Abstract

Abstract. Megafaunal organisms play a key role in ecosystem functioning in the deep-sea through bioturbation, bioirrigation and organic matter cycling. At 3500 m water depth in the Nazaré Canyon, NE Atlantic, very high abundances of the infaunal holothurian Molpadia musculus were observed. To quantify the role of M. musculus in sediment cycling, sediment samples and holothurians were collected using an ROV and in situ experiments were conducted with incubation chambers. The biochemical composition of the sediment (in terms of proteins, carbohydrates and lipids), the holothurians' gut contents and holothurians' faecal material were analysed. In the sediments, proteins were the dominant organic compound, followed by carbohydrates and lipids. In the holothurian's gut contents, protein concentrations were higher than the other compounds, decreasing significantly as the material passed through the digestive tract. Approximately 33±1% of the proteins were digested by the time sediment reached the mid gut, with a total digestion rate equal to 67±1%. Carbohydrates and lipids were ingested in smaller amounts and digested with lower efficiencies (23±11% and 50±11%, respectively). As a result, the biopolymeric C digestion rate was on average 62±3%. We estimated that the population of M. musculus could remove approximately 0.49±0.13 g biopolymeric C and 0.13±0.03 g N m−2 d−1 from the sediments. These results suggest that M. musculus plays a key role in the benthic tropho-dynamics and biogeochemical processes in the Nazaré Canyon.

Highlights

  • The deep sea is the largest ecosystem on Earth, covering about 60% of the globe’s surface

  • Deep-sea ecosystems provide the largest reservoirs of biomass and non-renewable resources (Gage and Tyler, 1991), which are linked to their biodiversity (Danovaro et al, 2008b)

  • The aim of our study is to understand the role of M. musculus in the ecosystem functioning of the Nazare Canyon at 3500 m

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Summary

Introduction

The deep sea is the largest ecosystem on Earth, covering about 60% of the globe’s surface. Deep-sea ecosystems provide the largest reservoirs of biomass and non-renewable resources (Gage and Tyler, 1991), which are linked to their biodiversity (Danovaro et al, 2008b). They act as the ultimate sink for organic material derived from the upper ocean’s primary production and are essential in the biogeochemical cycling of organic matter (OM) on a global scale (Dell’Anno and Danovaro, 2005; Danovaro et al, 2008a). Biodiversity is high as a result of their topographic complexity and spatio-temporal variability (Bianchelli et al, 2008; Ingels et al, 2009; Tyler et al, 2009; Vetter et al, 2010). Knowledge of their ecological functioning (e.g., community respiration, productivity, nutrient cycling, OM supply and remineralisation rates) are largely unknown

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