Dissolved organic carbon (DOC) is essential to balance the metabolic demands of North-Atlantic deep-sea sponges
Creators
- 1. Department of Freshwater and Marine Ecology, Institute for Biodiversity and Ecosystem Dynamics (IBED), University of Amsterdam, Amsterdam, Netherlands
- 2. Department of Freshwater and Marine Ecology, Institute for Biodiversity and Ecosystem Dynamics (IBED), University of Amsterdam, Amsterdam, Netherlands; Royal Netherlands Institute for Sea Research (NIOZ), Den Burg, Netherlands
- 3. Department of Fisheries and Oceans (DFO), Bedford Institute of Oceanography, Dartmouth, Nova Scotia, Canada; Faculty of Science, Dalhousie University, Halifax, Nova Scotia, Canada
- 4. Department of Marine Animal Ecology, University of Wageningen, Wageningen, Netherlands
- 5. Department of Fisheries and Oceans (DFO), Bedford Institute of Oceanography, Dartmouth, Nova Scotia, Canada
- 6. GEOMAR Helmholtz Centre for Ocean Research, Kiel, Germany
- 7. Department of Biological Sciences, University of Bergen, Bergen, Norway
Description
ABSTRACT
Sponges are ubiquitous components of various deep-sea habitats, including cold water coral reefs and deep-sea sponge grounds. Despite being surrounded by oligotrophic waters, these ecosystems are known to be hotspots of biodiversity and carbon cycling. To assess the role of sponges in the carbon cycling of deep-sea ecosystems, we studied the energy budgets of six dominant deep-sea sponges (the hexactinellid species Vazella pourtalesi, and demosponge species Geodia barretti, Geodia atlantica, Craniella zetlandica, Hymedesmia paupertas and Acantheurypon spinispinosum) in an ex situ aquarium setup. Additionally, we determined morphological metrics for all species (volume, dry weight (DW), wet weight (WW), carbon (C) content, and ash-free dry weight (AFDW)) and provide species-specific conversion factors. Oxygen (O2) removal rates averaged 3.3 ± 2.8 µmol O2 DWsponge h−1 (all values mean ± SD), live particulate (bacterial and phytoplankton) organic carbon (LPOC) removal rates averaged 0.30 ± 0.39 µmol C DWsponge h−1 and dissolved organic carbon (DOC) removal rates averaged 18.70 ± 25.02 µmol C DWsponge h−1. Carbon mass balances were calculated for four species (V. pourtalesi, G. barretti, G. atlantica and H. paupertas) and revealed that the sponges acquired 1.3–6.6 times the amount of carbon needed to sustain their minimal respiratory demands. These results indicate that irrespective of taxonomic class, growth form, and abundance of microbial symbionts, DOC is responsible for over 90 % of the total net organic carbon removal of deep-sea sponges and allows them to sustain in otherwise food-limited environments on the ocean floor.
Notes
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Bart et al 2020- 2020.09.21.305086v1.full.pdf
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Additional details
Related works
- Is derived from
- Journal article: https://aslopubs.onlinelibrary.wiley.com/doi/full/10.1002/lno.11652 (URL)
- Is supplement to
- Other: https://www.biorxiv.org/content/10.1101/2020.09.21.305086v1.supplementary-material (URL)
- Is supplemented by
- Figure: https://www.biorxiv.org/content/10.1101/2020.09.21.305086v1.supplementary-material (URL)
Funding
- SponGES – Deep-sea Sponge Grounds Ecosystems of the North Atlantic: an integrated approach towards their preservation and sustainable exploitation 679849
- European Commission
- SPONGE ENGINE – Fast and efficient sponge engines drive and modulate the food web of reef ecosystems 715513
- European Commission