Near-future ocean acidification does not alter the lipid content and fatty acid composition of adult Antarctic krill

Euphausia superba (Antarctic krill) is a keystone species in the Southern Ocean, but little is known about how it will respond to climate change. Ocean acidification, caused by sequestration of carbon dioxide into ocean surface waters (pCO₂), alters the lipid biochemistry of some organisms. This can have cascading effects up the food chain. In a year-long laboratory experiment adult krill were exposed to ambient seawater pCO₂ levels (400 μatm), elevated pCO₂ levels mimicking near-future ocean acidification (1000, 1500 and 2000 μatm) and an extreme pCO₂ level (4000 μatm). Total lipid mass (mg g⁻¹ DM) of krill was unaffected by near-future pCO₂. Fatty acid composition (%) and fatty acid ratios associated with immune responses and cell membrane fluidity were also unaffected by near-future pCO₂, apart from an increase in 18:3n-3/18:2n-6 ratios in krill in 1500 μatm pCO₂ in winter and spring_. Extreme pCO₂ had no effect on krill lipid biochemistry during summer. During winter and spring, krill in extreme pCO₂ had elevated levels of 18:2n-6 (up to 1.2% increase), 20:4n-6 (up to 0.8% increase), lower 18:3n-3/18:2n-6 and 20:5n-3/20:4n-6 ratios, and showed evidence of increased membrane fluidity (up to three-fold increase in phospholipid/sterol ratios). These results indicate that the lipid biochemistry of adult krill is robust to near-future ocean acidification.