The Paleozoic Era lasted 291 million years from the start of the Cambrian Period 542 million years ago until the end of the Permian Period 251 million years ago.
Life of every kind went through great changes.
The first evidence for plants predate the Paleozoic Era. Evidence that resembles green algae is found in rocks in the late Proterozoic Eon but exact classification into the Kingdom Plantae has not been confirmed.
The first confirmed plants come from the Cambrian Period(542 - 488.3Ma). They take the form of simple green algae possibly of the order Dasycladales. These normally live in aquatic environments. It is during this period that we find evidence for the first plants on land. Fossil species closely related to the river plant Charales have been found in rocks from around this age.
It was not until the Ordovician Period(488.3 - 443.7Ma) that the first Embryophytes evolved. Embryophytes is the clade of plants that contain most of the plants that you would recognise. These plants are primarily land plants although some species are considered semi- aquatic. Fossils from this period are fragmentary and exact classification is difficult.
The Silurian Period(443.7 - 416Ma) gives us the first complete fossils of Embroyophytes. This is the time in history that we can confirm wide spread land plants. Species such as the extinct Lycopodiophyta Baragwanathia longfolia become common in terrestrial environments.
During the Devonian Period(416 - 359.2Ma) we see the first evidence of the first trees. The earliest known trees the Wattieza & Archaropteris were closly related to ferns unlike most modern trees. They grew up into huge forests pumping vast amounts of oxygen into the atmosphere.
By the Carboniferous Period(359.2 - 299Ma) these forests covered the land. Most of the coal on the planet are the remains of these huge forests. The levels of oxygen in the atmosphere were much higher than today as a result of these forest. It was this that allowed the arthropods to become massive. The first conifers appear at this time in history.
The Permian Peroid(299 - 251Ma) saw the formation of the super-continent Pangaea. The interior of this continent was dominated by huge deserts. The changes in environment caused huge changes in the plants that dominated the land. By the end of the Permian the fern like trees, that had dominated for millions of years, had been replaced by conifers as the most common trees on the planet.
The end of the Paleozoic Era was marked by the planets worst extinction event, the Permian-Triassic Extinction or "The Great Dying". It shows a clear decline in the conifer species and the beginning of the Mesozoic Era a resurgence of the Lycopdhates.
It was not until the Mesozoic Era that plants that dominate most environments on land today such as flowering plants and grasses evolved.
The Devonian era is a geological period that occurred approximately 419 million to 359 million years ago. It is known for the diversification of marine life, including the appearance of early fish and amphibians, as well as the spread of forests on land.
The Cambrian period was part of the Paleozoic era. It occurred roughly 541 to 485 million years ago and is known for the rapid diversification of multicellular life forms, often referred to as the "Cambrian explosion."
The permian period was the end of the paleozoic era.
ok im going to start off by saying this, the last answerer is stupid, and doesnt know what he is talking about. it goes from: PERIOD ERA EPOCH there you go ;)
Precambrian Era Paleozoic Era Mesozoic Era Cenozoic Era
i cant answer this :(
The Paleozoic Era is also known as the age of ancient life.
The Paleozoic Era.
The Paleozoic Era, because rich fossil evidence displays that early life in the time of the Paleozoic Era, there existed a dicersity of marine life.
The Cambrian Period was from about 543 to 490 million years ago. It is the earliest period in the Paleozoic ("old life") Era. Until relatively recently paleontologists thought this marked the beginning of life. Primitive life is now know from the Pre-Cambrian Eon.
Marine life, Amphibians.
During the Paleozoic Era, dominant plant forms included ferns, horsetails, and early seed plants like conifers and cycads. These plants were the main producers in terrestrial ecosystems, contributing to the diversity and abundance of life during this time period.
The era that immediately follows the Precambrian is the Paleozoic Era. It is characterized by the diversification of life forms, including the rise of fishes, insects, and amphibians.
Yes. If no animals survived from the Paleozoic into the mesozoic, then there would be no animals today.
The Precambrian is actually the longest block (division) of time in earth geological history. But the Paleozoic era is the longest of the three "eras". The paleozoic era started about 550 million years ago and is marked by the appearance of abundant invertebrate life in the oceans. The paleozoic era ended about 225 million years ago with the forming of the supercontinent Pangaea.
The main characteristic that distinguishes the fossil record of the Paleozoic Era from the Precambrian Era is the appearance of diverse and complex multicellular organisms in the Paleozoic Era. In the Precambrian Era, the fossil record primarily consists of simpler single-celled organisms. Additionally, the Cambrian Explosion, which occurred at the beginning of the Paleozoic Era, marked a significant increase in the diversity of life forms.
The first period in the Paleozoic Era was the Cambrian.