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Blanchet, Cécile L; Tjallingii, Rik; Schleicher, Anja Maria; Schouten, Stefan; Frank, Martin; Brauer, Achim (2021): XRF elemental contents of sediment core POS362-2_73 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.930765, In: Blanchet, CL et al. (2021): XRF elemental contents, oxygen and carbon isotopes and biomarkers of sediment cores POS362-2_33, POS362-2_73 and POS362-2_99 [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.930796

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Abstract:
Ocean deoxygenation is a rising threat to marine ecosystems and food resources under present climate warming conditions. Organic-rich sapropel layers deposited in the Mediterranean Sea provide a natural laboratory to study the processes that have controlled the changes in seawater oxygen levels in the recent geological past. Our study is based on three sediment cores spanning the last 10 thousand years (10 kyr BP) and located on a bathymetric transect offshore the western distributaries of the Nile delta. These cores are partly to continuously laminated in the sections recording sapropel S1, which is indicative of bottom-water anoxia above the western Nile deep-sea fan. We used a combination of microfacies analyses and inorganic and organic geochemical measurements to reconstruct changes in oxygenation conditions at seasonal to millennial time-scales. The regular alternations of detrital, biogenic and chemogenic sublayers in the laminated sequences are interpreted in terms of seasonal changes. Our microfacies analyses reveal distinct summer floods and subsequent plankton blooms preceding the deposition of inorganic carbonates formed in the water-column during spring-early summer. The isotopic signature of these carbonates suggests year-round anoxic to euxinic bottom waters resulting in high levels of anaerobic remineralisation of organic matter and highlights their potential to reconstruct seawater chemistry at times when benthic fauna was absent. Synchronous changes in terrigenous input, primary productivity and past oxygenation dynamics on millennial time-scales obtained by our multi-proxy study show that runoff-driven eutrophication played a central role in driving rapid changes in oxygenation state of the entire Levantine Basin. Rapid fluctuations of oxygenation conditions in the upper 700 m water depth occurred above the Nile deep-sea fan between 10 and 6.5 ka BP while deeper cores recorded more stable anoxic conditions. These findings are further supported by other regional records and reveal time-transgressive changes in oxygenation state driven by rapid changes in primary productivity during a period of long-term deep-water stagnation.
Keyword(s):
deoxygenation; Geochemistry; Nile River; Sapropel S1
Supplement to:
Blanchet, Cécile L; Tjallingii, Rik; Schleicher, Anja Maria; Schouten, Stefan; Frank, Martin; Brauer, Achim (accepted): Deoxygenation dynamics above the western Nile deep-sea fan during sapropel S1 at seasonal to millenial time-scales. Climate of the Past, https://doi.org/10.5194/cp-2020-114
Coverage:
Latitude: 31.985360 * Longitude: 30.147230
Date/Time Start: 2008-02-21T13:52:00 * Date/Time End: 2008-02-21T13:52:00
Minimum DEPTH, sediment/rock: 0.07 m * Maximum DEPTH, sediment/rock: 5.38 m
Event(s):
POS362-2_73 * Latitude: 31.985360 * Longitude: 30.147230 * Date/Time: 2008-02-21T13:52:00 * Elevation: 570.0 m * Campaign: POS362/2 * Basis: Poseidon * Method/Device: Gravity corer (GC)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmBlanchet, Cécile LGeocode
AGEAgeka BPBlanchet, Cécile LGeocode
Age, errorAge e±Blanchet, Cécile L2s
log-ratiolog-ratioBlanchet, Cécile LLog ratio of sulfur over chlorine
log-ratiolog-ratioBlanchet, Cécile LLog ratio of potassium over titanium
log-ratiolog-ratioBlanchet, Cécile LLog ratio of titanium over calcium
ScoreScoreBlanchet, Cécile LZ-scored Log ratio of titanium over calcium
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
2595 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Depth sed [m]

Age [ka BP]

Age e [±]
(2s)

log-ratio
(Log ratio of sulfur over chlo...)

log-ratio
(Log ratio of potassium over t...)

log-ratio
(Log ratio of titanium over ca...)

Score
(Z-scored Log ratio of titaniu...)
0.070.030.08-1.64-0.40-0.57-0.46
0.080.040.09-1.64-0.40-0.54-0.40
0.090.040.10-1.65-0.39-0.58-0.48
0.100.050.11-1.65-0.41-0.46-0.26
0.110.050.13-1.64-0.44-0.300.02
0.120.060.14-1.65-0.47-0.200.19
0.130.060.15-1.66-0.46-0.260.09
0.140.070.16-1.66-0.46-0.270.08
0.150.070.17-1.65-0.45-0.32-0.01
0.160.100.19-1.67-0.45-0.35-0.06
0.170.160.22-1.65-0.45-0.33-0.03
0.180.210.27-1.67-0.45-0.300.03
0.190.260.33-1.63-0.39-0.62-0.54
0.200.310.40-1.64-0.35-0.81-0.88
0.210.360.43-1.62-0.30-0.96-1.14
0.220.410.43-1.60-0.32-0.90-1.04
0.230.460.44-1.60-0.26-1.09-1.37
0.240.510.46-1.60-0.26-1.06-1.32
0.250.560.49-1.60-0.31-1.03-1.26
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0.300.800.54-1.59-0.26-1.08-1.36
0.310.850.55-1.62-0.26-1.06-1.32
0.320.900.54-1.60-0.26-1.05-1.31
0.330.950.54-1.63-0.28-0.99-1.19
0.341.010.55-1.61-0.29-0.94-1.10
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0.361.110.57-1.62-0.29-0.93-1.10
0.371.160.56-1.63-0.29-0.91-1.06
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0.391.260.56-1.64-0.28-0.93-1.09
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0.441.500.55-1.60-0.21-1.15-1.48
0.451.550.56-1.56-0.15-1.32-1.78
0.461.600.56-1.54-0.12-1.39-1.91
0.471.640.54-1.53-0.15-1.33-1.79
0.481.680.53-1.53-0.09-1.50-2.11
0.491.730.53-1.49-0.06-1.58-2.24
0.501.770.54-1.49-0.05-1.59-2.25
0.511.810.53-1.49-0.06-1.54-2.17
0.521.850.52-1.47-0.06-1.54-2.17
0.531.890.51-1.49-0.05-1.57-2.22
0.541.930.50-1.49-0.04-1.59-2.27
0.551.970.51-1.51-0.02-1.63-2.34
0.562.010.50-1.47-0.02-1.61-2.30
0.572.050.48-1.48-0.03-1.59-2.27
0.582.090.47-1.49-0.01-1.64-2.35
0.592.120.47-1.49-0.01-1.63-2.33
0.602.160.47-1.50-0.02-1.61-2.30
0.612.200.46-1.51-0.03-1.61-2.29
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0.632.280.41-1.49-0.03-1.60-2.28
0.642.320.40-1.49-0.01-1.66-2.39
0.652.360.40-1.42-0.01-1.68-2.41
0.662.400.38-1.47-0.02-1.66-2.39
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0.772.970.27-1.410.06-1.85-2.71
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0.823.460.46-1.410.02-1.76-2.56
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0.944.130.60-1.51-0.13-1.31-1.77
0.954.160.62-1.51-0.13-1.30-1.75
0.964.200.61-1.52-0.15-1.25-1.66
0.974.240.62-1.52-0.17-1.19-1.55
0.984.280.62-1.49-0.14-1.28-1.70
0.994.310.64-1.53-0.17-1.18-1.54
1.004.350.65-1.52-0.17-1.19-1.54
1.014.390.64-1.52-0.19-1.13-1.45
1.024.430.64-1.51-0.20-1.10-1.40
1.034.470.65-1.52-0.20-1.10-1.39
1.044.510.65-1.54-0.21-1.09-1.38
1.054.540.66-1.53-0.22-1.04-1.29
1.064.580.66-1.55-0.22-1.04-1.29
1.074.620.66-1.53-0.21-1.05-1.31
1.084.660.67-1.55-0.21-1.06-1.32
1.094.700.68-1.56-0.20-1.10-1.38
1.104.730.69-1.55-0.22-1.04-1.28
1.114.770.68-1.52-0.22-1.01-1.24
1.124.810.68-1.50-0.23-0.98-1.19
1.134.860.68-1.54-0.23-0.96-1.15
1.144.900.69-1.55-0.23-0.96-1.14
1.154.930.70-1.55-0.23-0.97-1.17
1.164.970.69-1.54-0.24-0.88-1.01
1.175.010.69-1.54-0.24-0.91-1.05
1.185.050.69-1.56-0.25-0.89-1.02
1.195.090.70-1.52-0.25-0.87-0.99
1.205.130.71-1.52-0.25-0.87-0.98
1.215.170.70-1.54-0.25-0.85-0.96
1.225.210.70-1.52-0.25-0.86-0.97
1.235.250.70-1.52-0.24-0.86-0.97
1.245.290.71-1.49-0.24-0.87-0.99
1.255.330.71-1.51-0.25-0.86-0.97
1.265.370.70-1.50-0.25-0.86-0.97
1.275.410.69-1.52-0.26-0.83-0.92
1.285.450.69-1.48-0.25-0.84-0.93
1.295.490.69-1.51-0.25-0.83-0.91
1.305.530.69-1.52-0.24-0.85-0.95
1.315.560.68-1.51-0.24-0.84-0.93
1.325.600.67-1.48-0.24-0.83-0.92
1.335.640.67-1.50-0.24-0.82-0.89
1.345.680.68-1.52-0.25-0.82-0.90
1.355.720.68-1.50-0.26-0.78-0.82
1.365.760.67-1.50-0.26-0.75-0.77
1.375.800.66-1.51-0.26-0.74-0.75
1.385.840.66-1.51-0.27-0.72-0.73
1.395.880.66-1.49-0.27-0.72-0.73
1.405.920.67-1.49-0.27-0.71-0.70
1.415.960.65-1.49-0.28-0.66-0.62
1.426.000.64-1.49-0.28-0.63-0.57
1.436.040.64-1.49-0.28-0.66-0.62
1.446.080.63-1.48-0.27-0.67-0.63
1.456.120.63-1.48-0.27-0.68-0.65
1.466.160.61-1.48-0.27-0.71-0.70
1.476.200.60-1.48-0.27-0.65-0.60
1.486.240.59-1.48-0.27-0.65-0.59
1.496.280.59-1.47-0.27-0.68-0.64
1.506.320.59-1.45-0.27-0.62-0.54
1.516.360.57-1.44-0.28-0.62-0.54
1.526.400.56-1.45-0.28-0.56-0.44
1.536.440.55-1.40-0.29-0.53-0.39
1.546.480.55-1.41-0.29-0.53-0.38
1.556.520.55-1.42-0.29-0.51-0.35
1.566.560.53-1.41-0.30-0.48-0.29
1.576.600.51-1.40-0.30-0.47-0.29
1.586.640.50-1.37-0.30-0.46-0.26
1.596.680.50-1.37-0.30-0.44-0.23
1.606.720.50-1.35-0.31-0.42-0.20
1.616.750.47-1.34-0.31-0.44-0.22
1.626.790.45-1.33-0.31-0.42-0.19
1.636.830.43-1.32-0.31-0.41-0.18
1.646.870.42-1.33-0.31-0.37-0.10
1.656.910.42-1.28-0.32-0.32-0.02
1.666.950.38-1.25-0.32-0.32-0.01
1.676.980.35-1.25-0.32-0.300.01
1.687.020.33-1.24-0.32-0.32-0.01
1.697.060.31-1.21-0.33-0.270.07
1.707.100.31-1.20-0.33-0.250.12
1.717.120.28-1.22-0.33-0.270.08
1.727.150.27-1.18-0.33-0.230.15
1.737.170.25-1.21-0.33-0.170.25
1.747.200.25-1.21-0.33-0.200.21
1.757.220.25-1.22-0.34-0.130.31
1.787.270.22-1.10-0.34-0.230.15
1.797.290.22-1.18-0.33-0.190.21
1.807.300.21-1.20-0.34-0.190.22
1.817.310.20-1.13-0.33-0.250.12
1.827.320.18-1.20-0.33-0.270.08
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1.857.360.17-1.16-0.33-0.280.06
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1.877.370.17-1.10-0.33-0.180.23
1.887.370.17-1.03-0.33-0.250.11
1.897.380.17-1.10-0.34-0.260.10
1.907.380.17-1.05-0.34-0.220.16
1.917.390.17-1.03-0.33-0.300.03
1.927.390.17-1.04-0.34-0.230.14
1.937.400.17-1.00-0.34-0.160.26
1.947.400.17-0.97-0.35-0.100.38
1.957.410.17-1.04-0.35-0.150.29
1.967.410.17-1.02-0.35-0.110.36
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1.987.430.17-0.92-0.35-0.070.43
1.997.430.17-1.02-0.36-0.080.41
2.007.440.18-1.01-0.35-0.110.35
2.017.440.17-0.96-0.35-0.080.42
2.027.450.17-0.92-0.35-0.090.39
2.037.450.18-1.01-0.35-0.110.36
2.047.460.18-1.07-0.35-0.020.52
2.057.460.18-0.98-0.36-0.090.40
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2.077.470.18-0.95-0.360.000.55
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2.117.500.18-1.00-0.35-0.020.52
2.127.500.18-1.05-0.350.000.56
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2.147.510.18-1.12-0.360.000.56
2.157.520.18-1.13-0.350.010.56
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2.247.570.18-1.07-0.360.000.55
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2.267.580.18-1.08-0.35-0.010.54
2.277.590.18-1.06-0.360.030.61
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2.297.600.19-0.89-0.350.010.58
2.307.600.19-1.06-0.350.000.56
2.317.610.19-1.16-0.350.020.59
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2.367.640.19-1.12-0.35-0.020.52
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2.387.650.19-1.12-0.340.030.60
2.397.650.19-1.16-0.350.040.62
2.407.660.19-1.18-0.35-0.020.52
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2.427.670.19-1.19-0.340.020.59
2.437.670.19-1.10-0.340.000.55
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2.467.690.19-1.25-0.340.060.66
2.477.700.19-1.25-0.340.060.65
2.487.700.19-1.26-0.340.020.59
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2.537.730.19-1.26-0.340.090.71
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2.567.750.19-1.29-0.350.070.67
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2.597.760.19-1.27-0.350.060.67
2.607.770.19-1.25-0.350.060.66
2.617.770.19-1.28-0.340.050.64
2.627.780.19-1.28-0.340.050.63
2.637.780.19-1.28-0.340.040.62
2.647.790.20-1.27-0.350.030.61
2.657.800.19-1.30-0.34-0.020.52
2.667.800.19-1.29-0.33-0.040.48
2.677.810.19-1.27-0.33-0.080.42
2.687.810.19-1.28-0.32-0.130.32
2.697.810.20-1.31-0.31-0.170.25
2.707.820.20-1.27-0.30-0.230.15
2.717.820.20-1.30-0.31-0.210.19
2.727.830.20-1.28-0.32-0.170.25
2.737.830.20-1.29-0.31-0.190.22
2.747.840.20-1.28-0.32-0.160.26
2.757.840.21-1.22-0.32-0.160.28
2.767.850.21-1.22-0.32-0.110.36
2.807.870.21-1.04-0.37-0.050.47
2.817.870.22-1.02-0.35-0.120.34
2.827.880.22-1.00-0.34-0.130.33
2.837.880.22-1.02-0.35-0.020.52
2.847.890.22-1.01-0.36-0.010.53
2.857.890.22-0.77-0.36-0.020.51
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2.877.900.23-1.05-0.35-0.050.46
2.887.910.23-1.01-0.35-0.090.39
2.897.910.23-1.02-0.34-0.150.29
2.907.920.23-1.05-0.34-0.230.14
2.917.920.23-1.00-0.36-0.110.36
2.927.930.23-0.99-0.35-0.140.31
2.937.930.24-1.02-0.36-0.010.54
2.947.940.24-1.02-0.360.000.55
2.957.940.24-0.98-0.360.130.78
2.967.950.24-1.02-0.370.050.64
2.977.950.24-1.00-0.370.130.78
2.987.960.24-1.02-0.370.080.69
2.997.960.25-1.01-0.370.060.66
3.007.970.25-0.97-0.360.030.61
3.017.970.25-0.98-0.360.110.75
3.027.980.25-0.99-0.36-0.050.47
3.037.980.25-0.97-0.36-0.210.19
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