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・ Equipollence (geometry)
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Equisetaceae
・ Equisetales
・ Equisetidae
・ Equisetopsida
・ Equisetopsida sensu lato
・ Equisetum
・ Equisetum arvense
・ Equisetum bogotense
・ Equisetum californicum
・ Equisetum debile
・ Equisetum diffusum
・ Equisetum fluviatile
・ Equisetum giganteum
・ Equisetum hyemale
・ Equisetum laevigatum


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Equisetaceae : ウィキペディア英語版
Equisetaceae

| image = Equisetum arvense 001.JPG
| image_caption = Field Horsetail ''(Equisetum arvense)''
| image_width = 240px
| regnum = Plantae
| divisio = Pteridophyta
| classis = Equisetopsida
| ordo = Equisetales
| familia = Equisetaceae
| familia_authority=
| subdivision_ranks = Genera
| subdivision =
''Equisetum''

†''Equisetites''
}}
Equisetaceae, sometimes called the horsetail family, is the only extant family of the order Equisetales, with one surviving genus, ''Equisetum'', which comprises about twenty species.
== Evolution and systematics ==
Equisetaceae is the only surviving family of the Equisetales, a group with many fossils of large tree-like plants that possessed ribbed stems similar to modern horsetails. ''Pseudobornia'' is the oldest known relative of ''Equisetum''; it grew in the late Devonian, about 375 million years ago and is assigned to its own order.
All living horsetails are placed in the genus ''Equisetum''. But there are some fossil species that are not assignable to the modern genus. ''Equisetites'' is a "wastebin taxon" uniting all sorts of large horsetails from the Mesozoic; it is almost certainly paraphyletic and would probably warrant being subsumed in ''Equisetum''. But while some of the species placed there are likely to be ancestral to the modern horsetails, there have been reports of secondary growth in other ''Equisetites'', and these probably represent a distinct and now-extinct horsetail lineage. ''Equicalastrobus'' is the name given to fossil horsetail strobili, which probably mostly or completely belong to the (sterile) plants placed in ''Equisetites''.〔 (2005): ''Equisetites aequecaliginosus'' sp. nov., ein Riesenschachtelhalm aus der spättriassischen Formation Santa Clara, Sonora, Mexiko (aequecaliginosus'' sp. nov., a tall horsetail from the Late Triassic Santa Clara Formation, Sonora, Mexico ). ''Revue de Paléobiologie'' 24(1): 331-364 (with English abstract ). (PDf fulltext )〕

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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