WordNet

shape or cut with a flat surface
the act of putting into tabular form; "the tabulation of the results"
information set out in tabular form (同)tabular matter

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〈事実・数字など〉‘を'表にする
表にすること,表の作成

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出典(authority):フリー百科事典『ウィキペディア（Wikipedia）』「2015/09/09 22:18:24」(JST)

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The tabulate corals, forming the order Tabulata, are an extinct form of coral. They are almost always colonial, forming colonies of individual hexagonal cells known as corallites defined by a skeleton of calcite, similar in appearance to a honeycomb. Adjacent cells are joined by small pores. Their distinguishing feature is their well-developed horizontal internal partitions (tabulae) within each cell, but reduced or absent vertical internal partitions (septae). They are usually smaller than rugose corals, but vary considerably in shape, from flat to conical to spherical.

Around 300 species have been described. Among the most common tabulate corals in the fossil record are Aulopora, Favosites, Halysites, Heliolites, Pleurodictyum, Sarcinula and Syringopora. Tabulate corals with massive skeletons often contain endobiotic symbionts, such as cornulitids and Chaetosalpinx.^[1]^[2]

Like rugose corals, they lived entirely during the Paleozoic, being found from the Ordovician to the Permian. With Stromatoporoidea and rugose corals, the tabulate corals are characteristic of the shallow waters of the Silurian and Devonian. Sea levels rose in the Devonian, and tabulate corals became much less common. They finally became extinct in the Permian–Triassic extinction event.

Gallery

Halysites sp. from the Silurian of Ohio. View of colony surface.
Etched section of an Ordovician tabulate coral
Aulopora from the Silica Shale (Middle Devonian) of northwestern Ohio. Image shows colony origin encrusting a brachiopod.
The coral Protaraea richmondensis on the brachiopod Rafinesquina ponderosa; Whitewater Formation, Indiana, Upper Ordovician.

References

^ Vinn, O.; Mõtus, M.-A. (2012). "Diverse early endobiotic coral symbiont assemblage from the Katian (Late Ordovician) of Baltica". Palaeogeography, Palaeoclimatology, Palaeoecology. 321–322: 137–141. doi:10.1016/j.palaeo.2012.01.028. Retrieved 2014-06-11.
^ Vinn, O.; Mõtus, M.-A. (2008). "The earliest endosymbiotic mineralized tubeworms from the Silurian of Podolia, Ukraine". Journal of Paleontology 82: 409–414. doi:10.1666/07-056.1. Retrieved 2014-06-11.

Invertebrate Fossils; Moore, Lalicker, & Fischer; McGraw-Hill 1952.
Treatise on Invertebrate Paleontology Part F, Coelenterata. Geological Society of America and Univ Kansas Press. R.C. Moore (ed).

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Japanese Journal

宮崎県祇園山層産シルル紀クサリサンゴの1新種

Niko Shuji,Adachi Tomio
Bulletin of the National Museum of Nature and Science. Series C, Geology & paleontology 40, 11-13, 2014-12
NAID 40020318733

Early Carboniferous tabulate corals from the Nagatophyllum satoi zone (middle Visean) of the Akiyoshi Limestone Group, Yamaguchi Prefecture

Niko Shuji,Haikawa Takehiko,Fujikawa Masayuki
秋吉台科学博物館報告 (49), 1-5,図版5p, 2014-03
NAID 40020118164

Devonian tabulate corals from pebbles in Mesozoic conglomerate, Kotaki, Niigata Prefecture, central Japan Part 1 : Favositina

Niko Shuji,Ibaraki Yousuke,Tazawa Jun-ichi
Science reports of Niigata University. (Geology) 29, 53-66, 2014-03
… A float block of Mesozoic conglomerate, probably derived from the Lower Jurassic Kuruma Group, containing Devonian tabulate corals was collected in the Kotaki area, Itoigawa, Niigata Prefecture, central Japan. …
NAID 120005428137

Related Pictures

★リンクテーブル★

リンク元	「作表」「tabulation」「表にする」

「作表」

Tabulata; Temporal range: 488–251.4 Ma PreЄ Є O S D C P T J K Pg N Ordovician–Permian
	Tabulate coral (a syringoporid); Boone Limestone (Lower Carboniferous) near Hiwasse, Arkansas. Scale bar is 2.0 cm.
Scientific classification
Kingdom:	Animalia
Phylum:	Cnidaria
Class:	Anthozoa
Subclass:	Zoantharia
Order:	Tabulata