TY - JOUR
T1 - Distribution and export of particulate organic carbon in East Antarctic coastal polynyas
AU - Ratnarajah, Lavenia
AU - Puigcorbé, Viena
AU - Moreau, Sébastien
AU - Roca-Martí, Montserrat
AU - Janssens, Julie
AU - Corkill, Matthew
AU - Duprat, Luis
AU - Genovese, Cristina
AU - Lieser, Jan
AU - Masqué, Pere
AU - Lannuzel, Delphine
N1 - Funding Information:
This study was supported by the Australian Government's Cooperative Research Centres through the Antarctic Climate and Ecosystem Cooperative Research Centre, the Australian Antarctic Division research projects AAS 4131 and 4291 , and the Institute for Marine and Antarctic Studies, University of Tasmania . L. Ratnarajah also received support from BYONIC (ERC award number 724289 ). D. Lannuzel was supported by an Australian Research Council Future Fellowship (Project ID L0026677 ). S. Moreau and C. Genovese were supported by the Australian Research Council's Special Research Initiative for Antarctic Gateway Partnership (Project ID SR140300001 ). V. Puigcorbé was supported by Edith Cowan University through an Early Career Researcher Grant ( G1003456 ) and an ECU-Collaboration Enhancement Scheme grant ( G1003362 ). V. Puigcorbé received the support of a fellowship from “la Caixa” Foundation (ID 100010434 ) and from the European Union’s Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie grant agreement No 847648 (fellowship code 105183). M. Roca-Martí was supported by funding from the Woods Hole Oceanographic Institution's Ocean Twilight Zone study and the Ocean Frontier Institute . Thanks to Thomas Rodemann at the Central Science Laboratory, University of Tasmania, Australia for the POC analyses, to Stephen Tibben and the Marine National Facility, CSIRO, Australia for ammonium analyses, to Walter Geibert, Alfred Wegener Institute (Germany), for thorium recovery analyses, and to Tom Trull for providing critical comments on the development of this manuscript. We acknowledge the use of imagery from the NASA Worldview application ( https://worldview.earthdata.nasa.gov ), part of the NASA Earth Observing System Data and Information System (EOSDIS). The IAEA is grateful for the support provided to its Environment Laboratories by the Government of the Principality of Monaco. This work acknowledges the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S). Lastly, the authors would like to thank the officers and crew of the RSV Aurora Australis for their logistical support.
Funding Information:
This study was supported by the Australian Government's Cooperative Research Centres through the Antarctic Climate and Ecosystem Cooperative Research Centre, the Australian Antarctic Division research projects AAS 4131 and 4291, and the Institute for Marine and Antarctic Studies, University of Tasmania. L. Ratnarajah also received support from BYONIC (ERC award number 724289). D. Lannuzel was supported by an Australian Research Council Future Fellowship (Project ID L0026677). S. Moreau and C. Genovese were supported by the Australian Research Council's Special Research Initiative for Antarctic Gateway Partnership (Project ID SR140300001). V. Puigcorbé was supported by Edith Cowan University through an Early Career Researcher Grant (G1003456) and an ECU-Collaboration Enhancement Scheme grant (G1003362). V. Puigcorbé received the support of a fellowship from “la Caixa” Foundation (ID 100010434) and from the European Union's Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie grant agreement No 847648 (fellowship code 105183). M. Roca-Martí was supported by funding from the Woods Hole Oceanographic Institution's Ocean Twilight Zone study and the Ocean Frontier Institute. Thanks to Thomas Rodemann at the Central Science Laboratory, University of Tasmania, Australia for the POC analyses, to Stephen Tibben and the Marine National Facility, CSIRO, Australia for ammonium analyses, to Walter Geibert, Alfred Wegener Institute (Germany), for thorium recovery analyses, and to Tom Trull for providing critical comments on the development of this manuscript. We acknowledge the use of imagery from the NASA Worldview application (https://worldview.earthdata.nasa.gov), part of the NASA Earth Observing System Data and Information System (EOSDIS). The IAEA is grateful for the support provided to its Environment Laboratories by the Government of the Principality of Monaco. This work acknowledges the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S). Lastly, the authors would like to thank the officers and crew of the RSV Aurora Australis for their logistical support.
Publisher Copyright:
© 2022
PY - 2022/12
Y1 - 2022/12
N2 - Polynyas represent regions of enhanced primary production because of the low, or absent, sea-ice cover coupled with the proximity of nutrient sources. However, studies throughout the Southern Ocean suggest elevated primary production does not necessarily result in increased carbon export. Three coastal polynyas in East Antarctica and an off-shelf region were visited during the austral summer from December 2016 to January 2017 to examine the vertical distribution and concentration of particulate organic carbon (POC). Carbon export was also examined using thorium-234 (234Th) as a proxy at two of the polynyas. Our results show that concentrations and integrated POC stocks were higher within the polynyas compared to the off-shelf sites. Within the polynyas, vertical POC concentrations were higher in the Mertz and Ninnis polynyas compared to the Dalton polynya. Similarly, higher carbon export was measured in the diatom-dominated Mertz polynya, where large particles (>53 μm) represented a significant fraction of the particulate 234Th and POC (average 50% and 39%, respectively), compared to the small flagellate-dominated Dalton polynya, where almost all the particulate 234Th and POC were found in the smaller size fraction (1–53 μm). The POC to Chlorophyll-a ratios suggest that organic matter below the mixed layer in the polynyas consisted largely of fresh phytoplankton at this time of the year. In combination with a parallel study on phytoplankton production at these sites, we find that increased primary production at these polynyas does lead to greater concentrations and export of POC and a higher POC export efficiency.
AB - Polynyas represent regions of enhanced primary production because of the low, or absent, sea-ice cover coupled with the proximity of nutrient sources. However, studies throughout the Southern Ocean suggest elevated primary production does not necessarily result in increased carbon export. Three coastal polynyas in East Antarctica and an off-shelf region were visited during the austral summer from December 2016 to January 2017 to examine the vertical distribution and concentration of particulate organic carbon (POC). Carbon export was also examined using thorium-234 (234Th) as a proxy at two of the polynyas. Our results show that concentrations and integrated POC stocks were higher within the polynyas compared to the off-shelf sites. Within the polynyas, vertical POC concentrations were higher in the Mertz and Ninnis polynyas compared to the Dalton polynya. Similarly, higher carbon export was measured in the diatom-dominated Mertz polynya, where large particles (>53 μm) represented a significant fraction of the particulate 234Th and POC (average 50% and 39%, respectively), compared to the small flagellate-dominated Dalton polynya, where almost all the particulate 234Th and POC were found in the smaller size fraction (1–53 μm). The POC to Chlorophyll-a ratios suggest that organic matter below the mixed layer in the polynyas consisted largely of fresh phytoplankton at this time of the year. In combination with a parallel study on phytoplankton production at these sites, we find that increased primary production at these polynyas does lead to greater concentrations and export of POC and a higher POC export efficiency.
KW - Th
KW - East Antarctica
KW - Particulate organic carbon
KW - POC export
KW - Polynya
KW - Southern ocean
UR - http://www.scopus.com/inward/record.url?scp=85141256747&partnerID=8YFLogxK
U2 - 10.1016/j.dsr.2022.103899
DO - 10.1016/j.dsr.2022.103899
M3 - Article
AN - SCOPUS:85141256747
SN - 0967-0637
VL - 190
JO - Deep-Sea Research Part I: Oceanographic Research Papers
JF - Deep-Sea Research Part I: Oceanographic Research Papers
M1 - 103899
ER -