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Sometimes
divided into the Mississippian (363-330 mil.year.ago) and
Pennysilvanian (330-286 mil.year.ago)
The
warm and humid Carboniferous period (286-363
MYA)
saw the global
explosion of a new kind of ecosystem. Great swamps spread over much of the land
and giant trees towered over the dense vegetation. Dead plants
formed a layer of wet peat, which eventually became coal.
Carboniferous coal often contains
the fossils of leaves, trunks, roots and fruit. Many of these
come from a tree called Lepidodendron, which could grow
as high as 50 metres in just a few years. Different parts of the
tree have different latin names because they were originally
thought to belong to different species. The cones are called
Lepidostrobus and the thick root-bearing branches at the
base are called Stigmaria. The trees' great height
enabled them to catch sunlight way above the shorter plants, but
also made them rather precarious. Fully grown trees toppled over
and added to the swamp.
Arthropods like
Acantherpestes, the giant millipede, fed on the decomposing
plant debris. Some of its relatives also reached gigantic size -
90cm(inch)-long scorpions and enormous dragonflies also lived in
the forests.
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