| Ochrophytes Temporal range: Middle Proterozoic [1] | |
|---|---|
| | |
| Dense kelp forest with understory at Partridge Point near Dave's Caves, Cape Peninsula | |
| Scientific classification | |
| Domain: | Eukaryota |
| Clade: | Sar |
| Clade: | Stramenopiles |
| Clade: | Gyrista |
| Division: | Ochrophyta Cavalier-Smith 1986, emend. Cavalier-Smith & Chao 1996 [2] |
| Classes and possible taxa [3] [4] | |
| |
| Diversity | |
| 23,314 described species [5] >100,000 estimated species [6] | |
| Synonyms | |
Ochrophytes, also known as heterokontophytes or stramenochromes, are a phylum of algae. They are the photosynthetic stramenopiles, a group of eukaryotes, organisms with a cell nucleus, characterized by the presence of two unequal flagella, one of which has tripartite hairs called mastigonemes. In particular, they are characterized by photosynthetic organelles or plastids enclosed by four membranes, with membrane-bound compartments called thylakoids organized in piles of three, chlorophyll a and c as their photosynthetic pigments, and additional pigments such as β-carotene and xanthophylls. Ochrophytes are one of the most diverse lineages of eukaryotes, containing ecologically important algae such as brown algae and diatoms. They are classified either as phylum Ochrophyta, Heterokontophyta or as subphylum Ochrophytina within phylum Gyrista. Their plastids are of red algal origin.
Throughout history, different names have been used to describe photosynthetic stramenopiles. The more widely used name is the phylum —or division, in botanical nomenclature— Ochrophyta, [10] based on the golden alga Ochromonas . [11] This name was first coined by evolutionary biologist Thomas Cavalier-Smith in 1986 as Ochrista, [11] later renamed to Ochrophyta to comply with the recommendations of the International Code of Botanical Nomenclature. [12] [13] In 2017, the same author lowered it to a subphylum inside phylum Gyrista, and modified the name to Ochrophytina to match the -phytina suffix used for botanical subdivisions. [14] Despite this, Ochrophyta is preferred over Ochrophytina by the scientific community. [2]
The alternative name Heterokontophyta is more familiar among phycologists. [7] The origin of this name is the class Heterokontæ (from Greek hetero 'different'and kontos 'pole'), introduced by Finnish biologist Alexander Ferdinand Luther in 1899 to include yellow-green freshwater algae, [15] now part of Xanthophyceae and Raphidophyceae. This name referenced, among other traits, the two unequal flagella characteristic of all stramenopiles, also known as heterokonts. [16] : 229 Eventually it was expanded to include more algae and became the division Heterokontophyta, coined by Christiaan van den Hoek in 1978 [17] [a] and used to describe all photosynthetic stramenopiles. [16] : 229
Ochrophytes are eukaryotic organisms composed of cells that are either naked or covered by scales, lorica or a cell wall. They can be single-celled, colonial, coenocytic or multicellular. Some Phaeophyceae (brown algae, seaweeds) develop as large multicellular thalli with differentiated tissues. [7] All ochrophytes uniformly have tubular mitochondrial cristae. [18] This is a common trait shared with their relatives, heterotrophic stramenopiles, as well as other closely related groups such as Rhizaria, Telonemia and Alveolata. [19] [20] As primarily photosynthetic eukaryotes, they are considered algae, distinguished from other groups of algae by specific morphological and ultrastructural traits, such as their flagella, chloroplasts and pigments. [18]
As stramenopiles (=heterokonts), their swimming cells frequently display two markedly unequal flagella: an anterior flagellum ("tinsel") with straw-like hollow tripartite hairs called mastigonemes, and an immature posterior smooth flagellum ("whiplash") lacking these hairs. [21] [18] The ciliary transition zone of the flagellum generally has a transitional helix. [7]
The ochrophytes are mostly photosynthetic. As such, they may possess one or more photosynthetic plastids (chloroplasts) per cell. [22] Some groups contain species with leucoplasts, chloroplasts that have lost photosynthetic capacity and pigments but presumably continue to play a role in the synthesis of amino acids, lipids and heme groups. [18] Ochrophytes have a distinct plastid ultrastructure in comparison to other algal groups. [22] Their chloroplasts originate from an event of secondary endosymbiosis from a red alga, which lead to four [b] surrounding membranes: two inner membranes, corresponding to the primary plastid membranes; a third membrane, corresponding to the plasma membrane of the red alga; and an outermost layer, corresponding to the phagosome membrane. [25] This characteristic differentiates them from archaeplastid algae (glaucophytes, red algae and green algae), whose chloroplasts have only two membranes. [26] The two outer layers of ochrophyte plastids are continguous with the endoplasmic reticulum (ER), together composing the chloroplast endoplasmic reticulum (CER), [22] also known as the periplastidial endoplasmic reticulum (PER), which is often connected to the nuclear envelope. The tripartite flagellar hairs, characteristic of stramenopiles, are produced within either the PER or the nuclear envelope. [18]
The periplastid compartment (PC), between the second and third layers, is a separate region that in other algal groups (i.e. cryptomonads and chlorarachniophytes) contains a nucleomorph, the vestigial nucleus of the secondary endosymbiont; however, no nucleomorphs are known within the ochrophytes. Instead, other structures have been observed within the PC, similarly to those seen in haptophytes and chromerid algae: [22] "blob-like structures" where PC proteins are localized, and a vesicular network. [25] Within the CER, there is a prominent region of tight direct contacts between the periplastid membrane and the inner nuclear envelope, where lipid transfers might occur, and perhaps exchange of other molecules. [25]
Commonly, within the plastid stroma, three stacked thylakoids differentiate into the "girdle lamella", which runs around the periphery of the plastid, beneath the innermost membrane. [22] The remaining thylakoids are arranged in stacks of three. [18] In synchromophytes and aurearenophytes, a consortium of several plastids, each surrounded by two or three inner membranes respectively, is enveloped by a shared outer membrane. [22]
Ochrophyte chloroplasts contain chlorophylls a and c as photosynthetic pigments, in addition to fucoxanthin. [21] Chlorophyll a binds to thylakoids, while the c pigment is present in the stroma. [18] The most frequent accessory pigment in ochrophytes is the yellow β-carotene. The golden-brown or brown pigmentation in diatoms, brown algae, golden algae and others is conferred by the xanthophyll fucoxanthin. In the yellow-green or yellow-brown raphidophyceans, eustigmatophyceans and xanthophyceans, vaucheriaxanthin is dominant instead. These pigment combinations extend their photosynthetic ability beyond chlorophyll a alone. Additionally, xanthophylls protect the photosystems from high intensity light. [18]
Ochrophyte algae accumulate chrysolaminarin, a carbohydrate consisting of short chains of β-1,3-linked glucose molecules, as a storage product. [18] [27] It is stored in vesicles located within the cytoplasm, outside plastids, unlike other algae. [21] Cytoplasmic lipid droplets are also common. [18] They lack starch, which is the common storage product in green algae and plants. [7]
According to a 2024 survey, photosynthetic stramenopiles include 23,314 described species, with 490 species of uncertain position. [5] However, they may amount to more than 100,000 estimated species, of which the majority are diatoms. [6] They are divided into the following classes: [2] [23] [28]
Ochrophytes are capable of asexual reproduction by fragmentation, propagules, vegetative cell division, sporogenesis or zoosporogenesis. In addition, they are capable of sexual reproduction through gametes, by three different modes: isogamy, anisogamy or oogamy. [7]
Ochrophytes are present in nearly all environments. [27] Some classes are more common in marine habitats, while others are more frequent in freshwater or soil. [18] Among the ochrophyte lineages are the diatoms, the most abundant photosynthetic eukaryotes worldwide in marine habitats; multicellular seaweeds, such as brown algae (e.g., kelp) and golden algae; and an array of microscopic single-celled lineages that are also abundant, as evidenced by environmental sequencing. [22] Regarding nutrition, various ochrophytes are mixotrophic, usually through phagocytosis. [27]
Several classes of heterokont algae are exclusively known from marine habitats, such as Bolidophyceae, Pelagophyceae, Pinguiophyceae and Schizocladiophyceae. The brown algae (Phaeophyceae) are almost exclusively marine, with very few freshwater genera. [27]
Chrysophyceae, Phaeothamniophyceae and Xanthophyceae are predominantly freshwater classes. In lotic habitats (rivers, streams), golden algae (Chrysophyceae) and yellow-green algae (Xanthophyceae) are common and occasionally abundant. The golden algal genus Hydrurus , in particular, can be widespread in some drainage basins and is common in cold, clear, fast-flowing mountain streams, where it attaches to a firm substrate. Xanthophycean genera commonly found in rivers include Vaucheria , Tribonema and Bumilleria , either freely floating or attached to filamentous algae and plants. [41] Diatoms are more diverse, with more than 60 genera commonly found in rivers. Many river diatoms have developed different strategies to attach to the substrate to avoid being displaced by water currents. The most basic strategy is to produce extracellular polymeric substances, varied carbohydrate structures formed from the cell membrane. In faster-flowing waters, some diatoms (e.g., Cocconeis ) grow directly attached to the substrate through adhesive films. Others (e.g., Eunotia , Nitzschia ) grow stalks or colonial tubes capable of reaching higher into the water column to acquire more nutrients. [42] Brown algae (Phaeophyceae), although highly diversified, contain only seven species present in rivers. These lack any complex multicellular thalli, and instead exist as benthic filamentous forms that have evolved independently from marine ancestors. [43]
Two main lineages of photosynthetic stramenopiles include many toxic species. Within the class Raphidophyceae, strains of Heterosigma and Chattonella at high concentrations are responsible for fish mortality, although the nature and action of their toxins is not resolved. Freshwater Gonyostomum species are capable of mucilage secretion at high amounts detrimental to fish gills. Within the diatoms (Bacillariophyta), harmful effects can be due to physical damage or to toxin production. Centric diatoms like Chaetoceros live as colonial chains of cells with long spines (setae) that can clog fish gills, causing their death. Among diatoms, the only toxin producers have been found among pennate diatoms, almost entirely within the genus Pseudonitzschia . More than a dozen species of Pseudonitzschia are capable of producing a neurotoxin, domoic acid, the cause of amnesiac shellfish poisoning. [44]
The ochrophytes constitute a highly diverse clade within Stramenopila, a eukaryotic supergroup that also includes several heterotrophic lineages of protists such as oomycetes, hyphochytrids, labyrinthuleans, opalines and bicosoecids. [10] [45] [2] This lineage of stramenopiles originated from an event of secondary endosymbiosis where a red alga was transformed into the chloroplast of the common ancestor of ochrophytes. [45] [46] [14]
The total group of ochrophytes is estimated to have evolved between 874 and 543 million years ago (Ma) through molecular clock inference. However, the earliest fossil remains, assigned to the billion-year-old xanthophyte Palaeovaucheria , [1] suggest that ochrophytes had appeared by 1000 Ma. Other early putative representatives of photosynthetic stramenopiles are Jacutianema (750 Ma), Germinosphaera (750–700 Ma) and the brown alga Miaohephyton (600–550 Ma). Scales similar to modern chrysophyte scales, and valves resembling the modern centric diatom valves, have been found in 800–700 million-years-old sediments. [47]
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| Evolutionary relationships between all ochrophyte classes, based on a 2025 multiprotein phylogenetic analysis. [3] |
Relationships among many classes of ochrophytes remain unresolved, but three main clades (called SI, SII and SIII) are supported in most phylogenetic analyses. The SI lineage, containing the diverse and multicellular class Phaeophyceae, or brown algae, experienced an evolutionary radiation during the late Paleozoic (around 310 million years ago). The class Schizocladiophyceae is the sister lineage to brown algae, followed by a clade of closely related classes Xanthophyceae, Phaeosacciophyceae [28] and Chrysoparadoxophyceae. [23] This is in turn the sister lineage to a clade containing Aurearenophyceae and Phaeothamniophyceae, [45] which are sometimes treated as one class Aurophyceae. [14] The Raphidophyceae are the most basal within the SI. The SII lineage contains the golden algae or Chrysophyceae, as well as smaller classes Eustigmatophyceae, Pinguiophyceae, Synchromophyceae and Picophagea. Both clades, SI and SII, compose the Chrysista lineage. The remaining classes are grouped within the sister lineage Diatomista, equivalent to the SIII lineage: these are the diatoms or Diatomeae, and three closely related classes Bolidophyceae, Dictyochophyceae (including the silicoflagellates) and Pelagophyceae. [45] A new class of algae, Olisthodiscophyceae, was described in 2021 and recovered as part of the SII lineage. [34]
One group of heterotrophic heliozoan protists, Actinophryida, [48] is included in some classifications as the sister lineage to the raphidophytes, and both groups are treated as one class Raphidomonadea on the basis of 18S rDNA phylogenetic analyses. [4] However, a 2022 phylogenomic study placed one actinophryid, Actinophrys sol , as the probable sister group to ochrophytes. Although it lacks chloroplasts, plastidial genes have been found in the nuclear genome of this actinophryid, implying that its common ancestor with ochrophytes may have already begun domesticating plastids. [49] Later, a 2025 study recovered A. sol within the SII clade instead, implying that, much like the Picophagea, it evolved from ochrophytes that secondarily lost their chloroplasts. [3]
The first recorded stramenopile algae in history were the multicellular brown algae, such as kelp and other seaweeds. Their descriptions date back to early China (ca. 3000 BC), Japan (ca. 500 BC) and Greece (300 BC, such as Theophrastus). Knowledge of them likely predates recorded history, as they were potentially used by humans as a source for food, dyes, and medicine. [27] They likely played a role in the early dispersal of humans along seashores, [16] : 220 particularly from East Asia to the Americas, where brown algae may have formed a corridor rich in aquatic resources after deglaciation. This is known as the kelp highway hypothesis. [50] [51] The remaining stramenopile algae were not included in historical works, due to being microscopic. [52]
In the late 17th century, Antony van Leeuwenhoek became the first person to observe microbes, but he did not record microscopic stramenopiles. The first unmistakeable descriptions of diatoms belong to two illustrations published anonymously in England in 1703, 80 years before the first taxonomic description of a diatom. They are attributed to Charles King of Staffordshire. [53] [54]
The first formal description of any stramenopile was by Carl Linnaeus in his 1753 work Species Plantarum , for the brown alga Fucus . In the following years, single-celled chrysophytes and diatoms were described for the first time by Otto Friedrich Müller. [55] [56] These descriptions started a century-long era of exploration, during which brown algae were described as plants, while microscopic algae were treated as animals under the name of infusoria. [27] [16] : 220 Xanthophytes were first described in 1801 by Augustin Pyramus de Candolle, and raphidophytes were discovered by Karl Moriz Diesing in 1865. [16] : 228
Influential works were published around that time, such as the 1813 work by French naturalist Jean Vincent Félix Lamouroux with the use of pigment color to classify algae. [57] One of the most significant contributions was the 1838 publication by Christian Gottfried Ehrenberg, containing his observations of many stramenopiles under light microscopy. [58] [27] Still, these taxa remained separate from each other in the mind of taxonomists until the next period. [16] : 220
The 1882 work by M.J. Rostafinski [59] was the first to hypothesize an evolutionary link between the diatoms, golden algae, and brown algae. Several authors later developed this idea through various publications, such as Carl Correns, Georg Klebs, and Ernst Lemmermann, and phylogenetic relationships between very different algal groups were discussed. [27] This culminated in the 1900 phylogenetic study by Frederick Blackman, [16] : 221 who hypothesized that complex multicellular algae evolved from simple flagellated algae, and that this happened independently in green algae (giving rise to plants) and golden algae (giving rise to brown algae and diatoms). [60] In 1914, Adolf Pascher published a synthesis where he did not fully accept the evolutionary relationships between stramenopile algae. Pascher instead separated the Chrysophyta (including golden algae, xanthophytes and diatoms) and the Phaeophyta (brown algae alone).
During the following period, evolutionary discussions were mostly abandoned, because characters observed under light microscopy were insufficient to resolve evolutionary relationships. But many species were described.
During the 20th century, evolutionary and phylogenetic discussions began including heterokont algae. Transmission electron microscopy and molecular phylogenetic analysis led to the description of many new groups and several classes well into the 21st century. The sequencing of the first ochrophyte genome, belonging to Thalassiosira pseudonana , began in 2002. [27]
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