Schistura Quaesita
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Schistura Quaesita
''Schistura quaesita'' is a species of ray-finned fish, a stone loach, in the genus ''Schistura''. It has only been recorded from a single locality in the Nam Ngum drainage in Laos where it was seen in streams with a moderate to fast flow, among riffle A riffle is a shallow landform in a flowing channel. Colloquially, it is a shallow place in a river where water flows quickly past rocks. However, in geology a riffle has specific characteristics. Topographic, sedimentary and hydraulic indica ...s, over beds made up of gravel or stone. References Q Fish described in 2000 {{Nemacheilidae-stub ...
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Maurice Kottelat
Maurice Kottelat (born 16 July 1957 in Delémont, SwitzerlandCommissioners: Dr Maurice Kottelat
International Commission on Zoological Nomenclature (accessed 2014)
) is a specializing in Eurasian freshwater fishes. Kottelat obtained a License in Sciences at the University of Neuchâtel in 1987 and in 1989 a doctoral degree from the

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Ray-finned Fish
Actinopterygii (; ), members of which are known as ray-finned fish or actinopterygians, is a class of bony fish that comprise over 50% of living vertebrate species. They are so called because of their lightly built fins made of webbings of skin supported by radially extended thin bony spines called '' lepidotrichia'', as opposed to the bulkier, fleshy lobed fins of the sister clade Sarcopterygii (lobe-finned fish). Resembling folding fans, the actinopterygian fins can easily change shape and wetted area, providing superior thrust-to-weight ratios per movement compared to sarcopterygian and chondrichthyian fins. The fin rays attach directly to the proximal or basal skeletal elements, the radials, which represent the articulation between these fins and the internal skeleton (e.g., pelvic and pectoral girdles). The vast majority of actinopterygians are teleosts. By species count, they dominate the subphylum Vertebrata, and constitute nearly 99% of the over 30,000 extant ...
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Nemacheilidae
The Nemacheilidae, or stone loaches, are a family of cypriniform fishes that inhabit stream environments, mostly in Eurasia, with one genus, ''Afronemacheilus'' found in Africa Africa is the world's second-largest and second-most populous continent after Asia. At about 30.3 million km2 (11.7 million square miles) including adjacent islands, it covers 20% of Earth's land area and 6% of its total surfac .... The family includes about 790 species. Genera The following are the described genera of the family: References Taxa named by Charles Tate Regan Cypriniformes families {{Nemacheilidae-stub ...
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Schistura
''Schistura'' is a genus of fish in the stone loach family Nemacheilidae native to the streams and rivers of the southern and eastern Asia. Some of these species are troglobitic. Species There are currently over 200 recognized species in this genus: * '' Schistura absumbra'' ( Endruweit, 2017) * '' Schistura acuticephala'' ( Hora, 1929) * '' Schistura afasciata'' Mirza & Bănărescu, 1981 * '' Schistura aizawlensis'' Lal Ramliana, 2012 * '' Schistura albirostris'' X. Y. Chen & Neely, 2012 * '' Schistura albisella'' Kottelat, 2017 * '' Schistura alboguttata'' Cao & E. Zhang, 2018 * '' Schistura alticrista'' Kottelat, 1990 * '' Schistura altipedunculata'' ( Bănărescu & Nalbant, 1968) * '' Schistura altuscauda'' F.-M. Chen, Myint, L. Chu & X. Y. Chen, 2020 * '' Schistura amplizona'' Kottelat, 2000 * '' Schistura anambarensis'' ( Mirza & Bănărescu, 1970) * '' Schistura andrewi'' Solo, Lal Ramliana, Lalronunga & Lalnun Tluanga, 2014 * '' Schistura antennata'' Freyh ...
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Riffle
A riffle is a shallow landform in a flowing channel. Colloquially, it is a shallow place in a river where water flows quickly past rocks. However, in geology a riffle has specific characteristics. Topographic, sedimentary and hydraulic indicators Riffles are almost always found to have a very low discharge compared to the flow that fills the channel (approximately 10–20%), and as a result the water moving over a riffle appears shallow and fast, with a wavy, disturbed water surface. The water's surface over a riffle at low flow also has a much steeper slope than that over other in-channel landforms. Channel sections with a mean water surface slope of roughly 0.1 to 0.5% exhibit riffles, though they can occur in steeper or gentler sloping channels with coarser or finer bed materials, respectively. Except in the period after a flood (when fresh material is deposited on a riffle), the sediment on the riverbed in a riffle is usually much coarser than on that in any other in-chan ...
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