Abstract
Availability of iron limits productivity in the Southern Ocean where vast regions of high-nitrogen low-chlorophyll conditions are punctuated by hotspots of production surrounding the subAntarctic islands. Here, we compare patterns in accumulation of iron, as indicated by [Fe] and Fe : C (from Wing et al. 2014), with proxies for uptake of iron within food webs, as indicated by Fe : Al and delta Fe-56 within the subAntarctic Auckland Island ecosystem. We compare these proxies for dynamics of iron within egested material collected from six seabird species, representing three distinct foraging guilds. Fractions of biogenic iron, estimated from Fe : Al, were lowest in the coastal foraging guild (0.83 +/- 0.01), and higher in the oceanic and predator guilds (0.94 +/- 0.01 and 0.95 +/- 0.01), consistent with high rates of biological recycling. The isotopic ratio of iron Fe-56/Fe-54, reported as delta Fe-56, is depleted in the heavy isotope Fe-56 by recycling in the microbial loop, and is likely further depleted in Fe-56 when taken up by animals within the food web. delta Fe-56 was most negative for the oceanic foraging group indicating intensive recycling (-1.16 +/- 0.16 parts per thousand), most positive in the coastal group where direct lithogenic sources of iron are more available (-0.14 +/- 0.15 parts per thousand), and intermediate in the predatory group, representing a mixture and possible fractionation within food webs (-0.37 +/- 0.14 parts per thousand). These data reveal strong contrasts in bioaccumulation and recycling of iron between coastal and oceanic food webs, and important interactions between marine food web structure and biogeochemical processes supporting productivity in the Southern Ocean.