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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geostandards and geoanalytical research 28 (2004), S. 0 
    ISSN: 1751-908X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: This contribution aims to report the reflections we had with the scientific community during two international workshops on reference materials for stable isotopes in Davos (2002) and Nice (2003). After evaluating the isotopic homogeneity of some existing reference materials, based on either certificates, literature data or specific inter-laboratory rounds, we confirm these as primary reference materials or propose new ones relative to which stable isotope compositions should be reported. We propose DSM-3 for Mg, NIST SRM 915a for Ca, L-SVEC for Li and NBS28 for Si. Cadmium does not yet have a well identified delta zero material, although three commercial mono-elemental Cd solutions have yielded the same isotopic composition relative to one another. In order to scale the linearity of any mass spectrometer, some secondary reference materials are also proposed: Cambridge-1 solution for Mg, the “Münster-Cd” and JEPPIM Cd solutions for Cd and the “Big Batch” silicate for Si. The team from Nancy propose to prepare a mixed spike solution for Li isotopes. Well-characterised natural samples such as ocean or continental waters, diatoms, sponges, rocks and minerals are needed to validate the entire analytical procedure, particularly to take into account the effect of sample mineralisation and of chemical manipulations for elemental separation prior to analysis.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2019-01-22
    Description: This contribution aims to report the reflections we had with the scientific community during two international workshops on reference materials for stable isotopes in Davos (2002) and Nice (2003). After evaluating the isotopic homogeneity of some existing reference materials, based on either certificates, literature data or specific inter-laboratory rounds, we confirm these as primary reference materials or propose new ones relative to which stable isotope compositions should be reported. We propose DSM-3 for Mg, NIST SRM 915a for Ca, L-SVEC for Li and NBS28 for Si. Cadmium does not yet have a well identified delta zero material, although three commercial mono-elemental Cd solutions have yielded the same isotopic composition relative to one another. In order to scale the linearity of any mass spectrometer, some secondary reference materials are also proposed: Cambridge-1 solution for Mg, the “Münster-Cd” and JEPPIM Cd solutions for Cd and the “Big Batch” silicate for Si. The team from Nancy propose to prepare a mixed spike solution for Li isotopes. Well-characterised natural samples such as ocean or continental waters, diatoms, sponges, rocks and minerals are needed to validate the entire analytical procedure, particularly to take into account the effect of sample mineralisation and of chemical manipulations for elemental separation prior to analysis.
    Type: Article , PeerReviewed
    Format: text
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  • 3
    Publication Date: 2011-01-01
    Description: Mountain building exposes fossil organic carbon (OCfossil) in exhumed sedimentary rocks. Oxidation of this material releases carbon dioxide from long-term geological storage to the atmosphere. OCfossil is mobilized on hillslopes by mass wasting and transferred to the particulate load of rivers. In large fluvial systems, it is thought to be oxidised in transit, but in short, steep rivers that drain mountain islands, OCfossil may escape oxidation and re-enter geological storage due to rapid fluvial transfer to the ocean. In these settings, the rates of OCfossil transfer and their controls remain poorly constrained. Here we quantify the erosion of OCfossil from the Taiwan mountain belt, combining discharge statistics with measurements of particulate organic carbon load and source in 11 rivers. Annual OCfossil yields in Taiwan vary from 12 {+/-} 1 to 246 {+/-} 22 tC km-2 yr-1, controlled by the high physical erosion rates that accompany rapid crustal shortening and frequent typhoon impacts. Efficient transfer of this material ensures that 1.3 {+/-} 0.1 x 106 tC yr-1 of OCfossil exhumed in Taiwan is delivered to the ocean, with
    Print ISSN: 0091-7613
    Electronic ISSN: 1943-2682
    Topics: Geosciences
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  • 4
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    PANGAEA
    In:  Supplement to: Sime, N G; De La Rocha, Christina L; Tipper, Edward T; Tripati, Aradhna K; Galy, Albert; Bickle, Michael J (2007): Interpreting the Ca isotope record of marine biogenic carbonates. Geochimica et Cosmochimica Acta, 71(16), 3979-3989, https://doi.org/10.1016/j.gca.2007.06.009
    Publication Date: 2024-01-09
    Description: An 18 million year record of the Ca isotopic composition (d44/42Ca) of planktonic foraminiferans from ODP site 925, in the Atlantic, on the Ceara Rise, provides the opportunity for critical analysis of Ca isotope-based reconstructions of the Ca cycle. ?44/42Ca in this record averages +0.37+/-0.05 (1 sigma SD) and ranges from +0.21‰ to +0.52‰. The record is a good match to previously published Neogene Ca isotope records based on foraminiferans, but is not similar to the record based on bulk carbonates, which has values that are as much as 0.25‰ lower. Bulk carbonate and planktonic foraminiferans from core tops differ slightly in their d44/42Ca (i.e., by 0.06+/-0.06‰ (n = 5)), while the difference between bulk carbonate and foraminiferan values further back in time is markedly larger, leaving open the question of the cause of the difference. Modeling the global Ca cycle from downcore variations in d44/42Ca by assuming fixed values for the isotopic composition of weathering inputs (d44/42Ca_w) and for isotope fractionation associated with the production of carbonate sediments (D_sed) results in unrealistically large variations in the total mass of Ca2+ in the oceans over the Neogene. Alternatively, variations of +/-0.05‰ in the Ca isotope composition of weathering inputs or in the extent of fractionation of Ca isotopes during calcareous sediment formation could entirely account for variations in the Ca isotopic composition of marine carbonates. Ca isotope fractionation during continental weathering, such as has been recently observed, could easily result in variations in d44/42Ca_w of a few tenths of permil. Likewise a difference in the fractionation factors associated with aragonite versus calcite formation could drive shifts in D_sed of tenths of permil with shifts in the relative output of calcite and aragonite from the ocean. Until better constraints on variations in d44/42Ca_w and D_sed have been established, modeling the Ca2+ content of seawater from Ca isotope curves should be approached cautiously.
    Keywords: 154-925; COMPCORE; Composite Core; Joides Resolution; Leg154; Ocean Drilling Program; ODP; South Atlantic Ocean
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 5
    Publication Date: 2024-01-09
    Keywords: 129-801B; 129-801C; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Event label; Joides Resolution; Leg129; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label; Sample comment; δ13C, carbonate; δ18O, carbonate; δ18O, silicate
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
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  • 6
    Publication Date: 2024-01-09
    Keywords: 154-925; Age model; Calculated; COMPCORE; Composite Core; DEPTH, sediment/rock; Joides Resolution; Leg154; Multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS); Number of observations; Ocean Drilling Program; ODP; South Atlantic Ocean; δ44Ca; δ44Ca, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 144 data points
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  • 7
    Publication Date: 2024-01-09
    Keywords: 154-925; Age model; Calculated; COMPCORE; Composite Core; DEPTH, sediment/rock; Joides Resolution; Leg154; Multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS); Number of observations; Ocean Drilling Program; ODP; South Atlantic Ocean; δ44Ca; δ44Ca, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 56 data points
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  • 8
    Publication Date: 2024-01-09
    Keywords: 129-801B; Calculated; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Germanium; Germanium/Silica, biogenous opal ratio; Joides Resolution; Leg129; Multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS); North Pacific Ocean; Ocean Drilling Program; ODP; Rock type; Sample code/label; δ72Ge; δ72Ge, error; δ73Ge; δ73Ge, error; δ74Ge; δ74Ge, error
    Type: Dataset
    Format: text/tab-separated-values, 40 data points
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  • 9
    Publication Date: 2024-01-09
    Keywords: 129-801C; Aluminium (IV); Aluminium (VI); Aluminium oxide; Calcium; Calcium oxide; Calculated based on oxygen number; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Electron microprobe (EMP); Elements, total; Interlayer charge; Iron 2+ and 3+; Iron oxide, FeO; Joides Resolution; Leg129; Magnesium; Magnesium oxide; Manganese; Manganese oxide; Mineral name; North Pacific Ocean; Ocean Drilling Program; ODP; Potassium; Potassium oxide; Sample code/label; Silicon; Silicon dioxide; Sodium; Sodium oxide; Sum; Titanium; Titanium dioxide
    Type: Dataset
    Format: text/tab-separated-values, 147 data points
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  • 10
    Publication Date: 2024-01-09
    Keywords: 129-801C; Aluminium oxide; Barium; Calcium oxide; Carbon dioxide; Chromium; Cobalt; Copper; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Electron microprobe (EMP); Elements, total; Iron 3+/Iron total; Iron oxide, FeO; Joides Resolution; Leg129; Loss on ignition; Magnesium oxide; Manganese oxide; Nickel; Niobium; North Pacific Ocean; Ocean Drilling Program; ODP; Phosphorus pentoxide; Potassium oxide; Rubidium; Sample code/label; Silicon dioxide; Sodium oxide; Strontium; Titanium dioxide; Type; Water in rock; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 58 data points
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