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Metabolic physiology of the Humboldt squid, Dosidicus gigas: Implications for vertical migration in a pronounced oxygen minimum zone

The Humboldt (or jumbo) squid, Dosidicus gigas, is an active predator endemic to the Eastern Pacific that undergoes diel vertical migrations into a pronounced oxygen minimum layer (OML). Here, we investigate the physiological mechanisms that facilitate these migrations and assess the associated cost...

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Published in:Progress in oceanography 2010-07, Vol.86 (1-2), p.72-80
Main Authors: Rosa, Rui, Seibel, Brad A
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description The Humboldt (or jumbo) squid, Dosidicus gigas, is an active predator endemic to the Eastern Pacific that undergoes diel vertical migrations into a pronounced oxygen minimum layer (OML). Here, we investigate the physiological mechanisms that facilitate these migrations and assess the associated costs and benefits. Exposure to hypoxic conditions equivalent to those found in the OML (-10 mu M O sub(2) at 10 degree C) led to a significant reduction in the squid's routine metabolic rate (RMR), from 8.9 to 1.6 mu mol O sub(2) g super(-1) h super(-1) (p
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RMR increased significantly with temperature (p &lt;0.05), from 8.9 (at 10 degree C) to 49.85 mu mol O sub(2) g super(-1) h super(-1) (at 25 degree C) which yielded a Q sub(10) of 2.0 between 10 and 20 degree C and 7.9 between 20 and 25 degree C (p &lt;0.05). These results suggest that 25 degree C, although within the normal surface temperature range in the Gulf of California, is outside this species' normal temperature range. By following the scattering layer into oxygen-enriched shallow water at night, D. gigas may repay any oxygen debt accumulated during the daytime. The dive to deeper water may minimize exposure to stressful surface temperatures when most prey have migrated to depth during the daytime. 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RMR increased significantly with temperature (p &lt;0.05), from 8.9 (at 10 degree C) to 49.85 mu mol O sub(2) g super(-1) h super(-1) (at 25 degree C) which yielded a Q sub(10) of 2.0 between 10 and 20 degree C and 7.9 between 20 and 25 degree C (p &lt;0.05). These results suggest that 25 degree C, although within the normal surface temperature range in the Gulf of California, is outside this species' normal temperature range. By following the scattering layer into oxygen-enriched shallow water at night, D. gigas may repay any oxygen debt accumulated during the daytime. The dive to deeper water may minimize exposure to stressful surface temperatures when most prey have migrated to depth during the daytime. The physiological and ecological strategies demonstrated here may have facilitated the recent range expansion of this species into northern waters where expanding hypoxic zones prohibit competing top predators.</abstract><doi>10.1016/j.pocean.2010.04.004</doi><tpages>9</tpages></addata></record>
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subjects Daytime
Ecology
Marine
Migration
Physiology
Predators
Reduction
Squid
Stores
Surface temperature
title Metabolic physiology of the Humboldt squid, Dosidicus gigas: Implications for vertical migration in a pronounced oxygen minimum zone
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