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Foster, Gavin L; Lear, Caroline H; Rae, James W B (2012): (Table S1) Boron isotope and trace element data and reconstructed carbonate system parameters, ODP Holes 122-761B and 154-926A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.815855, Supplement to: Foster, GL et al. (2012): The evolution of pCO2, ice volume and climate during the middle Miocene. Earth and Planetary Science Letters, 341-344, 243-254, https://doi.org/10.1016/j.epsl.2012.06.007

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Abstract:
The middle Miocene Climatic Optimum (17-15 Ma; MCO) is a period of global warmth and relatively high CO2 and is thought to be associated with a significant retreat of the Antarctic Ice Sheet (AIS). We present here a new planktic foraminiferal d11B record from 16.6 to 11.8 Ma from two deep ocean sites currently in equilibrium with the atmosphere with respect to CO2. These new data demonstrate that the evolution of global climate during the middle Miocene (as reflected by changes in the cyrosphere) was well correlated to variations in the concentration of atmospheric CO2. What is more, within our sampling resolution (~1 sample per 300 kyr) there is no evidence of hysteresis in the response of ice volume to CO2 forcing during the middle Miocene, contrary to what is understood about the Antarctic Ice Sheet from ice sheet modelling studies. In agreement with previous data, we show that absolute levels of CO2 during the MCO were relatively modest (350-400 ppm) and levels either side of the MCO are similar or lower than the pre-industrial (200-260 ppm). These new data imply the presence of either a very dynamic AIS at relatively low CO2 during the middle Miocene or the advance and retreat of significant northern hemisphere ice. Recent drilling on the Antarctic margin and shore based studies indicate significant retreat and advance beyond the modern limits of the AIS did occur during the middle Miocene, but the complete loss of the AIS was unlikely. Consequently, it seems that ice volume and climate variations during the middle Miocene probably involved a more dynamic AIS than the modern but also some component of land-based ice in the northern hemisphere.
Further details:
Horita, Juske; Zimmermann, Heide; Holland, Heinrich D (2002): Chemical evolution of seawater during the Phanerozoic. Geochimica et Cosmochimica Acta, 66(21), 3733-3756, https://doi.org/10.1016/S0016-7037(01)00884-5
Project(s):
Coverage:
Median Latitude: -6.508950 * Median Longitude: 36.313450 * South-bound Latitude: -16.737000 * West-bound Longitude: -42.908100 * North-bound Latitude: 3.719100 * East-bound Longitude: 115.535000
Date/Time Start: 1988-07-19T10:00:00 * Date/Time End: 1994-02-21T10:30:00
Minimum DEPTH, sediment/rock: 37.3 m * Maximum DEPTH, sediment/rock: 290.8 m
Event(s):
122-761B  * Latitude: -16.737000 * Longitude: 115.535000 * Date/Time Start: 1988-07-19T10:00:00 * Date/Time End: 1988-07-21T09:00:00 * Elevation: -2179.0 m * Penetration: 286.7 m * Recovery: 199.08 m * Location: South Indian Ridge, South Indian Ocean * Campaign: Leg122 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 33 cores; 286.7 m cored; 0 m drilled; 69.4 % recovery
154-926A  * Latitude: 3.719100 * Longitude: -42.908100 * Date/Time Start: 1994-02-19T11:30:00 * Date/Time End: 1994-02-21T10:30:00 * Elevation: -3610.0 m * Penetration: 327 m * Recovery: 334.92 m * Location: South Atlantic Ocean * Campaign: Leg154 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 35 cores; 327 m cored; 0 m drilled; 102.4 % recovery
Comment:
Sediment depth is given in mcd. Carbonate system parameters calculated using d11B(seawater) = 37.82 per mil and ALK(surface) = 1292 mmol/kg and ALK(deep) = 1392 mmol/kg. All carbonate system calculations were carried out accounting for the effect of changing [Ca] and [Mg] on K1, K2 and Ksp.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEvent
Sample code/labelSample labelFoster, Gavin LDSDP/ODP/IODP sample designation
DEPTH, sediment/rockDepth sedmGeocode
AGEAgeka BPGeocode
SpeciesSpeciesFoster, Gavin L
Globigerinoides sacculifer, Magnesium/Calcium ratioG. sacculifer Mg/Cammol/molFoster, Gavin LICP-MS, Thermo Fisher Scientific, Element 2
Cibicidoides wuellerstorfi, Magnesium/Calcium ratioC. wuellerstorfi Mg/Cammol/molFoster, Gavin LICP-MS, Thermo Fisher Scientific, Element 2
Cibicidoides mundulus, Magnesium/Calcium ratioC. mundulus Mg/Cammol/molFoster, Gavin LICP-MS, Thermo Fisher Scientific, Element 2
δ11Bδ11B‰ SRMFoster, Gavin LMC-ICP-MS, Thermo Fisher Scientific NEPTUN#1
10 Standard errorStd e±Foster, Gavin LMC-ICP-MS, Thermo Fisher Scientific NEPTUNd11B 2 se, #1
11 BoronBmg/kgFoster, Gavin LMC-ICP-MS, Thermo Fisher Scientific NEPTUN#1
12 δ11Bδ11B‰ SRMFoster, Gavin LMC-ICP-MS, Thermo Fisher Scientific NEPTUN#2
13 Standard errorStd e±Foster, Gavin LMC-ICP-MS, Thermo Fisher Scientific NEPTUNd11B 2 se, #2
14 BoronBmg/kgFoster, Gavin LMC-ICP-MS, Thermo Fisher Scientific NEPTUN#2
15 δ11Bδ11B‰ SRMFoster, Gavin LMC-ICP-MS, Thermo Fisher Scientific NEPTUNaverage of two repeat measurements
16 δ11B, standard deviationδ11B std dev±Foster, Gavin LMC-ICP-MS, Thermo Fisher Scientific NEPTUN2 sd of average of two repeat measurements
17 Temperature, calculatedT cal°CFoster, Gavin LCalculatedfrom Mg/Ca using equations and the Mg/Ca ratio of seawater from Horita et al. (2002)
18 pHpHFoster, Gavin LCalculatedtotal scale
19 ErrorErrorFoster, Gavin LCalculateduncertainty due to measurement uncertainty on d11B determination
20 Carbonate ion[CO3]2-µmol/kgFoster, Gavin LCalculated
21 Carbonate ion, standard deviation[CO3]2- std dev±Foster, Gavin LCalculatedsummed uncertainty due to ± 200 mmol/kg total alkalinity and ± uncertainty in d11B, for pCO2 this also includes an uncertainty due to temperature
22 Carbon dioxide, partial pressurepCO2ppmvFoster, Gavin LCalculated
23 Carbon dioxide, partial pressure, standard deviationpCO2 std dev±Foster, Gavin LCalculated+ 2 sigma
24 Carbon dioxide, partial pressure, standard deviationpCO2 std dev±Foster, Gavin LCalculated- 2 sigma
Size:
342 data points

Data

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


Event

Sample label
(DSDP/ODP/IODP sample designation)

Depth sed [m]

Age [ka BP]

Species

G. sacculifer Mg/Ca [mmol/mol]
(ICP-MS, Thermo Fisher Scienti...)

C. wuellerstorfi Mg/Ca [mmol/mol]
(ICP-MS, Thermo Fisher Scienti...)

C. mundulus Mg/Ca [mmol/mol]
(ICP-MS, Thermo Fisher Scienti...)

δ11B [‰ SRM]
(#1, MC-ICP-MS, Thermo Fisher ...)
10 
Std e [±]
(d11B 2 se, #1, MC-ICP-MS, The...)
11 
B [mg/kg]
(#1, MC-ICP-MS, Thermo Fisher ...)
12 
δ11B [‰ SRM]
(#2, MC-ICP-MS, Thermo Fisher ...)
13 
Std e [±]
(d11B 2 se, #2, MC-ICP-MS, The...)
14 
B [mg/kg]
(#2, MC-ICP-MS, Thermo Fisher ...)
15 
δ11B [‰ SRM]
(average of two repeat measure...)
16 
δ11B std dev [±]
(2 sd of average of two repeat...)
17 
T cal [°C]
(from Mg/Ca using equations an...)
18 
pH
(total scale, Calculated)
19 
Error
(uncertainty due to measuremen...)
20 
[CO3]2- [µmol/kg]
(Calculated)
21 
[CO3]2- std dev [±]
(summed uncertainty due to ± 2...)
22 
pCO2 [ppmv]
(Calculated)
23 
pCO2 std dev [±]
(+ 2 sigma, Calculated)
24 
pCO2 std dev [±]
(- 2 sigma, Calculated)
122-761B 122-761B-5H-4,13-1537.312280Globigerinoides sacculifer (300-355 mm)3.8917.140.120.02917.150.120.03217.140.2330.08.090.02140271903636
122-761B122-761B-5H-4,123-12538.412720Globigerinoides sacculifer (300-355 mm)4.0016.500.080.05016.730.070.05516.620.2330.48.030.02129242234241
122-761B122-761B-5H-5,103-10539.713250Globigerinoides sacculifer (300-355 mm)4.0616.320.170.01816.330.150.02016.330.2630.58.000.03123232444746
122-761B122-761B-5H-6,8-1040.313480Globigerinoides sacculifer (300-355 mm)4.1216.300.220.01616.420.160.01816.360.2730.78.000.03123232434746
122-761B122-761B-5H-6,68-7040.913720Globigerinoides sacculifer (300-355 mm)4.2016.420.200.01516.430.180.01616.430.2730.98.010.03125242404645
122-761B122-761B-5H-6,98-10041.213830Globigerinoides sacculifer (300-355 mm)4.4416.260.220.01416.250.180.01516.250.2831.57.980.03122232575049
122-761B122-761B-5H-7,38-4042.114170Globigerinoides sacculifer (300-355 mm)4.3016.220.290.00915.950.240.01116.090.3231.27.970.03118222685452
122-761B122-761B-5H-cc,23-2542.514310Globigerinoides sacculifer (300-355 mm)4.0115.850.210.01616.070.170.01815.960.2730.47.960.03114212725251
122-761B122-761B-6H-1,133-13543.514800Globigerinoides sacculifer (300-355 mm)4.1714.910.370.00815.180.290.00815.040.3730.87.850.0595173748276
122-761B122-761B-6H-2,63-6544.315040Globigerinoides sacculifer (300-355 mm)3.9415.050.340.00715.620.280.00715.340.4030.27.890.05101193327569
122-761B122-761B-6H-3,103-10546.215560Globigerinoides sacculifer (300-355 mm)4.6915.750.260.01115.930.260.01315.840.2932.17.930.03113212985957
122-761B122-761B-6H-4,68-7047.415870Globigerinoides sacculifer (300-355 mm)4.5914.630.400.00615.370.400.00715.000.4131.97.830.0595183929284
122-761B122-761B-6H-5,93-9549.116380Globigerinoides sacculifer (300-355 mm)4.1916.470.220.01816.810.190.02016.640.2630.98.030.03130252254342
122-761B122-761B-5H-4,123-12538.412720Cibicidoides wuellerstorfi (>250 mm)2.0113.180.260.01013.370.220.01113.280.278.17.800.054993907166
122-761B122-761B-5H-4,123-12538.412720Cibicidoides mundulus (>250 mm)2.1212.930.090.03013.090.090.03213.010.238.57.750.044584467873
154-926A 154-926A-26H-5,30-32238.311800Globigerinoides sacculifer (300-355 mm)3.3916.020.090.02616.160.110.02816.090.2328.58.000.02118202474646
154-926A154-926A-29H-5,31-33266.813600Globigerinoides sacculifer (300-355 mm)3.7716.320.080.04116.510.060.04516.420.2329.78.020.02127212324343
154-926A154-926A-32H-2,30-32290.814940Globigerinoides sacculifer (300-355 mm)4.0515.180.080.03615.310.080.03915.240.2330.57.880.03101173466563