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  • AGE; Calculated from Mg/Ca ratios (Anand et al., 2003); Center for Marine Environmental Sciences; Coral Sea; DEPTH, sediment/rock; GC; GeoB22229-1; Globigerinoides ruber, Magnesium/Calcium ratio; Globigerinoides ruber, δ18O; Gravity corer; MARUM; Mass spectrometer Finnigan MAT 251; Mg/Ca; radiocarbon ages; Sea surface temperature; SO256; SO256_29-1; Sonne_2; TACTEAC; UK'37  (2)
  • 10Be; authigenic clay; beryllium; Cosmogenic nuclide; denudation; reverse weathering  (1)
Document type
Keywords
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Years
  • 1
    Publication Date: 2023-01-30
    Description: As reverse weathering has been shown to impact long-term changes in atmospheric CO2 levels, it is crucial to develop quantitative tools to reconstruct marine authigenic clay formation. We explored the potential of the beryllium (Be) isotope ratio (10Be/9Be) recorded in marine clay-sized sediment to track neoformation of authigenic clays. The power of such proxy relies on the orders-of-magnitude difference in 10Be/9Be ratios between continental Be and Be dissolved in seawater. On riverine and marine sediments collected along a Chilean margin transect we chemically extracted reactive phases and separated the clay-sized sediment fraction. We compare the riverine and marine 10Be/9Be ratio of this fraction. Moreover, we compare the elemental and mineralogical composition and the Nd and Sr-isotopic composition of these samples. 10Be/9Be ratios increase four-fold from riverine to marine sediment. We attribute this increase to the incorporation of Be high in 10Be/9Be from dissolved biogenic opal, which also serves as a Si-source for the precipitation of marine authigenic clays. 10Be/9Be ratios thus sensitively track reverse-weathering reactions forming marine authigenic clays.
    Keywords: 10Be; authigenic clay; beryllium; Cosmogenic nuclide; denudation; reverse weathering
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-05-08
    Description: Planktic foraminiferal oxygen isotopes, Mg/Ca and Mg/Ca-derived SST estimates of sediment core SO256_29-1 (GeoB22229-1). Oxygen isotope analyses were carried out by the isotope laboratory of MARUM, University of Bremen, on a Finnigan MAT 251 mass spectrometer, which is connected with automatic lines for carbonate preparation. Isotope data were calibrated against the international Vienna Pee Dee Belemnite (VPDB) standard by using an in‐house carbonate standard, which has been calibrated to the National Bureau of Standards 19 standard. The long‐term analytical standard deviation is below ±0.07‰. Sample preparation for Mg/Ca followed the procedure of Barker et al. (2003, doi:10.1029/2003GC000559). Mg/Ca measurements were performed at MARUM, University of Bremen, on an Agilent Technologies 700 Series Inductively Coupled Plasma Optical Emission Spectrophotometer (ICP-OES), which is connected to a Cetax ASX 520 autosampler. To convert Mg/Ca to temperature, we applied the species-specific Mg/Ca-temperature calibration of Anand et al. (2003; doi:10.1029/2002PA000846) with an assumed exponential constant of 0.09.
    Keywords: AGE; Calculated from Mg/Ca ratios (Anand et al., 2003); Center for Marine Environmental Sciences; Coral Sea; DEPTH, sediment/rock; GC; GeoB22229-1; Globigerinoides ruber, Magnesium/Calcium ratio; Globigerinoides ruber, δ18O; Gravity corer; MARUM; Mass spectrometer Finnigan MAT 251; Mg/Ca; radiocarbon ages; Sea surface temperature; SO256; SO256_29-1; Sonne_2; TACTEAC; UK'37
    Type: Dataset
    Format: text/tab-separated-values, 202 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-05-08
    Description: Planktic foraminiferal oxygen isotopes, Mg/Ca and Mg/Ca-derived SST estimates of sediment core SO256_29-1 (GeoB22229-1). Oxygen isotope analyses were carried out by the isotope laboratory of MARUM, University of Bremen, on a Finnigan MAT 251 mass spectrometer, which is connected with automatic lines for carbonate preparation. Isotope data were calibrated against the international Vienna Pee Dee Belemnite (VPDB) standard by using an in‐house carbonate standard, which has been calibrated to the National Bureau of Standards 19 standard. The long‐term analytical standard deviation is below ±0.07‰. Sample preparation for Mg/Ca followed the procedure of Barker et al. (2003, doi:10.1029/2003GC000559). Mg/Ca measurements were performed at MARUM, University of Bremen, on an Agilent Technologies 700 Series Inductively Coupled Plasma Optical Emission Spectrophotometer (ICP-OES), which is connected to a Cetax ASX 520 autosampler. To convert Mg/Ca to temperature, we applied the species-specific Mg/Ca-temperature calibration of Anand et al. (2003; doi:10.1029/2002PA000846) with an assumed exponential constant of 0.09.
    Keywords: AGE; Calculated from Mg/Ca ratios (Anand et al., 2003); Center for Marine Environmental Sciences; Coral Sea; DEPTH, sediment/rock; GC; GeoB22229-1; Globigerinoides ruber, Magnesium/Calcium ratio; Globigerinoides ruber, δ18O; Gravity corer; MARUM; Mass spectrometer Finnigan MAT 251; Mg/Ca; radiocarbon ages; Sea surface temperature; SO256; SO256_29-1; Sonne_2; TACTEAC; UK'37
    Type: Dataset
    Format: text/tab-separated-values, 565 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
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