# Pulau Langkai Makassar Strait 120 Year Coral 14C 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:10272 # # Online_Resource: https://www.ncdc.noaa.gov/paleo/study/24611 # # Original_Source_URL: ftp://ftp.ncdc.noaa.gov/pub/data/paleo/coral/west_pacific/langkai2008.txt # # Description/Documentation lines begin with # # Data lines have no # # # Archive: Corals and Sclerosponges #-------------------- # Contribution_Date # Date: 2011-01 #-------------------- # Title # Study_Name: Pulau Langkai, Makassar Strait 120 Year Coral 14C Data #-------------------- # Investigators # Investigators: Fallon, S.J.; Guilderson, T.P. #-------------------- # Description_and_Notes # Description: Coral radiocarbon (Delta-14C) on untreated, low-speed drilled samples. Precision is +/-3.5 per mil as documented by an in-house homogenized coral standard, and presented as AGE CORRECTED DELTA-14C [see Stuiver and Polach, 1977]. Cores were taken from a large Porites lutea coral in 4m water depth from the south coast of Langkai Island 35km west of Sulawesi by M. Moore. Cores were split and cleaned with distilled water. After identifying the major vertical growth axis, the coral was sequentially sampled at 2 mm increments with a low-speed drill. Splits (~1 mg) were reacted in vacuo in a modified autocarbonate device at 90 C and the purified CO2 analyzed on a gas source stable isotope ratio mass spectrometer. The remaining sample splits (~10 mg) were placed in individual reaction chambers, evacuated, heated, and then acidified with orthophosphoric acid at 90 C. The evolved CO2 was purified, trapped, and converted to graphite in the presence of hydrogen and an iron catalyst in individual reactors [Vogel et al., 1987]. Graphite targets were measured at the Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory [Davis et al., 1990]. Radiocarbon results are reported as age-corrected Delta-14C (per mil) as defined by Stuiver and Polach [1977] and include the d13C correction obtained from the stable isotope results. Analytical precision and accuracy of the radiocarbon measurements is ~+/-3.5 per mil (1s) based on repeated analyses of an in-house homogenized near-modern coral and accepted secondary and tertiary radiocarbon standards. An initial age-model was constructed using the seasonal variability in coral d13C. To generate the primary time series we pinned the minimum d13C to February of each year, and linearly interpolated the data between marker points. Coral d18O is negatively correlated with water temperature, the summer d18O coral signal is heavily influenced by rainfall and runoff, so we matched the coral d18O maxima to the winter SST minimum from the GOSTA SST atlas. Age model uncertainties are estimated to be better than +/- 2 months. In keeping with the definition of "high-precision radiocarbon" data have been rounded to zero significant figures. #-------------------- # Publication # Authors: Fallon, S.J.; Guilderson, T.P. # Published_Date_or_Year: 2008 # Published_Title: Surface water processes in the Indonesian throughflow as documented by a high-resolution coral D14C record # Journal_Name: Journal of Geophysical Research # Volume: 113 # Edition: # Issue: # Pages: # DOI: 10.1029/2008JC004722 # Online_Resource: # Full_Citation: Fallon, S.J. and T.P. Guilderson. 2008. Surface water processes in the Indonesian throughflow as documented by a high-resolution coral D14C record. J. Geophys. Res., 113, C09001, doi:10.1029/2008JC004722 # Abstract: To explore the seasonal to decadal variability in surface water masses that contribute to the Indonesian throughflow, we have generated a 115-year bimonthly coral-based radiocarbon time series from a coral in the Makassar Straits. In the pre-bomb (pre-1955) era from 1890 to 1954, the radiocarbon time series occasionally displays a small seasonal signal (10-15%). After 1954 the radiocarbon record increases rapidly, in response to the increased atmospheric 14C content caused by nuclear weapons testing. From 1957 to 1986 the record displays clear seasonal variability from 15 to 60% and the post-bomb peak (163 per mil) occurred in 1974. The seasonal cycle of radiocarbon can be attributed to variations of surface waters passing through the South Makassar Strait. Southern Makassar is under the influence of the Northwest Monsoon, which is responsible for the high austral summer radiocarbon (North Pacific waters) and the Southeast Monsoon that flushes back a mixture of low (South Pacific and upwelling altered) radiocarbon water from the Banda Sea. The coral record also shows a significant 14C peak in 1955 due to the bomb-14C water advected into this region from nuclear weapons tests in the Marshall Islands in 1954. #------------------ # 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: U.S. Department of Energy # Grant: #------------------ # Funding_Agency # Funding_Agency_Name: University of California Lawrene Livermore National Laboratory # Grant: 01-ERI-009 #------------------ # Funding_Agency_Name: National Science Foundation # Grant:AGS-1304263 # Funding_Agency_Name: National Oceanic and Atmospheric Administration # Grant:NA14OAR4310176 #------------------ # Site_Information # Site_Name: South Pulau Langkai Island # Location: Ocean>Indian Ocean>Indonesia # Country: Indonesia # Northernmost_Latitude: -5.033333 # Southernmost_Latitude: -5.033333 # Easternmost_Longitude: 119.066667 # Westernmost_Longitude: 119.066667 # Elevation: -4 m #------------------ # Data_Collection # Collection_Name: 08indo01a # Earliest_Year: 1870 # Most_Recent_Year: 1990 # Time_Unit: y_ad # Core_Length: 2.3 m # Notes: {"database":"LMR"} previous name- Langkai2008coralc14 #------------------ # Species # Species_Name: Porites lutea # Common_Name: Finger coral #------------------ # Chronology: # # # # # # # # #---------------- # 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, , Corals and Sclerosponges, , ,N ##d14C delta age-corrected delta 14 Carbon, Porites lutea, , permil NBS oxalic acid, , Corals and Sclerosponges, d13C age correction, stable isotope mass spectrometry, N # #---------------- # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing Values: NAN # age d14C 1990.5 113 1990.35 102 1990.19 105 1990.04 113 1989.86 107 1989.68 109 1989.5 108 1989.35 114 1989.19 104 1989.04 117 1988.93 113 1988.81 109 1988.7 111 1988.58 116 1988.45 116 1988.31 122 1988.18 115 1988.04 119 1987.92 108 1987.79 101 1987.67 108 1987.46 100 1987.25 105 1987.04 115 1986.93 110 1986.81 110 1986.7 109 1986.58 108 1986.4 109 1986.22 113 1986.04 125 1985.92 123 1985.79 120 1985.67 122 1985.54 122 1985.42 117 1985.29 119 1985.17 123 1985.04 124 1984.92 120 1984.79 115 1984.67 118 1984.54 117 1984.42 120 1984.23 126 1984.04 126 1983.97 132 1983.89 121 1983.82 121 1983.74 114 1983.67 108 1983.61 117 1983.56 115 1983.5 121 1983.27 126 1983.04 120 1982.95 119 1982.86 121 1982.77 117 1982.67 115 1982.58 127 1982.4 130 1982.22 132 1982.04 139 1981.93 127 1981.81 130 1981.7 134 1981.58 121 1981.47 124 1981.36 125 1981.26 118 1981.15 129 1981.04 139 1980.89 125 1980.74 121 1980.58 122 1980.45 129 1980.31 135 1980.18 128 1980.04 137 1979.86 139 1979.68 140 1979.5 131 1979.41 131 1979.32 136 1979.23 140 1979.13 136 1979.04 137 1978.95 146 1978.86 139 1978.77 147 1978.68 142 1978.58 138 1978.45 138 1978.31 134 1978.18 138 1978.04 151 1977.95 145 1977.86 131 1977.77 133 1977.68 135 1977.58 136 1977.31 142 1977.04 153 1976.97 149 1976.89 138 1976.81 146 1976.74 137 1976.66 135 1976.58 131 1976.4 130 1976.22 148 1976.04 151 1975.93 143 1975.81 128 1975.7 127 1975.58 131 1975.4 137 1975.22 141 1975.04 160 1974.95 152 1974.86 133 1974.77 137 1974.68 134 1974.58 133 1974.4 127 1974.22 140 1974.04 163 1973.93 137 1973.81 110 1973.7 115 1973.58 116 1973.4 138 1973.22 151 1973.04 149 1972.98 149 1972.91 139 1972.85 132 1972.78 128 1972.71 127 1972.65 122 1972.58 117 1972.45 124 1972.31 135 1972.18 153 1972.04 133 1971.89 131 1971.74 125 1971.58 113 1971.45 117 1971.31 131 1971.18 153 1971.04 141 1970.89 121 1970.74 110 1970.58 99 1970.45 107 1970.31 122 1970.18 131 1970.04 148 1969.95 145 1969.86 114 1969.77 108 1969.67 101 1969.58 109 1969.45 117 1969.31 122 1969.18 132 1969.04 132 1968.89 107 1968.74 99 1968.58 94 1968.51 86 1968.43 95 1968.35 109 1968.27 112 1968.2 119 1968.12 136 1968.04 123 1967.93 108 1967.81 86 1967.7 85 1967.58 79 1967.4 82 1967.22 97 1967.04 130 1966.95 132 1966.86 57 1966.77 90 1966.67 69 1966.58 76 1966.45 71 1966.31 81 1966.18 75 1966.04 100 1965.97 97 1965.89 74 1965.81 56 1965.74 46 1965.66 41 1965.58 47 1965.45 44 1965.31 62 1965.18 84 1965.04 74 1964.95 42 1964.86 35 1964.77 30 1964.67 11 1964.58 14 1964.45 21 1964.31 23 1964.18 33 1964.04 31 1963.95 15 1963.86 16 1963.77 5 1963.67 -6 1963.58 -6 1963.4 -7 1963.22 -2 1963.04 9 1962.95 24 1962.86 1 1962.77 -3 1962.67 -4 1962.58 -14 1962.45 -11 1962.31 -7 1962.18 -10 1962.04 6 1961.95 3 1961.86 -3 1961.77 -17 1961.67 -25 1961.58 -26 1961.45 -22 1961.31 -12 1961.18 1 1961.04 -3 1960.95 -9 1960.86 -25 1960.77 -23 1960.67 -24 1960.58 -25 1960.45 -30 1960.31 -19 1960.18 -14 1960.04 -11 1959.98 -10 1959.93 -9 1959.87 -17 1959.81 -22 1959.76 -21 1959.7 -25 1959.64 -28 1959.58 -23 1959.47 -24 1959.37 -24 1959.26 -23 1959.15 -18 1959.04 -26 1958.97 -19 1958.89 -20 1958.81 -28 1958.74 -36 1958.66 -34 1958.58 -33 1958.51 -35 1958.43 -33 1958.35 -35 1958.27 -29 1958.2 -22 1958.12 -28 1958.04 -31 1957.95 -35 1957.85 -43 1957.76 -38 1957.67 -42 1957.56 -42 1957.46 -35 1957.35 -34 1957.25 -37 1957.15 -38 1957.04 -35 1956.95 -32 1956.86 -29 1956.77 -30 1956.67 -34 1956.58 -37 1956.52 -31 1956.45 -28 1956.38 -27 1956.31 -26 1956.24 -27 1956.18 -26 1956.11 -30 1956.04 -42 1955.97 -34 1955.89 -17 1955.81 -11 1955.74 -10 1955.66 -13 1955.58 -13 1955.51 -7 1955.43 -13 1955.35 -8 1955.27 -17 1955.2 -20 1955.12 -43 1955.04 -50 1954.95 -48 1954.86 -51 1954.77 -47 1954.67 -52 1954.58 -47 1954.49 -51 1954.4 -52 1954.31 -51 1954.22 -57 1954.13 -52 1954.04 -55 1953.95 -60 1953.86 -54 1953.77 -54 1953.67 -57 1953.58 -54 1953.53 -54 1953.47 -55 1953.42 -48 1953.37 -53 1953.31 -50 1953.26 -51 1953.2 -51 1953.15 -59 1953.1 -59 1953.04 -55 1952.98 -54 1952.93 -52 1952.87 -53 1952.81 -69 1952.76 -55 1952.7 -63 1952.64 -56 1952.58 -60 1952.49 -61 1952.4 -58 1952.31 -53 1952.22 -56 1952.13 -56 1952.04 -54 1951.95 -59 1951.86 -58 1951.77 -55 1951.67 -59 1951.58 -56 1951.47 -55 1951.37 -59 1951.26 -55 1951.15 -57 1951.04 -59 1950.93 -59 1950.81 -61 1950.7 -58 1950.58 -51 1950.49 -61 1950.4 -55 1950.31 -60 1950.22 -55 1950.13 -53 1950.04 -58 1949.93 -54 1949.81 -60 1949.7 -58 1949.58 -57 1949.47 -54 1949.37 -57 1949.26 -62 1949.15 -56 1949.04 -55 1948.97 -57 1948.89 -57 1948.81 -66 1948.74 -57 1948.66 -63 1948.58 -55 1948.45 -56 1948.31 -56 1948.18 -52 1948.04 -55 1947.95 -55 1947.86 -55 1947.77 -56 1947.68 -49 1947.59 -56 1947.5 -55 1947.39 -60 1947.27 -52 1947.16 -45 1947.04 -58 1946.98 -56 1946.92 -58 1946.85 -58 1946.79 -58 1946.73 -58 1946.67 -57 1946.51 -61 1946.35 -59 1946.2 -61 1946.04 -53 1945.97 -60 1945.89 -65 1945.82 -64 1945.74 -59 1945.67 -55 1945.51 -53 1945.35 -52 1945.2 -52 1945.04 -59 1944.98 -62 1944.93 -60 1944.87 -57 1944.81 -53 1944.76 -51 1944.7 -58 1944.64 -60 1944.58 -51 1944.45 -54 1944.31 -56 1944.18 -55 1944.04 -55 1943.91 -63 1943.77 -50 1943.64 -55 1943.5 -55 1943.42 -55 1943.35 -59 1943.27 -55 1943.19 -60 1943.12 -53 1943.04 -58 1942.96 -60 1942.88 NAN 1942.81 -55 1942.73 -56 1942.65 -57 1942.58 -59 1942.5 -57 1942.41 -54 1942.32 -55 1942.23 -61 1942.13 -57 1942.04 -56 1941.93 -56 1941.81 -59 1941.7 -64 1941.58 -49 1941.31 -56 1941.04 -52 1940.98 -55 1940.93 -49 1940.87 -58 1940.81 -56 1940.76 -58 1940.7 -57 1940.64 -54 1940.58 -59 1940.47 -57 1940.37 -54 1940.26 -55 1940.15 -55 1940.04 -65 1939.94 -58 1939.84 -59 1939.74 -51 1939.64 -57 1939.54 -53 1939.44 -59 1939.34 -60 1939.24 -56 1939.14 -57 1939.04 -49 1938.95 -52 1938.86 -53 1938.77 -54 1938.67 -53 1938.58 -49 1938.4 -53 1938.22 -59 1938.04 -52 1937.98 -51 1937.93 -51 1937.87 -53 1937.81 -52 1937.76 -51 1937.7 -53 1937.64 -53 1937.58 -52 1937.45 -53 1937.31 -52 1937.18 -54 1937.04 -56 1936.95 -56 1936.86 -55 1936.77 -61 1936.67 -62 1936.58 -58 1936.45 -57 1936.31 -56 1936.18 -75 1936.04 -56 1935.93 -51 1935.81 -55 1935.7 -53 1935.58 -56 1935.31 -56 1935.04 -58 1934.95 -52 1934.86 -58 1934.77 -53 1934.68 -53 1934.59 -56 1934.5 -56 1934.41 -57 1934.31 -63 1934.22 -55 1934.13 -58 1934.04 -50 1933.98 -59 1933.91 -64 1933.85 -57 1933.78 -58 1933.71 -59 1933.65 -54 1933.58 -54 1933.47 -61 1933.37 -58 1933.26 -54 1933.15 -48 1933.04 -55 1932.95 -54 1932.86 -57 1932.77 -58 1932.68 -56 1932.59 -55 1932.5 -59 1932.41 -58 1932.31 -51 1932.22 -49 1932.13 -54 1932.04 -60 1931.96 -59 1931.89 -54 1931.81 -51 1931.73 -55 1931.66 -61 1931.58 -53 1931.5 -56 1931.43 -58 1931.35 -52 1931.27 -56 1931.2 -56 1931.12 -56 1931.04 -61 1930.93 -63 1930.81 -52 1930.7 -58 1930.58 -56 1930.49 -56 1930.4 -60 1930.31 -55 1930.22 -53 1930.13 -57 1930.04 -58 1929.93 -57 1929.83 -55 1929.72 -54 1929.61 -56 1929.5 -57 1929.41 -53 1929.32 -54 1929.23 -56 1929.08 -59 1928.92 -51 1928.8 -56 1928.67 -48 1928.55 -51 1928.42 -50 1928.3 -50 1928.17 -50 1928.05 -48 1927.92 -55 1927.77 -54 1927.62 -55 1927.46 -47 1927.28 -52 1927.1 -56 1926.92 -55 1926.83 -50 1926.74 -55 1926.65 -56 1926.55 -60 1926.46 -53 1926.28 -52 1926.1 -51 1925.92 -45 1925.83 -54 1925.74 -51 1925.65 -51 1925.55 -51 1925.46 -55 1925.33 -52 1925.19 -55 1925.06 -59 1924.92 -54 1924.86 -56 1924.79 -58 1924.73 -58 1924.66 -62 1924.59 -59 1924.53 -59 1924.46 -59 1924.35 -59 1924.25 -55 1924.14 -53 1924.03 -54 1923.92 -58 1923.81 -57 1923.69 -51 1923.58 -51 1923.46 -61 1923.33 -56 1923.19 -46 1923.06 -54 1922.92 -54 1922.87 -55 1922.82 -54 1922.77 -58 1922.72 -58 1922.75 -59 1922.7 -49 1922.65 -51 1922.59 -52 1922.49 -47 1922.38 -55 1922.28 -51 1922.17 -50 1922.06 -55 1921.95 -53 1921.88 -55 1921.8 -58 1921.72 -61 1921.65 -54 1921.57 -48 1921.49 -53 1921.4 -50 1921.31 -51 1921.22 -55 1921.13 -51 1921.04 -50 1920.95 -55 1920.84 -50 1920.72 -48 1920.61 -51 1920.49 -48 1920.36 -50 1920.22 -51 1920 -59 1919.86 -55 1919.63 -55 1919.47 -49 1919.2 -54 1918.93 -47 1918.84 -48 1918.75 -54 1918.66 -53 1918.56 -56 1918.47 -57 1918.38 -52 1918.29 -54 1918.2 -59 1918.11 -56 1918.02 -52 1917.93 -57 1917.78 -63 1917.63 -54 1917.47 -60 1917.2 -59 1916.93 -41 1916.86 -58 1916.78 -54 1916.7 -52 1916.63 -56 1916.55 -57 1916.47 -51 1916.34 -51 1916.2 -58 1916 -61 1915.86 -59 1915.63 -55 1915.4 -57 1915.13 -58 1914.86 -55 1914.77 -57 1914.68 -58 1914.59 -56 1914.49 -57 1914.4 -51 1914.22 -52 1914.04 -58 1913.86 -49 1913.77 -59 1913.68 -59 1913.59 -57 1913.49 -59 1913.4 -61 1913.27 -60 1913.13 -54 1913 -54 1912.86 -57 1912.71 -58 1912.56 -60 1912.4 -57 1912.27 -50 1912.13 -50 1912 -50 1911.86 -50 1911.75 -48 1911.63 -51 1911.52 -49 1911.4 -51 1911.22 -50 1911.04 -54 1910.86 -53 1910.75 -54 1910.63 -57 1910.52 -54 1910.4 -58 1910.27 -55 1910.13 -55 1910 -51 1909.86 -52 1909.77 -51 1909.68 -54 1909.59 -53 1909.49 -51 1909.4 -57 1909.22 -58 1909.04 -52 1908.86 -57 1908.79 -56 1908.71 -58 1908.63 -52 1908.56 -57 1908.48 -57 1908.4 -49 1908.22 -44 1908.04 -48 1907.86 -48 1907.79 -54 1907.71 -47 1907.63 -49 1907.56 -58 1907.48 -52 1907.4 -53 1907.29 -55 1907.19 -55 1907.08 -52 1906.97 -48 1906.86 -54 1906.75 -53 1906.63 -53 1906.52 -56 1906.4 -53 1906.22 -52 1906.04 -51 1905.86 -49 1905.77 -61 1905.68 -50 1905.59 -55 1905.49 -56 1905.4 -64 1905.13 -58 1904.86 -63 1904.8 -50 1904.73 -51 1904.67 -53 1904.6 -58 1904.53 -48 1904.47 -58 1904.4 -55 1904.22 -54 1904.04 -56 1903.86 -57 1903.63 -48 1903.4 NAN 1903.29 -50 1903.19 -49 1903.08 -46 1902.97 -50 1902.86 -52 1902.77 -54 1902.68 -46 1902.59 -53 1902.49 -48 1902.4 -51 1902.29 -53 1902.19 -56 1902.08 -41 1901.97 -53 1901.86 -54 1901.77 -58 1901.68 -52 1901.59 -60 1901.49 -60 1901.4 -56 1901.22 -51 1901.04 -60 1900.86 -53 1900.75 -57 1900.63 -64 1900.52 -58 1900.4 -57 1900.13 -54 1899.86 -52 1899.71 -56 1899.56 -56 1899.4 -55 1899.13 -54 1898.86 -55 1898.71 -61 1898.56 -58 1898.4 -56 1898.22 -49 1898.04 -47 1897.86 -56 1897.71 -61 1897.56 -52 1897.4 -61 1897.29 -53 1897.19 -52 1897.08 -50 1896.97 -50 1896.86 -45 1896.63 -51 1896.4 -45 1896.22 -49 1896.04 -53 1895.86 -49 1895.5 -52 1895.13 -50 1894.77 -54 1894.4 -53 1894.52 -53 1894.63 -52 1894.75 -57 1894.86 -51 1894.75 -50 1894.63 -51 1894.52 -53 1894.4 -53 1894.31 -57 1894.22 -55 1894.13 -51 1894.04 -52 1893.95 -48 1893.86 -50 1893.75 -53 1893.63 -53 1893.52 -52 1893.4 -57 1893.27 -44 1893.13 -51 1893 -53 1892.86 -51 1892.71 -51 1892.56 -58 1892.4 -52 1892.13 -48 1891.86 -46 1891.75 -51 1891.63 -59 1891.52 -49 1891.4 -54 1891.27 -50 1891.13 -55 1891 -49 1890.86 -49 1890.71 -52 1890.56 -52 1890.4 -51 1890.13 -50 1889.86 -51 1889.75 -51 1889.63 -53 1889.52 NAN 1889.4 -55 1889.13 -58 1888.86 -57 1888.63 -60 1888.4 -52 1888.13 -52 1887.86 -59 1887.71 -57 1887.56 -58 1887.4 -55 1887.13 -54 1886.86 -53 1886.75 -51 1886.63 -51 1886.52 -54 1886.4 -49 1886.22 -48 1886.04 -53 1885.86 -57 1885.77 -49 1885.68 -54 1885.59 -51 1885.49 -56 1885.4 -52 1885.22 -53 1885.04 -51 1884.86 -53 1884.71 -58 1884.56 -49 1884.4 -43 1884.22 -46 1884.04 -51 1883.86 -45 1883.75 -50 1883.63 -56 1883.52 -50 1883.4 -48 1883.22 -46 1883.04 -48 1882.86 -60 1882.71 -48 1882.56 -51 1882.4 -54 1882.29 -46 1882.19 -54 1882.08 -50 1881.97 -47 1881.86 -47 1881.75 -54 1881.63 -53 1881.52 -44 1881.4 -47 1881.27 -50 1881.13 -45 1881 -48 1880.86 -43 1880.71 -43 1880.56 -41 1880.4 -40 1880.22 -42 1880.04 -41 1879.86 -44 1879.75 -46 1879.63 -42 1879.52 -43 1879.4 -46 1879.27 -47 1879.13 -50 1879 -46 1878.86 -39 1878.75 -42 1878.63 -41 1878.52 -39 1878.4 -45 1878.27 -46 1878.13 -46 1878 -50 1877.86 -50 1877.63 -48 1877.4 -51 1877.13 -46 1876.86 -49 1876.63 -51 1876.4 -48 1876.13 -49 1875.86 -51 1875.63 -41 1875.4 -47 1875.22 -41 1875.04 -51 1874.86 -47 1874.63 -37 1874.4 -40 1874.22 -43 1874.04 -47 1873.86 -41 1873.75 -38 1873.63 -39 1873.52 -46 1873.4 -49 1873.29 -46 1873.19 -51 1873.08 -46 1872.97 -45 1872.86 -48 1872.8 -48 1872.73 -50 1872.67 -54 1872.6 -54 1872.53 -55 1872.47 -55 1872.4 -53 1872.31 -53 1872.22 -48 1872.13 -49 1872.04 NAN 1871.95 -48 1871.86 -49 1871.71 -52 1871.56 -47 1871.4 -47 1871.22 -45 1871.04 -47 1870.86 -48 1871.71 -52 1871.56 -47 1871.4 -47 1871.22 -45 1871.04 -47 1870.86 -48