Fensterer, Claudia; Scholz, Denis; Hoffmann, Dirk L; Mangini, Augusto; Pajon, Jesus M (2010): (Supplementary Table 1) 230Th/U results for stalagmite Cuba Grande (CG) from Pinar del Rio [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.736630, Supplement to: Fensterer, C et al. (2010): 230Th/U-dating of a late Holocene low uranium speleothem from Cuba. IOP Conference Series: Earth and Environmental Science, 9(1), 012015, https://doi.org/10.1088/1755-1315/9/1/012015
Always quote citation above when using data! You can download the citation in several formats below.
Abstract:
We present 22 U-series ages for a stalagmite from north-western Cuba based on multi-collector inductively coupled plasma mass spectrometry (MC-ICPMS) and thermal ionisation mass spectrometry (TIMS). Our results reveal that the stalagmite continuously grew within the last ~1400a. Low uranium content of the sample and thus, extremely low 230Th concentrations limit the precision and accuracy of 230Th/U-dating by TIMS. Samples measured by MC-ICPMS show a high variability of 232Th content along the growth axis with some sections significantly affected by initial 230Th from a detrital phase. An a-priori bulk earth ratio for (238U/232Th) cannot be used to accurately account for this initial 230Th. Using an age model based on the 230Th/U ages determined on samples with low or negligible 232Th concentration, we find that the (238U/232Th) activity ratio of the detrital phase is an order of magnitude larger than the bulk earth value, indicating the importance of an accurately determined correction factor.
Project(s):
Integrierte Analyse zwischeneiszeitlicher Klimadynamik (INTERDYNAMIK)
Funding:
German Research Foundation (DFG), grant/award no. 25575884: Integrierte Analyse zwischeneiszeitlicher Klimadynamik
Coverage:
Latitude: 22.383300 * Longitude: -83.966700
Minimum DISTANCE: 1.30 cm * Maximum DISTANCE: 72.00 cm
Event(s):
Comment:
Data acquired through subproject CaribClim (Control of seasonality and interannual to centennial climate in the Caribbean during the Holocene - Combining coral records, stalagmite records and climate models)
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
351 data points
Data
1 Distance [cm] | 2 238U [mg/kg] | 3 238U std dev [±] | 4 232Th [mg/kg] | 5 232Th std dev [±] | 6 (230Th/232Th) | 7 (230Th/232Th) std dev [±] | 8 230Th/238U (activity ratio) | 9 (230Th/238U) std dev [±] | 10 (234U/238U) | 11 234U std dev [±] (activity ratio) | 12 Age dated [ka] (Age uncorrected [ka b2k]) | 13 Age dated std dev [±] | 14 Age dated [ka] (Age corrected with (238U/232T...) | 15 Age dated std dev [±] | 16 Age dated [ka] (Age corrected with (238U/232T...) | 17 Age dated std dev [±] | 18 Comm |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1.30 | 0.1352 | 0.0005 | 0.00073930 | 0.00000210 | 6.50 | 0.05 | 0.01160 | 0.00010 | 2.345 | 0.004 | 0.534 | 0.005 | 0.467 | 0.034 | [0; 0.110] | ||
2.70 | 0.1355 | 0.0005 | 0.00018150 | 0.00000140 | 11.56 | 0.10 | 0.00507 | 0.00004 | 2.342 | 0.004 | 0.227 | 0.002 | 0.211 | 0.008 | 0.067 | 0.067 +0.070 -0.067 | |
13.50 | 0.1362 | 0.0005 | 0.00003180 | 0.00000040 | 79.81 | 1.24 | 0.00610 | 0.00010 | 2.361 | 0.004 | 0.273 | 0.004 | 0.270 | 0.004 | 0.246 | 0.015 | |
21.50 | 0.1241 | 0.0004 | 0.00003850 | 0.00000030 | 93.57 | 1.08 | 0.00950 | 0.00010 | 2.360 | 0.004 | 0.431 | 0.005 | 0.427 | 0.005 | 0.394 | 0.019 | |
34.00 | 0.1048 | 0.0004 | 0.00003520 | 0.00000060 | 127.18 | 3.41 | 0.01399 | 0.00031 | 2.363 | 0.004 | 0.639 | 0.015 | 0.635 | 0.015 | 0.599 | 0.024 | |
39.50 | 0.1344 | 0.0005 | 0.00003430 | 0.00000030 | 198.40 | 1.86 | 0.01656 | 0.00014 | 2.360 | 0.004 | 0.759 | 0.007 | 0.756 | 0.007 | 0.729 | 0.017 | |
54.00 | 0.0914 | 0.0003 | 0.00013670 | 0.00000160 | 54.71 | 0.67 | 0.02676 | 0.00023 | 2.347 | 0.004 | 1.242 | 0.011 | 1.224 | 0.014 | 1.064 | 0.089 | |
59.50 | 0.0906 | 0.0003 | 0.00001470 | 0.00000010 | 438.97 | 3.46 | 0.02328 | 0.00016 | 2.302 | 0.004 | 1.100 | 0.008 | 1.098 | 0.008 | 1.080 | 0.013 | |
66.50 | 0.0991 | 0.0004 | 0.00002850 | 0.00000030 | 271.78 | 2.63 | 0.02554 | 0.00023 | 2.266 | 0.004 | 1.227 | 0.011 | 1.224 | 0.011 | 1.192 | 0.022 | |
71.20 | 0.1014 | 0.0003 | 0.00001940 | 0.00000020 | 438.07 | 5.93 | 0.02750 | 0.00030 | 2.247 | 0.004 | 1.332 | 0.015 | 1.330 | 0.015 | 1.309 | 0.021 | |
4.00 | 0.1993 | 0.0004 | 0.00031650 | 0.00000570 | 9.60 | 0.90 | 0.00500 | 0.00050 | 2.349 | 0.007 | 0.227 | 0.022 | 0.208 | 0.022 | 0.038 | 0.038 +0.07 -0.38 | |
8.00 | 0.1847 | 0.0004 | 0.00005780 | 0.00000174 | 44.00 | 6.70 | 0.00450 | 0.00070 | 2.340 | 0.008 | 0.204 | 0.031 | 0.201 | 0.031 | 0.167 | 0.032 | |
11.80 | 0.1543 | 0.0003 | 0.00000580 | 0.00000006 | 301.20 | 24.90 | 0.00380 | 0.00030 | 2.342 | 0.007 | 0.169 | 0.015 | 0.169 | 0.015 | 0.165 | 0.015 | |
17.90 | 0.1267 | 0.0003 | 0.00005350 | 0.00000080 | 74.10 | 5.90 | 0.01030 | 0.00080 | 2.335 | 0.007 | 0.475 | 0.038 | 0.470 | 0.038 | 0.424 | 0.042 | |
26.00 | 0.1362 | 0.0003 | 0.00001050 | 0.00000008 | 574.40 | 21.10 | 0.01460 | 0.00050 | 2.378 | 0.007 | 0.666 | 0.025 | 0.665 | 0.025 | 0.657 | 0.025 | |
30.50 | 0.1423 | 0.0003 | 0.00004310 | 0.00000074 | 132.90 | 5.50 | 0.01320 | 0.00050 | 2.402 | 0.007 | 0.595 | 0.022 | 0.591 | 0.023 | 0.559 | 0.029 | |
37.65 | 0.1475 | 0.0002 | 0.00002320 | 0.00000034 | 297.80 | 24.50 | 0.01540 | 0.00120 | 2.341 | 0.008 | 0.713 | 0.059 | 0.711 | 0.058 | 0.694 | 0.058 | |
47.00 | 0.1318 | 0.0001 | 0.00000820 | 0.00000009 | 1147.50 | 59.90 | 0.02350 | 0.00120 | 2.339 | 0.004 | 1.194 | 0.057 | 1.194 | 0.056 | 1.087 | 0.057 | |
52.00 | 0.1309 | 0.0003 | 0.00006290 | 0.00000063 | 150.00 | 9.30 | 0.02360 | 0.00140 | 2.348 | 0.007 | 1.096 | 0.067 | 1.091 | 0.068 | 1.039 | 0.069 | |
61.60 | 0.1216 | 0.0002 | 0.00013230 | 0.00000225 | 85.50 | 4.30 | 0.03050 | 0.00140 | 2.285 | 0.008 | 1.458 | 0.070 | 1.444 | 0.070 | 1.325 | 0.091 | |
65.00 | 0.1212 | 0.0002 | 0.00001477 | 0.00000014 | 655.30 | 45.60 | 0.02610 | 0.00180 | 2.259 | 0.008 | 1.262 | 0.090 | 1.260 | 0.088 | 1.247 | 0.087 | |
72.00 | 0.1162 | 0.0002 | 0.00006888 | 0.00000103 | 164.80 | 10.00 | 0.03200 | 0.00190 | 2.253 | 0.008 | 1.552 | 0.091 | 1.545 | 0.095 | 1.479 | 0.096 |