Further information: Evolutionary history of plants
The evolution of plants has resulted in increasing levels of complexity, from the earliest algal mats, through bryophytes, lycopods, ferns to the complex gymnosperms and angiosperms of today. The groups which appeared earlier continue to thrive, especially in the environments in which they evolved.
Evidence suggests that an algal scum formed on the land 1,200 million years ago, but it was not until the Ordovician Period, around 450 million years ago, that land plants appeared.[29]
However, new evidence from the study of carbon isotope ratios in
Precambrian rocks has suggested that complex photosynthetic plants
developed on the earth over 1000 m.y.a.[30] These began to diversify in the late Silurian Period, around 420 million years ago, and the fruits of their diversification are displayed in remarkable detail in an early Devonian fossil assemblage from the Rhynie chert.
This chert preserved early plants in cellular detail, petrified in
volcanic springs. By the middle of the Devonian Period most of the
features recognised in plants today are present, including roots, leaves
and secondary wood, and by late Devonian times seeds had evolved.[31]
Late Devonian plants had thereby reached a degree of sophistication
that allowed them to form forests of tall trees. Evolutionary innovation
continued after the Devonian period. Most plant groups were relatively
unscathed by the Permo-Triassic extinction event,
although the structures of communities changed. This may have set the
scene for the evolution of flowering plants in the Triassic (~200 million years ago),
which exploded in the Cretaceous and Tertiary. The latest major group
of plants to evolve were the grasses, which became important in the mid
Tertiary, from around 40 million years ago. The grasses, as well as many other groups, evolved new mechanisms of metabolism to survive the low CO2 and warm, dry conditions of the tropics over the last 10 million years.
A proposed phylogenetic tree of Plantae, after Kenrick and Crane,[32] is as follows, with modification to the Pteridophyta from Smith et al.[33] The Prasinophyceae are a paraphyletic assemblage of early diverging green algal lineages.[34]
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