# 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-xl26-noaa.txt # Data_Download_Description: NOAA Template File; Stalagmite XL-26 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-26 # First_Year: 6651 # Last_Year: 2984 # 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 XL26 from Xianglong cave. XRD analyses results suggest XL26 is composed of pure aragonite, except for the bottom part below 36.8 cm which is composed of calcite (Fig. 3). The aragonite part of XL26 is included for this study. # 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 # XL26-1 1.5 1540.3 4.1 309.9 6.3 3134.2 64.2 379.1 2.8 0.03825 0.00016 3063 14 2998 15 382.4 2.8 # XL26-1a 50 2585.3 5.1 341.8 7.2 5513.3 117.1 386.7 2.4 0.04420 0.00016 3528 15 3464 15 390.6 2.5 # XL26-2a 74.5 4493.8 11.5 169.3 3.8 20311.9 465.0 385.2 2.6 0.04642 0.00018 3712 16 3650 16 389.2 2.6 # XL26-2 126.5 3091.3 9.7 321.4 6.6 8045.4 166.2 385.6 3.3 0.05073 0.00021 4061 20 3998 20 390.0 3.4 # XL26-4a 175.5 957.8 1.3 125.7 3.0 7087.1 171.1 379.8 2.2 0.05640 0.00024 4543 21 4479 21 384.7 2.2 # XL26-5a 195.5 2564.0 5.1 172.8 3.9 14375.3 329.0 375.3 2.4 0.05876 0.00018 4752 17 4690 17 380.4 2.4 # XL26-6a 217.5 4218.6 10.8 59.8 2.2 69798.4 2543.0 375.0 2.6 0.05998 0.00021 4854 20 4793 20 380.1 2.7 # XL26-3 233.5 1188.7 2.8 213.1 4.3 5564.1 115.2 374.7 2.7 0.06051 0.00028 4899 25 4835 26 379.9 2.8 # XL26-7a 236.5 957.0 1.4 271.5 5.7 3635.0 77.1 373.4 2.3 0.06255 0.00025 5073 22 5006 23 378.8 2.4 # XL26-8a 259.5 2099.3 4.2 159.6 3.7 14275.0 332.0 371.3 2.6 0.06582 0.00022 5353 21 5290 21 377.0 2.7 # XL26-4 278.5 624.0 0.9 168.6 3.6 4112.7 87.7 364.5 2.7 0.06738 0.00022 5510 22 5444 22 370.2 2.7 # XL26-9a 286.5 2102.1 3.2 308.1 6.4 8068.3 169.8 369.0 1.9 0.07171 0.00020 5854 19 5790 19 375.1 1.9 # XL26-10a 317.5 3206.1 8.6 190.5 4.1 21115.5 461.0 366.9 2.9 0.07608 0.00029 6229 28 6167 28 373.4 3.0 # XL26-11a 333.5 3598.6 7.1 123.0 2.8 37971.6 854.8 367.6 1.9 0.07875 0.00021 6451 20 6389 20 374.4 1.9 # XL26-5 363.5 2356.1 6.7 288.4 5.9 10972.1 225.0 364.5 2.8 0.08145 0.00032 6694 30 6631 31 371.4 2.8 #-------------------- # 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 0.1 2984 0.1 -5.98 -1.22 1 2993 0.1 -6.73 -2.61 2 3003 0.1 -6.51 -4.27 3 3013 0.1 -6.36 -4.3 4 3022 0.1 -6.41 -3.5 5 3032 0.1 -7.52 -5.64 6 3041 0.1 -7.31 -5.13 7 3051 0.1 -6.74 -5.31 8 3061 0.1 -7.59 -5.94 9 3070 0.1 -8.21 -7.13 10 3080 0.1 -7.86 -5.49 11 3089 0.1 -6.86 -5.03 12 3099 0.1 -7.21 -5.05 13 3109 0.1 -6.67 -4.57 14 3118 0.1 -6.91 -6.14 15 3128 0.1 -7.2 -6.58 16 3137 0.1 -7.61 -6.55 17 3147 0.1 -7.59 -5.83 18 3157 0.1 -7.42 -5.74 19 3166 0.1 -7.9 -6.28 20 3176 0.1 -7.99 -5.68 21 3185 0.1 -7.03 -4.93 22 3195 0.1 -7.69 -5.04 23 3205 0.1 -8.21 -5.7 24 3214 0.1 -7.25 -4.29 25 3224 0.1 -7.86 -5.35 26 3233 0.1 -7.65 -3.77 27 3243 0.1 -7.27 -3.77 28 3253 0.1 -7.26 -3.2 29 3262 0.1 -7.21 -4.62 30 3272 0.1 -7.38 -3.8 31 3281 0.1 -7.65 -5.28 32 3291 0.1 -7.4 -5.42 33 3301 0.1 -6.56 -4.23 34 3310 0.1 -6.81 -4.27 35 3320 0.1 -8.12 -6.63 36 3329 0.1 -8.07 -5.43 37 3339 0.1 -7.64 -5.85 38 3349 0.1 -7.54 -5.97 39 3358 0.1 -7.74 -5.86 40 3368 0.1 -8.06 -5.73 41 3377 0.1 -7.7 -5.99 42 3387 0.1 -7.41 -5.98 43 3397 0.1 -7.41 -6.24 44 3406 0.1 -7.69 -5.87 45 3416 0.1 -7.58 -5.44 46 3425 0.1 -7.35 -5.9 47 3435 0.1 -7.78 -6.79 48 3445 0.1 -6.85 -5.11 49 3454 0.1 -7.4 -4.97 50 3464 0.13 -7.62 -5.33 51 3471 0.13 -7.4 -5.09 52 3479 0.13 -7.25 -5.33 53 3487 0.13 -7.24 -4.65 54 3494 0.13 -7.1 -4.73 55 3502 0.13 -7.21 -5.29 56 3509 0.13 -8.03 -7.02 57 3517 0.13 -8.01 -5.75 58 3524 0.13 -7.67 -5.31 59 3532 0.13 -7.59 -4.6 60 3540 0.13 -7.93 -5.43 61 3547 0.13 -7.45 -5.19 62 3555 0.13 -7.3 -5.29 63 3562 0.13 -7.24 -5.09 64 3570 0.13 -7.4 -3.69 65 3578 0.13 -7.56 -5.04 66 3585 0.13 -7.83 -5.76 67 3593 0.13 -7.64 -5.81 68 3600 0.13 -7.02 -6.7 69 3608 0.13 -7.33 -6.23 70 3616 0.13 -7.36 -5.5 71 3623 0.13 -7.2 -4.8 72 3631 0.13 -6.45 -5.22 73 3638 0.13 -6.79 -4.79 74 3646 0.13 -7.42 -5.72 75 3653 0.15 -6.67 -5.54 76 3660 0.15 -6.46 -4.85 77 3666 0.15 -7.11 -5.54 78 3673 0.15 -7.84 -5.2 79 3680 0.15 -7.68 -5.48 80 3687 0.15 -7.05 -3.8 81 3693 0.15 -7.18 -4.37 82 3700 0.15 -7.89 -5.98 83 3707 0.15 -7.87 -5.44 84 3713 0.15 -7.57 -5.59 85 3720 0.15 -7.07 -5.26 86 3727 0.15 -7.32 -5.23 87 3733 0.15 -7.54 -4.96 88 3740 0.15 -7.53 -4.33 89 3747 0.15 -7.38 -4.88 90 3753 0.15 -6.66 -5.17 91 3760 0.15 -7.27 -6.22 92 3767 0.15 -6.98 -6.1 93 3774 0.15 -6.81 -3.96 94 3780 0.15 -7.39 -6.19 95 3787 0.15 -7.28 -5.41 96 3794 0.15 -7.27 -4.84 97 3800 0.15 -7.51 -3.88 98 3807 0.15 -7.16 -4.93 99 3814 0.15 -8.01 -6.04 100 3820 0.15 -7.95 -5.12 101 3827 0.15 -7.69 -5.42 102 3834 0.15 -7.72 -5.22 103 3840 0.15 -8 -5.94 104 3847 0.15 -8.44 -6.44 105 3854 0.15 -7.99 -6.29 106 3861 0.15 -7.58 -5.2 107 3867 0.15 -7.33 -5.63 108 3874 0.15 -7.79 -6.35 109 3881 0.15 -7.88 -5.79 110 3887 0.15 -7.88 -5.25 111 3894 0.15 -7.7 -5.75 112 3901 0.15 -8.04 -6.04 113 3907 0.15 -7.46 -4.63 114 3914 0.15 -7.84 -5.34 115 3921 0.15 -8.01 -6.03 116 3927 0.15 -8.13 -6.46 117 3934 0.15 -7.76 -5.55 118 3941 0.15 -7.63 -4.74 119 3948 0.15 -7.63 -5.38 120 3954 0.15 -6.98 -3.97 121 3961 0.15 -7.02 -3.49 122 3968 0.15 -7.2 -3.84 123 3974 0.15 -7.45 -4.31 124 3981 0.15 -7.21 -4.01 125 3988 0.15 -7.36 -3.76 126 3994 0.12 -7.98 -5.04 127 4003 0.1 -8.76 -6.49 128 4013 0.1 -7.52 -5.07 129 4022 0.1 -6.8 -3.15 130 4032 0.1 -6.97 -3.45 131 4042 0.1 -7.1 -4.08 132 4052 0.1 -7.46 -4.02 133 4062 0.1 -7.7 -5.01 134 4071 0.1 -7.69 -5.02 135 4081 0.1 -7.76 -6.04 136 4091 0.1 -7.52 -6.35 137 4101 0.1 -7.84 -5.48 138 4111 0.1 -8.04 -5.26 139 4121 0.1 -7.94 -5.99 140 4130 0.1 -7.82 -5.63 141 4140 0.1 -7.46 -5.03 142 4150 0.1 -8.68 -6.97 143 4160 0.1 -7.42 -3.89 144 4170 0.1 -8.17 -5.61 145 4179 0.1 -7.19 -3.61 146 4189 0.1 -7.86 -5.35 147 4199 0.1 -7.95 -4.62 148 4209 0.1 -7.84 -5.55 149 4219 0.1 -8.47 -5.86 150 4229 0.1 -7.73 -4.01 151 4238 0.1 -7.97 -4.87 152 4248 0.1 -7.31 -3.51 153 4258 0.1 -7.66 -5.03 154 4268 0.1 -6.59 -3.48 155 4278 0.1 -7.95 -5.82 156 4287 0.1 -8.24 -6.75 157 4297 0.1 -8.03 -6.15 158 4307 0.1 -7.15 -5.23 159 4317 0.1 -7.04 -4.51 160 4327 0.1 -7.91 -5.76 161 4337 0.1 -8.19 -5.16 162 4346 0.1 -8.4 -6.1 163 4356 0.1 -7.36 -4.36 164 4366 0.1 -7.84 -5.79 165 4376 0.1 -7.85 -6.17 166 4386 0.1 -8.22 -6.22 167 4396 0.1 -7.81 -6.1 168 4405 0.1 -7.69 -5.61 169 4415 0.1 -6.6 -4.66 170 4425 0.1 -6.97 -3.83 171 4435 0.1 -7.41 -4.3 172 4445 0.1 -8.03 -5.96 173 4454 0.1 -7.52 -5.54 174 4464 0.1 -7.77 -5.45 175 4474 0.1 -7.87 -5.52 176 4484 0.09 -7.35 -4.48 177 4495 0.09 -7.08 -3.95 178 4505 0.09 -6.97 -4.02 179 4516 0.09 -7.58 -4.7 180 4526 0.09 -7 -4.64 181 4537 0.09 -7.02 -5.26 182 4547 0.09 -7.19 -4.9 183 4558 0.09 -6.66 -4.25 184 4569 0.09 -7.31 -4.87 185 4579 0.09 -7.39 -4.74 186 4590 0.09 -7.27 -3.66 187 4600 0.09 -7.71 -4.56 188 4611 0.09 -7.54 -4.75 189 4621 0.09 -7.89 -4.67 190 4632 0.09 -7.84 -4.58 191 4642 0.09 -7.5 -4.05 192 4653 0.09 -7.94 -4.27 193 4663 0.09 -7.64 -4.08 194 4674 0.09 -7.68 -4.66 195 4684 0.13 -7.66 -4.85 196 4692 0.21 -8.75 -5.03 197 4697 0.21 -7.88 -4.06 198 4701 0.21 -7.76 -3.93 199 4706 0.21 -8.12 -4.68 200 4711 0.21 -7.5 -4.72 201 4716 0.21 -7.81 -4.69 202 4720 0.21 -8.05 -4.53 203 4725 0.21 -7.81 -4.06 204 4730 0.21 -7.76 -4.2 205 4734 0.21 -8.22 -4.88 206 4739 0.21 -8.11 -4.24 207 4744 0.21 -7.83 -4.22 208 4748 0.21 -7.43 -4.28 209 4753 0.21 -7.16 -3.99 210 4758 0.21 -7.81 -4.27 211 4763 0.21 -7.48 -4.2 212 4767 0.21 -7.93 -4.65 213 4772 0.21 -7.3 -4.35 214 4777 0.21 -7.57 -5.04 215 4781 0.21 -8.28 -5.43 216 4786 0.21 -7.21 -3.79 217 4791 0.27 -7.75 -5.58 218 4794 0.39 -8.07 -5.58 219 4797 0.39 -8.47 -5.7 220 4800 0.39 -9.09 -6.49 221 4802 0.39 -8.9 -6.47 222 4805 0.39 -8.38 -4.91 223 4807 0.39 -9.2 -5.23 224 4810 0.39 -7.8 -5.15 225 4813 0.39 -8.22 -5.5 226 4815 0.39 -7.87 -4.62 227 4818 0.39 -8.06 -5.51 228 4820 0.39 -7.57 -5.27 229 4823 0.39 -7.3 -4.83 230 4825 0.39 -6.83 -3.82 231 4828 0.39 -7.22 -4.91 232 4831 0.39 -8 -5.34 233 4833 0.03 -7.58 -3.79 234 4863 0.02 -8.09 -4.57 234.5 4892 0.02 -7.58 -3.42 235 4920 0.02 -6.7 -0.84 235.5 4949 0.02 -7.12 -1.6 236 4977 0.03 -7.62 -2.41 237 5012 0.08 -7.62 -3.07 238 5024 0.08 -7.9 -3.48 239 5037 0.08 -7.65 -3.21 240 5049 0.08 -8.08 -4.26 241 5062 0.08 -7.5 -2.99 242 5074 0.08 -7.86 -3.95 243 5086 0.08 -7.73 -3.69 244 5099 0.08 -7.38 -3.99 245 5111 0.08 -7.51 -3.8 246 5123 0.08 -7.67 -3.08 247 5136 0.08 -7.82 -3.45 248 5148 0.08 -7.57 -4.71 249 5160 0.08 -8.03 -3.59 250 5173 0.08 -7.87 -3.86 251 5185 0.08 -7.34 -2.78 252 5197 0.08 -8.72 -5.19 253 5210 0.08 -8 -4.69 254 5222 0.08 -7.29 -3.87 255 5234 0.08 -7.48 -3.27 256 5247 0.08 -7.83 -3.83 257 5259 0.08 -7.33 -2.98 258 5271 0.08 -8.22 -3.44 259 5284 0.1 -8.08 -3.58 260 5294 0.12 -7.77 -4.4 261 5302 0.12 -7.82 -3.49 262 5310 0.12 -8.29 -4.45 263 5318 0.12 -8.25 -3.23 264 5326 0.12 -8.21 -3.55 265 5334 0.12 -8.49 -4.13 266 5343 0.12 -8.15 -3.9 267 5351 0.12 -7.9 -3.51 268 5359 0.12 -8.32 -4.38 269 5367 0.12 -8.05 -4.22 270 5375 0.12 -8.63 -4.87 271 5383 0.12 -7.93 -4.05 272 5391 0.12 -7.8 -4.44 273 5399 0.12 -7.65 -4.38 274 5407 0.12 -7.57 -4.06 275 5415 0.12 -8.11 -4.81 276 5424 0.12 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