If you wound up in the Mesozoic would you recognize Earth?
So if you woke up in the Paleozoic, you probably wouldn't recognize Earth. How about if you woke up in the Mesozoic? In some ways, the planet would look a lot more like it does today. Animals would fill the niches you're used to seeing animals fill. But if you looked closely, you'd see that the animals are mostly all reptiles. And some of them may be interested in having you for dinner!
With most niches available after the mass extinction, a great diversity of organisms evolved. Mostly these niches were filled with reptiles.
Climate alternated between cool, warm, and tropical, but overall the planet was much warmer than today. These conditions were good for reptiles. Surprisingly, there was more oxygen in the Mesozoic atmosphere than there is today.
Tiny phytoplankton arose to become the base of the marine food web. At the beginning of the Mesozoic, Pangaea began to break apart, so more beaches and continental shelf areas were available for colonization by new species of marine organisms. Marine reptiles colonized the seas and diversified. Some became huge, filling the niches that are filled by large marine mammals today.
On land, seed plants and trees diversified and spread widely. Lush forests covered much of the land, especially at higher altitudes. Flowering plants evolved during the Cretaceous (Figure below).
The earliest known fossil of a flowering plant is this 125 million year old Cretaceous fossil.
Of course the most famous Mesozoic reptiles were the dinosaurs. Dinosaurs reigned for 160 million years and had tremendous numbers and diversity. Species of dinosaurs filled all the niches that are currently filled by mammals. Dinosaurs were plant eaters, meat eaters, bipedal, quadrupedal, endothermic (warm-blooded), exothermic (cold-blooded), enormous, small, and some could swim or fly.
Some examples of Mesozoic dinosaurs include the Ornithopods. Pictured far left: Camptosaurus, left: Iguanodon, center background: Shantungosaurus, center foreground: Dryosaurus, right: Corythosaurus, far right (small): Heterodontosaurus, far right (large) Tenontosaurus.
Scientists now think that some dinosaurs were endotherms (warm-blooded) due to the evidence that has been collected over the decades. There are still some scientists who do not agree, but the amount of evidence makes it likely. Some dinosaurs lived in polar regions where animals that needed sunlight for warmth could not survive in winter. Dinosaurs bones had canals, similar to those of birds, indicating that they grew fast and were very active. Fast growth usually indicates an active metabolism typical of endotherms. Dinosaurs had erect posture and large brains, both correlated with endothermy.
An interesting look at the points for dinosaur endothermy is seen here: http://www.ucmp.berkeley.edu/diapsids/endothermy.html.
Rise of the Mammals
Mammals appeared near the end of the Triassic, but the Mesozoic is known as the age of the reptiles. In a great advance over amphibians, which must live near water, reptiles developed adaptations for living away from water. Their thick skin keeps them from drying out, and the evolution of the amniote egg allowed them to lay their eggs on dry land. The amniote egg has a shell and contains all the nutrients and water required for the developing embryo.
Amniotic egg containing a tortoise hatchling.
Cretaceous Mass Extinction
Between the Mesozoic and the Cenozoic, 65 million years ago, about 50% of all animal species, including the dinosaurs, became extinct. Although there are other hypotheses, most scientists think that this mass extinction took place when a giant meteorite struck Earth with the energy of the most powerful nuclear weapon (Figure below).
An artist’s painting of the impact that caused the Cretaceous extinctions.
The impact kicked up a massive dust cloud, and when the particles rained back onto the surface they heated the atmosphere until it became as hot as a kitchen oven. Animals roasted. Dust that remained in the atmosphere blocked sunlight for a year or more, causing a deep freeze and temporarily ending photosynthesis. Sulfur from the impact mixed with water in the atmosphere to form acid rain, which dissolved the shells of the tiny marine plankton that form the base of the food chain. With little food being produced by land plants and plankton, animals starved. Carbon dioxide was also released from the impact and eventually caused global warming. Life forms could not survive the dramatic temperature swings.
You may be surprised to know that dinosaurs in one form survived the mass extinctions and live all over the world today. Birds evolved from theropod dinosaurs, and these creatures not only survived the asteroid impact and its aftermath, but they have also diversified into some of the most fantastic creatures we know (Figure below).
Archeopteryx, the earliest known bird, lived during the late Jurassic.
- Phytoplankton evolved to become the base of the marine food web.
- In the Mesozoic dinosaurs filled the niches that mammals fill today.
- Life of the Mesozoic appears to have ended with a giant asteroid impact.
Use this resource to answer the questions that follow.
1. When did the asteroid impact the Earth?
2. How large was the impact?
3. Where did it hit?
4. What were the primary killers from this impact?
5. Describe how the Earth looked from space after the impact.
6. How did most of the animals die?
7. Why did the fires burn so hot and intensely?
8. What animal survived the aftermath of the impact?
1. How did life in the Mesozoic resemble life today? How did it differ from life today?
2. What was the importance of the amniote egg for Mesozoic life?
3. Why do scientists say that dinosaurs didn't entirely go extinct? What is their evidence?