The Silurian went from 443.4 ± 1.5mya to 419.2 ± 3.2mya. It spanned from the conclusion of the Ordovician period to the beginning of the Devonian period. However the exact time frame of the Silurian period is unknown and could be off by millions of years because of the fact that that period was set during a significant extinction event. Therefore, the Silurian period lasted about 42 million years, give or take.
Life forms existed during the Cambrian period.
Ediacara life-forms are a group of soft-bodied, early multicellular organisms that existed in the Ediacaran Period, around 635-541 million years ago. They were some of the earliest complex organisms on Earth and existed prior to the Cambrian explosion. Ediacara biota are known for their diverse body plans and unique shapes.
Various life forms have existed on Earth, including bacteria, plants, animals, and humans. These life forms have evolved over billions of years to adapt to different environments and ecosystems on our planet. Additionally, extinct life forms such as dinosaurs and ancient mammals have also played a significant role in Earth's biodiversity.
These are periods in the geologic timescale, spanning from 145 million years ago (Cretaceous) to 443 million years ago (Ordovician). Each period represents a distinct time in Earth's history characterized by specific events and changes in life forms, such as the extinction of dinosaurs in the Cretaceous period or the diversification of marine life in the Ordovician period.
Plants, such as mosses and liverworts, began to colonize damp areas on land during the Silurian period. These early land plants played a crucial role in the colonization of terrestrial environments and paved the way for the diversification of plant life on land.
fish
Life forms existed during the Cambrian period.
The Silurian period started off with a mass extinction of 60% of all marine life. During the Silurian bony fishes evolved setting the stage for the Devonian, which is referred to as the "Age of the Fish".
Arthropods ( EARTH SCIENCE )
Ediacara life-forms are a group of soft-bodied, early multicellular organisms that existed in the Ediacaran Period, around 635-541 million years ago. They were some of the earliest complex organisms on Earth and existed prior to the Cambrian explosion. Ediacara biota are known for their diverse body plans and unique shapes.
Corals were a dominate life form during the Silurian period because the climate was much warmer in the oceans and the ocean's were actually larger than they are today. This gave coral a chance to grow large and strong.
Of or pertaining to, or designating, the older division of geological time during which life is known to have existed, including the Silurian, Devonian, and Carboniferous ages, and also to the life or rocks of those ages. See Chart of Geology.
Various life forms have existed on Earth, including bacteria, plants, animals, and humans. These life forms have evolved over billions of years to adapt to different environments and ecosystems on our planet. Additionally, extinct life forms such as dinosaurs and ancient mammals have also played a significant role in Earth's biodiversity.
These are periods in the geologic timescale, spanning from 145 million years ago (Cretaceous) to 443 million years ago (Ordovician). Each period represents a distinct time in Earth's history characterized by specific events and changes in life forms, such as the extinction of dinosaurs in the Cretaceous period or the diversification of marine life in the Ordovician period.
Plants, such as mosses and liverworts, began to colonize damp areas on land during the Silurian period. These early land plants played a crucial role in the colonization of terrestrial environments and paved the way for the diversification of plant life on land.
The middle Paleozoic era is known as the Devonian period. The period ended with the death of many species of vertebrate life. During this time, many life forms transitioned from living in the water to living on land.
During the Silurian period, most of the land was clustered around the equator in a supercontinent called Gondwana. It was mostly covered by shallow seas, with a warmer climate and diverse marine life. Compared to present-day continents, the landmasses were different in shape and position due to plate tectonics shifting over millions of years.