NOAA/WDS Paleoclimatology - Sugan Lake, NW China 1000 Year Chironomid Salinity Reconstruction
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 Climate Reconstruction. The data include parameters of climate reconstructions|insect|paleolimnology with a geographic location of China, Eastern Asia. The time period coverage is from 960 to -52 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.
Dataset Citation
- Cite as: Chen, J.; Chen, F.; Zhang, E.L.; Brooks, S.J.; Zhou, A.F.; Zhang, J.-W. (2012-03-09): NOAA/WDS Paleoclimatology - Sugan Lake, NW China 1000 Year Chironomid Salinity Reconstruction. [indicate subset used]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/5xz4-w563. Accessed [date].
- Please refer to Credit tab for full citation information.
Dataset Identifiers
- doi:10.25921/5xz4-w563
- noaa-recon-12823
- NCEI DSI 1200_02
- NCEI DSI 1200_01
ISO 19115-2 Metadata
noaa-recon-12823
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NOAA National Centers for Environmental Information ncei.info@noaa.gov |
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NOAA National Centers for Environmental Information ncei.info@noaa.gov |
Dataset Point of Contact | Data Center Contact NOAA World Data Service for Paleoclimatology 828-271-4800 paleo@noaa.gov |
Coverage Description | Date Range: 990 CE to 2002 CE; Date Range: 960 cal yr BP to -52 cal yr BP; |
Time Period | 990 to 2002 |
Spatial Bounding Box Coordinates |
West: 93.8833
East: 93.8833
South: 38.8667
North: 38.8667
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Data Presentation Form | Digital table - digital representation of facts or figures systematically displayed, especially in columns |
Dataset Progress Status | Complete - production of the data has been completed |
Data Update Frequency | Data update frequency not available |
Supplemental Information | STUDY NOTES: Chironomid-inferred water salinity data from Sugan Lake, Qaidam Basin, NW China, for the last millennium. Salinity was estimated using a chironomid-salinity transfer function for Tibetan Plateau lakes developed by Zhang et al (2007). The salinity record was standardized to have a zero mean and unit standard deviation. Chronology was established by varve counting (Zhou et al., 2007, 2009). ABSTRACT SUPPLIED BY ORIGINATOR: A 1000-year high-resolution (~10 years) chironomid record from varved sediments of Sugan Lake, Qaidam Basin on the northern Tibetan Plateau, is presented. The chironomid assemblages are mainly composed of the relatively high-saline-water taxa Psectrocladius barbimanus-type and Orthocladius/ Cricotopus, and the relatively low-saline-water taxa Procladius and Psectrocladius sordidellus-type. Variations in the chironomid fauna and inferred salinities suggest that over the last millennium, the Sugan Lake catchment has alternated between contrasting climatic conditions, having a dry climate during the period 990-1550 AD, a relatively humid climate during the Little Ice Age (LIA) (1550-1840 AD), and a dry climate again from 1840 AD onwards. At the decadal to centennial scale, a wet event around 1200-1230 AD, interrupting the generally arid period (990-1550 AD), and a dry event around 1590-1700 AD, punctuating the generally humid period (1550-1840 AD), are clearly documented. Trends in the chironomid-based salinity time series indicate a highly unstable climate during the LIA when salinity fluctuations were of greater magnitude and higher frequency. The effective moisture evolution in the Sugan Lake catchment during the last millennium reconstructed by chironomid analysis is in broad agreement with previous palaeo-moisture data derived from other sites in arid Northwest China (ANC). The LIA, characterized by generally humid conditions over the westerly-dominated ANC was distinctly different from that in monsoonal China, implying an "out-of-phase" relationship between moisture evolution in these two regions during the past 1000 years. |
Purpose | Records of past temperature, precipitation, and other climate variables derived from paleoclimate proxies. Parameter keywords describe what was measured in this data set. Additional summary information can be found in the abstracts of papers listed in the data set citations. |
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Last Modified: 2024-02-13
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For questions about the information on this page, please email: ncei.info@noaa.gov