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Schorndorf, Nils; Frank, Norbert; Ritter, Simon Michael; Warken, Sophie F; Scholz, Christian; Keppler, Frank; Scholz, Denis; Weber, Michael; Avilés Olguin, Jerónimo; Stinnesbeck, Wolfgang (2022): Trace element and stable isotope data of subaqueous grown speleothems (Hells Bells) from the northeastern Yucatán Peninsula [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.945784

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Abstract:
This dataset provides geochemical data (trace elements and stable isotopes) of subaqueous grown speleothems (Hells Bells) from the north-eastern Yucatán Peninsula. These secondary carbonates were collected from three different sinkholes (cenotes) southwest of Cancún, Quintana Roo, Mexico (20.51–20.52°N, 87.01–87.07°W) at water depths between -29.4 m a.s.l and -37.3 m a.s.l. Samples were collected in situ and their elevation was measured with a dive computer (+-0.1m). For samples taken from the bottom of the cenotes, we cannot assign a corresponding water depth since we have no information about their original position on the cave ceiling. Major and trace elements were determined by ICP-OES. Stable carbon and oxygen isotope measurements were carried out by a ThermoFinnigan MAT253Plus gas source mass spectrometer equipped with a Thermo Fisher Scientific Kiel IV carbonate device.
Keyword(s):
speleothem; Stable isotopes; trace elements; Yucatan Peninsula
Supplement to:
Schorndorf, Nils; Frank, Norbert; Ritter, Simon Michael; Warken, Sophie F; Scholz, Christian; Keppler, Frank; Scholz, Denis; Weber, Michael; Avilés Olguin, Jerónimo; Stinnesbeck, Wolfgang (2023): Mid- to late Holocene sea-level rise recorded in Hells Bells 234U/238U ratio and geochemical composition. Scientific Reports, 13(1), 10011, https://doi.org/10.1038/s41598-023-36777-y
Related to:
Source:
Ritter, Simon Michael; Isenbeck-Schröter, Margot; Scholz, Christian; Keppler, Frank; Gescher, Johannes; Klose, Lukas; Schorndorf, Nils; Avilés Olguin, Jerónimo; González-González, Arturo; Stinnesbeck, Wolfgang (2019): Subaqueous speleothems (Hells Bells) formed by the interplay of pelagic redoxcline biogeochemistry and specific hydraulic conditions in the El Zapote sinkhole, Yucatán Peninsula, Mexico. Biogeosciences, 16(11), 2285-2305, https://doi.org/10.5194/bg-16-2285-2019
Coverage:
Median Latitude: 20.858110 * Median Longitude: -87.118329 * South-bound Latitude: 20.853250 * West-bound Longitude: -87.126647 * North-bound Latitude: 20.871917 * East-bound Longitude: -87.023472
Event(s):
Cenote_El_Zapote-Big_Bell_1 * Latitude: 20.857717 * Longitude: -87.126647 * Location: Quintana Roo, Mexico * Method/Device: Speleothem sample (SPS) * Comment: samples taken from the bottom of the cenote
Cenote_El_Zapote-Big_Bell_6 * Latitude: 20.857717 * Longitude: -87.126647 * Location: Quintana Roo, Mexico * Method/Device: Speleothem sample (SPS) * Comment: samples taken from the bottom of the cenote
Cenote_El_Zapote-TL4 * Latitude: 20.857717 * Longitude: -87.126647 * Location: Quintana Roo, Mexico * Method/Device: Speleothem sample (SPS)
Status:
Curation Level: Enhanced curation (CurationLevelC) * Processing Level: PANGAEA data processing level 3 (ProcLevel3)
Size:
723 data points

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