- Prehistoric fish
Prehistoric fish are various groups of
fish es that lived before recordedhistory . A few, such as thecoelacanth still exist today and are consideredliving fossil s.The first fish and the first
vertebrate s, were theostracoderms , which appeared in theCambrian Period, about 510 million years ago, and becameextinct at the end of theDevonian , about 350 million years ago. Ostracoderms were jawless fishes found mainly in fresh water. They were covered with a bonyarmor or scales and were often less than 30 cm (1 ft) long. The ostracoderms are placed in the classAgnatha along with the living jawless fishes, thelamprey s andhagfish es, which are believed to be descended from the ostracoderms.The first fish with jaws, the acanthodians, or spiny
shark s, appeared in the lateSilurian , about 410 million years ago, and became extinct before the end of thePermian , about 250 million years ago. Acanthodians were generally small sharklike fishes varying from toothless filter-feeders to toothedpredator s. They were once often classified as an order of the classPlacodermi , another group of primitive fishes, but recent authorities tend to place the acanthodiaes or that both groups share a commonancestor .The
placoderm s, another group of jawed fishes, appeared at the beginning of theDevonian , about 395 million years ago, and became extinct at the end of theDevonian or the beginning of theMississippian (Carboniferous ), about 345 million years ago. Detailed anatomical studies of fossil remains by the Swedish scientistErik Stensiö strongly suggest that the placoderms were closely related to sharks. Placoderms were typically small, flattened bottom-dwellers, however, many, particularly the arthrodires, were active midwater predators. "Dunkleosteus " was the largest and most famous of these. The upper jaw was firmly fused to the skull, but there was a hinge joint between the skull and the bony plating of the trunk region. This allowed the upper part of the head to be thrown back, and in arthrodires, this allowed them to take larger bites.The cartilaginous-skeleton
shark s and rays, classChondrichthyes , which appeared about 370 million years ago in the middleDevonian , are generally believed to be descended from the bony-skeleton placoderms. The cartilaginous skeletons are considered to be a later development.The modern bony fishes, class
Osteichthyes , appeared in the lateSilurian or earlyDevonian , about 395 million years ago. The early forms were freshwater fishes, for no fossil remains of modern bony fishes have been found in marine deposits older thanTriassic time, about 230 million years ago. The Osteichthyes may have arisen from the acanthodians. A subclass of the Osteichthyes, the ray-finned fishes (subclassActinopterygii ), became and have remained the dominant group of fishes throughout the world. It was not the ray-finned fishes, however, that led to the evolution of the land vertebrates.The ancestors of the land vertebrates are found among another group of bony fishes called the
Choanichthyes orSarcopterygii .Choanate fish es are characterized by internal nostrils, fleshy fins called lobe fins, and cosmoid scales. The choanate fishes appeared in the lateSilurian or earlyDevonian , more than 390 million years ago, and possibly arose from the acanthodians. The choanate fishes include a group known as theCrossopterygii , which has one living representative, thecoelacanth (Latimeria ). During theDevonian Period some crossopterygian fishes of the order (or suborder)Rhipidistia crawled out of the water to become the firsttetrapods .The story of vertebrate evolution started in the seas of the
Cambrian period, when jawless, toothless, soft-bodied fishlike creatures wriggled through the water, sucking up microscopic food particles. Only after tough, non-decaying bone was developed (initially as a scaly outer covering and later within the body) didfossil s form and become preserved in the rocks. And only then couldpaleontologist s take up the story with any certainty.The earliest traces of bony scales are found in rocks of the Late
Cambrian period, and the first recognizable vertebrate fish has been found inAustralia n rocks of EarlyOrdovician age. So, the first chapter in the vertebrate evolution starts with the ancient "Arandaspis ", a fish about 6in/15cm long with no jaws, no teeth and no fins other than a tail. It did, however, have gills and a stiffening rod of cartilaginous material (thenotochord ) that served as a backbone.Groups of various prehistoric fishes include:
Jawless fish
*"
Arandaspis "
*"Astraspis "
*"Boreaspis "
*"Dartmuthia "
*"Doryaspis "
*"Drepanaspis "
*"Errivaspis "
*"Haikouichthys "
*"Hemicyclaspis "
*"Jamoytius "
*"Myllokunmingia "
*"Pikaia "
*"Pharyngolepis "
*"Promissum "
*"Pteraspis "
*"Thelodus "
*"Tremataspis "Cartilaginous fish
*"
Cladoselache "
*"Cobelodus "
*"Deltoptychius "
*"Heliobatis "
*"Hybodus "
*"Ischyodus "
*"Scapanorhynchus "
*"Sclerorhynchus "
*"Spathobathis "
*"Stethacanthus "
*"Tristychius "
*"Xenacanthus "harks and placoderms
*"
Bothriolepis "
*"Cladoselache "
*"Coccosteus "
*"Ctenurella "
*"Dunkleosteus "
*"Gemuendina "
*"Groenlandaspis "
*Megalodon orMegatooth shark
*"Ostracoderm "
*"Palaeospondylus "
*"Pterichthyodes "
*"Squalicorax "
*"Otodus obliquus "Primitive ray-finned fish
*"
Aspidorhynchus "
*"Canobius "
*"Cheirolepis "
*"Dapedium "
*"Lepidotes "
*"Moythomasia "
*"Palaeoniscum "
*"Perleidus "
*"Platysomus "
*"Pycnodus "
*"Saurichthys "
*"Semionotus "Modern ray-finned fish
*"
Berycopsis "
*"Enchodus "
*"Eobothus "
*"Gryouchus "
*"Gyrosteus "
*"Hypsidoris "
*"Hypsocormus "
*"Knightia "
*"Leptolepis "
*"Pholidophorus "
*"Protobrama "
*"Sphenocephalus "
*"Thrissops "Fleshy-lobed fish
* "
Chinlia "
* "Dipnorhynchus "
* "Dipterus "
* "Eusthenopteron "
* "Griphognathus "
* "Gyroptychius "
* "Holoptychius "
* "Macropoma "
* "Osteolepsis "
* "Strunius "See also
*
Prehistoric life References
* Janvier, Philippe. Early Vertebrates Oxford, New York: Oxford University Press, 1998. ISBN 0-19-854047-7
* Long, John A. The Rise of Fishes: 500 Million Years of Evolution Baltimore: The Johns Hopkins University Press, 1996. ISBN 0-8018-5438-5
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