They lived in the ocean because they were marine animals.
The went for a wlk
Earth is the planet with the most life forms.
Warm, shallow seas covered most of Earth's surface near the end of the Paleozoic Era.
we had the same question for homework. its paleozoic era it had alot of information in our textbook. and if you look on the geologic time scale it show you the Most information. hope this helped
All you need for life forms (most simple forms) is amino acids. They have actually been created by scientists.
Most extremophiles are simple, single-celled life forms, yet many are not. Extremophiles occur in all three domains of life: bacteria, archaea, and eukaryotes. ... However, archaea aren't restricted to extreme environments; they live in most of the same places as bacteria
The Precambrian life forms were less developed than the Paleozoic life forms.
The Precambrian life forms were less developed than the Paleozoic life forms.
The Precambrian life forms were less developed than the Paleozoic life forms. The Precambrian life forms were just starting to develop because this was 544 million years ago. that meant that things still needed to grow. This time didn't last very long though, due to the morphic and erosional processes. The Paleozoic Era began when organisms began developing new hard parts. This made it easier for fossils to be preserved.
yes
true. I think.
Earth is the planet with the most life forms.
paleozoic
If you're talking about geological eras, they would be the Precambrian - beginnings of life, mainly ruled by bacteria Paleozoic - most basic body forms evolved like insects, amphibians, etc. Mesozoic - dinosaurs Cenozoic - humans
If you're talking about geological eras, they would be the Precambrian - beginnings of life, mainly ruled by bacteria Paleozoic - most basic body forms evolved like insects, amphibians, etc. Mesozoic - dinosaurs Cenozoic - humans
Warm, shallow seas covered most of Earth's surface near the end of the Paleozoic Era.
Paleozoic
Most of the periods of the Paleozoic Era are named after the areas in which examples of the rocks of those periods were first described or are plentiful.