NOAA/WDS Paleoclimatology - Qunf Cave, Oman d18O, d13C, d17O Excess, Fluid Inclusion Hydrogen Isotope, and Trace Metal Data Over the Past 11,000 Years
This archived Paleoclimatology Study is available from the NOAA National Centers for Environmental Information (NCEI), under the World Data Service (WDS) for Paleoclimatology. The associated NCEI study type is Cave. The data include parameters of speleothems with a geographic location of Oman, Middle East. The time period coverage is from 10874 to 402 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.
- Cite as: Tian, Y. (2023-07-03): NOAA/WDS Paleoclimatology - Qunf Cave, Oman d18O, d13C, d17O Excess, Fluid Inclusion Hydrogen Isotope, and Trace Metal Data Over the Past 11,000 Years. [indicate subset used]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/vpmg-jm56. Accessed [date].
- Please refer to Credit tab for full citation information.
- doi:10.25921/vpmg-jm56
- noaa-cave-38279
- NCEI DSI 1200_02
- NCEI DSI 1200_01
noaa-cave-38279
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| Distributor | NOAA National Centers for Environmental Information
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| Dataset Point of Contact | NOAA National Centers for Environmental Information
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| Dataset Point of Contact | Data Center Contact
NOAA World Data Service for Paleoclimatology 828-271-4800 paleo@noaa.gov |
| Coverage Description | Date Range: 10874 cal yr BP to 402 cal yr BP; |
| Time Period | -8924 to 1548 |
| Spatial Bounding Box Coordinates |
N: 17.17
S: 17.17
E: 54.3
W: 54.3
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| Data Presentation Form | Digital table - digital representation of facts or figures systematically displayed, especially in columns
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| Dataset Progress Status | Complete - production of the data has been completed |
| Data Update Frequency | Data update frequency not available |
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ABSTRACT SUPPLIED BY ORIGINATOR: Qunf Cave oxygen isotope (d18Oc) record from southern Oman is one of the most significant of few Holocene Indian summer monsoon cave records. However, the interpretation of the Qunf d18Oc remains in dispute. Here we provide multiple proxy records from Qunf Cave and climate model simulations to reconstruct the Holocene local and regional hydroclimate changes. The results indicate that besides the Indian summer monsoon, the North African summer monsoon also contributes water vapor to southern Oman during the early to middle Holocene. In principle, Qunf d18Oc values reflect integrated oxygen-isotope fractionations over a broad moisture transport swath from moisture sources to the cave site, rather than local precipitation amount alone, and thus the Qunf d18Oc record characterizes primary changes in the super-monsoon regime across the Holocene. In contrast, other Qunf Cave proxy records appear to suggest an overall slightly increased or unchanged wetness over the Holocene at the cave site.
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| Purpose | Records of past temperature, precipitation, and other aspects of climate derived from mineral deposits found in caves. Parameter keywords describe what was measured in this dataset. Additional summary information can be found in the abstracts of papers listed in the dataset citations. |
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| Theme keywords | Global Change Master Directory (GCMD) Science Keywords
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| Data Center keywords | Global Change Master Directory (GCMD) Data Center Keywords
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Last Modified: 2023-09-01
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