Nicolas Steno and the Principles of Modern Geology

Niels Stensen

Niels Stensen (16381686)

In January, 1638, Danish Catholic bishop and scientist Nicolas Steno was born. He was both a pioneer in both anatomy and geology, and seriously questioned accepted knowledge of the natural world. Importantly he questioned explanations for tear production, the idea that fossils grew in the ground and explanations of rock formation. By some he is considered the founder of modern stratigraphy and modern geology.

“Beautiful is what we see, More Beautiful is what we know, most Beautiful by far is what we don’t.”
— Nicholas Steno

Early Years

Nicolas Steno was born as Niels Stensen, but is better known by the Latinized form Nicholas Steno. The son of a goldsmith was baptized Lutheran in the St. Nikolai Church in Copenhagen, Denmark, and attended the Latin School near the Liebfrauenkirche in his hometown from 1648 to 1656, the most prestigious school in the country at the time. He left Denmark around 1660 intending to study medicine at the University of Leiden. His studies of anatomy, which he continued in Rostock, Amsterdam, Leyden, Paris, Pisa, and Montpellier. There he came into contact with the leading physicians of his time. Through his own research, he discovered the parotid gland duct in the section of a sheep’s head in 1660. His lectures and anatomical demonstrations made him famous throughout Europe. In 1661 he wrote and defended his dissertation on the parotid gland duct duct which he discovered. After learning of the death of his stepfather in 1663, he returned to Copenhagen, where he published the book “Observations on Muscles and Glands“, in which he proved that the heart is a muscle.

Shark Teeth on the Rocks

In 1666 Steno travelled via Pisa and Rome to Florence. There he attracted the attention of the Grand Duke of Tuscany, Ferdinand II, who appointed Steno to a hospital post that left him time for his research. [1,2] At first, Nicolas Steno’s studies were focused on the muscular system as well as the nature of muscle contraction. When around 1666, fishermen caught a shark near LivornoDuke Ferdinand ordered his head to be sent to Steno, who dissected it and published the findings one year later. He noticed the resemblance of the shark’s teeth to certain stony objects found in rocks. As most contemporary scientists argued differently, Steno believed that these ‘stony objects’ looked so much like shark teeth because they actually were shark teeth.

Steno used this picture from an unpublished Vatican catalogue of 1667 in his treatise Canis carchariae dissectum caput to show that the "tongue stones" are fossil shark teeth

Steno used this picture from an unpublished Vatican catalogue of 1667 in his treatise Canis carchariae dissectum caput to show that the “tongue stones” are fossil shark teeth

Well, Steno was not the first who linked these so called ‘tongue stones’ with shark teeth. For instance, already Robert Hooke and John Ray argued that fossils were the remains of living organisms.[4,5] Important is however, that Nicolas Steno came to realize that it was not clear yet how how any solid object could come to be found inside another solid object like a rock.

The Principles of Stratigraphy

Nicolas Steno, in his ‘De solido intra solidum naturaliter contento dissertationis prodromus’ of 1669 is credited with four of the defining principles of the science of stratigraphy:

  • the law of superposition: “... at the time when any given stratum was being formed, all the matter resting upon it was fluid, and, therefore, at the time when the lower stratum was being formed, none of the upper strata existed“;
  • the principle of original horizontality: “Strata either perpendicular to the horizon or inclined to the horizon were at one time parallel to the horizon“;
  • the principle of lateral continuity: “Material forming any stratum were continuous over the surface of the Earth unless some other solid bodies stood in the way”; and
  • the principle of cross-cutting relationships: “If a body or discontinuity cuts across a stratum, it must have formed after that stratum.

These principles were applied and extended in 1772 by Jean-Baptiste L. Romé de l’Isle. Steno’s ideas still form the basis of stratigraphy and were key in the development of James Hutton‘s theory of infinitely repeating cycles of seabed deposition, uplifting, erosion, and submersion.

Nicolas Steno’s Law of Superposition

Nicolas Steno stated that a solid object will cause any solids that form around it later to conform to its own shape. Thus, the famous ‘tongue stone’ must have been buried in soft sediments which hardened later while crystals must have formed after the surrounding rock was a solid, because they often showed irregularities of form caused by having to conform to the surrounding solid rock. His further conclusions are referred to as Steno’s law of superposition. It means that layers of rock are arranged in a time sequence, with the oldest on the bottom and the youngest on the top, unless later processes disturb this arrangement. Steno also mentioned that rocks may be uplifted by subterranean forces. Steno also made efforts to distiguish different time periods in the Earth’s history, which would develop more accurately in the work of later scientists. [2,3]

Nicolas Steno was ordained as a priest in 1675 and essentially abandoned science. He became a bishop a few years later and spent the rest of his life ministering to the minority Roman Catholic populations in northern Germany, Denmark, and Norway. [3] On December 5, 1686, Niels Stensen died in Schwerin at the age of 48 after a five-week bilious disease associated with severe colics. His Hamburg friend Kerckring had his body embalmed on behalf of the Tuscan Grand Duke and transferred to Livorno by ship. He was buried in a chapel of the Basilica of San Lorenzo in Florence.

At yovisto academic video search, you may learn more about ‘What can Fossils teach us‘ in a video lecture by Paul Sereno.

References and Further Reading:

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