δ56Fe in seabird guano reveals extensive recycling of iron in the Southern Ocean ecosystem
Autor: | Melanie Gault-Ringold, Stephen R. Wing, Russell D. Frew, Lucy C. Wing, O. A. Shatova, Claudine H. Stirling |
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Rok vydání: | 2017 |
Předmět: |
0106 biological sciences
010504 meteorology & atmospheric sciences Ecology 010604 marine biology & hydrobiology Foraging Aquatic Science Biology Oceanography 01 natural sciences Food web Productivity (ecology) Guild Guano Marine ecosystem Ecosystem Microbial loop 0105 earth and related environmental sciences |
Zdroj: | Limnology and Oceanography. 62:1671-1681 |
ISSN: | 1939-5590 0024-3590 |
Popis: | 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 δ56Fe 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 56Fe/54Fe, reported as δ56Fe, is depleted in the heavy isotope 56Fe by recycling in the microbial loop, and is likely further depleted in 56Fe when taken up by animals within the food web. δ56Fe was most negative for the oceanic foraging group indicating intensive recycling (−1.16 ± 0.16‰), most positive in the coastal group where direct lithogenic sources of iron are more available (−0.14 ± 0.15‰), and intermediate in the predatory group, representing a mixture and possible fractionation within food webs (−0.37 ± 0.14‰). 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. |
Databáze: | OpenAIRE |
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