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Carpentier, Marion; Chauvel, Catherine; Mattielli, Nadine (2008): (Table 1) Trace element concentrations and Nd and Pb isotope ratios of sediment samples from Barbados Island [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.716566, In supplement to: Carpentier, M et al. (2008): Pb–Nd isotopic constraints on sedimentary input into the Lesser Antilles arc system. Earth and Planetary Science Letters, 272(1-2), 199-211, https://doi.org/10.1016/j.epsl.2008.04.036

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Coverage:
Median Latitude: 13.239157 * Median Longitude: -59.539879 * South-bound Latitude: 13.183300 * West-bound Longitude: -59.575000 * North-bound Latitude: 13.298300 * East-bound Longitude: -59.471700
Comment:
Nd isotope ratios are relative to the value recommended by Chauvel and Blichert-Toft (2001, doi:10.1016/S0012-821X(01)00379-X) for the Rennes Nd standard (143Nd/144Nd = 0.511961, which corresponds to a La Jolla value of 0.511856). Uncertainties reported on the Nd isotope ratios are in-run errors (2 sigma), where sigma is the standard deviation and n the number of measured 143Nd/144Nd ratios, generally 60). The Rennes Nd standard was run every second sample and its reproducibility (2sigma) calculated on each analyses session (~20 analyses) is typically 30 ppm. Reproducibility calculated using complete duplicate analyses of 7 samples is 1.2 * 10**-5 (2 sigma) on the measured 143Nd/144Nd ratio (25 ppm) and is better than the average in-run errors. Pb isotope ratios are relative to NBS 981 values of 206Pb/204Pb = 16.9405, 207Pb/204Pb = 15.4963 and 208Pb/204Pb = 36.7219 (Galer and Abouchami, 1998). The NBS 981 standard was run every second sample and its reproducibility (2 sigma) calculated on the entire period of analyses is 150, 180 and 200 ppm for 206Pb/204Pb, 207Pb/204Pb and 208Pb/204Pb ratios respectively (106 analysis). Reproducibility calculated using complete duplicate analyses of 8 samples, excluding the 4 duplicates of black shales (Site 144 - Unit 3), is 0.007 (370 ppm), 0.002 (130 pm) and 0.011 (300 ppm) for 206Pb/204Pb, 207Pb/204Pb and 208Pb/204Pb ratios respectively (2 sigma). The reproducibility of the black shale duplicates is not as good probably because of the strong heterogeneities of these samples.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
LATITUDELatitudeGeocode
LONGITUDELongitudeGeocode
Sample code/labelSample labelCarpentier, Marion
FormationFormationCarpentier, Marion
Sample commentSample commentCarpentier, MarionDR = duplicate run
NeodymiumNdmg/kgCarpentier, MarionInductively coupled plasma - mass spectrometry (ICP-MS)
SamariumSmmg/kgCarpentier, MarionInductively coupled plasma - mass spectrometry (ICP-MS)
LeadPbmg/kgCarpentier, MarionInductively coupled plasma - mass spectrometry (ICP-MS)
ThoriumThmg/kgCarpentier, MarionInductively coupled plasma - mass spectrometry (ICP-MS)
10 UraniumUmg/kgCarpentier, MarionInductively coupled plasma - mass spectrometry (ICP-MS)
11 Neodymium-143/Neodymium-144 ratio143Nd/144NdCarpentier, MarionAnion resin technique (Manhès et al. 1984)
12 Neodymium-143/Neodymium-144 ratio, error143Nd/144Nd e±Carpentier, MarionAnion resin technique (Manhès et al. 1984)2 sigma
13 Lead-206/Lead-204 ratio206Pb/204PbCarpentier, MarionAnion resin technique (Manhès et al. 1984)
14 Lead-206/Lead-204 ratio, error206Pb/204Pb e±Carpentier, MarionAnion resin technique (Manhès et al. 1984)2 sigma
15 Lead-207/Lead-204 ratio207Pb/204PbCarpentier, MarionAnion resin technique (Manhès et al. 1984)
16 Lead-207/Lead-204 ratio, error207Pb/204Pb e±Carpentier, MarionAnion resin technique (Manhès et al. 1984)2 sigma
17 Lead-208/Lead-204 ratio208Pb/204PbCarpentier, MarionAnion resin technique (Manhès et al. 1984)
18 Lead-208/Lead-204 ratio, error208Pb/204Pb e±Carpentier, MarionAnion resin technique (Manhès et al. 1984)2 sigma
Size:
186 data points

Data

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


Latitude

Longitude

Sample label

Formation

Sample comment

Nd [mg/kg]

Sm [mg/kg]

Pb [mg/kg]

Th [mg/kg]
10 
U [mg/kg]
11 
143Nd/144Nd
12 
143Nd/144Nd e [±]
13 
206Pb/204Pb
14 
206Pb/204Pb e [±]
15 
207Pb/204Pb
16 
207Pb/204Pb e [±]
17 
208Pb/204Pb
18 
208Pb/204Pb e [±]
13.1833-59.4717B-1Oceanic Fm11.003.415.302.012.10019.53290.001615.69750.001138.8420.003
13.1833-59.4717B-2Oceanic Fm13.503.975.523.102.8700.5130450.00001519.63360.001215.70390.001438.8550.003
13.1833-59.4717B-4Oceanic Fm19.004.188.575.381.5500.5123870.00001919.34420.001215.72740.001239.1610.004
13.2983-59.5750B-7Oceanic Fm7.651.682.962.070.4560.5122400.00001919.25610.003015.72900.002639.1410.007
13.2433-59.5533B-6Upper Scotland Fm17.303.587.825.561.6900.5120890.00001619.51560.001115.74440.001039.3200.003
13.2367-59.5433B-10bUpper Scotland Fm77.9018.209.307.863.5900.5120800.00002120.74330.001715.87900.001440.0370.004
13.2367-59.5433B-10bDR0.5121110.000010
13.2367-59.5433B-10cUpper Scotland Fm29.605.2114.0012.202.8500.5120140.00001019.87780.001215.79300.001139.7100.003
13.2367-59.5433B-10cDR0.5119980.000011
13.2433-59.5483B-11Upper Scotland Fm29.605.8218.8012.603.6100.5120410.00001919.98320.001515.80150.001339.6430.004
13.2750-59.5750B-8cLower Scotland Fm23.604.7513.307.742.5700.5121270.00002119.52240.001315.74200.000939.3480.003
13.2750-59.5750B-8dLower Scotland Fm32.506.1018.9013.503.1600.5120910.00001619.61530.000915.75870.001039.4030.003
13.2583-59.5717B-12aLower Scotland Fm30.105.7121.0012.502.5300.5122170.00001419.39100.001715.73530.001239.3010.003
13.2583-59.5717B-12bLower Scotland Fm29.405.6420.1013.103.8900.5121740.00001819.46300.001315.74040.001139.3470.003