The findings came from X-ray experiments by a team from The University of Manchester, working with colleagues at the US Department of Energy’s (DOE) SLAC National Accelerator Laboratory. The scientists were able to find chemical traces of the original ‘dinobird’ and dilute traces of plumage pigments in the 150 million-year-old fossil.
“This is a big leap forward in our understanding of the evolution of plumage and also the preservation of feathers,” said Dr Phil Manning, a palaeontologist at The University of Manchester and lead author of the report in the June 13 issue of the Journal of Analytical Atomic Spectrometry (Royal Society of Chemistry).
Only 11 specimens of Archaeopteryx have been found, the first one consisting of a single feather. Until a few years ago, researchers thought minerals would have replaced all the bones and tissues of the original animal during fossilisation, leaving no chemical traces behind, but two recently developed methods have turned up more information about the dinobird and its plumage.
The first is the discovery of melanosomes – microscopic ‘biological paint pot’ structures in which pigment was once made, but are still visible in some rare fossil feathers. A team led by researchers at Brown University announced last year that an analysis of melanosomes in the single Archaeopteryx feather indicated it was black. They identified the feather as a covert – a type of feather that covers the primary and secondary wing feathers – and said its heavy pigmentation may have strengthened it against the wear and tear of flight, as it does in modern birds.
However, that study examined melanosomes from just a few locations in the fossilised feather, explained SLAC’s Dr Uwe Bergmann: “It’s actually quite a beautiful paper,” he said, “but they took just tiny samples of the feather, not the whole thing.”
Read more at: Phys.org