Anguilla anguilla |
Sargasso Sea |
No category |
Deelder, 1970 |
Anguilla anguilla |
Sargasso Sea [Larvae hatch in region with low current] |
Flowing or turbulent water |
Bruslé and Quignard, 2001 |
Anguilla anguilla |
Sargasso sea |
No category |
Vollestad and Jonsson, 1986 |
Anguilla anguilla |
Fish spawning out of the tributary area: carp, pikeperch, catfish Silurus glanis and eel |
No category |
Hladik and Kubecka, 2003 |
Alosa alosa |
Rapid current |
Flowing or turbulent water |
Billard, 1997 |
Alosa alosa |
Quite rapid current |
Flowing or turbulent water |
Bruslé and Quignard, 2001 |
Alosa alosa |
Rapid current |
Flowing or turbulent water |
Spillmann, 1961 |
Alosa alosa |
Chiefly 50-100 m wide, with water current of 0.9-2 m/s |
Flowing or turbulent water |
Cassou-Leins et al, 2000 |
Alosa alosa |
Streams, water with current |
Flowing or turbulent water |
Bengen et al, 1991 |
Alosa alosa |
In flowing water |
Flowing or turbulent water |
Maitland and Hatton-Ellis, 2000 |
Alosa alosa |
Current ranges from 0.5-1.5 m/s, they show a preference for spawning in swift currents at the ends of pools where gravelly shallows begin [Unlike salmonids, shads do not enter narrow streams even when these are accessible] |
Flowing or turbulent water |
Maitland and Hatton-Ellis, 2000 |
Alosa alosa |
Water with current, 0.45 to 0.90 m/sec |
Flowing or turbulent water |
Boisneau et al, 1990 |
Alosa alosa |
Water ccurent about 1m/s |
Flowing or turbulent water |
Belaud et al, 2001 |
Alosa alosa |
Water with current |
Flowing or turbulent water |
Bensettiti and Gaudillat, 2002 |
Alosa alosa |
Water flows observed during spawning period over the three years varied between 2.7 and 47.6 m3 s-1. In 2001 and 2002, current surface speeds ranged between 0.1 and 1.5 m s-1. |
Flowing or turbulent water |
Acolas et al, 2006 |
Alosa fallax |
Turbide water |
No category |
Bruslé and Quignard, 2001 |
Alosa fallax |
Chiefly 50-100 m wide, with water current of 0.9-2 m/s, also in estuaries |
Flowing or turbulent water |
Cassou-Leins et al, 2000 |
Alosa fallax |
With constant current |
Flowing or turbulent water |
Spillmann, 1961 |
Alosa fallax |
Lower reaches of the large accessible rivers along the coasts |
No category |
Maitland and Lyle, 2005 |
Alosa fallax |
Upper tidal limit of the River |
No category |
Doherty et al, 2004 |
Alosa fallax |
A river where current is fast enough |
Flowing or turbulent water |
Doherty et al, 2004 |
Alosa fallax |
Flowing water |
Flowing or turbulent water |
Maitland and Hatton-Ellis, 2000 |
Alosa fallax |
Occurs in fresh water |
No category |
Aprahamian et al, 2001 |
Alosa fallax |
Unlike salmonids, shads do not enter narrow streams even when these are accessible |
No category |
Maitland and Hatton-Ellis, 2000 |
Alosa fallax |
Riffle areas, current generally described as "fast-flowing" |
Flowing or turbulent water |
Maitland and Hatton-Ellis, 2000 |
Alosa fallax |
Enter the lower and middle rivers to spawn. Ebro River characterized by laminar fast flow areas |
No category |
Lopez et al, 2007 |
Alosa fallax |
In this study, eggs, embryos and larvae of Twaite shad were only found in the upstream, riverine stations located close to the upper boundary of estuarine influence and the vicinity of the suspected spawning grounds in the River Mira |
No category |
Esteves and Andrade, 2008 |
Alosa sapidissima |
Concentrated near the shore, main channel [Freshwater, possibly brackish water] |
Stagnant water |
Internet, 2005 |
Alosa sapidissima |
Rarely if ever in lakes |
Stagnant water |
Scott and Crossman, 1973 |
Alosa sapidissima |
Freshwater of moderate current |
Flowing or turbulent water |
Everly and Boreman, 1999 |
Alosa sapidissima |
In the main channels of rivers, preferred moderate current for spawning, about 0.3-0.93 or 0.15-0.61 m/s |
Flowing or turbulent water |
Mills, 2004 |
Alosa sapidissima |
Primarily in tidal or sometimes in non-tidal freshwater |
No category |
Rue, 2001 |
Alosa sapidissima |
in their native coastal habitats, alewifes spawn in the upper reaches of coastal rivers, in slow-flowing sections of slightly brackish or freshwater. |
Flowing or turbulent water |
Anonymous, 2006 Chapter 3 |
Alosa sapidissima |
Spawn in rivers or brackish estuarine rivers, seldom if ever in lakes [River spawning usually takes place in moderate to strong flowing water, generally where there is sufficient velocity to eliminate silt deposits, and at the same time, far enough upstream for eggs to drift and hatch before reaching saltwater] |
Stagnant water |
Bradbury et al, 1999 |
Alosa sapidissima |
Spawning occurs in open water beyond tidal influence |
No category |
Zydlewski and McCormick, 1997 |
Alosa sapidissima |
Current velocities ranged from 0.5 to 2 ft/sec. |
Flowing or turbulent water |
Marcy, 1972 |
Alosa sapidissima |
American shad choose either tributary and spawn in upsream segments characterized by shallow depths, high dissoled oxygen,and relatively high currents |
Flowing or turbulent water |
Olney et al, 2006 |
Barbatula barbatula |
Low productivity streams or high productivity environments |
No category |
Fishbase, 2006 |
Barbatula barbatula |
Well oxygenated |
Flowing or turbulent water |
Losange, 1999 |
Barbatula barbatula |
[In three successive years, fish in aquarium, in which the water was still, did not spawn; but a circular concrete ponds out of doors supplied with water from jets set at an angle so that the water in the pond was continually moving |
Stagnant water |
Smyly, 1955 |
Cobitis taenia |
Slow-flowing or stagnant places with rich vegetation |
Stagnant water |
Vaino and Saat, 2003 |
Cobitis taenia |
Well-oxygenated |
Flowing or turbulent water |
Billard, 1997 |
Cobitis taenia |
Slow to still water |
Stagnant water |
Coad, 2006 |
Cobitis taenia |
Flowing water |
Flowing or turbulent water |
Fishbase, 2006 |
Cobitis taenia |
Water with current |
Flowing or turbulent water |
Bensettiti and Gaudillat, 2002 |
Cobitis taenia |
No eggs were found in the belt of rough detritus, which indicates a preference of vegetation in water of medium depth rather than detritus in shallow water by the spawning fish |
Stagnant water |
Bohlen, 2003 |
Blicca bjoerkna |
Oxbows, rich in vegetation but return to the river after spawning |
Stagnant water |
Molls, 1999 |
Blicca bjoerkna |
Some species seem to be strickly dependent on the tributary zone as they were never observed reproducing in the reservoir (asp, bleak, chub and white bream), while others are facultative tributary users (roach, bream, pike, perch, rudd). |
No category |
Hladik and Kubecka, 2003 |
Blicca bjoerkna |
Spawning grounds of white bream in Estonia are usually shallow water areas among roots of reed and rush, lifted by the ice. |
No category |
Vetemaa et al, 2008 |
Abramis brama |
In border of river [current about 30 cm/s] |
Flowing or turbulent water |
Bruslé and Quignard, 2001 |
Abramis brama |
Typical spawning sites are temporarily flooded water bodies, low-floodplains and lakes |
Stagnant water |
Sidorova, 2005 |
Abramis brama |
Near the shoreline |
Stagnant water |
Spillmann, 1961 |
Abramis brama |
Weed beds |
Stagnant water |
Internet, 2005 |
Abramis brama |
In border of river |
No category |
Olivier, 2001 |
Abramis brama |
Sheltered places, where the water is either still or the current is weak |
Flowing or turbulent water |
Backiel and Zawiska, 1968 |
Abramis brama |
Oxbows, with vegetation adults remain in that site after spawning |
Stagnant water |
Molls, 1999 |
Abramis brama |
Current velocity < 20 cm/s |
Flowing or turbulent water |
Mann, 1996 |
Abramis brama |
Some species seem to be strickly dependent on the tributary zone as they were never observed reproducing in the reservoir (asp, bleak, chub and white bream), while others are facultative tributary users (roach, bream, pike, perch, rudd). Generalists: fish spawning in suitable places both inthe tributary and the reservoir: bream, roach, perh, pike and ruffe |
No category |
Hladik and Kubecka, 2003 |
Abramis brama |
Consist of shallow areas, overgrown with vegetation and protected from winds, or old river beds connected with the main course, river mouths areas, lake shores. May also spawn on flooded meadows. |
Stagnant water |
Brylinska and Boron, 2004 |
Abramis brama |
Spawning grounds of bream in Estonia as relatively shallow places on water plants, e.g. dead Carex sp. |
Stagnant water |
Vetemaa et al, 2008 |
Abramis brama |
The spawning grounds of A. brama are the shallow waters of the lake where there is dense vegetation |
Stagnant water |
Herzig and Winkler, 1986 |
Alburnoides bipunctatus |
Fast-flowing water |
Flowing or turbulent water |
Coad, 2005 |
Alburnoides bipunctatus |
Water with current |
Flowing or turbulent water |
Persat, 2001 |
Alburnoides bipunctatus |
Current velocity 20-50 cm/s |
Flowing or turbulent water |
Mann, 1996 |
Alburnoides bipunctatus |
This may indicate that this species uses the reservoir as a refuge for overwintering and the river for spawing and feeding during spring and summer |
No category |
Hladik and Kubecka, 2003 |
Alburnus alburnus |
Near the shoreline |
Stagnant water |
Spillmann, 1961 |
Alburnus alburnus |
Current velocity < 20 cm/s |
Flowing or turbulent water |
Mann, 1996 |
Alburnus alburnus |
Some species seem to be strickly dependent on the tributary zone as they were never observed reproducing in the reservoir (asp, bleak, chub and white bream), while others are facultative tributary users (roach, bream, pike, perch, rudd). |
No category |
Hladik and Kubecka, 2003 |
Alburnus alburnus |
The roe of the bleak (Alburnus alburnus L.) was collected on evenings from artificial substrate (small branches of juniper placed in spawning areas - between coastal reeds) at the depth of 20-30 cm |
No category |
Winnicki and Korzelecka, 1997 |
Aristichthys nobilis |
Spawning takes place after a sharp rise in the water level and current velocity |
Flowing or turbulent water |
Abdusamadov, 1986 |
Aristichthys nobilis |
Flowing water |
Flowing or turbulent water |
Mikodina and Makeyeva, 1981 |
Aristichthys nobilis |
Typically occurs ar river confluences or behind sandbars, gravels bars, and islands charcaterized by current faster then 0.8 m/s and turbulent flow |
Flowing or turbulent water |
Schrank et al, 2001 |
Aristichthys nobilis |
Primarily used low velocity habitats behind wing dikes |
Flowing or turbulent water |
Kolar et al, 2005 |
Aristichthys nobilis |
Rapid flowing (current velocity of 0.6-2.3 m/S) turbid water |
Flowing or turbulent water |
Kolar et al, 2005 |
Aristichthys nobilis |
Spawning grounds are usually located in river reaches characterized by turbulent or whirlpool-like flow, often in the vicinity of islands or stream junctions [Reported current velocities of spawning areas in China ranged from 0.33 to0.90m/s] |
Flowing or turbulent water |
Scholfield, 2005 |
Aristichthys nobilis |
Natural reproduction occurs in channel of large rivers in swift current where velocities exceed 0.8 m/sec [The spawning is generally deposited among the rocks of rapids in river channels, behind sandbars, and at islands at the junction of the currents] |
Flowing or turbulent water |
Jennigs, 1988 |
Aristichthys nobilis |
Spawning typically occurs at the confluence of two rivers, behind sanbars, stonebeds, or islands. These areas are characterized by rapid current (>0.8 m/s) and mixing of water |
Flowing or turbulent water |
Schrank, 1999 |
Aristichthys nobilis |
The existence and the persistence of the increasing water level, the water flow up to 3 m per second |
No category |
Ciolac, 2004 |
Aristichthys nobilis |
En effet, en Chine, les géniteurs sont placés dans des bassins frayères traversés par un courant d'eau continu dont la vitesse est comprise entre 30 et 60 m/s, qui a pour but de créer un facteur mécanique rappelant aux géniteurs leurs lieux de ponte naturelle |
Flowing or turbulent water |
Lloze, 1967 |
Aspius aspius |
Open sections of the lake with the greatest flow, more rarely in places weaklt overgrown with very coarse submerged vegetation (mainly reeds and rushes) |
Stagnant water |
Shikhshabekov, 1979 |
Aspius aspius |
After riffles |
No category |
Bruslé and Quignard, 2001 |
Aspius aspius |
Water with current |
Flowing or turbulent water |
Billard, 1997 |
Aspius aspius |
Water with strong current |
Flowing or turbulent water |
Keith and Allardi, 2001 |
Aspius aspius |
Water with strong current |
Flowing or turbulent water |
Bensettiti and Gaudillat, 2002 |
Aspius aspius |
Some species seem to be strickly dependent on the tributary zone as they were never observed reproducing in the reservoir (asp, bleak, chub and white bream), while others are facultative tributary users (roach, bream, pike, perch, rudd). |
No category |
Hladik and Kubecka, 2003 |
Barbus barbus |
Fast-flowing waters |
Flowing or turbulent water |
Philippart et al, 1989 |
Barbus barbus |
28-43 cm:s |
No category |
Bruslé and Quignard, 2001 |
Barbus barbus |
Water with current |
Flowing or turbulent water |
Philippart, 1987 |
Barbus barbus |
Clear, flowing |
Flowing or turbulent water |
Hancock et al, 1976 |
Barbus barbus |
Current velocity: 25-49 cm/s |
Flowing or turbulent water |
Mann, 1996 |
Barbus barbus |
Water with current: 28-43 cm/s |
Flowing or turbulent water |
Baras , 1993 |
Carassius auratus |
Creeks, ditches, ponds and reservoirs |
Stagnant water |
Internet, 2005 |
Carassius auratus |
Seeks warm, weedy shallows |
Stagnant water |
Scott and Crossman, 1973 |
Carassius auratus |
Stagnant water or with a weak flow |
Stagnant water |
Belova, 1981 |
Carassius auratus |
Current-free areas in lower reaches of rivers, bays, harbors, lagoons, marshes, and flooded lowlands |
Flowing or turbulent water |
Goodyear et al, 1982 |
Carassius carassius |
Ponds |
Stagnant water |
Laurila et al, 1987 |
Carassius carassius |
Naturally reproduce in the still or running waters of Southern and Nothern China |
No category |
Naca, 1989 |
Carassius carassius |
Near-shore parts of water bodies |
Stagnant water |
Sczerbowski and Szczerbowski, 1996 |
Chondrostoma nasus |
Grounds with current : 1m/s |
Flowing or turbulent water |
Bruslé and Quignard, 2001 |
Chondrostoma nasus |
Water with current |
Flowing or turbulent water |
Spillmann, 1961 |
Chondrostoma nasus |
Riffles with high current velocities [high water current ranging from 70 to 120 cm/s] |
Flowing or turbulent water |
Heckeis et al, 1996 |
Chondrostoma nasus |
Water with strong current |
Flowing or turbulent water |
Nelva, 2001 |
Chondrostoma nasus |
Fairly strong current |
Flowing or turbulent water |
Gozlan et al, 1999 |
Chondrostoma nasus |
Current velocity: 70-90 cm/s |
Flowing or turbulent water |
Mann, 1996 |
Chondrostoma nasus |
Large rivers or tributaries, high current velocities (1-2 m/s) |
Flowing or turbulent water |
Schiemer et al, 2003 |
Chondrostoma nasus |
Current velocity: mean of 0.9 cm/s |
Flowing or turbulent water |
Kamler and Keckeis, 2000 |
Chondrostoma nasus |
Water velocities of 0.7-1.1 m/s |
Flowing or turbulent water |
Zbinden and Maier, 1996 |
Chondrostoma nasus |
Average current velocities between 0.4 and 0.6 m/s |
Flowing or turbulent water |
Keckeis, 2001 |
Chondrostoma nasus |
Sites with swift current |
Flowing or turbulent water |
Ahnelt and Keckeis, 1994 |
Chondrostoma nasus |
Nase spawn in numerous sectionsof the main channel of the Austrian Danube. […] This finding is in contrast with assumption that reproduction takes place only in shallow water tributaries |
No category |
Winkler et al, 1997 |
Chondrostoma toxostoma |
Water with current |
Flowing or turbulent water |
Bruslé and Quignard, 2001 |
Chondrostoma toxostoma |
Small rivers or near the shore of main stream |
Stagnant water |
Gozlan and Chappaz, 2001 |
Chondrostoma toxostoma |
Small tributary streams, deep pools just dowstream of riffles |
No category |
Gozlan et al, 1999 |
Chondrostoma toxostoma |
Small rivers with strong current |
Flowing or turbulent water |
Bensettiti and Gaudillat, 2002 |
Chondrostoma toxostoma |
Search for small tributaries with strong current |
Flowing or turbulent water |
Internet |
Ctenopharyngodon idella |
Slow current, sides of river |
Flowing or turbulent water |
Bruslé and Quignard, 2001 |
Ctenopharyngodon idella |
Water with current |
Flowing or turbulent water |
Billard, 1997 |
Ctenopharyngodon idella |
Water with current |
Flowing or turbulent water |
Le Houarn, 2001 |
Ctenopharyngodon idella |
Spawning takes place after a sharp rise in the water level and current velocity |
Flowing or turbulent water |
Abdusamadov, 1986 |
Ctenopharyngodon idella |
Flowing water |
Flowing or turbulent water |
Mikodina and Makeyeva, 1981 |
Ctenopharyngodon idella |
Places with a rapid and turbulent water current, about 0.7-1.4 m/s |
Flowing or turbulent water |
Krykhtin and Gorbach, 1982 |
Ctenopharyngodon idella |
Riverbeds with strong current |
Flowing or turbulent water |
Fishbase, 2006 |
Ctenopharyngodon idella |
Primary channels of rivers and canals during high water, upper part of the water column over rapids and sand bars, preferred spawning habitat is found in turbid, turbulent water at the confluence of rivers or below dams, prefer to spawn in water currents ranging from 0.6 and 1.5 m/s, but will spawn in current as low as 0.2 m/s, or even in ponds where current is absent [Increases in water level exceeding 122 cm within 12 hour period are required for spawning] |
Stagnant water |
Cudmore and Mandrak, 2004 |
Ctenopharyngodon idella |
Spawning grounds are usually located in river reaches characterized by turbulent or whirlpool-like flow, often in the vicinity of islands or stream junctions [Reported current velocities of spawning areas in China ranged from 0.33 to0.90m/s] |
Flowing or turbulent water |
Scholfield, 2005 |
Ctenopharyngodon idella |
In a water current of between 0.5-2.4 m/sec |
Flowing or turbulent water |
Scott and Cross, 1973 |
Ctenopharyngodon idella |
Adults spawn upstream in the tributaries [high current velocities and long segments of unimpounded river] |
Flowing or turbulent water |
Brown and Coon, 1991 |
Ctenopharyngodon idella |
The existence and the persistence of the increasing water level, the water flow up to 3 m per second |
No category |
Ciolac, 2004 |
Ctenopharyngodon idella |
Apparent minimum current velocity of 0.6 m/second to keep eggs supported in the water column |
Flowing or turbulent water |
Leslie et al, 1982 |
Ctenopharyngodon idella |
Spawn in the primary channels of rivers and canals. [In relatively-large rivers] |
Stagnant water |
Shireman and Smith, 1983 |
Cyprinus carpio |
Tidal and non-tidal fresh water, either in fresh water or oligohaline water (10 ppt) |
No category |
Internet, 2005 |
Cyprinus carpio |
Flooding areas if available |
No category |
Lafaille and Crivelli, 2001 |
Cyprinus carpio |
Weedy and grassy shallows |
Stagnant water |
Scott and Crossman, 1973 |
Cyprinus carpio |
Spawn in marginal, shallow, weed-infested areas |
Stagnant water |
Fishbase, 2006 |
Cyprinus carpio |
Stagnant water or with a weak flow |
Stagnant water |
Belova, 1981 |
Cyprinus carpio |
A shallow flooded area |
No category |
Crivelli, 1981 |
Cyprinus carpio |
Fish spawning out of the tributary area: carp, pikeperch, catfish Silurus glanis and eel |
No category |
Hladik and Kubecka, 2003 |
Cyprinus carpio |
Naturally reproduce in the still or running waters of Southern and Nothern China |
No category |
Naca, 1989 |
Cyprinus carpio |
Preferred spawning sites are lentic habitats with abundant food, warm water and protection from predators |
No category |
Smith, 2004 |
Cyprinus carpio |
Protected areas of lakes and rivers, including bays, harbors, marshes, sloughs, flooded shorelines, and river mouths; also on shoals and reefs |
Stagnant water |
Goodyear et al, 1982 |
Gobio gobio |
Rivulet of about 30 cm wide; canal of 2 m wide |
Stagnant water |
Kennedy and Fitzmaurice, 1972 |
Gobio gobio |
Slow-flowing current : 10 to 80 cm/s |
Flowing or turbulent water |
Bruslé and Quignard, 2001 |
Gobio gobio |
Water with some current |
Flowing or turbulent water |
Spillmann, 1961 |
Gobio gobio |
Current velocity: 2-80 cm/s |
Flowing or turbulent water |
Mann, 1996 |
Gobio gobio |
Dans une eau faiblement courante |
Flowing or turbulent water |
Brunet and Hoestlandt, 1972 |
Hypophthalmichthys molitrix |
River with stroung current |
Flowing or turbulent water |
Bruslé and Quignard, 2001 |
Hypophthalmichthys molitrix |
Water with strong current: 0.7-1.4 m/s |
Flowing or turbulent water |
Billard, 1997 |
Hypophthalmichthys molitrix |
Water with strong current: 0.7-1.4 m/s |
Flowing or turbulent water |
Barbier, 2001 |
Hypophthalmichthys molitrix |
Spawning takes place after a sharp rise in the water level and current velocity |
Flowing or turbulent water |
Abdusamadov, 1986 |
Hypophthalmichthys molitrix |
Flowing water |
Flowing or turbulent water |
Mikodina and Makeyeva, 1981 |
Hypophthalmichthys molitrix |
Places with a rapid and turbulent water current, about 0.7-1.4 m/s |
Flowing or turbulent water |
Krykhtin and Gorbach, 1982 |
Hypophthalmichthys molitrix |
Current velocities 0.3-3 m/s |
Flowing or turbulent water |
Kolar et al, 2005 |
Hypophthalmichthys molitrix |
Spawning grounds are usually located in river reaches characterized by turbulent or whirlpool-like flow, often in the vicinity of islands or stream junctions [Reported current velocities of spawning areas in China ranged from 0.33 to0.90m/s] |
Flowing or turbulent water |
Scholfield, 2005 |
Hypophthalmichthys molitrix |
The existence and the persistence of the increasing water level, the water flow up to 3 m per second |
No category |
Ciolac, 2004 |
Hypophthalmichthys molitrix |
Their spawning occurs in a considerable current |
Flowing or turbulent water |
Belova, 1981 |
Leucaspius delineatus |
Sunbleak typically lay their eggs on marginal macrophytes that generally grouw out of anoxic silt |
No category |
Pinder and Gozlan, 2004 |
Leuciscus cephalus |
Relatively swift-flowing streams |
Flowing or turbulent water |
Calta, 2000 |
Leuciscus cephalus |
Water with current |
Flowing or turbulent water |
Bruslé and Quignard, 2001 |
Leuciscus cephalus |
Lotic habitat conditions, moderate to high water flow [0.15-0.75 m/s], BUT one population found spawning without any current |
Flowing or turbulent water |
Arlinghaus and Wolter, 2003 |
Leuciscus cephalus |
Flowing water |
Flowing or turbulent water |
Fishbase, 2006 |
Leuciscus cephalus |
Current velocity: 20-50 cm/s |
Flowing or turbulent water |
Mann, 1996 |
Leuciscus cephalus |
Located near erosion banks or in shallow upstream of a bridge. The current speed near the spawning substratum ranged between 0.15 to 0.35 m/s |
Flowing or turbulent water |
Fredrich et al, 2003 |
Leuciscus cephalus |
Some species seem to be strickly dependent on the tributary zone as they were never observed reproducing in the reservoir (asp, bleak, chub and white bream), while others are facultative tributary users (roach, bream, pike, perch, rudd). |
No category |
Hladik and Kubecka, 2003 |
Leuciscus cephalus |
Fast current speed |
Flowing or turbulent water |
Zelepien, 1997 |
Leuciscus idus |
Water with current |
Flowing or turbulent water |
Billard, 1997 |
Leuciscus idus |
Ide spawn in rivers, streams, old arms, lakes, dam reservoirs, and meadows covered with flood waters. |
Stagnant water |
Witkowski et al, 1997 |
Leuciscus leuciscus |
Riffles : water with current |
Flowing or turbulent water |
Bruslé and Quignard, 2001 |
Leuciscus leuciscus |
Water with current |
Flowing or turbulent water |
Spillmann, 1961 |
Leuciscus leuciscus |
Flowing water |
Flowing or turbulent water |
Fishbase, 2006 |
Leuciscus leuciscus |
Current velocities: 20-50 cm/s |
Flowing or turbulent water |
Mann, 1996 |
Leuciscus leuciscus |
Prefers swifter currents |
Flowing or turbulent water |
Kennedy, 1969 |
Leuciscus leuciscus |
Fast-flowing waters |
Flowing or turbulent water |
Mills, 1981 |
Leuciscus leuciscus |
Fast flowinf rivers and streams |
No category |
Mann and Mills, 1985 |
Mylopharyngodon piceus |
Flowing water |
Flowing or turbulent water |
Mikodina and Makeyeva, 1981 |
Mylopharyngodon piceus |
Turbulent waters |
Flowing or turbulent water |
Fishbase, 2006 |
Mylopharyngodon piceus |
Spawning grounds are usually located in river reaches characterized by turbulent or whirlpool-like flow, often in the vicinity of islands or stream junctions [Reported current velocities of spawning areas in China ranged from 0.33 to0.90m/s] |
Flowing or turbulent water |
Scholfield, 2005 |
Mylopharyngodon piceus |
Their spawning occurs in a considerable current |
Flowing or turbulent water |
Belova, 1981 |
Phoxinus phoxinus |
Slow current |
Flowing or turbulent water |
Bruslé and Quignard, 2001 |
Phoxinus phoxinus |
Flowing water |
Flowing or turbulent water |
Fishbase, 2006 |
Phoxinus phoxinus |
Close to the shore of the river or brook |
Stagnant water |
Papadopol and Weinberger, 1975 |
Phoxinus phoxinus |
Water edge of lakes |
Stagnant water |
Wooton and Mills, 1979 |
Phoxinus phoxinus |
Current velocity: 20-30 cm/s |
Flowing or turbulent water |
Mann, 1996 |
Phoxinus phoxinus |
Tributary streams |
No category |
Scott, 1979 |
Phoxinus phoxinus |
Where the water is well-saturated with oxygen, mainly on bars and in channels |
No category |
Soin et al, 1982 |
Phoxinus phoxinus |
Running waters |
No category |
Frost, 1943 |
Pimephales promelas |
Ponds |
Stagnant water |
Gale and Buynak, 1982 |
Pimephales promelas |
Ponds |
Stagnant water |
DeWitt, 1993 |
Pimephales promelas |
Protected areas, such as lake margins and marshes |
Stagnant water |
Goodyear et al. et al, 1982 |
Pimephales promelas |
Ponds |
Stagnant water |
Markus, 1934 |
Pseudorasbora parva |
Warm, shallow and calm waters |
No category |
Coad, 2005 |
Pseudorasbora parva |
Warm and calm waters, inshore areas of ponds |
Stagnant water |
Makeyeva and Mokamed, 1982 |
Pseudorasbora parva |
Ponds and rivers |
Stagnant water |
Katano and Maekawa, 1997 |
Rhodeus sericeus |
In tributary of the river, near to banks |
No category |
Mills and Reynolds, 2002 |
Rutilus rutilus |
Canal |
Stagnant water |
Diamond, 1985 |
Rutilus rutilus |
Rivers, small tributaries of lakes |
Stagnant water |
Vila-Gispert and Moreno-Amich, 2000 |
Rutilus rutilus |
Stream near a lake |
Stagnant water |
Vollestad et al, 1987 |
Rutilus rutilus |
Current velocity: >20 cm/s |
Flowing or turbulent water |
Mann, 1996 |
Rutilus rutilus |
In lake Geneva, along the embankments |
Stagnant water |
Gillet and Quétin, 2006 |
Rutilus rutilus |
Some species seem to be strickly dependent on the tributary zone as they were never observed reproducing in the reservoir (asp, bleak, chub and white bream), while others are facultative tributary users (roach, bream, pike, perch, rudd). Generalists: fish spawning in suitable places both inthe tributary and the reservoir: bream, roach, perh, pike and ruffe |
No category |
Hladik and Kubecka, 2003 |
Rutilus rutilus |
Littoral waters, bays, creeks and small ponds, which are warm in spring |
Stagnant water |
Kortet et al, 2004b |
Rutilus rutilus |
Shallow, sheltered, and vegetated shores are important as spawning and larval areas for roach in lakes |
Stagnant water |
Härmä et al, 2008 |
Scardinius erythrophthalmus |
River, reservoir, lakes |
Stagnant water |
Vila-Gispert and Moreno-Amich, 2000 |
Scardinius erythrophthalmus |
Current velocity: < 5 cm/s |
Flowing or turbulent water |
Mann, 1996 |
Scardinius erythrophthalmus |
Some species seem to be strickly dependent on the tributary zone as they were never observed reproducing in the reservoir (asp, bleak, chub and white bream), while others are facultative tributary users (roach, bream, pike, perch, rudd). Generalists: fish spawning in suitable places both inthe tributary and the reservoir: bream, roach, perh, pike and ruffe |
No category |
Hladik and Kubecka, 2003 |
Tinca tinca |
Deep parts of littoral zone in lake or dam reservoir [Stays at the same place during the spawning season at about 25 m from a spawning place] |
Stagnant water |
Linhart and Billard, 1995 |
Tinca tinca |
Low or no flow |
No category |
Environment agency, ??? |
Tinca tinca |
Current velocity: < 5 cm/s |
Flowing or turbulent water |
Mann, 1996 |
Vimba vimba |
High rate flow : current of 0.6-0.9 m/second |
Flowing or turbulent water |
Shikhshabekov, 1979 |
Vimba vimba |
Water with current |
Flowing or turbulent water |
Bruslé and Quignard, 2001 |
Vimba vimba |
Current of 0.6-0.9 m/s |
Flowing or turbulent water |
Coad, 2005 |
Vimba vimba |
Water with current |
Flowing or turbulent water |
Maitland, 1977 |
Vimba vimba |
Spawns in a swift current |
Flowing or turbulent water |
Wajdowicz, 1974 |
Vimba vimba |
There is the largest number of vimba spawning grounds in this part of the river. For instance, one of the major factors, the average velocity of the flow in the Middle Nemunas fluctuates from 0.7 to 0.9 m/s and there are plenty of shallow gravelled segments of the riverbed there |
Flowing or turbulent water |
Kesminas et al, 1999 |
Vimba vimba |
Favorable places for this fish are water bodies with weak current: bays, lakes, and reservoirs. |
Stagnant water |
Ermolin and Shashulovskii, 2006 |
Vimba vimba |
For the spawning purposes the vimbs enter streams with clear water and fast current |
Flowing or turbulent water |
Trzebiatowski and Narozanski, 1973 |
Vimba vimba |
Fast-flowing river currents, in well oxygenated waters |
Flowing or turbulent water |
Luszczek et al, 2008 |
Gambusia affinis |
Variable: sluggish water, land-locked ponds, reservoirs, creeks, streams, and sloughs [Mostly in freshwater but oligohaline water] |
Stagnant water |
Internet, 2005 |
Esox masquinongy |
Spawn on shoals in the main river, with water velocity greater than 0.1 m/s |
Flowing or turbulent water |
Farrell et al, 1996 |
Esox masquinongy |
Flooded areas |
No category |
Scott and Crossman, 1973 |
Esox masquinongy |
Usually spawn at either the upper or lower ends of low gradient pools |
No category |
Kerr and Grant, 1999 |
Esox masquinongy |
Protected bays, harbors, marshes, stream mouths, feeder streams, and flooded lowlands; also in current-swept areas at edges of channels |
Flowing or turbulent water |
Goodyear et al, 1982 |
Esox masquinongy |
Lakes and rivers which have dense, aquatic or flooded terrestrial vegetation |
Stagnant water |
Wynne, 2006 |
Esox masquinongy |
The upper river muskellunge spawning distribution is usually restricted to bays and coastal marshes in shallow waters < 1.5 m deep |
No category |
Farrell et al, 2005 |
Esox masquinongy |
Shallow pools close to moving water |
No category |
Clemmons and Newman, 1997 |
Esox niger |
Lakes and/or ponds over submerged vegetation |
Stagnant water |
Coffie, 1998 |
Esox niger |
Flood benches of streams, lakes or ponds, very shrotly after the ice melts |
Stagnant water |
Scott and Crossman, 1973 |
Esox niger |
Flooded benches of streams, lakes and ponds |
Stagnant water |
Anonymous, 2006 |
Esox lucius |
Located in flooding areas and near the shore of lakes and ponds |
Stagnant water |
Souchon, 1983 |
Esox lucius |
Backwater habitats with little current or negligible current |
Flowing or turbulent water |
Farrell et al, 1996 |
Esox lucius |
Littoral zones of lake and border line of pond |
Stagnant water |
Bruslé and Quignard, 2001 |
Esox lucius |
Calm waters near the shoreline |
Stagnant water |
Spillmann, 1961 |
Esox lucius |
May spawn either in marshy areas of lakes or in connected soughs |
Stagnant water |
Franklin and Smith, 1963 |
Esox lucius |
At the lake edge or in flooded river areas |
Stagnant water |
Billard, 1996 |
Esox lucius |
Preferentially on flooding rivers and plants near shore |
Stagnant water |
Le Louarn and Feunteun, 2001 |
Esox lucius |
Rivers, marshes and bays of larger lakes |
Stagnant water |
Scott and Crossman, 1973 |
Esox lucius |
Small tributary streams, marshes to adjacent to lakes or in shallow, weedy days of larger lakes or rivers |
Stagnant water |
Kerr and Grant, 1999 |
Esox lucius |
No significant weter current and some protection from dominant winds. |
Flowing or turbulent water |
Bradbury et al, 1999 |
Esox lucius |
Shallow lake margins, inflowing streams, ditches and drainage marshes |
Stagnant water |
Giles et al, 1986 |
Esox lucius |
Shallow wind-sheltered area |
No category |
Wright and Shoesmith, 1988 |
Esox lucius |
Some species seem to be strickly dependent on the tributary zone as they were never observed reproducing in the reservoir (asp, bleak, chub and white bream), while others are facultative tributary users (roach, bream, pike, perch, rudd). Generalists: fish spawning in suitable places both inthe tributary and the reservoir: bream, roach, perh, pike and ruffe |
No category |
Hladik and Kubecka, 2003 |
Esox lucius |
Areas with sluggish water current, including shore line weeds beds and marshes, sloughs, bays and harbors, river mouths, ditches, feeder streams, and temporarily flooded lowlands |
Stagnant water |
Goodyear et al, 1982 |
Lota lota |
"Bras morts ou les annexes inondées en rivières" , 2-3 m in lakes |
Stagnant water |
Persat, 2001 |
Lota lota |
Shallow bays, usually spawn in the lake they are also know to move into rivers to spawn |
Stagnant water |
Scott and Crossman, 1973 |
Lota lota |
Lakes or rivers |
Stagnant water |
Vedeneev et al, 2003 |
Lota lota |
Both lakes and rivers |
Stagnant water |
Bradbury et al, 1999 |
Lota lota |
Spawning condition occurred both inshore and offshore, but they were observed in greater numbers in the inshore nets |
Stagnant water |
Hewson, 1955 |
Lota lota |
Typically in river beds. Spawning in lakes was reported as well. A part of burbot lacustrine populations in Sweden spawned in the lakes |
Stagnant water |
Kujawa et al, 2002 |
Lota lota |
Nearshore areas, including shorelines, river mouths, bays, and harbors; offshore bars and reefs; swift, open water in streams |
Stagnant water |
Goodyear et al. et al, 1982 |
Lota lota |
Burbot can spawn either in lakes or rivers. In washington, burbot evidently spawn in lakes and reservoirs except for some Lake Roosevelt fish that spawn in a flowing section of the Columbia River near the Canadian border |
Stagnant water |
Bonar et al, 2000 |
Gasterosteus aculeatus |
Shallow weedy areas [Freshwater and brackish water] |
Stagnant water |
Internet, 2005 |
Gasterosteus aculeatus |
Submerged areas |
No category |
Bruslé and Quignard, 2001 |
Gasterosteus aculeatus |
Ponds and rivers |
Stagnant water |
Poulin and Fitzgerald, 1989 |
Gasterosteus aculeatus |
Shallow tidal Pools |
No category |
Fitzgerald, 1983 |
Gasterosteus aculeatus |
Anadromous populations may spawn in brackish or freshwater [Spawning in freshwater has been observed in two distinct habitat types within lakes; open-water areas, or in association with aquatic vegetation |
Stagnant water |
Bradbury et al, 1999 |
Gasterosteus aculeatus |
Pools and rivers in the salt marshes, but most reproduce in pools whose salinity fluctuates between apprimatively 14 and 27 %o, but a considerable number reproduce in the freshwater section |
No category |
Belanger et al, 1987 |
Gasterosteus aculeatus |
Sheltered, current-free / areas along lake shore and in bays, creek mouths, and tributaries, usually close to shore |
Stagnant water |
Goodyear, 1982 |
Pungitius pungitius |
Shallow tidal Pools |
No category |
Fitzgerald, 1983 |
Pungitius pungitius |
Although ninespine stickleback have a relatively high salinity tolerance, they have only been reported to spawn in freshwater |
No category |
Bradbury et al, 1999 |
Pungitius pungitius |
Quiet areas in vegetated bays and creeks, 1-5 feet from shore; may also spawn along exposed shoreline but this is not as successful |
Stagnant water |
Goodyear, 1982 |
Ambloplites rupestris |
Lake, near the shorline |
Stagnant water |
Gross and Nowell, 1980 |
Ambloplites rupestris |
Sheltered nearshore areas, including bays, harbors, lagoons, marshes, creek mouths, and lower reaches of tributaries; current-swept lake shoals and ledges; moderateswift water in streams; |
Stagnant water |
Goodyear et al, 1982 |
Lepomis gibbosus |
Lakes, reservoirs, ponds and creeks |
Stagnant water |
Internet, 2005 |
Lepomis gibbosus |
Ponds, lakes or slow moving streams, near the shore |
Stagnant water |
Scott and Crossman, 1973 |
Lepomis gibbosus |
Near the shore |
Stagnant water |
Fishbase, 2006 |
Lepomis gibbosus |
Shallow water of ponds, lakes, slow-moving streams close to shore |
Stagnant water |
Kerr and Grant, 1999 |
Lepomis gibbosus |
Quiet nearshore areas, including bays, harbors, marshes, laggoons, backwaters, and creek mouths; also running waters of tributaries |
Stagnant water |
Goodyear, 1982 |
Micropterus dolomieui |
From stream to lake, water with little current |
Stagnant water |
Internet, 2005 |
Micropterus dolomieui |
Lakes and rivers |
Stagnant water |
Fishbase, 2006 |
Micropterus dolomieui |
Lakes and rivers, usually near the protection of rocks, logs, or more rarely, dense vegetation |
Stagnant water |
Scott and Crossman, 1973 |
Micropterus dolomieui |
Distance from the shore: 0-890 cm |
Stagnant water |
Iguchi et al, 2004 |
Micropterus dolomieui |
Shore of lake, or effluent canal |
Stagnant water |
Cooke et al, 2003 |
Micropterus dolomieui |
Mean distance from the shore 3.4 m |
Stagnant water |
McNeill, 1995 |
Micropterus dolomieui |
At a distance of 0.3-2.4 m from the leeward shore. Small lakes with controlled water levels may provide thermal and other environmental conditions suitable for natural reproduction |
Stagnant water |
Turner and MacCrimmon, 1970 |
Micropterus dolomieui |
Littoral zones of lakes and rivers |
Stagnant water |
Ridgway et al, 1989 |
Micropterus dolomieui |
Clear water in tributaries, river mouth, bays, harbors, lake shores or shoals |
Stagnant water |
Goodyear et al, 1982 |
Micropterus dolomieui |
Reduced water velocity |
Flowing or turbulent water |
Knotek and Orth, 1998 |
Micropterus salmoides |
Nest may be constructed almost anywhere in a lake, but it is not unusal for them to be grouped on certain shorelines or in specific coves |
Stagnant water |
Heidinger, 1976 |
Micropterus salmoides |
Calm waters |
No category |
Spillmann, 1961 |
Micropterus salmoides |
Waters of ponds, lakes, reservoirs, soughs of the Delta, creeks and some irrigation ditches [usually nests are built in areas without current or wave action] |
Stagnant water |
Internet, 2005 |
Micropterus salmoides |
Areas protected from wave action |
No category |
Mesing and Wickler, 1986 |
Micropterus salmoides |
Protected litoral areas in lakes or tributaries, including marshes, bays, harbors, sloughs, lagoons, and creek mouths |
Stagnant water |
Goodyear et al, 1982 |
Dicentrarchus labrax |
Coastal zones, at sea |
No category |
Billard, 1997 |
Dicentrarchus labrax |
Sea margin |
No category |
Secor, ??? |
Morone americana |
Spawn in estuaries, rivers, lakes and marshes. Spawning is usually in freshwater, but may occur in brackish water at salinities up to 4.2 ppt. Preferred spawning habitats are waters that are tidal and nontidal, clear or turbid, fast or slow |
Stagnant water |
Stanley and Danie, 1983 |
Morone americana |
Tales place mainly in a variety of protected habitats, such as shallow flats, embayments, and tidal creeks |
No category |
Everly and Boreman, 1999 |
Morone americana |
In the headwaters of Chesapaekae Bay and its tributaries [In tidal fresh and brackish waters] |
No category |
North and Houde, 2001 |
Morone americana |
Spawn in tidal freshwater or slightly brackish water |
No category |
Mansuetti, 1961 |
Morone chrysops |
Tuburlent areas of rivers |
No category |
Internet, 2005 |
Morone chrysops |
Tributaries, but in any suitable shoreline structure in the absence of tributaries |
Stagnant water |
Kohler, 1997 |
Morone chrysops |
Clear, swift tributaries; if tributaries are not available, will spawn on current-swept lake shores or shoals or in bays |
Stagnant water |
Goodyear, 1982 |
Morone saxatilis |
Move into fresh or brackish water to spawn |
No category |
Fishbase, 2006 |
Morone saxatilis |
Areas with good flow and/or tidal action which provides increased agitation and aeration to the eggs and help keeps tehm in suspension |
No category |
Internet, 2005 |
Morone saxatilis |
Deltaic channels |
No category |
Will et al, 2002 |
Morone saxatilis |
With some current |
Flowing or turbulent water |
Rue, 2001 |
Morone saxatilis |
Current velocities averaging 0.49-0.55 m/s [Areas with rapids, boulders and strounfg currents, typically associated with the fall line] |
Flowing or turbulent water |
Burdick and Hightower, 2005 |
Morone saxatilis |
In the headwaters of Chesapaekae Bay and its tributaries |
No category |
North and Houde, 2001 |
Morone saxatilis |
In these rapids, where the muddy current is exceedingly strong and rendered very erratic by islands, boulders and rocks, the fish spaws. Spawn in low-lying flooded delta country adjacent to Suisun Bay, where the borders between brackish and purely fresh |
Flowing or turbulent water |
Merriman, 1937 |
Morone saxatilis |
Anadromous, spawning in tidal rivers and migrating to estuarine and marine coastal waters to feed and mature |
No category |
McLaren et al, 1981 |
Gymnocephalus cernua |
Where the current is fairly rapid |
Flowing or turbulent water |
Craig, 2000 |
Gymnocephalus cernua |
Spawning of Eurasian ruffe in the the Baka side-arm system of the River Danube, in the Orava Reservoir, Lipno reservoir |
No category |
Kovac, 1998 |
Perca flavescens |
In the shallows of lakes, and often into tributary, where they live in brackish water, they migrate into fresh water |
Stagnant water |
Scott and Crossman, 1973 |
Perca flavescens |
Upper reaches of many major tributaries |
No category |
Mansueti, 1964 |
Perca flavescens |
Tales place in tidal and non-tidal water |
No category |
Rue, 2001 |
Perca flavescens |
Lakes and tributary streams [Sites protected from high winds and fast currents are chosen] |
Stagnant water |
Kerr and Grant, 1999 |
Perca fluviatilis |
Lakes, they would spawn anywhere away from fast currents |
Stagnant water |
Thorpe, 1977 |
Perca fluviatilis |
Near the shore, most within 3 meters |
Stagnant water |
Smith et al, 2001 |
Perca fluviatilis |
Near the shore |
Stagnant water |
Dubois, 2001 |
Perca fluviatilis |
Ponds, lakes, rivers |
Stagnant water |
Gillet et al, 1995 |
Perca fluviatilis |
Some species seem to be strickly dependent on the tributary zone as they were never observed reproducing in the reservoir (asp, bleak, chub and white bream), while others are facultative tributary users (roach, bream, pike, perch, rudd). Generalists: fish spawning in suitable places both inthe tributary and the reservoir: bream, roach, perh, pike and ruffe |
No category |
Hladik and Kubecka, 2003 |
Sander lucioperca |
Shallow inlets and bays, bays sheltered by islands, river outlets |
No category |
Lappaleinen et al, 2003 |
Sander lucioperca |
Slow-flowing current : < 1.5 m/s |
Flowing or turbulent water |
Bruslé and Quignard, 2001 |
Sander lucioperca |
Water velocities of 0.1-0.2 m.s-1 |
Flowing or turbulent water |
Craig, 2000 |
Sander lucioperca |
Water with current: 1.40-1.50 m/s |
Flowing or turbulent water |
Billard, 1997 |
Sander lucioperca |
Moving water, in a current of 1.4-1.5 m/sec |
Flowing or turbulent water |
Fishbase, 2006 |
Sander lucioperca |
Water with current 0.1-0.2 m/s |
Flowing or turbulent water |
Deeler and Willemsen, 1964 |
Sander lucioperca |
Occur mainly in sheltered archipelagoes and bays, with turbid waters. On contrats to lakes, where spawning takes place in the shallows of open lakes, Baltic pikeperch spawn entirely in estuaries, inlets and shallow bays. |
Stagnant water |
Lehtonen et al, 1996 |
Sander lucioperca |
In March, pikeperch were located in the parts of the canal where the bank vegetation was dominated by bushes. In April and May, pikeperch occurred in shallow parts with trees (ot high vegetation) or without vegetation but with woody debris. During June and early July, they were frequently found in deeper parts in tributaries with bank vegetation of grass and reed |
Stagnant water |
Poulet et al, 2005 |
Sander lucioperca |
Fish spawning out of the tributary area: carp, pikeperch, catfish Silurus glanis and eel |
No category |
Hladik and Kubecka, 2003 |
Sander vitreus |
Streams and lakes |
Stagnant water |
Colby et al, 1979 |
Sander vitreus |
Inlet streams, flooded wetland vegetation |
Stagnant water |
Malison and Held, 1996b |
Sander vitreus |
Quiet border waters, slow-moving water |
Stagnant water |
Corbett and Powles, 1986 |
Sander vitreus |
White water below impassable falls and dams in rivers, lakes |
Stagnant water |
Scott and Crossman, 1973 |
Sander vitreus |
Turbid streams and rivers, rocky wave-shaded shallows of lakes or flooded wetland vegetation |
Stagnant water |
Kerr and Grant, 1999 |
Sander vitreus |
White water or shoals of lakes |
Stagnant water |
Anonymous, 2006 Chapter 3 |
Coregonus lavaretus |
The spawning area is located below waterfall being 4.5 km upstream |
No category |
Skurdal et al, 1985 |
Coregonus lavaretus |
Shore of lakes |
Stagnant water |
Billard, 1997 |
Coregonus lavaretus |
Shore of lakes |
Stagnant water |
Gerdeaux, 2001 |
Coregonus lavaretus |
Shallow areas and rivers |
No category |
Salojarvi, 1982 |
Coregonus albula |
Located at the either steep or gentle slopes of shore lines and islands, in the region of under-water wells or river mouths, and in rivers with strong current |
Stagnant water |
Zuromska, 1982 |
Coregonus albula |
Spawning areas are mainly situated in the sublitoral zone. |
No category |
Anwand, 1998 |
Coregonus clupeaformis |
Spawning shoals of lakes |
Stagnant water |
Kerr and Grant, 1999 |
Coregonus clupeaformis |
Inshore areas, bays, ledges, shoals, reefs, often same sites used by lake trout |
Stagnant water |
Goodyear et al, 1982 |
Coregonus clupeaformis |
Unlike many other species, flowing water is not required for spawning |
Flowing or turbulent water |
Bradbury et al, 1999 |
Coregonus clupeaformis |
Lakes, streams |
Stagnant water |
Willson, 1997 |
Hucho hucho |
Water velocities : 0.61 m/s |
Flowing or turbulent water |
Bruslé and Quignard, 2001 |
Hucho hucho |
Water with current |
Flowing or turbulent water |
Perrin, 2001 |
Hucho hucho |
Water with current: 0.6-1 m/s |
Flowing or turbulent water |
Jatteau, 1991 |
Hucho hucho |
Migrate upstream into smaller and shallower streams |
No category |
Fishbase, 2006 |
Hucho hucho |
Rivers and larger streams on the region of the grayling |
No category |
Witokowski and Kokurewicz, 1981 |
Hucho hucho |
Upper courses of highland rivers, where the stream runs fairly rapidly |
No category |
Prawochensky and Kolder, 1968 |
Oncorhynchus gorbuscha |
Velocities 30 to 140 cm/sec |
Flowing or turbulent water |
Groot, 1996 |
Oncorhynchus gorbuscha |
Primarily in streams with riffles, but also brackish water conditions in river mouths |
No category |
Groot, 1996 |
Oncorhynchus gorbuscha |
Channel part of the river [Velocity of flow is about 0.2-1.1 m/s] |
Flowing or turbulent water |
Golobanov, 1982 |
Oncorhynchus gorbuscha |
Rivers and tributary streams, with current |
Flowing or turbulent water |
Scott and Crossman, 1973 |
Oncorhynchus gorbuscha |
Usually in brush-choked streams in shoal area nearest stream mouth where there is a suitable substrate and water velocity of 0.75-3.25 |
Flowing or turbulent water |
Goodyear et al, 1982 |
Oncorhynchus gorbuscha |
Streams, intertidal |
No category |
Willson, 1997 |
Oncorhynchus keta |
Prefer to spawn immediatly above turbulent areas, or where there is upwelling |
Flowing or turbulent water |
Groot, 1996 |
Oncorhynchus keta |
Summer races prefers sites influenced by intrasubstrate flow and fall races prefer outlets of groundwater |
No category |
Vronskii and Leman, 1991 |
Oncorhynchus keta |
Near the head waters, current speeds of about 20 cm/s |
Flowing or turbulent water |
Fishbase, 2006 |
Oncorhynchus keta |
Spawn in both small and large rivers, in the channel, and its tributaries of the first and second orders, and late O. keta spawn mainly in the middle and upper reaches of rivers |
No category |
Volobuev and Volobuev, 2000 |
Oncorhynchus keta |
Water velocities seclected by autumn chum salmon in Hokkaido were 10 to 20 cm/s [summer chum salmon in the My River spawned in velocities of 10 to 100 cm/sec] |
Flowing or turbulent water |
Bakkala, 1970 |
Oncorhynchus keta |
Streams, intertidal |
No category |
Willson, 1997 |
Oncorhynchus keta |
The ability of chum salmon and rainbow trout to detect upwellling currents, and the reduction in digging variability associated with development of the nest, suggest that the current pattern around the nest provides important locative information for the females. |
Flowing or turbulent water |
Tautz and Groot, 1975 |
Oncorhynchus keta |
Maximum spawning density is seen at sites with the most intensive input of groundwater |
No category |
Leman, 1993 |
Oncorhynchus keta |
Habitat ranging from tidal areas, to small streams only a few kilometres in length, to the mainstreams of large rivers over 200 km from salt water |
No category |
Beacham and Murray, 1987 |
Oncorhynchus kisutch |
Numerous small coastal streams, in large rivers, and in remote tributaries [water velocities vary from 18 to 76 cm/s] |
Flowing or turbulent water |
Groot, 1996 |
Oncorhynchus kisutch |
Avoid place with slow current and prefer spawning in the river channels in more rapid current |
Flowing or turbulent water |
Zorbidi, 1988 |
Oncorhynchus kisutch |
Outlets of groundwater |
No category |
Vronskii and Leman, 1991 |
Oncorhynchus kisutch |
Swifter water of river tributaries |
No category |
Scott and Crossman, 1973 |
Oncorhynchus kisutch |
Prefers smaller fresh water streams with lower velocities than O. tshawytscha |
Flowing or turbulent water |
Kerr and Grant, 1999 |
Oncorhynchus kisutch |
Riffles, with water velocity of 0.25-2.5fps, in mid-reaches or headwaters of streams, also reported along shore in St. Lawrence River |
Stagnant water |
Goodyear et al, 1982 |
Oncorhynchus kisutch |
Streams |
No category |
Willson, 1997 |
Oncorhynchus kisutch |
Coastal streams |
No category |
Crone and Bond, 1976 |
Oncorhynchus mykiss |
Large tributaries of river system, some coastal creeks, smaller tributaries within the estuary |
No category |
Internet, 2005 |
Oncorhynchus mykiss |
Spawning occurs in many small streams: cool, clear and well-oxygenated waters, with water velocities of 23-155 cm/sec |
Flowing or turbulent water |
Groot, 1996 |
Oncorhynchus mykiss |
Smaller tributaries of their rivers, or inlet or outlet streams of their lakes [in a riffle above a pool] |
Stagnant water |
Scott and Crossman, 1973 |
Oncorhynchus mykiss |
Permanent headwater tributaries with cool, cela water that is well oxygenated [Water velocities of 23 to 155 cm/m] |
Flowing or turbulent water |
Kerr and Grant, 1999 |
Oncorhynchus mykiss |
Upwelling does not appear to be important for spawning of rainbow trout |
No category |
Bradbury et al, 1999 |
Oncorhynchus mykiss |
Streams, lakes |
Stagnant water |
Willson, 1997 |
Oncorhynchus mykiss |
The ability of chum salmon and rainbow trout to detect upwellling currents, and the reduction in digging variability associated with development of the nest, suggest that the current pattern around the nest provides important locative information for the females. |
Flowing or turbulent water |
Tautz and Groot, 1975 |
Oncorhynchus mykiss |
Headwater spring streams to large , lower-crouese streams |
No category |
Greeley, 1932 |
Oncorhynchus nerka |
Outlets of groundwater |
No category |
Vronskii and Leman, 1991 |
Oncorhynchus nerka |
Inlet streams of the lake, along its shore |
Stagnant water |
Scott and Crossman, 1973 |
Oncorhynchus nerka |
Rivers and bowls |
No category |
Parensky et al, 2002 |
Oncorhynchus nerka |
Mid-reaches and headwaters of tributaries in areas with water valocity of less than 2.2 fps, if access tributaries is denied spawning occurs along lake shore, suually on wave-swpet beaches or on bars near stream mouth |
Stagnant water |
Goodyear et al, 1982 |
Oncorhynchus nerka |
Streams, lake shores |
Stagnant water |
Willson, 1997 |
Oncorhynchus nerka |
Spawn in the tributaries and around islands and mainland beaches of Iliamna Lake, Alaska. |
Stagnant water |
Hamon et al, 1999 |
Oncorhynchus tshawytscha |
From large river system to small tributaries 2 to 3 m wide |
No category |
Groot, 1996 |
Oncorhynchus tshawytscha |
Past, upper reaches of River, also in some tributaries |
No category |
Internet, 2005 |
Oncorhynchus tshawytscha |
Sites influenced by intrasubstrate flow [with a current not exceeding 2 m/s] |
Flowing or turbulent water |
Vronskii and Leman, 1991 |
Oncorhynchus tshawytscha |
Large tributaries, near riffles |
No category |
Scott and Crossman, 1973 |
Oncorhynchus tshawytscha |
Larger mainstream and headwater tributaries [Where water velocities are not less than 0.3 m/s], most frequently at head of riffles |
Flowing or turbulent water |
Kerr and Grant, 1999 |
Oncorhynchus tshawytscha |
Riffle areas with water velocity of 1-3 fps, in high gradient mid-reaches or headwaters of tributaries; spawning may also occur along lake shore or on shoals |
Stagnant water |
Goodyear et al, 1982 |
Oncorhynchus tshawytscha |
Streams |
No category |
Willson, 1997 |
Salmo salar |
Usually above or below a pool at the downstream end of riffles or upwellings of ground water |
No category |
Groot, 1996 |
Salmo salar |
In the upstream of river, near the shoreline (current speed of 40-50 cm/s) |
Stagnant water |
Bruslé and Quignard, 2001 |
Salmo salar |
Water current of about 44 cm/s |
Flowing or turbulent water |
Dumas and Darolles, 1999 |
Salmo salar |
Middle and upper part of river, with current |
Flowing or turbulent water |
Porcher and Baglinière, 2001 |
Salmo salar |
Areas with appreciable current |
Flowing or turbulent water |
Fishbase, 2006 |
Salmo salar |
Riffle area above or below a pool |
No category |
Scott and Crossman, 1973 |
Salmo salar |
Water velocities of 0.204-0.814 cm/s |
Flowing or turbulent water |
Crisp, 1996 |
Salmo salar |
Most redds are situated at a site where the current is accelerating |
Flowing or turbulent water |
Kerr and Grant, 1999 |
Salmo salar |
Streams |
No category |
Willson, 1997 |
Salmo salar |
Gravel-bottomed riffle sections of streams |
No category |
Bradbury et al, 1999 |
Salmo salar |
Redds are commonly located in pool-riffle transition zones. Such sites have comparitively high water velocities, down or upwelling flows and corase gravels |
Flowing or turbulent water |
de Gaudemar, et al, 2000 |
Salmo salar |
Water with current |
Flowing or turbulent water |
Bensettiti and Gaudillat, 2002 |
Salmo salar |
Spawn in freswater |
No category |
Johnston and McLay, 1997 |
Salmo salar |
Fast-water areas in clear, cold streams, with steep gradient; early runs usually spawn in the upper reaches, late runs in lower reaches; also on lake shoals which have seepage from springs |
Stagnant water |
Goodyear et al, 1982 |
Salmo salar |
Salmon spawned mostly in relatively deep, swift-velocity habitats (20-50 cm, 35-65 cm s-1) |
Flowing or turbulent water |
Louhi et al, 2008 |
Salmo trutta fario |
Rivers [Rapid current, 30 to 70/80 cm/s] |
Flowing or turbulent water |
Bruslé and Quignard, 2001 |
Salmo trutta fario |
Small streams at the head of riffle areas or on the downstream end of pools, where the gravel slopes upward [water freely flowing through the gravel and upwelling water, suitable velocities range from 15 to 90 cm/s] |
Flowing or turbulent water |
Groot, 1996 |
Salmo trutta fario |
Water with current [Upper parts] |
Flowing or turbulent water |
Ombredane et al, 2001 |
Salmo trutta fario |
Streams, headwaters |
No category |
Scott and Crossman, 1973 |
Salmo trutta fario |
Water velocities of 0.204-0.814 cm/s |
Flowing or turbulent water |
Crisp, 1996 |
Salmo trutta fario |
Riffles od sand and gravel beds |
No category |
Coad, 2006 |
Salmo trutta fario |
Spawn in clear headwaters of large rivers and streams or in tributaries of lakes, also known to spawn over shallow reefs and shoals alog lakes shores, stream spawning fishes use riggle areas |
Stagnant water |
Kerr and Grant, 1999 |
Salmo trutta fario |
Streams |
No category |
Landergren and Vallin, 1998 |
Salmo trutta fario |
Large chalk stream |
No category |
Acornley, 1999 |
Salmo trutta fario |
Spring streams, near sources of spring water |
No category |
Greeley, 1932 |
Salmo trutta fario |
Mot of the streams were first order streams running directly into the sea |
No category |
Jonsson and Jonsson, 2006 |
Salmo trutta fario |
Rivers [Rapid current, 30 to 70/80 cm/s] |
Flowing or turbulent water |
Papala et al, 1998 |
Salmo trutta fario |
Fast water in headwaters or mid-reaches of cool, shaded streams; if denied access to tributaries, spawning occurs on shoals near stream mouths, or elsewhere along shore |
Stagnant water |
Goodyear et al, 1982 |
Salmo trutta fario |
Trout selected slightly shallower and slower flowing spawning site (15-45 cm, 20-55 cm s-1) |
Flowing or turbulent water |
Louhi et al, 2008 |
Salvelinus alpinus |
Current velocities range from 0.2 to 0.8 cm/sec |
Flowing or turbulent water |
Groot, 1996 |
Salvelinus alpinus |
Bottom of lakes with constant and strong current, sometimes in plein water |
Stagnant water |
Billard, 1997 |
Salvelinus alpinus |
Shoals in lakes, quiet pools in rivers |
Stagnant water |
Scott and Crossman, 1973 |
Salvelinus alpinus |
Both lakes and rivers [Water velocities of 0.2-0.7 m/s] |
Stagnant water |
Kerr and Grant, 1999 |
Salvelinus alpinus |
Most spawning takes place in streams [May spawn either in streams or lakes in Labrador] |
Stagnant water |
Bradbury et al, 1999 |
Salvelinus alpinus |
Lakes, river pools |
Stagnant water |
Willson, 1997 |
Salvelinus alpinus |
Pools, or in association with large boulders downstream riffles [Water flow about 1 m/s] |
Flowing or turbulent water |
Beddow et al, 1998 |
Salvelinus alpinus |
Tyrolean lake |
Stagnant water |
Gruber and Wieser, 1983 |
Salvelinus fontinalis |
Near the shoreline (about 3 to 13 m) |
Stagnant water |
Bruslé and Quignard, 2001 |
Salvelinus fontinalis |
Shallows of headwaters of streams but may successfully accomplished in gravelly shallows of lakes if there is a spring upwelling and a moderate current |
Stagnant water |
Scott and Crossman, 1973 |
Salvelinus fontinalis |
Lakes ans streams |
Stagnant water |
Snucins et al, 1992 |
Salvelinus fontinalis |
Stream |
No category |
Curry et al, 1991 |
Salvelinus fontinalis |
Current: 24.2 ± 19.3 cm/s |
Flowing or turbulent water |
Bernier-Bourgault and Magnan, 2002 |
Salvelinus fontinalis |
Typically spawn in streams or in gravel surronding sprin-up-welling areas of lakes and ponds |
Stagnant water |
Groot, 1996 |
Salvelinus fontinalis |
Streams and occasionally in lakes |
Stagnant water |
Bradbury et al, 1999 |
Salvelinus fontinalis |
Streams |
No category |
Coad, 2006 |
Salvelinus fontinalis |
Both lakes and streams, and are closely associated with upwellings or seepages of ground water |
Stagnant water |
Kerr and Grant, 1999 |
Salvelinus fontinalis |
Streams, shoreline reefs |
Stagnant water |
Willson, 1997 |
Salvelinus fontinalis |
Spring streams, near sources of spring water |
No category |
Greeley, 1932 |
Salvelinus fontinalis |
Spawn directly over areas of upwelling groundwater or near spring-fed tributaries |
No category |
Carline, 1980 |
Salvelinus fontinalis |
Groundwater upwelling at redd sites |
No category |
Ridgway and Blanchfiled, 1998 |
Salvelinus fontinalis |
Riffles or pools near headwaters of clear, well-shaded streams, in spring-fed areas with gradient not more than 2%; also along lake shores with moderately swift current, usually near sites of upwellings |
Stagnant water |
Goodyear et al, 1982 |
Salvelinus namaycush |
Inland lakes, rarely in rivers |
Stagnant water |
Scott and Crossman, 1973 |
Salvelinus namaycush |
Mounds |
No category |
Beauchamp et al, 1992 |
Salvelinus namaycush |
Spawn in shallow inshore areas of lakes, rarely in streams [Spawning areas are often exposed to prevaling winds that wave action and water currents keep the area free of sand, silt and detritus] |
Stagnant water |
Bradbury et al, 1999 |
Salvelinus namaycush |
Lakes, streams |
Stagnant water |
Willson, 1997 |
Salvelinus namaycush |
Areas with current, including shorelines, reefs, shoals, ledges, bars, channels, bays, river mouths, and rivers |
Stagnant water |
Goodyear et al, 1982 |
Stenodus leucichthys |
Wide areas |
No category |
Chereshnev et al, 2000 |
Stenodus leucichthys |
Usually in mid and inferior part of big streams |
No category |
Maitland, 1977 |
Stenodus leucichthys |
Streams |
No category |
Willson, 1997 |
Thymallus thymallus |
Strong current : 40 to 70 cm/s |
Flowing or turbulent water |
Bruslé and Quignard, 2001 |
Thymallus thymallus |
Water velocities: about 20cm/s |
Flowing or turbulent water |
Poncin, 1996 |
Thymallus thymallus |
In small rivers, where water accelerates (40-60 cm/s) |
Flowing or turbulent water |
Persat, 2001 |
Thymallus thymallus |
Stream-dwelling, mean velocity 47.8 cm/s |
Flowing or turbulent water |
Sempeski and Gaudin, 1995 |
Thymallus thymallus |
40-70 cm/s |
Flowing or turbulent water |
Nykänen and Huusko, 2002 |
Thymallus thymallus |
Mean velocities of 40-70 |
Flowing or turbulent water |
Nykänen et al, 2004 |
Thymallus thymallus |
Spawn up rivers and streams, most often small clean tributaries |
No category |
Witkowski and Kowalewski, 1988 |
Thymallus thymallus |
Upstream border of a shallow riffle, varied between 0.33-0.46 m/s |
Flowing or turbulent water |
Meyer, 2001 |
Thymallus thymallus |
Fast-flowing tributaries, streams [Water velocities range from 23 to 90 cm/s] |
Flowing or turbulent water |
Northcote, 1995 |
Thymallus thymallus |
Mostly on the top of gravel riffles in water so shallow that the backs of the spawning fish broke the water surface |
No category |
Crisp, 1996 |
Thymallus thymallus |
European grayling are mainly a river fish, but those in slow flowing parts of rivers migrate to faster flowing tributaries near spawning time, and lae populations all depend on streams for spawning |
Flowing or turbulent water |
Northcote, 1993 |
Thymallus thymallus |
The coastal shoals, and offshore bars with gravel and gravel-boulder substrate serve as spawning grounds. As a rule, these parts have the most intensive circulation of water masses. |
Stagnant water |
Zaytsev, 1987 |
Thymallus thymallus |
Dans un courant rapide (0.75 m par seconde) |
Flowing or turbulent water |
Vivier, 1958 |
Thymallus arcticus |
Small tributaries, if not available spawning takes place in gravelly to rocky parts of the main river [Sometimes occurs in mud-bottomed vegetated poools below rapids] |
No category |
Scott and Crossman, 1973 |
Thymallus arcticus |
Tributaries |
No category |
Fishbase, 2006 |
Thymallus arcticus |
Use mainstream river tributaries and sidechannels, rarely in lakes [Flows of 0.5-1.0 m/s] |
Stagnant water |
Northcote, 1995 |
Thymallus arcticus |
Mainstream river tributaries and side-channels, tributary streams, also in lakes |
Stagnant water |
Northcote, 1993 |
Thymallus arcticus |
Spawning in lake Agnes occurs primarily in the largest inlet stream, with minor spawning activity in two smaller inlet streams an possibly along shawllow shoreline areas. Spawning in Deer Lake appears to occur only in the outlet stream |
Stagnant water |
Kaya, 1989 |
Thymallus arcticus |
The spawning area of Providence Creek was a depper part of the stream just below a riffle used as a feeding area, the current about 25 feet per second |
Flowing or turbulent water |
Bishop, 1971 |
Cottus gobio |
Creek, stream |
No category |
Marconato and Bisazza, 1988 |
Cottus gobio |
Tributaries, reaches with relatively steep river slope |
No category |
Abdoli et al, 2005 |
Ameiurus nebulosus |
Prefer shallow weedy areas of streams and lakes, most spawning probably occur in nontidal freshwater |
Stagnant water |
Internet, 2005 |
Ameiurus nebulosus |
Usually around the shores of lakes, or in coves, bays or creek mouths |
Stagnant water |
Scott and Crossman, 1973 |
Ameiurus nebulosus |
Near shoreline |
Stagnant water |
Kerr and Grant, 1999 |
Ameiurus nebulosus |
Marches in bays, harbors, coves, creek mouths, and lower reaches of creeks; also rivers with overhanging banks and abudant deadfall |
No category |
Goodyear et al. et al, 1982 |
Ictalurus punctatus |
Spawning takes place in seculed, semidark nests; they will not spawn in transparent ponds |
Stagnant water |
Scott and Crossman, 1973 |
Ictalurus punctatus |
Ponds |
Stagnant water |
Grizzle, 1985 |
Ictalurus punctatus |
Nearshore areas, including wetlands, marshes, bays, harbors, and creek mouths, backwaters, pools, and shoals in rivers, especially areas of strong current |
Stagnant water |
Goodyear et al. et al, 1982 |
Silurus glanis |
Spawn in Amudar'ya River, its backwaters and lakes adjacent to the river |
Stagnant water |
Zholdasova and Guseva, 1987 |
Silurus glanis |
Between plants, often near roots of trees |
Stagnant water |
Bruslé and Quignard, 2001 |
Silurus glanis |
Fish spawning out of the tributary area: carp, pikeperch, catfish Silurus glanis and eel |
No category |
Hladik and Kubecka, 2003 |
Osmerus eperlanus |
Enters rivers and spawns at high tide, some spawn near river mouths and do not ascend the rivers [Water velocity is about 0.3-2 m/s] |
Flowing or turbulent water |
Belyanina, 1969 |
Osmerus eperlanus |
In coastal streams, most smelt spawn above the tide. [Significant positive relationships between survival to the early-eyed stage and increasing water velocity (up to 60-80 cm/s)] |
Flowing or turbulent water |
Buckley, 1989 |
Osmerus eperlanus |
In freswater, near the tidal zone |
No category |
Billard, 1997 |
Osmerus eperlanus |
Spawning takes place in fresh water, usually, but not always, somewhere near the end of tide where there is a significant current |
Flowing or turbulent water |
Maitland, 2003 |
Osmerus eperlanus |
The fish usually congregate in the lower reaches of these rivers for a number of days prior to moving upstream to spawn [Spawning areas correspond to the maximum tidal influence on the river] |
No category |
Quigley et al, 2004 |
Osmerus eperlanus |
Lower reaches of streams, deeper parts of lakes |
Stagnant water |
Fishbase, 2006 |