Intra- and interspecific differences in palatability of Arctic macroalgae from Kongsfjorden (Spitsbergen) for two benthic sympatric invertebrates

Information on herbivore–macroalgae interactions is extremely scarce for Arctic habitats. In this study, the potential of 19 macroalgae as food source for herbivores was investigated for the first time in Arctic waters (Kongsfjorden, Spitsbergen) with emphasis on algal defense against grazing. Only two of the 19 tested macroalgae-associated invertebrates consumed macroalgae in measurable amounts, the locally abundant green sea urchin Strongylocentrotus droebachiensis (OF Müller) and the amphipod Gammarellus homari (JC Fabricius). In the inner basin of the fjord, the dense macroalgal stock represents a potential food source. However, in this area, herbivory plays only a minor role. In contrast, in the outer basin of Kongsfjorden S. droebachiensis exerts a strong top-down control on macroalgal assemblages.Laboratory feeding assays in the with the two herbivores showed grazer-specific feeding preferences. The amphipod G. homari exhibits a preference for delicate red algal species like Devaleraea ramentacea, whereas the sea urchin S. droebachiensis significantly preferred more leathery seaweeds like Laminaria and Alaria. The red alga Palmaria palmata is a very attractive food for both herbivores, while the brown alga Desmarestia viridis and the red alga Ptilota gunneri are among the least preferred algae. To distinguish between physical and tissue-specific plant properties, which have a deterring or stimulating effect on the grazing behaviour, both grazers were offered intact algal tissue and artificial food in separate feeding assays. While physical and tissue-specific plant properties–especially in the Laminariales–deterred G. homari, these properties did not deter S. droebachiensis.This study provides insights into herbivore consumption in the benthic food web of Kongsfjorden. As a general potential top-down factor controlling primary production, herbivory needs to be quantified further in Kongsfjorden to develop adequate carbon flow models for this important reference site for the study of climate change on high latitude marine ecosystems.