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Imbrie, John D (2000): Sea surface temperature reconstruction from sediment core K708-001 (specmap.037) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.56355

Always quote citation above when using data! You can download the citation in several formats below.

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Related to:
Imbrie, John D; Boyle, Edward A; Clemens, Steven C; Duffy, A; Howard, William R; Kukla, George J; Kutzbach, J; Martinson, Douglas G; McIntyre, Andrew; Mix, Alan C; Molfino, Barbara; Morley, Joseph J; Peterson, Larry S; Pisias, Nicklas G; Prell, Warren L; Raymo, Maureen E; Shackleton, Nicholas J; Toggweiler, J Robbie (1992): On the structure and origin of major glaciation cycles; 1. Linear responses to Milankovitch forcing. Paleoceanography, 7(6), 701-738, https://doi.org/10.1029/92PA02253
Imbrie, John D; McIntyre, Andrew; Mix, Alan C (1989): Oceanic response to orbital forcing in the late Quaternary: observational and experimental strategies. In: Berger, A; Schneider, S H & Duplessy, J C (eds.), Climate and Geosciences, A Challenge for Science and Society in the 21th Century. Boston (Kluwer Academic), 121-164, https://doi.org/10.1007/978-94-009-2446-8_7
McIntyre, Andrew; Ruddiman, William F; Karlin, K; Mix, Alan C (1989): Surface water response of the Equatorial Atlantic Ocean to orbital forcing. Paleoceanography, 4(1), 19-55, https://doi.org/10.1029/PA004i001p00019
Further details:
Duffy, A; Imbrie, John D (1989): Summary of Specmap archive No. 1. Spectral Mapping Project (Mapping Species Variability in Global Climate) (SPECMAP), hdl:10013/epic.32169.d001
Coverage:
Latitude: 50.000000 * Longitude: -23.733300
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 13.60 m
Event(s):
K708-001 * Latitude: 50.000000 * Longitude: -23.733300 * Elevation: -4053.0 m * Method/Device: Piston corer (PC)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
Sea surface temperature, summerSST sum°CImbrie, John DTransfer function (Imbrie & Kipp, 1971, in Turekian, Yale Univ Press)
Sea surface temperature, winterSST win°CImbrie, John DTransfer function (Imbrie & Kipp, 1971, in Turekian, Yale Univ Press)
Size:
378 data points

Data

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


Depth sed [m]

SST sum [°C]

SST win [°C]
0.0017.0211.01
0.1017.6711.27
0.2018.6412.16
0.3017.6011.57
0.4016.8611.14
0.4517.2911.07
0.5016.1310.80
0.5514.949.46
0.5814.489.79
0.6013.538.80
0.6212.455.61
0.6513.619.21
0.7012.518.46
0.7214.008.36
0.7514.168.93
0.8010.235.46
0.8510.245.64
0.906.500.57
0.956.610.53
1.006.320.29
1.106.620.70
1.206.530.42
1.306.540.56
1.406.750.59
1.507.831.71
1.606.670.79
1.706.891.11
1.806.960.50
1.906.400.42
2.009.151.46
2.108.972.88
2.206.850.79
2.3014.547.85
2.4013.367.74
2.5013.256.66
2.607.471.67
2.706.880.58
2.809.942.76
2.909.822.56
3.0011.085.86
3.1013.577.74
3.2013.518.78
3.306.640.57
3.407.341.88
3.5010.754.75
3.6011.615.32
3.7014.448.67
3.8010.754.03
3.899.463.36
4.0010.704.78
4.1011.455.78
4.207.141.31
4.307.041.34
4.327.451.52
4.366.680.81
4.406.410.30
4.447.562.08
4.486.641.08
4.5210.155.21
4.5614.568.36
4.6016.909.80
4.6416.489.66
4.6816.679.69
4.7212.397.29
4.7616.459.77
4.8017.5110.17
4.8414.218.40
5.0021.0412.84
5.1013.889.04
5.2018.9213.80
5.3014.7610.48
5.4016.0411.91
5.5015.5210.86
5.6013.146.69
5.7012.255.84
5.8018.3111.13
5.9012.517.16
6.0014.697.54
6.1014.238.21
6.2016.289.82
6.3014.739.30
6.4021.1212.61
6.5015.979.02
6.6017.2910.89
6.7014.028.19
6.8014.999.44
6.9014.448.59
7.0016.539.87
7.1016.619.52
7.2012.377.63
7.3016.899.60
7.4015.7710.16
7.5015.3710.04
7.6010.205.08
7.7017.8010.75
7.8017.7911.15
7.8519.0411.83
7.9021.1013.40
7.9521.4313.14
8.0019.0212.16
8.0518.5812.03
8.1018.1911.71
8.1518.8512.24
8.2018.0512.12
8.2519.8813.13
8.3019.9313.26
8.3517.0211.32
8.4017.5311.80
8.4517.6211.06
8.4816.8710.92
8.5017.7811.10
8.5314.629.13
8.559.624.21
8.588.403.11
8.608.764.01
8.639.564.41
8.655.96-0.13
8.706.360.22
8.756.840.97
8.808.572.19
8.908.792.70
9.006.08-0.01
9.107.431.45
9.209.272.04
9.307.721.84
9.406.120.04
9.506.220.33
9.6010.536.17
9.708.883.84
9.8014.618.12
9.908.852.84
10.0012.864.98
10.108.472.69
10.207.411.56
10.3011.776.81
10.407.602.07
10.507.141.13
10.607.401.31
10.7016.3410.10
10.8017.1710.04
10.9014.217.84
11.0018.1610.90
11.1017.1410.74
11.2015.969.70
11.3017.6210.77
11.4019.2811.89
11.4516.369.47
11.5017.4210.76
11.5515.788.78
11.6018.4311.16
11.6418.4310.40
11.6817.679.84
11.7218.0110.14
11.7614.367.46
11.7811.345.91
11.808.052.49
11.826.780.81
11.847.221.39
11.869.153.93
11.887.982.57
11.907.311.88
11.927.111.58
11.947.662.25
11.969.343.46
11.9717.1110.39
12.0016.057.82
12.0414.557.39
12.0815.7010.12
12.1216.619.25
12.1615.899.18
12.2016.5810.76
12.2415.429.55
12.2814.637.43
12.3017.4610.11
12.3513.306.09
12.4016.538.50
12.4517.9710.81
12.5016.409.28
12.5519.6112.32
12.6017.7910.90
12.6519.4711.90
12.7010.074.87
12.7510.986.23
12.908.293.26
13.059.964.88
13.2514.917.16
13.3511.477.02
13.5011.946.01
13.608.612.23