Sea butterfly

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Sea butterflies
Temporal range: Late Paleocene–recent
LimacinaHelicinaNOAA.jpg
Limacina helicina
Scientific classification e
Kingdom: Animalia
Phylum: Mollusca
Class: Gastropoda
Subclass: Heterobranchia
Clade: Euopisthobranchia
Clade: Thecosomata
Blainville, 1824
Families

Limacinidae
Cavoliniidae
Clionidae
Creseidae
Cuvierinidae
Praecuvierinidae
Peraclididae
Cymbuliidae
Desmopteridae

Sea butterflies, scientific name Thecosomata (thecosomes,[1] "case / shell-body"[2]), are a taxonomic suborder of small pelagic swimming sea snails. They are holoplanktonic opisthobranch gastropod mollusks. Most Thecosomata have some form of calcified shell, although it is often very light and / or transparent.[3]

The sea butterflies include some of the world's most abundant gastropod species,[1] and because of their large numbers are an essential part of the food chain, and a significant contributor to the oceanic carbon cycle.[3][4]

The sea butterflies are included in the Pteropoda order, and are also included in the informal group Opisthobranchia.

Morphology[edit]

Sea butterflies float and swim freely in the water, and are carried along with the currents. This has led to a number of adaptations in their bodies. The shell and the gill have disappeared in several families. Their gastropodal foot has taken the form of two wing-like lobes, or parapodia, which propel the animal through the sea by slow flapping movements.

Unidentified thecosome

Most Thecosomata have some form of calcified shell, although often very light.[3] They are rather difficult to see, since their shell (if present) is mostly transparent, very fragile, and usually tiny: Less than 1 cm in length. Although their shell may be so fine as to be transparent, it is nevertheless calcareous, and an important part of the ocean calcite cycle.[4] Their shells are bilaterally symmetric and can vary widely in shape: coiled, needle-like, triangular, or globular.

The shell is present in all stages of the Cavolinioidea (euthecosomata) life cycle. In the Cymbulioidea (pseudothecosomata), adult Peraclididae also bear shells; the Cymbuliidae shed their larval shells and develop a cartilaginous pseudoconch in adulthood; only the Desmopteridaen lack any rigid covering as adults.

Behaviour and distribution[edit]

Sea butterflies range from the tropics[5] to the poles.[6] They are "holoplanktonic": That is, they spend their whole lives floating among the plankton, rather than just being planktonic during their larval stage.[a] As such, the thecosomata are the most common (in terms of diversity, species richness, and abundance) in the top 25 metres (82 ft) of the ocean, and become rarer the deeper one samples.[5]

Sometimes, they swarm in large numbers and can be found washed up in flotsam, especially along the coast of eastern Australia.

Diurnal vertical migration[edit]

Thecosomata beat their wing-like parapodia to "fly" through the water.[6][7] When descending to deeper water, they hold their wings up.

They migrate vertically from day to night, so the community structure changes on a 24 hour cycle; during the day many organisms take refuge at water depths in excess of 100 m.[5]

Feeding[edit]

Little is known about the behaviour of sea butterflies, but they are known to have a peculiar way of feeding.[3]

They are generally herbivorous, mostly passive plankton feeders, just floating along with the currents, ventral-side up, although some may become active feeders at times.[3] They catch planktonic food by entangling it in a mucous web[6] that can be up to 5 cm wide – many times larger than themselves. If disturbed, they abandon the net and flap slowly away.

Every day, they migrate vertically in the water column, following their planktonic prey. At night they graze at the ocean surface and return to deeper water in the morning.[8]

Fossil record[edit]

This is, geologically speaking, a rather young group, having evolved from the Late Paleocene in the Cenozoic Era.[9]

Sea butterfly pseudoconch

The group is represented in the fossil record from shells of those groups within the clade that mineralized.[10][11] These carbonate shells are a major contributor to the oceanic carbon cycle, making up as much as 12% of global carbonate flux.[3] However the low stability of their aragonitic shells means that few end up being preserved in sediments as fossils, mostly being deposited in shallow waters of tropical seas.[3]

Importance in the food chain[edit]

These creatures, which range from lentil- to orange-sized, are eaten by various marine species, including a wide variety of fish that are, in turn, consumed by penguins and polar bears. The sea butterflies form the sole food source of their relatives, the Gymnosomata.[6] They are also consumed by sea birds, whales, and commercially important fish. However, if sea butterflies are consumed in large quantities fish can get "black gut", which makes them unsellable.[1]

Taxonomy[edit]

Along with its sister group, the sea angels (Gymnosomata), the sea butterflies (Thecosomata) are included in the order Pteropoda.[3] The validity of the pteropod order is not universally accepted; it fell out of favour for a number of years, but recent molecular evidence suggests that the taxon should be revived.[12] Although most Thecosomata have some form of calcified shell, mature Gymnosomata have none.[3]

Ponder & Lindberg[edit]

Order Thecosomata de Blainville, 1824

Bouchet & Rocroi[edit]

In the new taxonomy of Bouchet & Rocroi (2005) Thecosomata is treated differently :

Clade Thecosomata : [13]

  • Superfamily Cavolinioidea Gray, 1850 ( = Euthecosomata)
    • Family Cavoliniidae Gray, 1850 (1815)
      • Subfamily Cavoliinae Gray, 1850 (1815) (formerly Hyalaeidae Rafinesque, 1815 )
      • Subfamily Clioinae Jeffreys, 1869 (formerly Cleodoridae Gray, 1840 - nomen oblitum)
      • Subfamily Cuvierininae van der Spoel, 1967 (formerly : Cuvieriidae Gray, 1840 (nom. inv.); Tripteridae Gray, 1850 )
      • Subfamily Creseinae Curry, 1982
    • Family Limacinidae Gray, 1840 (formerly : Spirialidae Chenu, 1859 ; Spiratellidae Dall, 1921 )
    • † Family Sphaerocinidae A. Janssen & Maxwell, 1995
  • Superfamily Cymbulioidea Gray, 1840 ( = Pseudothecosomata)
    • Family Cymbuliidae Gray, 1840
      • Subfamily Cymbuliinae Gray, 1840
      • Subfamily Glebinae van der Spoel, 1976
    • Family Desmopteridae Chun, 1889
    • Family Peraclidae Tesch, 1913 (formerly Procymbuliidae Tesch, 1913

Bouchet & Rocroi (2005) move the family Limacinidae into the superfamily Cavolinioidea, making redundant the superfamily Limacinoidea erected for it in Ponder & Lindberg's taxonomy. The families Creseidae and Cuvierinidae are demoted to subfamilies of Cavoliniidae (Creseinae and Cuvierininae). The infraorder Pseudothecosomata becomes the superfamily Cymbulioidea. The family Peraclididae is included in the superfamily Cymbulioidea as the family Peraclidae, making the superfamily Peraclidoidea redundant.

See also[edit]

Footnotes[edit]

  1. ^ Compare the sea butterflies unusual whole-life residence in the plankton with the more common behavior of most other marine gastropods, whose veliger larvae are part of the meroplankton, but who leave the plankton once they reach adult form.

References[edit]

  1. ^ a b c Lalli, Carol M.; Gilmer, Ronald W. (1989). Pelagic Snails: The Biology of Holoplanktonic Gastropod Mollusks. ISBN 978-0-8047-1490-7.
  2. ^ "theco-". Oxford English Dictionary (Online ed.). Oxford University Press. (Subscription or participating institution membership required.) Sub-entry: "thecoˈsomate, thecoˈsomatous adjs. [Gr. σῶµα body], belonging to the Thecosomata"
  3. ^ a b c d e f g h i Hunt, B.P.V.; Pakhomov, E.A.; Hosie, G.W.; Siegel, V.; Ward, P.; Bernard, K. (2008). "Pteropods in Southern Ocean ecosystems". Progress in Oceanography. 78 (3): 193. doi:10.1016/j.pocean.2008.06.001.
  4. ^ a b Comeau, S.; Gorsky, G.; Jeffree, R.; Teyssié, J.-L.; Gattuso, J.-P. (2009). "Impact of ocean acidification on a key Arctic pelagic mollusc (Limacina helicina)". Biogeosciences. 6 (9): 1877. doi:10.5194/bg-6-1877-2009.
  5. ^ a b c Parra-Flores, A.; Gasca, R. (2009). "Distribution of pteropods (Mollusca: Gastropoda: Thecosomata) in surface waters (0–100 m) of the Western Caribbean Sea (winter, 2007)". Revista de Biología Marina y Oceanografía. 44 (3): 647–662. doi:10.4067/s0718-19572009000300011.
  6. ^ a b c d Seibel, B.A.; Dymowska, A.; Rosenthal, J. (2007). "Metabolic temperature compensation and coevolution of locomotory performance in pteropod molluscs". Integrative and Comparative Biology. 47 (6): 880–891. doi:10.1093/icb/icm089. PMID 21669767.
  7. ^ Murphy, D.; Adhikari, D.; Webster, D.; Yen, J. (2016). "Underwater flight by the planktonic sea butterfly". Journal of Experimental Biology. 219 (4): 535–543. doi:10.1242/jeb.129205. PMID 26889002.
  8. ^ "Sea Butterfly". Our Breathing Planet. Retrieved 12 October 2016.
  9. ^ Bé, A.W.H.; Gilmer, R.W. (1977). "A zoogeographic and taxonomic review of euthecosomatous pteropoda". In Ramsey, A.T.S. (ed.). Oceanic Micropaleontology. Vol. 1. London, UK: Academic Press. pp. 733–808.
  10. ^ Janssen, A.W. (2008). "Heliconoides linneensis sp. nov., a new holoplanktonic gastropod (Mollusca, Thecosomata) from the Late Oligocene of the Aquitaine Basin (France, Landes)". Zoologische Mededelingen. 82 (9): 69–72.
  11. ^ Lokho, K.; Kumar, K. (2008). "Fossil pteropods (Thecosomata, holoplanktonic Mollusca) from the Eocene of Assam-Arakan Basin, northeastern India". Current Science. 94 (5): 647–652.
  12. ^ Klussmann-Kolb, A.; Dinapoli, A. (2006). "Systematic position of the pelagic Thecosomata and Gymnosomata within Opisthobranchia (Mollusca, Gastropoda) - revival of the Pteropoda". Journal of Zoological Systematics and Evolutionary Research. 44 (2): 118. doi:10.1111/j.1439-0469.2006.00351.x.
  13. ^ van der Spoel, S. (1976). Pseudothecosomata, Gymnosomata and Heteropoda (Gastropoda). Utrecht: Bohn, Scheltema & Holkema. pp. 484 pp. ISBN 90-313-0176-0.

Sources[edit]

  • Bé, A.W.H.; Gilmer, R.W. (1977). "A zoogeographic and taxonomic review of euthecosomatous pteropoda". In Ramsey, A.T.S. (ed.). Oceanic Micropaleontology. Vol. 1. London, UK: Academic Press. pp. 733–808.
  • van der Spoel, S. (1967). Euthecosomata, a group with remarkable developmental stages (Gastropoda, Pteropoda) (Thesis). University of Amsterdam. Gorinchem (J. Noorduijn)
  • van der Spoel, S. (1976). Pseudothecosomata, Gymnosomata, and Heteropoda (Gastropoda). Utrecht: Bohn, Scheltema & Holkema.
  • [no author cited] (2003). "Regarding the raising of ranks". Cainozoic Research. 2 (1–2): 163–170. {{cite journal}}: |author= has generic name (help)