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  • 2020-2024  (36,732)
  • 1995-1999  (14)
  • 2023  (36,732)
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  • 1
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    The ocean-continent transition in the Western Central Red Sea (2023)
    Elsevier
    Details
    Publication Date: 2024-06-28
    Description: The Red Sea is an important example of a continental rift transitioning slowly to an oceanic basin. However, structures that can inform us of how that transition occurred have been poorly reported because deep seismic reflection data capable of imaging basement under the rift sediments are generally lacking publicly. Three lines of multichannel seismic reflection data have recently been published revealing structures on the Nubian side of the central part of the basin. In this study, we reassess these data in the light of recent studies of the central Red Sea. Over continental crust, the data reveal reflection sequences likely due to strata at or near the base of the evaporites, in two cases with varied dips suggesting the presence of syn-rift growth stratigraphy. Almost all of those reflections dip downwards towards the rift axis, not away as would be expected from tilted fault blocks of bookshelf faulting types. That observation, and low relief of basement, confirm inferences made earlier based on gravity anomalies that this part of the Red Sea lacks large-relief fault escarpments and is most likely a syn-rift sag basin. In the transition to oceanic crust, an abnormally broad magnetic anomaly of estimated Chron 5 age is found not to be associated with structures such as sills, so it likely arises from deeper sources. One of the seismic lines traverses a ridge in Bouguer gravity anomalies that runs across the axis. This feature has previously been interpreted as a volcanic ridge similar to those observed at other ultra-slow spreading ridges. The seismic data reveal diffuse basement reflections and confirm that the record immediately above basement lacks reflections typical of sedimentary strata. Both observations are consistent with the presence of oceanic crust. Modelling of gravity anomalies suggests the ridge is likely underlain by igneous intrusive rocks displacing mantle rocks, as expected for a volcanic ridge. The seismic data, combined with recently updated multibeam and high-resolution sparker seismic results, further suggest how the evaporite movements have been modulated by basement topography. These results add to our knowledge of the evaporite movements and continent-ocean transition structures in the central Red Sea.
    Type: Article , PeerReviewed
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  • 2
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    Advances in New Zealand's Tephrochronostratigraphy Using Marine Drill Sites: The Neogene (2023)
    AGU (American Geophysical Union) | Wiley
    Details
    Publication Date: 2024-06-28
    Description: Three volcanic arcs have been the source of New Zealand's volcanic activity since the Neogene: Northland arc, Coromandel Volcanic Zone (CVZ) and Taupō Volcanic Zone (TVZ). The eruption chronology for the Quaternary, sourced by the TVZ, is well studied and established, whereas the volcanic evolution of the precursor arc systems, like the CVZ (central activity c. 18 to 2 Ma), is poorly known due to limited accessibility to, or identification of, onshore volcanic deposits and their sources. Here, we investigate the marine tephra record of the Neogene, mostly sourced by the CVZ, of cores from IODP Exp. 375 (Sites U1520 and U1526), ODP Leg 181 (Sites 1123, 1124 and 1125), IODP Leg 329 (Site U1371) and DSDP Leg 90 (Site 594) offshore of New Zealand. In total, we identify 306 primary tephra layers in the marine sediments. Multi-approach age models (e.g. biostratigraphy, zircon ages) are used in combination with geochemical fingerprinting (major and trace element compositions) and the stratigraphic context of each marine tephra layer to establish 168 tie-lines between marine tephra layers from different holes and sites. Following this approach, we identify 208 explosive volcanic events in the Neogene between c. 17.5 and 2.6 Ma. This is the first comprehensive study of New Zealand's Neogene explosive volcanism established from tephrochronostratigraphic studies, which reveals continuous volcanic activity between c. 12 and 2.6 Ma with an abrupt compositional change at c. 4.5 Ma, potentially associated with the transition from CVZ to TVZ. Key Points New Zealand's Neogene explosive volcanism based on the marine tephra record Geochemical fingerprinting of marine tephra layers across the study area to establish volcanic events Insights into geochemical variations with time, repose times and spatiotemporal distribution
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
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  • 3
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    Variations in Volcanism and Tectonics Along the Hotspot‐Influenced Reykjanes Ridge (2023)
    AGU (American Geophysical Union) | Wiley
    Details
    Publication Date: 2024-06-28
    Description: Mapping and sampling four sections of the slow-spreading Reykjanes Ridge provide insight into how tectonic and volcanic activity varies with distance from the Iceland plume. The studied areas are characterized by significant variations in water depth, lava chemistry, crustal thickness, thermal structure, and ridge morphology. For each study area, fault pattern and dimension, tectonic strain, seamount morphology, and density are inferred from 15 m-resolution bathymetry. These observations are combined with geochemical analysis from glass samples and sediment thickness estimations along Remotely Operated Vehicle-dive videos. They reveal that (a) tectonic and volcanic activity along the Reykjanes Ridge, do not systematically vary with distance from the plume center. (b) The tectonic geometry appears directly related to the deepening of the brittle/ductile transition and the maximum change in tectonic strain related to the rapid change in crustal thickness and the transition between axial-high and axial valley (∼59.5°N). (c) Across-axis variations in the fault density and sediment thickness provide similar widths for the neo-volcanic zone except in regions of increased seamount emplacement. (d) The variations in seamount density (especially strong for flat-topped seamounts) are not related to the distance from the plume but appear to be correlated with the interaction between the V-shape ridges (VSR) flanking the ridge and the ridge axis. These observations are more compatible with the buoyant upwelling melting instability hypothesis for VSR formation and suggest that buoyant melting instabilities create many small magma batches which by-pass the normal subaxial magmatic plumbing system, erupting over a wider-than-normal area. Key Points The distance from the plume center is not the only factor controlling tectonic and volcanic activity along the Reykjanes Ridge Fault dimensions are primarily controlled by the variation of crustal thermal structure with distance from the hotspot Flat-topped seamount abundances peak where a V-shaped ridge intersects the axis, consistent with a buoyant upwelling melting instability
    Type: Article , PeerReviewed
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  • 4
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    Five new species of water mite genus Atractides Koch, 1837 from Bhutan with new records (Acari: Hydrachnidia: Hygrobatidae) (2023)
    Les Amis d'Acarologia
    In:  Acarologia vol. 63 no. 1, pp. 148-168
    Details
    Publication Date: 2024-06-28
    Description: Water mites of the genus Atractides Koch, 1837 are among the most frequently found mites in running waters of the Himalayas. In the present study seven species of this genus are identified from material collected in 2021 from Bhutan. Five species new for science are described, i.e., Atractides mangdensis sp. nov., A. conflatus sp. nov., A. bhutanicus sp. nov., A. indentatus sp. nov., and A. himalayicus sp. nov.
    Keywords: Himalayas ; taxonomy ; new species ; running waters
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 5
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    Omnipresent authigenic carbonates distort Arctic radiocarbon chronology (2023)
    PANGAEA
    Details
    Publication Date: 2024-06-28
    Description: The dataset submitted provides a photo documentation on the preservation status of Neogloboquadrina pachyderma shells in sediments of two Arctic sediment cores (PS72/413-3 and PS2185-6). In the accompanying paper different preservation indices (PI_1-3) were introduced to describe the progressive diagenetic alteration from 1 to 3, and the documentation helps to understand how the shells were assigned to the different categories. The data set also serves as a guide for future shell-based work, showing differences between biologically precipitated shell and authigenic overgrowth. This dataset is the first comprehensive documentation that illustrates diagenitic calcite on N. pachyderma shells and as isolated sedimentary crystals at none-seepage sites in the Arctic. Furthermore, the shells and crystals that were used for radiocarbon dating and isotope analyses as shown in the accompanying paper are illustrated in respective documentary files.
    Keywords: Arctic Ocean; ARK-VIII/3; ARK-XXIII/3; Binary Object; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; File content; Foraminifera; Giant box corer; GKG; KAL; Kasten corer; Lomonosov Ridge, Arctic Ocean; Polarstern; PS19/186; PS19 ARCTIC91; PS2185-6; PS72; PS72/413-3; radiocarbon; age model; Stable carbon and oxygen isotopes
    Type: Dataset
    Format: text/tab-separated-values, 144 data points
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  • 6
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    Compilation of deglacial Southern Ocean planktic foraminiferal d18O data (2023)
    PANGAEA
    Details
    Publication Date: 2024-06-28
    Description: This dataset contains a compilation of planktic foraminiferal d18O from sediment cores spanning the last deglaciation in the Southern Ocean. The compilation includes 4610 data points from 64 individual records. The dataset includes the original reference for the data, the name of the sediment core, the latitude (°N), longitude (°E), and water depth (m) at which the sediment core was taken, the sediment depth at which the d18O analysis was conducted (cm), the age of the sediment at which the d18O analysis was conducted (ka, using the age model given in the original publication), the foraminiferal species on which the d18O analysis was conducted, the measured d18O value (VPDB). The sediment cores in the compilation span 20 – 70°S across the Southern Ocean. The individual d18O records cover the last 30 ka. The d18O data were measured on N. pachyderma (np), G. bulloides (gb), and G. ruber (gr).
    Keywords: 177-1089; 177-1094; 20; 202-1233; 35MF20120125, OISO_21, INDIEN SUD 2; 64PE-174P13; AGE; AGSO Cruise 147; Amundsen Sea, continental rise (unnamed Marie Byrd Seamount); ANTIPROD; ANT-IV/3; ANT-V/4; ANT-VIII/3; APSARA2; APSARA4; Argentine Basin; Atka Bay; AUSCAN; BC; Box corer; Brazil Basin; CALYPSO; CALYPSO2; Calypso Corer; Calypso Corer II; Calypso square corer; Calypso Square Core System; CASQ; CASQS; CDRILL; CHIPAL; COMPCORE; Composite Core; CONDOR-Ia; Core; CORE; Core drilling; DEPTH, sediment/rock; E11-2; Eastern Weddell Sea, Southern Ocean; East Pacific; ELEVATION; Event label; FR01/97; FR01/97-12; Franklin; GC; GeoB1028-5; GeoB2107-3; GeoB3302-1; GeoB3359-3; GeoB6201-5; GeoB6211-2; GeoB7165-1; GGC; Giant gravity corer; Giant piston corer; Giant piston corer (Calypso); GIK16160-3; GIK17747-2; GIK17748-2; GL1090; GL-1090; Globigerina bulloides, δ18O; Globigerinoides ruber, δ18O; GPC; GPC-C; Gravity corer; Gravity corer (Kiel type); Hikurangi margin; HOTLINE, HYGAPE; Identification; IMAGES II; IMAGES XV - Pachiderme; INMD; INMD-115BX; James Clark Ross; Joides Resolution; JR179; JR179-TC493; JR20080221; Kerguelen Plateau; KN159-5; Knorr; KNR159-5; KNR159-5-36GGC; LATITUDE; Leg177; Leg202; LONGITUDE; M23/2; M46/2; M6/6; M75/3; M75/3_137-3; Marion Dufresne (1972); Marion Dufresne (1995); MD00-2361; MD02-2488; MD02-2594; MD032611G; MD03-2611G; MD07-3076; MD07-3076Q; MD07-3082; MD07-3088; MD07-3100; MD07-3119; MD07-3128; MD104; MD105; MD12-3396Cq; MD12-3401; MD125; MD 125 / SWIFT BIS-CARHOT; MD128; MD131; MD159; MD189; MD38; MD80-304; MD84-527; MD84-551; MD88-769; MD88-770; MD94-103; MD96-2048; MD96-2080; MD962080, ABS; MD962094; MD96-2094; MD97-257; Melville; Meteor (1986); Meteor Rise; Neogloboquadrina pachyderma, δ18O; North West Cape, Western Australia; off Chile; Outer Walvis Ridge; P69; PC; PEGASE; Piston corer; Polarstern; PS08; PS08/374; PS10; PS10/816; PS1394-4; PS1506-1; PS16; PS16/311; PS1768-8; PUCK; RC11; RC1112; RC11-120; RC13; RC13-271; Reference/source; Rig Seismic; Robert Conrad; RR0503-125JPC; RR0503-79JPC; RR0503-87JPC; RS147; RS147-GC07; Sambesi Fan; Shona Ridge; SL; SO101; SO101/3_2-1; SO102/1; SO136; SO136_111GC-12; SO156/3; SO80_2; SO80_4; SO80a; Sonne; South Atlantic Ocean; South-East Pacific; Southern Agulhas Bank; Southern Ocean; South Indian Ocean; South Pacific; Southwest Pacific; Station 6, MD189-3396; Subantarctic Pacific Ocean; SWAF; TAN0803; TAN0803-09; TAN1106; TAN1106/34; TAN1106/43; Tangaroa; Tasman Sea; TASQWA; TC; TC493 CORE_NO 493; TN057-10; TN057-13-PC4; TN057-6; Trigger corer; Uniform resource locator/link to source data file; Walvis Ridge; Walvis Ridge, Southeast Atlantic Ocean; western South Atlantic
    Type: Dataset
    Format: text/tab-separated-values, 17388 data points
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  • 7
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    Last Glacial Maximum seawater temperature estimates based on planktonic foraminifera (2023)
    PANGAEA
    Details
    Publication Date: 2024-06-28
    Description: Estimates of Last Glacial Maximum annual mean seawater temperatures at 50 m depth. The temperature estimates are derived using the Modern Analogue Technique using the ForCenS synthesis (https://doi.org/10.1594/PANGAEA.873570; https://doi.org/10.1038/sdata.2017.109) and World Ocean Atlas 1998 temperature (http://www.nodc.noaa.gov/oc5/woa98.html) for calibration. Dissimilarity to the core top data was calculated using the square-chord distance and the temperatures are the weighted averages of the 10 closest analogues. Estimates were averaged for sites where more than a single sample is available. The data contain a unique ID for each site, a core name, longitude and latitude, temperature in degree Celsius, the temperature anomaly with respect to the World Ocean Atlas climatology, an estimate of species turnover with respect to the nearest core top sample (Bray-Curtis dissimilarity), the number of data points and the uncertainty of the temperature estimate. This uncertainty considers spatial autocorrelation in the training set. It is reduced by the square root of n whenever multiple samples were available for a site.
    Keywords: 06MT15_2; 06MT41_3; 087-1; 101; 108-658C; 111-677B; 117-723A; 122-760A; 122-762B; 134-828; 138-846B; 145-883D; 160-969; 160-973; 161-975; 161-977; 165-999A; 181-1123; 202-1240; 2065N; 21SL; 31-KL; 39KL; 41; 47KL; 509-1; 63F/NL; 6706-2; 70-506B; 7SL; 80KB11; 90-588; 90-591; 90-592; 90-593; 90-594; 94a; 99; A150/180; A15558; A156-4; A164-24; A164-5; A164-6; A164-61; A167-13; A167-14; A172-1; A172-2; A173-4; A179-15; A180-15; A180-16; A180-32; A180-39; A180-47; A180-48; A180-56; A180-72; A180-73; A180-74; A180-76; A180-9; Aegean Sea; After Bray & Curtis (1957); AGSO Cruise 147; Agulhas Current; Akademik M.A. Lavrentyev; Alboran Sea; ALIENOR; also published as VM28-122; AMADEUS; Amazon Fan; Angola Basin; Antarctic Ocean; ANT-IV/1c; APSARA4; Arabian Sea; Arctic Ocean; Argentine Basin; ARK-II/4; ARK-IV/3; ARK-IX/4; ARK-V/3b; ARK-VII/3b; ARK-VIII/2; ARK-X/2; ARK-XIII/2; ARK-XIII/3; Atlantic Ocean; AUSCAN; B0914c/53; Barents Sea; Baruna Jaya I; Bay of Biscay; BC; BC15; Bear Island Fan; Belgica; BG09/14c; Biscaya; BOFS11882#4; BOFS11886#2; BOFS11896#1; BOFS11902#1; BOFS11905#1; BOFS14K; BOFS16K; BOFS17K; BOFS31/1K; BOFS31#1; BOFS5K; BOFS8K; Box corer; Brazil Basin; BS79-22; BS79-33; BS79-37; BS79-38; CALYPSO; CALYPSO2; Calypso Corer; Calypso Corer II; Calypso square corer; Canarias Sea; Cape Basin; Caribbean Sea; CASQ; CD154; CD154-17-17K; CD53; Center for Marine Environmental Sciences; CEPAG; CH82-24; CH8X; Charles Darwin; CHAT_1k; CLIVAMPcruises; Cocos Ridge; COMPCORE; Composite Core; CONDOR-Ia; Coral Sea; Core; CORE; D184; DED87-07; DEDALE87; Denmark Strait; DGKS9603; Discovery (1962); DRILL; Drilling/drill rig; E26-1; E27-23; E27-30; E45-027; E45-078; E45-102; E45-29; E48-003; E48-022; E48-023; E48-027; E48-028; E48-035; E48-11A; E49-023; E49-18; E49-21; E55-6; East Atlantic; East Brazil Basin; Eastern Basin; Eastern Rio Grande Rise; eastern Romanche Fracture Zone; Eastern slope of Kurile Basin; East Pacific; Emperor Seamounts; EN6610; Equatorial Atlantic; Equatorial East Pacific; ETNA80; ETNA82; Event label; FAEGAS_IV; Faeroes Bank; FGGE-Equator 79 - First GARP Global Experiment; FR1/94-GC3; FR10/95; FR10/95-11; FR10/95-14; FR10/95-17; FR10/95-20; FR10/95-29; FR10/95-GC05; FR10/95 GC-29; FR2/96; FR2/96-10; FR2/96-17; FR2/96-27; Fram Strait; Franklin; French Guiana; GC; Genesis III, RR9702A; GeoB10029-4; GeoB10038-4; GeoB10042-1; GeoB10043-3; GeoB10053-7; GeoB10069-3; GeoB1008-3; GeoB1016-3; GeoB1028-5; GeoB1031-4; GeoB1032-3; GeoB1034-3; GeoB1041-3; GeoB1101-5; GeoB1105-4; GeoB1112-4; GeoB1115-4; GeoB1117-2; GeoB1214-1; GeoB1220-1; GeoB12615-4; GeoB1306-1; GeoB1309-2; GeoB1312-2; GeoB1413-4; GeoB1417-1; GeoB1419-2; GeoB1501-4; GeoB1503-1; GeoB1505-1; GeoB1508-4; GeoB1515-1; GeoB1523-1; GeoB16224-1; GeoB1701-4; GeoB1706-2; GeoB1711; GeoB1711-4; GeoB1722-1; GeoB18530-1; GeoB1903-3; GeoB1905-3; GeoB2004-2; GeoB2016-1; GeoB2019-1; GeoB2021-5; GeoB20616-1; GeoB2104-3; GeoB2109-1; GeoB2116-4; GeoB2117-1; GeoB2125-1; GeoB2202-4; GeoB2204-2; GeoB2215-10; GeoB2819-1; GeoB3104-1; GeoB3117-1; GeoB3175-1; GeoB3176-1; GeoB3302-1; GeoB3603-2; GeoB3722-2; GeoB3801-6; GeoB3808-6; GeoB3813-3; GeoB5112-5; GeoB5115-2; GeoB5121-2; GeoB5133-3; GeoB5140-3; GeoB7010-2; GEOFAR; GEOTROPEX 83, NOAMP I; Giant box corer; Giant piston corer; GIK12309-2; GIK12310-4; GIK12328-5; GIK12329-6; GIK12337-5; GIK12345-5; GIK12347-2; GIK12379-1; GIK12392-1; GIK13289-3; GIK13291-1; GIK13519-1; GIK13521-1; GIK15612-2; GIK15627-3; GIK15637-1; GIK15669-1; GIK16017-2; GIK16396-1; GIK16397-2; GIK16415-2; GIK16457-2; GIK16458-1; GIK16458-2; GIK16772-2; GIK16776-1; GIK16867-2; GIK17045-3; GIK17049-6; GIK17050-1; GIK17051-3; GIK17055-1; GIK17724-2; GIK17725-1; GIK17730-4; GIK17938-2; GIK17940-2; GIK17954-1; GIK21533-3 PS11/412; GIK21730-2 PS13/224; GIK23056-2; GIK23065-2; GIK23071-3; GIK23074-1; GIK23230-1 PS05/416; GIK23262-2; GIK23294-4; GIK23351-1; GIK23354-6; GIK23419-8; GIK23519-5; GKG; GL1090; GL-1090; GL-77; Glomar Challenger; GPC; Gravity corer; Gravity corer (Kiel type); Greenland Sea; Greenland Slope; Guinea Basin; Gulf of Cádiz, Atlantic Ocean; Hikurangi margin; HU87-033-008; HU90-13-013; HU91-045-090; HUD90/13; Hudson; Hunter Channel; Identification; IMAGES I; IMAGES III - IPHIS; IMAGES IV-IPHIS III; IMAGES V; IMAGES VIII - MONA; IMAGES VII - WEPAMA; IMAGES XV - Pachiderme; Indian Ocean; Jean Charcot; Joides Resolution; JOPSII-6; K12; K708-004; K708-006; K708-007; K708-008; K714-3; KAL; KALMAR II; Kasten corer; KET80-03; KET80-19; KET80-22; KET80-39; KET82-16; KF09; KF13; KF16; KH90-3-P2; KH92-1-3a; KH92-1-5a; KL; KL96; KN708-1; KOL; KOMEX II; KS310; LATITUDE; LC01; LC04_LGM; LC07; LC21, LC-21; Leg108; Leg111; Leg117; Leg122; Leg134; Leg138; Leg145; Leg160; Leg161; Leg165; Leg181; Leg202; Leg70; Leg90; Le Noroit; Le Suroît; LGM; LONGITUDE; LV29-114-3; LV29-2; M11/1; M12/1; M123; M123_175-1; M12392-1; M13/2; M15/2; M16/1; M16/2; M17/2; M2/2; M20/2; M23/1; M23/2; M23/3; M25; M29/2; M34/1; M34/2; M34/3; M35/1; M35003-4; M35027-1; M39; M41/3; M49/4; M51; M53; M53_169; M57; M6/5; M6/6; M60; M65; M7/2; M7/3; M7/5; M75/2; M75/2_103-4; M9/4; Marge Ibérique; Maria S. Merian; Marion Dufresne (1972); Marion Dufresne (1995); MARUM; MATACORE; MD012390; MD01-2390; MD012394; MD01-2394; MD012398; MD01-2398; MD012409; MD01-2409; MD012416; MD01-2416; MD022489; MD02-2489; MD022520; MD02-2520; MD022523; MD02-2523; MD022529; MD02-2529; MD032607; MD03-2607; MD03-2705; MD04-2797CQ; MD04-2805CQ; MD04-2805Q; MD04-2845; MD062986; MD06-2986; MD07-3082; MD07-3088; MD07-3100; MD10; MD101; MD104; MD106; MD111; MD114; MD122; MD126; MD13; MD131; MD134; MD140; MD141; MD152; MD159; MD76-131; MD77-169; MD77-171; MD77-179; MD77-180; MD77-191; MD77-194; MD77-203; MD81; MD81-LC07; MD81-LC21; MD84-627; MD84-629; MD84-632; MD84-641; MD88-770; MD90-901; MD90-917; MD952011; MD95-2011; MD952012; MD95-2012; MD952039; MD95-2039; MD952040; MD95-2040; MD952041; MD95-2041; MD952042; MD95-2042; MD952043; MD95-2043; MD96-2048; MD972121; MD97-2121; MD972138; MD97-2138; MD972142; MD97-2142; MD972148; MD97-2148; MD972151; MD97-2151; MD982195; MD98-2195; MD982196; MD98-2196; MD99-2281; MD99-2285; MD99-2331; MD99-2339; MD99-2344; MD99-2346; ME0005A-3JC; Mediterranean Sea; Meteor (1964); Meteor (1986); Mid Atlantic Ridge; MONITOR MONSUN; MSM20/3; MSM39; MUC; MultiCorer; N.Faeroes; NA87-22; Namibia continental slope; NE-Brazilian continental margin; Neofan; Niger Sediment Fan; NOE; North Atlantic; Northeast Atlantic; North East Atlantic; Northern Cape Basin; North Levantine Basin; North Pacific/MOUND; North Pacific Ocean; Northwest Atlantic; Norwegian-Greenland Sea; Norwegian Sea; NS07-25; Number of samples; OD-041-04; Oden; ODEN-96; off Gabun; off Iceland; off Liberia; off NW Africa; off West Africa; OSIRIS5; OSIRIS II; OSIRIS III; P69; PABESIA; Pacific/off Hawaii; PALAEOFLUX; PALEOCINAT; PALEOCINAT II; PC; PC17; PEGASE; PICABIA; Piston corer; Piston corer (BGR type); Piston corer (Kiel type); Planktonic foraminifera; PO158/B; Polarstern; Porto Seamount; POS158/2; POS210/2; Poseidon; PRIVILEGE; PROMETEI; PROMETEII; PS05; PS08; PS11; PS1230-1; PS13 GRÖKORT; PS1533-3; PS17; PS17/242; PS17/245; PS17/251; PS17/290; PS1730-2; PS19/100; PS19/112; PS1919-2; PS1922-1; PS1927-2; PS1951-1; PS19 EPOS II; PS2129-1; PS2138-1; PS2446-4; PS2613-6; PS2644-5; PS27; PS27/020; PS2837-5; PS2876-1; PS2887-1; PS31; PS31/113; PS31/160-5; PS44; PS44/065; PS45; PS45/029; PS45/058; Q200; Q585; R657; RC08; RC08-145; RC08-148; RC08-39; RC08-78; RC09; RC09-124; RC09-126; RC09-150; RC09-161; RC09-162; RC09-178; RC09-191; RC09-225; RC09-49; RC10; RC10-11_LGM; RC10-131; RC10-16_LGM; RC10-50; RC10-62; RC10-97; RC11; RC1112; RC11-120; RC11-121; RC11-126; RC11-134; RC11-145; RC11-147; RC11-21; RC11-210; RC11-213; RC11-22; RC11-23; RC11-26; RC11-86; RC12; RC12-10; RC12-109; RC12-113; RC12-234; RC12-241; RC12-267; RC12-291; RC12-294; RC12-328; RC12-339; RC12-340; RC12-341; RC12-343; RC12-344; RC12-36; RC13; RC13-11; RC13-110; RC13-115; RC13-151; RC13-152; RC13-153; RC13-
    Type: Dataset
    Format: text/tab-separated-values, 4529 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 8
    facet.materialart.
    Unknown
    Global marine radiocarbon data compilation for the last deglaciation, zonal averages for each major ocean basin and each deglacial time-slice (2023)
    PANGAEA
    Details
    Publication Date: 2024-06-28
    Description: Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages that are independently derived and/or are consistent with the Marine20 radiocarbon calibration curve. The data have been screened and include data flags pertaining to anomalous values (e.g. negative offsets relative to the contemporary atmosphere), low sedimentation rates 〈2 cm/kyr, and/or deviations from dominant regional-temporal trends. The data are further grouped by ocean basin, and according to their associated calendar ages as belonging to a succession of time slices across the last deglaciation: the Last Glacial Maximum (LGM), Heinrich Stadial 1 (HS1), the Bolling-Allerod (BA), the Younger Dryas, the Early Holocene (7-11ka BP), and the late Holocene (〈6 ka BP).
    Keywords: 0050PG; 0066PG; 145-887; 146-893A; 167-1019; 17/1GCA; 1K-SUERC; 1P-OS-75; 1P-SUERC; 202-1240; 22SL; 310-M0015A; 310-M0016A; 310-M0018A; 310-M0020A; 310-M0021A; 310-M0023A; 310-M0023B; 310-M0024A; 310-M0025A; 310-M0025B; 310-M0026A; 313-M0027A; 313-M0029A; 341-U1419; 35MF20120125, OISO_21, INDIEN SUD 2; 47396B; 4P-OS-75; 4P-SUERC; 50-37KL; 5P-OS-79; 5P-SUERC; 64-480; 90b; 94-609; AII125-8-55; AII125-8-56; AK-AA-1; Akademik M.A. Lavrentyev; AK-BC-2; AK-F-1; AK-L-1; ALIENOR; also published as VM28-122; ALV; ALV-3884; ALV-3885; ALV-3887; ALV-3890; ALV-3891; ALV-3892; ALV-4162; ALVIN; ANT-XI/4; ANT-XXIII/9; ANT-XXVI/2; ARA04-43E; Argentine Basin; ARK-II/5; ARK-X/2; AT07-35; AT12-01; Atlantis (1997); B34-91; BC; Bering Sea; BO04-PC11; Box corer; Brazil Basin; Burdwood_Bank; CALYPSO; CALYPSO2; Calypso Corer; Calypso Corer II; Calypso square corer; Calypso Square Core System; CASQ; CASQS; CD159; CD159-10; CD38-17P; CDRILL; Cenderawasih Bay; CH84-14; Charles Darwin; CHAT 10K; CHAT-10K; CHAT-16K; CHAT-3K; CHAT-5K; CHR-4; CHR-5; CHR-6; CHR-7; COMPCORE; Composite Core; Conrad Rise; Coral; Core; CORE; Core drilling; Corner Rise; DAPC2; deglacial; Denmark Strait; DH117; DH43; DH74; DP Hunter; DR23; DR27; DR34; DR35; DR38; DR40; Drake Passage; Dredge; DRG; DRILL; Drill9A_Tasmaloum; Drilling/drill rig; Eastern Equatorial Pacific; Eastern slope of Kurile Basin; East Pacific; EBA1; EBA10; EBA11; EBA2; EBA3; EBA4; EBA5; EBA6; EBA7; EBA8; EBA9; EBB1; EBB2; EBB3; EBB4; EBB5; EBB6; EBB7; ENG-111; Equatorial East Pacific; Equatorial Indian Ocean; ESTASE1; ET97-7T; EW0408; EW0408-26JC; EW0408-87JC; Exp310; Exp313; Exp341; f0001carcs; F2-92-P3; F8-90-G21; FLAMINGO; Foraminifera; GC; GC_POI; GeoB1503-1; GeoB2104-3; GeoB7149-2; GeoB7162-6; GeoB7163-7; GeoB7167-6; GEOSCIENCES, MARMARCORE; GGC; GGC5; gh02-1030; Giant box corer; Giant gravity corer; Giant piston corer; GIK23243-2 PS05/431; GIK23415-9; GKG; Glomar Challenger; GPC; Gramberg Seamount; Gravity corer; Gravity corer (Kiel type); Gravity corer (POI); GS07-150-20/2A; Gulf of California; H209; H213; HU72-021-3; HU72-021-7; HU89038-8PC; IMAGES I; IMAGES III - IPHIS; IMAGES IV-IPHIS III; IMAGES V; IMAGES VII - WEPAMA; IMAGES XII - MARCO POLO; IMAGES XV - Pachiderme; Indian Ocean; INOPEX; Interim_Seamount; James Cook; Japan Trench; JC094; JC094_GRM; Jean Charcot; JFA17; JFA2; JFA20; JFA24; JF-FI-19PC; Joides Resolution; JPC; JT96-09; JT96-09PC; Jumbo Piston Core; KAL; KALMAR II; Kasten corer; Kayd; KL; KN_USA; KN11002; KN159-5; Knorr; KNR110-50; KNR110-66; KNR110-82a; KNR110-82GGC; KNR140; KNR140-01JPC; KNR140-02JPC; KNR140-12JPC; KNR140-2-12JPC; KNR140-2-22JPC; KNR140-22JPC; KNR140-2-30GGC; KNR140-2-51GGC; KNR140-26GGC; KNR140-30GGC; KNR140-37JPC; KNR140-39GGC; KNR140-43GGC; KNR140-50GGC; KNR140-51GGC; KNR140-56GGC; KNR140-66GGC; KNR159-5; KNR159-5-78GGC; KNR176-17GC; KNR176-2; KNR176-2-JPC30; KNR178; KNR178-2GGC; KNR178-32JPC; KNR195-5-CDH23; KNR195-5-CDH26; KNR195-5-CDH41; KNR195-5-GGC43; KNR197-10; KNR197-10CDH42; KNR197-10-CDH42; KNR197-10-CDH46; KNR197-10-GGC17; KNR197-10-GGC5; KNR198-CDH36; KNR198-GGC15; KNR198-GGC35; KNR31GPC5; KNR73-3PC; KNR73-4PC; KNR73-6PG; KOL; KOMEX; KOMEX II; KR02-15-PC06; Kronotsky Peninsula; KT89-18-P4; Lakshadweep Sea; Laurentian fan; Leg145; Leg146; Leg167; Leg202; Leg64; Leg94; Le Suroît; LMG06-05-9; LPAZ21P; LV27/GREGORY; LV27-2-4; LV29-114-3; LV29-2; M16/2; M17/2; M23/2; marine; Marion Dufresne (1972); Marion Dufresne (1995); MAT-1A; MAT-3A; Maurice Ewing; MD012386; MD01-2386; MD012420; MD01-2420; MD01-2461; MD02-2461; MD022489; MD02-2489; MD03-2697; MD03-2707; MD04-2829CQ; MD04-2845; MD052896; MD05-2896; MD052904; MD05-2904; MD07-3076; MD07-3076Q; MD07-3088; MD08-3169; MD09-3256; MD09-3256Q; MD09-3257; MD101; MD106; MD111; MD114; MD122; MD123; MD12-3396Cq; MD13; MD134; MD141; MD147; MD159; MD173; MD189; MD77-176; MD952002; MD95-2002; MD952007; MD95-2007; MD972106; MD97-2106; MD972121; MD97-2121; MD972138; MD97-2138; MD982165; MD98-2165; MD982181; MD98-2181; MD99-2331; MD99-2334; ME0005-24JC; Melville; Meriadzec; Meteor (1986); ML1208-01PC; MR01-K03; MR06-04_PC04A; MUC; MULT; MultiCorer; Multiple investigations; Mururoa; MV1007; MV1007-DO3; MV99-GC31; MV99-GC38; MV99-MC17/GC32/PC10; MV99-MC19; MV99-PC08; NA064-117-1; NA064-118-1; NA87-22; Nathaniel B. Palmer; NBP0805; NBP0805-DR23; NBP0805-DR27; NBP0805-DR34; NBP0805-DR35; NBP0805-DR36; NBP0805-DR38; NBP0805-DR40; NBP0805-TB04; NBP1103; NBP1103-DH07; NBP1103-DH112; NBP1103-DH113; NBP1103-DH115; NBP1103-DH117; NBP1103-DH120; NBP1103-DH134; NBP1103-DH14; NBP1103-DH140; NBP1103-DH143; NBP1103-DH15; NBP1103-DH22; NBP1103-DH43; NBP1103-DH74; NBP1103-DH95; Nesmeyanov25-1-GGC15; Nesmeyanov25-1-GGC18; Nesmeyanov25-1-GGC20; Nesmeyanov25-1-GGC27; New England Mountains; New Jersey Shallow Shelf; North Atlantic; North Atlantic/FLANK; Northeast Atlantic; North East Atlantic; North Pacific/Gulf of California/BASIN; North Pacific Ocean; Northwest Atlantic; Norwegian Sea; OCE326-GGC14; OCE326-GGC26; OCE326-GGC5; off Chile; off Nova Scotia; OK-3; OK-8; OKB-36A; OKB-53B; OKB-B3; OSIRIS III; Pacific Ocean; PALEOCINAT; PALEOCINAT II; papua; PC; PC75-1; PC75-2; Philippine Sea; PICABIA; Piston corer; Piston corer (BGR type); Piston corer (Kiel type); PLDS-007G; PLDS-1; Pleiades; Polarstern; PS05; PS1243-2; PS2606-6; PS2644-5; PS30; PS30/144; PS31; PS31/160-5; PS69; PS69/907-2; PS69/912-3; PS69/912-4; PS75/059-2; PS75/100-4; PS75/104-1; PS75 BIPOMAC; PUCK; radiocarbon dates; RAPiD-10-1P; RBDASS05; RBDASS05_H11; RBDASS05_H15; RC11; RC1112; RC11-238; RC24; RC24-8GC; RC27; RC27-14; RC27-23; Remote operated vehicle; Remote operated vehicle Jason II; RETRO-2; RGF_Barbados; RGF-12; RGF-15; RGF-16; RGF-9; RNDB-GGC15; RNDB-GGC5; RNDB-PC11; RNDB-PC13; Robert Conrad; ROV; ROVJ; RR0503-06JPC; RR0503-36JPC; RR0503-64JPC; RR0503-79JPC; RR0503-831C; RR0503-83GC; S67-FFC15; S794; S931; S938; Sakhalin shelf and slope; Sars_Seamount; SC4_ST2_SW2_SX1; Scotia Sea; Sea of Okhotsk; SEDCO; Sediment corer; Shackleton_Fracture_Zone; SHAK03-6K; SHAK05-3K; SHAK06-4K; SHAK10-10K; SHAK14-4G; Shirshov Ridge; Sindhu Sadhana; Site_1471; Site_2088; Site_21210009; Site_2307; Site_2631; Site_2657; Site_2706; Site_2774; Site_47396; Site_654; Site_660; Site_936; SK129-CR2; SL; Smithsonian_48735.1; SO156/2; SO156/3; SO161/5; SO161/5_22SL; SO178; SO178-13-6; SO201/2; SO201-2-101; SO201-2-12KL; SO201-2-77; SO201-2-85; SO202/1; SO202/1_18-6; SO213/2; SO213/2_76-2; SO213/2_79-2; SO213/2_82-1; SO213/2_84-1; Sonne; SOPATRA; South Atlantic; South Atlantic Ocean; South China Sea; Southern Alaska Margin: Tectonics, Climate and Sedimentation; South of Iceland; South Pacific Ocean; South Tasman Rise; Southwest Pacific; Southwest Pacific Ocean; SPOC; SS152; SS172; SSD-044; SSD044_GC-01; Station 6, MD189-3396; St Kildas Basin; SU90-08; SU92; SU92-03; Submersible Alvin; TAH-01A-3A; TAH-02A-4F; TAH-02A-4G; TAH-02A-4H; TAH-02A-5D; TAH-02A-5F; TAH-02A-5G; TAH-02A-5H; TAH-03A-1; TAH-03A-1A; TAH-03A-1E; Tahiti, offshore Faaa; Tahiti, offshore Maraa; Tahiti, offshore Tiarei; Tahiti Sea Level; Ta-P6; Ta-P7; Ta-P8; Tasman Sea; Thomas G. Thompson; Thomas G. Thompson (1964); Thomas Washington; TN228; TN228_J2_382; TN228_J2_383; TN228_J2_387; TN228_J2_389; TN228_J2_393; TN228_J2_395; TNO57-21; TR163-22; TR163-23; TR163-31; TROPICS; TT154-10; TTN013-18; TTXXX; U938; U939; urlepa; V19; V19-27; V21; V21-40; V28; V28-122; V28-238; V34; V34-98; V35; V35-5; V35-6; VAY1; VEM1_8; Vema; ventilation; Vigo; VINO19-4-GGC17; VINO19-4GGC-37; VINO19-4-GGC37; VM21-30; VNTR01; VNTR01-10GC; Vuolep Allakasjaure; W8709A; W8709A-13; Wecoma
    Type: Dataset
    Format: application/x-hdf, 493.1 kBytes
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 9
    facet.materialart.
    Unknown
    Water column raw data (Kongsberg EM 122 entire dataset) of RV SONNE during cruise SO268/3 (2023)
    PANGAEA
    Details
    Publication Date: 2024-06-28
    Description: Water column raw data using the ship's own Kongsberg EM 122 multibeam echosounder was almost continuously recorded during RV SONNE cruise SO268/3. Data were recorded 30 days between 2019-05-31 and 2019-06-28 in the North Pacific Ocean. The data are archived at the Federal Maritime and Hydrographic Agency of Germany (Bundesamt für Seeschifffahrt und Hydrographie, BSH) and provided to PANGAEA database for data curation and publication. Ancillary sound velocity profiles (SVP) files from the cruise are archived at the BSH and added to the corresponding multibeam raw dataset doi:10.1594/PANGAEA.952266 This publication is conducted within the efforts of the German Marine Research Alliance in the core area 'Data management and Digitalization' (Deutsche Allianz Meeresforschung, DAM).
    Keywords: Bathymetry; Binary Object; Comment; DAM_Underway; DAM Underway Research Data; Data file recording distance; Data file recording duration; DATE/TIME; ELEVATION; Event label; Extracted from file; Extracted with MB-System; File content; KEM122; Kongsberg datagram raw file name; KONGSBERG EM122; LATITUDE; LONGITUDE; Multibeam Echosounder; North Pacific Ocean, western part; Number of pings; Ship speed; SO268/3; SO268/3_0_Underway-1; Sonne_2; Start of data file, depth; Start of data file, heading; Start of data file recording, date/time; Start of data file recording, latitude; Start of data file recording, longitude; Stop of data file, depth; Stop of data file, heading; Stop of data file recording, date/time; Stop of data file recording, latitude; Stop of data file recording, longitude; Water Column Data
    Type: Dataset
    Format: text/tab-separated-values, 12060 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 10
    facet.materialart.
    Unknown
    Raw data of physical oceanography of Underway ScanFish CTD during RV ELISABETH MANN BORGESE cruise EMB304 (2023)
    PANGAEA
    Details
    Publication Date: 2024-06-28
    Description: This raw data of physical oceanography was acquired during research cruise EMB304 of 'RV Elisabeth Mann Borgese' from October 25th to November 02nd 2022. Thereby data was measured by a Seabird SBE911+ as part of ROTV ScanFish III. Default ROTV CTD system of consists of the SBE9 with 1x SBE43 for oxygen, 1 SBE3 temperature sensor, 1 SBE4 conductivity sensor, pressure sensor, altimeter, fluorometer, turbidity meter. ROTV is a ScanFish III from EIVA a/s.
    Keywords: Baltic Sea; Binary Object; Binary Object (File Size); CTD; CTD, Sea-Bird, SBE 911plus; CTD-Scanfish; CTD-SF; DAM_Underway; DAM Underway Research Data; Elisabeth Mann Borgese; EMB304; EMB304_15-1; EMB304_19-1; EMB304_21-1; EMB304_24-1; EMB304_26-1; EMB304_28-1; EMB304_31-1; EMB304_33-1; EMB304_35-1; EMB304_37-1; EMB304_39-1; EMB304_41-1; EMB304_43-1; EMB304_45-1; EMB304_47-1; EMB304_49-1; EMB304_5-1; EMB304_51-1; EMB304_54-1; EMB304_56-1; Event label; File content; ROTV; ScanFish; underway CTD
    Type: Dataset
    Format: text/tab-separated-values, 162 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
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