Scientists at The University of Manchester and the University of Bristol have used powerful X-rays to peer inside the skeletons of some of our oldest vertebrate relatives, solving a 160-year-old mystery about the origin of our skeletons.
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| A fossil heterostracan, Errivaspis waynensis, from the early Devonian (approximately 419 million years ago) of Herefordshire, UK [Credit: Keating et al. 2018] |
Evidence for the early evolution of our skeletons can be found in a group of fossil fishes called heterostracans, which lived over 400 million years ago. These fishes include some of the oldest vertebrates with a mineralised skeleton that have ever been discovered. Exactly what tissue heterostracan skeletons were made from has long puzzled scientists.
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| Reconstruction of Anglaspis heintzi [Credit: Keating et al. 2018] |
Lead researcher Dr. Joseph Keating, from Manchester's School of Earth of Environmental Scientists, explained: "Heterostracan skeletons are made of a really strange tissue called 'aspidin'. It is crisscrossed by tiny tubes and does not closely resemble any of the tissues found in vertebrates today. For a 160 years, scientists have wondered if aspidin is a transitional stage in the evolution of mineralised tissues."
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| Detailed models of the skeletal tissue (left) and image of mysterious tissue 'aspidin' (right) [Credit: Keating et al. 2018] |
These findings enabled Dr. Keating to rule out all but one hypothesis for the tissue's identity: aspidin is the earliest evidence of bone in the fossil record.
Co-author, Professor Phil Donoghue from the University of Bristol concludes: "These findings change our view on the evolution of the skeleton. Aspidin was once thought to be the precursor of vertebrate mineralised tissues. We show that it is, in fact, a type of bone, and that all these tissues must have evolved millions of years earlier."
Source: University of Manchester [July 31, 2018]









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