Taxodium

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Taxodium
Temporal range: Late Cretaceous–Present
Taxodium distichum NRCSMS01010.jpg
Bald Cypress forest
in a central Mississippi lake
Scientific classification
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Taxodium

Species

Taxodium ascendens - Pond cypress
Taxodium distichum - Bald cypress
Taxodium mucronatum - Montezuma cypress
Taxodium dubium

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Taxodium /tækˈsdiəm/[2] is a genus of one to three species (depending on taxonomic opinion) of extremely flood-tolerant conifers in the cypress family, Cupressaceae. The generic name is derived from the Latin word taxus, meaning "yew", and the Greek word εἶδος (eidos), meaning "similar to."[3] Within the family, Taxodium is most closely related to Chinese swamp cypress (Glyptostrobus pensilis) and sugi (Cryptomeria japonica).

Species of Taxodium occur in the southern part of the North American continent and are deciduous in the north and semi-evergreen to evergreen in the south. They are large trees, reaching 100–150 ft (30–46 m) tall and 2–3 m (6.6–9.8 ft) (exceptionally 11 m or 36 ft) trunk diameter. The needle-like leaves, 0.5–2 cm (0.20–0.79 in) long, are borne spirally on the shoots, twisted at the base so as to appear in two flat rows on either side of the shoot. The cones are globose, 2–3.5 cm (0.79–1.38 in) diameter, with 10-25 scales, each scale with 1-2 seeds; they are mature in 7–9 months after pollination, when they disintegrate to release the seeds. The male (pollen) cones are produced in pendulous racemes, and shed their pollen in early spring. Taxodium species grow pneumatophores, or cypress roots, when growing in or beside water; these are woody projections which rise above the water and are said to help carry oxygen to the root systems.

Species

The three extant taxa of Taxodium are treated here as distinct species, though some botanists treat them in just one or two species, with the others considered as varieties of the first described. The three are distinct in ecology, growing in different environments, but hybridise where they meet.

The pond cypress occurs within the range of bald cypress, but only on the southeastern coastal plain from North Carolina to Louisiana. It occurs in still blackwater rivers, ponds and swamps without silt-rich flood deposits.

The most familiar species in the genus is the bald cypress, native to much of the southeastern United States, from Delaware to Texas, especially Louisiana and inland up the Mississippi River to southern Indiana. It occurs mainly along rivers with silt-rich flood deposits.

The Montezuma cypress occurs from the Lower Rio Grande Valley south to the highlands of Guatemala, and differs from the other two species in being substantially evergreen. A specimen in Santa María del Tule, Oaxaca, the Árbol del Tule, is 43 m (141 ft) tall and has the greatest trunk thickness of all trees, 11.42 m (37.5 ft) in diameter. It is a riparian tree, occurring on the banks of streams and rivers, not in swamps like the bald and pond cypresses.

Formerly placed here

Uses

Cypress knees at low water, Wee Tee Lake, South Carolina

The trees are especially prized for their wood, of which the heartwood is extremely rot- and termite-resistant. The heartwood contains a sesquiterpene called cypressene,[5] which acts as a natural preservative. It takes decades for cypressene to accumulate in the wood, so lumber taken from old-growth trees is more rot resistant than that from second-growth trees.[6] However, age also increases susceptibility to Pecky Rot fungus (Stereum taxodii), which attacks the heartwood and causes some damaged trees to become hollow and thus useless for timber. Bald Cypress wood was much used in former days in the southeastern United States for roof shingles.[7] The shredded bark of these trees is used as a mulch, the current harvest rate for this product is easily sustainable with an annual growth rate of 6 times that of its harvest.[8]

Evolution

File:Fossil-leaf Taxodium dubium Tertiary Germany.jpg
Fossil leaf of Taxodium dubium, 8 Mil. years old, Hambach lignite open pit mine, Germany

In earth's history Taxodium was much more widespread in the Northern Hemisphere than today. The oldest fossils were found in Late Cretaceous deposits from North America. The trees persisted in Europe until around 2.5 million years ago, during the Pliocene.[9]

See also

References

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  2. Sunset Western Garden Book, 1995:606–607
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External links