Bootherium bombifrons is the scientific term used to describe the regal woodland musk ox. During the Pleistocene era, this large mammal was one of the most prominent musk ox species in North America. Woodland musk ox fossils have been discovered all over the country, including in Alaska, Texas, California, New Jersey, and Oklahoma.
The woodland musk ox is most closely related to the modern musk ox, frequently found in Arctic regions. This species evolved to live best in less frigid climates, which is why it only remained in North America. Bootherium bombifrons were much more significant than their modern descendants, weighing nearly 1,000 pounds. Also, their skulls were thicker, and their snouts were longer. Their horns sat high on the head and curved downwards. Woodland musk oxen ate a diet rich in plants, dining mostly on woody plants, willows and a wide variety of upland grasses.
Most common in Central and South America, the short-faced bear, or Arctotherium angustidens, was present on Earth during the late Pliocene era. These animals are the most closely related to the spectacled bear, a native of South America. Contrary to its name, the short-faced bear did not, in fact, have a little face. Its limbs were so long they made its head look tiny in comparison.
The long appendages of the short-faced bear made them excellent at running. Bears today can run in short bursts, but not for an extended period of time. Arctotherium angustidens were skilled runners and would pounce on their prey like cats. This species weighed between 2,000 and 4,500 pounds, making it the largest bear genus ever discovered and the largest carnivorous land mammal of all time. Experts believe the short-faced bear evolved to be so large because of increased competition from other species like jaguars.
Another member of the Pleistocene megafauna was the woolly rhinoceros. Scientifically known as Coelodonta antiquitatis, these animals most commonly lived in Europe and northern Asia. This animal is the last member of the rhinoceros lineage of the Pleistocene epoch.
The woolly rhinoceros was suited for icy environments. Their stocky legs and woolly fur made it easy for them to withstand freezing tundra conditions. Coelodonta antiquitatis were roughly 9 to 13 feet tall and weighed between 4,000 and 6,000 pounds. They had two keratin horns on the top of their skull and one prominent horn between their eyes for defense. These mammals were grazers and browsers, dining on foliage and other nutritious plants. Woolly rhinos are most closely related to the modern Sumatran rhinoceros.
Research shows that the wild horses living in North America were most likely wiped out by early humans. Toward the end of the Pleistocene era, the extinction of North American horses, mammoths and other large mammals coincided with the Ice Age. These horses, ancestors of modern donkeys, went extinct in North America, but somehow survived in Africa and Eurasia.
The subspecies of the modern horses we know today evolved in North America roughly 1 million to 2 million years ago. Horses began being domesticated by humans starting in 4,000 BC. Fossils indicate that the North American horses went extinct approximately 12,500 years ago. It’s fascinating to imagine the landscape being overrun by majestic North American horses all those years ago.
Mastodons are distant relatives of the wooly mammoth. They migrated to North America via the Bering Strait land bridge roughly 15 million years ago. These creatures were prominent in North and Central America until they went extinct 10,00 years ago due to overharvesting by Clovis hunters.
Typically, mastodons traveled in herds and lived in cold spruce woodland areas. Their eating habits were very similar to modern elephants. They would browse and graze for mixed plants. The bulk of the mastodon diet was coniferous twigs. Mastodons in America had thick, shaggy coats like the wooly mammoth. Their tusks could reach over 16 feet in length and curved slightly upwards. These mammals reached heights up to 9 feet tall and weighed nearly 10 tons.
Known as Smilodon, the saber-toothed tiger most commonly lived in North, South and Central America during the Pleistocene epoch. These animals are notable for their large canine teeth that extend from their mouth. The teeth were used to capture and kill prey quickly and could be as long as 1 foot.
Most saber-toothed tigers are roughly the size of modern cats and built compactly. They had shorter spines, feet, and tails than most felines. Comparable to a jaguar, saber-toothed tigers weighed between 120 and 220 pounds. These mammals were considered apex predators and preyed on large mammals. Bison, pig-like animals called Platygonus and a llama-related creature called Hemiauchenia were targets of the cunning saber-toothed tiger. The dire wolf and American lion were competitors of the saber-toothed tiger. Although it’s named tiger, this mammal is not related to tigers or other modern cats.
Related to modern dragonflies, the Meganeura is the biggest predatory flying insect ever discovered. Its wingspan reaches from 25 to 28 inches. This terrifying insect lived on Earth roughly 300 million years ago. Higher oxygen concentrations in prehistoric times made it possible for this bug to breathe enough to support its size. Luckily, we don’t have to worry about encountering these bugs that are one quarter the size of a human!
Additionally, a lack of predators contributed to the Meganeura being able to evolve to be so large. Scientists also believe that because they were developed in water before appearing on land as adults, they were more equipped to handle high oxygen levels. Meganeura was a predatory species and feasted on other insects. It’s also possible that they ate small amphibians.