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| Main Authors: | , , , , , , , , |
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| Format: | Dataset Open Access |
| Language: | en |
| Published: |
PANGAEA
2025
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| Subjects: | |
| Online Access: | https://doi.org/10.1594/PANGAEA.986506 |
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| _version_ | 1867171901380493312 |
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| author | Torner, Judit Cacho, Isabel Stoll, Heather M Moreno, Ana Grimalt, Joan O Sierro, Francisco Javier Fornós, Joan J Cheng, Hai Edwards, R Lawrence |
| author_facet | Torner, Judit Cacho, Isabel Stoll, Heather M Moreno, Ana Grimalt, Joan O Sierro, Francisco Javier Fornós, Joan J Cheng, Hai Edwards, R Lawrence |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | This dataset comprises U-Th dating results from the RAT speleothem. The data were used to reconstruct past climate variability in the western Mediterranean region over the interval 387 to 209 ka, encompassing several glacial terminations (TIV, TIII, and TIIIa). The speleothem was collected in winter 2011 from Murada Cave, located on Menorca Island (39°57′58″N; 3°57′53″E). Element isolation was performed according to Shen et al. (2002) and Cheng et al. (2009). U-Th dating was conducted using a multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS) with parallel ion-counting (Finnigan Neptune) at the University of Minnesota and Xi'an Jiaotong University. Age-depth models were calculated with the StalAge package in R (Scholz and Hoffmann, 2011). |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_986506 |
| institution | PANGAEA |
| language | en |
| publishDate | 2025 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | U–Th Dating of the RAT Speleothem from Menorca Island (387–209 ka) Torner, Judit Cacho, Isabel Stoll, Heather M Moreno, Ana Grimalt, Joan O Sierro, Francisco Javier Fornós, Joan J Cheng, Hai Edwards, R Lawrence Age, dated; Age, dated, standard deviation; DEPTH, sediment/rock; glacial terminations; MC-ICP-MS Thermo-Finnigan Neptune; Mediterranean; Murada Cave, Menorca, Spain; Paleoclimate; RAT_collection; Sample code/label; Sample number; Speleothems; Speleothem sample; SPS; Thorium-230/Thorium-232 atomic ratio; Thorium-230/Thorium-232 atomic ratio, standard deviation; Thorium-230/Uranium-238 activity ratio; Thorium-230/Uranium-238 activity ratio, standard deviation; Thorium-232; Thorium-232, standard deviation; U/Th dating; Uranium-238; Uranium-238, standard deviation; δ234 Uranium; δ234 Uranium, standard deviation This dataset comprises U-Th dating results from the RAT speleothem. The data were used to reconstruct past climate variability in the western Mediterranean region over the interval 387 to 209 ka, encompassing several glacial terminations (TIV, TIII, and TIIIa). The speleothem was collected in winter 2011 from Murada Cave, located on Menorca Island (39°57′58″N; 3°57′53″E). Element isolation was performed according to Shen et al. (2002) and Cheng et al. (2009). U-Th dating was conducted using a multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS) with parallel ion-counting (Finnigan Neptune) at the University of Minnesota and Xi'an Jiaotong University. Age-depth models were calculated with the StalAge package in R (Scholz and Hoffmann, 2011). |
| title | U–Th Dating of the RAT Speleothem from Menorca Island (387–209 ka) |
| topic | Age, dated; Age, dated, standard deviation; DEPTH, sediment/rock; glacial terminations; MC-ICP-MS Thermo-Finnigan Neptune; Mediterranean; Murada Cave, Menorca, Spain; Paleoclimate; RAT_collection; Sample code/label; Sample number; Speleothems; Speleothem sample; SPS; Thorium-230/Thorium-232 atomic ratio; Thorium-230/Thorium-232 atomic ratio, standard deviation; Thorium-230/Uranium-238 activity ratio; Thorium-230/Uranium-238 activity ratio, standard deviation; Thorium-232; Thorium-232, standard deviation; U/Th dating; Uranium-238; Uranium-238, standard deviation; δ234 Uranium; δ234 Uranium, standard deviation |
| url | https://doi.org/10.1594/PANGAEA.986506 |