The findings came from X-ray experiments
undertaken by our 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 AtomicSpectrometry (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, said 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.”
The second is a method that Uwe Bergmann, Phil
Manning and Roy Wogelius have developed for rapidly scanning entire fossils and
analysing their chemistry with an X-ray beam at SLAC’s Stanford Synchrotron
Radiation Lightsource (SSRL) in the USA.
Over the past three years, a team led by
Bergmann (SLAC), Manning and Wogelius of the University of Manchester used this
method to discover chemical
traces locked in the dinobird’s bones, feathers and in the surrounding
rock, as well as pigments from the fossilised feathers of two specimens of another
species of early bird. This allowed the team to recreate
the plumage pattern of an extinct bird for the very first time.
In the latest study, the team scanned the
entire fossil of the first Archaeopteryx
feather with the SSRL X-ray beam. They found trace-metals that have been shown
to be associated with pigment and organic sulphur compounds that could only
have come from the animal’s original feathers. ‘The fact that these compounds have been preserved in-place for 150
million years is extraordinary’, Manning said.
‘Together
these chemical traces show that the feather was light in colour, with areas of
darker pigment along one edge and on the tip. Scans of a second fossilised
Archaeopteryx, known as the Berlin counterpart, also show that the trace-metal
inventory supported the same plumage pigmentation pattern’, Manning said.
Co-author Dr. Roy Wogelius, also based in
Manchester’s School of Earth, Atmospheric and Environmental Sciences, said:
“This work refines our understanding of pigment patterning in perhaps the most
important known fossil. Our technique shows that complex patterns were present
even at the very earliest steps in the evolution of birds.”
The team’s results show that the chemical
analysis provided by synchrotron X-ray sources, such as SSRL, is crucial when
studying the fossil remains of such pivotal species. The plumage patterns can
begin to help scientists review their possible role in the courtship,
reproduction and evolution of birds and possibly shed new light on their
health, eating habits and environment. More importantly, said Manning, ‘It is
remarkable that x-rays brighter than a million suns can shed new light on our understanding of the processes that have
locked elements in place for such vast periods of time. Ultimately this research
might help inform scientists on the mechanisms acting during long-term burial, from
animal remains to hazardous waste. The fossil record has potential to provide
the experimental hindsight required in such studies.’
The research team included scientists from
the University of Manchester (UK); SLAC (USA); the Black Hills Institute of
Geological Research in South Dakota (USA); and the Museum für Naturkunde in
Berlin (Germany), which provided the stunning Archaeopteryx fossils for analysis.
The paper is free to download at this LINK.
The paper is free to download at this LINK.
Does this work clarify the patterns sufficiently to confirm that the original feather (which I believe is the type of A. lithographica) comes from the same species as the skeletal specimens with feathers, rather than from some other maniraptoran which was knocking around the area at about the same time?
ReplyDeleteThis is a great question. The single feather is indeed the former holotype, but it lost it's holotype status last year to the London specimen, due to the isolated nature of the feather (i.e. no skeleton). The associated bone that we were able to image just below the surface next to the sigle feather does show similar chemistry to other Archaeopteryx bones we have scanned at SLAC, but we really need to scan many more Solnhofen bones (of as many vertebrate species as possible) to be sure of its identity (hence or guarded approach in the paper). However, when we scanned the Berlin 1880 specimen counterpart, we saw a similar distribution of Cu (a biomarker for eumelanin pigment) in the feathers of this more complete specimen, when compared to the single feather. The concentration and distribution of the chemistry shared between these two fossils (and the feathers) is enough to suggest the two are indeed from the same genus of beastie. I hope this answers your question. Cheers Phil
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