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  • Foraminifera  (2)
  • Ocean Drilling Program; ODP  (2)
  • 112-680A; Bromine; Bromine/total organic carbon ratio; Calculated; Carbon, organic, total; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Instrumental neutron activation analysis (INAA); Iodine; Iodine/Bromine ratio; Iodine/total organic carbon ratio; Joides Resolution; Leg112; Ocean Drilling Program; ODP; Sample code/label; South Pacific Ocean  (1)
  • 112-680B; 112-681; 112-682A; 112-683A; 112-683B; 112-684B; 112-684C; 112-685A; 112-687B; 112-688A; 112-688E; Comment; COMPCORE; Composite Core; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg112; Ocean Drilling Program; ODP; Principal investigator; Sample code/label; South Pacific Ocean; δ18O, water; δ Deuterium, water  (1)
  • 112-682A; Bromide; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Iodide; Iodometric chemical method; Joides Resolution; Leg112; Ocean Drilling Program; ODP; Sample code/label; South Pacific Ocean; Spectrophotometry  (1)
Collection
Keywords
Years
  • 1
    Publication Date: 2024-01-09
    Keywords: 112-682A; Bromide; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Iodide; Iodometric chemical method; Joides Resolution; Leg112; Ocean Drilling Program; ODP; Sample code/label; South Pacific Ocean; Spectrophotometry
    Type: Dataset
    Format: text/tab-separated-values, 30 data points
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  • 2
    Publication Date: 2024-01-09
    Keywords: 112-680A; Bromine; Bromine/total organic carbon ratio; Calculated; Carbon, organic, total; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Instrumental neutron activation analysis (INAA); Iodine; Iodine/Bromine ratio; Iodine/total organic carbon ratio; Joides Resolution; Leg112; Ocean Drilling Program; ODP; Sample code/label; South Pacific Ocean
    Type: Dataset
    Format: text/tab-separated-values, 41 data points
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  • 3
    Publication Date: 2024-01-09
    Keywords: 112-680B; 112-681; 112-682A; 112-683A; 112-683B; 112-684B; 112-684C; 112-685A; 112-687B; 112-688A; 112-688E; Comment; COMPCORE; Composite Core; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg112; Ocean Drilling Program; ODP; Principal investigator; Sample code/label; South Pacific Ocean; δ18O, water; δ Deuterium, water
    Type: Dataset
    Format: text/tab-separated-values, 76 data points
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  • 4
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    PANGAEA
    In:  Supplement to: Martin, Jonathan B (1994): Diagenesis and hydrology at the New Hebrides Forearc and intra-arc Aoba Basin. In: Green, HG; Collot, J-Y; Stokking, LB; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 134, 109-130, https://doi.org/10.2973/odp.proc.sr.134.008.1994
    Publication Date: 2024-01-09
    Description: Depending on the temperature and the extent of diagenetic alteration of fluid chemistry, fluid flow at convergent margins may transfer important quantities of heat and mass between the crust and seawater, thereby influencing global mass, isotopic and heat budgets. In the North Aoba Basin, an intra-arc basin located at the New Hebrides Island Arc, alteration of volcanic ash to clay minerals and zeolites forms a CaCl2 brine, perhaps in less than 1 to 3 m.y. The brine results from an exchange of Ca for Na, K, and Mg, and an increase in Cl concentrations to a maximum of 1241 mM. The Cl increase is partly due to the transfer of H2O from the pore fluid into authigenic minerals, but water mass balances, d18O-Cl correlations, and Br/Cl ratios suggest that there is a source of Cl in the sediments. Concentration profiles indicate that Li is transferred from the fluid to solid phase at depths 〈300 meters below seafloor (mbsf), but at greater depths it is transferred from the solid to fluid phase, at temperatures possibly as low as 25°C. In the accretionary wedge extensive fluid flow appears to be confined to highly faulted regions. Although Cl concentrations less than seawater value are common at convergent margins, the New Hebrides margin contains little low-Cl fluid. Br/Cl ratios suggest the low-Cl fluid is from dilution, and d18O values indicate the water may be derived from mineral dehydration and mixing with meteoric water. The New Hebrides margin exhibits few surface manifestations of venting (e.g., sulfide-oxidizing benthic biological communities, carbonate crusts, mud volcanoes) and thus fluid fluxes may be smaller than at many other margins.
    Keywords: Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 5
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    Unknown
    PANGAEA
    In:  Supplement to: Malone, Mitchell J; Martin, Jonathan B (2000): Data report: Isotopic composition of pore fluids, New Jersey shelf and slope. In: Christie-Blick, N; Austin, JA Jr.; Malone, MJ (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 174A, 1-11, https://doi.org/10.2973/odp.proc.sr.174A.156.2000
    Publication Date: 2024-01-09
    Description: An investigation of the isotopic composition of the interstitial waters was conducted at Sites 1071, 1072, and 1073 on the New Jersey continental shelf and slope during Ocean Drilling Program Leg 174A. Sites 1071 and 1072 are closely spaced drill holes on the continental shelf located ~130 km from the shoreline in 88 and 98 m of water, respectively. Site 1073 is located on the continental slope in 640 m water and penetrated a total of 664 m of sediment of which ~520 m is Quaternary age. A total of 125 oxygen and hydrogen isotopic analyses of pore fluids are presented from all three sites. Twelve strontium isotopic ratios are reported from Site 1071.
    Keywords: Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 6
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2010. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 25 (2010): PA2211, doi:10.1029/2009PA001846.
    Description: Carbon isotopes of foraminiferal tests provide a widely used proxy for past oceanographic environmental conditions. This proxy can be calibrated using live specimens, which are reliably identified with observations of cell ultrastructure. Observations of ultrastructures can also be used for studies of biological characteristics such as diet and presence of symbionts. Combining biological and isotopic studies on individual foraminifera could provide novel information, but standard isotopic methods destroy ultrastructures by desiccating specimens and observations of ultrastructure require removal of carbonate tests, preventing isotope measurements. The approach described here preserves cellular ultrastructure during isotopic analyses by keeping the foraminifera in an aqueous buffer (Phosphate Buffered Saline (PBS)). The technique was developed and standardized with 36 aliquots of NBS-19 standard of similar weight to foraminiferal tests (5 to 123 μg). Standard errors ranged from ± 0.06 to ± 0.85‰ and were caused by CO2 contaminants dissolved in the PBS. The technique was used to measure δ13C values of 96 foraminifera, 10 of which do not precipitate carbonate tests. Calcareous foraminiferal tests had corrected carbon isotope ratios of −8.5 to +3.2‰. This new technique allows comparisons of isotopic compositions of tests made by foraminifera known to be alive at the time of collection with their biological characteristics such as prey composition and presence or absence of putative symbionts. The approach may be applied to additional biomineralizing organisms such as planktonic foraminifera, pteropods, corals, and coccolithophores to elucidate certain biological controls on their paleoceanographic proxy signatures.
    Description: Support was provided by NSF grants OCE‐0550396 (to J.B.M.), OCE‐0551001 (to J.M.B.), and OCE‐ 0550401 (to A.E.R.).
    Keywords: Foraminifera ; Ultrastructure ; Carbon isotopes
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 7
    Publication Date: 2022-05-26
    Description: Author Posting. © American Geophysical Union, 2010. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 25 (2010): PA4206, doi:10.1029/2010PA001930.
    Description: Numerous previous studies show disequilibrium between stable carbon isotope ratios of foraminiferal calcite and pore water dissolved inorganic carbon in hydrocarbon seeps, calling into question the utility of this widely used paleoceanographic tracer as a proxy. We use a recently developed method to compare stable carbon isotope ratios of foraminiferal carbonate with cell ultrastructural observations from individual benthic foraminifera from seep (under chemosynthetic bivalves) and nonseep habitats in Monterey Bay, California, to better understand control(s) of benthic foraminiferal carbon isotope ratios. Two attributes previously proposed to cause the isotopic offsets are diet and symbionts. Ultrastructural analysis shows that positive staining with Rose Bengal indicates presence of foraminiferal cytoplasm, bacterial biomass, or a combination of both and, thus, is not an unequivocal indicator of viability. We also show for the first time that some living seep foraminifera have endobionts. Results from our unique, yet limited, data set are consistent with suggestions that, in our sites, several foraminiferal species collected from seep clam beds may not survive there, diet and symbiont presence do not appear to be major contributors to disequilibrium, little calcification of seep-tolerant foraminiferal species occurs while seep conditions prevail, and microscale variability in habitats could influence δ13C of benthic foraminiferal carbonate. Results further suggest that our knowledge of benthic foraminiferal ecology and biomineralization, especially in extreme habitats such as seeps, must be bolstered before we fully understand the fidelity of paleoenvironmental records derived from benthic foraminiferal test δ13C data.
    Description: This collaborative research was supported by NSF Marine Geology and Geophysics Program (OCE‐0551001 (to J.M.B), OCE‐0550396 (to J.B.M.), and OCE‐0550401 (to A.E.R.)).
    Keywords: Clam Flats ; Monterey Bay ; Carbon isotopes ; Disequilibrium ; Foraminifera ; Cold seep
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Format: image/tiff
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