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The red algae, or Rhodophyta ( or ; from Ancient Greek: ῥόδον ''rhodon'', "rose" and φυτόν ''phyton'', "plant"), are one of the oldest groups of eukaryotic algae, and also one of the largest, with about 5,000–6,000 species of mostly multicellular, marine algae, including many notable seaweeds. Other references indicate as many as 10,000 species; more detailed counts indicate about 4,000 in about 600 genera (3,738 marine species in 546 genera in 10 orders, plus the unclassifiable; and 164 freshwater species in 30 genera in eight orders). The red algae form a distinct group characterized by having eukaryotic cells without flagella and centrioles, chloroplasts that lack external endoplasmic reticulum, contain unstacked thylakoids〔 and use phycobiliproteins as accessory pigments (giving them their red color). They store floridean starch, a type of starch that consists of highly-branched amylopectin without amylose, as food reserves outside their plastids. Most red algae are also multicellular, macroscopic, marine, and use sexual reproduction to reproduce. They have alternation of generations and may have three generations rather than two.〔http://autocww.colorado.edu/~toldy2/E64ContentFiles/AlgaeAndFungi/Algae.html〕 The coralline algae, which secrete calcium carbonate and play a major role in building coral reefs, belong here. Red algae such as dulse ''(Palmaria palmata)'' and laver (nori/gim) are a traditional part of European and Asian cuisines and are used to make other products such as agar, carrageenans and other food additives. ==Habitat== Most rhodophytes are marine, although freshwater species are found; these generally prefer clean, running water, but with some exceptions. ==Fossil record== One of the oldest fossils identified as a red alga is also the oldest fossil eukaryote that belongs to a specific modern taxon. ''Bangiomorpha pubescens'', a multicellular fossil from arctic Canada, strongly resembles the modern red alga ''Bangia'' despite occurring in rocks dating to 1.2 billion years ago. Red algae are important builders of limestone reefs. The earliest such coralline algae, the solenopores, are known from the Cambrian period. Other algae of different origins filled a similar role in the late Paleozoic, and in more recent reefs. Calcite crusts, which have been interpreted as the remains of coralline red algae, date to the terminal Proterozoic. Thallophytes resembling coralline red algae are known from the late Proterozoic Doushantuo formation. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「red algae」の詳細全文を読む スポンサード リンク
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