The earliest fossils of animal-like organisms occur in Ediacaran rocks that are approximately 571 million years old. Yet 24-isopropylcholestanes and other C₃₀ fossil sterol molecules have been suggested to reflect an important ecological role of demosponges as the first abundant animals by the end of the Cryogenian period (>635 million years ago). Here, we demonstrate that C₃₀ 24-isopropylcholestane is not diagnostic for sponges and probably formed in Neoproterozoic sediments through the geological methylation of C₂₉ sterols of chlorophyte algae, the dominant eukaryotes at that time. These findings reconcile biomarker evidence with the geological record and revert the oldest evidence for animals back into the latest Ediacaran
The dawn of animals remains one of the most mysterious milestones in the evolution of life. The foss...
The period 800-717 million years (Ma) ago, in the lead-up to the Sturtian Snowball glaciation, saw a...
The biomarker distributions of mid-Neoproterozoic sediments (800–717 million yr, Ma) from various l...
The earliest fossils of animal-like organisms occur in Ediacaran rocks that are approximately 571 mi...
Sterane biomarkers preserved in ancient sedimentary rocks hold promise for tracking the diversificat...
Living organisms often leave molecular traces in the fossil record and these can provide a lens to u...
Molecular fossils (or biomarkers) are key to unraveling the deep history of eukaryotes, especially i...
Molecular fossils (or biomarkers) are key to unraveling the deep history of eukaryotes, especially i...
Molecular fossils (or biomarkers) are key to unraveling the deep history of eukaryotes, especially i...
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...
The transition from simple, single cellular eukaryotes to more complex multicellular organisms, incl...
The dawn of animals remains one of the most mysterious milestones in the evolution of life. The foss...
The dawn of animals remains one of the most mysterious milestones in the evolution of life. The foss...
The Neoproterozoic era (1,000–542 Myr ago) was an era of climatic extremes and biological evolutiona...
The dawn of animals remains one of the most mysterious milestones in the evolution of life. The foss...
The period 800-717 million years (Ma) ago, in the lead-up to the Sturtian Snowball glaciation, saw a...
The biomarker distributions of mid-Neoproterozoic sediments (800–717 million yr, Ma) from various l...
The earliest fossils of animal-like organisms occur in Ediacaran rocks that are approximately 571 mi...
Sterane biomarkers preserved in ancient sedimentary rocks hold promise for tracking the diversificat...
Living organisms often leave molecular traces in the fossil record and these can provide a lens to u...
Molecular fossils (or biomarkers) are key to unraveling the deep history of eukaryotes, especially i...
Molecular fossils (or biomarkers) are key to unraveling the deep history of eukaryotes, especially i...
Molecular fossils (or biomarkers) are key to unraveling the deep history of eukaryotes, especially i...
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...
The transition from simple, single cellular eukaryotes to more complex multicellular organisms, incl...
The dawn of animals remains one of the most mysterious milestones in the evolution of life. The foss...
The dawn of animals remains one of the most mysterious milestones in the evolution of life. The foss...
The Neoproterozoic era (1,000–542 Myr ago) was an era of climatic extremes and biological evolutiona...
The dawn of animals remains one of the most mysterious milestones in the evolution of life. The foss...
The period 800-717 million years (Ma) ago, in the lead-up to the Sturtian Snowball glaciation, saw a...
The biomarker distributions of mid-Neoproterozoic sediments (800–717 million yr, Ma) from various l...