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Carboniferous Forest - Artist's view of a forest in North America 350 million years ago....
IMAGE
number
PIX4632896
Image title
Carboniferous Forest - Artist's view of a forest in North America 350 million years ago. The species presented here are Lepidodendron aculeatum (which resemble feathers on long sticks), Sigillaria scutellata, Asteroxylon mackiei (at this scale can be confused with grass), and ferns. A Carboniferous forest of Midwestern North America 350 million years ago featuring Lepidodendron aculeatum (resembling feather dusters on long sticks), Sigillaria scutellata (resembling toilet bowl brushes), Asteroxylon mackiei (at this scale may be mistaken for grass), and ferns. Some Lepidodendron grew as tall as 150 feet. 360 million years ago the Earth entered a period known as the Carboniferous, a 60 million year span remarkable for worldwide high temperatures, high humidity, and the emergence of thousands of new terrestrial plant and animal species. Dense forests of arboreal lycopods covered much of the vast continent of Pangaea. This enormous biomasset eventually became the source for the great bituminous coal fields of North America, Europe and Asia
Carboniferous Forest - Artist's view of a forest in North America 350 million years ago. The species presented here are Lepidodendron aculeatum (which resemble feathers on long sticks), Sigillaria scutellata, Asteroxylon mackiei (at this scale can be confused with grass), and ferns. A Carboniferous forest of Midwestern North America 350 million years ago featuring Lepidodendron aculeatum (resembling feather dusters on long sticks), Sigillaria scutellata (resembling toilet bowl brushes), Asteroxylon mackiei (at this scale may be mistaken for grass), and ferns. Some Lepidodendron grew as tall as 150 feet. 360 million years ago the Earth entered a period known as the Carboniferous, a 60 million year span remarkable for worldwide high temperatures, high humidity, and the emergence of thousands of new terrestrial plant and animal species. Dense forests of arboreal lycopods covered much of the vast continent of Pangaea. This enormous biomasset eventually became the source for the great bituminous coal fields of North America, Europe and Asia
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