# Wanxiang Cave, China Stalagmite Oxygen Isotope Data #----------------------------------------------------------------------- # World Data Center for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program #----------------------------------------------------------------------- # NOTE: Please cite Publication, and Online_Resource and date accessed when using these data. # If there is no publication information, please cite Investigators, Title, and Online_Resource and date accessed. # # # Online_Resource: https://www.ncdc.noaa.gov/cdo/f?p=519:1:::::P1_STUDY_ID:8629 # # Online_Resource: https://www.ncdc.noaa.gov/paleo/study/24611 # # Original_Source_URL: http://www1.ncdc.noaa.gov/pub/data/paleo/speleothem/china/wanxiang2008.txt # # Description/Documentation lines begin with # # Data lines have no # # # Archive: Speleothems #-------------------- # Contribution_Date # Date: 2009-09-01 #-------------------- # Title # Study_Name: Wanxiang Cave, China Stalagmite Oxygen Isotope Data #-------------------- # Investigators # Investigators: Zhang, P.; Cheng, H.; Edwards, R.L.; Chen, F.; Wang, Y.; Yang, X.; Liu, J.; Tan, M.; Wang, X. #-------------------- # Description_and_Notes # Description: Stalagmite Oxygen Isotope Data (d18O, VPDB) from Wanxiang Cave, Wudu County, Gansu Province, central China: 33deg 19'N, 105deg 00'E, 1200 m above sea level #-------------------- # Publication # Authors: Zhang, P.; Cheng, H.; Edwards, R.L.; Chen, F.; Wang, Y.; Yang, X.; Liu, J.; Tan, M.; Wang, X. # Published_Date_or_Year: 2008 # Published_Title: A Test of Climate, Sun, and Culture Relationships from an 1810-Year Chinese Cave Record # Journal_Name: Science # Volume: 322 # Edition: # Issue: # Pages: 940-942 # DOI: # Online_Resource: # Full_Citation: Zhang, P., Cheng, H., Edwards, R.L., Chen, F., Wang, Y., Yang, X., Liu, J., Tan, M., Wang, X., Liu, J., An, C., Dai, Z., Zhou, J., Zhang, D., Jia, J., Jin, L., Johnson, K.R. 2008. A Test of Climate, Sun, and Culture Relationships from an 1810-Year Chinese Cave Record. Science, 322, 940-942. # Abstract: A record from Wanxiang Cave, China, characterizes Asian Monsoon (AM) history over the past 1810 years. The summer monsoon correlates with solar variability, Northern Hemisphere and Chinese temperature, Alpine glacial retreat, and Chinese cultural changes. It was generally strong during Europe's Medieval Warm Period and weak during Europe's Little Ice Age, as well as during the final decades of the Tang, Yuan, and Ming Dynasties, all times that were characterized by popular unrest. It was strong during the first several decades of the Northern Song Dynasty, a period of increased rice cultivation and dramatic population increase. The sign of the correlation between the AM and temperature switches around 1960, suggesting that anthropogenic forcing superseded natural forcing as the major driver of AM changes in the late 20th century. #------------------ # Authors: Anderson, D.M., Tardif, R., Horlick, K., Erb, M.P., Hakim, G.J., Noone, D., Perkins, W.A., and E. Steig # Published_Date_or_Year: 2018 # Published_Title: Additions to the last millennium reanalysis multi-proxy database # Journal_Name: Data Science Journal # Volume: # Edition: # Issue: # Pages: # Report_Number: # DOI: # Online_Resource: # Full_Citation: Anderson, D.M., Tardif, R., Horlick, K., Erb, M.P., Hakim, G., J., Noone, D., Perkins, W.A., and E. Steig, submitted. Additions to the last millennium reanalysis multi-proxy database. Data Science Journal. # Abstract: Progress in paleoclimatology increasingly occurs via data syntheses. We describe additions to a collection prepared for use in paleoclimate state estimation, specifically the Last Millennium Reanalysis (LMR). The 2290 additional series include 2152 tree ring chronologies and 138 other series. They supplement the collection used previously and together form a database titled LMRdb 1.0.0. The additional data draws from lake core, ice core, coral, speleothem, and tree ring archives, using published data primarily from the NOAA Paleoclimatology archive and a set of tree ring width chronologies standardized from raw International Tree Ring Data Bank ring width series. In contrast to many previous paleo compilations, the data were not selected (screened) on the basis of their environmental correlation, multi-century length, or other attributes. The inclusion of proxies sensitive to moisture and other environmental variables expands their use in data assimilation. A preliminary calibration using linear regression with mean annual temperature reveals characteristics of the proxy series and their relationship to temperature, as well as the noise and error characteristics of the records. The additional records are structured as individual files in the NOAA Paleoclimatology format and archived at NOAA Paleoclimatology (Anderson et al. 2018) and will continue to be improved and expanded as part of the LMR Project. The additions represent a four-fold increase in the number of records available for assimilation, provide expanded geographic coverage, and add additional proxy variables. Applications include data assimilation, proxy system model development, and paleoclimate reconstruction using climate field reconstruction and other methods. #------------------ # Funding_Agency # Funding_Agency_Name: United States National Science Foundation # Grant: ESH 0502535 #------------------ # Funding_Agency # Funding_Agency_Name: China National Science Foundation # Grant: NSFC 40421101, 40471137, 40721061, 40225007 #------------------ # Funding_Agency # Funding_Agency_Name: Gary Comer Science and Education Foundation # Grant: #------------------ # Funding_Agency # Funding_Agency_Name: Ministry of Science and Technology of China # Grant: 2006CB400503 #------------------ # Funding_Agency # Funding_Agency_Name: Chinese Academy of Sciences # Grant: KZCX2-YW- 316 #------------------ # Funding_Agency_Name: National Science Foundation # Grant:AGS-1304263 # Funding_Agency_Name: National Oceanic and Atmospheric Administration # Grant:NA14OAR4310176 #------------------ # Site_Information # Site_Name: Wanxiang Cave, Wudu County, Gansu Province, central China # Location: Asia>Eastern Asia>China # Country: China # Northernmost_Latitude: 33.316 # Southernmost_Latitude: 33.316 # Easternmost_Longitude: 105.00 # Westernmost_Longitude: 105.00 # Elevation: 1200 m #------------------ # Data_Collection # Collection_Name: 08chin01a # Earliest_Year: 192 # Most_Recent_Year: 2003 # Time_Unit: y_ad # Core_Length: # Notes: {"database":"LMR"} #------------------ # Species # Species_Name: # Common_Name: #------------------ # Chronology: #1. Table S1. 230Th dating results. The error is 2 sigma error # #Sample Distance 238U 232Th 230Th/232Th d234U* 230Th/238U 230Th Age(yr) 230Th Age(yr) 230Th Age(AD) #Number (mm) (ppb) (ppt) (atomicx10e6) (measured) (activity) (uncorrected) (corrected) (corrected) #WX42B-2-1 1 8863 +/- 1 2340 +/- 30 27 +/- 1 1926 +/- 0.4 0.00043 +/- 0.00001 16 +/- 0.3 13 +/- 1 1990 +/- 1 #WX42B-2-2 1 9034 +/- 1 990 +/- 20 56 +/- 2 1927.2 +/- 0.9 0.00037 +/- 0.00001 14 +/- 0.2 13 +/- 1 1990 +/- 1 #WX42B-0 4 10848 +/- 1 500 +/- 20 320 +/- 10 1884.4 +/- 0.6 0.00089 +/- 0.00001 34 +/- 0.3 33 +/- 1 1970 +/- 1 #WX42B-2-2 8.1 9955 +/- 1 2240 +/- 30 121 +/- 2 1878.9 +/- 0.7 0.00165 +/- 0.00001 63 +/- 0.4 60 +/- 1 1943 +/- 1 #WX42B-1 13.2 8518 +/- 1 350 +/- 20 1140 +/- 60 1846.4 +/- 0.8 0.00278 +/- 0.00001 107 +/- 0.5 106 +/- 1 1897 +/- 1 #WX42B-2-3 16 7454 +/- 1 260 +/- 20 1640 +/- 110 1833.4 +/- 0.7 0.00352 +/- 0.00002 136 +/- 0.6 135 +/- 1 1868 +/- 1 #WX42B-2 22.7 7585 +/- 1 240 +/- 20 4060 +/- 330 1829.5 +/- 0.8 0.00762 +/- 0.00002 295 +/- 1 294 +/- 1 1709 +/- 1 #WX42B2-4 27.8 5818 +/- 1 1250 +/- 30 800 +/- 20 1831.5 +/- 1.2 0.01044 +/- 0.00003 403 +/- 1 401 +/- 2 1602 +/- 2 #WX42B-3 35.5 7844 +/- 1 80 +/- 20 24800 +/- 5800 1832 +/- 0.9 0.01498 +/- 0.00003 579 +/- 1 579 +/- 1 1424 +/- 1 #WX42B2-5 39.3 6475 +/- 0 430 +/- 20 3400 +/- 240 1835.3 +/- 0.8 0.01738 +/- 0.00005 671 +/- 2 670 +/- 2 1333 +/- 2 #WX42B-4 45.5 7860 +/- 1 310 +/- 20 8600 +/- 600 1831.1 +/- 1.4 0.02038 +/- 0.00004 788 +/- 2 788 +/- 2 1215 +/- 2 #WX42B2-6 50.4 7461 +/- 1 110 +/- 20 26000 +/- 5500 1828.9 +/- 0.7 0.02321 +/- 0.00005 899 +/- 2 899 +/- 2 1104 +/- 2 #WX42B-5 57 7167 +/- 1 3680 +/- 40 890 +/- 10 1834 +/- 1.0 0.02682 +/- 0.00005 1037 +/- 2 1032 +/- 3 971 +/- 3 #WX42B2-7 60 6077 +/- 1 1520 +/- 30 1900 +/- 30 1835 +/- 0.9 0.02866 +/- 0.00006 1108 +/- 2 1106 +/- 3 897 +/- 3 #WX42B-7 67 8446 +/- 1 120 +/- 20 37000 +/- 6000 1837.8 +/- 0.7 0.03236 +/- 0.00006 1251 +/- 2 1251 +/- 2 752 +/- 2 #WX42B-8 76.5 9325 +/- 1 410 +/- 30 13800 +/- 900 1838.9 +/- 1.0 0.03705 +/- 0.00007 1433 +/- 3 1432 +/- 3 571 +/- 3 #WX42B-9 86 9397 +/- 2 390 +/- 20 15500 +/- 800 1837.9 +/- 1.2 0.03914 +/- 0.00013 1514 +/- 5 1514 +/- 5 489 +/- 5 #WX42B2-9 92 9128 +/- 1 730 +/- 30 8400 +/- 310 1838.7 +/- 0.8 0.04076 +/- 0.00008 1577 +/- 3 1576 +/- 3 427 +/- 3 #WX42B-10 99 7547 +/- 1 410 +/- 30 13100 +/- 840 1840.9 +/- 0.4 0.04282 +/- 0.00010 1656 +/- 4 1655 +/- 4 348 +/- 4 #WX42B-11 115.5 10159 +/- 1 2660 +/- 40 3000 +/- 50 1845.6 +/- 0.6 0.04694 +/- 0.00009 1813 +/- 3 1811 +/- 4 192 +/- 4 # #Lamda 230 = 9.1577 x 10-6 y-1, Lamda234 = 2.8263 x 10-6 y-1, Lamda238 = 1.55125 x 10-10 y-1. #*d234U = ([234U/238U]activity +/- 1)x1000. ** d234Uinitial was calculated based on 230Th age (T), i.e., d234Uinitial = d234Umeasured x e lambda 234xT #Corrected 230Th ages assume the initial 230Th/232Th atomic ratio of 4.4 +/- 2.2 x10-6. Those are the 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%. # # # # # # # #---------------- # Variables # # Data variables follow that are preceded by "##" in columns one and two. # Data line variables format: Variables list, one per line, shortname-tab-longname-tab-longname components (9 components: what, material, error, units, seasonality, archive, detail, method, C or N for Character or Numeric data) # ##age age, , , years AD, , , , ,N ##d18O delta 18 Oxygen,,,permil VPDB,,Speleothems,,,N ##depth depth in core, , , mm, , , , ,N # #---------------- # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing Values: NAN # age d18O depth 2003 -8.23 0 2002 -8.19 0.1 2001 -8.15 0.1 2000 -8.02 0.3 1999 -7.98 0.3 1998 -7.95 0.4 1997 -8.13 0.5 1996 -8.09 0.6 1995 -8.06 0.6 1994 -8.07 0.7 1993 -8.08 0.8 1992 -8.23 0.9 1991 -8.23 1 1990 -8.23 1 1989 -7.92 1.2 1988 -8.4 1.3 1987 -8.51 1.5 1986 -8.18 1.7 1985 -8.32 1.8 1984 -8.34 1.9 1983 -8.37 2 1982 -8.22 2.2 1981 -8.25 2.3 1980 -8.31 2.5 1979 -8.19 2.7 1978 -8.17 2.8 1977 -8.21 3 1976 -8.29 3.1 1975 -8.39 3.2 1974 -8.15 3.3 1972 -8.09 3.7 1971 -8.12 3.8 1970 -8.25 4 1969 -8.15 4.2 1968 -8.21 4.3 1967 -8.28 4.4 1966 -8.33 4.5 1965 -8.07 4.7 1964 -8.32 4.8 1963 -8.21 5 1962 -8.29 5.2 1961 -8.36 5.3 1960 -8.25 5.5 1959 -8.37 5.7 1958 -8.27 5.8 1957 -8.13 6 1956 -8.15 6.1 1955 -8.17 6.2 1954 -8.23 6.3 1953 -8.28 6.5 1952 -8.31 6.7 1951 -8.58 6.8 1950 -8.3 7 1949 -8.37 7.2 1948 -8.4 7.3 1947 -8.01 7.5 1946 -8.19 7.7 1945 -8.12 7.8 1943 -8.05 8 1942 -8.21 8.2 1941 -8.17 8.3 1939 -7.91 8.5 1938 -8.1 8.7 1936 -7.9 8.8 1935 -7.8 9 1933 -8.03 9.2 1932 -8.18 9.3 1930 -8.06 9.5 1929 -8.24 9.7 1927 -8.2 9.8 1926 -8.02 10 1924 -8.06 10.2 1923 -8.3 10.3 1921 -8.09 10.5 1920 -8.08 10.7 1918 -8.15 10.8 1917 -8.46 11 1915 -8.18 11.2 1914 -8.24 11.3 1912 -8.22 11.5 1911 -8.21 11.7 1909 -8.21 11.8 1908 -8.18 12 1906 -8.03 12.2 1904 -8.25 12.3 1903 -8.26 12.5 1901 -8.12 12.7 1900 -8.35 12.8 1898 -8.19 13 1897 -8.31 13.2 1895 -8.49 13.3 1894 -8.5 13.5 1892 -8.47 13.7 1890 -8.33 13.8 1888 -8.4 14 1887 -8.19 14.2 1885 -8.31 14.3 1883 -8.24 14.5 1881 -8.31 14.7 1880 -8.41 14.8 1878 -8.21 15 1876 -8.25 15.2 1874 -8.17 15.3 1873 -8.16 15.5 1871 -8.16 15.7 1869 -8.11 15.8 1868 -8.1 16 1864 -8 16.2 1860 -8.03 16.3 1856 -7.92 16.5 1852 -7.86 16.7 1848 -8.09 16.8 1844 -8.04 17 1840 -7.95 17.2 1836 -8 17.3 1833 -8.39 17.5 1831 -8.3 17.5 1828 -8.03 17.7 1824 -7.96 17.8 1820 -8.1 18 1816 -7.94 18.2 1812 -8.01 18.3 1808 -7.87 18.5 1804 -7.88 18.7 1800 -8.29 18.8 1796 -8.1 19 1792 -7.92 19.2 1789 -8.11 19.3 1785 -7.89 19.5 1781 -7.85 19.7 1777 -7.99 19.8 1773 -7.94 20 1769 -7.99 20.2 1765 -8.04 20.3 1761 -7.96 20.5 1757 -7.97 20.7 1753 -8.01 20.8 1749 -7.88 21 1745 -8 21.2 1741 -7.98 21.3 1737 -8.01 21.5 1733 -8.04 21.7 1729 -7.99 21.8 1725 -7.99 22 1721 -8.05 22.2 1717 -7.96 22.3 1713 -8.02 22.5 1708 -7.75 22.7 1705 -8.23 22.9 1703 -8.17 23 1700 -7.85 23.1 1696 -7.89 23.3 1691 -7.98 23.5 1687 -8.13 23.7 1684 -8.02 23.9 1681 -7.99 24 1679 -7.72 24.1 1675 -7.68 24.3 1670 -7.78 24.5 1666 -7.69 24.7 1662 -7.87 24.9 1659 -7.97 25.1 1655 -7.92 25.3 1652 -7.94 25.4 1648 -7.71 25.6 1645 -7.74 25.8 1644 -8.06 25.8 1641 -7.77 25.9 1637 -7.94 26.1 1636 -8.13 26.2 1634 -7.77 26.3 1631 -7.67 26.4 1630 -7.99 26.5 1627 -7.56 26.6 1624 -7.58 26.8 1620 -8.08 27 1617 -7.5 27.1 1613 -7.55 27.3 1610 -7.7 27.4 1606 -7.79 27.6 1603 -7.73 27.8 1599 -7.73 27.9 1595 -7.69 28.1 1591 -7.61 28.3 1588 -7.84 28.4 1584 -7.63 28.6 1580 -7.88 28.8 1576 -8.01 28.9 1572 -8.18 29.1 1568 -8.16 29.3 1564 -7.8 29.4 1561 -8.01 29.6 1557 -7.98 29.8 1553 -7.78 29.9 1548 -8.34 30.1 1544 -8.13 30.3 1541 -7.69 30.4 1538 -7.77 30.6 1534 -7.71 30.8 1530 -7.76 30.9 1526 -8.05 31.1 1524 -8.05 31.2 1522 -7.87 31.3 1518 -7.81 31.4 1514 -7.87 31.6 1511 -7.99 31.8 1507 -7.93 31.9 1505 -8.16 32 1502 -8.01 32.1 1499 -7.74 32.3 1495 -7.59 32.4 1491 -7.65 32.6 1488 -7.72 32.8 1486 -7.9 32.8 1484 -7.71 32.9 1481 -8.34 33.1 1480 -7.85 33.1 1476 -7.99 33.3 1472 -8.21 33.4 1468 -7.7 33.6 1467 -8.03 33.7 1464 -7.94 33.8 1461 -8.03 33.9 1457 -7.95 34.1 1453 -8.27 34.3 1449 -8.16 34.4 1448 -8.3 34.5 1445 -7.77 34.6 1441 -7.91 34.8 1438 -7.85 34.9 1434 -8.04 35.1 1430 -7.76 35.3 1428 -8.01 35.3 1426 -7.84 35.4 1422 -7.82 35.6 1418 -7.67 35.8 1414 -7.8 35.9 1410 -8.03 36.1 1408 -8.08 36.2 1406 -7.71 36.3 1402 -8.32 36.4 1398 -8.44 36.6 1397 -8.11 36.6 1394 -7.95 36.8 1393 -7.91 36.8 1391 -8.03 36.9 1389 -8.05 37 1386 -7.56 37.1 1382 -7.83 37.3 1378 -7.96 37.4 1374 -7.88 37.6 1370 -7.72 37.8 1366 -8.03 37.9 1362 -7.87 38.1 1358 -7.56 38.3 1353 -7.66 38.4 1349 -8.01 38.6 1345 -7.91 38.8 1341 -7.98 38.9 1337 -7.92 39.1 1333 -8.23 39.3 1330 -8.07 39.4 1327 -8.02 39.6 1324 -8.11 39.8 1321 -8.15 39.9 1318 -8.33 40.1 1317 -8.5 40.1 1314 -8.05 40.3 1311 -8.13 40.4 1308 -7.97 40.6 1305 -8.06 40.8 1302 -8.15 40.9 1298 -8.14 41.1 1295 -8.28 41.3 1292 -8.16 41.4 1289 -8.16 41.6 1286 -8.11 41.8 1283 -8.15 41.9 1280 -8.16 42.1 1276 -8.34 42.3 1273 -7.97 42.4 1270 -8.03 42.6 1267 -8.2 42.8 1264 -8.25 42.9 1261 -8.18 43.1 1257 -8.18 43.3 1254 -8.3 43.4 1251 -8.3 43.6 1248 -8.01 43.8 1245 -8.33 43.9 1242 -8.25 44.1 1239 -7.93 44.3 1235 -8.18 44.4 1232 -8.19 44.6 1229 -8.1 44.8 1226 -8.29 44.9 1223 -8.14 45.1 1220 -7.93 45.3 1216 -8.22 45.4 1213 -8.26 45.6 1212 -8.44 45.6 1209 -8.3 45.8 1205 -8.27 45.9 1202 -8.18 46.1 1198 -8.24 46.3 1194 -8.24 46.4 1190 -8.08 46.6 1187 -7.92 46.8 1183 -8.1 46.9 1179 -8.22 47.1 1175 -8.29 47.3 1171 -8.15 47.4 1168 -8.16 47.6 1164 -8.03 47.8 1160 -8.15 47.9 1156 -8.24 48.1 1153 -8.24 48.3 1149 -8.52 48.4 1145 -8.36 48.6 1141 -8.37 48.8 1137 -8.36 48.9 1134 -8.39 49.1 1130 -8.25 49.3 1126 -8.24 49.4 1122 -8.46 49.6 1119 -8.12 49.8 1115 -8.15 49.9 1111 -8.55 50.1 1107 -8.5 50.3 1107 -8.64 50.3 1104 -8.44 50.4 1100 -8.3 50.6 1097 -8.4 50.8 1093 -8.2 50.9 1090 -8.25 51.1 1087 -8.01 51.3 1083 -8.11 51.4 1080 -7.99 51.6 1077 -8.14 51.8 1073 -8.16 51.9 1070 -8.06 52.1 1067 -7.95 52.3 1062 -8.2 52.5 1060 -7.97 52.6 1056 -7.94 52.8 1053 -7.98 52.9 1050 -8.14 53.1 1047 -8.46 53.2 1046 -8.38 53.3 1043 -7.98 53.4 1040 -7.8 53.6 1036 -7.92 53.8 1033 -7.98 53.9 1029 -8.19 54.1 1026 -8.35 54.3 1023 -8.1 54.4 1019 -8.25 54.6 1016 -8.21 54.8 1013 -8.23 54.9 1009 -8.35 55.1 1006 -8.44 55.3 1003 -8.15 55.4 999 -8.22 55.6 996 -8.44 55.8 992 -8.25 56 989 -8.33 56.1 988 -8.4 56.1 986 -8.33 56.3 982 -8.34 56.4 982 -8.34 56.5 979 -8.53 56.6 978 -8.35 56.6 976 -8.64 56.8 972 -8.34 56.9 968 -8.3 57.1 968 -8.56 57.1 964 -8.38 57.3 960 -8.36 57.4 956 -8.19 57.6 952 -8.17 57.8 948 -8.3 57.9 944 -8.07 58.1 940 -8.16 58.3 936 -7.94 58.4 932 -7.92 58.6 928 -7.78 58.8 923 -7.9 58.9 919 -8.13 59.1 915 -7.92 59.3 911 -8.01 59.4 907 -8.1 59.6 903 -8.09 59.8 899 -8.01 59.9 895 -7.9 60.1 892 -8.12 60.3 888 -7.89 60.4 885 -7.96 60.6 881 -8.13 60.8 878 -7.92 60.9 875 -7.94 61.1 871 -8.11 61.3 868 -7.86 61.4 864 -7.93 61.6 861 -7.77 61.8 857 -7.97 61.9 854 -7.96 62.1 850 -8.11 62.3 847 -8.09 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