Perciformes, also called the Acanthopteri, is an order or superorder of ray-finned fish in the clade Percomorpha. Perciformes means "perch-like". Among the well-known members of this group are perches and darters (Percidae), and also sea basses and groupers (Serranidae).
Lepisosteus is a genus of gars in the family Lepisosteidae. It contains four extant species, found throughout eastern and central North America. It is one of two extant gar genera alongside Atractosteus.
Ichthyornis is an extinct genus of toothy seabird-like ornithuran from the late Cretaceous period of North America. Its fossil remains are known from the chalks of Alberta, Alabama, Kansas, New Mexico, Saskatchewan, and Texas, in strata that were laid down in the Western Interior Seaway during the Turonian through Campanian ages, about 95–83.5 million years ago. Ichthyornis is a common component of the Niobrara Formation fauna, and numerous specimens have been found.
Polarornis is a genus of prehistoric bird, possibly an anserimorph. It contains a single species Polarornis gregorii, known from incomplete remains of one individual found on Seymour Island, Antarctica, in rocks which are dated to the Late Cretaceous.
Acanthomorpha is an extraordinarily diverse taxon of teleost fishes with spiny fin rays. The clade contains about one-third of the world's modern species of vertebrates: over 14,000 species.
Mawsonia is an extinct genus of prehistoric coelacanth fish. It is amongst the largest of all coelacanths, with one quadrate specimen possibly belonging to an individual measuring 5.3 metres in length. It lived in freshwater and brackish environments from the late Jurassic to the mid-Cretaceous of South America, eastern North America, and Africa. Mawsonia was first described by British paleontologist Arthur Smith Woodward in 1907.
Eomuraena is an extinct genus of prehistoric marine moray eel that lived during the lower Eocene, with potential Late Cretaceous records also known. It contains a single species, E. sagittidens.
Stromerichthys is an extinct genus of potentially chimaeric freshwater bony fish that lived during the Late Cretaceous epoch. It contains a single species, S. aethiopicus, described from a now-lost specimen with bones & scales from Egypt.
Eolamprogrammus is an extinct genus of prehistoric marine cusk-eel that lived during the earliest Eocene. It contains a single species, E. senectus from the earliest Ypresian-aged Danata Formation of Turkmenistan. It may potentially represent an early member of the Neobythitinae.
Callipteryx is an extinct genus of prehistoric marine percomorph fish that lived during the early Eocene. It is the only known member of the extinct family Callipterygidae. It contains a single species, C. speciosus, known from the famous Monte Bolca site of Italy.
Properca is an extinct genus of marine percomorph ray-finned fish that lived in Europe throughout much of the Cenozoic, from the Paleocene to the Miocene epochs.
Cretatriacanthus is an extinct genus of prehistoric marine ray-finned fish from the Late Cretaceous. It contains a single species, C. guidottii from the late Campanian or early Maastrichtian of Nardò, Italy. It is generally placed as a basal tetraodontiform, although more recent studies have disputed this, finding it to instead represent an early basal percomorph.
Diaphyodus is an extinct genus of prehistoric marine ray-finned fish, generally considered a drumfish, from the Late Paleocene and Eocene, and potentially to the mid-Oligocene of Europe and North America.
Cylindracanthus is an extinct, enigmatic genus of marine ray-finned fish with fossils known throughout North America, Europe, Asia and Africa from the Late Cretaceous to the late Eocene, with potential Oligocene records and a possible Miocene record also known. It is exclusively known from its distinctive partial remains, which are long cylindrical bony spines that are usually considered rostrum fragments, as well as some associated teeth. These spines are abundant & widespread throughout this timespan, and are useful indicators of a nearshore marine environment, but the taxonomic identity of the fish is still highly uncertain and debated.
Egertonia is an extinct genus of prehistoric marine and estuarine ray-finned fish known from the Late Cretaceous to the middle Eocene. It contains one known species, E. isodonta, although indeterminate remains potentially referable to other species are also known. It was a member of the Phyllodontidae, an extinct family of elopomorph fish with crushing tooth plates, which are the primary remains found of the genus.
Elopoides is an extinct genus of prehistoric marine ray-finned fish known from the Early Cretaceous of Europe. It contains a single species, E. tomassoni, known from the late Albian of Aube, France. It is thought to be a stem-group megalopid, making it closely related to modern tarpons.
The Intertrappean Beds are a Late Cretaceous and early Paleogene geologic unit in India. These beds are found as interbeds between Deccan Traps layers, including the slightly older Lameta Formation. They consist a number of different subgroups and formations, and span the Cretaceous–Paleogene boundary.
Egg fossils are the fossilized remains of eggs laid by ancient animals. As evidence of the physiological processes of an animal, egg fossils are considered a type of trace fossil. Under rare circumstances a fossil egg may preserve the remains of the once-developing embryo inside, in which case it also contains body fossils. A wide variety of different animal groups laid eggs that are now preserved in the fossil record beginning in the Paleozoic. Examples include invertebrates like ammonoids as well as vertebrates like fishes, possible amphibians, and reptiles. The latter group includes the many dinosaur eggs that have been recovered from Mesozoic strata. Since the organism responsible for laying any given egg fossil is frequently unknown, scientists classify eggs using a parallel system of taxonomy separate from but modeled after the Linnaean system. This "parataxonomy" is called veterovata.
Percomorpha is a large clade of ray-finned fish with more than 17 000 known species that includes the tuna, seahorses, gobies, cichlids, flatfish, wrasse, perches, anglerfish, and pufferfish.
Lepisosteusindicus, the Indian gar, is an extinct species of gar known from the Late Cretaceous (Maastrichtian) and early Paleocene of India. It is known from a single articulated but poorly-preserved skull and a lost set of vertebrae from the Lameta Formation, in addition to numerous isolated scales and teeth from the Lameta Formation and Intertrappean Beds.
