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Plant fossils

Leaf, frond and stem impressions, mostly in Carboniferous shales.

Mostly Carboniferous, with Jurassic and Cretaceous plant beds elsewhere. · Easy to find

What is it?

Plant fossils are usually preserved as thin carbon films or impressions in fine-grained shale and mudstone. Carboniferous coal-measure rocks produce the classic British material — ferns, horsetails and the bark patterns of giant clubmoss trees.

What does it look like?

Flat black or brown impressions on a split rock face: feathery fronds, ribbed stems, or diamond and oval leaf-scar patterns on bark.

How to identify it

  1. 01Split shale along its natural layers with a chisel; plants appear on the freshly opened face.
  2. 02Impressions dry out and fade — photograph finds promptly.
  3. 03Repeating geometric patterns on bark are fossil leaf scars, not mineral markings.

Where to find plant fossils in the UK

Regions

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