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  • 1
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Discordant zebra dolomite bodies occur locally in the Middle Cambrian Cathedral and Eldon Formations of the Main Ranges of the Canadian Rocky Mountains Fold and Thrust Belt. They are characterized by alternating dark grey (a) and white (b) bands, forming an ‘abba’ diagenetic cyclicity. These bands developed parallel to both bedding and cleavage. Dark grey (a) bands consist of fine (〈 300 μm) non-planar crystalline impure dolomite. The white (b) bands are composed of coarse (up to several millimetres) milky-white pure saddle dolomites (b1) which are often covered by pore-lining zoned dolomite (b2). The b phases often possess a saddle-shaped morphology. In contrast to the replacement origin of the a dolomite, the zoned b2 dolomite rims are interpreted as a cement formed in open cavities. The b1 dolomite is interpreted as the result of recrystallization with diagenetic leaching of non-carbonate components.All the zebra dolomites studied are (nearly) stoichiometric and are characterized by enriched Na and depleted Sr concentrations. Fe and Mn concentrations in these dolomites differ depending on the sample locality. Fluid inclusion data indicate that the dolomites formed from relatively hot (TH = 130–200 °C), saline (20–23 wt% CaCl2 eq.) fluids. A diagenetic high temperature origin is also supported by depleted δ18O values (−20 to −14‰ VPDB). A contribution of 87Sr-enriched fluids is reflected in the 87Sr/86Sr values (0·7091–0·7123).Zebra dolomite development is explained by focused fluid flow, which exploited areas of structural weaknesses (e.g. basin-platform, rim areas, faults, etc.). Expulsion of hot basinal brines in a tectonically active regime generated overpressures, which explains the development of secondary porosity during zebra dolomitization as well as the intra-zebra fracturing at decimetre to micrometre scale.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 133 (1998), S. 51-59 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The Myggbukta caldera complex and a swarm of basic dykes constitute the latest Tertiary magmatism in the Hold with Hope region, East Greenland. The Sr and Nd isotope ratios of these rocks show coherent variations which extend to high 87Sr/86Sr and low 143Nd/144Nd values and require a contribution from continental lithosphere. Broad correlations with major element differentiation indices suggest that the continental component was incorporated during magmatic differentiation thereby favouring a crustal contamination process. Trace element concentrations are strongly correlated with isotopic compositions but display ranges for many incompatible elements which extend beyond likely crustal contaminant compositions. This is readily modelled by AFC processes in which the dominant cause of trace element enrichment is the concentration effect of fractional crystallisation rather than the composition of the contaminant. The simplest such models still require unrealistically high degrees of fractional crystallisation to explain the ten-fold enrichment of some trace elements. This can be overcome if the primary magmas entering the crust already had highly variable trace element compositions. Such variability is readily achieved if melts from different parts of the melting column escape without thorough homogenization. An AFC model which incorporates variability in parental magma composition is then able to simulate the range of compositions observed at Hold with Hope. This carries the implication that the variations observed are more readily attributed to changes in uncontaminated parental magma than to variations in the composition or amount of contaminant.
    Type of Medium: Electronic Resource
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  • 3
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    PANGAEA
    In:  Supplement to: Modestou, Sevasti; Gutjahr, Marcus; Van der Schee, Marlies; Ellam, Rob M; Flecker, Rachel (2019): Precessional Cyclicity of Seawater Pb Isotopes in the Late Miocene Mediterranean. Paleoceanography and Paleoclimatology, 34(12), 2201-2222, https://doi.org/10.1029/2018PA003538
    Publication Date: 2023-01-13
    Description: This dataset is presented in the article "Precessional cyclicity of seawater Pb isotopes in the late Miocene Mediterranean" (accepted, Paleoceanography and Paleoclimatology). Marginal Mediterranean marine sediments from three separate basins were sampled at sub-precessional resolution (~4-10 samples per precessional cycle). Authigenic Pb isotope compositions of the bulk sediment were extracted using acid reductive leaching and measured with MC-ICP-MS. In addition, strong leaching and total dissolution was applied to a subset of samples. This dataset includes the results of all of the measurements, plus an extensive set of secondary standard measurements performed at the same periods for quality control purposes, on two different MC-ICP-MS (Nu Plasma and Thermo Neptune Plus, GEOMAR Helmholtz Institute for Ocean Research, Kiel). Finally, there is a table of alternative sample ages based on different orbital tuning options (see manuscript text).
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 4
    Publication Date: 2023-01-13
    Description: Pb isotope results of secondary standards and calculation of external reproducibility for measurements performed on Nu Plasma MCICPMS and Neptune Plus MCICPMS, GEOMAR. Uncertainties in the table are internal measurement uncertainties reported in 2 SE format.
    Keywords: Analysis run; Comment; Lead-206/Lead-204 ratio; Lead-206/Lead-204 ratio, error; Lead-207/Lead-204 ratio; Lead-207/Lead-204 ratio, error; Lead-207/Lead-206, error; Lead-207/Lead-206 ratio; Lead-208/Lead-204 ratio; Lead-208/Lead-204 ratio, error; Lead-208/Lead-206 ratio; Lead-208/Lead-206 ratio, error; Method comment; Number
    Type: Dataset
    Format: text/tab-separated-values, 2590 data points
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  • 5
    Publication Date: 2023-01-13
    Description: Pb isotope results of acid-reductive leaching of bulk sediments from the Sorbas and Caltanissetta Basins and the Apennine Foredeep. Uncertainties in the table are internal measurement uncertainties reported to 2 SE. Some samples were repeated; if RPT# is noted, this is a repeated measurement of the same solution. Otherwise, the repeat measurement was performed with a separate leaching of a new portion of sediment. An average value of these measurements is provided where relevant. The analytical session in which the measurement was performed is explained in the table footnote.
    Keywords: AGE; Analysis run; Event label; Falconara-2; Italy; Lead-206/Lead-204 ratio; Lead-206/Lead-204 ratio, error; Lead-207/Lead-204 ratio; Lead-207/Lead-204 ratio, error; Lead-207/Lead-206, error; Lead-207/Lead-206 ratio; Lead-208/Lead-204 ratio; Lead-208/Lead-204 ratio, error; Lead-208/Lead-206 ratio; Lead-208/Lead-206 ratio, error; Los_Molinos; Method comment; Monte_del_Casino; OUTCROP; Outcrop sample; Sample ID; Spain
    Type: Dataset
    Format: text/tab-separated-values, 1976 data points
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  • 6
    Publication Date: 2023-01-13
    Description: Pb isotope results from total dissolution of bulk sediment samples from the Sorbas Basin. Uncertainties in the table are internal measurement uncertainties and reported in 2 SE format.
    Keywords: AGE; Lead-206/Lead-204 ratio; Lead-206/Lead-204 ratio, error; Lead-207/Lead-204 ratio; Lead-207/Lead-204 ratio, error; Lead-207/Lead-206, error; Lead-207/Lead-206 ratio; Lead-208/Lead-204 ratio; Lead-208/Lead-204 ratio, error; Lead-208/Lead-206 ratio; Lead-208/Lead-206 ratio, error; Lithology/composition/facies; Los_Molinos; OUTCROP; Outcrop sample; Sample ID; Spain
    Type: Dataset
    Format: text/tab-separated-values, 120 data points
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  • 7
    Publication Date: 2023-01-13
    Description: Pb isotope results of strong leachates performed on bulk sediments from the Sorbas Basin. Uncertainties in the table are internal measurement uncertainties, reported in 2SE format.
    Keywords: AGE; Lead-206/Lead-204 ratio; Lead-206/Lead-204 ratio, error; Lead-207/Lead-204 ratio; Lead-207/Lead-204 ratio, error; Lead-207/Lead-206, error; Lead-207/Lead-206 ratio; Lead-208/Lead-204 ratio; Lead-208/Lead-204 ratio, error; Lead-208/Lead-206 ratio; Lead-208/Lead-206 ratio, error; Lithology/composition/facies; Los_Molinos; OUTCROP; Outcrop sample; Sample ID; Spain
    Type: Dataset
    Format: text/tab-separated-values, 132 data points
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  • 8
    Publication Date: 2023-06-27
    Description: Pb isotope results of acid-reductive leaching of late Miocene bulk sediments from ODP Leg 161 Site 978. Uncertainties in the table are internal measurement uncertainties reported to 2 SE. One sample produced a strikingly different result; to confirm, a new measurement was performed on a new portion of sediment. An average value of these measurements is provided.
    Keywords: 161-978A; AGE; Alboran Sea; Comment; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Lead-206/Lead-204 ratio; Lead-206/Lead-204 ratio, error; Lead-207/Lead-204 ratio; Lead-207/Lead-204 ratio, error; Lead-207/Lead-206, error; Lead-207/Lead-206 ratio; Lead-208/Lead-204 ratio; Lead-208/Lead-204 ratio, error; Lead-208/Lead-206 ratio; Lead-208/Lead-206 ratio, error; Leg161; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 57 data points
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  • 9
    Publication Date: 2023-07-10
    Description: Results of alternate tuning experiments using (1) the original sapropel midpoints only, (2) sapropel mid-points and Pb isotope 'peaks' based on the 206Pb/204Pb record, and (3) based on only the 206Pb/204Pb 'peaks.'
    Keywords: AGE; Age, difference; Comment; Cycles; Depth, relative; Falconara-2; Italy; Lithology/composition/facies; OUTCROP; Outcrop sample; Sample ID
    Type: Dataset
    Format: text/tab-separated-values, 397 data points
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  • 10
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    PANGAEA
    In:  Supplement to: Pichevin, Laetitia; Reynolds, Ben C; Ganeshram, Raja S; Cacho, Isabel; Pena, L; Keefe, K; Ellam, Rob M (2009): Enhanced carbon pump inferred from relaxation of nutrient limitation in the glacial ocean. Nature, 459, 1114-1117, https://doi.org/10.1038/nature08101
    Publication Date: 2024-01-09
    Description: The modern Eastern Equatorial Pacific (EEP) Ocean is a large oceanic source of carbon to the atmosphere1. Primary productivity over large areas of the EEP is limited by silicic acid and iron availability, and because of this constraint the organic carbon export to the deep ocean is unable to compensate for the outgassing of carbon dioxide that occurs through upwelling of deep waters. It has been suggested that the delivery of dust-borne iron to the glacial ocean could have increased primary productivity and enhanced deep-sea carbon export in this region, lowering atmospheric carbon dioxide concentrations during glacial periods. Such a role for the EEP is supported by higher organic carbon burial rates documented in underlying glacial sediments but lower opal accumulation rates cast doubts on the importance of the EEP as an oceanic region for significant glacial carbon dioxide drawdown. Here we present a new silicon isotope record that suggests the paradoxical decline in opal accumulation rate in the glacial EEP results from a decrease in the silicon to carbon uptake ratio of diatoms under conditions of increased iron availability from enhanced dust input. Consequently, our study supports the idea of an invigorated biological pump in this region during the last glacial period that could have contributed to glacial carbon dioxide drawdown. Additionally, using evidence from silicon and nitrogen isotope changes, we infer that, in contrast to the modern situation, the biological productivity in this region is not constrained by the availability of iron, silicon and nitrogen during the glacial period. We hypothesize that an invigorated biological carbon dioxide pump constrained perhaps only by phosphorus limitation was a more common occurrence in low-latitude areas of the glacial ocean.
    Keywords: 202-1240A; DRILL; Drilling/drill rig; Joides Resolution; Leg202; North Pacific Ocean; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 2 datasets
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