Benthic faunal assimilation pathways and depth-related changes in food-web structure across the Canadian Arctic. (August 2015)

• Record Type: Journal Article
• Authors: Roy, Virginie; Iken, Katrin; Gosselin, Michel; Tremblay, Jean-Éric; Bélanger, Simon; Archambault, Philippe
• Is Part Of: Deep sea research. Volume 102(2015)
• Page Start: 55
• Page End: 71
• Publication Date: 2015-08
• Subjects: Stable isotopes -- Benthos -- Food web -- Arctic -- Sea-ice algae -- Depth; Oceanography -- Periodicals; Océanographie -- Périodiques; 551.4605
• DOI: 10.1016/j.dsr.2015.04.009
• Languages: English
• ISSNs: 0967-0637

Abstract

Abstract: Climate changes in the Arctic are expected to decrease the currently tight pelagic–benthic coupling, yet large-scale, regional understanding of the origin of food for benthic organisms across both biological productivity and depth gradients is still missing. The organic matter assimilation pathways of benthic organisms, along with food-web structure, were investigated at shelf and slope locations spanning 2000 km across the Canadian Arctic using stable carbon and nitrogen isotope analysis. Three potential food sources and over 75 benthic taxa belonging to four feeding guilds were analyzed, but the δ 13 C end-members for the benthic food-webs could not be clearly discerned. While spatial patterns of δ 13 C for pelagic particulate organic matter were linked to phytoplankton biomass at the time of sampling, sediment δ 13 C values reflected the relative composition of terrestrial and marine organic matter. On average, benthic primary consumers were enriched in 13 C by 5 and 7‰ compared to the potential organic matter sources sampled in sediment and the water column, respectively. The δ 13 C discrepancy between identified sources of organic matter and benthic organisms suggests that an uncharacterized food source provided a significant carbon source to these animals. We propose that the 13 C enrichment of benthic organisms may be largely caused by the assimilation of ice algae (which were not sampled in this study), particularly in regions of known high ice-algal standing stock such as Barrow Strait and Eclipse Sound. The δ 15 N values of bottom-water particulate organic matter and of benthic primary consumers increased with depth due to greater degradation of the settling organic material. The δ 15 N values of secondary consumers did not increase with depth, leading to a decrease of their trophic position compared with shallower regions and likely reflecting an increase in omnivory due to scarcity of prey at depth. This study emphasizes the potential importance of sea-ice algae as a carbon source for benthic communities in the Canadian Arctic and suggests that distinct food-web structures prevail over the shelf and slope. Highlights: We examine C and N stable isotope ratios of various food sources and benthic feeding guilds. Primary consumer C stable isotope ratios are as high as reported for ice algae. Highest benthic faunal C stable isotope ratios overlap with recorded areas of maximal ice-algal biomass. Primary consumers assimilate degraded organic matter as water depth increase. Secondary consumers likely increase their level of omnivory with depth.