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  • 1
    Call number: AWI Bio-98-0164
    In: Antarctic research series
    Type of Medium: Monograph available for loan
    Pages: XI, 198 S. : graph. Darst.
    ISBN: 0875909019
    Series Statement: Antarctic research series 73
    Branch Library: AWI Library
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  • 2
    Publication Date: 2023-05-12
    Keywords: Ammonium; Amundsen Gulf, Canada; Beaufort Sea; CCGSA_4-10_CFL08; CCGS Amundsen; CFL08_1200; CFL08_1216-1; CFL08_405B-1; CFL08_421-2; CFL08_435; CFL08_6006-2; Chlorophyll a; Circumpolar Flaw Lead Leg 4-10a; Darnley_Bay08; DATE/TIME; DEPTH, water; Depth of the euphotic zone; Elevation, mean; Event label; Franklin_Bay08; International Polar Year 2007-2008; IPY-4; Latitude of event; Longitude of event; Mixed layer depth; MOOR; Mooring; MULT; Multiple investigations; Nitrate and Nitrite; Phosphate; Radiation, photosynthetically active; Salinity; Silicate; Station label; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 164 data points
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  • 3
    Publication Date: 2023-07-28
    Keywords: Amundsen Gulf, Canada; Chlorophyll a; Darnley_Bay08; DATE/TIME; DEPTH, water; Depth of the euphotic zone; Event label; Fixation of carbon in chlorophyll; International Polar Year 2007-2008; IPY-4; Light absorption by phytoplankton per chlorophyll a; Mixed layer depth; MULT; Multiple investigations; Nitrate; Photoinhibition in carbon per chlorophyll a; Photosynthetic efficiency, carbon production; Quantum yield; Radiation, photosynthetically active; Ratio; Sample comment; Sample type; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 104 data points
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  • 4
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    PANGAEA
    In:  Supplement to: Eagle, Meagan; Paytan, Adina; Arrigo, Kevin R; van Dijken, Gert L; Murray, Richard W (2003): A comparison between excess barium and barite as indicators of carbon export. Paleoceanography, 18(1), 1021, https://doi.org/10.1029/2002PA000793
    Publication Date: 2023-12-12
    Description: Since Dymond et al. (1992, doi:10.1029/92PA00181) proposed the paleoproductivity algorithm based on “Bio-Ba”, which relies on a strong correlation between Ba and organic carbon fluxes in sediment traps, this proxy has been applied in many paleoproductivity studies. Barite, the main carrier of particulate barium in the water column and the phase associated with carbon export, has also been suggested as a reliable paleoproductivity proxy in some locations. We demonstrate that Ba(excess) (total barium minus the fraction associated with terrigenous material) frequently overestimates Ba(barite) (barium associated with the mineral barite), most likely due to the inclusion of barium from phases other than barite and terrigenous silicates (e.g., carbonate, organic matter, opal, Fe-Mn oxides, and hydroxides). A comparison between overlying oceanic carbon export and carbon export derived from Ba(excess) shows that the Dymond et al. (1992) algorithm frequently underestimates carbon export but is still a useful carbon export indicator if all caveats are considered before the algorithm is applied. Ba(barite) accumulation rates from a wide range of core top sediments from different oceanic settings are highly correlated to surface ocean 14C and Chlorophyll a measurements of primary production. This relationship varies by ocean basin, but with the application of the appropriate f ratio to 14C and Chlorophyll a primary production estimates, the plot of Ba(barite) accumulation and carbon export for the equatorial Pacific, Atlantic, and Southern Ocean converges to a global relationship that can be used to reconstruct paleo carbon export.
    Keywords: 11031802 Spadecore1; 11080400 Spadecore2; 11110100 Spadecore3; 11182336 Multicorer14; 11212105 Multicorer17; 11230530 Multicorer18; 11270742 Multicorer22; 11290827 Multicorer25; 12052336 Multicorer35; Accumulation rate per year; Agulhas Ridge; Aluminium; ANT-XI/2; Barium; Barium, flux; Barium/PP (Dymond et al 1992); Barium barite/barium excess ratio; Barium excess; Barium excess, flux; Barium in barite; BC; Box corer; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Equatorial Pacific; ERDC; ERDC-088BX; ERDC-125BX; Event label; Export production; f-Ratio; GC; Gravity corer; INMD; INMD-106BX; K7905-21BC; MANOP; Melville; MUC; MultiCorer; Nathaniel B. Palmer; NBP9802; NBP9802-03; NBP9802-04; NBP9802-05; NBP9802-06; NBP9802-07; NBP9802-08; NBP9802-09; PC; Piston corer; PLDS-081BX; PLDS-107BX; PLDS-3; Pleiades; PLTO03MV; PLUTO-2-25; PLUTO-3; Polarstern; Primary production of carbon per area, yearly; PS2489-4; PS2493-3; PS2498-2; PS2499-1; PS28; PS28/256; PS28/280; PS28/304; PS28/314; RC24; RC24-8GC; Robert Conrad; Sample code/label; South Atlantic; South Pacific Ocean; Spade box corer; Thomas G. Thompson; Thomas Washington; TN057; TNO57-10; TNO57-13; TT013; TT013_104; TT013_113; TT013_143; TT013_20; TT013_35; TT013_6; TT013_69; TT013_82; TT013_88; V30; V30-41; VEGBOXC; Vema; W7706; W7706-44; Wecoma
    Type: Dataset
    Format: text/tab-separated-values, 700 data points
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  • 5
    Publication Date: 2023-12-12
    Keywords: Amundsen Sea; Area/locality; Density, sigma, in situ; Density, standard deviation; Depth, bottom/max; Depth, relative; Depth, top/min; DEPTH, water; Depth of the euphotic zone; DynaLiFe; Light attenuation coefficient; Mixed layer depth; Nathaniel B. Palmer; NBP0901; NBP0901_var; Radiation, photosynthetically active, standard deviation; Radiation, photosynthetically active per day; Salinity, standard deviation; Sample amount; Sea surface salinity, summer; Sea surface temperature, standard deviation; Sea surface temperature, summer; Standard deviation; Water sample; WS
    Type: Dataset
    Format: text/tab-separated-values, 100 data points
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  • 6
    Publication Date: 2023-12-12
    Keywords: Amundsen Sea; Area/locality; Cryptophyta; Depth, bottom/max; Depth, top/min; DEPTH, water; Diatoms; DynaLiFe; Green algae; Maximum photochemical quantum yield of photosystem II; Maximum photochemical quantum yield of photosystem II, standard deviation; Nathaniel B. Palmer; NBP0901; NBP0901_var; Phaeocystis antarctica; Phaeocystis spp.; Sample amount; Standard deviation; Water sample; WS
    Type: Dataset
    Format: text/tab-separated-values, 80 data points
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  • 7
    Publication Date: 2023-12-12
    Keywords: Amundsen Sea; Area/locality; Assimilation rate of carbon per chlorophyll a; Depth, bottom/max; Depth, top/min; DEPTH, water; DynaLiFe; Nathaniel B. Palmer; NBP0901; NBP0901_var; Quantum yield; Quantum yield, standard deviation; Sample amount; Saturation light intensity; Slope; Standard deviation; Water sample; WS
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 8
    Publication Date: 2023-12-12
    Keywords: Amundsen Sea; Area/locality; Chlorophyll a, areal concentration; Chlorophyll a, standard deviation; DynaLiFe; Nathaniel B. Palmer; NBP0901; NBP0901_var; Nitrate, integrated; Nitrate, standard deviation; Primary production of carbon, standard deviation; Primary production of carbon per area, daily; Sample amount; Water sample; WS
    Type: Dataset
    Format: text/tab-separated-values, 63 data points
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  • 9
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    PANGAEA
    In:  Supplement to: Sedwick, Peter; Marsay, Christopher M; Sohst, Bettina M; Aguilar-Islas, Ana M; Lohan, Maeve C; Long, Matthew C; Arrigo, Kevin R; Dunbar, Robert B; Saito, Mak A; Smith, Walker O Jr; DiTullio, Giacomo R (2011): Early season depletion of dissolved iron in the Ross Sea polynya: Implications for iron dynamics on the Antarctic continental shelf. Journal of Geophysical Research, 116(C12), C12019, https://doi.org/10.1029/2010JC006553
    Publication Date: 2023-12-13
    Description: The Ross Sea polynya is among the most productive regions in the Southern Ocean and may constitute a significant oceanic CO2 sink. Based on results from several field studies, this region has been considered seasonally iron limited, whereby a "winter reserve" of dissolved iron (dFe) is progressively depleted during the growing season to low concentrations (~0.1 nM) that limit phytoplankton growth in the austral summer (December-February). Here we report new iron data for the Ross Sea polynya during austral summer 2005-2006 (27 December-22 January) and the following austral spring 2006 (16 November-3 December). The summer 2005-2006 data show generally low dFe concentrations in polynya surface waters (0.10 ± 0.05 nM in upper 40 m, n = 175), consistent with previous observations. Surprisingly, our spring 2006 data reveal similar low surface dFe concentrations in the polynya (0.06 ± 0.04 nM in upper 40 m, n = 69), in association with relatively high rates of primary production (~170-260 mmol C/m**2/d). These results indicate that the winter reserve dFe may be consumed relatively early in the growing season, such that polynya surface waters can become "iron limited" as early as November; i.e., the seasonal depletion of dFe is not necessarily gradual. Satellite observations reveal significant biomass accumulation in the polynya during summer 2006-2007, implying significant sources of "new" dFe to surface waters during this period. Possible sources of this new dFe include episodic vertical exchange, lateral advection, aerosol input, and reductive dissolution of particulate iron.
    Keywords: Bottle, Niskin; CORSACS-1_NX1; CORSACS-1_NX10; CORSACS-1_NX11; CORSACS-1_NX2; CORSACS-1_NX3; CORSACS-1_NX4; CORSACS-1_NX5; CORSACS-1_NX6; CORSACS-1_NX7; CORSACS-1_NX8; CORSACS-1_NX9; CORSACS-2_NX12; CORSACS-2_NX13; CORSACS-2_NX14; CORSACS-2_NX15; CORSACS-2_NX16; CORSACS-2_NX17; CORSACS-2_NX18; CORSACS-2_NX19; CORSACS-2_NX20; CORSACS I; CORSACS II; DEPTH, water; Event label; International Polar Year (2007-2008); IPY; Iron, dissolvable; Iron, dissolved; Iron, particulate; Mixed layer depth; Nathaniel B. Palmer; NBP0601; NBP0601_NX1; NBP0601_NX10; NBP0601_NX11; NBP0601_NX2; NBP0601_NX3; NBP0601_NX4; NBP0601_NX5; NBP0601_NX6; NBP0601_NX7; NBP0601_NX8; NBP0601_NX9; NBP0608; NBP0608_NX12; NBP0608_NX13; NBP0608_NX14; NBP0608_NX15; NBP0608_NX16; NBP0608_NX17; NBP0608_NX18; NBP0608_NX19; NBP0608_NX20; NIS; Nitrate and Nitrite; Phosphorus, inorganic, dissolved; Ross Sea; Silicic acid
    Type: Dataset
    Format: text/tab-separated-values, 1365 data points
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  • 10
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    PANGAEA
    In:  Supplement to: Munro, David R; Dunbar, Robert B; Mucciarone, David A; Arrigo, Kevin R; Long, Matthew C (2010): Stable isotope composition of dissolved inorganic carbon and particulate organic carbon in sea ice from the Ross Sea, Antarctica. Journal of Geophysical Research, 115(C9), C09005, https://doi.org/10.1029/2009JC005661
    Publication Date: 2024-03-08
    Description: We examined controls on the carbon isotopic composition of sea ice brines and organic matter during cruises to the Ross Sea, Antarctica in November/December 1998 and November/December 2006. Brine samples were analyzed for salinity, nutrients, total dissolved inorganic carbon (sum CO2), and the 13C/12C ratio of Sum CO2 (d13C(sum CO2)). Particulate organic matter from sea ice cores was analyzed for percent particulate organic carbon (POC), percent total particulate nitrogen (TPN), and stable carbon isotopic composition (d13C(POC)). Sum CO2 in sea ice brines ranged from 1368 to 7149 µmol/kg, equivalent to 1483 to 2519 µmol/kg when normalized to 34.5 psu salinity (s sum CO2), the average salinity of Ross Sea surface waters. Sea ice primary producers removed up to 34% of the available sum CO2, an amount much higher than the maximum removal observed in sea ice free water. Carbonate precipitation and CO2 degassing may reduce s sum CO2 by a similar amount (e.g., 30%) in the most hypersaline sea ice environments, although brine volumes are low in very cold ice that supports these brines. Brine d13C(sum CO2) ranged from -2.6 to +8.0 per mil while d13C(POC) ranged from -30.5 to -9.2 per mil. Isotopic enrichment of the sum CO2 pool via net community production accounts for some but not all carbon isotopic enrichment of sea ice POC. Comparisons of s sum CO2, d13C(sum CO2), and d13C(POC) within sea ice suggest that epsilon p (the net photosynthetic fractionation factor) for sea ice algae is ~8 per mil smaller than the epsilon p observed for phytoplankton in open water regions of the Ross Sea. These results have implications for modeling of carbon uptake and transformation in the ice-covered ocean and for reconstruction of past sea ice extent based on stable isotopic composition of organic matter in sediment cores.
    Keywords: Ammonium; Ammonium, standard deviation; Auto-analyzer II, Technicon; Carbon, organic, particulate; Carbon, organic, particulate, integrated; Carbon, organic, particulate, standard deviation; Carbon dioxide; Carbon dioxide, standard deviation; CORSACS II; DATE/TIME; Date/time end; Event label; International Polar Year (2007-2008); IPY; Mass spectrometer Finnigan MAT 252; Nathaniel B. Palmer; NBP0608; NBP0608_all; NBP9807; NBP9807_all; NBP9807_early; NBP9807_late; Nitrate; Nitrate, standard deviation; Nitrite; Nitrite, standard deviation; Nitrogen, inorganic; Nitrogen, inorganic, standard deviation; Nitrogen, particulate; Nitrogen, particulate, standard deviation; Phosphate; Phosphate, standard deviation; ROAVERRS; Ross Sea; Salinity, brine; Salinity, standard deviation; Sample amount, subset; Sample type; Silicate; Silicate, standard deviation; SNOW; Snow/ice sample; δ13C, carbon dioxide, atmospheric; δ13C, carbon dioxide, standard deviation; δ13C, particulate organic carbon; δ13C, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 404 data points
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