Table 2: Age-Depth relationship for samples from Whipray core 25B. Sedimentation rate, based on 210Pb analysis is 0.43 cm/yr +/- 0.07. Core was collected in 1997. | |||||||
Depth (cm) |
Years before present (ybp) |
Average Year | Positive error (ybp) |
Maximum year | Negative error (ybp) |
Minimum Year | Range of Years |
---|---|---|---|---|---|---|---|
2 | 4.66 | 1992 | 4.00 | 1993 | 5.72 | 1991 | 1991-1993 |
4 | 9.32 | 1988 | 8.00 | 1989 | 11.44 | 1986 | 1985-1989 |
6 | 13.98 | 1983 | 12.00 | 1985 | 17.16 | 1980 | 1979-1985 |
8 | 18.64 | 1978 | 16.00 | 1981 | 22.88 | 1974 | 1974-1981 |
10 | 23.30 | 1974 | 20.00 | 1977 | 28.60 | 1968 | 1968-1977 |
12 | 27.96 | 1969 | 24.00 | 1973 | 34.32 | 1963 | 1962-1973 |
14 | 32.62 | 1964 | 28.00 | 1969 | 40.04 | 1957 | 1956-1969 |
16 | 37.28 | 1960 | 32.00 | 1965 | 45.76 | 1951 | 1951-1965 |
18 | 41.94 | 1955 | 36.00 | 1961 | 51.48 | 1946 | 1945-1961 |
20 | 46.60 | 1950 | 40.00 | 1957 | 57.20 | 1940 | 1939-1957 |
22 | 51.26 | 1946 | 44.00 | 1953 | 62.92 | 1934 | 1934-1953 |
24 | 55.92 | 1941 | 48.00 | 1949 | 68.64 | 1928 | 1928-1949 |
26 | 60.58 | 1936 | 52.00 | 1945 | 74.36 | 1923 | 1922-1945 |
28 | 65.24 | 1932 | 56.00 | 1941 | 80.08 | 1917 | 1916-1941 |
30 | 69.90 | 1927 | 60.00 | 1937 | 85.80 | 1911 | 1911-1937 |
32 | 74.56 | 1922 | 64.00 | 1933 | 91.52 | 1905 | 1905-1933 |
34 | 79.22 | 1918 | 68.00 | 1929 | 97.24 | 1900 | 1899-1929 |
36 | 83.88 | 1913 | 72.00 | 1925 | 102.96 | 1894 | 1894-1925 |
38 | 88.54 | 1908 | 76.00 | 1921 | 108.68 | 1888 | 1888-1921 |
40 | 93.20 | 1904 | 80.00 | 1917 | 114.40 | 1883 | 1882-1917 |
42 | 97.86 | 1899 | 84.00 | 1913 | 120.12 | 1877 | 1876-1913 |
44 | 102.52 | 1894 | 88.00 | 1909 | 125.84 | 1871 | 1871-1909 |
46 | 107.18 | 1890 | 92.00 | 1905 | 131.56 | 1865 | 1865-1905 |
48 | 111.84 | 1885 | 96.00 | 1901 | 137.28 | 1860 | 1859-1901 |
50 | 116.50 | 1881 | 100.00 | 1897 | 143.00 | 1854 | 1854-1897 |
52 | 121.16 | 1876 | 104.00 | 1893 | 148.72 | 1848 | 1848-1893 |
54 | 125.82 | 1871 | 108.00 | 1889 | 154.44 | 1843 | 1842-1889 |
56 | 130.48 | 1867 | 112.00 | 1885 | 160.16 | 1837 | 1836-1885 |
58 | 135.14 | 1862 | 116.00 | 1881 | 165.88 | 1831 | 1831-1881 |
60 | 139.80 | 1857 | 120.00 | 1877 | 171.60 | 1825 | 1825-1877 |
62 | 144.46 | 1853 | 124.00 | 1873 | 177.32 | 1820 | 1819-1873 |
64 | 149.12 | 1848 | 128.00 | 1869 | 183.04 | 1814 | 1813-1869 |
66 | 153.78 | 1843 | 132.00 | 1865 | 188.76 | 1808 | 1808-1865 |
68 | 158.44 | 1839 | 136.00 | 1861 | 194.48 | 1803 | 1802-1861 |
70 | 163.10 | 1834 | 140.00 | 1857 | 200.20 | 1797 | 1796-1857 |
72 | 167.76 | 1829 | 144.00 | 1853 | 205.92 | 1791 | 1791-1853 |
74 | 172.42 | 1825 | 148.00 | 1849 | 211.64 | 1785 | 1785-1849 |
76 | 177.08 | 1820 | 152.00 | 1845 | 217.36 | 1780 | 1779-1845 |
78 | 181.74 | 1815 | 156.00 | 1841 | 223.08 | 1774 | 1773-1841 |
80 | 186.40 | 1811 | 160.00 | 1837 | 228.80 | 1768 | 1768-1837 |
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U.S. Department of the Interior, U.S. Geological Survey
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Last updated: 17 March, 2005 @ 09:07 AM (KP)