The role of diatom resting spores for pelagic-benthic coupling in the Southern Ocean

<jats:p>Abstract. Natural iron fertilization downstream of Southern Ocean island plateaus support large phytoplankton blooms and promote carbon export from the mixed layer. In addition to sequestering atmospheric CO2, the biological carbon pump also supplies organic matter (OM) to deep-ocean e...

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Main Authors: Rembauville, Mathieu, Blain, Stéphane, Manno, Clara, Tarling, Geraint, Thompson, Anu, Wolff, George, Salter, Ian
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus GmbH 2018
Subjects:
Online Access:http://livrepository.liverpool.ac.uk/3020642/
http://livrepository.liverpool.ac.uk/3020642/1/bg-2017-414_Final_Submission.pdf
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spelling ftunivliverpool:oai:livrepository.liverpool.ac.uk:3020642 2023-05-15T13:59:07+02:00 The role of diatom resting spores for pelagic-benthic coupling in the Southern Ocean Rembauville, Mathieu Blain, Stéphane Manno, Clara Tarling, Geraint Thompson, Anu Wolff, George Salter, Ian 2018-04-21 text http://livrepository.liverpool.ac.uk/3020642/ http://livrepository.liverpool.ac.uk/3020642/1/bg-2017-414_Final_Submission.pdf en eng Copernicus GmbH http://livrepository.liverpool.ac.uk/3020642/1/bg-2017-414_Final_Submission.pdf Rembauville, Mathieu, Blain, Stéphane, Manno, Clara, Tarling, Geraint, Thompson, Anu, Wolff, George and Salter, Ian (2018) The role of diatom resting spores for pelagic-benthic coupling in the Southern Ocean. Article NonPeerReviewed 2018 ftunivliverpool 2022-04-25T09:15:42Z <jats:p>Abstract. Natural iron fertilization downstream of Southern Ocean island plateaus support large phytoplankton blooms and promote carbon export from the mixed layer. In addition to sequestering atmospheric CO2, the biological carbon pump also supplies organic matter (OM) to deep-ocean ecosystems. Although the total flux of OM arriving at the seafloor sets the energy input to the system, the chemical nature of OM is also of significance. However, a quantitative framework linking ecological flux vectors to OM composition is currently lacking. In the present study we report the lipid composition of export fluxes collected by five-moored sediment traps deployed in contrasting productivity regimes of Southern Ocean island systems (Kerguelen, Crozet and South Georgia) and compile them with quantitative data on diatom and fecal pellet fluxes. At the three naturally iron fertilized sites, the relative contribution of labile lipids (mono- and polyunsaturated fatty acids, unsaturated fatty alcohols) is 2–4 times higher than at low productivity sites. There is a strong attenuation of labile components as a function of depth, irrespective of productivity. The three island systems also display regional characteristics in lipid export. The diversity of sterols is greater in the relatively warm waters of the Polar Frontal Zone when compared to the Antarctic zone, reflecting the transition from mixed phytoplankton communities to principally diatom-derived OM. An enrichment of zooplankton dietary sterols, such as C27Δ5, at South Georgia is consistent with high zooplankton and krill biomass in the region and the importance of fecal pellets to POC flux. There is a strong association of diatom resting spore fluxes that dominate productive flux regimes with energy rich unsaturated fatty acids. At the Kerguelen Plateau we provide a statistical framework to link seasonal variation in ecological flux vectors and lipid composition over a complete annual cycle. Our analyses demonstrate that ecological processes in the upper ocean, e.g. resting spore formation and grazing, not only impact the magnitude and stoichiometry of the Southern Ocean biological pump, but also regulate the composition of exported OM and the nature of pelagic-benthic coupling. </jats:p> Article in Journal/Newspaper Antarc* Antarctic Southern Ocean Ocean Island The University of Liverpool Repository Antarctic Kerguelen Southern Ocean The Antarctic
institution Open Polar
collection The University of Liverpool Repository
op_collection_id ftunivliverpool
language English
description <jats:p>Abstract. Natural iron fertilization downstream of Southern Ocean island plateaus support large phytoplankton blooms and promote carbon export from the mixed layer. In addition to sequestering atmospheric CO2, the biological carbon pump also supplies organic matter (OM) to deep-ocean ecosystems. Although the total flux of OM arriving at the seafloor sets the energy input to the system, the chemical nature of OM is also of significance. However, a quantitative framework linking ecological flux vectors to OM composition is currently lacking. In the present study we report the lipid composition of export fluxes collected by five-moored sediment traps deployed in contrasting productivity regimes of Southern Ocean island systems (Kerguelen, Crozet and South Georgia) and compile them with quantitative data on diatom and fecal pellet fluxes. At the three naturally iron fertilized sites, the relative contribution of labile lipids (mono- and polyunsaturated fatty acids, unsaturated fatty alcohols) is 2–4 times higher than at low productivity sites. There is a strong attenuation of labile components as a function of depth, irrespective of productivity. The three island systems also display regional characteristics in lipid export. The diversity of sterols is greater in the relatively warm waters of the Polar Frontal Zone when compared to the Antarctic zone, reflecting the transition from mixed phytoplankton communities to principally diatom-derived OM. An enrichment of zooplankton dietary sterols, such as C27Δ5, at South Georgia is consistent with high zooplankton and krill biomass in the region and the importance of fecal pellets to POC flux. There is a strong association of diatom resting spore fluxes that dominate productive flux regimes with energy rich unsaturated fatty acids. At the Kerguelen Plateau we provide a statistical framework to link seasonal variation in ecological flux vectors and lipid composition over a complete annual cycle. Our analyses demonstrate that ecological processes in the upper ocean, e.g. resting spore formation and grazing, not only impact the magnitude and stoichiometry of the Southern Ocean biological pump, but also regulate the composition of exported OM and the nature of pelagic-benthic coupling. </jats:p>
format Article in Journal/Newspaper
author Rembauville, Mathieu
Blain, Stéphane
Manno, Clara
Tarling, Geraint
Thompson, Anu
Wolff, George
Salter, Ian
spellingShingle Rembauville, Mathieu
Blain, Stéphane
Manno, Clara
Tarling, Geraint
Thompson, Anu
Wolff, George
Salter, Ian
The role of diatom resting spores for pelagic-benthic coupling in the Southern Ocean
author_facet Rembauville, Mathieu
Blain, Stéphane
Manno, Clara
Tarling, Geraint
Thompson, Anu
Wolff, George
Salter, Ian
author_sort Rembauville, Mathieu
title The role of diatom resting spores for pelagic-benthic coupling in the Southern Ocean
title_short The role of diatom resting spores for pelagic-benthic coupling in the Southern Ocean
title_full The role of diatom resting spores for pelagic-benthic coupling in the Southern Ocean
title_fullStr The role of diatom resting spores for pelagic-benthic coupling in the Southern Ocean
title_full_unstemmed The role of diatom resting spores for pelagic-benthic coupling in the Southern Ocean
title_sort role of diatom resting spores for pelagic-benthic coupling in the southern ocean
publisher Copernicus GmbH
publishDate 2018
url http://livrepository.liverpool.ac.uk/3020642/
http://livrepository.liverpool.ac.uk/3020642/1/bg-2017-414_Final_Submission.pdf
geographic Antarctic
Kerguelen
Southern Ocean
The Antarctic
geographic_facet Antarctic
Kerguelen
Southern Ocean
The Antarctic
genre Antarc*
Antarctic
Southern Ocean
Ocean Island
genre_facet Antarc*
Antarctic
Southern Ocean
Ocean Island
op_relation http://livrepository.liverpool.ac.uk/3020642/1/bg-2017-414_Final_Submission.pdf
Rembauville, Mathieu, Blain, Stéphane, Manno, Clara, Tarling, Geraint, Thompson, Anu, Wolff, George and Salter, Ian (2018) The role of diatom resting spores for pelagic-benthic coupling in the Southern Ocean.
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