ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

X
feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • PANGAEA  (38,001)
  • 2020-2024  (34,743)
  • 1985-1989  (3,258)
Collection
Keywords
Publisher
Language
Years
Year
  • 1
    facet.materialart.
    Unknown
    Sedimentological, palynological, geochemical, palaeomagnetic, geochronological, and sediment physical investigations of cores 1R to 5R from MARUM-MeBo70 Site PS104_21-3 (2022)
    PANGAEA
    Details
    Publication Date: 2024-07-05
    Description: Here we present sedimentological, micropalaeontological, inorganic and organic geochemical, palaeomagnetic, geochronological, and sediment physical data obtained from successional drill cores 1R to 5R at MARUM-MeBo70 Site PS104_21-3 (73.31°S,107.11°W; 882 m water depth). The site is located within the Pine Island cross-shelf trough in the Amundsen Sea Embayment (ASE), West Antarctica and was drilled during RV Polarstern Expedition PS104 in 2017.
    Keywords: climate; Eocene-Oligocene Transition; palaeoenvironment; West Antarctica; West Antarctic Ice Sheet
    Type: Dataset
    Format: application/zip, 14 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 2
    facet.materialart.
    Unknown
    Centrolophus niger south of Iceland in July 2017 and July 2021 (2023)
    PANGAEA
    Details
    Publication Date: 2024-07-05
    Description: This data set has biological measurements and stomach content analysis for fourteen specimens of Centrolophus niger which were frozen whole at sea during the Icelandic part of the International Ecosystem Summer Survey in Nordic Seas (IESSNS) in July 2017 and July 2021. In 2017, three specimens were collected to confirm species identification by a specialist at home institute. In 2021, all caught specimens were collected for detailed biological study. The C. niger were by-catch in a scientific pelagic ecosystem survey which includes trawling, cod-end mesh size 50 mm, in the surface layer, trawl headline visible in surface and foot rope at approximately 35 m depth. For detailed information about the surveys see the cruise reports attached to the campaigns. The data is provided by the Marine and Freshwater Research Institute (MFRI) in Iceland.
    Keywords: Centrolophus niger; mesopelagic; prey; rare; Stomach contents; SUMMER; Sustainable Management of Mesopelagic Resources
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 3
    facet.materialart.
    Unknown
    Hydrographic CTD and bottle (stable water isotope, nutrient, and alkalinity) data for August-September 2017 on the Northeast Greenland shelf (2023)
    PANGAEA
    Details
    Publication Date: 2024-07-05
    Description: This is a hydrographic dataset containing CTD cast and rosette bottle data from two consecutive cruises (NEG2017 and NorthGreen) on the research vessel RV Dana between 23-08-2017 and 01-10-2017 of 2017 on the Northeast Greenland shelf. Both cruises took place between 73.3197 to 80.0519 latitude and 2.1011 to 21.2039 longitude (decimal). The NEG2017 cruise took place from 23 August 2017 to 11 September 2017 was part of the Strategic Environmental program for Northeast Greenland with as its goal to provide environmental impact information pertaining to potential oil exploitation and oil spill response activities in the region. The cruise leader for NEG2017 was Eva Friis Møller. The NorthGreen2017 cruise took place directly after the first between 11 September 2017 and 1 October 2017. It aimed to collect data pertaining to hydroraphical and environmental changes on the shelf. The cruise leader for the NorthGreen2017 cruise was Marit-Solveig Seidenkrantz.
    Keywords: CTD/Casts; CTD/Rosette; Northeast Greenland
    Type: Dataset
    Format: application/zip, 6 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 4
    facet.materialart.
    Unknown
    Palynological, palaeomagnetic, and sediment physical investigations of cores 1R to 3R from MARUM-MeBo70 Site PS104_21-2 (2022)
    PANGAEA
    Details
    Publication Date: 2024-07-05
    Description: Here we present palynological, palaeomagnetic, and sediment physical data obtained from successional drill cores 1R to 3R at MARUM-MeBo70 Site PS104_21-2 (73.31°S,107.11°W; 882 m water depth). The site is located within the Pine Island cross-shelf trough in the Amundsen Sea Embayment (ASE), West Antarctica and was drilled during RV Polarstern Expedition PS104 in 2017. The site is less than a kilometer away from MARUM-MeBo70 Site PS104_21-3.
    Keywords: climate; Eocene-Oligocene Transition; palaeoenvironment; West Antarctica; West Antarctic Ice Sheet
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 5
    facet.materialart.
    Unknown
    Point mass balance of Mullwitzkees, Austria, 2006/07 et seq (2024)
    PANGAEA
    Details
    Publication Date: 2024-07-05
    Description: Glaciological mass balance parameters are measured as part of the monitoring program at Mullwitzkees in the Hohe Tauern Range, Austria, since the 2006/07 hydrological season. The data sets include glacier wide subseasonal, seasonal and annual point mass balance for the ablation stake and snow pit network, as well as records of snow depth probing. Fixed date values for the hydrological season (winter: 1 Oct - 30 Apr; year: 1 Oct - 30 Sep) are derived by extrapolating from the measurement dates closest to the fixed dates. Detailed information is given in Hartl et al. (2024) and in the associated readme files. New data will be added every year.
    Keywords: Glacier mass balance; LTER; Mountain meteorology
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 6
    facet.materialart.
    Unknown
    Point mass balance of Venedigerkees, Austria, 2011/12 et seq (2024)
    PANGAEA
    Details
    Publication Date: 2024-07-05
    Description: Glaciological mass balance parameters are measured as part of the monitoring program at Venedigerkees in the Hohe Tauern Range, Austria, since 2011/12. The data sets include glacier wide subseasonal, seasonal and annual point mass balance for the ablation stake and snow pit network, as well as records of snow depth probing. Fixed date values for the hydrological season (winter: 1 Oct - 30 Apr; year: 1 Oct - 30 Sep) are derived by extrapolating from the measurement dates closest to the fixed dates. Detailed Information is given in Hartl et al. (2024) and in the associated readme files. New data will be added every year.
    Keywords: Glacier mass balance; LTER; Mountain meteorology
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 7
    facet.materialart.
    Unknown
    Concentrations of total N, total P, and gases in an oxygen-deficient upwelling system during El Niño (2019) (2023)
    PANGAEA
    Details
    Publication Date: 2024-07-05
    Description: Seawater samples were collected in four stations along a cross-shore transect in front of the Port of Mazatlán (Mexico) during the oceanographic cruise Maz V (April 2019) on board the R/V “El Puma” (UNAM). Samples were collected at different depths based on the oxygen and chlorophyll-a profiles: surface (5 m depth); mixed layer, deep chlorophyll maximum (at 10–45 m depth); oxycline, base of the oxycline (at 60–125 m depth); upper OMZ; OMZ core (at 250 m depth); and bottom (between 23 m depth in S1 and 670 m depth in S4). Total N and P were determined using a Skalar San-Plus segmented-flow autoanalyzer. Dissolved gases were analyzed through the addition of 5 mL of ultrapure helium into the vials to generate a static-headspace equilibration. N2O was analyzed with a Varian 3380 gas chromatograph using an electron capture detector. CH4 was analyzed with a Schimadzu 17A gas chromatograph with a flame ionization detector and a capillary column.
    Keywords: Campaign; CTD, Sea-Bird, SBE 19plus; Depth, description; DEPTH, water; El Nino Southern Oscillation; El Puma; Event label; Gas chromatograph, Shimadzu, 17A; Gas chromatograph, Varian, Inc.. 3380; Maz_V_S1; Maz_V_S2; Maz_V_S3; Maz_V_S4; Maz V; Methane, dissolved; Mexican Pacific; Nitrogen, total; nitrogen genes; Nitrous oxide, dissolved; oxygen minimum zone; Phosphorus, total; Port of Mazatlán; prokaryotic community; Sample code/label; Segmented flow auto-analyzer, Skalar Analytical B.V, San++; Station label
    Type: Dataset
    Format: text/tab-separated-values, 192 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 8
    facet.materialart.
    Unknown
    Abundance of N-cycling genes in an oxygen-deficient upwelling system during La Niña (2018) and El Niño (2019) (2023)
    PANGAEA
    Details
    Publication Date: 2024-07-05
    Description: Seawater samples were collected with 10-L Niskin bottles in four stations along a cross-shore transect in front of the Port of Mazatlán (Mexico) during the oceanographic cruises Maz IV (April 2018) and Maz V (April 2019) on board the R/V "El Puma" (UNAM). Samples for molecular analyses (abundance of N-cycling genes) were collected at different depths based on the oxygen and chlorophyll-a profiles: surface (5 m depth); mixed layer, deep chlorophyll maximum (at 10–45 m depth); oxycline, base of the oxycline (at 60–125 m depth); upper OMZ (only for Maz V); OMZ core (at 250 m depth); and bottom (between 23 m depth in S1 and 670 m depth in S4). Water samples were filtered on board through polycarbonate membranes (0.22-μm pore, Merck Millipore). Genomic DNA was extracted with the DNeasy PowerWater Kit (Qiagen). The abundance of N-cycling genes was assessed using the gene copy number of bacterial and archaeal amoA, anammox bacterial 16S rRNA, nirK, nirS, and nrfA, using a StepOnePlus real-time PCR system (Applied Biosystems).
    Keywords: Campaign; CTD, Sea-Bird, SBE 19plus; Date/Time of event; Depth, description; DEPTH, water; Elevation of event; El Nino Southern Oscillation; El Puma; Event label; Gene copies per volume; Gene name; Latitude of event 2; Longitude of event; Maz_IV_S1; Maz_IV_S2; Maz_IV_S3; Maz_IV_S4; Maz_V_S1; Maz_V_S2; Maz_V_S3; Maz_V_S4; Maz IV; Maz V; Mexican Pacific; nitrogen genes; oxygen minimum zone; Port of Mazatlán; prokaryotic community; Real-Time PCR, Applied Biosystems, StepOnePlus; Sample code/label; Station label
    Type: Dataset
    Format: text/tab-separated-values, 1620 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 9
    facet.materialart.
    Unknown
    Seasonality of zooplankton active flux in the Canary Current System during COCA I and COCA II cruises in 2002 and 2003 (2024)
    PANGAEA
    Details
    Publication Date: 2024-07-05
    Description: The biological carbon pump is the mechanism by which the organic matter is exported or sequestered in the deep ocean from years to millennia. This downward transport is performed through physical transport of dissolved and particulate organic carbon, the sinking of particles or passive flux, and the active transport by diel and seasonal vertical migrants. The latter mechanism is still poorly studied, and seasonality of this active flux is even less known. We studied active flux by zooplankton in two transects from the productive coastal transition zone off Northwest Africa to the warm oligotrophic ocean. We estimated the metabolic activity from the surface to 900 m depth using the enzymatic activity of the electron transfer system (ETS) as a proxy for respiration. We found zooplankton ETS activity significantly higher during spring than during fall in the mesopelagic zone. Even at similar migrant biomass values, respiratory flux was higher during spring compared to fall due to the important differences in respiration rates in the mesopelagic zone. These striking differences of respiration rates in the mesopelagic zone was mainly due to the smaller body size of zooplankton during the productive season (spring). These results should be considered in models of active carbon export in the ocean. Here, we provide the data compiled during both cruises (spring and fall).
    Keywords: 02; 08; 14; 22; 29HE20020910; 29HE20030520; 32; 42; 48; 52; 60; 66; biological carbon pump; Calculated; COCA-1; COCA-1_02-4; COCA-1_08-4; COCA-1_14-4; COCA-1_22-4; COCA-1_32-4; COCA-1_42-4; COCA-1_48-4; COCA-1_52-4; COCA-1_60-4; COCA-1_66-4; COCA-2; COCA-2_02-4; COCA-2_08-4; COCA-2_14-4; COCA-2_22-4; COCA-2_42-4; COCA-2_48-4; COCA-2_52-4; COCA-2_60-4; COCA-2_66-4; Date/Time of event; DEPTH, water; Electron transport system activity of oxygen per mass; ETS activity; Event label; Hespérides; Latitude of event; LHPR; Longitude of event; OPC; Optical plankton counter, Focal Technologies Inc., OPC-1L; Optional event label; Plankton recorder, Longhurst-Hardy; respiration flux; Spectrophotometry according to Lowry et al. (1951) [modified after Rutter (1967)]; SUMMER; Sustainable Management of Mesopelagic Resources; Tetrazolium reduction technique according to Packard (1971); Time of day; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management; Zooplankton; Zooplankton, biomass as protein; Zooplankton, biomass as protein per individual
    Type: Dataset
    Format: text/tab-separated-values, 6153 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 10
    facet.materialart.
    Unknown
    Nitrous oxide distribution in the continental shelf off Central Chile (2005-2009) (2020)
    PANGAEA
    Details
    Publication Date: 2024-07-05
    Description: Continental shelves tend to have high standing stocks of organic carbon and high rates of primary production relative to the open ocean and serve as important link between land and the ocean interior and between the sediment and the water column, playing a key role in the N and C balance, and accounting for up to 50% of the total N loss. One of the widest continental shelves in the eastern South Pacific (ESP) is present off central Chile (36°S). This is an important geographic feature in terms of physical and biological interactions owing to the large area available for coupling between the benthic and pelagic systems. In addition, this area is subjected to a strong coastal upwelling during austral spring and summer; when winds shift to a predominantly northward direction, stressing the sea surface layer and producing an intense cross-shelf transport and uplift of Equatorial Subsurface waters (ESSW) over the shelf. The ESSW, characterized by high NO3- and low O2 content, promotes surface fertilization and, subsequently, intense organic matter respiration and remineralization at depth, along with an efflux of subsurface-accumulated N2O (Farías et al. 2009, Cornejo & Farías, 2012). Thus, periods of maximum productivity and intense suboxia, or even anoxia, when diverse electron donors (e.g., organic matter, NH4+, NO2-, H2S) are present, represent a potential hotspot for fixed N removal processes. We present a data set that has been obtained during different FIP cruises (Fondo de Investigaciones Pesqueras) (2005-2009) which consisted of several transects perpendicular to the coast between 35° and 40°S and from the coast to 77.8° W (central Chile). Data collected include classical oceanographic variables including N2O and important greenhouse gas.
    Keywords: Abate Molina; Automated WInkler method (AULOX); Colorimetry, flow-segmented (Grasshoff et al. 1983); Cruise/expedition; CTD/Rosette; CTD-O probe; CTD-RO; Date/Time of event; DEPTH, water; eastern South Pacific; Event label; Gas chromatograph (Shimadzu 17A) with an electron capture detector (ECD); Greenhouse gases; Latitude of event; Longitude of event; MOBIO; MOBIO-2005-1; MOBIO-2005-10; MOBIO-2005-11; MOBIO-2005-13; MOBIO-2005-17; MOBIO-2005-20; MOBIO-2005-21; MOBIO-2005-23; MOBIO-2005-25; MOBIO-2005-27; MOBIO-2005-3; MOBIO-2005-30; MOBIO-2005-31; MOBIO-2005-33; MOBIO-2005-35; MOBIO-2005-37; MOBIO-2005-40; MOBIO-2005-41; MOBIO-2005-43; MOBIO-2005-45; MOBIO-2005-47; MOBIO-2005-5; MOBIO-2005-50; MOBIO-2005-7; MOBIO-2006-1; MOBIO-2006-11; MOBIO-2006-12; MOBIO-2006-13; MOBIO-2006-14; MOBIO-2006-15; MOBIO-2006-16; MOBIO-2006-17; MOBIO-2006-18; MOBIO-2006-19; MOBIO-2006-2; MOBIO-2006-20; MOBIO-2006-21; MOBIO-2006-22; MOBIO-2006-23; MOBIO-2006-25; MOBIO-2006-26; MOBIO-2006-27; MOBIO-2006-28; MOBIO-2006-29; MOBIO-2006-3; MOBIO-2006-30; MOBIO-2006-31; MOBIO-2006-32; MOBIO-2006-33; MOBIO-2006-34; MOBIO-2006-35; MOBIO-2006-36; MOBIO-2006-37; MOBIO-2006-38; MOBIO-2006-39; MOBIO-2006-4; MOBIO-2006-40; MOBIO-2006-41; MOBIO-2006-42; MOBIO-2006-43; MOBIO-2006-45; MOBIO-2006-47; MOBIO-2006-48; MOBIO-2006-49; MOBIO-2006-5; MOBIO-2006-50; MOBIO-2006-6; MOBIO-2006-7; MOBIO-2006-8; MOBIO-2008-10; MOBIO-2008-11; MOBIO-2008-12; MOBIO-2008-13; MOBIO-2008-14; MOBIO-2008-15; MOBIO-2008-16; MOBIO-2008-17; MOBIO-2008-18; MOBIO-2008-2; MOBIO-2008-20; MOBIO-2008-21; MOBIO-2008-22; MOBIO-2008-23; MOBIO-2008-25; MOBIO-2008-26; MOBIO-2008-27; MOBIO-2008-28; MOBIO-2008-29; MOBIO-2008-3; MOBIO-2008-30; MOBIO-2008-31; MOBIO-2008-32; MOBIO-2008-33; MOBIO-2008-34; MOBIO-2008-35; MOBIO-2008-36; MOBIO-2008-38; MOBIO-2008-39; MOBIO-2008-4; MOBIO-2008-40; MOBIO-2008-41; MOBIO-2008-42; MOBIO-2008-43; MOBIO-2008-44; MOBIO-2008-45; MOBIO-2008-46; MOBIO-2008-47; MOBIO-2008-48; MOBIO-2008-5; MOBIO-2008-52; MOBIO-2008-53; MOBIO-2008-54; MOBIO-2008-55; MOBIO-2008-56; MOBIO-2008-57; MOBIO-2008-58; MOBIO-2008-6; MOBIO-2008-62; MOBIO-2008-63; MOBIO-2008-64; MOBIO-2008-65; MOBIO-2008-66; MOBIO-2008-67; MOBIO-2008-7; MOBIO-2008-73; MOBIO-2008-74; MOBIO-2008-75; MOBIO-2008-76; MOBIO-2008-77; MOBIO-2008-78; MOBIO-2008-79; MOBIO-2008-8; MOBIO-2008-80; MOBIO-2008-81; MOBIO-2008-82; MOBIO-2008-83; MOBIO-2008-84; MOBIO-2008-85; MOBIO-2008-86; MOBIO-2008-9; MOBIO-2009-10; MOBIO-2009-11; MOBIO-2009-13; MOBIO-2009-15; MOBIO-2009-16; MOBIO-2009-17; MOBIO-2009-18; MOBIO-2009-19; MOBIO-2009-2; MOBIO-2009-20; MOBIO-2009-22; MOBIO-2009-23; MOBIO-2009-24; MOBIO-2009-25; MOBIO-2009-26; MOBIO-2009-27; MOBIO-2009-28; MOBIO-2009-30; MOBIO-2009-32; MOBIO-2009-33; MOBIO-2009-34; MOBIO-2009-35; MOBIO-2009-37; MOBIO-2009-38; MOBIO-2009-39; MOBIO-2009-4; MOBIO-2009-41; MOBIO-2009-42; MOBIO-2009-6; MOBIO-2009-8; MOBIO-2009-9; Nitrate; Nitrite; nitrogen cycle; nitrous oxide; Nitrous oxide, dissolved; nutrients; oceanography; Oxygen, dissolved; Phosphate; Salinity; Silicate; Station label; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 9902 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...