# Xianglong Cave, China 6,650 year Speleothem Stable Isotope Data #---------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program # National Centers for Environmental Information (NCEI) #---------------------------------------------------- # Template Version 4.0 # Encoding: UTF-8 # NOTE: Please cite original publication, NOAA Landing Page URL, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, study title, NOAA Landing Page URL, and date accessed. # # Description/Documentation lines begin with # # Data lines have no # # # NOAA_Landing_Page: https://www.ncei.noaa.gov/access/paleo-search/study/23870 # Landing_Page_Description: NOAA Landing Page of this file's parent study, which includes all study metadata. # # Study_Level_JSON_Metadata: https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/json/noaa-cave-23870.json # Study_Level_JSON_Description: JSON metadata of this data file's parent study, which includes all study metadata. # # Data_Type: Speleothems # # Dataset_DOI: 10.25921/8d0j-jt40 # # Science_Keywords: #-------------------- # Resource_Links # # Data_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/speleothem/asia/china/xianglong2018-xl16-noaa.txt # Data_Download_Description: NOAA Template File; Stalagmite XL-16 Stable Isotope Data # #-------------------- # Contribution_Date # Date: 2018-04-12 #-------------------- # File_Last_Modified_Date # Date: 2025-03-31 #-------------------- # Title # Study_Name: Xianglong Cave, China 6,650 year Speleothem Stable Isotope Data #-------------------- # Investigators # Investigators: Tan, L.(https://orcid.org/0000-0003-1932-7102); Cai, Y.(https://orcid.org/0000-0001-7063-5050); Cheng, H.(https://orcid.org/0000-0002-5305-9458); Edwards, R.L.(https://orcid.org/0000-0002-7027-5881); Gao, Y.; Xu, H.(https://orcid.org/0000-0002-5356-8156); Zhang, H.(https://orcid.org/0000-0002-0855-1283); An, Z.(https://orcid.org/0000-0002-9538-9826) #-------------------- # Description_Notes_and_Keywords # Description: Speleothem oxygen and carbon isotope records from Xianglong Cave, upper Hanjiang River region over the last 6650 years. Provided Keywords: Speleothem, oxygen and carbon isotope, Xianglonglong cave, paleoclimate #-------------------- # Publication # Authors: Liangcheng Tan, Yanjun Cai, Hai Cheng, R. Lawrence Edwards, Yongli Gao, Hai Xu, Haiwei Zhang, Zhisheng An # Journal_Name: Earth and Planetary Science Letters # Published_Title: Centennial- to decadal-scale monsoon precipitation variations in the upper Hanjiang River region, China over the past 6650 years # Published_Date_or_Year: 2018 # Volume: 482 # Pages: 580-590 # Issue: # Report_Number: # DOI: 10.1016/j.epsl.2017.11.044 # Full_Citation: # Abstract: The upper Hanjiang River region is the recharge area of the middle route of South-to-North Water Transfer Project. The region is under construction of the Hanjiang-Weihe River Water Transfer Project in China. Monsoon precipitation variations in this region are critical to water resource and security of China. In this study, high-resolution monsoon precipitation variations were reconstructed in the upper Hanjiang River region over the past 6650 years from d18O and d13C records of four stalagmites in Xianglong cave. The long term increasing trend of stalagmite d18O record since the middle Holocene is consistent with other speleothem records from monsoonal China. This trend follows the gradually decreasing Northern Hemisphere summer insolation, which indicates that solar insolation may control the orbital-scale East Asian summer monsoon (EASM) variations. Despite the declined EASM intensity since the middle Holocene, local precipitation may not have decreased remarkably, as revealed by the d13C records. A series of centennial- to decadal-scale cyclicity was observed, with quasi-millennium-, quasi-century-, 57-, 36- and 22-year cycles by removing the long-term trend of stalagmite d18O record. Increased monsoon precipitation during periods of 4390-3800 a BP, 3590-2960 a BP, 2050-1670 a BP and 1110–790 a BP had caused four super-floods in the upper reach of Hanjiang River. Dramatically dry climate existed in this region during the 5.0 ka and 2.8 ka events, coinciding with notable droughts in other regions of monsoonal China. Remarkably intensified and southward Westerly jet, together with weakened summer monsoon, may delay the onset of rainy seasons, resulting in synchronous decreasing of monsoon precipitation in China during the two events. During the 4.2 ka event and the Little Ice Age, the upper Hanjiang River region was wet, which was similar to the climate conditions in central and southern China, but was the opposite of drought observed in northern China. We propose that weakened summer monsoon and less strengthened or normal Westerly jet may cause rain belt stay longer in the southward region, which reduced rainfall in northern China but enhanced it in central and southern China. #-------------------- # Funding_Agency # Funding_Agency_Name: Chinese Academy of Sciences West Light Foundation # Grant: #-------------------- # Funding_Agency # Funding_Agency_Name: National Natural Science Foundation China # Grant: 41372192, 41001061 #-------------------- # Funding_Agency # Funding_Agency_Name: State Key Laboratory of Loess and Quaternary Geology of China # Grant: #-------------------- # Funding_Agency # Funding_Agency_Name: National Key Research and Development Program of China # Grant: 2017YFA0603401 #-------------------- # Funding_Agency # Funding_Agency_Name: Young Scientist Program of Shaanxi, China # Grant: 2015KJXX-57 #-------------------- # Site_Information # Site_Name: Xianglong Cave # Location: China # Northernmost_Latitude: 32.9975 # Southernmost_Latitude: 32.9975 # Easternmost_Longitude: 106.3281 # Westernmost_Longitude: 106.3281 # Elevation_m: 940 #-------------------- # Data_Collection # Collection_Name: Xianglong2018iso XL-16 # First_Year: 4912 # Last_Year: 653 # Time_Unit: cal yr BP # Core_Length_m: # Parameter_Keywords: carbon isotopes, oxygen isotopes # Notes: #-------------------- # Chronology_Information # Chronology: Uranium-Thorium # Chronology_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/templates/noaa-wds-paleo-uth-terms.csv # Chronology_Download_Description: Uranium-Thorium terms and definitions. # Chronology_Notes: 230Th dating results of XL16 from Xianglong cave. XRD analyses results suggest XL16 is composed of pure aragonite. # Rejection_Rationale: # 238U_Decay_Constant: # 234U_Decay_Constant: # 230Th_Decay_Constant: # Initial_230Th/232Th: 4.4 +/- 2.2 x 10-6 # Initial_230Th/232Th_Method: Values for a material at secular equilibrium, with the bulk earth 232Th/238U value of 3.8. The errors are arbitrarily assumed to be 50%. # Age_Model_Method: linear interpolation # Missing_Values: na # Chronology_Table: # samp_id depth_top_mm 238U_ppb 238U_2s_ppb 232Th_ppt 232Th_2s_ppt 230Th_232Th_atom_ppm 230Th_232Th_atom_2s_ppm d234U_meas_permil d234U_meas_2s_permil 230Th_238U_act 230Th_238U_act_2s age_uncorr_BM age_uncorr_2s_yr age_corr_BP1950 age_corr_2s_yr d234U_init_permil d234U_init_2s_permil # XL16-1 4 1671.6 3.8 2493.0 50.2 123.6 2.5 302.5 2.3 0.01118 0.00005 940 5 847 24 303.3 2.4 # XL16-1a 7.5 3528.6 8.6 952.1 19.3 806.0 16.5 305.4 2.1 0.01319 0.00005 1107 5 1041 6 306.4 2.1 # XL16-2a 15.5 3581.9 8.8 192.6 4.0 4180.8 87.5 306.7 2.2 0.01364 0.00005 1143 5 1082 5 307.7 2.3 # XL16-2 23 1941.9 4.6 293.9 6.0 1615.3 33.3 305.9 2.6 0.01482 0.00006 1244 5 1181 6 307.0 2.6 # XL16-3 28 368.5 2.5 173.2 3.6 599.6 13.6 305.5 14.9 0.01709 0.00020 1436 24 1365 25 306.7 15.0 # XL16-3a 48 2088.2 4.6 32.9 1.6 21327.8 1066.0 302.9 2.2 0.02038 0.00008 1718 8 1658 8 304.4 2.2 # XL16-4 66.5 557.5 0.6 141.7 3.0 1382.7 30.0 304.1 1.9 0.02132 0.00012 1797 11 1731 11 305.6 1.9 # XL16-4a 80.5 2467.2 6.5 132.5 2.9 6920.3 152.0 302.0 2.7 0.02255 0.00009 1904 9 1842 9 303.6 2.7 # XL16-5 106.5 1386.6 2.3 287.1 5.9 1946.4 40.7 304.2 2.4 0.02444 0.00010 2062 9 1997 10 305.9 2.4 # XL16-5a 124 1400.8 2.5 97.6 2.2 5974.1 137.6 303.6 2.4 0.02524 0.00010 2130 9 2069 9 305.4 2.4 # XL16-6 144 1667.0 3.0 101.7 2.4 7267.4 169.7 299.6 2.3 0.02689 0.00009 2278 9 2217 9 301.5 2.4 # XL16-6a 160.5 1072.2 2.1 186.0 4.1 2667.4 60.3 297.9 2.6 0.02807 0.00015 2382 13 2318 14 299.9 2.6 # XL16-7 186.5 2502.3 5.8 71.7 1.6 17447.1 400.8 302.9 2.3 0.03032 0.00010 2566 10 2505 10 305.1 2.3 # XL16-2T 208.5 1091.9 1.4 68.6 16.0 8302.7 1942.7 306.6 2.4 0.03159 0.00025 2670 22 2609 22 308.9 2.4 # XL16-8 236.5 1422.6 2.6 64.3 1.6 12186.7 313.2 300.4 2.3 0.03342 0.00011 2836 10 2775 11 302.8 2.3 # XL16-8a 246 1670.4 3.4 501.1 10.2 1917.8 39.3 302.0 2.3 0.03490 0.00012 2960 12 2893 13 304.5 2.4 # XL16-9 265 1280.7 2.5 176.6 3.9 4461.3 99.7 307.3 2.5 0.03732 0.00014 3155 13 3092 13 310.0 2.6 # XL16-9a 272 1671.0 3.6 128.0 3.0 8301.5 198.8 308.6 2.4 0.03857 0.00014 3259 14 3197 14 311.5 2.4 # XL16-10 292 1013.8 1.7 127.3 2.7 5348.5 115.5 310.5 2.0 0.04073 0.00012 3439 12 3376 12 313.5 2.0 # XL16-10a 301.5 672.8 1.1 1031.1 20.8 510.1 10.6 306.8 2.4 0.04741 0.00026 4024 23 3930 34 310.3 2.5 # XL16-11a 307 756.0 1.2 470.1 9.5 1296.3 26.7 311.6 2.4 0.04889 0.00018 4136 17 4063 20 315.2 2.4 # XL16-11 311.5 1079.2 1.7 392.4 7.9 2261.0 46.0 308.4 2.2 0.04987 0.00014 4231 14 4163 15 312.1 2.2 # XL16-1T 317.5 490.1 1.5 1461.3 21.9 313.5 5.8 311.0 5.0 0.05661 0.00062 4812 57 4692 65 315.2 5.1 #-------------------- # Variables # PaST_Thesaurus_Download_Resource: https://www.ncei.noaa.gov/access/paleo-search/skos/past-thesaurus.rdf # PaST_Thesaurus_Download_Description: Paleoenvironmental Standard Terms (PaST) Thesaurus terms, definitions, and relationships in SKOS format. # # Data variables follow that are preceded by '##' in columns one and two. # Variables list, one per line, shortname-tab-var components: what, material, error, units, seasonality, data type, detail, method, C or N for Character or Numeric data) # ## depth_mm depth,,,millimeter,,speleothems,,,N,from SISAL v2 database ## age age,,,calendar year before present,,speleothems,,,N, ## GR growth rate,calcium carbonate,,millimeter per year,,speleothems,,,N, ## d18O delta 18O,calcium carbonate,,per mil VPDB,,speleothems,,,N, ## d13C delta 13C,calcium carbonate,,per mil VPDB,,speleothems,,,N, #-------------------- # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing_Values: depth_mm age GR d18O d13C 0.5 653 0.01804 -5.57 -0.24 1 681 0.01804 -5.71 -0.63 1.5 708 0.01804 -5.84 -0.24 2 736 0.01804 -6.03 -0.95 2.6 769 0.01804 -6.33 0.02 3.2 803 0.01804 -6.39 0.2 3.5 819 0.01804 -7.18 -1.79 4 847 0.01804 -7.12 -1.77 4.6 880 0.01804 -7.32 -1.89 5.1 908 0.01804 -6.62 -2.08 5.5 930 0.01804 -6.68 -2.16 6 958 0.01804 -6.12 -0.35 6.6 991 0.01804 -6.22 -0.34 7 1013 0.01804 -6.75 -2.11 7.5 1041 0.19512 -6.66 -2.05 8 1044 0.19512 -6.59 -2.61 8.5 1046 0.19512 -6.72 -2.42 9.1 1049 0.19512 -6.61 -3.27 9.5 1051 0.19512 -6.62 -4.14 10 1054 0.19512 -6.72 -4.12 10.5 1056 0.19512 -6.54 -4.13 11 1059 0.19512 -6.75 -4.35 11.5 1062 0.19512 -6.66 -4.81 12 1064 0.19512 -6.67 -4.34 12.5 1067 0.19512 -6.29 -4.84 13 1069 0.19512 -5.92 -4.41 13.5 1072 0.19512 -6.09 -4.41 14 1074 0.19512 -6.51 -5.09 14.5 1077 0.19512 -6.48 -5.37 15 1079 0.19512 -6.72 -5.55 15.5 1082 0.07576 -6.6 -4.76 16 1089 0.07576 -6.48 -4.83 16.5 1095 0.07576 -6.72 -4.87 17 1102 0.07576 -6.73 -5.54 17.5 1108 0.07576 -6.83 -5.16 18 1115 0.07576 -6.89 -5.76 18.5 1122 0.07576 -6.34 -5.91 19 1128 0.07576 -6.13 -5.67 19.5 1135 0.07576 -6.22 -5.21 20 1141 0.07576 -6.3 -6.36 20.5 1148 0.07576 -6.14 -5.73 21 1155 0.07576 -6.46 -5.1 21.5 1161 0.07576 -6.12 -3.75 22 1168 0.07576 -6.64 -4.35 22.5 1174 0.07576 -6.27 -3.81 23 1181 0.02717 -6.35 -3.63 23.5 1199 0.02717 -5.98 -3.17 24 1218 0.02717 -6.14 -2.98 24.5 1236 0.02717 -6.4 -2.14 25 1255 0.02717 -6.55 -2.11 25.5 1273 0.02717 -5.99 -0.67 26 1291 0.02717 -6.34 -2.71 26.5 1310 0.02717 -6.08 -2.25 27 1328 0.02717 -6.01 -3.4 27.5 1347 0.02717 -6.03 -2.94 28 1365 0.06826 -5.87 -1.08 28.5 1372 0.06826 -5.78 -1.9 29 1380 0.06826 -6.32 -2.61 29.5 1387 0.06826 -6.26 -2.76 30 1394 0.06826 -6.44 -3.32 30.5 1402 0.06826 -6.28 -2.62 31 1409 0.06826 -5.77 -1.37 31.5 1416 0.06826 -6.04 -2.63 32 1424 0.06826 -5.96 -2.46 32.5 1431 0.06826 -6.32 -2.9 33 1438 0.06826 -6.07 -2.88 33.5 1446 0.06826 -6.53 -3.66 34 1453 0.06826 -6.45 -3.3 34.5 1460 0.06826 -6.63 -3.68 35 1468 0.06826 -6.43 -4.05 35.5 1475 0.06826 -6.01 -2.97 36 1482 0.06826 -6.16 -4.41 36.5 1490 0.06826 -6.06 -4.2 37 1497 0.06826 -6.45 -4.01 37.5 1504 0.06826 -6.56 -4.06 38 1512 0.06826 -6.96 -4.52 38.5 1519 0.06826 -6.9 -5.02 39 1526 0.06826 -7.11 -4.89 39.5 1533 0.06826 -6.63 -4.58 40 1541 0.06826 -7.12 -5.4 40.5 1548 0.06826 -5.92 -4.2 41 1555 0.06826 -5.74 -4.68 41.5 1563 0.06826 -5.51 -3.79 42 1570 0.06826 -5.61 -4.38 42.5 1577 0.06826 -6.03 -3.39 43 1585 0.06826 -6.19 -3.52 43.5 1592 0.06826 -6.19 -3.39 44 1599 0.06826 -5.99 -3.49 44.5 1607 0.06826 -6.22 -4.53 45 1614 0.06826 -6.44 -5.08 45.5 1621 0.06826 -6.52 -4.77 46 1629 0.06826 -6.76 -4.82 47 1643 0.06826 -5.36 -7.28 48 1658 0.25342 -6.99 -4.56 49 1662 0.25343 -6.57 -4.28 50 1666 0.25342 -6.19 -4.35 51 1670 0.25343 -6.03 -3.6 52 1674 0.25342 -6.03 -4.19 53 1678 0.25342 -7.09 -3.02 54 1682 0.25343 -7.08 -4.29 55 1686 0.25342 -7.32 -3.61 56 1690 0.25343 -6.9 -5.1 57 1694 0.25342 -7.38 -3.55 58 1697 0.25342 -6.67 -5.67 59 1701 0.25343 -7.08 -3.55 60 1705 0.25342 -6.45 -5.59 61 1709 0.25343 -7.03 -4.08 62 1713 0.25342 -6.44 -4.88 63 1717 0.25342 -7.35 -2.97 64 1721 0.25343 -7.25 -5.01 65 1725 0.25342 -7.42 -3.26 66 1729 0.16843 -6.57 -3.58 67 1735 0.12613 -7.03 -4.34 68 1743 0.12613 -7.16 -4.65 69 1751 0.12613 -6.69 -4.93 70 1759 0.12613 -6.33 -3.98 71 1767 0.12613 -7.16 -4.7 72 1775 0.12613 -6.53 -4.47 73 1783 0.12613 -6.68 -4.82 74 1790 0.12613 -6.37 -5.56 75 1798 0.12613 -6.69 -5.12 76 1806 0.12613 -7.03 -4.43 77 1814 0.12613 -6.73 -4.91 78 1822 0.12613 -6.13 -4.07 79 1830 0.12613 -6.66 -4.42 80 1838 0.14399 -7.3 -5.23 81 1845 0.16774 -6.52 -5.26 82 1851 0.16774 -7.18 -5.31 83 1857 0.16774 -6.94 -5.52 84 1863 0.16774 -6.53 -4.75 85 1869 0.16774 -6.66 -5.09 86 1875 0.16774 -6.67 -5.29 87 1881 0.16774 -6.63 -3.97 88 1887 0.16774 -6.81 -5.01 89 1893 0.16774 -6.03 -4.71 90 1899 0.16774 -7.11 -5.98 91 1905 0.16774 -6.2 -4.63 92 1911 0.16774 -6.63 -5.35 93 1917 0.16774 -6.74 -4.12 94 1922 0.16774 -7.07 -5.97 95 1928 0.16774 -6.63 -4.93 96 1934 0.16774 -6.22 -4.12 97 1940 0.16774 -6.72 -4.92 98 1946 0.16774 -6.79 -4.4 99 1952 0.16774 -6.99 -3.89 100 1958 0.16774 -6.29 -4.69 101 1964 0.16774 -7.17 -4.64 102 1970 0.16774 -6.51 -3.94 103 1976 0.16774 -7.16 -5.17 104 1982 0.16774 -6.45 -5.28 105 1988 0.16774 -6.67 -6.05 106 1994 0.1985 -6.74 -5.56 107 1999 0.24306 -6.22 -4.47 108 2003 0.24306 -6.58 -4.91 109 2007 0.24306 -6.89 -4.6 110 2011 0.24306 -6.25 -4.66 111 2016 0.24306 -6.63 -4.76 112 2020 0.24306 -6.1 -4.07 113 2024 0.24306 -7.04 -4.32 114 2028 0.24306 -6.8 -4.52 115 2032 0.24306 -7.04 -4.69 116 2036 0.24306 -6.72 -4.53 117 2040 0.24306 -6.67 -4.52 118 2044 0.24306 -6.22 -4.64 119 2048 0.24306 -6.3 -4.17 120 2053 0.24306 -6.7 -4.48 121 2057 0.24306 -6.84 -4.49 122 2061 0.24306 -6.62 -5.2 123 2065 0.24306 -6.55 -5.71 124 2069 0.13514 -6.26 -4.7 125 2076 0.13514 -6.69 -4.28 126 2084 0.13514 -6.91 -4.94 127 2091 0.13514 -6.5 -5.34 128 2099 0.13514 -6.27 -4.9 129 2106 0.13514 -6.47 -5.23 130 2113 0.13514 -6.39 -4.86 131 2121 0.13514 -6.92 -5.37 132 2128 0.13514 -6.69 -5.03 133 2136 0.13514 -6.31 -4.01 134 2143 0.13514 -6.36 -4.35 135 2150 0.13514 -6.4 -3.84 136 2158 0.13514 -6.47 -4.75 137 2165 0.13514 -6.84 -4.41 138 2173 0.13514 -6.01 -3.82 139 2180 0.13514 -6.34 -4.41 140 2187 0.13514 -5.87 -5.02 141 2195 0.13514 -6.38 -4.73 142 2202 0.13514 -6.28 -3.38 143 2210 0.16337 -6.61 -3.91 144 2217 0.16337 -6.23 -4.2 145 2223 0.16337 -6.28 -4.58 146 2229 0.16337 -6.51 -5.08 147 2235 0.16337 -7.18 -5.35 148 2241 0.16337 -6.86 -3.54 149 2248 0.16337 -7.09 -5.58 150 2254 0.16337 -7.19 -5.82 151 2260 0.16337 -7.1 -5.41 152 2266 0.16337 -6.81 -4.68 153 2272 0.16337 -6.68 -4.87 154 2278 0.16337 -6.27 -5.18 155 2284 0.16337 -6.4 -3.36 156 2290 0.16337 -6.42 -4.15 157 2297 0.16337 -6.44 -4.01 158 2303 0.16337 -6.86 -3.58 159 2309 0.15022 -6.69 -3.59 160 2315 0.13904 -6.26 -3.19 161 2322 0.13904 -6.59 -4.76 162 2329 0.13904 -6.14 -4.74 163 2336 0.13904 -6.56 -5.4 164 2343 0.13904 -6.86 -4.84 165 2350 0.13904 -6.74 -4.44 166 2358 0.13904 -6.98 -4.56 167 2365 0.13904 -6.56 -4.95 168 2372 0.13904 -6.34 -4.26 169 2379 0.13904 -6.34 -4.24 170 2386 0.13904 -6.28 -4.29 171 2394 0.13904 -6.87 -4.34 172 2401 0.13904 -6.02 -3.69 173 2408 0.13904 -6.56 -4.24 174 2415 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