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Retropinnidae

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The Retropinnidae are a family of bony fishes that contains the Southern Hemisphere smelts and graylings. They are the only members of the suborder Retropinnoidei. They are closely related to the northern smelts (Osmeroidei), which they greatly resemble, but not to the northern graylings (Thymallus). Species from this family are only found in southeastern Australia and New Zealand, although a fossil otolith suggests that they may have also inhabited southern South America during the Neogene.

OsmeriformesOsmeriformesThe Osmeriformes are an order of ray-finned fish that includes the true or freshwater smelts and allies, such as the noodlefishes; they are also collectively called osmeriforms. They belong to the teleostsuperorderProtacanthopterygii, which also includes pike and salmon, among others. The order's name means "smelt-shaped", from Osmerus (the type genus) + the standard fish order suffix "-formes".ThymallusThymallusThymallus, commonly known as graylings, is a genus of freshwaterray-finned fish and the only genus within the subfamilyThymallinae of the familySalmonidae. Although all Thymallus species can be generically called graylings, without specific qualification the term "grayling" typically refers to the type speciesThymallus thymallus, the European grayling.GalaxiidaeGalaxiidaeThe Galaxiidae are a family of mostly small freshwater fish in the Southern Hemisphere. The majority live in Southern Australia or New Zealand, but some are found in South Africa, southern South America, Lord Howe Island, New Caledonia, and the Falkland Islands. One galaxiid species, the common galaxias (Galaxias maculatus), is probably the most widely naturally distributed freshwater fish in the Southern Hemisphere.Family (taxonomy)Family (taxonomy)Family (Latin: familia, pl.: familiae) is one of the eight major hierarchical taxonomic ranks in Linnaean taxonomy. It is classified between order and genus. A family may be divided into subfamilies, which are intermediate ranks between the ranks of family and genus.AustraliaAustraliaCountry in OceaniaAustralia, officially the Commonwealth of Australia, is a country comprising the mainland of the Australian continent, the island of Tasmania and numerous smaller islands. It has a land area of 7,688,287 km (2,968,464 sq mi), making it the sixth-largest country in the world, and is the world's flattest and driest inhabited continent.Brackish waterBrackish waterBrackish water, sometimes termed brack water, is water occurring in a natural environment that has more salinity than freshwater, but not as much as seawater. It may result from mixing seawater (salt water) and fresh water, as in estuaries, or it may occur in brackish fossil aquifers. The word comes from the Middle Dutch root .New ZealandNew ZealandNew Zealand is an island country in the southwestern Pacific Ocean. It comprises two main landmasses—the North Island (Te Ika-a-Māui) and the South Island (Te Waipounamu)—and over 700 smaller islands. It is the sixth-largest island country by area and lies east of Australia across the Tasman Sea and south of the islands of New Caledonia, Fiji, and Tonga.Fresh waterFresh waterFresh water or freshwater is any naturally occurring liquid or frozen water containing low concentrations of dissolved salts and other total dissolved solids. The term excludes seawater and brackish water, but it does include non-salty mineral-rich waters, such as chalybeate springs.Saline waterSaline waterSaline water (more commonly known as salt water) is water that contains a high concentration of dissolvedsalts (mainly sodium chloride). On the United States Geological Survey (USGS) salinity scale, saline water is saltier than brackish water, but less salty than brine. The salt concentration is usually expressed in parts per thousand (permille, ‰) and parts per million (ppm). The USGS salinity scale defines three levels of saline water.NeogeneNeogeneThe Neogene ( NEE-ə-jeen) is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period 23.04 Ma (million years ago) to the beginning of the present Quaternary Period 2.58 Ma. It is the second period of the Cenozoic and the eleventh period of the Phanerozoic. The Neogene is sub-divided into two epochs, the earlier Miocene and the later Pliocene.OtolithOtolithAn otolith (Ancient Greek: ὠτο-, ōto- ear + λῐ́θος, líthos, a stone), also called otoconium, statolith, or statoconium, is a calcium carbonate structure in the saccule or utricle of the inner ear, specifically in the vestibular system of vertebrates. The saccule and utricle, in turn, together make the otolith organs. These organs are what allows an organism, including humans, to perceive linear acceleration, both horizontally and vertically (gravity).OsteichthyesOsteichthyesOsteichthyes ( ; from Ancient Greek (ostéon)'bone' and (ikhthús)'fish'), also known as osteichthyans or commonly referred to as the bony fish, is a diverseclade of vertebrateanimals that have endoskeletons primarily composed of bone tissue, encompassing both the conventional bony fishes and, in a cladistic sense, all tetrapods, including mammals and reptiles.

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