Description of Phaeodarea

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Circumscription: A group of marine radiolaria (protists with axopodia, skeletons, and no flagella in the trophic state). Most have a skeleton of amorphous silica with associated organic matter, cytoplasm separated into an inner area by a thick capsule, and an inner layer that is further divided by a cape of vesicles-the cape having three openings: an apical astropyle that seems to be associated with the formation of feeding pseudopodia and two parapyles from which axonemal microtubules arise. Contain aggregates of waste material: the phaeodium. Life cycle may be complex, and flagellated distributive stages are produced. Ultrastructural identity: Little studied, mitochondria probably tubulocristate. Synapomorphy: Radiolaria with central capsule with three openings: an apical astropyle and two parapyles.
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Radiolaria

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Part of a series onPlanktonPlankton collage.jpg

The Radiolaria, also called Radiozoa, are protozoa of diameter 0.1–0.2 mm that produce intricate mineral skeletons, typically with a central capsule dividing the cell into the inner and outer portions of endoplasm and ectoplasm. The elaborate mineral skeleton is usually made of silica.[1] They are found as zooplankton throughout the global ocean. As zooplankton, radiolarians are primarily heterotrophic, but many have photosynthetic endosymbionts and are, therefore, considered mixotrophs. The skeletal remains of some types of radiolarians make up a large part of the cover of the ocean floor as siliceous ooze. Due to their rapid change as species and intricate skeletons, radiolarians represent an important diagnostic fossil found from the Cambrian onwards.

Description

Radiolarians have many needle-like pseudopods supported by bundles of microtubules, which aid in the radiolarian's buoyancy. The cell nucleus and most other organelles are in the endoplasm, while the ectoplasm is filled with frothy vacuoles and lipid droplets, keeping them buoyant. The radiolarian can often contain symbiotic algae, especially zooxanthellae, which provide most of the cell's energy. Some of this organization is found among the heliozoa, but those lack central capsules and only produce simple scales and spines.

Some radiolarians are known for their resemblance to regular polyhedra, such as the icosahedron-shaped Circogonia icosahedra pictured.

Taxonomy

The radiolarians belong to the supergroup Rhizaria together with (amoeboid or flagellate) Cercozoa and (shelled amoeboid) Foraminifera.[2] Traditionally the radiolarians have been divided into four groups—Acantharea, Nassellaria, Spumellaria and Phaeodarea. Phaeodaria is however now considered to be a Cercozoan.[3][4] Nassellaria and Spumellaria both produce siliceous skeletons and were therefore grouped together in the group Polycystina. Despite some initial suggestions to the contrary, this is also supported by molecular phylogenies. The Acantharea produce skeletons of strontium sulfate and is closely related to a peculiar genus, Sticholonche (Taxopodida), which lacks an internal skeleton and was for long time considered a heliozoan. The Radiolaria can therefore be divided into two major lineages: Polycystina (Spumellaria + Nassellaria) and Spasmaria (Acantharia + Taxopodida).[5][6]

There are several higher-order groups that have been detected in molecular analyses of environmental data. Particularly, groups related to Acantharia[7] and Spumellaria.[8] These groups are so far completely unknown in terms of morphology and physiology and the radiolarian diversity is therefore likely to be much higher than what is currently known.

The relationship between the Foraminifera and Radiolaria is also debated. Molecular trees supports their close relationship—a grouping termed Retaria.[9] But whether they are sister lineages or if the Foraminifera should be included within the Radiolaria is not known.

Biogeography

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Radiolarian biogeography with observed and predicted responses to temperature change
The color polygons in all three panels represent generalized radiolarian biogeographic provinces, as well as their relative water mass temperatures (cooler colors indicate cooler temperatures, and vice versa). Globe image adapted from NASA Blue Marble: Next Generation imagery. Ocean floor bathymetry from Google Earth seafloor elevation profile (5°N–74°S, at 120°W).

In the diagram on the right, a Illustrates generalized radiolarian provinces [10][11] and their relationship to water mass temperature (warm versus cool color shading) and circulation (gray arrows). Due to high-latitude water mass submergence under warm, stratified waters in lower latitudes, radiolarian species occupy habitats at multiple latitudes, and depths throughout the world oceans. Thus, marine sediments from the tropics reflect a composite of several vertically stacked faunal assemblages, some of which are contiguous with higher latitude surface assemblages. Sediments beneath polar waters include cosmopolitan deep-water radiolarians, as well as high-latitude endemic surface water species. Stars in (a) indicate the latitudes sampled, and the gray bars highlight the radiolarian assemblages included in each sedimentary composite. The horizontal purple bars indicate latitudes known for good radiolarian (silica) preservation, based on surface sediment composition.[12][13]

Data show that some species were extirpated from high latitudes but persisted in the tropics during the late Neogene, either by migration or range restriction (b). With predicted global warming, modern Southern Ocean species will not be able to use migration or range contraction to escape environmental stressors, because their preferred cold-water habitats are disappearing from the globe (c). However, tropical endemic species may expand their ranges toward midlatitudes. The color polygons in all three panels represent generalized radiolarian biogeographic provinces, as well as their relative water mass temperatures (cooler colors indicate cooler temperatures, and vice versa).[13]

Radiolarian shells

Radiolarian shapes
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Drawings by Haeckel 1904 (click for details)

Radiolarians are unicellular predatory protists encased in elaborate globular shells usually made of silica and pierced with holes. Their name comes from the Latin for "radius". They catch prey by extending parts of their body through the holes. As with the silica frustules of diatoms, radiolarian shells can sink to the ocean floor when radiolarians die and become preserved as part of the ocean sediment. These remains, as microfossils, provide valuable information about past oceanic conditions.[14]

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Animation of radiolarian diversity [15]
Turing and radiolarian morphology
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Shell of a spherical radiolarian
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Shell micrographs
Computer simulations of Turing patterns on a sphere
closely replicate some radiolarian shell patterns[16]

Fossil record

Fossil radiolarian
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X-ray microtomography of Triplococcus acanthicus
This is a microfossil from the Middle Ordovician with four nested spheres. The innermost sphere is highlighted red. Each segment is shown at the same scale.[17]

The earliest known radiolaria date to the very start of the Cambrian period,[18][19][20][21] appearing in the same beds as the first small shelly fauna—they may even be terminal Precambrian in age. They have significant differences from later radiolaria, with a different silica lattice structure and few, if any, spikes on the test.[20] Ninety percent of radiolarian species are extinct. The skeletons, or tests, of ancient radiolarians are used in geological dating, including for oil exploration and determination of ancient climates.[22]

Some common radiolarian fossils include Actinomma, Heliosphaera and Hexadoridium

References

  1. ^ Smalley, I.J. (1963). "Radiolarians:construction of spherical skeleton". Science. 140: 396–397. doi:10.1126/science.140.3565.396.
  2. ^ Pawlowski J, Burki F (2009). "Untangling the phylogeny of amoeboid protists". J. Eukaryot. Microbiol. 56 (1): 16–25. doi:10.1111/j.1550-7408.2008.00379.x. PMID 19335771.
  3. ^ Yuasa T, Takahashi O, Honda D, Mayama S (2005). "Phylogenetic analyses of the polycystine Radiolaria based on the 18s rDNA sequences of the Spumellarida and the Nassellarida". European Journal of Protistology. 41 (4): 287–298. doi:10.1016/j.ejop.2005.06.001.
  4. ^ Nikolaev SI, Berney C, Fahrni JF, et al. (May 2004). "The twilight of Heliozoa and rise of Rhizaria, an emerging supergroup of amoeboid eukaryotes". Proc. Natl. Acad. Sci. U.S.A. 101 (21): 8066–71. doi:10.1073/pnas.0308602101. PMC 419558. PMID 15148395.
  5. ^ Krabberød AK, Bråte J, Dolven JK, et al. (2011). "Radiolaria divided into Polycystina and Spasmaria in combined 18S and 28S rDNA phylogeny". PLoS ONE. 6 (8): e23526. Bibcode:2011PLoSO...623526K. doi:10.1371/journal.pone.0023526. PMC 3154480. PMID 21853146.
  6. ^ Cavalier-Smith T (December 1993). "Kingdom protozoa and its 18 phyla". Microbiol. Rev. 57 (4): 953–94. doi:10.1128/mmbr.57.4.953-994.1993. PMC 372943. PMID 8302218.
  7. ^ Decelle J, Suzuki N, Mahé F, de Vargas C, Not F (May 2012). "Molecular phylogeny and morphological evolution of the Acantharia (Radiolaria)". Protist. 163 (3): 435–50. doi:10.1016/j.protis.2011.10.002. PMID 22154393.
  8. ^ Not F, Gausling R, Azam F, Heidelberg JF, Worden AZ (May 2007). "Vertical distribution of picoeukaryotic diversity in the Sargasso Sea". Environ. Microbiol. 9 (5): 1233–52. doi:10.1111/j.1462-2920.2007.01247.x. PMID 17472637.
  9. ^ Cavalier-Smith T (July 1999). "Principles of protein and lipid targeting in secondary symbiogenesis: euglenoid, dinoflagellate, and sporozoan plastid origins and the eukaryote family tree". J. Eukaryot. Microbiol. 46 (4): 347–66. doi:10.1111/j.1550-7408.1999.tb04614.x. PMID 18092388.
  10. ^ Boltovskoy, D., Kling, S. A., Takahashi, K. & BjØrklund, K. (2010) "World atlas of distribution of recent Polycystina (Radiolaria)". Palaeontologia Electronica, 13: 1–230.
  11. ^ Casey, R. E., Spaw, J. M., & Kunze, F. R. (1982) "Polycystine radiolarian distribution and enhancements related to oceanographic conditions in a hypothetical ocean". Am. Assoc. Pet. Geol. Bull., 66: 319–332.
  12. ^ Lazarus, David B. (2011). "The deep-sea microfossil record of macroevolutionary change in plankton and its study". Geological Society, London, Special Publications. 358 (1): 141–166. Bibcode:2011GSLSP.358..141L. doi:10.1144/SP358.10. S2CID 128826639.
  13. ^ a b Trubovitz, Sarah; Lazarus, David; Renaudie, Johan; Noble, Paula J. (2020). "Marine plankton show threshold extinction response to Neogene climate change". Nature Communications. 11 (1): 5069. Bibcode:2020NatCo..11.5069T. doi:10.1038/s41467-020-18879-7. PMC 7582175. PMID 33093493. CC-BY icon.svg Material was copied from this source, which is available under a Creative Commons Attribution 4.0 International License.
  14. ^ Wassilieff, Maggy (2006) "Plankton - Animal plankton", Te Ara - the Encyclopedia of New Zealand. Accessed: 2 November 2019.
  15. ^ Kachovich, Sarah (2018) "Minds over Methods: Linking microfossils to tectonics" Blog of the Tectonics and Structural Geology Division of the European Geosciences Union.
  16. ^ Varea, C.; Aragon, J.L.; Barrio, R.A. (1999). "Turing patterns on a sphere". Physical Review E. 60 (4): 4588–92. Bibcode:1999PhRvE..60.4588V. doi:10.1103/PhysRevE.60.4588. PMID 11970318.
  17. ^ Kachovich, S., Sheng, J. and Aitchison, J.C., 2019. Adding a new dimension to investigations of early radiolarian evolution. Scientific reports, 9(1), pp.1-10. doi:10.1038/s41598-019-42771-0. CC-BY icon.svg Material was copied from this source, which is available under a Creative Commons Attribution 4.0 International License.
  18. ^ Chang, Shan; Feng, Qinglai; Zhang, Lei (14 August 2018). "New Siliceous Microfossils from the Terreneuvian Yanjiahe Formation, South China: The Possible Earliest Radiolarian Fossil Record". Journal of Earth Science. 29 (4): 912–919. doi:10.1007/s12583-017-0960-0.
  19. ^ name=Zhang2019>Zhang, Ke; Feng, Qing-Lai (September 2019). "Early Cambrian radiolarians and sponge spicules from the Niujiaohe Formation in South China". Palaeoworld. 28 (3): 234–242. doi:10.1016/j.palwor.2019.04.001.
  20. ^ a b Braun, Chen, Waloszek & Maas (2007), "First Early Cambrian Radiolaria", in Vickers-Rich, Patricia; Komarower, Patricia (eds.), The Rise and Fall of the Ediacaran Biota, Special publications, 286, London: Geological Society, pp. 143–149, doi:10.1144/SP286.10, ISBN 9781862392335, OCLC 156823511CS1 maint: uses authors parameter (link)
  21. ^ Maletz, Jörg (June 2017). "The identification of putative Lower Cambrian Radiolaria". Revue de Micropaléontologie. 60 (2): 233–240. doi:10.1016/j.revmic.2017.04.001.
  22. ^ Zuckerman, L.D., Fellers, T.J., Alvarado, O., and Davidson, M.W. "Radiolarians", Molecular Expressions, Florida State University, 4 February 2004.

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Radiolaria: Brief Summary

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The Radiolaria, also called Radiozoa, are protozoa of diameter 0.1–0.2 mm that produce intricate mineral skeletons, typically with a central capsule dividing the cell into the inner and outer portions of endoplasm and ectoplasm. The elaborate mineral skeleton is usually made of silica. They are found as zooplankton throughout the global ocean. As zooplankton, radiolarians are primarily heterotrophic, but many have photosynthetic endosymbionts and are, therefore, considered mixotrophs. The skeletal remains of some types of radiolarians make up a large part of the cover of the ocean floor as siliceous ooze. Due to their rapid change as species and intricate skeletons, radiolarians represent an important diagnostic fossil found from the Cambrian onwards.

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