Data Description

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Cai, P et al. (2010): Radionuclides measured on 37 water bottle profiles during POLARSTERN cruise ARK-XXII/2. doi:10.1594/PANGAEA.708354,
Supplement to: Cai, Pinghe; Rutgers van der Loeff, Michiel M; Stimac, Ingrid; Nöthig, Eva-Maria; Lepore, Kate; Moran, S Bradley (2010): Low export flux of particulate organic carbon in the central Arctic Ocean as revealed by 234Th:238U disequilibrium. Journal of Geophysical Research-Oceans, 115, C10037, doi:10.1029/2009JC005595
The loss of Arctic sea ice has accelerated in recent years. With the decline in sea ice cover, the Arctic Ocean biogeochemistry is undergoing unprecedented change. A key question about the changing Arctic Ocean biogeochemistry is concerning the impact of the shrinking sea ice cover on the particulate organic carbon (POC) export from the upper Arctic Ocean. Thus far, there are still very few direct measurements of POC export in the permanently ice-covered central Arctic Ocean. A further issue is that the magnitude of the POC export so far documented in this region remains controversial. During the ARK-XXII/2 expedition to the Arctic Ocean from 28 July to 7 October in 2007, we conducted a high-resolution study of POC export using 234Th/238U disequilibrium. Depth profiles of total 234Th in the upper 200 m were collected at 36 stations in the central Arctic Ocean and its adjacent seas, i.e., the Barents Sea, the Kara Sea and the Laptev Sea. Samples were processed using a small-volume MnO2 coprecipitation method with addition of a yield tracer, which resulted in one of the most precise 234Th data sets ever collected. Thorium-234 deficit with respect to 238U was found to be evident throughout the upper 100 m over the Arctic shelves. In comparison, 234Th deficit was confined to the upper 25 m in the central Arctic Ocean. Below 25 m, secular equilibrium was approached between 234Th and 238U. The observed 234Th deficit was generally associated with enhanced total chlorophyll concentrations, indicating that in situ production and export of biogenic particles are the main mechanism for 234Th removal in the Arctic Ocean. Thorium-234-derived POC fluxes were determined with a steady state model and pump-normalized POC/234Th ratios on total suspended particles collected at 100 m. Results showed enhanced POC export over the Arctic shelves. On average, POC export fluxes over the various Arctic shelves were 2.7 ± 1.7 mmol m**-2 d**-1 (the Barents Sea), 0.5 ± 0.8 mmol m**-2 d**-1 (the Kara Sea), and 2.9 ± 1.8 mmol m**-2 d**-1 (the Laptev Sea) respectively. In comparison, the central Arctic Ocean was characterized by the lowest POC export flux ever reported, 0.2 ± 1.0 mmol m**-2 d**-1 (1 standard deviation, n = 26). This value is very low compared to prior estimates and is also much lower than the POC export fluxes reported in other oligotrophic oceans. A ThE ratio (234Th-derived POC export/primary production) of <6% in the central Arctic Ocean was estimated using the historical measurements of primary production. The low ThE ratio indicates that like other oligotrophic regimes, the central Arctic Ocean is characterized by low POC export relative to primary production, i.e., a tightly coupled food web. Our study strongly suggests that the current role of the central Arctic Ocean in C sequestration is still very limited. Meanwhile, this role might be altered because of global warming and future decline in sea ice cover.
Related to:
Nöthig, Eva-Maria; Kuckero, Lilith; Lorenzen, Christiane (2015): Chlorophyll a measured on water bottle samples during POLARSTERN cruise ARK-XXII/2. doi:10.1594/PANGAEA.846873
Further details:
Cai, Pinghe; Rutgers van der Loeff, Michiel M: Analytical Procedure for 234Th/238U in 4-L of seawater. Xiamen University and Alfred Wegener Institute, hdl:10013/epic.31584.d001 *
Median Latitude: 82.551938 * Median Longitude: 99.948759 * South-bound Latitude: 75.000500 * West-bound Longitude: 33.907000 * North-bound Latitude: 88.179200 * East-bound Longitude: -135.034800
Date/Time Start: 2007-07-30T10:14:00 * Date/Time End: 2007-09-23T23:11:00
Minimum DEPTH, water: 10.0 m * Maximum DEPTH, water: 200.0 m
PS70/228-1 * * Latitude: 75.000500 * Longitude: 34.000000 * Date/Time: 2007-07-30T10:14:00 * Elevation: -178.0 m * Location: Arctic Ocean * * Campaign: ARK-XXII/2 (PS70 SPACE DAMOCLES) * * Basis: Polarstern * * Device: CTD/Rosette, ultra clean (CTD-UC) *
PS70/236-5 * * Latitude: 77.508600 * Longitude: 33.991600 * Date/Time: 2007-07-31T10:11:00 * Elevation: -197.0 m * Location: Barents Sea * * Campaign: ARK-XXII/2 (PS70 SPACE DAMOCLES) * * Basis: Polarstern * * Device: CTD/Rosette (CTD-RO) * * Comment: INST.:AWI; CTD-SN:T2423-C2078
PS70/237-3 * * Latitude: 78.999100 * Longitude: 33.941700 * Date/Time: 2007-07-31T20:19:00 * Elevation: -271.0 m * Location: Barents Sea * * Campaign: ARK-XXII/2 (PS70 SPACE DAMOCLES) * * Basis: Polarstern * * Device: CTD/Rosette (CTD-RO) * * Comment: INST.:AWI; CTD-SN:T2423-C2078
Volume sampled: 4 L of seawater
#NameShort NameUnitPrincipal InvestigatorMethodComment
1Event label *Event
2Date/Time of event *Date/Time
3Latitude of event *Latitude
4Longitude of event *Longitude
5Elevation of event *Elevationm
6DEPTH, water *Depth waterm
7Salinity *SalCai, Pinghe *CTD *
8Uranium 238 *238Udpm/lCai, Pinghe *see Further details *
9Uranium 238, standard deviation *238U std dev±Cai, Pinghe *see Further details *
10Thorium 234, total *234Th totdpm/lCai, Pinghe *see Further details *
11Thorium 234, total, standard deviation *234Th std dev±Cai, Pinghe *see Further details *
12Thorium 234/Uranium 238 activity ratio *(234Th/238U)Cai, Pinghe *see Further details *
13Thorium 234/Uranium 238 activity ratio, standard deviation *(234Th/238U) std dev±Cai, Pinghe *see Further details *
1673 data points

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