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  • 1
    Publication Date: 2023-11-15
    Keywords: AWI_BioOce; Biological Oceanography @ AWI; DATE/TIME; DEPTH, water; Depth comment; Event label; IN2016-V03; IN2016-V03_118; IN2016-V03_12; IN2016-V03_121; IN2016-V03_124; IN2016-V03_128; IN2016-V03_13; IN2016-V03_131; IN2016-V03_136; IN2016-V03_139; IN2016-V03_140; IN2016-V03_17; IN2016-V03_20; IN2016-V03_21; IN2016-V03_23; IN2016-V03_24; IN2016-V03_26; IN2016-V03_27; IN2016-V03_3; IN2016-V03_30; IN2016-V03_31; IN2016-V03_33; IN2016-V03_34; IN2016-V03_36; IN2016-V03_37; IN2016-V03_38; IN2016-V03_39; IN2016-V03_40; IN2016-V03_43; IN2016-V03_44; IN2016-V03_47; IN2016-V03_50; IN2016-V03_52; IN2016-V03_53; IN2016-V03_56; IN2016-V03_6; IN2016-V03_77; IN2016-V03_8; IN2016-V03_9; Investigator (2014); LATITUDE; LONGITUDE; Nitrate; Nitrification rate; Nitrogen-15, atmospheric, in nitrate; South Pacific Ocean; Water sample; WS; δ15N, nitrate; δ18O, nitrate
    Type: Dataset
    Format: text/tab-separated-values, 612 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-11-15
    Keywords: Ammonium uptake rate; AWI_BioOce; Biological Oceanography @ AWI; DATE/TIME; DEPTH, water; Event label; IN2016-V03; IN2016-V03_102; IN2016-V03_103; IN2016-V03_105; IN2016-V03_106; IN2016-V03_107; IN2016-V03_109; IN2016-V03_110; IN2016-V03_114; IN2016-V03_115; IN2016-V03_118; IN2016-V03_119; IN2016-V03_12; IN2016-V03_121; IN2016-V03_122; IN2016-V03_124; IN2016-V03_125; IN2016-V03_126; IN2016-V03_128; IN2016-V03_129; IN2016-V03_13; IN2016-V03_131; IN2016-V03_132; IN2016-V03_134; IN2016-V03_136; IN2016-V03_139; IN2016-V03_140; IN2016-V03_15; IN2016-V03_17; IN2016-V03_19; IN2016-V03_2; IN2016-V03_20; IN2016-V03_21; IN2016-V03_23; IN2016-V03_24; IN2016-V03_26; IN2016-V03_27; IN2016-V03_29; IN2016-V03_3; IN2016-V03_30; IN2016-V03_31; IN2016-V03_33; IN2016-V03_34; IN2016-V03_36; IN2016-V03_37; IN2016-V03_38; IN2016-V03_39; IN2016-V03_40; IN2016-V03_41; IN2016-V03_43; IN2016-V03_44; IN2016-V03_47; IN2016-V03_49; IN2016-V03_5; IN2016-V03_50; IN2016-V03_52; IN2016-V03_53; IN2016-V03_54; IN2016-V03_56; IN2016-V03_57; IN2016-V03_59; IN2016-V03_6; IN2016-V03_60; IN2016-V03_62; IN2016-V03_64; IN2016-V03_65; IN2016-V03_66; IN2016-V03_67; IN2016-V03_69; IN2016-V03_70; IN2016-V03_71; IN2016-V03_73; IN2016-V03_74; IN2016-V03_76; IN2016-V03_77; IN2016-V03_78; IN2016-V03_8; IN2016-V03_80; IN2016-V03_81; IN2016-V03_84; IN2016-V03_86; IN2016-V03_88; IN2016-V03_89; IN2016-V03_9; IN2016-V03_90; IN2016-V03_92; IN2016-V03_93; IN2016-V03_94; IN2016-V03_95; IN2016-V03_96; IN2016-V03_98; IN2016-V03_99; Investigator (2014); LATITUDE; LONGITUDE; Mixed layer depth; Nitrate uptake rate; South Pacific Ocean; Water sample; WS
    Type: Dataset
    Format: text/tab-separated-values, 270 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2023-11-15
    Description: The distribution of diazotrophs and the magnitude of N2 fixation along with the input of new N through this process remains poorly constrained globally, but particularly in the Southern Pacific Ocean. Here we present a high-resolution dataset (every 0.5° latitude) describing the different N-cycling pathways which control the fixation and sequestration of carbon in the surface waters along a 7000 km transect in the South Pacific Ocean. Key oceanographic features along the P15S GO-SHIP transect from the Antarctic ice edge to the equator, included crossing of the subtropical front (STF), from the sub-Antarctic waters towards the oligotrophic tropics, and the equatorial upwelling region. We show how the natural isotopic abundance of particulate organic matter relate to different biogeochemical transformations in the N-cycle across four oceanic provinces. At all stations we measured N2 fixation rates. In the cold and nutrient rich waters of the Southern Ocean we found measurable N2 fixation rates (〉0.2 nmol L-1.d-1), which increased after the subtropical front, and remained at about 15 nmol L-1.d-1 until the equator. In the subtropical and tropical waters, the input of new nitrogen through N2 fixation could fuel on average 13±19% of the net primary productivity. Our data analysis showed that nitrifying organisms, from bacterial and archaeal genera such as Nitrospina, Nitrospinaceae, Nitrosopumilus, Nitrosopelagicus and Nitrosoarchaeum, prevailed in the Southern Ocean and within the STF. Nitrification rates ranged up to 60 nmol L-1.d-1 within the mixed layer depth in the Southern Ocean. Our results suggest that nitrification above the pycnoclines is an important component of the N cycle in the Southern Ocean. Our data has given us a better understanding of how the different N-cycling pathways relate to primary productivity in the South Pacific Ocean, as well as insights into the potential geographical N pathway shifts in light of the rapidly changing climate.
    Keywords: AWI_BioOce; Biological Oceanography @ AWI
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2024-02-16
    Description: Nitrogen fixation rates (nmol/l/day) were calculated using the 15N-15N enrichments of 6.6, 3.9 and 10.1.% (Klawonn et al 2015)
    Keywords: AWI_BioOce; Biological Oceanography @ AWI; DATE/TIME; DEPTH, water; Event label; IN2016-V03; IN2016-V03_102; IN2016-V03_103; IN2016-V03_105; IN2016-V03_106; IN2016-V03_107; IN2016-V03_109; IN2016-V03_110; IN2016-V03_114; IN2016-V03_115; IN2016-V03_118; IN2016-V03_119; IN2016-V03_12; IN2016-V03_121; IN2016-V03_122; IN2016-V03_124; IN2016-V03_125; IN2016-V03_126; IN2016-V03_128; IN2016-V03_129; IN2016-V03_13; IN2016-V03_131; IN2016-V03_132; IN2016-V03_134; IN2016-V03_136; IN2016-V03_139; IN2016-V03_140; IN2016-V03_15; IN2016-V03_17; IN2016-V03_19; IN2016-V03_2; IN2016-V03_20; IN2016-V03_21; IN2016-V03_23; IN2016-V03_24; IN2016-V03_26; IN2016-V03_27; IN2016-V03_29; IN2016-V03_3; IN2016-V03_30; IN2016-V03_31; IN2016-V03_33; IN2016-V03_34; IN2016-V03_36; IN2016-V03_37; IN2016-V03_38; IN2016-V03_39; IN2016-V03_40; IN2016-V03_41; IN2016-V03_43; IN2016-V03_44; IN2016-V03_47; IN2016-V03_49; IN2016-V03_5; IN2016-V03_50; IN2016-V03_52; IN2016-V03_53; IN2016-V03_54; IN2016-V03_56; IN2016-V03_57; IN2016-V03_6; IN2016-V03_60; IN2016-V03_62; IN2016-V03_64; IN2016-V03_65; IN2016-V03_66; IN2016-V03_67; IN2016-V03_69; IN2016-V03_70; IN2016-V03_71; IN2016-V03_73; IN2016-V03_76; IN2016-V03_77; IN2016-V03_78; IN2016-V03_8; IN2016-V03_80; IN2016-V03_81; IN2016-V03_84; IN2016-V03_86; IN2016-V03_88; IN2016-V03_89; IN2016-V03_9; IN2016-V03_90; IN2016-V03_92; IN2016-V03_95; IN2016-V03_96; IN2016-V03_98; IN2016-V03_99; Investigator (2014); LATITUDE; LONGITUDE; Nitrogen, total; Nitrogen-15, atmospheric; Nitrogen fixation rate; South Pacific Ocean; Water sample; WS; δ15N
    Type: Dataset
    Format: text/tab-separated-values, 1265 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2024-02-16
    Description: Nitrogen fixation rates (nmol/l/day) were calculated using the 15N-15N enrichments of 3.8 % (Klawonn et al 2015)
    Keywords: AWI_BioOce; Biological Oceanography @ AWI; DATE/TIME; DEPTH, water; Event label; IN2016_03_CTD102A-N2; IN2016_03_CTD102B-N2; IN2016_03_CTD103A-N2; IN2016_03_CTD103B-N2; IN2016_03_CTD105A-N2; IN2016_03_CTD105B-N2; IN2016_03_CTD106A-N2; IN2016_03_CTD106B-N2; IN2016_03_CTD107A-N2; IN2016_03_CTD107B-N2; IN2016_03_CTD109A-N2; IN2016_03_CTD109B-N2; IN2016_03_CTD110-N2; IN2016_03_CTD114A-N2; IN2016_03_CTD114B-N2; IN2016_03_CTD114C-N2; IN2016_03_CTD115A-N2; IN2016_03_CTD115B-N2; IN2016_03_CTD118B-N2; IN2016_03_CTD118-N2; IN2016_03_CTD119A-N2; IN2016_03_CTD119B-N2; IN2016_03_CTD121A-N2; IN2016_03_CTD121B-N2; IN2016_03_CTD122-N2; IN2016_03_CTD124A-N2; IN2016_03_CTD124B-N2; IN2016_03_CTD125A-N2; IN2016_03_CTD125B-N2; IN2016_03_CTD126-N2; IN2016_03_CTD128A-N2; IN2016_03_CTD128B-N2; IN2016_03_CTD129A-N2; IN2016_03_CTD129B-N2; IN2016_03_CTD12-N2; IN2016_03_CTD131-N2; IN2016_03_CTD132A-N2; IN2016_03_CTD132B-N2; IN2016_03_CTD134A-N2; IN2016_03_CTD134B-N2; IN2016_03_CTD136-N2; IN2016_03_CTD139A-N2; IN2016_03_CTD139B-N2; IN2016_03_CTD13-N2; IN2016_03_CTD140A-N2; IN2016_03_CTD140B-N2; IN2016_03_CTD14-N2; IN2016_03_CTD17B-N2; IN2016_03_CTD17-N2; IN2016_03_CTD18-N2; IN2016_03_CTD20-N2; IN2016_03_CTD21-N2; IN2016_03_CTD23A-N2; IN2016_03_CTD23-N2; IN2016_03_CTD24-N2; IN2016_03_CTD26-N2; IN2016_03_CTD27-N2; IN2016_03_CTD29-N2; IN2016_03_CTD2-N2; IN2016_03_CTD30-N2; IN2016_03_CTD31-N2; IN2016_03_CTD33-N2; IN2016_03_CTD34-N2; IN2016_03_CTD36-N2; IN2016_03_CTD37-N2; IN2016_03_CTD38-N2; IN2016_03_CTD39-N2; IN2016_03_CTD3-N2; IN2016_03_CTD40-N2; IN2016_03_CTD41-N2; IN2016_03_CTD43-N2; IN2016_03_CTD44-N2; IN2016_03_CTD47-N2; IN2016_03_CTD48-N2; IN2016_03_CTD50-N2; IN2016_03_CTD52-N2; IN2016_03_CTD53-N2; IN2016_03_CTD56-N2; IN2016_03_CTD57-N2; IN2016_03_CTD59-N2; IN2016_03_CTD5-N2; IN2016_03_CTD60-N2; IN2016_03_CTD62-N2; IN2016_03_CTD63-N2; IN2016_03_CTD64-N2; IN2016_03_CTD66-N2; IN2016_03_CTD67-N2; IN2016_03_CTD69-N2; IN2016_03_CTD6-N2; IN2016_03_CTD70-N2; IN2016_03_CTD71-N2; IN2016_03_CTD73-N2; IN2016_03_CTD74-N2; IN2016_03_CTD76-N2; IN2016_03_CTD77-N2; IN2016_03_CTD78-N2; IN2016_03_CTD80-N2; IN2016_03_CTD81-N2; IN2016_03_CTD83-N2; IN2016_03_CTD86A-N2; IN2016_03_CTD86B-N2; IN2016_03_CTD86C-N2; IN2016_03_CTD86D-N2; IN2016_03_CTD88-N2; IN2016_03_CTD89-N2; IN2016_03_CTD8-N2; IN2016_03_CTD90A-N2; IN2016_03_CTD90B-N2; IN2016_03_CTD91B-N2; IN2016_03_CTD91-N2; IN2016_03_CTD92-N2; IN2016_03_CTD93B-N2; IN2016_03_CTD93-N2; IN2016_03_CTD95B-N2; IN2016_03_CTD95-N2; IN2016_03_CTD96A-N2; IN2016_03_CTD96B-N2; IN2016_03_CTD96C-N2; IN2016_03_CTD98-N2; IN2016_03_CTD99B-N2; IN2016_03_CTD99-N2; IN2016_03_CTD9-N2; IN2016_04_CTD54-N2; LATITUDE; LONGITUDE; Nitrogen; Nitrogen, total; Nitrogen-15, atmospheric; Nitrogen fixation rate; Sample ID; South Pacific Ocean; Water sample; WS; δ15N
    Type: Dataset
    Format: text/tab-separated-values, 1205 data points
    Location Call Number Limitation Availability
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