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  • 1
    Publikationsdatum: 2024-04-30
    Beschreibung: The application of stable oxygen isotopic ratio of surface dwelling Globigerinoides ruber (white variety) (δ¹⁸Oruber) to reconstruct past hydrological changes requires precise understanding of the effect of ambient parameters on δ¹⁸Oruber. The northern Indian Ocean, with huge freshwater influx and being a part of the Indo-Pacific Warm Pool, provides a unique setting to understand the effect of both the salinity and temperature on δ18Oruber. Here, we use a total of 400 surface samples (252 from this work and 148 from previous studies), covering the entire salinity end member region, to assess the effect of seawater salinity and temperature on δ¹⁸Oruber in the northern Indian Ocean. For δ¹⁸O analysis, 10-15 well preserved shells of Globigerinoides ruber white variety, were picked from 250-355 μm size range. The stable oxygen isotopic ratio was measured by using Finnigan MAT 253 isotope ratio mass spectrometer, coupled with Kiel IV automated carbonate preparation device. The precision of oxygen isotope measurements was better than 0.08‰. The analyzed surface δ¹⁸Oruber very well mimics the expected δ¹⁸O calcite estimated from the modern seawater parameters (temperature, salinity and seawater δ¹⁸O). We report a large diagenetic overprinting of δ18Oruber in the surface sediments with an increase of 0.18‰ per kilometer increase in water depth. The salinity exerts the major control on δ¹⁸Oruber (R2 = 0.63) in the northern Indian Ocean, with an increase of 0.29‰ per unit increase in salinity. The relationship between temperature and salinity corrected δ¹⁸Oruber (δ¹⁸Oruber - δ¹⁸Osw) in the northern Indian Ocean [T= -0.59*(δ¹⁸Oruber - δ¹⁸Osw) + 26.40] is different than reported previously based on the global compilation of plankton tow δ¹⁸Oruber data. The revised equations will help in better paleoclimatic reconstruction from the northern Indian Ocean.
    Schlagwort(e): 63KA; 905B; 93KL; A15558; A15612; AAS6GC-3; AAS6GC-6; AAS9_21; AAS9/21; AII15-596; AII15-597; AII15-612; All15-585; All15-586; All15-591; All15-592; Andaman Sea; Arabian Sea; BARP-9406; BARP-9407; BARP-9409; BARP-9412; BARP-9413; BARP-9415; BARP-9422; BARP-9426; BARP-9435; BARP-9437; BC; BC21WP7; BCR; Box corer; Box corer (Reineck); Core; CORE; DOD-200; DOD-201; DOD-204; DODO-197; Eastern Arabian Sea; Elevation of event; Event label; Foraminifera; GC; GEMINO I; Globigerinoides ruber; Globigerinoides ruber white, δ18O; Grab; GRAB; Gravity corer; Indian Ocean; IOE_143KK; KAL; Kasten corer; KL; KL-15, AS-03; KL-26, AS-02; KL-36, AS-04; KL-51, AS-07; KL-57, AS-08; KL-74, AS-12; KL-79; KL-87, AS-15; Latitude of event; Longitude of event; M5/3a; M5/3a_422QM; MAKRAN 2; Marion Dufresne (1972); Mass spectrometer MAT253; MD10; MD10-26; MD10-27; MD10-28; MD10-29; MD13; MD13-29; MD13-36; MD13-42; MD13-44; MD13-50; MD13-59; MD13-60; MD13-67; MD13-68; MD76-123; MD76-125; MD76-127; MD76-128; MD76-129; MD76-131; MD76-132; MD76-135; MD76-136; MD77-164; MD77-169; MD77-171; MD77-176; MD77-177; MD77-178; MD77-179; MD77-180; MD77-181; MD77-185; MD77-191; MD77-194; MD77-195; MD77-197; MD77-200; MD77-202; MD77-203; MD77-204; Meteor (1986); MUC; MultiCorer; NIOP_905; NIOP_929; NIOP-B0/C0; NIOP-C2; Northeastern Arabian Sea; northern Indian Ocean; ORKS_08; OSIRIS II; OSIRIS III; oxygen isotope; PAKOMIN; PC; Piston corer; Piston corer (BGR type); QM; Quantameter; RC12; RC12-328; RC12-329; RC12-331; RC12-339; RC12-340; RC12-341; RC12-343; RC12-344; RC12-347; RC14; RC14-35; RC14-36; RC14-37; RC14-39; RC17; RC17-126; RC9-155; RC9-161; RC9-162; Reference/source; Robert Conrad; RVG_167/1_3904; Sagar Kanya; Sample ID; sediment; Sindhu Sadhana; Sindhu Sankalp; Size fraction; SK117; SK117_SC_05; SK117_SC_08; SK117_SC_11; SK117_SC_12; SK117_SC_14; SK117_SC_15; SK117_SC_16; SK117_SC_17; SK117_SC_18; SK117_SC_19; SK117_SC_20; SK117_SC_23; SK117_SC_25; SK117_SC_26; SK117_SC_27; SK117_SC_30; SK117_SC_31; SK117_SC_32; SK117_SC_33; SK117_SC_34; SK117_SC_39; SK117_SC_40; SK117_SC_43; SK117_SC_44; SK117_SC_45; SK117_SC_46; SK117_SC_51; SK126-GC39; SK129-CR05; SK148-GC4; SK157_GC_12; SK157_GC_14; SK157_GC_20; SK157-GC04; SK157-GC18; SK168-GC01; SK17; SK175; SK175_GB_02; SK175_GB_102; SK175_GB_103; SK175_GB_105; SK175_GB_111; SK175_GB_113; SK175_GB_116; SK175_GB_117; SK175_GB_118; SK175_GB_119; SK175_GB_121; SK175_GB_122; SK175_GB_123; SK175_GB_125; SK175_GB_127; SK175_GB_128; SK175_GB_129; SK175_GB_14; SK175_GB_19; SK175_GB_26; SK175_GB_28; SK175_GB_29; SK175_GB_30; SK175_GB_31; SK175_GB_33; SK175_GB_41; SK175_GB_58; SK175_GB_59; SK175_GB_60; SK175_GB_76; SK175_GB_77; SK175_GB_83; SK175_GB_84; SK175_GB_85; SK175_GB_86; SK175_GB_87; SK175_GB_89; SK175_GB_90; SK175_GB_91; SK175_GB_92; SK175_GB_93; SK175_GB_94; SK175_GB_96; SK175_GB_98; SK175_GB_99; SK20-GC185; SK218_1; SK237; SK237_GC09; SK237_SC_03; SK237_SC_04; SK237_SC_05; SK237_SC_06; SK237_SC_07; SK237_SC_11; SK237_SC_12; SK237_SC_13; SK237_SC_14; SK237_SC_16; SK237_SC_21; SK237_SC_22; SK237_SC_23; SK237_SC_27; SK237_SC_29; SK237_SC_32; SK237_SC_33; SK237_SC_34; SK237_SC_36; SK237_SC_37; SK237_SC_42; SK237_SC_43; SK237_SC_44; SK237_SC_46; SK237_SC_47; SK308; SK308_MC-02; SK308_MC-03; SK308_MC-04; SK308_MC-05; SK308_MC-08; SK308_MC-12; SK308_MC-14; SK308_MC-16; SK308_MC-18; SK308_MC-19; SK308_MC-23; SK308_MC-35; SK308_MC-36; SK308_MC-37; SK308_MC-38; SK308_MC-39; SK308_MC-41; SK308_MC-43; SK308_MC-44; SK308_MC-45; SK308_MC-47; SK308_MC-51; SK308_MC-55; SK308_MC-58; SK308_MC-59; SK308_MC-61; SK308_MC-63; SK308_MC-64; SK308_MC-66; SK31_GC_11; SL-1; SL-4; SN-6; SO130; SO130_211KG; SO130_282KG; SO130_285MC; SO28; SO28-05KL; SO28-11KL; SO28-18KL; SO42; SO42-15KL; SO42-26KL; SO42-36KL; SO42-51KL; SO42-57KL; SO42-74KL; SO42-79KL; SO42-87KL; SO90; SO90_39KG; SO90_56KA; Sonne; Southeastern Arabian Sea; Southwestern Bay of Bengal; SPAC; Spade Corer; SS3827G; SSD004; SSD004_G-01; SSD004_G-02; SSD004_G-03; SSD004_G-04; SSD004_G-05; SSD004_MC-01; SSD004_MC-02; SSD004_MC-03; SSD004_MC-04; SSD004_MC-05; SSD004_MC-06; SSD004_MC-07; SSD004_MC-08; SSD004_MC-09; SSD004_MC-10; SSD004_MC-11; SSD004_MC-12; SSD004_MC-13; SSD004_MC-14; SSD004_MC-15; SSD004_MC-16; SSD004_MC-17; SSD004_MC-18; SSD004_MC-19; SSD004_MC-20; SSD004_MC-21; SSD004_MC-23; SSD004_MC-26; SSD004_MC-27; SSD004_MC-28; SSD004_MC-29; SSD004_MC-30; SSD004_MC-31; SSD004_MC-32; SSD004_MC-53; SSD004_MC-54; SSD004_MC-55; SSD004_MC-56; SSD004_MC-57; SSD004_MC-59; SSD004_MC-60; SSD055; SSD055_MC01; SSD055_MC02; SSD055_MC03; SSD055_MC04; SSD055_MC05; SSD055_MC06; SSD055_MC08; SSD055_MC09; SSD055_MC10; SSD055_MC11; SSD055_MC12; SSD067; SSD067_GR04; SSD067_GR05; SSD067_GR10; SSD067_GR11; SSD067_MC02; SSD067_MC04; SSD067_MC05; SSD067_MC06; SSD067_MC07; SSD067_MC08; SSD067_MC09; SSD067_MC10; SSD067_MC11; SSD067_MC12; SSD067_MC13; SSD067_MC14; SSD067_MC16; SSD067_MC17; SSD067_MC21; SSD067_MC22; SSD067_MC24; SSD067_MC26; SSD067_MC29; SSD067_MC30; SSD067_MC31; SSD067_MC32; SSD067_MC33; SSD067_MC34; SSD067_MC36; SSD067_MC37; SSD067_MC38; SSD067_MC41; SSD067_MC42; SSD067_MC43; SSD067_MC44; SSD067_MC45; SSD067_MC46; SSD067_MC47; SSD067_MC49; SSD067_MC50; SSD067_MC51; SSD067_MC53; SSD067_MC54; SSD067_MC55; SSD067_MC56; SSK35; SSK35_SPC-25; SSK35_SPC-26; SSK35_SPC-27; SSK35_SPC-28; SSK35_SPC-29; SSK35_SPC-32; SSK35_SPC-33; SSK35_SPC-34; SSK35_SPC-37; SSK35_SPC-39; SSK35_SPC-42; SSK35_SPC-43; SSK35_SPC-45; SSK98; SSK98_GR01; SSK98_GR02; SSK98_GR03; SSK98_GR04; SSK98_GR05; SSK98_GR06; SSK98_GR10; SSK98_SPC01; SSK98_SPC02; SSK98_SPC03; SSK98_SPC07; SSK98_SPC11; SSK98_SPC12; SSK98_SPC13; SSK98_SPC14; Surface; TN41_32MC; TN47_6GGC; Tyro; V14; V14-101; V14-103; V14-104; V14-106; V14-107; V14-108; V19; V19-176; V19-177; V19-178; V19-183; V19-185; V19-188; V29; V29-15; V29-19; V29-29; V29-30; V34; V34-80; V34-83; V34-85; V34-88; Vema; Western Bay of Bengal
    Materialart: Dataset
    Format: text/tab-separated-values, 1522 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
  • 3
    Publikationsdatum: 2016-07-01
    Print ISSN: 0006-291X
    Digitale ISSN: 1090-2104
    Thema: Biologie , Chemie und Pharmazie , Physik
    Publiziert von Elsevier
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
    Digitale Medien
    Digitale Medien
    s.l. : American Chemical Society
    The @journal of organic chemistry 49 (1984), S. 4905-4912 
    ISSN: 1520-6904
    Quelle: ACS Legacy Archives
    Thema: Chemie und Pharmazie
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
    Digitale Medien
    Digitale Medien
    s.l. : American Chemical Society
    The @journal of organic chemistry 56 (1991), S. 3619-3623 
    ISSN: 1520-6904
    Quelle: ACS Legacy Archives
    Thema: Chemie und Pharmazie
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
    Digitale Medien
    Digitale Medien
    s.l. : American Chemical Society
    The @journal of organic chemistry 56 (1991), S. 1689-1692 
    ISSN: 1520-6904
    Quelle: ACS Legacy Archives
    Thema: Chemie und Pharmazie
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
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  • 7
    Digitale Medien
    Digitale Medien
    [S.l.] : American Institute of Physics (AIP)
    Journal of Applied Physics 91 (2002), S. 3764-3768 
    ISSN: 1089-7550
    Quelle: AIP Digital Archive
    Thema: Physik
    Notizen: The amorphous alloys Nd40Fe40Co5Al8B7, Nd57Fe20Co5Al10B8, and Nd57Fe20Cu5Al10B8 were prepared by copper mold casting, melt spinning, and mechanical alloying. Despite their similar x-ray diffraction patterns, samples display different magnetic and thermal behavior correlated with the method of preparation. The fully amorphous melt-spun ribbons exhibit relatively soft magnetic properties with coercivities (approximate)40 kA/m at room temperature and a Curie temperature (TC)(approximate)474 K. Apparently only the mold-cast cylinders of 3 mm diameter show hard magnetic behavior with a coercivity in the range of 258–270 kA/m (depending on composition) and have approximately the same TC as that of the melt-spun ribbons. An additional magnetic transition at 585 K due to the presence of Nd2Fe14B phase in the case of Nd40Fe40Co5Al8B7 cast rod has been observed. Heat treatment above crystallization temperature in as-cast Nd57Fe20Co5Al10B8 and Nd57Fe20Cu5Al10B8 samples destroys the hard magnetic properties. In contrast, mechanically alloyed amorphous samples are soft magnetic with maximum coercivity up to 11 kA/m but show an entirely different TC(approximate)680–740 K, which is rather characteristic of an Fe solid solution. The magnetic properties are discussed in terms of different local atomic environment and cluster sizes in amorphous samples prepared by different methods. © 2002 American Institute of Physics.
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
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  • 8
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical prospecting 28 (1980), S. 0 
    ISSN: 1365-2478
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geologie und Paläontologie , Physik
    Notizen: The combined observation of first and later arrivals in shallow seismic refraction surveys, particularly on hard rock terrains, is discussed. Details of experimental weathered-zone investigations by the correlation refraction method in a granite terrain (i.e. field procedure, seismograms obtained, plotting of the data, and identification of the waves are presented). Complete travel time data and interpreted subsurface sections of a few test refraction surveys are included. In one instance the interpreted results of normal and converted refracted wave data have been tested by drilling at three points along a 220 m long profile.
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
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  • 9
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical prospecting 27 (1979), S. 0 
    ISSN: 1365-2478
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geologie und Paläontologie , Physik
    Notizen: The blind zone problem is examined with a view to provide a simple means of solving the problem in the general case of arbitrary number of refraction layers constituting the overburden to the masked layers. Considering the first arrival refraction interval corresponding to the masked layer which reduces to zero under blind zone conditions, a method to solve the problem is presented. Derivation of the critical distance expression is also included and convenient solutions to compute the thicknesses of the blind zone and its immediate overlayer are worked out. Based on test calculations on some known instances, the efficacy of the method is illustrated. A Fortran program for use when large numbers of refraction layers are involved under the overburden or when more than one masked layer is encountered is available from the authors.
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
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  • 10
    ISSN: 1520-510X
    Quelle: ACS Legacy Archives
    Thema: Chemie und Pharmazie
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
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