Where is dinosaurs live

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. Deserts present a harsh ecological challenge to all forms of life, and dinosaurs were no exception. 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. 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.

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.

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. The world's continents may have been arranged differently 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. This web site gives you a look at just how far back that was hereistoday.

When you get to the current aeon, you will notice three eras: Paleozoic, Mesozoic, and Cenozoic. Dinosaurs existed only in the Mesozoic era, we are at the very end of the Cenozoic period. Well, to answer that, we need to talk about something called plate tectonics remember that we learnt about back in Planet Earth week.

The centre of the Earth is mostly molten, liquid rocks that the crust floats on. This map lets you see which dinosaurs lived in your hometown. Share this story Share this on Facebook Share this on Twitter Share All sharing options Share All sharing options for: This map lets you see which dinosaurs lived in your hometown.

Reddit Pocket Email Linkedin. Now, you can see, thanks to an interactive map. Screenshot, Ian Webster California paleontologist Ian Webster has created a new interactive map that lets you see which dinosaurs lived in your hometown millions of years ago. The world is warm and has no polar ice caps. Large reptiles dominate and mammals remained small. Flowering plants evolve and spread throughout the world. The extinction of plants reduced food supply for large herbivorous reptiles, and removed habitat for insects.

The history of Earth is longer than we can conceive, and the current arrangement of plate tectonics and continents is an accident of time. These regions became more distinct later in the period.

Temperatures fell slightly, although it was still warmer than today due to higher amounts of carbon dioxide in the atmosphere. Rainfall increased as a result of the large seas appearing between the land masses.

These changes allowed plants such as ferns and horsetails to grow over huge areas. Some of this vegetation became the fossil fuels that we mine today. Elsewhere there were forests of tall conifer trees such as sequoias and monkey puzzles. The large sauropod dinosaur Diplodocus lived in the Jurassic Period. Explore other dinosaurs from the Late Jurassic. The plentiful plant supply allowed the huge plant-eating sauropods - such as Apatosaurus , Diplodocus and Brachiosaurus - to evolve. These are some of the largest animals to have ever walked the Earth.

By the end of the Jurassic their herds dominated the landscape. Sauropods became even larger in the Cretaceous. During the Cretaceous the land separated further into some of the continents we recognise today, although in different positions. This meant that dinosaurs evolved independently in different parts of the world, becoming more diverse.

Can you spot the dinosaur in this Cretaceous environment? See more dinosaurs that lived in the Late Cretaceous. Other groups of organisms also diversified.

The first snakes evolved during this time, as well as the first flowering plants. Various insect groups appeared, including bees, which helped increase the spread of flowering plants.

And mammals now included tree climbers, ground dwellers and even predators of small dinosaurs. Sea levels rose and fell repeatedly during the Cretaceous Period.