Sabal palmetto (Walter, 1788) - cabbage palm trees in Florida, USA. (summer 2009)

Plants are multicellular, photosynthesizing eucaryotes. Most species occupy terrestrial environments, but they also occur in freshwater and saltwater aquatic environments. The oldest known land plants in the fossil record are Ordovician to Silurian. Land plant body fossils are known in Silurian sedimentary rocks - they are small and simple plants (e.g., Cooksonia). Fossil root traces in paleosol horizons are known in the Ordovician. During the Devonian, the first trees and forests appeared. Earth's initial forestation event occurred during the Middle to Late Paleozoic. Earth's continents have been partly to mostly covered with forests ever since the Late Devonian. Occasional mass extinction events temporarily removed much of Earth's plant ecosystems - this occurred at the Permian-Triassic boundary (251 million years ago) and the Cretaceous-Tertiary boundary (65 million years ago).

The most conspicuous group of living plants is the angiosperms, the flowering plants. They first unambiguously appeared in the fossil record during the Cretaceous. They quickly dominated Earth's terrestrial ecosystems, and have dominated ever since. This domination was due to the evolutionary success of flowers, which are structures that greatly aid angiosperm reproduction.

The plants shown above are cabbage palm trees, Sabal palmetto. Between two and three thousand species of palms have been described. The cabbage palm is native to Florida and the tree is widely used in landscaping. This species' distribution includes the northern Caribbean and Bahamas Platform, plus the subtropical portions of America's Gulf of Mexico and North Atlantic coastlines.

Classification: Plantae, Angiospermophyta, Arecales, Palmae/Arecaceae

Locality: just inland from Bowman's Beach, southern shoreline of western Sanibel Island, Gulf of Mexico coast of southwestern Florida, USA

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