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  • 1
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    PANGAEA
    In:  Supplement to: Bonifacie, Magali; Monnin, Christophe; Jendrzejewski, Nathalie; Agrinier, Pierre; Javoy, Marc (2007): Chlorine stable isotopic composition of basement fluids of the eastern flank of the Juan de Fuca Ridge (ODP Leg 168). Earth and Planetary Science Letters, 260(1-2), 10-22, https://doi.org/10.1016/j.epsl.2007.05.011
    Publication Date: 2024-07-19
    Description: This paper presents chlorine stable isotope compositions (delta37Cl) of sediment pore waters collected by squeezing sediment cores from the sediment-basement interface along an East-West transect through the eastern flank of the Juan de Fuca Ridge (ODP Leg 168). These "near basement fluids" (NBF) are generally thought to be representative of low-temperature fluids circulating in the off-axis basaltic crust. The delta37Cl value of the fluid directly sampled from a flow at the base of Site 1026 (WSTP1026) is also reported. NBF display delta37Cl values between -2.09 per mil and -0.12 per mil relative to the Standard Mean Ocean Chloride (SMOC defined as 0 per mil ) and small variations in chlorinity (~4%). These data contrast with the homogeneity of delta37Cl values associated with highly variable chlorinities observed in high-temperature on-axis fluids [Bonifacie et al., 2005, doi:10.1016/j.chemgeo.2005.06.008]. The NBF delta37Cl values show a general decreasing trend with distance from the ridge-axis except for two fluids. When plotted against delta18O values, the delta37Cl of the NBF show two different trends. This paper discusses the possible contributions on NBF delta37Cl values of fluid-mixing, water-rock interactions and transport processes (diffusion, ion membrane filtration) that can occur in the igneous basement. However, as none of these processes can fully explain the observed delta37Cl variations, the potential effect of the sediment cover is also investigated. At site 1026, the interstitial pore fluid displays a delta37Cl signature significantly lower than that of the fluid discharge sample (-1.90 per mil and -0.28 per mil , respectively). This difference, demonstrated here cannot be an artifact of the sampling method, rather indicates the influence of the sediment cover on NBF delta37Cl values. The potential contributions of physical processes associated with transport/compaction (e.g., diffusion, ion membrane filtration, adsorption, ion exchange) on NBF delta37Cl values are qualitatively discussed here but require additional studies for further insights. However, this study indicates that "near basement fluids" (NBF) are not, at least for Cl isotopic compositions, necessarily as representative of fluids circulating in the basaltic crust as initially thought. These results add new constraints on Cl geodynamics and show that Cl-isotopes fractionate during low-temperature circulation of fluids in off-axis and off-margin flow contexts, but not to the extent observed for active margins. Fluids circulating at low-temperature in the magmatic and/or the sedimentary part of the oceanic crust might have played a major role on the delta37Cl evolution of seawater over geologic time.
    Keywords: 168-1023A; 168-1024B; 168-1025B; 168-1026C; 168-1027B; 168-1028A; 168-1029A; 168-1030B; 168-1031A; 168-1032A; DRILL; Drilling/drill rig; Joides Resolution; Juan de Fuca Ridge, North Pacific Ocean; Leg168; North Pacific Ocean; Ocean Drilling Program; ODP
    Type: dataset publication series
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-07-19
    Keywords: 168-1026C; 168-1027B; 168-1028A; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Joides Resolution; Juan de Fuca Ridge, North Pacific Ocean; Latitude of event; Leg168; Longitude of event; Mass spectrometer VG Optima; Ocean Drilling Program; ODP; Sample code/label; Standard deviation; δ37Cl
    Type: dataset
    Format: text/tab-separated-values, 9 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-07-19
    Keywords: 168-1023A; 168-1024B; 168-1025B; 168-1026C; 168-1027B; 168-1028A; 168-1029A; 168-1030B; 168-1031A; 168-1032A; AGE; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Joides Resolution; Juan de Fuca Ridge, North Pacific Ocean; Latitude of event; Leg168; Longitude of event; Mass spectrometer VG Optima; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label; Sample code/label 2; δ37Cl
    Type: dataset
    Format: text/tab-separated-values, 32 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2024-09-11
    Description: Recent culture studies of living coccolithophores have established a biogeochemical framework for the use of the geochemical compositions of their calcite biominerals as proxies in palaeoceanography. Yet, questions remain regarding the transferability of such experimental data to fossil coccoliths. Here we analysed the carbon and oxygen isotopic composition of Miocene coccoliths to assess the suitability of such data for reconstructing the past environment. We found that the oxygen isotopic compositions of the relatively small Noelaerhabdaceae coccoliths gathered in the 3-5 μm fractions appear to be a suitable material to derive temperatures after a correction for a constant vital offset of 0.8‰. The interpretation of the isotopic signal of the relatively large Coccolithales coccoliths (5-8 μm fractions) is more complex, but supports results from cultures. The expression of the carbon and oxygen vital effect in coccoliths appears to be limited during the so-called Miocene Climate Optimum (MCO), a period of relatively elevated atmospheric pCO~2~. Subsequently, during the Miocene Climatic Transition (MCT; 14 Ma), which saw a decline in pCO~2, large carbon and oxygen vital effects were expressed in coccolith calcite. This phenomenon predates the postulated “Late Miocene Threshold” by approximately 4 Ma, and cannot be reconciled as a temporally-synchronous nor localised feature. Furthermore, we observed a statistically significant correlation between the oxygen and carbon offsets of the small relative to large coccoliths (hence, the vital effect per se) that is likely linked to variations in atmospheric CO~2~. This biogeochemical correlation further supports a forcing of the environment on the cellular physiology (growth rate and utilisation of intracellular carbon) and ultimately the magnitude of isotopic vital effects in fossil coccoliths.
    Keywords: 90-588A; 90-588C; AGE; coccolith; Coccoliths, δ13C; Coccoliths, δ18O; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Event label; Glomar Challenger; Leg90; Miocene; Size fraction 〈3 µm; Size fraction 10-12 µm; Size fraction 12-20 µm; Size fraction 3-5 µm; Size fraction 5-8 µm; Size fraction 8-10 µm; South Pacific/Tasman Sea/CONT RISE; Tasman Sea; Vital effects; δ18O, seawater, reconstructed
    Type: dataset
    Format: text/tab-separated-values, 454 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2021-06-30
    Description: Here we report on a set of six apatite reference materials (chlorapatites MGMH#133648, TUBAF#38 and fluorapatites MGMH#128441A, TUBAF#37, 40, 50) which we have characterised for their chlorine isotope ratios; these RMs span a range of Cl mass fractions within the apatite Ca10(PO4)6(F,Cl,OH)2 solid solution series. Numerous apatite specimens, obtained from mineralogical collections, were initially screened for 37Cl/35Cl homogeneity using SIMS followed by δ37Cl characterisation by gas source mass spectrometry using both dual‐inlet and continuous‐flow modes. We also report major and key trace element compositions as determined by EPMA. The repeatability of our SIMS results was better than ± 0.10% (1s) for the five samples with 〉 0.5% m/m Cl and ± 0.19% (1s) for the low Cl abundance material (0.27% m/m). We also observed a small, but significant crystal orientation effect of 0.38% between the mean 37Cl/35Cl ratios measured on three oriented apatite fragments. Furthermore, the results of GS‐IRMS analyses show small but systematic offset of δ37ClSMOC values between the three laboratories. Nonetheless, all studied samples have comparable chlorine isotope compositions, with mean 103δ37ClSMOC values between +0.09 and +0.42 and in all cases with 1s ≤ ± 0.25.
    Description: Key Points: Six apatite reference materials having various Cl mass fractions were characterised for chlorine isotope ratios by SIMS and three GS‐IRMS laboratories. A small, but significant, crystal orientation effect was recorded by SIMS analyses. Correlation of instrumental mass fractionation factor with Cl mass fraction is visible along the apatite solid solution series.
    Description: Narodowe Centrum Nauki
    Description: Deutscher Akademischer Austauschdienst
    Description: Helmholtz Recruiting Initiative
    Description: Institute of Geological Sciences, Polish Academy of Sciences
    Keywords: 551.9 ; chlorine isotopes ; apatite ; matrix effect ; crystal orientation effect ; secondary ion mass spectrometry
    Type: article
    Location Call Number Limitation Availability
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