The Jurassic Period (201-145 Ma) is in the Mesozoic Era, occurring after the Triassic Period, and before the Cretaceous Period. The Jurassic Period is the middle Mesozoic Era.
201.3–145.0 Ma
Late Jurassic: 163.5–145.0 Ma
Tithonian: 152.1±0.9–145.0 Ma
Kimmeridgian: 157.3±1.0–152.1±0.9 Ma
Oxfordian: 163.5±1.0–157.3±1.0 Ma
Middle Jurassic: 174.1–163.5 Ma
Callovian: 166.1±1.2–163.5±1.0 Ma
Bathonian: 168.3±1.3–166.1±1.2 Ma
Bajocian: 170.3±1.3–168.3±1.3 Ma
Aalenian: 174.1±1.0–170.3±1.4 Ma
Early Jurassic: 201.3–174.1 Ma
Toarcian: 182.7±0.7–174.1±1.0 Ma
Pliensbachian: 190.8±1.0–182.7±0.7 Ma
Sinemurian: 199.3±0.3–190.8±1.0 Ma
Hettangian: 201.3±0.2–199.3±0.3 Ma
Flora
Coralline red algae appear
Ferns
Cyatheaceae tree ferns become abundant in the tropical region
Osmundaceous, Matoniaceous, and Dipteridaceous ferns are dominant undergrowth in Jurassic forests
Marsileaceae is first recorded in the Middle to Late Jurassic, and diversify in the Aptian–Albian of the Early Cretaceous (De Benedetti et al., 2021)
Diversification of ginkgophytes
Common in mid-latitude to high, northern latitudes
Domination of conifers
Araucariaceae, Cephalotaxaceae, Pinaceae, Podocarpaceae, Taxaceae, and Cupressaceae
Cheirolepidaceae dominate in low-latitude areas
Cycads are common throughout the landscape
Increase in the Bennettitales, which dominate in low-latitude areas
Caytoniales are small-sized trees, possibly related to angiosperms
Czekanowskiales were present, but not common
Angiosperms may have originated during this time
Fauna
Domination of dinosaurs (saurischian)
Earliest known squids and birds
Earliest known frogs and salamanders
Warm tropical greenhouse conditions worldwide
Carbon dioxide level begin ~1,350 ppm, and increase to ~1,600 ppm before dropping to 1,330 ppm
Oxygen levels hover around 20-21%
The break-up of Pangaea; super-continent begins to rotate,
North America was drifting westward, opening the Gulf of Mexico, forming the central Atlantic.
Mountain-building events are triggered that created the Rocky Mountains and the Sierra Nevada
Sea level rose and flooded large portions of the continents; shallow continental seas spilled out of the Tethys and Proto-Atlantic and spread across Europe,
Warm shallow seas were home to a rich diversity of life.
Much of central North America was flooded by wide sea way that at its height extended into central Utah called the Sundance Sea
Plant thermogenesis has played key role in attracting pollinating insects for at least 200 million years, study suggests (Phys.org 6Sep2024)
└Peris et al., (2024) The impact of thermogenesis on the origin of insect pollination
Jurassic Ecosystems Were Similar to Modern: Animals Flourish Among Lush Plants
Conifers evolve larger female cones due to dinosaur herbivory (Leslie, 2011)