Silurian Period (444MYA - 419MYA)
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A Silurian Period (444MYA - 419MYA) is a geologic period (spanning 24.6 million years) from the end of the Ordovician Period to the beginning of the Devonian Period.
References
2018
- (Wikipedia, 2018) ⇒ https://en.wikipedia.org/wiki/Silurian Retrieved:2018-2-21.
- The Silurian is a geologic period and system spanning 24.6 million years from the end of the Ordovician Period, at million years ago (Mya), to the beginning of the Devonian Period, Mya. As with other geologic periods, the rock beds that define the period's start and end are well identified, but the exact dates are uncertain by several million years. The base of the Silurian is set at a major Ordovician–Silurian extinction events when 60% of marine species were wiped out.
A significant evolutionary milestone during the Silurian was the diversification of jawed and bony fish. Multi-cellular life also began to appear on land in the form of small, bryophyte-like and vascular plants that grew beside lakes, streams, and coastlines, and terrestrial arthropods are also first found on land during the Silurian. However, terrestrial life would not greatly diversify and affect the landscape until the Devonian.
- The Silurian is a geologic period and system spanning 24.6 million years from the end of the Ordovician Period, at million years ago (Mya), to the beginning of the Devonian Period, Mya. As with other geologic periods, the rock beds that define the period's start and end are well identified, but the exact dates are uncertain by several million years. The base of the Silurian is set at a major Ordovician–Silurian extinction events when 60% of marine species were wiped out.