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Lea, David W (1989): Ba/Ca ratios in benthic foraminifera from recent core tops [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.399803, Supplement to: Lea, David W; Boyle, Edward A (1989): Barium content of benthic foraminifera controlled by bottom-water composition. Nature, 338, 751-753, https://doi.org/10.1038/338751a0

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Abstract:
The carbon isotope ratio (delta13C) and cadmium content (Cd/Ca) of benthic foraminifera shells have been used to reconstruct deep-water circulation patterns of the glacial oceans. These tracers co-vary with phosphorus in the modern ocean because they are nearly quantitatively regenerated from sinking biological debris in the upper water column. Hence they can be used to reconstruct the distribution of labile nutrients in glacial water masses. Independent constraints on glacial deep-ocean circulation patterns could be provided by a tracer of the distribution of silica and alkalinity, the deeply regenerated constituents of planktonic hard parts. Barium shares key aspects of its behaviour with these refractory nutrients because it is removed from solution in surface waters and incorporated into sinking particles which slowly dissolve deep in the water column and in the sediments. The fractionation of Ba between deep-water masses of the major ocean basins is largely controlled by thermohaline circulation patterns, so Ba conforms to different boundary conditions from Cd and 13C. As Ba substitutes into trigonal carbonates, it is a potential palaeoceano-graphic tracer if the Ba content of foraminifera shells reflects ambient dissolved Ba concentrations. Here we present data from Recent core-top benthic foraminifera which indicate that the Ba content of some recent calcitic benthic foraminifera does co-vary with bottom-water Ba.
Coverage:
Median Latitude: 12.677898 * Median Longitude: -21.743405 * South-bound Latitude: -54.550000 * West-bound Longitude: -106.183300 * North-bound Latitude: 78.000000 * East-bound Longitude: 158.800000
Minimum DEPTH, sediment/rock: 0.010 m * Maximum DEPTH, sediment/rock: 0.160 m
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
LATITUDELatitudeGeocode
LONGITUDELongitudeGeocode
Sample code/labelSample labelLea, David W* denotes cores with > 15 cm Holocene sediment
DEPTH, sediment/rockDepth sedmGeocode
Depth, top/minDepth topmLea, David W
Depth, bottom/maxDepth botmLea, David W
Depth, bathymetricBathy depthmLea, David W
BariumBaµmol/lLea, David W
Barium/Calcium ratioBa/Caµmol/molLea, David WCibicidoides wuellerstorfi
10 Standard deviationStd dev±Lea, David WCibicidoides wuellerstorfi
11 Barium/Calcium ratioBa/Caµmol/molLea, David WCibicidoides kullenbergi
12 Standard deviationStd dev±Lea, David WCibicidoides kullenbergi
13 Barium/Calcium ratioBa/Caµmol/molLea, David WUvigerina spp.
14 Standard deviationStd dev±Lea, David WUvigerina spp.
Size:
288 data points

Data

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


Latitude

Longitude

Sample label
(* denotes cores with > 15 cm ...)

Depth sed [m]

Depth top [m]

Depth bot [m]

Bathy depth [m]

Ba [µmol/l]

Ba/Ca [µmol/mol]
(Cibicidoides wuellerstorfi)
10 
Std dev [±]
(Cibicidoides wuellerstorfi)
11 
Ba/Ca [µmol/mol]
(Cibicidoides kullenbergi)
12 
Std dev [±]
(Cibicidoides kullenbergi)
13 
Ba/Ca [µmol/mol]
(Uvigerina spp.)
14 
Std dev [±]
(Uvigerina spp.)
-54.5500-77.8500V18-68*0.1100.100.1239720.1133.433.94
-43.516779.8667RC11-1200.0600.050.0731350.0933.41
-32.0333-36.1833All107 65GGC0.0550.040.0727950.0662.15
-31.9167-36.2000All107 67GGC0.0100.000.0225870.0651.890.06
-31.6667-36.0167All107 69GGC0.0600.050.0721580.0682.26
-31.6000-35.9833All107 70GGC0.0300.020.0420790.0682.202.04
-31.5167-35.9333All107 71GGC0.0100.000.0218870.0702.242.00
-29.3167-86.2333TR163-280.0150.010.0232000.1384.09
-10.0667-12.8167V22-174*0.1000.090.1126300.0781.94
-7.4167-89.1667All54 5PG0.0300.020.0441650.1364.184.16
-3.9500-85.9667TR163-31B*0.0600.010.1132100.1364.410.244.504.020.47
-2.4833-82.9833TR163-320.0300.020.0428900.1375.043.930.15
-2.2500-86.5833TR163-270.0250.020.0331800.1384.66
-0.3667-106.1833KNR73 3PC*0.0550.050.0636060.1374.95
0.4333158.8000V24-1090.0650.050.0823670.1393.76
2.4667-19.7333EN66 32GGC*0.0150.000.0350030.0793.00
3.0833-20.0167EN66 26GGC0.0200.010.0347450.0792.86
4.2333-20.6333EN66 21GGC*0.0750.030.1239950.0772.752.35
4.3167-20.2167EN66 36GGC0.0250.020.0342700.0772.45
4.9167-20.5000EN66 38GGC0.0300.020.0429310.0732.312.392.56
5.2667-21.7167EN66 44GGC0.0150.010.0234280.0752.892.72
5.4667-21.1333EN66 16GGC0.0200.010.0331520.0752.792.87
5.6833-87.2333TR163-140.0400.030.0523650.1354.12
6.6500-21.9000EN66 10GGC0.0150.010.0235270.0762.582.28
14.1667-18.5833V22-197*0.1550.140.1731670.0743.102.80
14.5833-19.6667V22-1980.0500.040.0610820.0642.52
16.5333-74.8000KNR64 5PG0.0700.060.0830470.0572.262.42
28.5333134.1333V28-3040.0750.060.0929420.1423.69
31.9000-64.3000OC173 G0.0500.040.0644690.0672.160.10
36.10007.1667CHN82 1PC0.0300.020.048300.0482.18
41.6333-27.3333CHN82 3PC0.1450.130.1625250.0521.77
41.7167-32.8500CHN82 4PC*0.0100.000.0234270.0572.442.260.01
41.8500-26.4500CHN82 9PC0.0850.070.1028300.0531.85
42.3833-31.8000CHN82 11PC*0.0350.010.0632090.0562.252.180.06
42.3833-23.516710S82 PCS010.0300.020.0435400.0632.54
43.2333-28.1333CHN82 15PC0.0400.030.0521550.0511.980.022.630.16
43.2833-29.8333CHN82 21PC0.0600.040.0821030.0501.922.67
43.5000-29.8667CHN82 20PC*0.0550.040.0730700.0541.822.520.04
48.6667147.4000V32-1590.1600.150.1712350.1122.94
66.60001.1167V27-86*0.0650.050.0829000.0521.90
68.0333-6.1167V28-560.0350.030.0429410.0521.97
72.18338.5667V27-600.0650.050.0825250.0502.11
78.00002.4167PS21295-4*0.0150.010.0231120.0472.03