2013
DOI: 10.1134/s0032945213010116
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Transition to viviparity in the order Scorpaeniformes: Brief review

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Cited by 17 publications
(11 citation statements)
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“…). Ocean perch are live‐bearing (Pavlov and Emel'yanova ) and have a winter reproductive period with fertilization occurring in May/June, followed by gestation through the winter and parturition in October/November (Park ). The timing of increases in otolith Sr:Ca corresponds with gestation and parturition, and it is possible the seasonal environmental signal (i.e., upwelling) aliases the underlying cause of Sr:Ca fluctuation in ocean perch otoliths.…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…). Ocean perch are live‐bearing (Pavlov and Emel'yanova ) and have a winter reproductive period with fertilization occurring in May/June, followed by gestation through the winter and parturition in October/November (Park ). The timing of increases in otolith Sr:Ca corresponds with gestation and parturition, and it is possible the seasonal environmental signal (i.e., upwelling) aliases the underlying cause of Sr:Ca fluctuation in ocean perch otoliths.…”
Section: Discussionmentioning
confidence: 99%
“…a) at depths between 43 and 119 m (mean 80 m). Ocean perch are lecithotrophic (live bearing; Pavlov and Emel'yanova ) and demersal as both juveniles and adults (Park , Smith et al. ).…”
Section: Methodsmentioning
confidence: 99%
“…While the females of S. guttata , from the Southern Californian Bight, and S. porcus also grow to a larger size than their males, further paralleling the situation with N. pandus , the reverse is true for S. cardinalis and S. notata . The large disparity in the I GS values between females and males of N. pandus and other Scorpaena species may be an adaptation towards a reproductive strategy of internal fertilization exhibited by the closely related Helicolenus and Sebastes ( e.g ., Sequeira et al ., 2003; Wourms, 1991), as this strategy does not require males to produce/store large volumes of sperm (Pavlov & Emel'yanova, 2013).…”
Section: Discussionmentioning
confidence: 99%
“…Base maps and transects generated using Ocean Data View software (Schlitzer et al, 2015). (Data sources for A: Bostock et al, 2013;Ganachaud et al, 2014;Qu et al, 2009;Ridgway and Dunn, 2003;Sokolov and Rintoul, 2000. ) southwest Pacific Ocean; (ii) compare the linear increase of regional otolith-based 14 C curves for the southwest Pacific Ocean to examine temporal 14 C transport through the water column; and (iii) present a compilation of regional otolith, coral and atmospheric 14 C curves for the southwest Pacific Ocean to examine temporal trends in 14 C transport.…”
Section: Oceanographic Setting Of the Southwest Pacific Oceanmentioning
confidence: 99%
“…1A). The Australia/New Zealand region of the southern Pacific Ocean is primarily influenced by the South Equatorial Current (SEC) of the South Pacific Gyre (SPG) transporting three main water masses: Upper Thermocline Waters (UTW, σ θ ∼ 24.5; origin: subducted centre of SPG), Lower Thermocline Waters (LTW, σ θ ∼ 26.2; origin: subducted in part northeast of New Zealand) and Southeast Pacific Antarctic Intermediate Water (SP AAIW, σ θ ∼ 27.1; origin: sub- Bostock et al, 2013;Qu et al, 2009). The SEC turns south as it nears Australia and becomes the East Australian Current (EAC), the highly variable, western boundary current of the SPG.…”
Section: Oceanographic Setting Of the Southwest Pacific Oceanmentioning
confidence: 99%