Carpediemonas

Carpediemonas is genus of Metamonada, and belongs to the group Excavata. This organism is a unicellular flagellated eukaryote that was first discovered in substrate samples from the Great Barrier Reef.[2] Carpediemonas can be found in anaerobic intertidal sediment, where it feeds on bacteria. A feature of this species is the presence of a feeding groove, a characteristic of the excavates. Like most other metamonads, Carpediemonas does not rely on an aerobic mitochondria to produce energy. Instead, it contains hydrogenosomes that are used to produce ATP.[3] This organism has two flagella:[3] a posterior one used for feeding on the substrate, and an anterior one that moves in a slower sweeping motion.[2] Carpediemonas is assigned to the fornicates, where similar Carpediemonas-like organisms are used in researching the evolution within excavates.[4] Although Carpediemonas is a member of the metamonads, it is unusual in the sense that it is free-living and has three basal bodies.[5]

Carpediemonas
Scientific classification
Domain:	Eukaryota
(unranked):	Excavata
Phylum:	Metamonada
Subphylum:	Fornicata
Superclass:	Carpediemonadia Cavalier-Smith
Class:	Carpediemonadea Cavalier-Smith
Order:	Carpediemonadida Cavalier-Smith
Genus:	Carpediemonas Ekebom, Patterson & Vørs, 1996 [1]
Species
Carpediemonas bialata Carpediemonas frisia Carpediemonas membranifera

Etymology

The name Carpediemonas originates from three Latin roots, with carpe meaning ‘seize’, die meaning ‘the day’, and the suffix of monas, indicating a unicellular organism. The organism was named after ‘carpe diem’, meaning ‘to seize the day’, in honour of the wife of one of the authors, who had recently died.[6]

History of Knowledge

Carpediemonas was first discovered by Larsen and Patterson (1990) with the original name of Percolomonas. The species found was named Percolomonas membranifera. Larsen and Patterson classified this organism as Percolomonas, a heterolobosean, because it would occasionally have four flagella and contain a longitudinal groove. However, they did not have any evidence that the non-dividing organisms had more than two flagella. The species also contained a pouch with threads that may be difficult to discern from flagella. Therefore, Ekebom et al. (1996) then renamed the organism as Carpediemonas when it was found from substrate samples in the Great Barrier Reef and classified it as a metamonad.[2] Additionally, a metabolic relationship of Carpediemonas with prokaryotic communities was found in Carpediemonas frisia. C. frisia was found to release biomolecules that have been predigested. Prokaryotic communities would rely on C. frisia for incompletely digested organic material and the oxidation of various biomolecules. On the other hand, C. frisia relies on the prokaryotic organism, Deltaproteobacteria, for its hydrogen oxidizing activity.[7]

Habitat and Ecology

Carpediemonas can be found in anaerobic intertidal sediment, where it feeds on bacteria.[3] It can be found co-existing with Cafeteria marsupialis in these anaerobic environments.[2]

Description of Organism

Ekebom et al. (1996) describes Carpediemonas as organisms with a size of approximately 5 µm long (with a range of 4-7.5 µm). Carpediemonas has a longitudinal depression that spans almost the entire ventral side of the cell. It often has two unequal flagella inserting to the anterior side of the ventral groove, but may sometimes have three or four flagella. The acronematic posterior flagellum is used in feeding and to attach to substrate, while the anterior flagellum beats less rapidly and in a slow sweeping motion.[2] Further studies by Simpson and Patterson (1999) go into greater detail about the flagella and describe the flagellar apparatus as having a third, barren basal body. Supporting the dorsal side of the cell is a microtubular fan with a microtubular root at the anterior end. On the ventral side, microtubules extending from different flagellar roots support the ventral groove. The anterior flagellum has a ‘9+2’ axoneme. Simpson and Patterson described that in addition to the ‘9+2’ axoneme, the posterior flagellum also has “three radiating lamellae of electron-dense material which form the central components of vanes”. The first lamella arises from after the flagellar insertion and is directed ventrally. The second lamella originates opposite from the first lamella. The third lamella supports the third vane, which is located more distally and lies perpendicular to the other two vanes or lamellae. All three lamella have striations when viewed in a longitudinal section and these striations are perpendicular to the ‘9+2’ axoneme. Carpediemonas contains a single ovate nucleus, located anteriorly in the cell. The nucleolus can also be found subcentrally within the nucleus. Carpediemonas also has no mitochondria, which is typical of metamonads. Instead, it has hydrogenosomes, likely derived from anaerobic mitochondria. It also contains a single Golgi dictyosome, located anteriorly, dorsally, and to the left of the flagellar apparatus.[3] The endoplasmic reticulum in this genus is mainly found near the periphery of the cell. Around the cytoplasm, food vacuoles containing bacterial contents can be found.[3] Also, three centrioles are present in Carpediemonas.[8]

Taxonomy

Carpediemonas is classified as an excavate because it has the characteristic feeding groove of the group. Within the excavates, Carpediemonas is assigned to the fornicates. In the fornicates, Carpediemonas-like organisms (CLOs) have allowed for the better understanding of the evolution of anaerobic excavates by studying their cytoskeletal traits and modified mitochondria. An example of a Carpediemonas-like organism that was used to study the evolutionary history within excavates is Kipferlia bialata.[4]

References

1. J. Ekebom; D. J. Patterson; N. Vørs (1996). "Heterotrophic flagellates from coral reef sediments (Great Barrier Reef, Australia)". Archiv für Protistenkunde. 146 (3–4): 251–272. doi:10.1016/S0003-9365(96)80013-3.
2. Ekebom, J.; Patterson, D.J.; Vørs, N. (1996). "Heterotrophic Flagellates from Coral Reef Sediments (Great Barrier Reef, Australia)". Archiv für Protistenkunde. 146 (3–4): 251–272. doi:10.1016/s0003-9365(96)80013-3. ISSN 0003-9365.
3. Simpson, Alastair G.B.; Patterson, David J. (1999). "The ultrastructure of Carpediemonas membranifera (Eukaryota) with reference to the "excavate hypothesis"". European Journal of Protistology. 35 (4): 353–370. doi:10.1016/s0932-4739(99)80044-3. ISSN 0932-4739.
4. Yubuki, Naoji; Simpson, Alastair G.B.; Leander, Brian S. (2013). "Comprehensive Ultrastructure of Kipferlia bialata Provides Evidence for Character Evolution within the Fornicata (Excavata)". Protist. 164 (3): 423–439. doi:10.1016/j.protis.2013.02.002. ISSN 1434-4610. PMID 23517666.
5. "CARPEDIEMONADA". comenius.susqu.edu. Retrieved 2019-04-22.
6. "Taxonomy – It Came from the Pond". Retrieved 2019-04-22.
7. Hamann, Emmo; Tegetmeyer, Halina E; Riedel, Dietmar; Littmann, Sten; Ahmerkamp, Soeren; Chen, Jianwei; Hach, Philipp F; Strous, Marc (2017-02-17). "Syntrophic linkage between predatory Carpediemonas and specific prokaryotic populations". The ISME Journal. 11 (5): 1205–1217. doi:10.1038/ismej.2016.197. ISSN 1751-7362. PMC 5437931. PMID 28211847.
8. Cavalier-Smith, T. (2003-11-01). "The excavate protozoan phyla Metamonada Grasse emend. (Anaeromonadea, Parabasalia, Carpediemonas, Eopharyngia) and Loukozoa emend. (Jakobea, Malawimonas): their evolutionary affinities and new higher taxa". International Journal of Systematic and Evolutionary Microbiology. 53 (6): 1741–1758. doi:10.1099/ijs.0.02548-0. ISSN 1466-5026. PMID 14657102.