Line | The dry mountain ranges of the western United |
States contain rocks dating back 440 to 510 million | |
years, to the Ordovician period, and teeming with | |
evidence of tropical marine life. This rock record | |
(5) | provides clues about one of the most significant |
radiations (periods when existing life-forms gave rise | |
to variations that would eventually evolve into entirely | |
new species) in the history of marine invertebrates. | |
During this radiation the number of marine biological | |
(10) | families increased greatly, and these families included |
species that would dominate the marine ecosystems | |
of the area for the next 215 million years. Although | |
the radiation spanned tens of millions of years, | |
major changes in many species occurred during a | |
(15) | geologically short time span within the radiation and, |
furthermore, appear to have occurred worldwide, | |
suggesting that external events were major factors | |
in the radiation. In fact, there is evidence of major | |
ecological and geological changes during this period: | |
(20) | the sea level dropped drastically and mountain ranges |
were formed. In this instance, rather than leading to | |
large-scale extinctions, these kinds of environmental | |
changes may have resulted in an enriched pattern of | |
habitats and nutrients, which in turn gave rise to the | |
(25) | Ordovician radiation. However, the actual relationship |
between these environmental factors and the | |
diversification of life-forms is not yet fully understood. |