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  • 1
    Publication Date: 2023-06-21
    Description: The gravity core (SK237 GC09) was collected from the central equatorial Indian Ocean (12°00.59′N, 70°52.20′E) from a water depth of 3001 m, during the 237th cruise of the ORV Sagar Kanya. The top section of the core was dated by four accelerator mass spectrometer radiocarbon dates on mixed planktic foraminifera, measured at the Center for Applied Isotope Studies, the University of Georgia, USA. The 14C dates were calibrated by using Calib7.0 software and MARINE13 dataset (Stuiver et al., 2018). The chronology of the older section was established by comparing the stable oxygen isotopic (δ18O) ratio of surface-dwelling planktic foraminifera Globigerinoides ruber (white) with the LR04 global isostack (Lisiecki and Raymo, 2005). The elemental (Mg/Ca) and stable oxygen isotopic (δ18O) ratio of surface-dwelling planktic foraminifera Globigerinoides ruber (white) was analyzed to reconstruct SST and evaporation-precipitation changes.
    Keywords: AGE; Age, 14C calibrated; Age, error; Age model; Age model according to Lisiecki & Raymo (2005) [LR04]; DEPTH, sediment/rock; GC; Glacial; Globigerinoides ruber; Gravity corer; Indian Ocean; Indo Pacific Warm Pool; Interglacial; Interval comments; Isotopic event; Mg/Ca; northern Indian Ocean; Sedimentation rate; SK237_GC09; δ18O
    Type: Dataset
    Format: text/tab-separated-values, 46 data points
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  • 2
    Publication Date: 2023-06-21
    Description: The gravity core (SK237 GC09) was collected from the central equatorial Indian Ocean (12°00.59′N, 70°52.20′E) from a water depth of 3001 m, during the 237th cruise of the ORV Sagar Kanya. The top section of the core was dated by four accelerator mass spectrometer radiocarbon dates on mixed planktic foraminifera, measured at the Center for Applied Isotope Studies, the University of Georgia, USA. The 14C dates were calibrated by using Calib7.0 software and MARINE13 dataset (Stuiver et al., 2018). The chronology of the older section was established by comparing the stable oxygen isotopic (δ18O) ratio of surface-dwelling planktic foraminifera Globigerinoides ruber (white) with the LR04 global isostack (Lisiecki and Raymo, 2005). The elemental (Mg/Ca) and stable oxygen isotopic (δ18O) ratio of surface-dwelling planktic foraminifera Globigerinoides ruber (white) was analyzed to reconstruct SST and evaporation-precipitation changes.
    Keywords: AGE; Calculated; DEPTH, sediment/rock; Estimated; GC; Glacial; Globigerinoides ruber; Globigerinoides ruber white, Magnesium/Calcium ratio; Globigerinoides ruber white, δ18O; Gravity corer; Indian Ocean; Indo Pacific Warm Pool; Interglacial; Isotope ratio mass spectrometry; Mg/Ca; northern Indian Ocean; SK237_GC09; Temperature, water; δ18O; δ18O, seawater, reconstructed
    Type: Dataset
    Format: text/tab-separated-values, 695 data points
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  • 3
    Publication Date: 2023-12-02
    Description: Here, we reconstructed sea surface temperature (SST) and upwelling intensity record from the northern tropical Indian Ocean for the last glacial termination (8-24 kyr BP). The marine sedimentary archive was collected during forth voyage of ORV Sindhu Sadhana and SST record was reconstructed using Mg/Ca in G. ruber white (sensu stricto). The upwelling intensity was reconstructed using percentage abundance of G. bulloides. The record demonstrates that the northern tropical Ocean began warming well before the increase in the atmospheric carbo dioxide and has potential implications for the strengthening of the AMOC as well as the eventual glacial termination.
    Keywords: Age, 14C AMS; Age, 14C calibrated; Age, dated; Age, dated material; Age, dated standard error; Calendar age, maximum/old; Calendar age, median; Calendar age, minimum/young; DEPTH, sediment/rock; G. ruber white; GC; Gravity corer; Laboratory code/label; Mg/Ca paleothermometry; Number; SSD004_GC03; Tropical Indian Ocean
    Type: Dataset
    Format: text/tab-separated-values, 120 data points
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  • 4
    Publication Date: 2023-12-02
    Description: Here, we reconstructed sea surface temperature (SST) and upwelling intensity record from the northern tropical Indian Ocean for the last glacial termination (8-24 kyr BP). The marine sedimentary archive was collected during forth voyage of ORV Sindhu Sadhana and SST record was reconstructed using Mg/Ca in G. ruber white (sensu stricto). The upwelling intensity was reconstructed using percentage abundance of G. bulloides. The record demonstrates that the northern tropical Ocean began warming well before the increase in the atmospheric carbo dioxide and has potential implications for the strengthening of the AMOC as well as the eventual glacial termination.
    Keywords: AGE; Agilent Technologies 700 Series Inductively Coupled Plasma-Optical Emission Spectrometer equipped with an autosampler (ASX-520) (MARUM); Calculated from Mg/Ca ratios (Anand et al., 2003); Counting 〉150 µm fraction; DEPTH, sediment/rock; G. ruber white; GC; Globigerina bulloides; Globigerinoides ruber sensu stricto, Barium/Calcium ratio; Globigerinoides ruber sensu stricto, Magnesium/Calcium ratio; Globigerinoides ruber sensu stricto, δ18O; Gravity corer; Ice volume corrected; Mass spectrometer, Thermo Fisher Scientific MAT 253; Mg/Ca paleothermometry; Sea surface temperature, annual mean; SSD004_GC03; Tropical Indian Ocean; δ18O, seawater, reconstructed
    Type: Dataset
    Format: text/tab-separated-values, 1376 data points
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  • 5
    Publication Date: 2024-04-20
    Description: The atlas contains a collection of 2,106 published and previously unpublished downcore stable isotope records of various planktonic and benthic species of foraminifera from 1,265 globally distributed sediment cores. Uncalibrated radiocarbon dates are provided for 598 cores in the collection. Each stable isotope and radiocarbon series is stored in a separate netCDF file containing fundamental meta data as attributes. The data set can be further explored and analyzed with the free software tool PaleoDataView (Langner, M. and Mulitza, S.: Clim. Past, 15, 2067–2072, https://doi.org/10.5194/cp-15-2067-2019).
    Keywords: Carbon isotopes; Foraminifera; oxygen isotopes; PAGES_OC3; PAGES - OC3 - Ocean Circulation and Carbon Cycling; PaleoDataView; Paleo Modelling; PalMod; radiocarbon
    Type: Dataset
    Format: application/zip, 4.8 MBytes
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  • 6
    Publication Date: 2024-04-13
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1522 data points
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  • 7
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    ELSEVIER SCIENCE BV
    In:  EPIC3Palaeogeography Palaeoclimatology Palaeoecology, ELSEVIER SCIENCE BV, 483, pp. 147-156, ISSN: 0031-0182
    Publication Date: 2017-09-01
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 8
    Publication Date: 2019-10-01
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 9
    Publication Date: 2019-12-08
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 10
    Publication Date: 2022-11-02
    Description: 〈jats:p〉Abstract. We present a global atlas of downcore foraminiferal oxygen and carbon isotope ratios available at https://doi.org/10.1594/PANGAEA.936747 (Mulitza et al., 2021a). The database contains 2106 published and previously unpublished stable isotope downcore records with 361 949 stable isotope values of various planktic and benthic species of Foraminifera from 1265 sediment cores. Age constraints are provided by 6153 uncalibrated radiocarbon ages from 598 (47 %) of the cores. Each stable isotope and radiocarbon series is provided in a separate netCDF file containing fundamental metadata as attributes. The data set can be managed and explored with the free software tool PaleoDataView. The atlas will provide important data for paleoceanographic analyses and compilations, site surveys, or for teaching marine stratigraphy. The database can be updated with new records as they are generated, providing a live ongoing resource into the future. 〈/jats:p〉
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , NonPeerReviewed
    Format: application/pdf
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