January 11, 1638, birthday of Danish physician Niels Steensen or latinized Nicolas Steno.

He popularized the first stratigraphical principles and recognized the true origin of fossils studying “tongue-stones” - petrified shark teeth.

Trained as physician and surgeon and a keen observer of the natural world, while visiting the Italian region of Tuscany, Steno recognized that sedimentary rock formations follow certain rules:

  • Layers of sedimentary rocks are arranged in a time sequence, with the oldest on the bottom and the youngest on the top, unless later processes disturb this arrangement (principle of superposition).

  • Layers of sedimentary rocks are deposited in a horizontal position if not being disturbed later (principle of original horizontality).

  • A stratum is deposited continuously unless some other solid body is in the way (principle of strata continuity).

  • Any geologic feature (like a fault, dike, or erosional surface) that cuts across another feature must be younger than the feature it disrupts (principle of cross-cutting relationships).

In 1666, during the dissection of a shark’s head, he noted the similarities of shark teeth with glossopetrae or tongue-stones found in the ground.

Steno was not the first to speculate about an organic origin of fossils, however, he was the first to propose a “theory” to explain how remains of sea animals could be petrified and become embedded in rocks.

  • The layers of a sedimentary rock were formed by sediment deposition in water. The now hard rock was once a soft mud.

  • An animal living in the sea (like a shark) would, after its death, sink slowly into the soft mud. Mud and water would seep into an animal’s hardest parts (like teeth and bones) and preserve them.

  • Movements of Earth’s crust push the mud with the fossil inside above water. Exposed to air, the mud dries and becomes hard rock.

  • The hardened layer is pushed back below water and new sediment covers it, forming a new layer.

  • In the end, all the layers are uplifted again, this time high enough to form a mountain, where a curious naturalist can find the fossils eroding from the rocks.

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