Вопрос задан 09.11.2023 в 18:12. Предмет Окружающий мир. Спрашивает Александров Артём.

Палеозой дәуірінде не пайда болды?​

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Palaeozoic or Paleozoic era is a formative time in Earth's history that lasted from approximately 541 to 252 million years ago. During this era, significant geological, biological, and environmental changes occurred, shaping the planet's future.

One major event during the Palaeozoic era was the emergence of the first complex multicellular life forms, which evolved from simpler single-celled organisms. This era is often called the "Age of Invertebrates" because it saw the rise and dominance of a wide variety of marine invertebrates, such as trilobites, brachiopods, and coral reefs.

The Palaeozoic era also witnessed the colonization of land by plants and animals. Plants evolved from simple spore-bearing organisms to more complex forms, including the first trees and forests. This transformation of the land allowed for the emergence of terrestrial animals, starting with arthropods like millipedes and spiders, followed by amphibians as the first vertebrates to venture onto land.

Another significant event during the Palaeozoic era was the diversification of fish. Jawless fish, such as lampreys, were succeeded by jawed fish, which eventually gave rise to the first sharks and bony fish. This era also witnessed the evolution of early amphibians, which eventually led to the development of reptiles and ultimately dinosaurs.

The Palaeozoic era ended with the largest mass extinction event in Earth's history, known as the Permian-Triassic extinction event. This cataclysmic event resulted in the extinction of approximately 96% of marine species and 70% of terrestrial vertebrate species. It marked the transition from the Palaeozoic era to the Mesozoic era, which saw the rise of dinosaurs and the eventual appearance of mammals.

In conclusion, the Palaeozoic era was an incredibly transformative time in Earth's history, witnessing the emergence of complex life forms both in the ocean and on land. It laid the foundation for future biological and ecological developments, ultimately shaping the world as we know it today.

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