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  • 2005-2009  (865,676)
  • 2009  (416,303)
  • 2007  (449,398)
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  • 1
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    Unknown
    PANGAEA
    In:  European Pollen Database (EPD)
    Publication Date: 2024-07-05
    Keywords: Abies; Alnus; ARAL86; Artemisia; Betula; Brassica; Bryales; Cannabaceae; Carpinus; Caryophyllaceae; Chenopodiaceae; Compositae; Core86; Corylus; Cyperaceae; DEPTH, sediment/rock; Ephedra; Euphorbia; Euphorbiaceae; Fagus; Gramineae; Iridaceae; Juglans; Labiatae; Lake Aral, Kazakhstan; Leguminosae; Lycopodiaceae; Lycopodium; Malva; Malvaceae; Myriophyllum; Ostrya; Picea; Pinus; Plantaginaceae; Polygonaceae; Polypodiaceae; Potamogeton; Quercus; Ranunculaceae; Rubiaceae; Salix; Sparganium; Sphagnum; Tilia; Typha; Ulmus; Umbelliferae; Unknown pollen and spores; Zygophyllaceae
    Type: Dataset
    Format: text/tab-separated-values, 1518 data points
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  • 2
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    Unknown
    PANGAEA
    In:  European Pollen Database (EPD)
    Publication Date: 2024-07-05
    Keywords: Alnus undifferentiated; Alnus viridis subsp. fruticosa; Artemisia; Asteroideae; Betula exilis; Betula fruticosae; Betula platyphylla; Botrychium; Bryales; Caryophyllaceae; CHERNYAR; Cherny Yar, Russia; Cyperaceae; DEPTH, sediment/rock; Diphasium alpinum; Equisetum; Ericales; Euphorbia; Gramineae; Huperzia selago; Labiatae; Larix; Leguminosae; Lycopodium clavatum; Lycopodium undifferentiated; Menyanthes trifoliata; Myriophyllum; Pinus pumila; Polypodiaceae; Ranunculaceae; Rosaceae; Salix; Sphagnum; Thalictrum; Umbelliferae
    Type: Dataset
    Format: text/tab-separated-values, 480 data points
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  • 3
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    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-07-02
    Keywords: ARK-XIV/1a; AWI_Paleo; CT; DATE/TIME; LATITUDE; LONGITUDE; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; ParaSound (Atlas Hydrographic); Polarstern; PS51; PS51/1a-track; Underway cruise track measurements; Uniform resource locator/link to raw data file
    Type: Dataset
    Format: text/tab-separated-values, 3373 data points
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  • 4
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    Unknown
    PANGAEA
    In:  Institute for Chemistry and Biology of the Marine Environment, Carl von Ossietzky Universität Oldenburg, Germany
    Publication Date: 2024-07-02
    Keywords: Alkalinity, total; Aluminium oxide; Antimony; Barium; Biogeochemistry of Tidal Flats; Bismuth; BrumsackHJ_SENK_020213_TP3; Cadmium; Calcium oxide; Carbon, inorganic, total; Carbon, organic, dissolved; Carbon, organic, particulate; Carbon, total; Chromium; Cobalt; Copper; DATE/TIME; DEPTH, water; ICP-MS, see further details; ICP-OES, see further details; Iron oxide, Fe2O3; LATITUDE; Lead; LONGITUDE; Magnesium oxide; Manganese; Molybdenum; Nickel; Otzumer Balje Tidal Inlet, Spiekeroog Backbarrier Tidal Flat, German Bight; Phosphorus pentoxide; Potassium oxide; Rubidium; see further details; SPM_GF, see further details; SPM_PC, see further details; Strontium; Suspended matter, particulate/solids; Thallium; Titanium dioxide; Uranium; Vanadium; Water sample; WATT; WS; Yttrium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 856 data points
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  • 5
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    Unknown
    PANGAEA
    In:  Institute for Chemistry and Biology of the Marine Environment, Carl von Ossietzky Universität Oldenburg, Germany
    Publication Date: 2024-07-02
    Keywords: Alkalinity, total; Aluminium oxide; Antimony; Barium; Biogeochemistry of Tidal Flats; Bismuth; BrumsackHJ_SENK_020213_TP3; BrumsackHJ_SENK_020527_TP3; BrumsackHJ_SENK_020820_TP3; BrumsackHJ_SENK_021118_TP3; BrumsackHJ_SENK_030210_TP3; BrumsackHJ_SENK_030211_TP3; BrumsackHJ_SENK_030422_TP3; BrumsackHJ_SENK_030424_TP3; BrumsackHJ_SENK_030722_TP3; BrumsackHJ_SENK_030811_TP3; BrumsackHJ_SENK_030812_TP3; BrumsackHJ_SENK_031110_TP3; BrumsackHJ_SENK_031112_TP3; Cadmium; Calcium oxide; Carbon, inorganic, total; Carbon, organic, dissolved; Carbon, organic, particulate; Carbon, total; Central Backbarrier Area, Spiekeroog Backbarrier Tidal Flat, German Bight; Cerium; Chromium; Cobalt; Copper; DATE/TIME; DEPTH, water; Event label; Iron oxide, Fe2O3; Lanthanum; LATITUDE; Lead; LONGITUDE; Magnesium oxide; Manganese; Molybdenum; Nickel; Otzmer Balje Tidal Inlet, Spiekeroog Backbarrier Tidal Flat, German Bight; Otzumer Balje Tidal Inlet, Spiekeroog Backbarrier Tidal Flat, German Bight; Phosphorus pentoxide; Potassium oxide; Rubidium; see further details; Strontium; Suspended matter, particulate/solids; Thallium; Titanium dioxide; Uranium; Vanadium; Water sample; WATT; WS; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 13814 data points
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  • 6
    Publication Date: 2024-07-02
    Keywords: 86-577A; AGE; Deep Sea Drilling Project; Depth, relative; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Inductively coupled plasma - mass spectrometry (ICP-MS); Iridium; Leg86; North Pacific; Osmium; Osmium/Iridium ratio; Osmium-187/Osmium-188, error; Osmium-187/Osmium-188 ratio; Platinum; Platinum/Iridium ratio; Reference/source; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 318 data points
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  • 7
    Monograph available for loan
    Monograph available for loan
    [Dordrecht [u.a.]] : Springer
    Call number: M 24.95741
    Type of Medium: Monograph available for loan
    Pages: XVIII, 831 Seiten , Illustrationen, Karten , 193 x 260 mm
    Edition: Second edition 2. rev. and enl. ed. of the 1. ed. publ. by Chapman and Hall, 1994
    ISBN: 9789402404470 , 9402404473
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 8
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    Unknown
    PANGAEA
    In:  Supplement to: Dorschel, Boris; Hebbeln, Dierk; Rüggeberg, Andres; Dullo, Wolf-Christian (2007): Carbonate budget of a cold-water coral carbonate mound: Propeller Mound, Porcupine Seabight. International Journal of Earth Sciences, 96(1), 73-83, https://doi.org/10.1007/s00531-005-0493-0
    Publication Date: 2024-07-01
    Description: High resolution studies from the Propeller Mound, a cold-water coral carbonate mound in the NE Atlantic, show that this mound consists of 〉50% carbonate justifying the name "carbonate mound". Through the last ~300,000 years approximately one third of the carbonate has been contributed by cold-water corals, namely Lophelia pertusa and Madrepora oculata. This coral bound contribution to the carbonate budget of Propeller Mound is probably accompanied by an unknown portion of sediments buffered from suspension by the corals. However, extended hiatuses in Propeller Mound sequences only allow the calculation of a net carbonate accumulation. Thus, net carbonate accumulation for the last 175 kyr accounts for only 〈0.3 g/cm2/kyr, which is even less than for the off-mound sediments. These data imply that Propeller Mound faces burial by hemipelagic sediments as has happened to numerous buried carbonate mounds found slightly to the north of the investigated area.
    Keywords: Center for Marine Environmental Sciences; ECOMOUND; Environmental controls on mound formation along the european margin; GeoB6718-2; GeoB6719-1; GeoB6725-1; GeoB6728-1; GeoB6729-1; GeoB6730-1; Gravity corer (Kiel type); MARUM; Porcupine Seabight; POS265; POS478-2; POS479-1; POS485-1; POS488-1; POS489-1; POS490-1; Poseidon; SL
    Type: Dataset
    Format: application/zip, 16 datasets
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  • 9
    Publication Date: 2024-07-01
    Description: Phase equilibria simulations were performed on naturally quenched basaltic glasses to determine crystallization conditions prior to eruption of magmas at the Mid-Atlantic Ridge (MAR) east of Ascension Island (7°11°S).The results indicate that midocean ridge basalt (MORB) magmas beneath different segments of the MAR have crystallized over a wide range of pressures (100-900MPa). However, each segment seems to have a specific crystallization history. Nearly isobaric crystallization conditions (100-300MPa) were obtained for the geochemically enriched MORB magmas of the central segments, whereas normal (N)-MORB magmas of the bounding segments are characterized by polybaric crystallization conditions (200-900MPa). In addition, our results demonstrate close to anhydrous crystallization conditions of N-MORBs, whereas geochemically enriched MORBs were successfully modeled in the presence of 0.4-1wt% H2O in the parental melts.These estimates are in agreement with direct (Fourier transform IR) measurements of H2O abundances in basaltic glasses and melt inclusions for selected samples. Water contents determined in the parental melts are in the range 0.04-0.09 and 0.30-0.55 wt% H2O for depleted and enriched MORBs, respectively. Our results are in general agreement (within ±200MPa) with previous approaches used to evaluate pressure estimates in MORB. However, the determination of pre-eruptive conditions of MORBs, including temperature and water content in addition to pressure, requires the improvement of magma crystallization models to simulate liquid lines of descent in the presence of small amounts of water. KEY WORDS: MORB; Mid-Atlantic Ridge; depth of crystallization; water abundances; phase equilibria calculations; cotectic crystallization; pressure estimates; polybaric fractionation
    Keywords: DERIDGE; Dredge; DRG; From Mantle to Ocean: Energy-, Material- and Life-cycles at Spreading Axes; M41/2; M41/2_132; M41/2_133; M41/2_136; M41/2_137; M41/2_138; M41/2_139; M41/2_140; M41/2_141; M41/2_142; M41/2_143; M41/2_144; M41/2_145; M41/2_146; M41/2_147; M41/2_148; M41/2_149; M41/2_151; M41/2_152; M41/2_153; M41/2_154; M41/2_155; M41/2_156; M41/2_157; M41/2_158; M41/2_159; M41/2_160; M41/2_161; M41/2_162; M41/2_163; M41/2_164; M41/2_166; M41/2_167; M41/2_169; M41/2_170; M41/2_171; M41/2_172; M41/2_173; M41/2_174; M41/2_188; M41/2_189; M41/2_190; M41/2_191; M41/2_194; M41/2_195; M41/2_196; M41/2_197; M41/2_198; M41/2_199; M41/2_200; M41/2_201; M41/2_202; M41/2_203; Meteor (1986); Mid-Atlantic Ridge at 4-11°S
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 10
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    Unknown
    PANGAEA
    In:  Supplement to: Feseker, Tomas; Pape, Thomas; Wallmann, Klaus; Klapp, Stephan A; Schmidt-Schierhorn, Friederike; Bohrmann, Gerhard (2009): The thermal structure of the Dvurechenskii mud volcano and its implications for gas hydrate stability and eruption dynamics. Marine and Petroleum Geology, 26(9), 1812-1823, https://doi.org/10.1016/j.marpetgeo.2009.01.021
    Publication Date: 2024-07-01
    Description: The sediment temperature distribution at mud volcanoes provides insights into their activity and into the occurrence of gas hydrates. If ambient pressure and temperature conditions are close to the limits of the gas hydrate stability field, the sediment temperature distribution not only limits the occurrence of gas hydrates, but is itself influenced by heat production and consumption related to the formation and dissociation of gas hydrates. Located in the Sorokin Trough in the northern Black Sea, the Dvurechenskii mud volcano (DMV) was in the focus of detailed investigations during the M72/2 and M73/3a cruises of the German R/V Meteor and the ROV Quest 4000 m in February and March 2007. A large number of in-situ sediment temperature measurements were conducted from the ROV and with a sensor-equipped gravity corer. Gas hydrates were sampled in pressurized cores using a dynamic autoclave piston corer (DAPC). The thermal structure of the DMV suggests a regime of fluid flow at rates decreasing from the summit towards the edges of the mud volcano, accompanied by intermittent mud expulsion at the summit. Modeled gas hydrate dissociation temperatures reveal that the gas hydrates at the DMV are very close to the stability limits. Changes in heat flow due to variable seepage rates probably do not result in changes in sediment temperature but are compensated by gas hydrate dissociation and formation.
    Keywords: 1; 10; 11; 12; 13; 14; 15; 16; 17; 18; 19; 2; 20; 3; 4; 5; 6; 7; 8; 9; Center for Marine Environmental Sciences; DAPC; DAPC-5; DAPC-6; DAPC-7; Dvurechenskii; Dvurechenskii mud volcano; Dynamic autoclave piston corer; GC_T; GeoB11911; GeoB11914; GeoB11916; Gravity Corer/temperature probe; M72/2; M72/2_273; M72/2_274; M72/2_275; M72/2_276; M72/2_277; M72/2_297; M72/2_298; M72/2_299; M72/2_300; M72/2_302; M72/2_303; M72/2_304; M72/2_305; M72/2_306; M72/2_307; M72/2_310; M72/2_311; M72/2_313; M72/2_314; M72/2_316; M72/3a; MARUM; Meteor (1986)
    Type: Dataset
    Format: application/zip, 3 datasets
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