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  • 2010-2014  (3,084,844)
  • 1970-1974  (755,911)
  • 1940-1944  (110,020)
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Year
  • 1
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    Unknown
    (Supplementary Table S1) Tephra ages and sea surface reservoir 14C ages estimates in core MD07-3088 (2013)
    PANGAEA
    Details
    Publication Date: 2024-06-06
    Keywords: Age, 14C conventional; Age, dated; Age, dated material; Age, dated standard deviation; Calendar age; CALYPSO2; Calypso Corer II; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Eruption; IMAGES XV - Pachiderme; Marion Dufresne (1995); MD07-3088; MD159; Origin; Reference/source; Reservoir effect/correction; Reservoir effect/correction, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 139 data points
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  • 2
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    Bathymetry of Sleipner region during ALKOR cruise AL374 (phi, lambda, depth) (2012)
    PANGAEA
    In:  IFM-GEOMAR Leibniz-Institute of Marine Sciences, Kiel University
    Details
    Publication Date: 2024-06-06
    Keywords: AL374; AL374-track; Alkor (1990); CT; Depth, bathymetric; ECO2; LATITUDE; LONGITUDE; Sleipner; Sub-seabed CO2 Storage: Impact on Marine Ecosystems; Swath-mapping system SeaBeam 1000 (L-3 ELAC Nautik); Underway cruise track measurements; UTM Easting, Universal Transverse Mercator; UTM Northing, Universal Transverse Mercator; UTM Zone, Universal Transverse Mercator
    Type: Dataset
    Format: text/tab-separated-values, 1039540 data points
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  • 3
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    Profiles of sediment echo sounding of Sleipner region during ALKOR cruise AL374 with links to SGY data files (2012)
    PANGAEA
    In:  IFM-GEOMAR Leibniz-Institute of Marine Sciences, Kiel University
    Details
    Publication Date: 2024-06-06
    Keywords: AL374; AL374_510-1; AL374_519-1; AL374_523-1; AL374_539-1; Alkor (1990); ECO2; Event label; File size; MULT; Multiple investigations; Sample code/label; Sleipner; Sub-bottom profiler, SES-2000, Innomar; Sub-seabed CO2 Storage: Impact on Marine Ecosystems; Uniform resource locator/link to metadata file; Uniform resource locator/link to sgy data file
    Type: Dataset
    Format: text/tab-separated-values, 250 data points
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  • 4
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    Mid-Pleistocene (800-400 ka) planktic foraminfer assemblages of IODP Site 306-U1314 (2011)
    PANGAEA
    Details
    Publication Date: 2024-06-06
    Keywords: 306-U1314; Accumulation rate, planktic foraminifera by number; AGE; COMPCORE; Composite Core; Counting 〉150 µm fraction; DEPTH, sediment/rock; Exp306; Foraminifera, planktic; Foraminifera, planktic, subtropical; Globigerina bulloides; Globigerinita glutinata; Globorotalia inflata; Globorotalia scitula; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Neogloboquadrina pachyderma dextral; Neogloboquadrina pachyderma sinistral; North Atlantic; North Atlantic Climate 2; Turborotalita quinqueloba
    Type: Dataset
    Format: text/tab-separated-values, 3450 data points
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  • 5
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    (Table 1) Age determination of sediment core SONK_11_D (2014)
    PANGAEA
    Details
    Publication Date: 2024-06-06
    Keywords: Age, 14C AMS; Age, 14C calibrated; Age, 14C milieu/reservoir corrected; Age, dated; Age, dated material; Age, dated standard deviation; Age, maximum/old; Age, minimum/young; Core; CORE; DEPTH, sediment/rock; GeoForschungszentrum Potsdam; GFZ; Kyrgyzstan; Laboratory code/label; Lake_Son-Kol; SONK_11_D
    Type: Dataset
    Format: text/tab-separated-values, 222 data points
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  • 6
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    Age versus depth correlation of sediment core POS200/10_28-1 (2014)
    PANGAEA
    Details
    Publication Date: 2024-06-06
    Keywords: Age model; DEPTH, sediment/rock; Gravity corer (Kiel type); PO200-10-28-1; POS200/10; POS200/10_28-1; Poseidon; SL
    Type: Dataset
    Format: text/tab-separated-values, 7 data points
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  • 7
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    Summer sea surface temperature and export production sediment core POS200/10_28-1 (2014)
    PANGAEA
    Details
    Publication Date: 2024-06-06
    Keywords: AGE; DEPTH, sediment/rock; Export production; Globigerina bulloides, δ18O; Gravity corer (Kiel type); Modern analog technique (MAT), SIMMAX28, non-distance-weighted; Neogloboquadrina pachyderma sinistral; PO200-10-28-1; POS200/10; POS200/10_28-1; Poseidon; Sea surface temperature, summer; SL
    Type: Dataset
    Format: text/tab-separated-values, 108 data points
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  • 8
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    Planktonic foraminifera of IODP Site 306-U1314 (2011)
    PANGAEA
    In:  Supplement to: Alonso-Garcia, Montserrat; Sierro, Francisco Javier; Flores, José-Abel (2011): Arctic front shifts in the subpolar North Atlantic during the Mid-Pleistocene (800–400 ka) and their implications for ocean circulation. Palaeogeography, Palaeoclimatology, Palaeoecology, 311(3-4), 268-280, https://doi.org/10.1016/j.palaeo.2011.09.004
    Details
    Publication Date: 2024-06-06
    Description: Surface water conditions at the Integrated Ocean Drilling Program (IODP) Site U1314 (Southern Gardar Drift, 56° 21.8' N, 27° 53.3' W, 2820 m depth) were inferred using planktic foraminifer assemblages between Marine Isotope Stage (MIS) 19 and 11 (ca. 800-400 ka). Factor analysis of the planktic foraminifer assemblages suggests that the assemblage was controlled by three factors. The first factor (which explained 49% of the variance) is dominated by transitional and subpolar species and points to warm and salty surface water conditions (Atlantic water). The second factor (37%) is dominated by Neogloboquadrina pachyderma sin and has been associated with the presence of cold and low saline surface waters (Arctic water). Finally, the third factor (9%), linked to a significant presence of Turborotalita quinqueloba, reflects the closeness of the Arctic front (the boundary between Atlantic and Arctic water). The position of the Arctic and Polar fronts has been estimated across the glacial-interglacial cycles studied according to planktic foraminifer abundances from Site U1314 (and their factor analysis) combined with a synthesis of planktic foraminifer and diatom data from other North Atlantic sites. Regarding at the migrations of the Arctic front and the surface water masses distribution across each climatic cycle we determined five phases of development. Furthermore, deep ocean circulation changes observed in glacial-interglacial cycles have been associated with each phase. The high abundance of transitional-subpolar foraminifers (above 65% at Site U1314) during the early interglacial phase indicated that the Arctic front position and surface water masses distribution were similar to present conditions. During the late interglacial phase, N. pachyderma sin and T. quinqueloba slightly increased indicating that winter sea ice slightly expanded southwestwards whereas the ice volume remained stable or was still decreasing. N. pachyderma sin increased rapidly (above 65% at Site U1314) at the first phase of glacial periods indicating the expansion of the Arctic waters in the western subpolar North Atlantic. During the second phase of glacial periods the transitional-subpolar assemblage throve again in the central subpolar North Atlantic associated with strong warming events that followed ice-rafting events. The third phase of glacial periods corresponds to full glacial conditions in which N. pachyderma sin dominated the assemblage for the whole subpolar North Atlantic. This division in phases may be applied to the last four climatic cycles.
    Keywords: 306-U1314; COMPCORE; Composite Core; Exp306; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; North Atlantic; North Atlantic Climate 2
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 9
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    Estimation of seismic velocities of upper oceanic crust from ocean bottom reflection loss data (2010)
    AIP Publishing
    Details
    Publication Date: 2024-06-06
    Description: This paper describes a Bayesian inversion of acoustic reflection loss versus angle measurements to estimate the compressional and shear wave velocities in young uppermost oceanic crust, Layer 2A. The data were obtained in an experiment on the thinly sedimented western flank of the Endeavor segment of the Juan de Fuca Ridge, using a towed horizontal hydrophone array and small explosive charges as sound sources. Measurements were made at three sites at increasing distance from the ridge spreading center to determine the effect of age of the crust on seismic velocities. The inversion used reflection loss data in a 1/3-octave band centered at 16 Hz. The compressional and shear wave velocities of the basalt were highly sensitive parameters in the inversion. The compressional wave velocity increased from 2547±30 to 2710±18 m/s over an age span of 1.4 million years (Ma) from the spreading center, an increase of 4.5±1.0%/Ma. The basalt shear wave velocity increased by nearly a factor of 2, from ∼725 to 1320 m/s over the same age span. These results show a decreasing trend of Poisson’s ratio with age, from a value of 0.46 at the youngest site closest to the ridge axis.
    Type: Article , PeerReviewed
    Format: text
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    PAPER (OCEANREP)
  • 10
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    Strontium isotope ratios of plant and soil samples from France (2013)
    PANGAEA
    In:  Research School of Earth Sciences, The Australian National University, Canberra | Supplement to: Willmes, Malte; McMorrow, Linda; Kinsley, Les; Armstrong, R; Aubert, Maxime; Eggins, Stephen M; Falguères, Christophe; Maureille, Bruno; Moffat, Ian; Grün, R (2014): The IRHUM (Isotopic Reconstruction of Human Migration) database - bioavailable strontium isotope ratios for geochemical fingerprinting in France. Earth System Science Data, 6(1), 117-122, https://doi.org/10.5194/essd-6-117-2014
    Details
    Publication Date: 2024-06-04
    Description: The dataset consists of 87Sr/86Sr isotope ratios of plant samples and soil leachates covering the major geologic regions of France. In addition to the isotope data it provides the spatial context for each sample, including background geology, field observations and soil descriptions. The dataset can be used to create Sr isoscapes for France, which can be applied in a wide range of fields including archaeology, ecology, soil, food, and forensic sciences.
    Keywords: Age, comment; Age, maximum/old; Age, minimum/young; Area/locality; Comment; ELEVATION; Environment; Event label; F06(F)-001; F06(F)-002; F06(F)-004; F06(F)-006; F06(F)-008; F06(F)-012; F06(F)-016; F06(F)-018; F06(F)-021; F06(F)-023; F06(F)-024; F06(F)-025; F06(F)-027; F06(F)-033; F06(F)-034; F06(F)-035; F06(F)-037; F06(F)-038; F06(F)-040; F06-002; F06-003; F06-005; F06-007; F06-008; F06-009; F06-010; F06-011; F06-012; F06-014; F06-015; F06-016; F06-017; F06-019; F06-020; F06-023; F06-024; F06-026; F06-027; F06-029; F06-030; F06-031; F06-032; F06-033; F06-036; F06-037; F06-038; F06-040; F06-042; F06-043; F06-044; F06-045; F06-046; F06-047; F06-050; F06-051; F06-054; F06-055; F06-056; F06-057; F06-058; F06-059; F06-061; F06-062; F09-001; F09-002; F09-003; F09-004; F09-005; F09-006; F09-007; F09-008; F09-009; F09-010; F09-011; F09-012; F09-013; F09-014; F09-015; F09-016; F09-017; F09-018; F09-019; F09-020; F09-021; F09-022; F09-023; F09-024; F09-025; F09-026; F09-027; F09-028; F09-029; F09-030; F09-031; F09-032; F09-033; F09-034; F09-035; F09-036; F09-037; F09-038; F09-039; F09-040; F09-041; F09-042; F09-043; F09-044; F09-045; F09-046; F09-047; F09-048; F09-049; F09-050; F09-051; F09-052; F09-053; F09-054; F09-055; F09-056; F09-057; F09-058; F09-060; F09-061; F09-062; F09-063; F09-064; F09-065; F09-066; F09-067; F09-068; F09-069; F09-070; F09-071; F09-072; F09-073; F09-074; F09-075; F09-076; F09-077; F09-078; F09-079; F09-080; F09-081; F09-082; F09-083; F09-084; F09-085; F09-086; F09-087; F09-088; F09-089; F09-090; F09-091; F09-092; F09-093; F09-094; F09-095; F09-096; F09-097; F09-098; F09-099; F09-100; F09-101; F09-102; F09-103; F09-104; F09-105; F09-106; F09-107; F09-108; F09-109; F09-110; F09-111; F09-112; F09-113; F09-114; F09-115; F09-116; F09-117; F09-118; F11-001; F11-002; F11-003; F11-004; F11-005; F11-006; F11-007; F11-008; F11-009; F11-010; F11-011; F11-012; F11-013; F11-014; F11-015; F11-016; F11-017; F11-018; F11-019; F11-020; F11-021; F11-022; F11-023; F11-024; F11-025; F11-026; F11-027; F11-028; F11-029; F11-030; F11-031; F11-032; F11-033; F11-034; F11-035; F11-036; F11-037; F11-038; F11-039; F11-040; F11-041; F11-042; F11-043; F11-044; F11-045; F11-046; F11-047; F11-048; F11-049; F11-050; F11-051; F11-052; F11-053; F11-054; F11-055; F11-056; F11-057; F11-058; F11-059; F11-060; F11-061; F11-062; F11-063; F11-064; F11-065; F11-066; F11-067; F11-068; F11-069; F11-070; F11-071; F11-072; F11-073; F11-074; F11-075; F11-076; F11-077; F11-078; F11-079; F11-080; F11-081; F11-082; F11-083; F11-084; F11-085; F11-086; F11-087; F11-088; F11-089; F11-090; F11-091; F11-092; F11-093; F11-094; F11-095; F11-096; F11-097; F11-099; F11-100; F11-101; F11-102; F11-103; F11-104; F11-105; F11-106; F11-107; F11-108; F11-109; F11-110; F11-111; F11-112; F11-113; F11-114; F11-115; F11-116; F11-117; F11-118; F11-119; F11-120; F11-121; F11-122; F11-123; F11-124; F11-125; F11-126; F11-127; F11-128; F11-129; F11-130; F11-131; F11-132; F11-133; F11-134; F11-135; F11-136; F11-137; F11-138; F11-139; F11-140; F11-141; F11-142; F11-143; F11-144; F11-145; F11-146; F11-147; F11-148; F11-149; F11-150; F11-151; F11-152; F11-153; F11-154; F11-155; F11-156; F11-157; F11-158; F11-159; F11-160; F11-161; F11-162; F11-163; F11-164; F11-165; F11-166; F11-167; F11-168; F11-169; F11-170; F11-171; F11-172; F11-173; F11-174; F11-175; F11-176; F11-178; F11-179; F11-180; F11-181; F11-182; F11-183; F11-184; F11-185; F11-186; F11-187; F11-188; F11-189; F11-190; F11-191; F11-192; F11-193; F11-194; F11-195; F11-196; F11-197; F11-198; F12-001; F12-002; F12-003; F12-004; F12-005; F12-006; F12-007; F12-008; F12-009; F12-010; F12-011; F12-012; F12-013; F12-014; F12-015; F12-016; F12-017; F12-018; F12-019; F12-020; F12-021; F12-022; F12-023; F12-024; F12-025; F12-026; F12-027; F12-028; F12-029; F12-030; F12-031; F12-032; F12-033; F12-034; F12-035; F12-036; F12-037; F12-038; F12-039; F12-040; F12-041; F12-042; F12-044; F12-045; F12-046; F12-047; F12-048; F12-049; F12-050; F12-051; F12-052; F12-053; F12-054; F12-055; F12-056; F12-057; F12-058; F12-060; F12-061; F12-062; F12-063; F12-064; F12-065; F12-066; F12-067; F12-068; F12-069; F12-070; F12-071; F12-072; F12-073; F12-074; F12-075; F12-076; F12-077; F12-078; F12-079; F12-080; F12-081; F12-082; F12-083; F12-084; F12-085; F12-086; F12-087; F12-088; F12-089; F12-090; F12-091; F12-092; F12-093; F12-094; F12-095; F12-096; F12-097; F12-098; F12-099; F12-100; F12-101; F12-102; F12-103; F12-104; F12-105; F12-106; F12-107; F12-108; F12-109; F12-110; F12-111; F12-112; F12-113; F12-114; F12-115; F12-116; F12-117; F12-118; F12-119; F12-120; F12-121; F12-122; F12-123; F12-124; F12-125; F12-126; F12-127; F12-128; F12-129; F12-130; F12-131; F12-132; F12-133; F12-134; F12-135; F12-136; F12-137; F12-138; F12-139; F12-140; F12-141; F12-142; F12-143; F12-144; F12-145; F12-146; F12-147; F12-148; F12-149; F12-150; F12-151; F12-153; F12-154; F12-155; F12-156; F12-157; F12-158; F12-159; F12-160; F12-161; F12-162; F12-163; F12-164; F12-165; F12-166; F12-167; F12-168; F12-169; F12-170; F12-171; F12-172; F12-173; F12-174; F12-175; F12-176; F12-177; F12-178; F12-179; F12-180; F12-181; F12-182; F12-183; F12-184; F12-185; F12-186; F12-187; F12-188; F12-189; F12-190; F12-191; F12-192; F12-193; F12-194; F12-195; F12-196; F12-197; F12-198; F12-199; F12-200; F12-201; F12-202; F12-203; F12-204; F12-205; F12-206; F12-207; F12-208; F12-209; F12-210; F12-211; F12-212; F12-213; F12-214; F12-215; F12-216; F12-217; F12-218; F12-219; F12-220; F12-221; F12-222; F12-223; F12-224; F12-225; F12-226; F12-227; F12-228; F12-229; F12-230; F12-231; F12-232; F12-233; F12-234; F12-235; F12-236; F12-237; F12-238; F13-001; F13-002; F13-003; F13-004; F13-005; F13-006; F13-007; F13-008; F13-009; F13-010; F13-011; F13-012; F13-013; F13-014; F13-015; F13-016; F13-017; F13-018; F13-019; F13-020; F13-021; F13-022; F13-023; F13-024; F13-025; F13-026; F13-027; F13-028; F13-029; F13-030; F13-031; F13-032; F13-033; F13-034; F13-035; F13-036; F13-037; F13-038; F13-039; F13-040; F13-042; F13-043; F13-044; F13-045; F13-046; F13-047; F13-048; F13-049; F13-051; F13-052; F13-053; F13-054; F13-055; F13-056; F13-057; F13-058; F13-059; F13-060; F13-061; F13-062; F13-063; F13-064; F13-065; F13-066; F13-067; F13-068; F13-069; F13-070; F13-071; F13-072; F13-073; F13-074; F13-075; F13-076; F13-077; F13-078; F13-079; F13-080; F13-081; F13-082; F13-084; F13-085; F13-086; F13-087; F13-088; F13-089; F13-090; F13-092; F13-093; F13-094; F13-095; F13-096; F13-097; F13-098; F13-099; F13-100; F13-101; F13-102; F13-103; F13-104; F13-105; F13-106; F13-107; F13-108; F13-109; F13-110; F13-111; F13-112; F13-113; F13-114; F13-115; F13-116; F13-117; F13-118; F13-119; F13-120; F13-121; F13-122; F13-123; F13-124; F13-125; F13-126; F13-127; F13-129; F13-130; F13-131; F13-132; F13-133; F13-134; F13-135; F13-136; F13-137; F13-138; F13-139; F13-140; F13-141; F13-142; F13-143; F13-144; F13-145; F13-146; F13-147; F13-148; F13-149; F13-150; F13-151; F13-152; F13-153; F13-154; F13-155; F13-156; F13-157; F13-158; F13-159; F13-160; F13-161; F13-162; F13-163; F13-164; F13-165; F13-166; F13-167; F13-168; F13-169; F13-170; F13-171; F13-172; F13-173; F13-174; F13-175; F13-176; F13-177; F13-178; F13-179; F13-180; F13-181; F13-182; F13-183; F13-184; F13-185; F13-186; F13-187; F13-188; F13-189; F13-190; F13-191; F13-192; F13-193; F13-194; F13-195; F13-196; F13-197; F13-198; F13-199; F13-200; F13-201; F13-202; F13-203; F13-204; F13-205; F13-206; F13-207; F13-208; F13-209; F13-210; F13-211; F13-212; F13-213; F13-214; F13-215; F13-216; F13-217; F13-218; F13-219; F13-220; F13-221; F13-222; F13-223; F13-224; F13-225; F13-226; F13-227; F13-228; France; HAND; Latitude of event; Lithologic unit/sequence; Longitude of event; Name; Observation; Outcrop ID; Rock type; Sample comment; Sample type; Sampling by hand; Strontium-87/Strontium-86 ratio; Strontium-87/Strontium-86 ratio, error
    Type: Dataset
    Format: text/tab-separated-values, 15675 data points
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