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  • PANGAEA  (8)
  • Copernicus  (4)
  • American Geophysical Union  (2)
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  • 1
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    PANGAEA
    In:  Supplement to: Roca-Martí, Montserrat; Puigcorbé, Viena; Rutgers van der Loeff, Michiel M; Katlein, Christian; Fernández-Méndez, Mar; Peeken, Ilka; Masqué, Pere (2016): Carbon export fluxes and export efficiency in the central Arctic during the record sea-ice minimum in 2012: A joint 234Th/238U and 210Po/210Pb study. Journal of Geophysical Research: Oceans, 121(7), 5030-5049, https://doi.org/10.1002/2016JC011816
    Publication Date: 2023-01-13
    Description: The Arctic sea-ice extent reached a record minimum in September 2012. Sea-ice decline increases the absorption of solar energy in the Arctic Ocean, affecting primary production and the plankton community. How this will modulate the sinking of particulate organic carbon (POC) from the ocean surface remains a key question. We use the 234Th/238U and 210Po/210Pb radionuclide pairs to estimate the magnitude of the POC export fluxes in the upper ocean of the central Arctic in summer 2012, covering time scales from weeks to months. The 234Th/238U proxy reveals that POC fluxes at the base of the euphotic zone were very low (2 ± 2 mmol C/m**2/d) in late summer. Relationships obtained between the 234Th export fluxes and the phytoplankton community suggest that prasinophytes contributed significantly to the downward fluxes, likely via incorporation into sea-ice algal aggregates and zooplankton-derived material. The magnitude of the depletion of 210Po in the upper water column over the entire study area indicates that particle export fluxes were higher before July/August than later in the season. 210Po fluxes and 210Po-derived POC fluxes correlated positively with sea-ice concentration, showing that particle sinking was greater under heavy sea-ice conditions than under partially ice-covered regions. Although the POC fluxes were low, a large fraction of primary production (〉30%) was exported at the base of the euphotic zone in most of the study area during summer 2012, indicating a high export efficiency of the biological pump in the central Arctic. This article is protected by copyright. All rights reserved.
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 2
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    PANGAEA
    In:  Supplement to: Roca-Martí, Montserrat; Puigcorbé, Viena; Iversen, Morten Hvitfeldt; Rutgers van der Loeff, Michiel M; Klaas, Christine; Cheah, Wee; Bracher, Astrid; Masqué, Pere (2015): High particulate organic carbon export during the decline of a vast diatom bloom in the Atlantic sector of the Southern Ocean. Deep Sea Research Part II: Topical Studies in Oceanography, https://doi.org/10.1016/j.dsr2.2015.12.007
    Publication Date: 2023-08-01
    Description: Carbon fixation by phytoplankton plays a key role in the uptake of atmospheric CO2 in the Southern Ocean. Yet, it still remains unclear how efficiently the particulate organic carbon (POC) is exported and transferred from ocean surface waters to depth during phytoplankton blooms. In addition, little is known about the processes that control the flux attenuation within the upper twilight zone. Here, we present results of downward POC and particulate organic nitrogen fluxes during the decline of a vast diatom bloom in the Atlantic sector of the Southern Ocean in summer 2012. We used thorium-234 (234Th) as a particle tracer in combination with drifting sediment traps (ST). Their simultaneous use evidenced a sustained high export rate of 234Th at 100 m depth in the weeks prior to and during the sampling period. The entire study area, of approximately 8000 km**2, showed similar vertical export fluxes in spite of the heterogeneity in phytoplankton standing stocks and productivity, indicating a decoupling between production and export. The POC fluxes at 100 m were high, averaging 26 ± 15 mmol C/m**2/d, although the strength of the biological pump was generally low. Only 〈20% of the daily primary production reached 100 m, presumably due to an active recycling of carbon and nutrients. Pigment analyses indicated that direct sinking of diatoms likely caused the high POC transfer efficiencies (~60%) observed between 100 and 300 m, although faecal pellets and transport of POC linked to zooplankton vertical migration might have also contributed to downward fluxes.
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 3
    Publication Date: 2024-06-26
    Keywords: ANT-XXVIII/3; AWI_MarGeoChem; Carbon, organic, particulate, flux; Carbon, organic, particulate/Thorium-234 ratio; Carbon, organic, particulate/Thorium-234 ratio, standard deviation; Date/Time of event; DEPTH, water; Duration; Elevation of event; Event label; Latitude of event; Longitude of event; Marine Geochemistry @ AWI; Nitrogen, organic, particulate, flux; Nitrogen, organic, particulate/Thorium-234 ratio; Nitrogen, organic, particulate/Thorium-234 ratio, standard deviation; Polarstern; PS79; PS79/086-4; PS79/087-1; PS79/091-3; PS79/098-1; PS79/100-1; PS79/114-1; PS79/128-12; PS79/136-11; PS79/137-1; PS79/139-1; PS79/140-1; South Atlantic Ocean; Trap, sediment; TRAPS
    Type: Dataset
    Format: text/tab-separated-values, 139 data points
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  • 4
    Publication Date: 2024-06-26
    Keywords: ANT-XXVIII/3; AWI_MarGeoChem; Bottle number; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; Marine Geochemistry @ AWI; Polarstern; PS79; PS79/057-4; PS79/063-2; PS79/069-5; PS79/075-9; PS79/081-5; PS79/084-12; PS79/085-3; PS79/086-2; PS79/087-2; PS79/091-1; PS79/091-5; PS79/093-4; PS79/095-1; PS79/095-3; PS79/102-1; PS79/102-3; PS79/106-1; PS79/106-4; PS79/115-1; PS79/115-4; PS79/119-1; PS79/119-3; PS79/128-14; PS79/129-1; PS79/137-7; PS79/139-3; PS79/139-6; PS79/140-12; PS79/147-1; PS79/152-1; PS79/166-1; PS79/170-1; PS79/173-1; PS79/174-20; South Atlantic Ocean; Thorium-234, total; Thorium-234, total, standard deviation; Thorium-234/Uranium-238 activity ratio; Thorium-234/Uranium-238 activity ratio, standard deviation; Uranium-238; Uranium-238, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 2261 data points
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  • 5
    Publication Date: 2024-06-26
    Keywords: ANT-XXVIII/3; AWI_MarGeoChem; Carbon, organic, particulate; Carbon, organic, particulate/Thorium-234 ratio; Carbon, organic, particulate/Thorium-234 ratio, standard deviation; Date/Time of event; DEPTH, water; Elevation of event; Event label; In situ pump; ISP; Latitude of event; Longitude of event; Marine Geochemistry @ AWI; Nitrogen, organic, particulate; Nitrogen, organic, particulate/Thorium-234 ratio; Nitrogen, organic, particulate/Thorium-234 ratio, standard deviation; Polarstern; PS79; PS79/057-5; PS79/069-4; PS79/081-3; PS79/084-11; PS79/091-10; PS79/139-13; PS79/174-17; South Atlantic Ocean; Thorium-234, particulate; Thorium-234, particulate, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 154 data points
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  • 6
    Publication Date: 2024-07-01
    Keywords: Arctic Ocean; ARK-XXVII/3; Bottle number; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; Polarstern; PS80/231-2; PS80/246-1; PS80/265-1; PS80/281-1; PS80/324-1; PS80/343-1; PS80/353-1; PS80/365-1; PS80/390-1; PS80 IceArc; Station label; Thorium-234, total; Thorium-234, total, standard deviation; Thorium-234/Uranium-238 activity ratio; Thorium-234/Uranium-238 activity ratio, standard deviation; Uranium-238; Uranium-238, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 856 data points
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  • 7
    Publication Date: 2024-07-01
    Keywords: Arctic Ocean; ARK-XXVII/3; Bottle number; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; Latitude of event; Lead-210; Lead-210, standard deviation; Longitude of event; Polarstern; Polonium-210; Polonium-210, standard deviation; Polonium-210/Lead-210, standard deviation; Polonium-210/Lead-210 activity ratio; PS80/231-1; PS80/245-1; PS80/264-1; PS80/280-1; PS80/342-1; PS80/353-1; PS80/365-1; PS80 IceArc; Station label
    Type: Dataset
    Format: text/tab-separated-values, 656 data points
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  • 8
    Publication Date: 2024-07-01
    Keywords: Arctic Ocean; ARK-XXVII/3; Carbon, organic, particulate; Carbon, organic, particulate/Polonium-210 ratio; Carbon, organic, particulate/Polonium-210 ratio, standard deviation; Carbon, organic, particulate/Thorium-234 ratio; Carbon, organic, particulate/Thorium-234 ratio, standard deviation; Date/Time of event; DEPTH, water; Elevation of event; Event label; In situ pump; ISP; Latitude of event; Lead-210, particulate; Lead-210, particulate, standard deviation; Longitude of event; Nitrogen, organic, particulate; Polarstern; Polonium-210, particulate; Polonium-210, particulate, standard deviation; PS80/232-1; PS80/247-1; PS80/266-1; PS80/283-1; PS80/325-1; PS80/344-1; PS80/352-1; PS80/366-1; PS80/391-1; PS80 IceArc; Station label; Thorium-234, particulate; Thorium-234, particulate, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 371 data points
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  • 9
    Publication Date: 2022-10-26
    Description: Author Posting. © American Geophysical Union, 2019. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research-Oceans 124(5), (2019): 2943-2968, doi:10.1029/2019JC015071.
    Description: In the Southern Ocean, polynyas exhibit enhanced rates of primary productivity and represent large seasonal sinks for atmospheric CO2. Three contrasting east Antarctic polynyas were visited in late December to early January 2017: the Dalton, Mertz, and Ninnis polynyas. In the Mertz and Ninnis polynyas, phytoplankton biomass (average of 322 and 354 mg chlorophyll a (Chl a)/m2, respectively) and net community production (5.3 and 4.6 mol C/m2, respectively) were approximately 3 times those measured in the Dalton polynya (average of 122 mg Chl a/m2 and 1.8 mol C/m2). Phytoplankton communities also differed between the polynyas. Diatoms were thriving in the Mertz and Ninnis polynyas but not in the Dalton polynya, where Phaeocystis antarctica dominated. These strong regional differences were explored using physiological, biological, and physical parameters. The most likely drivers of the observed higher productivity in the Mertz and Ninnis were the relatively shallow inflow of iron‐rich modified Circumpolar Deep Water onto the shelf as well as a very large sea ice meltwater contribution. The productivity contrast between the three polynyas could not be explained by (1) the input of glacial meltwater, (2) the presence of Ice Shelf Water, or (3) stratification of the mixed layer. Our results show that physical drivers regulate the productivity of polynyas, suggesting that the response of biological productivity and carbon export to future change will vary among polynyas.
    Description: This work was cofunded by the Australian Antarctic Division research projects AAS 4131 and 4291. This project was also supported by the Australian Government Cooperative Research Centres Programme through the Antarctic Climate & Ecosystems (ACE CRC). 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 and M. Roca‐Martí are grateful for the support from Pere Masque and Edith Cowan University. M.C. Arroyo was supported by the Dickhut Fellowship, administered by the Virginia Institute of Marine Science. The authors would like to thank the officers and crew of the R/V Aurora Australis for their logistic support, the CSIRO hydrochemists for their analyses of nutrient concentrations, and E. J. Yang for her microscope analysis of phytoplankton species. We also want to thank two anonymous reviewers for their very good comments on this study. The data presented in this paper are available on the Australian Antarctic Division (AAD) Data Centre at https://data.aad.gov.au/aadc/metadata/metadata_by_parameter.cfm.
    Description: 2019-09-28
    Keywords: Polynyas ; Primary productivity ; Phytoplankton biomass ; Ice shelves ; Sea ice ; Iron
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 10
    Publication Date: 2018-09-14
    Description: Vertical distributions of total and particulate polonium-210 (210Po) and lead-210 (210Pb) activities in the water column were measured at 11 stations in the North Atlantic during the GEOTRACES GA01 transect: GEOVIDE cruise in May–June 2014. Total 210Po activity was on average 24 % lower than 210Pb activity in the upper 100 m, and it was closer to unity in the mesopelagic (100–1000 m). The partitioning coefficients (Kd) along the transect suggest the preferential association of 210Po relative to 210Pb onto particles. The prominent role of small particles in sorption was confirmed by the observation that over 80 % of the particulate radionuclide activity was on small particles. To account for the observed surface water 210Po ∕ 210Pb disequilibria, particulate radionuclide activities and export of both small (1–53 µm) and large (〉53 µm) particles must be considered. A comparison between the GEOVIDE total particulate 210Po ∕ 210Pb activity ratios (ARs) and the ratios in previous studies revealed a distinct geographic distribution, with lower particulate ARs in the high-latitude North Atlantic (including this study) and Arctic in relation to all other samples. For the samples where apparent oxygen utilization (AOU) was calculated at the same depth and time as the 210Po ∕ 210Pb AR (40 stations including this study), there was a two-phase correlation between the total particulate AR and AOU, likely reflecting the nature of the particles and demonstrating the forces of remineralization and radionuclide decay from particles as they age.
    Print ISSN: 1726-4170
    Electronic ISSN: 1726-4189
    Topics: Biology , Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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