Dependency of Antarctic zooplankton species on ice algae-produced carbon suggests a sea ice-driven pelagic ecosystem during winter

摘要

How the abundant pelagic life of the Southern Ocean survives winter darkness, when the sea is covered by pack ice and phytoplankton production is nearly zero, is poorly understood. Ice-associated (sympagic) microalgae could serve as a high-quality carbon source during winter, but their significance in the food web is so far unquantified. To better understand the importance of ice algae-produced carbon for the overwintering of Antarctic organisms, we investigated fatty acid (FA) and stable isotope compositions of 10 zooplankton species, and their potential sympagic and pelagic carbon sources. FA-specific carbon stable isotope compositions were used in stable isotope mixing models to quantify the contribution of ice algae-produced carbon ((Ice)) to the body carbon of each species. Mean (Ice) estimates ranged from 4% to 67%, with large variations between species and depending on the FA used for the modelling. Integrating the (Ice) estimates from all models, the sympagic amphipod Eusirus laticarpus was the most dependent on ice algal carbon ((Ice): 54%-67%), and the salp Salpa thompsoni showed the least dependency on ice algal carbon ((Ice): 8%-40%). Differences in (Ice) estimates between FAs associated with short-term vs. long-term lipid pools suggested an increasing importance of ice algal carbon for many species as the winter season progressed. In the abundant winter-active copepod Calanus propinquus, mean (Ice) reached more than 50% in late winter. The trophic carbon flux from ice algae into this copepod was between 3 and 5mgCm(-2)day(-1). This indicates that copepods and other ice-dependent zooplankton species transfer significant amounts of carbon from ice algae into the pelagic system, where it fuels the food web, the biological carbon pump and elemental cycling. Understanding the role of ice algae-produced carbon in these processes will be the key to predictions of the impact of future sea ice decline on Antarctic ecosystem functioning.