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Metasequoia

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This article is about the tree named Metasequoia glyptostroboides. For other uses, see Metasequoia (disambiguation).

Metasequoia glyptostroboides

Conservation status

Critically endangered (IUCN)

Scientific classification

Kingdom:	Plantae
Division:	Pinophyta
Class:	Pinopsida
Order:	Pinales
Family:	Cupressaceae
Genus:	Metasequoia Miki, 1941
Species:	M. glyptostroboides

Binomial name

Metasequoia glyptostroboides
Hu & W.C.Cheng, 1948

Metasequoia glyptostroboides (Dawn Redwood) is a fast growing tree in the conifer family Cupressaceae native to the Sichuan-Hubei region of China. Metasequoia, along with Sequoia, Sequoiadendron and several other genera, was transferred from the Taxodiaceae family to Cupressaceae using DNA analysis.^[1] It is the only living species in the ancient redwood genus Metasequoia, but three fossil species are known.

Dawn Redwood foliage - note opposite arrangement

While the bark and foliage are similar to another closely related redwood genus Sequoia, Metasequoia differs from the California redwood in that it is deciduous like Taxodium distichum (Bald Cypress), and like that species, older specimens form wide buttresses on the lower trunk. It is a fast-growing tree to 40-45 m tall and 2 m trunk diameter in cultivation so far (with the potential to grow to even greater heights). The leaves are opposite, 1-3 cm long, and bright fresh green, turning a foxy red-brown in fall. The cones are globose to ovoid, 1.5-2.5 cm in diameter with 16-28 scales, arranged in opposite pairs in four rows, each pair at right angles to the adjacent pair; they mature in about 8-9 months after pollination. The pollen cones are 5-6 mm long, produced on long spikes in early spring; they are only produced on trees growing in regions with hot summers. Metasequoia was first described as a fossil from the Mesozoic Era by Shigeru Miki in 1941, but in 1944 a small stand of an unidentified tree was discovered in China in Modaoxi by Zhan Wang; due to World War II, these were not studied further until 1946 and only finally described as a new living species of Metasequoia in 1948 by Wan Chun Cheng and Hu Hsen Hsu. In 1948 the Arnold Arboretum of Harvard University sent an expedition to collect seeds and, soon after, seedling trees were distributed to various universities and arboreta worldwide for growth trials. In the late 1980s, it was discovered that many of the second generation trees in cultivation suffered from inbreeding depression (extremely low genetic variability) which could lead to increased susceptibility to disease and reproductive failure. This was because most of the trees were grown from seeds and cuttings derived from as few as three trees that the Arnold Arboretum had used as its source. More widespread seed-collecting expeditions in China in the 1990s sought to resolve this problem and restore genetic diversity to cultivated Metasequoia. Metasequoia has proved an easy tree to grow in temperate regions, and is now widely planted as an ornamental tree. Planted specimens have already reached 25-40 m in height and 1-1.3 m in diameter, despite being in cultivation for under 60 years. This rapid rate of growth has led to consideration for using the tree in forestry plantations. It has been discovered that Metasequoia will thrive in standing water, much like the baldcypress, and if left branched to the ground in full sun, will develop the large, contorted boles that have made it famous. Limbing at an early age will prohibit this formation later on.

1 Paleontology
2 See also
3 References
4 Further reading
5 External links

Paleontology

Metasequoia redwood fossils are known from many areas in the Northern Hemisphere; over 20 fossil species have been named (some are even identified as the genus Sequoia), but are now treated in just three species, M. foxii, M. milleri, and M. occidentalis (Farjon 2005). During the Paleocene-Eocene Thermal Maximum, extensive forests of Metasequoia occurred as far north as Axel Heiberg Island [1] (northern Canada) at around 80°N latitude. Large petrified trunks and stumps of the extinct Metasequoia occidentalis (sometimes identified as Sequoia occidentalis) also make up the major portion of Tertiary fossil plant material in the badlands of western North Dakota in the United States.

References

^ Gadek, P.A., Alpers, D.L., Heslewood, M.M., and Quinn, C.J. (2000). Relationships within Cupressaceae sensu lato: A combined morphological and molecular approach. American Journal of Botany, 87(7): 1044-1057.

Conifer Specialist Group (1998). Metasequoia glyptostroboides. 2006 IUCN Red List of Threatened Species. IUCN 2006. Retrieved on 06 May 2006. Listed as Critically Endangered (CR A1c, C2a v2.3)
Farjon, A. (2005). Monograph of Cupressaceae and Sciadopitys. Royal Botanic Gardens, Kew. ISBN 1-84246-068-4.
Hanks, D.A. Crescent Ridge Dawn Redwoods Preserve (2005). http://www.dawnredwood.org
Jahren, A. H. & Sternberg, L. S. L. (2003). Humidity estimate for the middle Eocene Arctic rain forest. Geology May 2003 pdf file
Metasequoia Glyptostroboides (TSN 505864). Integrated Taxonomic Information System. Accessed on September 25 2006.
Metasequoia stumps, Axel Heiberg Island (pdf file)
Williams C.J., LePage, B.A., Vann D.R., Tange, T., Ikeda, H., Ando, M., Kusakabe, T., Tsuzuki, T. and T. Sweda. (2003). Structure, allometry, and biomass of plantation Metasequoia glyptostroboides in Japan. Forest Ecology and Management, 180(103): 287-301. [2]
Williams C.J., Johnson A.H., LePage, B.A., Vann D.R. and T. Sweda. 2003. Reconstruction of Tertiary Metasequoia Forests II. Structure, Biomass and Productivity of Eocene Floodplain Forests in the Canadian Arctic. Paleobiology, 29(2): 271-292. [3]