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Algae have conventionally been regarded as simple plants within the study of botany. All are Eukaryota, though Chromophyta have Bacterial (see Blue-green algae) characteristics and some authorities consider them all to be Protists, however this view is now considered to be outdated.[1] They may still be included in the algae as plants. Some authors often include the blue-green algae (Cyanophyta) but note that they are not eukaryote. Algae do not represent a single evolutionary direction or line but a level of organization that may have developed several times in the early history of life on Earth.

The protists are traditionally considered more animal-like (see Protozoa).

The prokaryotic forms, referred to as blue-green algae are only half-algae with a mixture of bacterial characteristics. However, they are quite distant from the bacteria and are referred to by some as Cyanochloronta. All other forms belong as true eukaryota algae within the study of Botany, they have a nucleus enclosed within a membrane.[2] The protoctists are defined by some as eukaryotic microorganisms with the exception of animals and plants and including fungi and algae, slime moulds and other obscure eukaryotes.[3] There is still some disagreement on some of these matters.

Algae range from single-cell organisms to multicellular organisms, some with fairly complex differentiated form and (if marine) called seaweeds. All lack leaves, roots, flowers, seeds and other organ structures that characterize higher plants (vascular plants). They are distinguished from other protozoa in that they are photoautotrophic although this is not a hard or vast distinction as some groups contain members that are mixotrophic, deriving energy both from photosynthesis and uptake of organic carbon either by osmotrophy, myzotrophy, or phagotrophy. Some unicellular species rely entirely on external energy sources and have reduced or lost their photosynthetic apparatus.

All algae have photosynthetic machinery ultimately derived from the cyanobacteria, and so produce oxygen as a byproduct of photosynthesis, unlike non-cyanobacterial photosynthetic bacteria. It is estimated that algae produce about 73 to 87 percent of the net global production of oxygen[4] - which is available to humans and other animals for respiration.


Algae are usually found in damp places or bodies of water and thus are common in terrestrial as well as aquatic environments. However, terrestrial algae are usually rather inconspicuous and far more common in moist, tropical regions than dry ones, because algae lack vascular tissues and other adaptations to live on land. Algae can, however, endure dryness and other conditions in symbiosis with a fungus as lichen.

The various sorts of algae play significant roles in aquatic ecology. Microscopic forms that live suspended in the water column — called phytoplankton — provide the food base for most marine food chains. In very high densities (so-called algal blooms) these algae may discolor the water and outcompete or poison other life forms. Seaweeds grow mostly in shallow marine waters, however some have been recorded to a depth of 300 m.[2]Some are used as human food or harvested for useful substances such as agar or fertilizer.

Study of algae

The study of marine and freshwater algae is called phycology or algology.

The US Algal Collection is represented by almost 300,000 accessioned and inventoried herbarium specimens.[1]


The lineage of algae according to Thomas Cavallier-Smith. The three supergroups Archaeplastida, Chromalveolata and Cabozoa of eukaryotic algae are denoted to reflect the table below. Endosymbiotic events are noted by dotted lines.

Prokaryotic algae

Cyanobacteria have been included among the algae, referred to as the cyanophytes or Blue-green algae, (the term "algae" refers to any aquatic organisms capable of photosynthesis)[5] though some recent treatises on algae specifically exclude them. Cyanobacteria are some of the oldest organisms to appear in the fossil record dating back to the Precambrian, possibly as far as about 3.5 billion years.[6] Ancient cyanobacteria likely produced much of the oxygen in the Earth's atmosphere.

Cyanobacteria can be unicellular, colonial, or filamentous. They have a prokaryotic cell structure typical of bacteria and conduct photosynthesis on specialized cytoplasmic membranes called thylakoid membranes, rather than in organelles. Some filamentous blue-green algae have specialized cells, termed heterocysts, in which nitrogen fixation occurs.[7] the perfect prokaryotic cell consist of miscalgnous sheath covering cellwall that consistof pectinic substance and sachride while the cellwall consist of 4 layer outer and inner and middle layer while the fourth layer is attached to plasma membrane and the protoplast consist of 2 part peripheral coloured partknown by chromatoplasm which contain the pigments in case of algae and contain photothynsis producte.g in cyanobacteria it contain chlorophylla, b-caroteinand c-phycocyanin and c-phycoerthyrin

Eukaryotic algae

All other algae are eukaryotes and conduct photosynthesis within membrane-bound structures (organelles) called chloroplasts. Chloroplasts contain DNA and are similar in structure to cyanobacteria, presumably representing reduced cyanobacterial endosymbionts. The exact nature of the chloroplasts is different among the different lines of algae, reflecting different endosymbiotic events. The table below lists the three major groups of eukaryotic algae and their lineage relationship is shown in the figure on the left. Note many of these groups contain some members that are no longer photosynthetic. Some retain plastids, but not chloroplasts, while others have lost them entirely.

Supergroup affiliation Members Endosymbiont Summary
Cyanobacterium These algae have primary chloroplasts, i.e. the chloroplasts are surrounded by two membranes and probably developed through a single endosymbiosis. The chloroplasts of red algae have a more or less typical cyanobacterial pigmentation, while those of the green alga have chloroplasts with chlorophyll a and b, the latter found in some cyanobacteria and not most. Higher plants are pigmented similarly to green algae and probably developed from them.
Excavata and Rhizaria
  • Chlorarachniophytes
  • Euglenids
Green alga

These groups have green chloroplasts containing chlorophyll b. Their chloroplasts are surrounded by three and four membranes, respectively, and were probably retained from an ingested green alga.

Chlorarachniophytes, which belong to the phylum Cercozoa, contain a small nucleomorph, which is a relict of the alga's nucleus.

Euglenids, which belong to the phylum Euglenozoa, have chloroplasts with only three membranes. It has been suggested that the endosymbiotic green algae were acquired through myzocytosis rather than phagocytosis.

Chromista and Alveolata
Red alga

These groups have chloroplasts containing chlorophylls a and c. The latter chlorophyll type is not known from any prokaryotes or primary chloroplasts, but genetic similarities with the red algae suggest a relationship there.

In the first three of these groups (Chromista), the chloroplast has four membranes, retaining a nucleomorph in cryptomonads, and they likely share a common pigmented ancestor.

The typical dinoflagellate chloroplast has three membranes, but there is considerable diversity in chloroplasts among the group, as some members have acquired theirs from different sources. The Apicomplexa, a group of closely related parasites, also have plastids called apicoplasts. Apicoplasts are not photosynthetic but appear to have a common origin with dinoflagellates chloroplasts.

It was W.H.Harvey (1811 — 1866) who first divided the algae into four divisions based on their pigmentation. This is the first use of a biochemical criterion in plant systematics. Harvey's four divisions were: red algae (Rhodophyta), brown algae (Heteromontophyta), green algae (Chlorophyta) and Diatomaceae (Dixon, 1973 p.232).

Forms of algae

Most of the simpler algae are unicellular flagellates or amoeboids, but colonial and non-motile forms have developed independently among several of the groups. Some of the more common organizational levels, more than one of which may occur in the life cycle of a species, are

  • Colonial: small, regular groups of motile cells
  • Capsoid: individual non-motile cells embedded in mucilage
  • Coccoid: individual non-motile cells with cell walls
  • Palmelloid: non-motile cells embedded in mucilage
  • Filamentous: a string of non-motile cells connected together, sometimes branching
  • Parenchymatous: cells forming a thallus with partial differentiation of tissues

In three lines even higher levels of organization have been reached, imma hit with full tissue differentiation. These are the brown algae [2]—some of which may reach 50 m in length (kelps)[8]—the red algae [3], and the green algae [4]. The most complex forms are found among the green algae (see Charales and Charophyta), in a lineage that eventually led to the higher land plants. The point where these non-algal plants begin and algae stop is usually taken to be the presence of reproductive organs with protective cell layers, a characteristic not found in the other alga groups.

The first plants on earth were algae and these still thrive in a range of aquatic habitats today. The land plants evolved from the algae, more specifically green algae. Some 400 million years ago freshwater, green, filamentous algae invaded the land. These probably had an isomorphic alternation of generations and were probably heterotrichous. Fossils of isolated land plant spores suggest land plants may have been around as long as 475 million years ago.

Fresh-water algae

Algae and symbioses

Some species of algae form symbiotic relationships with other organisms. In these symbioses, the algae supply photosynthates (organic substances) to the host organism providing protection to the algal cells. The host organism derives some or all of its energy requirements from the algae. Examples include

  • lichens: a fungus is the host, usually with a green alga or a cyanobacterium as its symbiont. Both fungal and algal species found in lichens are capable of living independently, although habitat requirements may be greatly different from those of the lichen pair.
  • corals: algae known as zooxanthellae are symbionts with corals. Notable amongst these is the dinoflagellate Symbiodinium, found in many hard corals. The loss of Symbiodinium, or other zooxanthellae, from the host is known as coral bleaching.
  • sponges: green algae live close to the surface of some sponges, for example, breadcrumb sponge (Halichondria panicea). The alga is thus protected from predators; the sponge is provided with oxygen and sugars which can account for 50 to 80% of sponge growth in some species.[9]


Rhodophyta, Chlorophyta and Heterokontophyta, the three main algal Phyla, have life-cycles which show tremendous variation with considerable complexity. In general there is an asexual phase where the seaweed's cells are diploid, a sexual phase where the cells are haploid followed by fusion of the male and female gametes. Asexual reproduction is advantageous in that it permits efficient population increases, but less variation is possible. Sexual reproduction allows more variation but is more costly because of the waste of gametes that fail to mate, among other things. Often there is no strict alternation between the sporophyte and gametophyte phases and also because there is often an asexual phase, which could include the fragmentation of the thallus.[8][10][5]

See also


Numbers and distribution

In the British Isles the UK Biodiversity Steering Group Report estimated there to be 20,000 algal species in the UK, freshwater and marine, about 650 of these are seaweeds. Another checklist of freshwater algae reported only about 5000 species. It seems therefore that the 20,000 is an overestimate or an error (John, 2002 p.1).[11]

World-wide it is thought that there are over 5,000 species of red algae, 1,500 — 2,000 of brown algae and 8,000 of green algae. In Australia it is estimated that there are over 1,300 species of red algae, 350 species of brown algae and approximately 2,000 species of green algae totalling 3,650 species of algae in Australia.[12]

Around 400 species appear to be an average figure for the coastline of South African west coast.[13]

669 marine species have been described from California (U.S.A.).[14]

642 entities are listed in the check-list of Britain and Ireland (Hardy and Guiry, 2006).[15]


No publication has been found which attempts to discuss the general distribution of algae in the seas world-wide. However, notes and comments have been made by some authors. The floristic discontinuities may appear to determined by geographical features such as Antarctica, long distances of ocean or general land masses. However, the distances between Norway, the Faroes and Iceland do not show great changes in distribution.[2]

There has been dispersal in some species by ships, water currents and the like, further some algae drifting algae can quickly become entangled and easily drift.[16] Two red species have been introduced from the Pacific to Europe and the Mediterranean: Bonnemaisonia hamifera Hariot and Asparagopsis armata Harvey,[17] A. armata is a native of Australia.[2][6]Colpomenia peregrina is a native of the Pacific but has also invaded Europe

Britain and Ireland

  • Hardy, F.G. and Guiry, M.D. 2006. A Check-list and Atlas of the Seaweeds of Britain and Ireland. British Phycological Society, London. ISBN 3 906166 35 X

Northumberland and Durham (England)

  • Hardy, F.G. and Aspinall, R.J. 1988. An Atlas of the Seaweeds of Northumberland and Durham. Northumberland Biological Records Centre. The Hancock Museum. The University Newcastle upon Tyne. Special publication: 3. ISBN 0 9509680 5 6

Northern Ireland

  • Morton, O. 1994. Marine Algae of Northern Ireland. Ulster Museum, Belfast. ISBN 0 900761 28 8

Ireland: County Donegal

  • Morton, O. The marine macroalgae of County Donegal, Ireland. Bull. Ir. biogeog. Soc. 27:3 - 164.

Isle of Man

  • Knight, M. and Park, M.W. 1931. Manx algae. An algal survey of the south end of the Isle of Man. L.M.B.C. Mem. Typ. Br. Mar. Pl. 390: 1 - 155.


  • Kjellman, F.R. 1883. The algae of the Arctic Sea. K. sevenka. VetenskAkad. Handl. 20: 1 - 350.


  • Lund, S. 1959. The Marine Algae of East Greenland. I. Taxonomical part. Meddr. Grønland 156: 1 - 247.


  • Borgesen, F. 1903. Marine Algae, pp.339 - 532. In, Warming, E. (Ed.), Botany of the Faröes Based Upon Danish Investigations. Part II. Copenhagen. [reprint 1970]

Atlantic(east coast)/Europe

  • Cabioc'h,J., Floc'h,J-Y., Le Toquin, A., Boudouresque, C-F., Meinesz, A. and Verlaque, M. 1992. Guide des algues des mers d'Europe. Delachaux et Niestlé, Switzerland.
  • Gayral, P. 1958 Algues de la Côte Atlantique Marocaine. Rabat.
  • Gayral, P. 1966. Algues des Côtes Françaises. Paris.

Canary Islands.

  • Borgesen,F. 1925. Marine algae from the Canary Islands, especially from Tenerife and Gran Canaria. I. Chlorophyceae. Biol. Meddr 5: 1 - 113.
  • Borgesen,F. 1926. Marine algae from the Canary Islands especially from Tenerife and Gran Canaria. II. Phaeophyceae. Biol. Meddr 6: 1 - 112.
  • Borgesen,F. 1927. Marine algae from the Canary Islands. III. Rhodophyceae. Part I, Bangiales and Nemalionales. Biol. Meddr 6: 1 - 97.
  • Borgesen,F. 1929. Marine algae from the Canary Islands. III Rhodophyceae. Part II. Cryptonemiales, Gigartinales and Rhodymeniales. Biol. Meddr 8: 1 - 97.
  • Borgesen,F. 1930. Marine algae from the Canary Islands. III Rhodophyceae. Part II. Cryptonemiales, Gigartinales and Rhodymeniales. Biol. Meddr 9: 1 - 159.

North America

  • Taylor, W.R. 1957. Marine Algae of the Northeastern Coast of North America. University of Michigan Press, Ann Arbor.
  • Abbott, I.A. and Hollenberg, G.J. 1976. Marine Algae of Californa anne

South Africa

  • Stegenga, H. Bolton, J.J. and Anderson, R.J. 1997. Seaweeds of the South African West Coast. Bolus Herbarium Number 18, Publication jointly financed by the Fourcade Bequest and the Research Committee of the University of Cape Town and the Foundation for Research Development.


  • Huisman, J.M. 2000. Marine Plants of Australia. University of Western Australia Press, Nedlands, Western Australia 6907.

New Zealand

  • Lindauer, V.W., Chapman, V.J. and Aiken, M. 1961. The Marine Algae of New Zealand. Part II. Phaeophyta. Nova Hedwigia 3: 129 - 350.
  • Chapman, V.J. 1969. The Marine Algae of New Zealand. Part III issues 1. Lehre: J.Cramer, 1 - 113.
  • Chapman, V.J. and Dromgoole, F.I. 1970. The Marine Algae of New Zealand. Part III issues 2. Lehre: J.Cramer, 115 - 154.
  • Chapman, V.J. and Parkinson, P.G. 1974 The Marine Algae of New Zealand. Part III issues 3. Lehre: J.Cramer,155 - 278.
  • Chapman, V.J. 1979 The Marine Algae of New Zealand. Part III issues 4. Lehre: J.Cramer, 279 - 420.

Uses of algae

Seaweed is used as a fertilizer


For centuries seaweed has been used as a fertilizer; Orwell writing in the 16th Century referring to drift weed in South Wales: "This kind of ore they often gather and lay in heaps where it heats and rots, and will have a strong and loathsome smell; when being so rotten they cast it on the land, as they do their muck, and thereof springeth good corn, especially barley" and "After spring tides or great rigs of the sea, they fetch it in sacks on horse brackets, and carry the same three, four, or five miles, and cast it on the lande, which doth very much better the ground for corn and grass" (Chapman p.35).[18]

Algae are used by humans in many ways. They are used as fertilizers, soil conditioners and are a source of livestock feed.[8] Because many species are aquatic and microscopic, they are cultured in clear tanks or ponds and either harvested or used to treat effluents pumped through the ponds. Algaculture on a large scale is an important type of aquaculture in some places.

Maerl is commonly used as a soil conditioner, it is dredged from the sea floor and crushed to form a powder.[8] It is still harvested around the coasts of Brittany in France and off Falmouth, Cornwall (also extensively in western Ireland) and is a popular fertilizer in these days of organic gardening investigated Falmouth maerl and found that L. corallioides predominated down to 6 m and P. calcareum from 6-10 m (Blunden et al., 1981).[19][20]

Chemical analysis of maerl showed that it contained 32.1% CaCO3 and 3.1% MgCO3 (dry weight).

Energy source

  • Algae can be used to make biodiesel (see algaculture), and by some estimates can produce vastly superior amounts of oil, compared to terrestrial crops grown for the same purpose.
  • Algae can be grown to produce hydrogen. In 1939 a German researcher named Hans Gaffron, while working at the University of Chicago, observed that the algae he was studying, Chlamydomonas reinhardtii (a green-alga), would sometimes switch from the production of oxygen to the production of hydrogen.[7] Gaffron never discovered the cause for this change and for many years other scientists failed to repeat his findings. In the late 1990s professor Anastasios Melis, a researcher at the University of California at Berkeley, discovered that if the algae culture medium is deprived of sulfur it will switch from the production of oxygen (normal photosynthesis), to the production of hydrogen. He found that the enzyme responsible for this reaction is hydrogenase, but that the hydrogenase lost this function in the presence of oxygen. Melis found that depleting the amount of sulfur available to the algae interrupted its internal oxygen flow, allowing the hydrogenase an environment in which it can react, causing the algae to produce hydrogen. [8] Chlamydomonas moeweesi is also a good strain for the production of hydrogen.
  • Algae can be grown to produce biomass, which can be burned to produce heat and electricity. [9]

Pollution control

  • Algae are used in wastewater treatment facilities, reducing the need for greater amounts of toxic chemicals than are already used.
  • Algae can be used to capture fertilizers in runoff from farms. When subsequently harvested, the enriched algae itself can be used as fertilizer.
  • Algae Bioreactors are used by some powerplants to reduce CO2 emissions. [10] The CO2 can be pumped into a pond, or some kind of tank, on which the algae feed. Alternatively, the bioreactor can be installed directly on top of a smokestack. This technology has been pioneered by Massachusetts-based GreenFuelTechnologies.[11]

Stabilizing substances

Chondrus crispus, (probably confused with Mastocarpus stellatus, common name: Irish moss), is also used as "carrageen". The name carrageenan comes from the Irish Gaelic for Chondrus crispus. It is an excellent stabiliser in milk products - it reacts with the milk protein caesin, other products include: petfoods, toothpaste, ice-creams and lotions etc.[13][21] Alginates in creams and lotions are absorbable through the skin.[22]


Seaweeds are an important source of food, especially in Asia; They are excellent sources of many vitamins including: A, B1, B2, B6, niacin and C. They are rich in iodine, potassium, iron, magnesium and calcium.[23]

Algae is commercially cultivated as a nutritional supplement. One of the most popular microalgal species is Spirulina (Arthrospira platensis), which is a Cyanobacteria (known as blue-green algae), and has been hailed by some as a superfood.[12] Other algal species cultivated for their nutritional value include; Chlorella (a green algae), and Dunaliella (Dunaliella salina), which is high in beta-carotene and is used in vitamin C supplements.

In China at least 70 species of algae are eaten as is the Chinese "vegetable" known as fat choy (which is actually a cyanobacterium). Roughly 20 species of algae are used in everyday cooking in Japan.[23]

Certain species are edible; the best known, especially in Ireland is Palmaria palmata (Linnaeus) O. Kuntze (Rhodymenia palmata (Linnaeus) Kuntze, common name:dulse).[13] This is a red alga which is dried and may be bought in the shops in Ireland. It is eaten raw, fresh or dried, or cooked like spinach. Similarly, Durvillaea Antarctica [14] is eaten in Chile, common name: cochayuyo. [15]

Porphyra (common name: purple laver), is also collected and used in a variety of ways (e.g. "laver bread" in the British Isles). In Ireland it is collected and made into a jelly by stewing or boiling. Preparation also involves frying with fat or converting to a pinkish jelly by heating the fronds in a saucepan with a little water and beating with a fork. It is also collected and used by people parts of Asia, specifically China and Japan as nori and along most of the coast from California to British Columbia. The Hawaiians and the Maoris of New Zealand also use it.

One particular use is in "instant" puddings, sauces and creams. Ulva lactuca (common name: sea lettuce), is used locally in Scotland where it is added to soups or used in salads. Alaria esculenta (common name: badderlocks or dabberlocks), is used either fresh or cooked, in Greenland, Iceland, Scotland and Ireland.

The oil from some algae have high levels of unsaturated fatty acids. Arachidonic acid (a polyunsaturated fatty acid), is very high in Parietochloris incisa, (a green alga) where it reaches up to 47% of the triglyceride pool (Bigogno C et al. Phytochemistry 2002, 60, 497). [16] [17]

Other uses

There are also commercial uses of algae as agar.[21]

The natural pigments produced by algae can be used as an alternative to chemical dyes and coloring agents.[18] Many of the paper products used today are not recyclable because of the chemical inks that they use, paper recyclers have found that inks made from algae are much easier to break down. There is also much interest in the food industry into replacing the coloring agents that are currently used with coloring derived from algal pigments. In Israel, a species of green algae is grown in water tanks, then exposed to direct sunlight and heat which causes it to become bright red in color. It is then harvested and used as a natural pigment for foods such as Salmon. [19]


Between 100,000 and 170,000 wet tons of Macrocystis are harvested annually in California for alginate extraction and abalone feed.[20] [21]

Further references to the uses

  • Guiry, M.D. and Blunden, G. (Eds) 1991. Seaweed Resources in Europe: Uses and Potential. John Wiley & Sons. ISBN 0-471-92947-6
  • Mumford, T.F. and Miura, A. 1988. 4. Porphyra as food: cultivation and economics. p.87 — 117. In Lembi, C.A. and Waaland, J.R. (Ed.) Algae and Human Affairs. 1988. Cambridge University Press. ISBN 0 521 32115 8

History of Phycology

Collecting and preserving specimens

Seaweed specimens can be collected and preserved for research. Such preserved specimens will keep for two or three hundred years. Those of Carl von Linné (1707 — 1778) are still available for reference, and are used. Specimens may be collected from the shore; those below low tide must be collected by diving or dredging. The whole algal specimen should be collected, that is the holdfast, stipe and lamina. Specimens of algae reproducing will be the more useful for identification and research. When collected the details of the location and site should be noted. They can then be preserved pressed on paper or in a preserving liquid such as alcohol or solution of 5 per cent formalin/seawater. However, formalin is reported to be carcinogenic.[12]


Biological Exposure Scale

The ecology of the shores of the British Isles, including a discussion of the different shores from sheltered to exposed along with an exposure scale, is given by Lewis (1964).[24] An exposure scale of five stages is given:- Very Exposed Shores; Exposed Shores; Semi-exposed Shores; Sheltered Shores and Very Sheltered Shores. Factors indicating the differences between these exposure scales are detailed. Very Exposed Shores have a wide Verrucaria zone entirely above the upper tide level, a Porphyra zone above the barnacle level and Lichina pygmaea is locally abundant. The eulittoral zone is dominated by barnacles and limpets with a coralline belt in the very low littoral along with other Rhodophyta and Alaria in the upper sublittoral. Exposed shores show a Verrucaria belt mainly above the high tide, with Porphyra and Lichina pygmaea. The mid shore is dominated by barnacles, limpets and some Fucus. Some Rhodophyta. Himanthalia and some Rhodophyta such as Mastocarpus and Corallina are found in the low littorral with Himanthalia, Alaria and Laminaria digitata dominant in the upper sublittoral. The semi-exposed shores show a Verrucaria belt just above high tide with clear Pelvetia in the upper-littoral and Fucus serratus in the lower-littoral. Limpets, barnacles and short Fucus vesiculosus midshore. Fucus serratus with Rhodophyta, (Laurencia, Mastocarpus, Rhodymenia and Lomentaria). Laminaria and Saccorhiza polyschides and small algae common in the sublittoral. The sheltered shores show a narrow Verrucaria zone at high water and a full sequence of fucoids: Pelvetia, Fucus spiralis, Fucus vesiculosus, Fucus serratus Ascophyllum nodosum. Laminaria digitata is dominant the upper sublittoral. The very sheltered shores show a very narrow zone of Verrucaria, the dominance of the littoral by a full sequence of the fucoids and Ascophyllum covering the rocks. Laminaria saccharina, Halidrys, Chondrus and or Furcellaria.[24]

Common names

Chorda filum Sea lace[25]

Colpomena peregrina Oyster thief[25]

Laminaria Orwaeed[25]

Laminaria digitata Tangle[25]

Laminaria hyperborea Curvie[25]

Laminaria saccharina Sea belt[25]

Ulva lactuca Sea lettuce[25]


Atractophora hypnoides P.L.Crouan and H.M.Crouan (red algae)

Ascophyllum nodosum

Charales (green algae)



Ulva lactuca




Mastocarpus stellatus

Pelvetia canaliculata

Palmaria palmata


Postelsia palmaeformis

See also


Cited references

  1. Allaby, M ed. 1992. The Concise Dictionary of Botany. Oxford University Press, Oxford
  2. 2.0 2.1 2.2 2.3 Round, F.E. 1981. The Ecology of Algae. Cambridge University Press, London. ISBN 0 521 22583 3
  3. Margulis, L., Corliss, J.O., Melkonian,M. and Chapman, D.J. 1990. Handbook of Protoctista. Jones and Bartlett, Boston ISBN 0 86720 052 9
  6. Schopf, JW, and Packer, BM, Science, 400 b.c.,. 237, 70
  8. 8.0 8.1 8.2 8.3 Thomas, D.N. 2002 Seaweeds. The Natural History Museum, London. ISBN 0 565 09175 1
  10. Lobban, C.S. and Harrison, P.J. 1997. Seaweed Ecology and Physiology. Cambridge Uiversity Press. ISBN 0-521-40897-00
  11. John, D.M., Whitton, B.A. and Brook, A.J. 2002. The Freshwater Algae Flora of the British Isles. Cambridge University Press, Cambridge. ISBN 0 521 77051 3
  12. 12.0 12.1 Huisman, J.M. 2000. Marine Plants of Australia. University of Western Australian Press, Australian Biological Resources Study. ISBN 1 876268 33 6
  13. 13.0 13.1 Stegenga, H., Bolton, J.J. and Anderson, R.J. 1997. In Hall, A.V. (Ed.) Seaweeds of the South African West coast. Bolus Herbarim No. 18. ISBN 0-7992-1793-X
  14. Abbott, I.A. and Hollenberg, G.J. 1976. Marine Algae of California. Stanford University Press, California. ISBN 0-8047-0867-3
  15. Hardy, F.G. and Guiry, M.D. 2006. A Check-list and Atlas of the Seaweeds of Britain and Ireland. Britiah Phycological Society, London. ISBN 3-906166-35-X
  16. Kain, J.M. and Noron, T.A. 1990. Marine ecology. p.397. in Cole, K.M. and Sheath, R.G. 1990. Biology of Red Algae. Cambridge University Press. ISBN 0 521 343101 1
  17. Guiry, M.D. and Garbary, D.J.. A Geographical and Taxonomic Guide to European Seaweeds of Economic Importance. in Seaweeds Resources In Europe: Uses and Potential. ed. Guiry, M.D. and Blunden, G. 1991. John Wiley and Sons. ISBN 0 471 92947 6
  18. Chapman, V.J. 1950. Seaweeds and their Uses. Methuen & Co. Ltd., London
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External links

ar:أشنيات bg:Водорасли ca:Alga cs:Řasy da:Alge de:Alge et:Vetikad eo:Algo gl:Alga ko:조류 (수생 생물) id:Ganggang it:Alga he:אצות lv:Aļģes lt:Dumbliai hu:Alga mk:Алги nl:Algen no:Alge nn:Alge qu:Laqu simple:Algae sl:Alge sr:Алге sh:Alge fi:Levä sv:Alg ta:பாசிகள் th:สาหร่าย uk:Водорості ur:طحالب

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