a fish/squid diet. It demonstrates that multi-staged mineralization, driven by sulfur-metabolizing microbes and local redox shifts, was the key to the wing's 3D preservation. And it fundamentally reframes the role of microbial oxidation from a purely destructive force to a necessary, constructive step in certain types of exceptional fossil preservation .
Comments
0 comments