Charnia fossils were originally found in the Charnwood Forest in England, hence named Charnia. These fossils are from marine organisms that lived on the bottom of the ocean floor. The fossils have a fractal body plan and were frond shaped, meaning they resembled broad-leafed plants such as ferns. However they could not have been plants since they resided in the dark depths of the ocean floor. In Charnwood Forest, Charnia was found as an isolated species, however there were many more fossils found on the East Coast of Canada in Mistaken Point in Newfoundland. Charnia was attached to the bottom of the ocean floor, and was strongly current aligned. This is seen because there are disk-like shapes at the bottom of the Charnia fossil, which show where Charnia was tethered, and all the nearby fossils are facing the same direction. These fossils at Mistaken Point were preserved well under volcanic ash and layers of soft mud. It has been determined via radiometric dating of the fossils that Charnia must have lived around 565 million years ago.