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Data Publisher for Earth & Environmental Science

Frank, Martin (2002): Accumulation rate and vertical rain rate of sediment core PS1772-8 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.81100

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Related to:
Frank, Martin; Gersonde, Rainer; Mangini, Augusto (1999): Sediment redistribution, 230Thex - nomalization and implications for the reconstruction of particle flux and export productivity. In: Fischer, G & Wefer, G (eds.), Use of Proxies in Paleoceanography - Examples from the South Atlantic, Springer, Berlin, Heidelberg, 409-426
Coverage:
Latitude: -55.458330 * Longitude: 1.163330
Date/Time Start: 1989-11-13T16:25:00 * Date/Time End: 1989-11-13T16:25:00
Minimum DEPTH, sediment/rock: 0.06 m * Maximum DEPTH, sediment/rock: 6.35 m
Event(s):
PS1772-8 (PS16/321) * Latitude: -55.458330 * Longitude: 1.163330 * Date/Time: 1989-11-13T16:25:00 * Elevation: -4137.0 m * Recovery: 13.3 m * Location: Atlantic Ridge * Campaign: ANT-VIII/3 (PS16) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 14 core sections: 0-0.4, 0.4-1.41, 1.41-2.41, 2.41-3.41, 3.41-4.41, 4.41-5.41, 5.41-6.41, 6.41-7.41, 7.41-8.41, 8.41-9.4, 9.4-10.4, 10.4-11.4, 11.4-12.4, 12.4-13.3 m
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
Accumulation rate, massMARg/cm2/kaFrank, MartinCalculated
Accumulation rate, sediment, standard deviationMAR std dev±Frank, MartinCalculated
Vertical rain rateRain rateg/cm2/kaFrank, Martin
Vertical rain rate, standard deviationRain rate std dev±Frank, Martin
Size:
276 data points

Data

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


Depth sed [m]

MAR [g/cm2/ka]

MAR std dev [±]

Rain rate [g/cm2/ka]

Rain rate std dev [±]
0.060.530.020.880.03
0.120.490.020.840.03
0.170.430.010.720.02
0.231.580.050.770.02
0.281.540.050.740.02
0.361.630.050.790.03
0.451.750.060.850.03
0.551.900.110.920.05
0.650.260.010.980.04
0.750.250.010.940.04
0.850.630.030.740.03
0.950.710.030.840.04
1.050.460.020.830.03
1.150.440.020.790.03
1.250.760.071.390.12
1.330.450.030.820.05
1.381.030.071.320.09
1.450.530.030.660.03
1.554.240.425.480.54
1.655.530.707.150.91
1.743.270.324.230.41
1.853.841.024.971.32
1.954.530.895.851.15
2.054.851.026.271.32
2.155.620.757.270.97
2.254.010.765.180.98
2.354.371.265.651.63
2.454.480.645.790.83
2.556.010.757.770.97
2.653.610.734.660.94
2.754.680.486.040.62
2.855.091.166.581.50
2.954.591.215.931.57
3.053.860.304.980.39
3.155.580.627.210.81
3.254.210.795.441.02
3.354.331.365.601.75
3.451.380.151.770.19
3.552.360.293.040.38
3.651.030.081.200.09
3.750.690.030.790.04
3.850.680.050.780.06
3.950.680.040.770.04
4.050.660.030.760.04
4.150.780.060.900.07
4.250.850.100.980.12
4.351.010.071.160.08
4.450.720.050.820.05
4.550.590.030.670.04
4.650.520.040.620.05
4.750.460.020.550.03
4.850.710.050.860.07
4.950.700.050.850.06
5.050.670.050.810.07
5.150.760.080.920.10
5.250.760.090.920.10
5.350.510.060.830.09
5.450.550.080.900.13
5.550.600.100.990.17
5.650.600.080.990.13
5.750.530.070.880.12
5.850.520.090.860.15
5.930.840.181.120.24
5.980.810.151.080.20
6.030.870.131.170.17
6.081.670.432.260.58
6.151.570.292.120.39
6.251.570.572.110.77
6.350.610.070.810.09