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  • 106KL; 138-846; 201-1228; 54-2-PG9; Alkenone, unsaturation index UK'37; AMPH-019G; AMPH01AR; AMPH-025G; AMPHITRITE; Argo; B0406; BC; Box corer; Calculated from UK'37 (Prahl et al., 1988); CARR12; Cocos Ridge; COMPCORE; Composite Core; Core; CORE; DEPTH, sediment/rock; DWBG-140G; DWBG-143; DWBG-144; Eastern Equatorial Pacific; Equatorial East Pacific; Event label; GC; GC_10; Genesis III, RR9702A; Giant piston corer; GPC; Gravity corer; GS7202-18; GS7202-19; GS7202-20; GS7202-22; GS7202-23; GS7202-24; GS7202-38; GS7202-40; GS7202-46; GS7202-52; Hakuho-Maru; HY06; IMAGES VIII - MONA; interpolated; Joides Resolution; KH-03-1; KL; Knorr; KNR176-2; KNR176-2-MC11; KNR176-2-MC14; KNR176-2-MC21; KNR176-2-MC24; KNR176-2-MC28; KNR176-2-MC33; KNR176-2-MC37; KNR176-2-MC4; KNR176-2-MC40; KNR176-2-MC5; KNR176-2-MC7; KNR182-9; KNR182-9-MC10; KNR182-9-MC12; KNR182-9-MC13; KNR182-9-MC14; KNR182-9-MC15; KNR182-9-MC16; KNR182-9-MC17; KNR182-9-MC2; KNR182-9-MC3; KNR182-9-MC4; KNR182-9-MC6; KNR182-9-MC7; KNR182-9-MC8; KNR182-9-MC9; KNR195-5; KNR195-5-MC11; KNR195-5-MC12; KNR195-5-MC16; KNR195-5-MC18; KNR195-5-MC22; KNR195-5-MC25; KNR195-5-MC33; KNR195-5-MC34; KNR195-5-MC38; KNR195-5-MC42; KNR195-5-MC9; Leg138; Leg201; Longitude of event; Marion Dufresne (1995); MD022529; MD02-2529; MD126; ME0005A; ME0005A-04MC4; ME0005A-07MC3; ME0005A-08MC3; ME0005A-14MC2; ME0005A-15MC6; ME0005A-20MC8; ME0005A-21MC3; ME0005A-25MC5; ME0005A-29MC2; ME0005A-35MC1; ME0005A-38MC2; ME0005A-41MC2; Melville; Moana Wave; MUC; MultiCorer; MW8708; MWSC2; MWSC7; NEMO; P6702-11G; P6702-13G; P6702-34G; P6702-4G; P6702-52G; P6702-59; Pacific Ocean; Panama Basin; PC; Peru_Upwelling; Peru1MC3; Peru2MC4; Peru3MC1; Peru4MC2; PERU-AUFTRIEB; Piston corer; Piston corer (BGR type); PLDS-066BX; PLDS-068BX; PLDS-070BX; PLDS-072BX; PLDS-074BX; PLDS-077BX; PLDS-090BX; PLDS-3; Pleiades; PUBS I; RC11; RC1112; RC11-238; RC13; RC13-106; RC13-108; RC13-142; RC18; RC18-46; RC18-48; RC23; RC23-20; Reference/source; Robert Conrad; Roger A. Revelle; RR9702A; RR9702A-62MC3; RR9702A-64MC1; RR9702A-66MC1; RR9702A-68MC3; RR9702A-70MC3; RR9702A-72MC3; RR9702A-74MC2; RR9702A-77MC2; RR9702A-80MC7; RR9702A-82MC; RR9702A-83MC; SC3; SCAN; SCAN-095G; Sea surface temperature, annual mean; SO147; SO147_106KL; Sonne; South-East Pacific; South Pacific Ocean; Temperature, difference; TG7; Thomas Washington; TR163-19; TR163-22; TR163-31; V19; V19-27; V19-28; V19-30; V21; V21-30; Vema; VNTR01; VNTR01-10GC; VNTR01-12GC; VNTR01-19PC; VNTR01-21GC; VNTR01-8PC; VNTR01-9PC; W7706; W7706-40; Wecoma; World Ocean; Y69-71P; YALOC69; Yaquina  (1)
  • 118-735B; 129-801C; 137-504B; 140-504B; 147-894F; 148-504B; 185-801C; 206-1256D; 309-U1256D; 37-332B; 52-418A; 53-418A; 70-504B; 83-504B; Amphibole; Chlorine; Chlorite; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Exp309; Glomar Challenger; Instrumental neutron activation analysis (INAA) (Reimann et al., 1998); Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Latitude of event; Leg118; Leg129; Leg137; Leg140; Leg147; Leg148; Leg185; Leg206; Leg37; Leg52; Leg53; Leg70; Leg83; Lithology/composition/facies; Longitude of event; Mass spectrometer, Finnigan, MAT 253; North Atlantic/CONT RISE; North Atlantic/VALLEY; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label; South Indian Ridge, South Indian Ocean; Superfast Spreading Rate Crust 2; X-ray diffraction (XRD); δ37Cl  (1)
  • 14C uptake; Akademik Mstislav Keldysh; AMK40; AMK40-3745-M; AMK40-3754-M; Archive of Ocean Data; ARCOD; BC; Box corer; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; GC; Gravity corer; Greenland Sea; Latitude of event; Longitude of event; MIR; MIR deep-sea manned submersible; Norwegian Sea; PL15; PL15-22; PL15-23; PL15-74; PL15-78; Professor Logachev; δ13C, particulate organic carbon
  • PANGAEA  (3)
  • 2010-2014  (3)
  • 1980-1984
  • 1940-1944
  • 2012  (3)
Collection
Keywords
Publisher
  • PANGAEA  (3)
Years
  • 2010-2014  (3)
  • 1980-1984
  • 1940-1944
Year
  • 2012  (3)
  • 1
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    (Table 13) Isotopic composition of organic carbon in surface layer bottom sediments of the Norwegian Sea (2012)
    PANGAEA
    Details
    Publication Date: 2023-03-16
    Keywords: 14C uptake; Akademik Mstislav Keldysh; AMK40; AMK40-3745-M; AMK40-3754-M; Archive of Ocean Data; ARCOD; BC; Box corer; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; GC; Gravity corer; Greenland Sea; Latitude of event; Longitude of event; MIR; MIR deep-sea manned submersible; Norwegian Sea; PL15; PL15-22; PL15-23; PL15-74; PL15-78; Professor Logachev; δ13C, particulate organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 18 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 2
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    (Table 1) Sea surface temperature reconstruction for eastern equatorial Pacific surface sediment samples (2012)
    PANGAEA
    In:  Supplement to: Kienast, Markus; MacIntyre, G; Dubois, Nathalie; Higginson, S; Normandeau, Claire; Chazen, S; Herbert, Timothy D (2012): Alkenone unsaturation in surface sediments from the eastern equatorial Pacific: Implications for SST reconstructions. Paleoceanography, 27(1), PA1210, https://doi.org/10.1029/2011PA002254
    Details
    Publication Date: 2024-02-05
    Description: Significant uncertainties persist in the reconstruction of past sea surface temperatures in the eastern equatorial Pacific, especially regarding the amplitude of the glacial cooling and the details of the post-glacial warming. Here we present the first regional calibration of alkenone unsaturation in surface sediments versus mean annual sea surface temperatures (maSST). Based on 81 new and 48 previously published data points, it is shown that open ocean samples conform to established global regressions of Uk'37 versus maSST and that there is no systematic bias from seasonality in the production or export of alkenones, or from surface ocean nutrient concentrations or salinity. The flattening of the regression at the highest maSSTs is found to be statistically insignificant. For the near-coastal Peru upwelling zone between 11-15°S and 76-79°W, however, we corroborate earlier observations that Uk'37 SST estimates significantly over-estimate maSSTs at many sites. We posit that this is caused either by uncertainties in the determination of maSSTs in this highly dynamic environment, or by biasing of the alkenone paleothermometer toward El Niño events as postulated by Rein et al. (2005).
    Keywords: 106KL; 138-846; 201-1228; 54-2-PG9; Alkenone, unsaturation index UK'37; AMPH-019G; AMPH01AR; AMPH-025G; AMPHITRITE; Argo; B0406; BC; Box corer; Calculated from UK'37 (Prahl et al., 1988); CARR12; Cocos Ridge; COMPCORE; Composite Core; Core; CORE; DEPTH, sediment/rock; DWBG-140G; DWBG-143; DWBG-144; Eastern Equatorial Pacific; Equatorial East Pacific; Event label; GC; GC_10; Genesis III, RR9702A; Giant piston corer; GPC; Gravity corer; GS7202-18; GS7202-19; GS7202-20; GS7202-22; GS7202-23; GS7202-24; GS7202-38; GS7202-40; GS7202-46; GS7202-52; Hakuho-Maru; HY06; IMAGES VIII - MONA; interpolated; Joides Resolution; KH-03-1; KL; Knorr; KNR176-2; KNR176-2-MC11; KNR176-2-MC14; KNR176-2-MC21; KNR176-2-MC24; KNR176-2-MC28; KNR176-2-MC33; KNR176-2-MC37; KNR176-2-MC4; KNR176-2-MC40; KNR176-2-MC5; KNR176-2-MC7; KNR182-9; KNR182-9-MC10; KNR182-9-MC12; KNR182-9-MC13; KNR182-9-MC14; KNR182-9-MC15; KNR182-9-MC16; KNR182-9-MC17; KNR182-9-MC2; KNR182-9-MC3; KNR182-9-MC4; KNR182-9-MC6; KNR182-9-MC7; KNR182-9-MC8; KNR182-9-MC9; KNR195-5; KNR195-5-MC11; KNR195-5-MC12; KNR195-5-MC16; KNR195-5-MC18; KNR195-5-MC22; KNR195-5-MC25; KNR195-5-MC33; KNR195-5-MC34; KNR195-5-MC38; KNR195-5-MC42; KNR195-5-MC9; Leg138; Leg201; Longitude of event; Marion Dufresne (1995); MD022529; MD02-2529; MD126; ME0005A; ME0005A-04MC4; ME0005A-07MC3; ME0005A-08MC3; ME0005A-14MC2; ME0005A-15MC6; ME0005A-20MC8; ME0005A-21MC3; ME0005A-25MC5; ME0005A-29MC2; ME0005A-35MC1; ME0005A-38MC2; ME0005A-41MC2; Melville; Moana Wave; MUC; MultiCorer; MW8708; MWSC2; MWSC7; NEMO; P6702-11G; P6702-13G; P6702-34G; P6702-4G; P6702-52G; P6702-59; Pacific Ocean; Panama Basin; PC; Peru_Upwelling; Peru1MC3; Peru2MC4; Peru3MC1; Peru4MC2; PERU-AUFTRIEB; Piston corer; Piston corer (BGR type); PLDS-066BX; PLDS-068BX; PLDS-070BX; PLDS-072BX; PLDS-074BX; PLDS-077BX; PLDS-090BX; PLDS-3; Pleiades; PUBS I; RC11; RC1112; RC11-238; RC13; RC13-106; RC13-108; RC13-142; RC18; RC18-46; RC18-48; RC23; RC23-20; Reference/source; Robert Conrad; Roger A. Revelle; RR9702A; RR9702A-62MC3; RR9702A-64MC1; RR9702A-66MC1; RR9702A-68MC3; RR9702A-70MC3; RR9702A-72MC3; RR9702A-74MC2; RR9702A-77MC2; RR9702A-80MC7; RR9702A-82MC; RR9702A-83MC; SC3; SCAN; SCAN-095G; Sea surface temperature, annual mean; SO147; SO147_106KL; Sonne; South-East Pacific; South Pacific Ocean; Temperature, difference; TG7; Thomas Washington; TR163-19; TR163-22; TR163-31; V19; V19-27; V19-28; V19-30; V21; V21-30; Vema; VNTR01; VNTR01-10GC; VNTR01-12GC; VNTR01-19PC; VNTR01-21GC; VNTR01-8PC; VNTR01-9PC; W7706; W7706-40; Wecoma; World Ocean; Y69-71P; YALOC69; Yaquina
    Type: Dataset
    Format: text/tab-separated-values, 631 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 3
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    (Table 2) Chlorine geochemistry and mineralogy of altered oceanic crust samples (2012)
    PANGAEA
    In:  Supplement to: Barnes, Jaime D; Cisneros, Miguel (2012): Mineralogical control on the chlorine isotope composition of altered oceanic crust. Chemical Geology, 326-327, 51-60, https://doi.org/10.1016/j.chemgeo.2012.07.022
    Details
    Publication Date: 2024-05-15
    Description: Bulk chlorine concentrations and chlorine stable isotope compositions were determined for hydrothermally altered basalt (extrusive lavas and sheeted dikes) and gabbro samples (n = 50) from seven DSDP/ODP/IODP drill sites. These altered oceanic crust (AOC) samples span a range of crustal ages, tectonic settings, alteration type, and crustal depth. Bulk chlorine concentrations range from 〈 0.01 wt.% to 0.09 wt.%. In general, higher chlorine concentrations coincide with an increase in temperature of alteration and amphibole content. d37Cl values of whole rock AOC samples range from -1.4 to +1.8 per mil. High d37Cl values (〉=~0.5 per mil) are associated with areas of higher amphibole content. This observation is consistent with theoretical calculations that estimate amphibole should be enriched in 37Cl compared to co-existing fluid. Negative to near zero d37Cl values are found in areas dominated by clay minerals. Chlorine geochemistry is a rough indicator of metamorphic grade and mineralogy. AOC is a major Cl host in the subducting oceanic lithospheric slab. Here we show that bulk chlorine concentrations are ~3 times higher than previous estimates resulting in a greater contribution of Cl to the mantle.
    Keywords: 118-735B; 129-801C; 137-504B; 140-504B; 147-894F; 148-504B; 185-801C; 206-1256D; 309-U1256D; 37-332B; 52-418A; 53-418A; 70-504B; 83-504B; Amphibole; Chlorine; Chlorite; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Exp309; Glomar Challenger; Instrumental neutron activation analysis (INAA) (Reimann et al., 1998); Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Latitude of event; Leg118; Leg129; Leg137; Leg140; Leg147; Leg148; Leg185; Leg206; Leg37; Leg52; Leg53; Leg70; Leg83; Lithology/composition/facies; Longitude of event; Mass spectrometer, Finnigan, MAT 253; North Atlantic/CONT RISE; North Atlantic/VALLEY; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label; South Indian Ridge, South Indian Ocean; Superfast Spreading Rate Crust 2; X-ray diffraction (XRD); δ37Cl
    Type: Dataset
    Format: text/tab-separated-values, 293 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
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