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PANGAEA.
Data Publisher for Earth & Environmental Science

Curry, William B; Duplessy, Jean-Claude; Labeyrie, Laurent D; Shackleton, Nicholas J (2006): Sedimentology on core EN066-36PG [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.357352, In supplement to: Sarnthein, Michael; Winn, Kyaw; Duplessy, Jean-Claude; Fontugne, Michel R (1988): Global variations of surface ocean productivity in low and mid latitudes: influence on CO2 reservoirs of the deep ocean and atmosphere during the last 21,000 years. Paleoceanography, 3(3), 361-399, https://doi.org/10.1029/PA003i003p00361

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Coverage:
Latitude: 4.305000 * Longitude: -20.212000
Date/Time Start: 1981-05-30T00:00:00 * Date/Time End: 1981-05-30T00:00:00
Minimum DEPTH, sediment/rock: 0.04 m * Maximum DEPTH, sediment/rock: 0.80 m
Event(s):
EN066-36PG (0036PG) * Latitude: 4.305000 * Longitude: -20.212000 * Date/Time: 1981-05-30T00:00:00 * Elevation: -4095.0 m * Campaign: EN06601 * Basis: Endeavor * Method/Device: Gravity corer (GC)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
Sedimentation rateSRcm/kaCurry, William BCalculated
Density, dry bulkDBDg/cm3Curry, William BCalculated from weight/volume
Paleoproductivity as carbonPP Cg/m2/aCurry, William BPP calculated (Sarnthein et al. 1992 in Summeshayes, Geol Soc Spec Pub 63)
Productivity of carbonPnewg/m2/aCurry, William BPP calculated (Sarnthein et al. 1992 in Summeshayes, Geol Soc Spec Pub 63)
Size:
74 data points

Data

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


Depth sed [m]

SR [cm/ka]

DBD [g/cm3]

PP C [g/m2/a]

Pnew [g/m2/a]
0.042.350.65120.9037.68
0.042.350.65120.9037.68
0.072.350.63116.6935.19
0.102.350.63103.9728.14
0.142.350.60116.2734.94
0.172.350.58121.2237.87
0.202.350.56118.5936.30
0.242.350.54116.4935.07
0.271.790.52110.0531.42
0.301.790.52109.4731.09
0.341.790.52114.3633.84
0.341.790.52114.3633.84
0.371.790.50111.4132.17
0.401.790.50117.1835.47
0.441.790.50122.0038.35
0.471.790.50122.3738.57
0.501.790.50120.4737.43
0.601.790.50
0.701.790.50
0.801.790.50