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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)
  • 8.2 ka event; Accumulation rate, biogenic silica per year; Accumulation rate per year; After Mortlock and Froelich (1981); biogenic opal; DEPTH, sediment/rock; GC; Gravity corer; Holocene; Labrador Sea; Labrador Shelf; Maria S. Merian; MSM45; MSM45_418-2; MSM45-19-2; Opal, biogenic silica; primary production  (1)
  • Denitrification
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Years
  • 1
    Publication Date: 2024-07-19
    Description: Biogenic opal (BSi) concentrations were analysed as indicator for past primary productivity on gravity core MSM45_19-2 from the northern Labrador Shelf. Gravity core MSM45_19-2 was obtained during R/V Maria S. Merian expedition MSM45 (58°45.68'N, 61°56.25'W, water depth: 202 m) in 2015 (Schneider et al., 2016). Biogenic opal was determined at Dalhousie University following the method of (Mortlock and Froelich , 1989). Briefly, amorphous silica was extracted from ca. 20 mg subsamples using a 2 M Na2 CO3 solution at 85°C for 5 h, followed by the measurement of dissolved silica concentrations by molybdenum blue spectrophotometry.
    Keywords: 8.2 ka event; Accumulation rate, biogenic silica per year; Accumulation rate per year; After Mortlock and Froelich (1981); biogenic opal; DEPTH, sediment/rock; GC; Gravity corer; Holocene; Labrador Sea; Labrador Shelf; Maria S. Merian; MSM45; MSM45_418-2; MSM45-19-2; Opal, biogenic silica; primary production
    Type: dataset
    Format: text/tab-separated-values, 655 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-07-22
    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
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  • 3
    Publication Date: 2024-07-22
    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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