Fragilariopsis kerguelensis explained
Fragilariopsis kerguelensis,[1] is a pennate diatom native to the Southern Ocean. It has been characterized as "the most abundant diatom in the Antarctic Seas".[2]
Description
Fragilariopsis kerguelensis is a unicellular, phototrophic, microalga with a range in size of 10 - 80 μm.[3] It is encased in a heavily silicified cell wall, called the frustule, and is identified by its unique theca, raphe and striations, which distinguish it from other diatoms.[4] They are native to pelagic environments of the Southern Ocean within a temperature range of -1° to 18° C. F. kerguelensis is known to form community chains that consist of 20-100 cells and can be up to 300 μm long.[5]
Use as a paleoceanographic proxy
Fragilariopsis kerguelensis is well preserved in the fossil record and commonly referenced as a paleoceanographic or paleoclimatic proxy. F. kerguelensis comprises the largest deposit of biogenic silica in the world (~75%) despite only accounting for 20% of global production.[6] It is an open water species and is found in its highest abundance between the Antarctic Circumpolar Current and the Subtropical Front.[7] This, along with its tendency to increase valve size near polar fronts, makes F. kerguelensis an ideal indicator of paleoclimate polar front or low-carbon, high-silica exporting regimes.[8] [9] Modern assemblages with F. kerguelensis can be used to calculate past sea surface temperature through the use of transfer functions.[10]
Notes and References
- O'Meara. E. the diatomaceous gatherings made at Kerguelen's Land. Journal of the Linnean Society, Botany. 1877. 15. 55–59.
- Hart. T.J. Phytoplankton periodicity in Antarctic surface waters. Discovery Rep. 1942.
- Smetacek. V. Diatoms and the ocean carbon cycle. Protist. 1999. 150. 1. 25–32. 10.1016/s1434-4610(99)70006-4. 10724516.
- Web site: Fragilariopsis kerguelensis (O'Meara) Hustedt, 1952. World Register of Marine Species. World Register of Marine Species.
- Smetacek. V. Assmy. P. Henjes. J. The role of grazing in structuring Southern Ocean pelagic ecosystems and biogeochemical cycles. Antarctic Science. 2004. 16. 4. 541–558. 10.1017/s0954102004002317. 2004AntSc..16..541S. 131176101.
- Verity. P.G. Smetacek. V. Organism life cycles, predation, and the structure of marine pelagic ecosystems. Marine Ecology Progress Series. 1996. 130. 1. 231–250. 10.3354/meps130277. 1996MEPS..130..277V. free.
- Crosta. X. Romero. O. Armand. L.K. Pichon. J.J. The biogeography of major diatom taxa in Southern Ocean sediments: 2. Open ocean related species. Palaeogeography, Palaeoclimatology, Palaeoecology. 2005. 223. 1. 6–92. 10.1016/j.palaeo.2005.03.028. 2005PPP...223...66C.
- Cortese. G. Gersonde. R. Morphometric variability in the diatom Fragilariopsis kerguelensis: Implications for Southern Ocean paleoceanography. Earth Planet. Sci. Lett.. 2007. 257. 3–4. 526–544. 10.1016/j.epsl.2007.03.021. 2007E&PSL.257..526C.
- Web site: Profile: Fragilariopsis kerguelensis - Biota - Confluence. SOKI Wiki. Antarctic Climate and Ecosystems Co-operative Research Centre.
- Zielinski. U. Gersonde. R. Diatom distribution in Southern Ocean surface sediments (Atlantic sector): Implications for paleoenvironmental reconstructions. Palaeogeography, Palaeoclimatology, Palaeoecology. 1997. 129. 3–4. 213–250. 10.1016/s0031-0182(96)00130-7. 1997PPP...129..213Z.