Arthropod - biology.
Publié le 11/05/2013
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through a series of distinct phases to become adults.
Larvae may also inhabit different environments and eat different foods than their parents.
The life spans ofarthropods range from a few weeks to several decades.
V ARTHROPOD EVOLUTION
The evolutionary origins of modern arthropods are unclear and complex.
It is generally accepted that the phylum is polyphyletic—that is, derived from several separateancestral lines.
The ancestors of arthropods were ancient aquatic segmented worms, similar to present-day annelids, although the fossil evidence is sketchy.
The ancientseas of the Cambrian and Ordovician periods (570 million to 435 million years ago) were teeming with aquatic arthropods, especially trilobites.
During the Silurian and Devonian periods (435 million to 360 million years ago), the arthropods were among the first animals to leave the water and colonize the land.When they emerged from the water, they had few, if any, competitors.
They swiftly adapted to the demands of terrestrial life, occupying new niches as predators, planteaters, parasites, and decomposers.
The earliest terrestrial arthropod fossil is of a scorpion-like arachnid.
The earliest insect fossils come from a few million years later.These early terrestrial arthropods sometimes reached great size, much larger than any land arthropods known today.
Scientists have found evidence that Earth’satmosphere had more oxygen (perhaps as high as 40 percent compared to 21 percent in our modern world).
Higher oxygen pressure would have enabled animals withrelatively primitive breathing systems, such as those found in land arthropods, to be active even in very large animals.
By the end of the Carboniferous period (360million to 290 million years), four-legged vertebrates (amphibians and reptiles) dominated the land and used arthropods as a major source of food.
Scientific classification: Arthropods make up the phylum Arthropoda, which is divided into three living subphyla: Chelicerata, Crustacea, and Unirama.
Contributed By:David George GordonMicrosoft ® Encarta ® 2009. © 1993-2008 Microsoft Corporation.
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