by Jane Thaler
What’s in a Name?
Derived from the words for “middle life” in Greek, the Mesozoic Era consisted of three geological periods: the Triassic, Jurassic, and Cretaceous. While many of us might be aware of all three, the term “Jurassic” has seeped into our everyday lives in a way that the Triassic and Cretaceous have not. We can attribute much of this ubiquity to the wildly popular Jurassic Park books by Michael Crichton and their subsequent film adaptations, but have you ever wondered what “Jurassic” actually means and how scientists define the period’s geological boundaries?
Coining “Jurassic”
The “Jura” in Jurassic refers to the Jura Mountains that run along a large portion of the Swiss and French border. Named for the ancient Celtic word for forest, the Jura Mountains are known for their tree-covered peaks and the folded rocks that comprise them (Jones, 2020, p. 94).
It was here in 1795 that Alexander von Humboldt, a Prussian explorer and naturalist, documented a series of carbonate shelf deposits from the period now known as the Jurassic and dubbed them the “Jura Kalstein.” Alexander Brongniart, a French scientist known for arranging and describing the geologic formations of the Tertiary Period (66.0 to 2.6 million years ago), coined the term “Terrains Jurassiques” to refer to all Jurassic strata in 1829. In 1832, German geologist Leopold von Buch established the three-fold subdivision of epochs based on the folds of limestone in the Jura: the Lias (Early Jurassic), the Dogger (Middle Jurassic), and the Malm (Late Jurassic). This arrangement remains the basic framework for our geological understanding of the Jurassic to this day (Ogg et al., 2012b, p. 732; Encyclopedia Britannica, 2021a).
Beginning of the Jurassic
Nestled between the Triassic and Cretaceous periods, the Jurassic spanned from 201.3 million years ago to 145 million years ago (National Park Service, 2020). The end of the Triassic (so named because it is a group of three strata) and the beginning of the Jurassic is marked by the Triassic–Jurassic (Tr–J) extinction event, sometimes called the end-Triassic extinction. The fourth of five major extinction episodes on Earth (or sixth if you count the current, anthropogenic extinction), the Tr–J extinction wiped out around 75 percent of all marine and terrestrial life (Encyclopedia Britannica, 2021b).
Current evidence suggests that the Tr–J extinction was initially set into motion by movements of the Earth’s crust. As the all-encompassing mega-continent Pangea began to break apart, the associated tectonic shifts caused significant volcanic activity that spewed carbon dioxide into the atmosphere. The resulting global warming disrupted the Earth’s carbon cycle and contributed to ocean acidification (Fuge, 2020).
The ecological niches left open by the Tr–J extinction were quickly filled by remaining species of pterosaurs, crocodilians, turtles, mammals, many species of plants and invertebrates, marine life, and dinosaurs. Though many species died out during the extinction event, the wet and warm climate of the Jurassic in many places encouraged the growth of lush vegetation along with the proliferation and diversification of fauna. Oceans teemed with life, forests flourished, and dinosaurs became the dominant forms of backboned animal life on land during this time (Encyclopedia Britannica, 2021b).
End of the Jurassic Period
The end of the Jurassic is a bit of a mystery as the geological boundary between it and the Cretaceous Period (the latter name derived from the Latin for “chalk”) remains formally undefined. In fact, the Cretaceous is the only period in the Phanerozoic Eon (541 million years ago to present day) that “does not yet have an accepted global boundary definition” (Ogg et al., 2012a, p. 795). This definitional challenge is due to a number of factors but is mostly attributed to the concept of provincialism or provinciality, which means that plant or animal populations were restricted to a particular area or group of areas (Gale et al., 2020). This resulted in endemic populations, particularly of ammonites, which left uneven or unclear fossil markers in the stratigraphic record (Wimbledon, 2017; see Énay, 2019 for more detail on the J/K boundary debates).
We do know that the end of the Jurassic was marked by the Tithonian–early Barremian cool interval, which began 150 million years ago and continued well into the Early Cretaceous (Ogg et al., 2012a). During this time, some groups of animals did go extinct or become less diverse, like the dinosaurian subgroup Stegosauria that included Stegosaurus, while others increased in abundance, like some ammonite subgroups who survived the Tr–J event. Plants were also developing in important ways during this time. Around 130 million years ago, angiosperms (flowering plants) began to diversify, and they became increasingly dominant throughout the Cretaceous (Friis et al., 2010). Taking the unknowns and variables into account, the end of the Jurassic is currently placed at 145 million years ago.
Naming Geological Periods
Many of the names we still use for geological periods went through a similar process to that of the Jurassic: a scientist named a phenomenon based on the strata they were studying and the nomenclature (the system of names) developed from there. Nowadays, defining and naming geological units is left to the International Commission on Stratigraphy of the International Union of Geological Sciences. The process by which this happens feels about as long as the geologic periods themselves, at least to those of us watching from outside the commission. This is, of course, an exaggeration, but it does take years of work and rounds of voting to arrive at an official stratigraphic boundary designation.
Check out https://stratigraphy.org for the latest updates on humanity’s understanding of geologic time.
Jane Thaler is a Gallery Experience Presenter and Floor Captain in CMNH’s LifeLong Learning Department. Museum staff, volunteers, and interns are encouraged to blog about their unique experiences and knowledge gained from working at the museum.
References:
enay, Raymond (2019). The Jurassic/Cretaceous System Boundary is at an impasse: Why not go back to Oppel’s 1865 original and historic definition of the Tithonian? Cretaceous Research. https://doi.org/10.1016/j.cretres.2019.104241.
Encyclopedia Britannica (2021a). Alexandre Brongniart. https://www.britannica.com/biography/Alexandre-Brongniart
Encyclopedia Britannica (2021b). End-Triassic extinction. https://academic-eb-com.pitt.idm.oclc.org/levels/collegiate/article/end-Triassic-extinction/474417
Fuge, L. (2020). Volcano link to end of Triassic extinction. Cosmos. https://cosmosmagazine.com/history/palaeontology/volcano-link-to-end-of-triassic-extinction/
Friis E. M., Pedersen K. R., Crane P. R. (2010). Diversity in obscurity: fossil flowers and the early history of angiosperms. Philosophical Transactions of the Royal Society B, 365. https://doi.org/10.1098/rstb.2009.0227
Gale, A. S., Mutterlose, J., Batenburg, S., Gradstein, F. M., Agterberg, F. P., Ogg, J. G., Petrizzo, M. R. (2020). The Cretaceous Period. In The Geologic Time Scale 2020 (Gradstein, F. M., Ogg, J. G., Schmitz, M. D., & Ogg, G. M., Eds.). Elsevier. https://doi.org/10.1016/B978-0-12-824360-2.00027-9
Gore, R. (n.d.), The rise of mammals. In National Geographic. https://www.nationalgeographic.com/science/article/rise-mammals
Ogg, J. G., Hinnov, L. A., Huang, C. (2012a). Cretaceous. In The Geologic Time Scale 2012 (Gradstein, F. M., Ogg, J. G., Schmitz, M. D., & Ogg, G. M., Eds.). Elsevier.
Ogg, J. G., Hinnov, L. A., Huang, C. (2012b). Jurassic. In The Geologic Time Scale 2012 (Gradstein, F. M., Ogg, J. G., Schmitz, M. D., & Ogg, G. M., Eds.). Elsevier.
Jones, P. (2020). Jura Mountains, France/Switzerland. In Around the World in 80 Words. University of Chicago Press. https://doi.org/10.7208/9780226682822-026
National Park Service (2020). Geologic time scale. https://www.nps.gov/subjects/geology/time-scale.htm
Pfiffner, O. A. (2006). Thick-skinned and thin-skinned styles of continental contraction. Special Paper of the Geological Society of America, 414.
Sauquet, H., von Balthazar, M., Magallón, S. et al. (2017). The ancestral flower of angiosperms and its early diversification. Nature Communications, 8. https://doi.org/10.1038/ncomms16047
Scotese, C. R., Song, H., Mills, B. J. W., van der Meer, D. G. (2021). Phanerozoic paleotemperatures: the Earth’s changing climate during the last 540 million years. Earth-Science Reviews, 215. https://doi.org/10.1016/j.earscirev.2021.103503
Wimbledon, W. A. P. (2017). Developments with fixing a Tithonian/Berriasian (J/K) boundary. Volumina Jurassica, XV. https://doi.org/10.5604/01.3001.0010.7467
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Carnegie Museum of Natural History Blog Citation Information
Blog author: Thaler, JanePublication date: July 29, 2021
