Abstract

Abstract. The size distribution and mean spatial trends of large particles (>100 μm, in equivalent spherical diameter, ESD) and mesozooplankton were investigated across the Mackenzie Shelf (southeast Beaufort Sea, Arctic Ocean) in July–August 2009. Our main objective was to combine results from an Underwater Vision Profiler 5 (UVP5) and traditional net tows (200 μm mesh size) to characterize the structural diversity and functioning of the Arctic shelf-basin ecosystem and to assess the large-scale correspondence between the two methodological approaches. The core dataset comprised 154 UVP5 profiles and 29 net tows conducted in the shelf (<100 m isobath), slope (100–1000 m) and basin (>1000 m) regions of the study area. The mean abundance of total particles and zooplankton in the upper water column (<75 m depth) declined exponentially with increasing distance from shore. Vertical and latitudinal patterns in total particle concentration followed those of chlorophyll a (chl a) concentration, with maximum values between 30 and 70 m depth. Based on the size-spectra derived from the UVP5 dataset, living organisms (0.1–10 mm ESD) accounted for an increasingly large proportion of total particle abundance (from 0.1 % to >50 %) when progressing offshore and as the ESD of particles was increasing. Both the UVP5 and net tows determined that copepods dominated the zooplankton community (~78–94 % by numbers) and that appendicularians were generally the second most abundant group (~1–11 %). The vertical distribution patterns of copepods and appendicularians indicated a close association between primary production and the main grazers. Manual taxonomic counts and ZooScan image analyses shed further light on the size-structure and composition of the copepod community – which was dominated at ~95 % by a guild of 10 typical taxa. The size distributions of copepods, as evaluated with the 3 methods (manual counts, ZooScan and UVP5), showed consistent patterns co-varying in the same order of magnitude over the upper size range (>1 mm ESD). Copepods <1 mm were not well quantified by the UVP5, which estimated that only ~13–25 % of the assemblage was composed of copepods <1 mm ESD compared with ~77–89 % from the net tow estimates. However, the biovolume of copepods was overwhelmingly dominated (~93–97 %) by copepods >1 mm ESD. Our results illustrate that the combination of traditional sampling methods and automated imaging techniques is a powerful approach that enabled us to conclude on the prevalence of a relatively high productivity regime and dominant herbivorous food web over the shelf when compared with the low-productive recycling system detected offshore.

Highlights

  • Particles in aquatic systems can be divided in two fundamental groups: living and non-living.Size of non-living particles is the net result of aggregation and destruction processes, which include a large variety of physical and biological mechanisms such as coagulation, packaging, consumption, dissolution and fragmentation

  • The particle size distribution (PSD) of non-living particles is instructive for vertical flux studies if the settling velocity of observed particles is known (e.g. McDonnell and Buesseler, 2010) or if the PSD can be related to sediment trap measurements (e.g. Guidi et al, 2008; Iversen et al, 2010)

  • This study investigated the PSD of large particles >100 μm across the shelf-slope-basin interface in the southeast Beaufort Sea (Arctic Ocean) in late July–August 2009 (Fig. 1)

Read more

Summary

Introduction

Size of non-living particles (named marine snow for sizes >500 μm; Suzuki and Kato, 1953) is the net result of aggregation and destruction processes, which include a large variety of physical and biological mechanisms such as coagulation, packaging, consumption, dissolution and fragmentation (see Burd and Jackson, 2009 for a review). The particle size distribution (PSD) of non-living particles is instructive for vertical flux studies if the settling velocity of observed particles is known Knowledge on the contribution of living particles to the total particle pool and on the plankton size distribution is essential if the dynamics of downward carbon export and trophic energy fluxes are to be adequately understood and modeled in marine ecosystems. Information on the variability of the size spectrum of particles support the characterization of various ecological processes and is key to our comprehension of the structure and function of pelagic food webs (e.g. Platt and Denman, 1978; Legendre and Michaud, 1998; Stemmann and Boss, 2012)

Methods
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call