Abstract
Fossil arachnids—especially those dating from the Carboniferous period, 360–299 million years ago—are often found in mines or quarries within concretions of siderite (FeCO3). Most of the methods to study these fossils are either destructive or damaging to the specimens and are limited in their resolution, thereby limiting the information that can be derived from the fossil. In an elegant study, Russell Garwood, Jason Dunlop, and Mark Sutton have demonstrated that X-ray micro-tomography (XMT) can reveal hitherto unseen details in such fossils without damaging the specimens.
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