Scientific Frontline: "At a Glance" Summary: 3D Preservation of Marine Reptile Fossils
- Main Discovery: Anaerobic sulfur-cycling microbes are responsible for the exceptional three-dimensional preservation of marine fossils in oxygen-depleted environments by triggering chemical reactions that form structural minerals inside and around the bones prior to skeletal collapse.
- Methodology: Researchers analyzed the anomalous mineral composition and geochemical signals of an ichthyosaur fossil encased in a carbonate concretion from Germany's Posidonia Shale, specifically isolating evidence of localized chemical oxidation within an anoxic seabed environment.
- Key Data: The evaluated fossil is a 183-million-year-old ichthyosaur specimen. Analysis revealed the internal formation of barite, a mineral requiring oxidizing conditions, alongside external calcium carbonate crystallization, which functioned as a protective rock shell against sediment loading.
- Significance: The research refutes the longstanding scientific assumption that the absence of oxygen is the sole driver of fossil preservation in anoxic marine environments, establishing that internal microbiomes and localized chemical changes dictate the fossilization continuum.
- Future Application: The identified microbial preservation mechanisms establish a framework for detecting biosignatures within ancient geological formations on Earth and for guiding astrobiological surveys exploring signs of life in extreme planetary environments.
- Branch of Science: Earth Science, Paleontology, Geochemistry, and Microbiology.
Scientists at Curtin University have solved a long-standing mystery about how some of the world’s best-preserved fossils formed in ancient oxygen-free ocean floor settings.
The research, published in Communications Earth & Environment, focuses on a 183-million-year-old ichthyosaur – a dolphin-like marine reptile, preserved three dimensionally inside a carbonate concretion from Germany’s Posidonia Shale.
For years, scientists believed these fossils were preserved simply because the seafloor had no oxygen, which slowed decay. However, recent discoveries from around the world show signs of oxidation – a process that typically requires oxygen.
Lead author Andrew Jian, a PhD researcher at Curtin, said the team at the Western Australian Organic & Isotope Geochemistry Centre, and in close collaboration with Kiel University, set out to understand how this was possible.
“We wanted to know why fossils from oxygen-free seas still showed signs of chemical oxidation and how that helped preserve them so well,” Mr. Jian said.
“Marine paleontological sites around the world, like the Posidonia Shale, have produced fossils with an unexpected mineral makeup and geochemical signal that is very different to their surrounding sediment.”
The researchers found that after the ichthyosaur died, it sank to the anoxic seafloor, where an assemblage of anaerobic sulfur-cycling microbes colonized the decaying remains.
As they broke down fatty tissues, the microbes triggered chemical reactions that caused different minerals to form inside the bones.
One mineral, barite, formed deep within the bones and could only develop under oxidizing conditions. Meanwhile, calcium carbonate formed around the bones, creating a hard rock shell.
This process strengthened the skeleton before it would be crushed under sediment loading.
Mr Jian said the bones held the answer all along.
“Ironically, these microbes acted like tiny builders even as they consumed the ichthyosaur’s fats and tissues. They filled the bones with minerals before the skeleton could collapse,”
“Barite within Posidonia Shale fossils has been noted for a long time, but few researchers have tried to explain its presence. For decades, scientists assumed no oxygen meant no oxidation. What we found shows the fossilization story is far more complex.”
Senior author and John Curtin Distinguished Professor Kliti Grice, founding director of the Western Australian Organic and Isotope Geochemistry Centre in Curtin’s School of Earth and Planetary Sciences, said the findings alter how scientists understand fossil preservation.
“This shows that even in oxygen-free seas, tiny chemical changes driven by a sulfur cycling microbiome can determine where a fossil falls along a preservation continuum – from being completely replaced by minerals to being exceptionally well-preserved,” Professor Grice said.
“It’s not just the regional environment around the organism that matters, but what happens at the level of microbes and chemistry and microbiome inside the decaying material that can determine how a fossil forms.”
The research also helps scientists better understand how life functioned in extreme environments in the Earth’s past.
“These same processes may help guide how we look for signs of life in ancient rocks and even on other planets,” Professor Grice said.
Funding: The study was conducted with international collaborators and supported by the Australian Research Council through Professor Grice’s Laureate Fellowship and an Australian Government Research Training Program Scholarship.
Published in journal: Communications Earth & Environment
Authors: Andrew Ji Yao Jian, Lorenz Schwark, Stephen Francis Poropat, Alex Ian Holman, Luke Marshall Brosnan, Maria Diaz Mateus, Michael Ernst Böttcher, and Kliti Grice
Source/Credit: Curtin University | Laura Thomas
Reference Number: es032626_01