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Martin, Pamela A; Lea, David W (1998): (Table 1) Cd/Ca and Mn/Ca ratios of benthic foraminifera of sediment core V30-49 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.857388, In supplement to: Martin, PA; Lea, DW (1998): Comparison of water mass changes in the deep tropical Atlantic derived from Cd/Ca and carbon isotope records: Implications for changing Ba composition of Deep Atlantic Water Masses. Paleoceanography, 13(6), 572-585, https://doi.org/10.1029/98PA02670

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Coverage:
Latitude: 18.433000 * Longitude: -21.080000
Date/Time Start: 1973-03-05T00:00:00 * Date/Time End: 1973-03-05T00:00:00
Minimum DEPTH, sediment/rock: 0.33 m * Maximum DEPTH, sediment/rock: 6.64 m
Event(s):
V30-49 * Latitude: 18.433000 * Longitude: -21.080000 * Date/Time: 1973-03-05T00:00:00 * Elevation: -3093.0 m * Recovery: 9.35 m * Campaign: V30 * Basis: Vema * Method/Device: Piston corer (PC)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmMartin, Pamela AGeocode
Cadmium/Calcium ratioCd/Caµmol/molMartin, Pamela AInductively coupled plasma - mass spectrometry (ICP-MS)Cibicidoides wuellerstorfi
Cadmium/Calcium ratioCd/Caµmol/molMartin, Pamela AInductively coupled plasma - mass spectrometry (ICP-MS)Uvigerina sp.
DifferenceDiffMartin, Pamela ACd/Ca C. wuellerstorfi - Uvigerina sp.
Manganese/Calcium ratioMn/Cammol/molMartin, Pamela AInductively coupled plasma - mass spectrometry (ICP-MS)Cibicidoides wuellerstorfi
Manganese/Calcium ratioMn/Cammol/molMartin, Pamela AInductively coupled plasma - mass spectrometry (ICP-MS)Uvigerina sp.
DifferenceDiffMartin, Pamela AMn/Ca C. wuellerstorfi - Uvigerina sp.
Size:
124 data points

Data

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


Depth sed [m]

Cd/Ca [µmol/mol]
(Cibicidoides wuellerstorfi)

Cd/Ca [µmol/mol]
(Uvigerina sp.)

Diff
(Cd/Ca C. wuellerstorfi - Uvig...)

Mn/Ca [mmol/mol]
(Cibicidoides wuellerstorfi)

Mn/Ca [mmol/mol]
(Uvigerina sp.)

Diff
(Mn/Ca C. wuellerstorfi - Uvig...)
0.330.0720.130-0.0580.0200.022-2
0.520.1100.142-0.0320.0580.04414
0.570.1470.1420.0050.0770.00374
0.640.1500.176-0.0260.063
0.930.1520.197-0.0450.1020.07230
0.990.1440.1430.0010.1340.05777
2.270.1960.1170.0790.2100.023187
2.400.1700.1070.0630.1910.019172
2.900.1380.1150.0230.1920.043149
3.340.1360.143-0.0070.0880.07117
3.570.1670.1080.0590.1960.027169
4.190.1400.1260.0140.1280.05672
4.400.1260.1210.0050.1900.058132
5.100.1290.1110.0180.2080.086122
5.440.1350.1120.0230.1520.05993
5.540.1360.1100.0260.1980.094104
5.690.1570.1190.0380.1830.08499
5.920.1010.118-0.0170.1790.15227
6.120.1630.1580.0050.1710.07794
6.510.1260.1230.0030.1850.060125
6.640.1090.133-0.0240.2200.092128