The occurrence of intact sterols has been restricted to immature Cretaceous (~125 Ma) sediments with one report from the Late Jurassic (~165 Ma). Here we report the oldest occurrence of intact sterols in a Crustacean fossil preserved for ca. 380 Ma within a Devonian concretion. The exceptional preservation of the biomass is attributed to microbially induced carbonate encapsulation, preventing full decomposition and transformation thus extending sterol occurrences in the geosphere by 250 Ma. A suite of diagenetic transformation products of sterols was also identified in the concretion, demonstrating the remarkable coexistence of biomolecules and geomolecules in the same sample. Most importantly the original biolipids were found to be the mos...
In the vast majority of fossils, the organic matter is degraded with only an impression or cast of t...
Sediments from five contrasting stations in the western Mexican margin (Pacific Ocean) were investig...
The earliest fossils of animal-like organisms occur in Ediacaran rocks that are approximately 571 mi...
Natural products preserved in the geological record can function as ‘molecular fossils’, providing i...
Steroids, a class of triterpenoid lipids with high preservation potential, are widely distributed in...
The absence of unambiguous animal body fossils in rocks older than the late Ediacaran has rendered f...
Sterane biomarkers preserved in ancient sedimentary rocks hold promise for tracking the diversificat...
The transition from simple, single cellular eukaryotes to more complex multicellular organisms, incl...
Sedimentary hydrocarbon remnants of eukaryotic C26–C30 sterols can be used to reconstruct early alga...
The Neoproterozoic era (1,000–542 Myr ago) was an era of climatic extremes and biological evolutiona...
Living organisms often leave molecular traces in the fossil record and these can provide a lens to u...
In this investigation, we monitored the stratigraphic occurrence and abundance of the fossil C30 ste...
The biomarker distributions of mid-Neoproterozoic sediments (800–717 million yr, Ma) from various l...
The period 800-717 million years (Ma) ago, in the lead-up to the Sturtian Snowball glaciation, saw a...
In the vast majority of fossils, the organic matter is degraded with only an impression or cast of t...
Sediments from five contrasting stations in the western Mexican margin (Pacific Ocean) were investig...
The earliest fossils of animal-like organisms occur in Ediacaran rocks that are approximately 571 mi...
Natural products preserved in the geological record can function as ‘molecular fossils’, providing i...
Steroids, a class of triterpenoid lipids with high preservation potential, are widely distributed in...
The absence of unambiguous animal body fossils in rocks older than the late Ediacaran has rendered f...
Sterane biomarkers preserved in ancient sedimentary rocks hold promise for tracking the diversificat...
The transition from simple, single cellular eukaryotes to more complex multicellular organisms, incl...
Sedimentary hydrocarbon remnants of eukaryotic C26–C30 sterols can be used to reconstruct early alga...
The Neoproterozoic era (1,000–542 Myr ago) was an era of climatic extremes and biological evolutiona...
Living organisms often leave molecular traces in the fossil record and these can provide a lens to u...
In this investigation, we monitored the stratigraphic occurrence and abundance of the fossil C30 ste...
The biomarker distributions of mid-Neoproterozoic sediments (800–717 million yr, Ma) from various l...
The period 800-717 million years (Ma) ago, in the lead-up to the Sturtian Snowball glaciation, saw a...
In the vast majority of fossils, the organic matter is degraded with only an impression or cast of t...
Sediments from five contrasting stations in the western Mexican margin (Pacific Ocean) were investig...
The earliest fossils of animal-like organisms occur in Ediacaran rocks that are approximately 571 mi...