The Moronidae are a family of
perciform
Perciformes (), also called the Percomorpha or Acanthopteri, is an order (biology), order or superorder of Actinopterygii, ray-finned fish. If considered a single order, they are the most numerous order of vertebrates, containing about 41% of a ...
fish
Fish are aquatic, craniate, gill-bearing animals that lack limbs with digits. Included in this definition are the living hagfish, lampreys, and cartilaginous and bony fish as well as various extinct related groups. Approximately 95% of li ...
es, commonly called the temperate basses, consisting of at least six freshwater, brackish water, and marine species. Many members of this family are anadromous.
Description
These fishes reach 45 cm to one meter long and silvery in colour, with seven or eight longitudinal stripes on the flanks. The body is moderately elongated, and somewhat flattened on the sides. The head and body are covered with large comb scales. They have two short spines on the gill cover. The gill cover is round and slightly sawn. The mouth is large, the maxillary is extended, and there is no supramaxillary. There are rows of small, conical teeth in the mouth. Special fangs are missing. The base of the tongue is also provided with two rows of small teeth, and there are teeth on the skull (vomer) and the palatine bone (palatine). The number of branchiostegal rays is seven. Of a total of 25 vertebrae, 12 are trunk vertebrae and 13 are tail vertebrae located behind the anus.
The
lateral line
The lateral line, also called the lateral line organ (LLO), is a system of sensory organs found in fish, used to detect movement, vibration, and pressure gradients in the surrounding water. The sensory ability is achieved via modified epithelial ...
organ is continuous and extends to the base of the caudal fin. It is accompanied by 50 to 72 pored scales. The swim bladder extends into a cavity of the first fin ray carrier (pterygiophore) of the anal fin.
The dorsal fin is clearly divided by an indentation. The last fin spine is in the second dorsal fin. The anal fin lies below or behind the soft-rayed part of the dorsal fin. The pectoral fins are small and asymmetrical, the upper rays are longer. The caudal fin is forked and heavily scaled at its base. It is supported by eight to nine fin rays, seven to eight of which are branched.
Fins formula: dorsal 1 VIII – X, dorsal 2 I / 10–13, anal III / 9–12, pectoral 15–18, ventral I / 5
Genera
The members of this family are most commonly found near the coastal regions of eastern
North America
North America is a continent in the Northern Hemisphere and almost entirely within the Western Hemisphere. It is bordered to the north by the Arctic Ocean, to the east by the Atlantic Ocean, to the southeast by South America and the Car ...
(including the
Gulf of Mexico
The Gulf of Mexico ( es, Golfo de México) is an oceanic basin, ocean basin and a marginal sea of the Atlantic Ocean, largely surrounded by the North American continent. It is bounded on the northeast, north and northwest by the Gulf Coast of ...
), northern
Africa
Africa is the world's second-largest and second-most populous continent, after Asia in both cases. At about 30.3 million km2 (11.7 million square miles) including adjacent islands, it covers 6% of Earth's total surface area ...
, and
Europe
Europe is a large peninsula conventionally considered a continent in its own right because of its great physical size and the weight of its history and traditions. Europe is also considered a Continent#Subcontinents, subcontinent of Eurasia ...
.
The family includes the genera ''
Morone
''Morone'' is a genus of temperate basses native to the Atlantic coast of North America and the freshwater systems of the southwestern and eastern United States
The United States of America (U.S.A. or USA), commonly known as the United ...
'' and''
Dicentrarchus
''Dicentrarchus'' is a genus of temperate basses native to the eastern Atlantic Ocean and the Mediterranean Sea
The Mediterranean Sea is a sea connected to the Atlantic Ocean, surrounded by the Mediterranean Basin and almost completely encl ...
''.
Asian seabasses, ''
Lateolabrax
''Lateolabrax'' is a genus of commercially important fishes known as the Asian seabasses. It is the only genus in the family Lateolabracidae. This genus is native to the coastal waters of the western Pacific Ocean. This genus has also been in ...
'' spp., are sometimes
[ placed in this family instead of their own family, the ]Lateolabracidae
''Lateolabrax'' is a genus of commercially important fishes known as the Asian seabasses. It is the only genus in the family Lateolabracidae. This genus is native to the coastal waters of the western Pacific Ocean. This genus has also been in ...
; this would increase the species number of this family to eight.
They are highly prized as sport fish
Game fish, sport fish or quarry refer to popular fish pursued by recreational anglers, and can be freshwater or saltwater fish
Saltwater fish, also called marine fish or sea fish, are fish that live in seawater. Saltwater fish can swim and live ...
.
Timeline
ImageSize = width:1000px height:auto barincrement:15px
PlotArea = left:10px bottom:50px top:10px right:10px
Period = from:-65.5 till:10
TimeAxis = orientation:horizontal
ScaleMajor = unit:year increment:5 start:-65.5
ScaleMinor = unit:year increment:1 start:-65.5
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: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: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: -65.5 till: -55.8 color:paleocene text:Paleocene
The Paleocene, ( ) or Palaeocene, is a geological epoch (geology), epoch that lasted from about 66 to 56 mya (unit), million years ago (mya). It is the first epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), E ...
from: -55.8 till: -33.9 color:eocene text:Eocene
The Eocene ( ) Epoch is a geological epoch (geology), epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name ''Eocene' ...
from: -33.9 till: -23.03 color:oligocene text:Oligocene
The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified but the ...
from: -23.03 till: -5.332 color:miocene text:Miocene
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recen ...
from: -5.332 till: -2.588 color:pliocene text: Plio.
from: -2.588 till: -0.0117 color:pleistocene text:Pleist.
The Pleistocene ( , often referred to as the ''Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in ...
from: -0.0117 till: 0 color:holocene text: H.
bar:eratop
from: -65.5 till: -23.03 color:paleogene text:Paleogene
The Paleogene ( ; British English, also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period, geologic period and system that spans 43 million years from the end of the Cretaceous Period million yea ...
from: -23.03 till: -2.588 color:neogene text:Neogene
The Neogene ( ), informally Upper Tertiary or Late Tertiary, 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 Mya. ...
from: -2.588 till: 0 color:quaternary text: Q.
PlotData=
align:left fontsize:M mark:(line,white) width:5 anchor:till align:left
color:eocene bar:NAM1 from: -55.8 till: 0 text: Morone
''Morone'' is a genus of temperate basses native to the Atlantic coast of North America and the freshwater systems of the southwestern and eastern United States
The United States of America (U.S.A. or USA), commonly known as the United ...
PlotData=
align:center textcolor:black fontsize:M mark:(line,black) width:25
bar:period
from: -65.5 till: -55.8 color:paleocene text:Paleocene
The Paleocene, ( ) or Palaeocene, is a geological epoch (geology), epoch that lasted from about 66 to 56 mya (unit), million years ago (mya). It is the first epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), E ...
from: -55.8 till: -33.9 color:eocene text:Eocene
The Eocene ( ) Epoch is a geological epoch (geology), epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name ''Eocene' ...
from: -33.9 till: -23.03 color:oligocene text:Oligocene
The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified but the ...
from: -23.03 till: -5.332 color:miocene text:Miocene
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recen ...
from: -5.332 till: -2.588 color:pliocene text: Plio.
from: -2.588 till: -0.0117 color:pleistocene text:Pleist.
The Pleistocene ( , often referred to as the ''Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in ...
from: -0.0117 till: 0 color:holocene text: H.
bar:era
from: -65.5 till: -23.03 color:paleogene text:Paleogene
The Paleogene ( ; British English, also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period, geologic period and system that spans 43 million years from the end of the Cretaceous Period million yea ...
from: -23.03 till: -2.588 color:neogene text:Neogene
The Neogene ( ), informally Upper Tertiary or Late Tertiary, 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 Mya. ...
from: -2.588 till: 0 color:quaternary text: Q.
References
Percoidei
Ray-finned fish families
{{Percoidea-stub