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- W1973596711 abstract "The late Dr. M. W. Johnson studied Panulirus interruptus phyllosome larval natural history from samples collected between 1949 and 1955 inclusive on the California Cooperative Oceanic Fisheries Investigations (CalCOFI) grid. Despite wide broadcasting of larvae, he concluded that gyres and countercurrents must retain larvae to ensure recruitment to the population. The conclusions are reviewed and the data reinterpreted in light of both recent physical oceanographic information and congeneric biology. Phyllosome concentrations are highly aggregated within the California Current: 66% of the larvae were located in 12% of the areal distribution, with the concentrations located off central Baja California. Stage I larvae cooccurred nearshore in areas of moderate Ekman wind drift. They were quickly (about 13 d) transported southward, likely by the California Current, to a perennially occurring, semipermanent gyre. Phyllosome maturation to stage VIII occurred over a 5-mo period within the gyre. Late-stage (IX–XI) concentrations occurred slightly northwest of the gyre, possibly transported by the counter-flowing Davidson Current. Pueruli were rarely encountered, suggesting a deepwater (> 140 m) distribution. Onshore movement is likely made by the puerulus stage. Phyllosome concentrations in the Southern California Bight were rare (stage IV only). Evidence is presented to support the hypothesis that recruitment to this northern, relatively impoverished brood stock area may be episodic, influenced by the large-scale, interannual El Niño events." @default.
- W1973596711 created "2016-06-24" @default.
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- W1973596711 date "1986-11-01" @default.
- W1973596711 modified "2023-09-27" @default.
- W1973596711 title "California Spiny Lobster (<i>Panulirus interruptus</i>) Larval Retention and Recruitment: A Review and Synthesis" @default.
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- W1973596711 doi "https://doi.org/10.1139/f86-263" @default.
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