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  • 1
    Publication Date: 2024-05-14
    Description: This paper represents a continuation of taxonomic publications on the benthic fauna of polymetallic nodule fields in the eastern Clarion-Clipperton Zone (CCZ) using material collected during baseline environmental survey work targeting two exploration contract areas (“UK-1” and “OMS”) and one Area of Particular Environmental Interest, “APEI-6.” Families Poecilochaetidae Hannerz, 1956 and Spionidae Grube, 1850 of the annelid suborder Spioniformia were studied here. Taxonomic data are presented for 25 species from 98 records as identified by a combination of morphological and genetic approaches. Although sub-optimal morphological condition can prevent new species being formally described, it is essential that morphological, molecular, and voucher data are made available for future surveys. Descriptions of two new species— Poecilochaetus brenkei sp. nov. and Laonice shulseae sp. nov.—increase the number of formally described new annelid species from the areas targeted in this study to 15 and CCZ-wide to 46. We also discuss the commonly reported “cosmopolitan” deep-sea spionid Aurospio dibranchiata Maciolek, 1981, which we show represents several genetically distinct species (three of these from CCZ area alone) but without reliable morphological characters to separate them. Molecular data provide evidence that 15 out of 25 species reported here have a wide distribution within the eastern CCZ and that Aurospio sp. “NHM_2186” and the known species Prionospio amarsupiata Neal & Altamira in Paterson et al. 2016 may be cosmopolitan. Lastly, the molecular data provide insights into relationships within Spioniformia, suggesting that both Poecilochaetidae and Trochochaetidae belong within Spionidae.
    Type: Article , PeerReviewed
    Format: text
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  • 2
    Publication Date: 2024-05-14
    Description: Holothurians are the dominant megabenthic deposit feeders in the Peru Basin (SE Pacific) and feed to various degrees of selectivity on a heterogenous pool of sedimentary detritus, but drivers of feeding selectivity and diet preferences for most holothurian species are unknown. This study reconstructs the diets of 13 holothurian species of the orders Elasipodida, Holothuriida, and Synallactida. Bulk stable isotope analyses (δ13C, δ15N) of holothurian body wall and gut wall tissues, gut contents, and feces were combined with compound-specific stable isotope analyses of amino acids, phospholipid-derived fatty acids, and neutral-lipid-derived fatty acids in the body wall. We further assessed how holothurians in the Peru Basin partition their resources and calculated how much of the daily particulate organic carbon (POC) flux to the area is ingested by them using information about gut contents of nine species. To assess the dependence of holothurians on fresh phytodetritus, we performed in situ pulse-chase experiments using 13C- and 15N-enriched phytodetritus. By measuring the uptake of this phytodetritus in fatty acids and amino acids and by comparing it with the presence of these compounds in the sediment, we calculated net accumulation and net deficiency for specific fatty acids and amino acids and discussed how climate change might affect the dependence on specific compounds. A Sørensen–Dice coefficient-based cluster analysis using data from trophic levels, levels of heterotrophic re-synthesis of amino acids, feeding selectivity, and food sources/diet suggested two major trophic groups with two optional subgroups each. Species-specific traits of locomotion, tentacle morphology, and gut structure likely allow resource partitioning and differences in selectivity among the holothurians, of which a subpopulation of 65% of all specimens can ingest 4 to 27% of the daily POC flux to the Peru Basin. Holothurians are specifically dependent on the uptake of arachidonic acid from phytodetritus, while most essential amino acids are available in the Peru Basin in sufficient concentrations.
    Type: Article , PeerReviewed
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  • 3
    Publication Date: 2024-05-14
    Description: The deep seafloor of the Northeastern Pacific Ocean between the Clarion and Clipperton Fracture Zones (CCZ) hosts large deposits of polymetallic nodules that are of great commercial interest as they are rich in valuable metals such as manganese, nickel, copper and cobalt. However, mining of these nodules has the potential to severely affect the benthic fauna, whose distribution and diversity are still poorly understood. The CCZ is characterized by strong gradients in sea surface productivity and hence changes in the amount of organic carbon reaching the seafloor, decreasing from mesotrophic conditions in the southeast to oligotrophic conditions in the northwest. Uncovering and understanding changes in community composition and structure along this productivity gradient are challenging but important, especially in the context of future mining impacts. Here, we summarize published data on benthic annelids (polychaetes), a major component of macrobenthic communities in the CCZ. Unlike previous studies, we attempt to explore all available data based on both morphology and genetics collected by box corer and epibenthic sledge. In this regard, we specifically aimed to (a) summarize and compare morphological and molecular data in relation to surface water nutrient conditions and (b) provide recommendations to advance the studies of polychaete biodiversity. Although initial studies on polychaetes in the CCZ were performed as far back as the 1970s, there are still large data gaps further explored in our review. For example, most of the current data are from the eastern CCZ, limiting understanding of species ranges across the region. An association between polychaete communities and the available food supply was generally observed in this study. Indeed, mesotrophic conditions supported higher abundance and species richness in polychaetes as a whole, but for certain groups of species, the patterns appear to be opposite — illustrating that relationships are likely more complex at lower taxonomic levels. A better understanding of biogeographical, ecological and evolutionary processes requires a concerted effort involving increased sampling and sharing of data and material to close existing knowledge gaps.
    Type: Article , PeerReviewed
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  • 4
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    PANGAEA
    In:  Institut für Interdisziplinäre Gebirgsforschung der Österreichischen Akademie der Wissenschaften, Innsbruck
    Publication Date: 2024-05-14
    Description: The glacier mass balance of Jamtalferner has been measured annually since 1988/1989 with the direct/glaciological method. Winter mass balance has been determined for 1st May in all years. The mass balance records are complemented by precipitation measurements at a gauge close to the glacier tongue and climate data recorded at the village of Galtür. New data will be added every year.
    Type: Dataset
    Format: application/zip, 69 datasets
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  • 5
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    PANGAEA
    In:  Institut für Interdisziplinäre Gebirgsforschung der Österreichischen Akademie der Wissenschaften, Innsbruck
    Publication Date: 2024-05-14
    Description: The annual glacier mass balance of Mullwitzkees in Hohe Tauern is measured since 2006-10-01 with the direct glaciological method in the fixed date system (1st October to 30th September of the following year). The accumulation of snow is measured by determination of the water equivalent in 6 snow pits, the ice ablation is measured with 15 stakes drilled into the ice. Results are the annual net mass balance in kg, the total accumulation and ablation, the glacier area and the portions of the area which are subject to ablation and accumulation, the elevation of the equilibrium line and the specific mass balance in kg/m**3 (= mm w.e.). The accumulation during the winter is determined by the 1st May. The project is funded by the "Hydrographischer Dienst der Abteilung Wasserwirtschaft des Amtes der Tiroler Landesregierung and National Park Hohe Tauern". New data will be added every year.
    Keywords: Glaciers Austria; Mullwitzkees, Hohe Tauern, Austria; MWK
    Type: Dataset
    Format: application/zip, 34 datasets
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  • 6
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    In:  Supplement to: Myers-Smith, Isla H; Harden, J W; Wilmking, Martin; Fuller, C C; McGuire, A David; Chapin, F Stuart (2008): Wetland succession in a permafrost collapse: interactions between fire and thermokarst. Biogeosciences, 5(5), 1273-1286, https://doi.org/10.5194/bg-5-1273-2008
    Publication Date: 2024-05-14
    Description: To determine the influence of fire and thermokarst in a boreal landscape, we investigated peat cores within and adjacent to a permafrost collapse feature on the Tanana River Floodplain of Interior Alaska. Radioisotope dating, diatom assemblages, plant macrofossils, charcoal fragments, and carbon and nitrogen content of the peat profile indicate ~600 years of vegetation succession with a transition from a terrestrial forest to a sedge-dominated wetland over 100 years ago, and to a Sphagnum-dominated peatland in approximately 1970. The shift from sedge to Sphagnum, and a decrease in the detrended tree-ring width index of black spruce trees adjacent to the collapse coincided with an increase in the growing season temperature record from Fairbanks. This concurrent wetland succession and reduced growth of black spruce trees indicates a step-wise ecosystem-level response to a change in regional climate. In 2001, fire was observed coincident with permafrost collapse and resulted in lateral expansion of the peatland. These observations and the peat profile suggest that future warming and/or increased fire disturbance could promote permafrost degradation, peatland expansion, and increase carbon storage across this landscape; however, the development of drought conditions could reduce the success of both black spruce and Sphagnum, and potentially decrease the long-term ecosystem carbon storage.
    Keywords: Alaska, USA; International Polar Year (2007-2008); IPY; PERM; Sampling permafrost; Tanana_R-plain
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 7
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    PANGAEA
    In:  Institut für Interdisziplinäre Gebirgsforschung der Österreichischen Akademie der Wissenschaften, Innsbruck
    Publication Date: 2024-05-14
    Description: The annual glacier mass balance of Hallstätter Gletscher in Austria is measured since 2006-10-01 with the direct glaciological method in the fixed date system (1st October to 30th September of the following year). The accumulation of snow is measured by determination of the water equivalent in 6 snow pits, the ice ablation is measured with 15 stakes drilled into the ice. Results are the annual net mass balance in kg, the total accumulation and ablation, the glacier area and the portions of the area which are subject to ablation and accumulation, the elevation of the equilibrium line and the specific mass balance in kg/m**2 (= mm w.e.). The accumulation during the winter is determined by the 1st May. The project is funded by the Amt der Oberösterreichischen Landesregierung and the Energie AG. The measurements are carried out by the Institute for Interdisciplinary Mountain Research (http://www.mountainresearch.at/index.php/en/) of the Austrian Academy of Sciences and the company Blue Sky in Gmunden, Austria. New data will be added every year.
    Keywords: Glaciers Austria; Hallstätter Gletscher, Dachstein, Austria; HSG
    Type: Dataset
    Format: application/zip, 39 datasets
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  • 8
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    In:  Institut für Interdisziplinäre Gebirgsforschung der Österreichischen Akademie der Wissenschaften, Innsbruck
    Publication Date: 2024-05-14
    Description: The Venedigerkees in the Hohe Tauern National Park is the easternmost tributary glacier to the former tongue of Obersulzbachkees. As a result of the strong retreat of Obersulzbachkees, the glacier disintegrated into several tributary glaciers, with a large lake remaining at the location of a famous serac zone, the 'Türkische Zeltstadt'. Hydrological monitoring of the area is done by the Hydrological Survey of the Federal Government of Salzburg (DI Hans Wiesenegger) who initiated the mass balance monitoring programme together with Heinz Slupetzky and the Institute of Interdisciplinary Mountain Research of the Austrian Academy of Sciences. The mass balance of the Venedigerkees is measured since 2011/12 with the direct or glaciological method. New data will be added every year.
    Keywords: Glaciers Austria
    Type: Dataset
    Format: application/zip, 24 datasets
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  • 9
    Publication Date: 2024-05-14
    Description: We report the levels of airborne PCB concentrations at 18 locations for three consecutive periods, from July to November of 2015, and one extra period from July to August of 2016 in New Bedford, Fairhaven, Dartmouth, and Acushnet, MA, USA. Measurements were obtained using polyurethane foam passive air samplers (PUF-PAS), deployed for ~40 days. Effective volumes for individual PCB congeners were calculated from a previously published model and included here. Further, the limit of detection from the PUF for individual PCB congeners are included, together with the masses of the PCB congeners measured in the PUF.
    Keywords: airborne concentration; congeners; effective volumes; New Bedford; PCB; Superfund
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 10
    Publication Date: 2024-05-14
    Keywords: 02260100; 02281147; 03041555; 03071108; 03081605; 03092330; 03112138; 03130720; 03181915; 03200715; 03211750; 03281830; 09070100; 09080637; 09171830; 119-745B; 61SL; 7TOW_5; 7TOW05WT; 7TOW-072; 7TOW-105; ANTA95-157; ANTA96-1; ANTA96-16; ANTA96-17; ANTIPODE; ANT-IV/3; ANT-IX/3; ANTP-226G; ANTP-231G; ANT-V/4; ANT-VI/3; ANT-VIII/6; APSARA1; APSARA2; APSARA3; APSARA4; AT_II-107_71; AT_II-107_78; AT_USA; ATII_USA; Atka Bay; Atlantis (1931); Atlantis II (1963); Barents Sea; C12/8712GC9; Camp Norway; Coral Sea; cruise 11; CTD/Rosette; CTD-RO; DEPTH, sediment/rock; DF85; DF85.062-PC; DF85.072-PC; DF85.114-PC; DF85.119-PC; DF85.125-PC; DRILL; Drilling/drill rig; Eastern Weddell Sea, Southern Ocean; Elevation of event; ELT05; ELT05.012-PC; ELT05.016-PC; ELT05.017-PC; ELT05.018-PC; ELT05.019-PC; ELT05.024-PC; ELT05.025-PC; ELT07; ELT07.001-PC; ELT07.007-PC; ELT07.008-PC; ELT07.009-PC; ELT07.010-PC; ELT07.011-PC; ELT07.012-PC; ELT07.013-PC; ELT07.014-PC; ELT07.015-PC; ELT07.017-PC; ELT08; ELT08.006-PC; ELT08.008-PC; ELT08.010-PC; ELT08.012-PC; ELT08.013-PC; ELT08.019-PC; ELT09; ELT09.013-PC; ELT09.015-PC; ELT09.016-PC; ELT10; ELT10.005-PC; ELT10.008-PC; ELT10.009-PC; ELT10.010-PC; ELT10.012-PC; ELT10.013-PC; ELT10.014-PC; ELT10.016-PC; ELT10.018-PC; ELT10.019-PC; ELT10.020-PC; ELT10.021-PC; ELT10.022-PC; ELT10.024-PC; ELT10.025-PC; ELT10.027-PC; ELT10.028-PC; ELT10.029-PC; ELT10.030-PC; ELT10.031-PC; ELT10.032-PC; ELT11; ELT11-001-PC; ELT11-002-PC; ELT11-003-PC; ELT11-004-PC; ELT11-006-PC; ELT11-007-PC; ELT11-008-PC; ELT11-010-PC; ELT11-012-PC; ELT11-014-PC; ELT11-015-PC; ELT11-018-PC; ELT11-020-PC; ELT11-022-PC; ELT11-023-PC; ELT11-025-PC; ELT11-026-PC; ELT11-029-PC; ELT11-031-PC; ELT11-035-PC; ELT13; ELT13.001-PC; ELT13.002-PC; ELT13.003-PC; ELT13.004-PC; ELT13.005-PC; ELT13.006-PC; ELT13.008-PC; ELT13.009-PC; ELT13.011-PC; ELT13.013-PC; ELT13.015-PC; ELT13.016-PC; ELT13.017-PC; ELT13.019-PC; ELT13.020-PC; ELT13.021-PC; ELT13.022-PC; ELT13.024-PC; ELT14; ELT14.003-PC; ELT14.004-PC; ELT14.005-PC; ELT14.006-PC; ELT14.008-PC; ELT14.010-PC; ELT14.011-PC; ELT14.012-PC; ELT14.013-PC; ELT14.015-PC; ELT14.016-PC; ELT15; ELT15.002-PC; ELT15.004-PC; ELT15.005-PC; ELT15.006-PC; ELT15.007-PC; ELT15.009-PC; ELT15.011-PC; ELT15.015-PC; ELT15.022-PC; ELT15.023-PC; ELT15.028-PC; ELT17; ELT17.005-PC; ELT17.006-PC; ELT17.007-PC; ELT17.009-PC; ELT17.011-PC; ELT17.013-PC; ELT17.014-PC; ELT17.015-PC; ELT17.016-PC; ELT17.017-PC; ELT17.018-PC; ELT17.020-PC; ELT17.021-PC; ELT17.022-PC; ELT17.023-PC; ELT17.026-PC; ELT17.028-PC; ELT17.029-PC; ELT17.030-PC; ELT17.032-PC; ELT17.033-PC; ELT18; ELT18.002-PC; ELT18.003-PC; ELT18.004-PC; ELT19; ELT19.001-PC; ELT19.004-PC; ELT19.005-PC; ELT19.006-PC; ELT19.008-PC; ELT19.014-PC; ELT19.015-PC; ELT19.024-PC; ELT19.026-PC; ELT19.027-PC; ELT20; ELT20.004-PC; ELT20.006-PC; ELT20.007-PC; ELT20.008-PC; ELT20.009-PC; ELT20.010-PC; ELT20.011-PC; ELT20.014-PC; ELT21; ELT21.016-PC; ELT21.018-PC; ELT21.020-PC; ELT21.021-PC; ELT21.023-PC; ELT22; ELT22.001-PC; ELT22.005-PC; ELT22.006-PC; ELT22.009-PC; ELT22.010-PC; ELT22.033-PC; ELT22.034-PC; ELT23; ELT23.001-PC; ELT23.004-PC; ELT23.005-PC; ELT23.006-PC; ELT23.008-PC; ELT23.009-PC; ELT23.010-PC; ELT23.011-PC; ELT23.012-PC; ELT23.013-PC; ELT23.014-PC; ELT23.016-PC; ELT23.017-PC; ELT23.019-PC; ELT25; ELT25.007-PC; ELT25.008-PC; ELT25.009-PC; ELT25.010-PC; ELT25.011-PC; ELT25.012-PC; ELT25.013-PC; ELT25.014-PC; ELT25.015-PC; ELT25.016-PC; ELT26; ELT26.001-PC; ELT27; ELT27.004-PC; ELT33; ELT33.002-PC; ELT33.004-PC; ELT33.005-PC; ELT33.006-PC; ELT33.007-PC; ELT33.010-PC; ELT33.012-PC; ELT33.014-PC; ELT33.015-PC; ELT33.017-PC; ELT33.018-PC; ELT33.019-PC; ELT33.022-PC; ELT37; ELT37.004-PC; ELT39; ELT39.075-PC; ELT39.077-PC; ELT42; ELT42.004-PC; ELT42.005-PC; ELT42.007-PC; ELT42.008-PC; ELT42.009-PC; ELT42.010-PC; ELT42.011-PC; ELT42.012-PC; ELT43; ELT43.003-PC; ELT43.005-PC; ELT45; ELT45.029-PC; ELT45.063-PC; ELT45.064-PC; ELT49; ELT49.006-PC; ELT49.007-PC; ELT49.019-PC; ELT49.033-PC; ELT49.051-PC; ELT50; ELT50.009-PC; ELT50.011-PC; ELT50.013-PC; ELT50.017-PC; Eltanin; Event label; Filchner Trough; GC; Giant box corer; Giant gravity corer AWI; GKG; Glacier; Gravity corer; Gravity corer (Kiel type); GSL; Halley Bay; Indian Ocean; IO0775; IO0775.046-PC; IO0775.047-PC; IO0775.048-PC; IO0775.050-PC; IO0775.051-PC; IO0775.052-PC; IO0775.053-PC; IO0775.054-PC; IO0775.055-PC; IO0775.057-PC; IO1176; IO1176.055-PC; IO1176.079-PC; IO1277; IO1277.010-PC; IO1578; IO1578.002-PC; IO1578.004-PC; IO1578.049-PC; IO1678; IO1678.018-PC; IO1678.019-PC; IO1678.020-PC; IO1678.021-PC; IO1678.022-PC; IO1678.023-PC; IO1678.024-PC; IO1678.025-PC; IO1678.026-PC; IO1678.027-PC; IO1678.028-PC; IO1678.029-PC; IO1678.030-TC; IO1678.032-PC; IO1678.033-PC; IO1678.034-PC; IO1678.035-PC; IO1678.036-PC; IO1678.096-PC; Islas Orcadas; Joides Resolution; Kapp Norvegia; KR87-02; KR87-07; KR88-08; KR88-10; KR88-15; KR88-24; Latitude of event; Lazarev Sea; Leg119; Longitude of event; Lyddan Island; Marion Dufresne (1972); Maud Rise; MD10; MD38; MD76-118; MD82-424; MD82-434; MD84-527; MD84-551; MD87-715; MD88-014; MD88-769; MD88-770; MD88-773; Melville; MUC; MultiCorer; Nathaniel B. Palmer; NBP9604; NBP9604-02-2; NBP9604-03-2; NBP9604-07-1; NBP9802; NBP9802-01-4; NBP9802-02-5; NBP9802-03-9; NBP9802-04-2; NBP9802-05-12; NBP9802-05-3; NBP9802-06-3; NBP9802-07-4; NBP9802-08-1; NBP9802-09-10; NBP9802-09-2; NBP9802-10-5; NZ-80-G-10; NZ-80-G-11; NZ-80-G-12; NZ-80-G-13; NZ-80-G-6; NZ-80-G-7; Opal, biogenic silica; OPR-476156; OPR-476184; OPR-476208; OSIRIS II; PC; Piston corer; Polarstern; PS08; PS08/347; PS08/365; PS08/366; PS10; PS10/672; PS10/675; PS10/678; PS10/699; PS10/701; PS10/711; PS10/719; PS10/725; PS10/738; PS10/784; PS10/816; PS10/818; PS10/820; PS10/824; PS12; PS12/248; PS12/289; PS12/300; PS12/302; PS12/305; PS12/310; PS12/312; PS12/319; PS12/336; PS12/338; PS12/340; PS12/344; PS12/352; PS12/366; PS12/368; PS12/374; PS12/380; PS12/382; PS12/458; PS12/465; PS12/486; PS12/490; PS12/536; PS1375-3; PS1387-3; PS1388-3; PS1472-3; PS1474-3; PS1475-2; PS1483-3; PS1484-3; PS1487-1; PS1488-3; PS1489-3; PS1490-3; PS1500-2; PS1506-1; PS1507-3; PS1508-1; PS1509-2; PS1575-1; PS1587-1; PS1590-2; PS1591-1; PS1593-3; PS1595-1; PS1596-3; PS1599-3; PS16; PS16/534; PS1605-1; PS1606-3; PS1607-3; PS1609-3; PS1613-1; PS1619-3; PS1620-1; PS1622-3; PS1625-3; PS1626-2; PS1635-3; PS1636-1; PS1638-3; PS1639-3; PS1648-1; PS18; PS18/185; PS1821-6; PS2038-2; R05-32; RC08; RC08-78; RC08-79; RC08-80; RC08-81; RC08-82; RC08-83; RC08-85; RC08-87; RC08-89; RC08-91; RC08-93; RC09; RC09-109; RC09-110; RC09-111; RC09-112; RC09-113; RC09-114; RC09-115; RC09-117; RC09-118; RC09-121; RC09-150; RC10; RC10-117; RC11; RC11-116; RC11-117; RC1112; RC11-123; RC11-124; RC11-125; RC11-126; RC11-134; RC11-139; RC11-76; RC11-77; RC11-78; RC11-83; RC11-86; RC11-94; RC11-97; RC12; RC12-100; RC12-101; RC12-103; RC12-206; RC12-210; RC12-213; RC12-214; RC12-215; RC12-217; RC12-218; RC12-219; RC12-220; RC12-221; RC12-223; RC12-224; RC12-225; RC12-227; RC12-228; RC12-230; RC12-231; RC12-232; RC12-267; RC12-305; RC13; RC13-254; RC13-255; RC13-256; RC13-259; RC13-261; RC13-263; RC13-269; RC13-271; RC13-41; RC13-42; RC13-43; RC13-45TW; RC14; RC14-7; RC15; RC15-30; RC15-31; RC15-37; RC15-40; RC15-65; RC15-94; RC17; RC17-54; RC17-61; Robert Conrad; Ross Sea; S68PC16; S68PC22; Sample code/label; Silicon Cycling in the World Ocean; SINOPS; SL; SO36/2; SO36/2_61SL; Sonne; South Atlantic; South Atlantic Ocean; Southern East Pacific Rise; Southern Ocean; South Indian Ocean; South Orkney; South Pacific; South Pacific Ocean; South Tasman Rise; Tasman Sea; Thomas Washington; V16; V16-127; V16-129; V16-131; V16-133; V16-134; V16-81; V16-82; V16-87; V16-91; V16-96; V18; V18-188; V18-189; V18-192; V18-68; V19; V19-80; V19-87; V19-88; V20; V20-200; V21; V21-52; V21-53; V21-54; V21-55; V21-56; V21-57; V22; V22-108; V24; V24-206; V29; V29-104; V29-105; van Veen Grab; Vema; VGRAB; Weddell Sea; Wegener Canyon
    Type: Dataset
    Format: text/tab-separated-values, 990 data points
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