Myctophiformes
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The Myctophiformes are an order of ray-finned fishes consisting of two families of deep-sea marine fish, most notably the highly abundant lanternfishes (Myctophidae). The blackchins (Neoscopelidae) contain six species in three genera, while the bulk of the family belongs to the Myctophidae, with over 30 genera and some 252 species.Nelson (2006): p.223 The
scientific name In Taxonomy (biology), taxonomy, binomial nomenclature ("two-term naming system"), also called binary nomenclature, is a formal system of naming species of living things by giving each a name composed of two parts, both of which use Latin gramm ...
ultimately derives from
Ancient Greek Ancient Greek (, ; ) includes the forms of the Greek language used in ancient Greece and the classical antiquity, ancient world from around 1500 BC to 300 BC. It is often roughly divided into the following periods: Mycenaean Greek (), Greek ...
''myktér'' (μυκτήρ, "nose") + ''óphis'' (ὄφῖς, "serpent") +
Latin Latin ( or ) is a classical language belonging to the Italic languages, Italic branch of the Indo-European languages. Latin was originally spoken by the Latins (Italic tribe), Latins in Latium (now known as Lazio), the lower Tiber area aroun ...
''forma'' ("external form"), the Greek part in reference to the long, slender, and heavy-headed shape of these fishes.


Description and ecology

These smallish fishes inhabit the pelagic and benthopelagic zones of the deep sea. They are laterally compressed and usually have photophores (light organs). The eyes are large, in some decidedly huge, and generally directed straight sideways. The mouth also quite large and located at the tip of the snout; its gape extends to below the eyes or even beyond. They have an adipose fin. The
pelvic fin Pelvic fins or ventral fins are paired fins located on the ventral (belly) surface of fish, and are the lower of the only two sets of paired fins (the other being the laterally positioned pectoral fins). The pelvic fins are homologous to the hi ...
has eight rays in most myctophiforms, and the number of branchiostegal rays is usually higher than six and lower than 12.


Systematics

The two families of the Myctophiformes are: * Myctophidae – lanternfishes * Neoscopelidae – blackchins The extinct family Sardinioididae (containing '' Sardinioides'' and possibly '' Volcichthys'') is known from the
Late Cretaceous The Late Cretaceous (100.5–66 Ma) is the more recent of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after ''cre ...
(
Cenomanian The Cenomanian is, in the International Commission on Stratigraphy's (ICS) geological timescale, the oldest or earliest age (geology), age of the Late Cretaceous epoch (geology), Epoch or the lowest stage (stratigraphy), stage of the Upper Cretace ...
to Campanian). The genus '' Neocassandra'' from the Late Paleocene is either considered its own family or a member of the Neoscopelidae. Some members were previously confused with aulopiforms. The order Myctophiformes is anatomically similar to the grinners (Aulopiformes), but their pharyngobranchials and retractor muscles are more
plesiomorph In phylogenetics, a plesiomorphy ("near form") and symplesiomorphy are synonyms for an ancestral Phenotypic trait, character shared by all members of a clade, which does not distinguish the clade from other clades. Plesiomorphy, symplesiomorph ...
ic. It was also allied with the more advanced spiny- rayed Teleostei (e.g. Paracanthopterygii) as " Ctenosquamata". These apomorphically have a fifth upper pharyngeal toothplate and a third internal levator muscle to move it, and molecular data also support the long-held view that these two lineages are at least closely related. Other sources ally them with the Lampriformes, which are often placed in a
monotypic In biology, a monotypic taxon is a taxonomic group (taxon) that contains only one immediately subordinate taxon. A monotypic species is one that does not include subspecies or smaller, infraspecific taxa. In the case of genera, the term "unisp ...
superorder "Lampridiomorpha". In a similar fashion, separation of the Myctophiformes in superorder "Scopelomorpha" has been proposed. The Aulopiformes, though, are usually considered to be closer or even among the Protacanthopterygii, one of the core groups of moderately advanced teleosts. As modern
taxonomy image:Hierarchical clustering diagram.png, 280px, Generalized scheme of taxonomy Taxonomy is a practice and science concerned with classification or categorization. Typically, there are two parts to it: the development of an underlying scheme o ...
tries to avoid a profusion of small taxa, and the delimitation of the Euteleostei (Protacanthopterygii '' sensu stricto'' and their allies) versus "Ctenosquamata" such as the Paracanthopterygii remains uncertain, the
systematics Systematics is the study of the diversification of living forms, both past and present, and the relationships among living things through time. Relationships are visualized as evolutionary trees (synonyms: phylogenetic trees, phylogenies). Phy ...
and taxonomy of the Myctophiformes among the teleosts are in need of further study.Nelson (2006): p.223, Diogo (2008)


Timeline of genera

ImageSize = width:1500px height:auto barincrement:15px PlotArea = left:10px bottom:50px top:10px right:10px Period = from:-145.5 till:15 TimeAxis = orientation:horizontal ScaleMajor = unit:year increment:10 start:-145.5 ScaleMinor = unit:year increment:1 start:-145.5 TimeAxis = orientation:hor AlignBars = justify Colors = #legends id:CAR value:claret id:ANK value:rgb(0.4,0.3,0.196) id:HER value:teal id:HAD value:green id:OMN value:blue id:black value:black id:white value:white id:cretaceous value:rgb(0.5,0.78,0.31) id:earlycretaceous value:rgb(0.63,0.78,0.65) id:latecretaceous value:rgb(0.74,0.82,0.37) id:cenozoic value:rgb(0.54,0.54,0.258) id:paleogene value:rgb(0.99,0.6,0.32) id:paleocene value:rgb(0.99,0.65,0.37) id:eocene value:rgb(0.99,0.71,0.42) id:oligocene value:rgb(0.99,0.75,0.48) id:neogene value:rgb(0.999999,0.9,0.1) id:miocene value:rgb(0.999999,0.999999,0) id:pliocene value:rgb(0.97,0.98,0.68) id:quaternary value:rgb(0.98,0.98,0.5) id:pleistocene value:rgb(0.999999,0.95,0.68) id:holocene value:rgb(0.999,0.95,0.88) BarData= bar:eratop bar:space bar:periodtop bar:space bar:NAM1 bar:NAM2 bar:NAM3 bar:NAM4 bar:NAM5 bar:NAM6 bar:NAM7 bar:NAM8 bar:NAM9 bar:NAM10 bar:NAM11 bar:NAM12 bar:NAM13 bar:NAM14 bar:NAM15 bar:NAM16 bar:NAM17 bar:NAM18 bar:NAM19 bar:NAM20 bar:NAM21 bar:NAM22 bar:NAM23 bar:NAM24 bar:NAM25 bar:NAM26 bar:NAM27 bar:space bar:period bar:space bar:era PlotData= align:center textcolor:black fontsize:M mark:(line,black) width:25 shift:(7,-4) bar:periodtop from: -145.5 till: -99.6 color:earlycretaceous text: Early from: -99.6 till: -65.5 color:latecretaceous text: Late from: -65.5 till: -55.8 color:paleocene text: Paleo. from: -55.8 till: -33.9 color:eocene text: Eo. from: -33.9 till: -23.03 color:oligocene text: Oligo. from: -23.03 till: -5.332 color:miocene text: Mio. from: -5.332 till: -2.588 color:pliocene text: Pl. from: -2.588 till: -0.0117 color:pleistocene text: Pl. from: -0.0117 till: 0 color:holocene text: H. bar:eratop from: -145.5 till: -65.5 color:cretaceous text:
Cretaceous The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ...
from: -65.5 till: -23.03 color:paleogene text: Paleogene from: -23.03 till: -2.588 color:neogene text:
Neogene The Neogene ( ,) is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period million years ago ( Mya) to the beginning of the present Quaternary Period million years ago. It is the second period of th ...
from: -2.588 till: 0 color:quaternary text: Q. PlotData= align:left fontsize:M mark:(line,white) width:5 anchor:till align:left color:latecretaceous bar:NAM1 from: -99.6 till: -70.6 text: Sardinoides color:latecretaceous bar:NAM2 from: -85.8 till: -83.5 text: Chirothrix color:latecretaceous bar:NAM3 from: -83.5 till: -70.6 text: Sardinius color:paleocene bar:NAM4 from: -65.5 till: -55.8 text: Neocassandra color:paleocene bar:NAM5 from: -65.5 till: -55.8 text: Eokrefftia color:eocene bar:NAM6 from: -55.8 till: 0 text: Diaphus color:eocene bar:NAM7 from: -48.6 till: -23.03 text: Eomyctophum color:oligocene bar:NAM8 from: -28.4 till: 0 text: Lobianchia color:oligocene bar:NAM9 from: -28.4 till: 0 text: Hygophum color:miocene bar:NAM10 from: -23.03 till: 0 text: Symbolophorus color:miocene bar:NAM11 from: -23.03 till: 0 text: Lampanyctus color:miocene bar:NAM12 from: -23.03 till: 0 text: Bolinichthyes color:miocene bar:NAM13 from: -15.97 till: 0 text: Notoscopelus color:miocene bar:NAM14 from: -15.97 till: 0 text: Benthosema color:miocene bar:NAM15 from: -11.608 till: 0 text: Myctophum color:miocene bar:NAM16 from: -11.608 till: 0 text: Lampichthyes color:miocene bar:NAM17 from: -11.608 till: 0 text: Lampanyctodes color:miocene bar:NAM18 from: -11.608 till: 0 text: Electrona color:pliocene bar:NAM19 from: -5.332 till: 0 text: Triphoturus color:pliocene bar:NAM20 from: -5.332 till: 0 text: Tarletonbeania color:pliocene bar:NAM21 from: -5.332 till: 0 text: Stenobrachius color:pliocene bar:NAM22 from: -5.332 till: 0 text: Scopelopsis color:pliocene bar:NAM23 from: -5.332 till: 0 text: Protomyctophum color:pliocene bar:NAM24 from: -5.332 till: 0 text: Parvilux color:pliocene bar:NAM25 from: -5.332 till: 0 text: Lampadena color:pliocene bar:NAM26 from: -5.332 till: 0 text: Gymnoscopelus color:pliocene bar:NAM27 from: -5.332 till: 0 text: Ceratoscopelus PlotData= align:center textcolor:black fontsize:M mark:(line,black) width:25 bar:period from: -145.5 till: -99.6 color:earlycretaceous text: Early from: -99.6 till: -65.5 color:latecretaceous text: Late from: -65.5 till: -55.8 color:paleocene text: Paleo. from: -55.8 till: -33.9 color:eocene text: Eo. from: -33.9 till: -23.03 color:oligocene text: Oligo. from: -23.03 till: -5.332 color:miocene text: Mio. from: -5.332 till: -2.588 color:pliocene text: Pl. from: -2.588 till: -0.0117 color:pleistocene text: Pl. from: -0.0117 till: 0 color:holocene text: H. bar:era from: -145.5 till: -65.5 color:cretaceous text:
Cretaceous The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ...
from: -65.5 till: -23.03 color:paleogene text: Paleogene from: -23.03 till: -2.588 color:neogene text:
Neogene The Neogene ( ,) is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period million years ago ( Mya) to the beginning of the present Quaternary Period million years ago. It is the second period of th ...
from: -2.588 till: 0 color:quaternary text: Q.


Footnotes


References

* (2008): On the cephalic and pectoral girdle muscles of the deep sea fish ''Alepocephalus rostratus'', with comments on the functional morphology and phylogenetic relationships of the Alepocephaloidei (Teleostei). '' Anim. Biol.'' 58(1): 23–29. * (2006)
Order Myctophiformes
Version of 2006-OCT-09. Retrieved 2009-SEP-28. * (1968–1982): ''
Oxford Latin Dictionary The ''Oxford Latin Dictionary'' (or ''OLD'') is the standard English lexicon of Classical Latin, compiled from sources written before AD 200. Begun in 1933, it was published in fascicles between 1968 and 1982; a lightly revised second edition ...
'' (1st ed.). Oxford University Press, Oxford. * (2006): '' Fishes of the World'' (4th ed.). John Wiley & Sons, Inc. * (1910): ''English-Greek Dictionary - A Vocabulary of the Attic Language''. George Routledge & Sons Ltd., Broadway House, Ludgate Hill, E.C
Searchable JPEG fulltext
* {{Authority control Deep sea fish Ray-finned fish orders Extant Cenomanian first appearances