Science, Tech, Math › Animals & Nature Where Dinosaurs Lived Share Flipboard Email Print Travelpix Ltd / Getty Images Animals & Nature Dinosaurs Basics Paleontologists Carnivores Dinosaurs & Birds Herbivores Marine Reptiles Prehistoric Mammals Amphibians Birds Habitat Profiles Mammals Reptiles Wildlife Conservation Insects Marine Life Forestry Evolution View More By Bob Strauss Science Writer B.S., Cornell University Bob Strauss is a science writer and the author of several books, including "The Big Book of What, How and Why" and "A Field Guide to the Dinosaurs of North America." our editorial process Bob Strauss Updated October 29, 2019 Dinosaurs lived over 180 million-year span that ranged from the Triassic Period when all continents were joined as a single landmass known as Pangea beginning 250 million years ago through the Cretaceous Period ending 66 million years ago. The Earth looked a lot different during the Mesozoic Era, from 250 million to 65 million years ago. Although the layout of the oceans and continents may be unfamiliar to modern eyes, not so the habitats in which dinosaurs and other animals lived. Here's a list of the 10 most common ecosystems inhabited by dinosaurs, ranging from dry, dusty deserts to lush, green equatorial jungles. 01 of 10 Plains Photo by Supoj Buranaprapapong / Getty Images The vast, windswept plains of the Cretaceous period were very similar to those of today, with one major exception: 100 million years ago, grass had yet to evolve, so these ecosystems were instead covered with ferns and other prehistoric plants. These flatlands were traversed by herds of plant-eating dinosaurs (including ceratopsians, hadrosaurs, and ornithopods), interspersed with a healthy assortment of hungry raptors and tyrannosaurs that kept these dimwitted herbivores on their toes. 02 of 10 Wetlands Corbis via Getty Images / Getty Images Wetlands are soggy, low-lying plains that have been flooded with sediments from nearby hills and mountains. Paleontologically speaking, the most important wetlands were the ones that covered much of modern Europe during the early Cretaceous period, yielding numerous specimens of Iguanodon, Polacanthus and the tiny Hypsilophodon. These dinosaurs fed not on grass (which had yet to evolve) but more primitive plants known as horsetails. 03 of 10 Riparian Forests Steve Waters / Getty Images A riparian forest consists of lush trees and vegetation growing alongside a river or marsh; this habitat provides ample food for its denizens but is also prone to periodic flooding. The most famous riparian forest of the Mesozoic Era was in the Morrison Formation of late Jurassic North America—a rich fossil bed that has yielded numerous specimens of sauropods, ornithopods, and theropods, including the giant Diplodocus and the fierce Allosaurus. 04 of 10 Swamp Forests Brian W. Downs / Getty Images Swamp forests are very similar to riparian forests, with one important exception: The swamp forests of the late Cretaceous period were matted with flowers and other late-evolving plants, providing an important source of nutrition for huge herds of duck-billed dinosaurs. In turn, these "cows of the Cretaceous" were preyed on by smarter, more agile theropods, ranging from Troodon to Tyrannosaurus Rex. 05 of 10 Deserts janetteasche / Getty Images Deserts present a harsh ecological challenge to all forms of life, and dinosaurs were no exception. The most famous desert of the Mesozoic Era, the Gobi of central Asia, was inhabited by three very familiar dinosaurs—Protoceratops, Oviraptor, and Velociraptor. In fact, the entwined fossils of a Protoceratops locked in combat with a Velociraptor were preserved by a sudden, violent sandstorm one unlucky day during the late Cretaceous period. The world's largest desert—the Sahara—was a lush jungle during the age of the dinosaurs. 06 of 10 Lagoons Abdul Azis / Getty Images Lagoons—large bodies of calm, tepid water trapped behind reefs—weren't necessarily more common in the Mesozoic Era than they are today, but they tend to be overrepresented in the fossil record (because dead organisms that sink to the bottom of lagoons are easily preserved in silt.) The most famous prehistoric lagoons were located in Europe. For example, Solnhofen in Germany has yielded numerous specimens of Archaeopteryx, Compsognathus, and assorted pterosaurs. 07 of 10 Polar Regions Andrew Peacock / Getty Images During the Mesozoic Era, the North and South Poles weren't nearly as cold as they are today—but they were still plunged in darkness for a significant portion of the year. That explains the discovery of Australian dinosaurs like the tiny, big-eyed Leaellynasaura, as well as the unusually small-brained Minmi, a presumably cold-blooded ankylosaur that couldn't fuel its metabolism with the same abundance of sunlight as its relatives in more temperate regions. 08 of 10 Rivers and Lakes Martin Steinthaler / Getty Images Although most dinosaurs didn't actually live in rivers and lakes—that was the prerogative of marine reptiles—they did prowl around the edges of these bodies, sometimes with startling results, evolutionwise. For example, some of the biggest theropod dinosaurs of South America and Eurasia—including Baryonyx and Suchomimus—fed primarily on fish, to judge by their long, crocodile-like snouts. And we now have compelling evidence that Spinosaurus was, in fact, a semiaquatic or even fully aquatic dinosaur. 09 of 10 Islands by JBfotoblog / Getty Images The world's continents may have been arranged differently 100 million years ago than they are today, but their lakes and shorelines were still studded with tiny islands. The most famous example is Hatzeg Island (located in present-day Romania), which has yielded the remains of the dwarf titanosaur Magyarosaurus, the primitive ornithopod Telmatosaurus, and the giant pterosaur Hatzegopteryx. Clearly, millions of years of confinement on island habitats have a pronounced effect on reptile body plans. 10 of 10 Shorelines Peter Unger / Getty Images Like modern humans, dinosaurs enjoyed spending time by the shore—but the shorelines of the Mesozoic Era were located in some very odd places. For example, preserved footprints hint at the existence of a vast, north-south dinosaur migration route along the western edge of the Western Interior Sea, which ran through Colorado and New Mexico (rather than California) during the Cretaceous period. Carnivores and herbivores alike traversed this well-worn path, doubtless in pursuit of scarce food.