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Science2 publishers3 min readPublished

A feather in a dinosaur dropping puts modern plumage architecture in a lineage that died out

The best Mesozoic feather yet described came out of a coprolite from Montana's Hell Creek, and it belonged to a flightless diver the asteroid killed, which makes modern feather architecture older than the survivors.

The Scientist · Science desk

Photograph accompanying A feather in a dinosaur dropping puts modern plumage architecture in a lineage that died out
Photo: newscientist.com

What happened

  • David DeMar, Jr of the University of Washington was collecting fish fossils in Montana's Hell Creek Formation in 2016 when he found a broken fossil dropping with a feather visible along the fracture.
  • DeMar brought in Jingmai O'Connor and colleagues, who read the coprolite's contents with micro-CT scans and 3D surface scanning rather than by breaking it apart further.
  • A 9.3-centimetre primary feather and a smaller wing feather both had spongy cores inside a harder outer layer, the light-and-stiff construction that characterises modern feathers.

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Why it matters

  • constraint Explanations for neornithine survival can no longer treat modern feather architecture as a post-extinction innovation, because it is now dated to before the impact in a branch that died.
  • capability Prospecting for feather microstructure gains a target beyond skeletons and amber: predator droppings, which held this plumage intact enough to read its internal core.
  • exposure The insulation argument rests on one individual and on morphology alone, so a plumage-based account of extinction selectivity is exposed to the first contemporaneous neornithine body feather anyone finds.
  • decision Anyone building on O'Connor's middle-ground reading has to decide whether branch arrangement is an adequate proxy for thermal performance, since nothing here measures warmth.

The dating claim is the one that travels furthest. A vane with a water-repellent structure comparable to a modern pelican's [9], and shafts with lightweight spongy cores inside a harder outer layer, the combination that makes modern feathers both light and stiff [10], is now on record at 66 million years [1]. That is ten million years earlier than the previous evidence for feathers like those on living birds [2], which places the older benchmark at roughly 56 million years ago, after the impact rather than before it [18]. And the bird wearing it, on the team's reading, was a hesperornithiform: related to Neornithes, but not one of them, and therefore not among the survivors [8][4][21].

The identification runs through two leg-bone fragments, 18 and 12 millimetres long, that resemble material previously collected at Hell Creek and attributed to the group [7]. That is a resemblance argument on fragments, which is what a partially digested carcass leaves you.

Two fluffy body feathers in the same dropping had loosely arranged branches, echoing primitive feathers described from 100-million-year-old Myanmar amber in a lineage that also died out [11]. Taken with the wing feathers, Jingmai O'Connor of the Field Museum reads this bird as occupying a middle ground: flight and tail feathers good enough for diving, body feathers that would have insulated poorly, leaving the animal exposed to the post-impact winter [12]. Her framing is explicitly conditional, that plumage good enough for a Mesozoic greenhouse was not good enough for the catastrophe [13], and she calls plumage differences a contributing factor rather than the cause [14].

Insulation here is inferred from branch arrangement, not measured, and it is not clear whether that insulation deficit was thermally consequential; the comparison that would test it, body feathers from a neornithine of the same age and place, is not in this specimen. The amber material is what anchors the word "primitive" at all, since this plumage passed through a predator's gut before it was buried [1], and morphology read off digested feathers needs an external reference point.

One more inference sits inside the same object. The dropping probably came from a Nanotyrannus or a young Tyrannosaurus rex [15], and it also held two diamond-shaped scales, 3 to 4 millimetres long, assigned to a gar and judged too small to have been the big predator's meal, so the bird likely ate the fish [16]. Frank Muzio of the University of Connecticut notes that a single coprolite is teaching palaeontologists about at least three species [17]. The trophic chain is a side note; the load-bearing result is chronological. Modern feather architecture existed before the asteroid, in a branch the asteroid removed, and any account of why only neornithes came through has to start from there.

What to watch

  • Body feathers from a neornithine of the same age and formation would supply the comparison the plumage hypothesis currently lacks.
  • Any measured or modelled thermal performance for the two feather types, rather than insulation inferred from branch arrangement.
  • Whether other Hell Creek coprolites yield feathers, which would show whether this preservation is repeatable or a single lucky fracture.
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