Not Extinct Through out the Cenozoic era, the oceans were home to nearly the same invertebrate animals as today. Foraminifera were common as well. Sponges, coral, starfish, seaurchens, and sand dollars were common as well Brachiopods and cephalopods were rare. Mollusksclams, oysters, mussels, and snails- thrived through out the era. Crabs and barnacles were common as well. A land, the spiders, centipedes, scorpions, and insects continued to thrive. Insects including butterflies, moths, bees, wasps, ants, beetles, and many others. Most Cenozoic fish were like that of late Mesozoic time. Sharks and rays were abundant and gigantic. Some sharks were 20 meters long with jaws nearly 2 meters wide. Amphibians, such as frogs, toads, and salamanders, were about as common as they are now. The reptiles-turtles, lizards, snake, and crocodiles- resemble those of today. Birds developed that were similar to those of today. At times, there were many large, flightless, ostrich like types. Some were three meters tall. Extinct Creodonts, oreodons an early grazing animal that resembles a deer, the mastodon a kind of gigantic elephant, brontotherium a gigantic rhino like animal, blachitherium rhino like animal , armadillo a gigantic sloth like animal. These are just some of the animals that lived in the Cenozoic era that are now extinct.
The common femoral vein is medial to the common femoral artery. The common femoral artery lies farther from the body's midline.
Quarry is a common noun. Quiz is a common noun.
The term common wealth comes from the Latin common weal, meaning common good.
Yarrow (common name) Ylang-ylang (common name) Yew (common name) Yasmin (common name) Yucca (botanical name)
Mass extinction
Mammals became the dominant land animals in the early Paleocene period of the Cenozoic era, after the extinction of the non-avian dinosaurs at the end of the Cretaceous period of the Mesozoic era.
Some common abbreviations for geologic time periods are: Cenozoic (CE), Mesozoic (ME), Paleozoic (PE), Precambrian (PC), Quaternary (Q), Tertiary (T), Jurassic (J), Triassic (Tri), and Devonian (Dev).
"Age of the dinosaurs" is a common nickname for the Mesozoic Era because it was a period when dinosaurs dominated the Earth.
Rocks from the Precambrian period are typically igneous and metamorphic, formed before complex life existed. Sedimentary rocks become more common in the Paleozoic, Mesozoic, and Cenozoic eras, which include the Quaternary period, reflecting changes in Earth's environment and life forms over time. The Quaternary period is also characterized by glacial deposits and other evidence of ice ages.
stromatolites
Trilobites are common fossils throughout the Paleozoic.
cycads
"Pangaea" is a proper noun. It refers to the supercontinent that existed during the late Paleozoic and early Mesozoic eras.
Paleozoic
stromatolites
Western