# Samonil - Zofinsky prales - FASY - ITRDB CZEC004 #---------------------------------------------------- # 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/19261 # 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-tree-19261.json # Study_Level_JSON_Description: JSON metadata of this data file's parent study, which includes all study metadata. # # Data_Type: Tree Ring # # Dataset_DOI: # # Science_Keywords: #-------------------- # Resource_Links # # Data_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/treering/measurements/europe/czec004r-crn-noaa.txt # Data_Download_Description: Raw Measurements - NOAA Template File; czec004r-crn-noaa.txt # # Related_Online_Resource: https://www.ncei.noaa.gov/pub/data/paleo/treering/chronologies/europe/czec004r.crn # Related_Online_Description: CRN File; Chronology - Tucson Decadal File # #-------------------- # Contribution_Date # Date: 2015-08-07 #-------------------- # File_Last_Modified_Date # Date: 2015-08-07 #-------------------- # Title # Study_Name: Samonil - Zofinsky prales - FASY - ITRDB CZEC004 #-------------------- # Investigators # Investigators: Šamonil, P.; Doleželová, P.; Vašíčková, I.; Adam, D.; Valtera, M.; Král, K.; Janík, D.; Šebková, B. #-------------------- # Description_Notes_and_Keywords # Description: NOAA Template Chronology file added 2018-12-19. NOAA Template Raw Measurements file added 2019-02-05. #-------------------- # Publication # Authors: Pavel Šamonil, Petra Doleželová, Ivana Vašíčková, Dušan Adam, Martin Valtera, Kamil Král, David Janík and Barbora Šebková # Journal_Name: Journal of Vegetation Science # Published_Title: Individual-based approach to the detection of disturbance history through spatial scales in a natural beech-dominated forest # Published_Date_or_Year: 2013 # Volume: 24 # Pages: 1167-1184 # Issue: 6 # Report_Number: # DOI: 10.1111/jvs.12025 # Full_Citation: None # Abstract: We connected tree-census and dendrochronological research data (74.2 ha) in order to answer the following questions: How do we apply an individual-based approach, which allows us to abandon the traditional patch model, in the research of disturbance history through spatial scales? What is the disturbance history of the natural forest? How do we understand the influence of the Kyrill storm, which affected the reserve on 18 January 2007? How does the disturbance history in dendrochronological records correspond to real disturbances? # Location # # Žofínský Prales (48 °40′ N, 14 °42′ E, 735-830 m a.s.l., granite, Czech Republic) # Methods # # Repeated tree-censuses (>20 000 trees) were carried out in 1975, 1997 and 2008. These surveys served as the basis of dendrochronological research, during which 3 020 trees were sampled. A boundary line (BL) approach and geostatistical techniques were used to detect disturbance intensity and its spatial pattern. # Results # # The mean disturbance rate was 11.0% canopy loss per decade (maximum 33.7%) in the core zone. Bordering forests were directly affected by humans after 1800. A maximum of nine disturbance events were recorded per tree, but there were also 3% of non-suppressed trees without records of disturbance events. The Kyrill storm represented a singular event in the forest history from the point of view of its exceptional spatial pattern (ranges up to 320.0 m), but not from the perspective of disturbance intensity. The relationship between disturbance intensity (y) and the range of spatial autocorrelation (x) can be explained by the equation y = 10.6863 + 0.0783*x (R2 = 0.546, P = 0.009). The spatial variability of releases ≥50% of BL corresponds to real disturbance events, while the insertion of weak releases led to the overestimation of range. The frequency of releases was affected by a decrease in air pollution at the beginning of the 1990s. # Conclusions # # Effects of small-scale disturbances predominate in forest dynamics. Disturbance intensity was often not directly in accordance with the range of spatial autocorrelation. The ecological role of disturbance is therefore biased if disturbance intensity is used as the sole criterion. The results suggest the importance of historical and geographical contingency in ecosystem development. #-------------------- # Funding_Agency # Funding_Agency_Name: # Grant: #-------------------- # Site_Information # Site_Name: Zofinsky prales # Location: Czech Republic # Northernmost_Latitude: 48.6667 # Southernmost_Latitude: 48.6667 # Easternmost_Longitude: 14.7 # Westernmost_Longitude: 14.7 # Elevation_m: 785 #-------------------- # Data_Collection # Collection_Name: CZEC004 # First_Year: 1603 # Last_Year: 2010 # Time_Unit: CE # Core_Length_m: # Parameter_Keywords: ring width # Notes: #-------------------- # Species # Species_Name: Fagus sylvatica L. # Common_Name: European beech # Tree_Species_Code: FASY #-------------------- # 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 format: shortname-tab-var components: what, material, error, units, seasonality, data type, detail, method, C or N for Character or Numeric data) # ## age_CE age,,,year Common Era,,tree ring,,,N, ## trsgi tree ring standardized growth index,,,,,tree ring,composited,standard chronology method,N, ## numsamp number of samples,,,count,,tree ring,,,N, #--------------------- # Data: # Missing_Values: NA age_CE trsgi numsamp 1613 1.491 1 1614 0.568 1 1615 0.671 1 1616 0.975 1 1617 1.399 1 1618 1.737 1 1619 1.586 1 1620 2.046 1 1621 0.945 1 1622 0.568 1 1623 0.896 1 1624 0.806 1 1625 0.867 1 1626 0.799 1 1627 0.858 1 1628 0.538 1 1629 1.326 1 1630 1.125 1 1631 1.162 1 1632 0.483 1 1633 0.685 1 1634 1.367 1 1635 1.536 1 1636 0.469 1 1637 0.734 1 1638 0.798 1 1639 2.601 1 1640 0.894 1 1641 0.928 1 1642 1.618 1 1643 1.202 1 1644 -0.091 1 1645 0.885 1 1646 1.118 1 1647 1.339 1 1648 1.423 1 1649 0.601 1 1650 1.244 1 1651 0.415 1 1652 0.661 1 1653 1.142 1 1654 0.685 1 1655 0.923 1 1656 0.258 1 1657 0.518 1 1658 0.519 1 1659 0.448 1 1660 0.718 1 1661 0.643 1 1662 1.263 1 1663 0.957 1 1664 1.438 1 1665 1.042 1 1666 1.163 1 1667 0.959 1 1668 0.64 1 1669 0.668 1 1670 0.703 1 1671 1.846 1 1672 1.616 1 1673 1.014 1 1674 0.803 1 1675 0.612 1 1676 1.095 1 1677 0.912 2 1678 1.206 2 1679 0.576 2 1680 1.398 2 1681 1.279 2 1682 1.239 2 1683 1.285 2 1684 1.042 2 1685 0.893 2 1686 1.24 2 1687 0.742 2 1688 1.078 3 1689 0.855 3 1690 1.269 3 1691 1.394 3 1692 0.985 3 1693 1.17 3 1694 0.982 3 1695 1.165 3 1696 0.894 3 1697 0.868 3 1698 0.789 3 1699 0.722 3 1700 0.858 3 1701 0.793 3 1702 0.582 3 1703 1.129 3 1704 1.437 3 1705 0.954 3 1706 0.672 3 1707 0.993 3 1708 0.912 3 1709 0.943 3 1710 1.218 3 1711 0.748 3 1712 0.694 3 1713 0.995 3 1714 0.756 3 1715 1.037 3 1716 0.67 3 1717 0.737 3 1718 1.349 3 1719 1.321 3 1720 1.834 3 1721 1.072 3 1722 0.826 6 1723 1.146 6 1724 0.945 6 1725 1.034 6 1726 0.98 6 1727 1.126 6 1728 0.957 6 1729 0.895 6 1730 1.078 7 1731 0.839 7 1732 0.783 7 1733 0.958 7 1734 0.986 10 1735 0.901 10 1736 0.846 10 1737 0.844 10 1738 1.262 10 1739 0.932 11 1740 0.994 11 1741 1.269 12 1742 1.049 13 1743 1.005 14 1744 0.873 14 1745 1.045 14 1746 1.06 14 1747 1.022 15 1748 0.961 15 1749 0.937 15 1750 0.973 16 1751 0.97 16 1752 0.834 17 1753 0.955 18 1754 1.06 18 1755 0.909 19 1756 0.858 19 1757 0.967 20 1758 0.904 20 1759 0.894 20 1760 1.16 21 1761 0.833 21 1762 0.766 21 1763 1.044 21 1764 1.081 21 1765 0.935 21 1766 0.948 21 1767 1.009 21 1768 1.017 22 1769 1.174 22 1770 0.876 22 1771 1.026 23 1772 0.961 23 1773 1.072 23 1774 0.983 23 1775 1.079 23 1776 1.089 24 1777 1.107 24 1778 0.89 24 1779 0.981 24 1780 0.981 24 1781 0.95 24 1782 0.897 24 1783 0.94 24 1784 1.034 24 1785 0.969 24 1786 1.089 24 1787 0.878 25 1788 0.966 25 1789 1.034 26 1790 0.983 27 1791 0.835 27 1792 0.924 27 1793 0.79 27 1794 0.897 27 1795 0.924 27 1796 0.816 27 1797 0.89 27 1798 0.917 27 1799 0.985 27 1800 0.873 28 1801 0.865 29 1802 0.897 29 1803 0.889 30 1804 0.884 30 1805 1.068 30 1806 0.816 30 1807 1.09 30 1808 1.112 30 1809 1.053 30 1810 1.079 30 1811 0.941 30 1812 0.948 30 1813 1.059 31 1814 1.02 31 1815 1.023 31 1816 1.022 31 1817 0.948 31 1818 0.997 31 1819 1.034 31 1820 0.997 31 1821 0.926 33 1822 1.037 33 1823 0.897 33 1824 1.092 33 1825 0.916 33 1826 1.02 33 1827 0.932 33 1828 1.163 34 1829 0.989 34 1830 0.879 35 1831 0.995 35 1832 0.824 36 1833 0.935 37 1834 0.961 37 1835 1.029 37 1836 0.921 37 1837 1.035 38 1838 0.98 38 1839 0.944 38 1840 0.807 38 1841 1.017 38 1842 0.815 39 1843 1.061 39 1844 0.87 39 1845 1.008 39 1846 0.973 39 1847 1.128 39 1848 1.061 39 1849 0.959 40 1850 0.986 42 1851 1.081 42 1852 1.095 43 1853 1.022 44 1854 0.987 44 1855 1.084 44 1856 1.034 45 1857 0.895 45 1858 1.159 45 1859 0.83 45 1860 1.134 46 1861 0.809 46 1862 1.102 47 1863 0.89 47 1864 1.085 47 1865 0.896 47 1866 0.874 49 1867 0.716 51 1868 0.981 55 1869 1.018 55 1870 0.766 57 1871 0.991 58 1872 1.045 61 1873 0.977 61 1874 0.988 62 1875 0.867 65 1876 0.954 66 1877 0.61 71 1878 0.953 73 1879 1.049 75 1880 1.123 81 1881 0.834 83 1882 1.058 86 1883 0.933 90 1884 1.035 93 1885 1.144 96 1886 0.898 100 1887 1 103 1888 0.985 107 1889 0.962 111 1890 1.05 112 1891 1.196 117 1892 0.995 119 1893 1.04 121 1894 0.96 122 1895 1.075 123 1896 1.04 125 1897 0.948 125 1898 0.964 128 1899 1.032 129 1900 1.068 131 1901 0.935 131 1902 1.03 132 1903 1.075 135 1904 1.008 136 1905 0.949 141 1906 1.04 143 1907 1.045 144 1908 0.899 146 1909 1.075 146 1910 1.022 147 1911 1.036 149 1912 1.079 150 1913 0.965 150 1914 0.739 151 1915 0.631 152 1916 0.981 152 1917 1.113 152 1918 1.174 152 1919 0.726 152 1920 0.946 152 1921 0.855 152 1922 0.974 152 1923 0.891 152 1924 1.104 152 1925 0.946 152 1926 1.113 152 1927 0.971 152 1928 0.714 152 1929 0.758 152 1930 1.086 153 1931 0.91 153 1932 1.083 153 1933 1.367 153 1934 1.047 153 1935 1.103 153 1936 0.84 153 1937 1.007 153 1938 0.913 153 1939 1.12 155 1940 0.946 156 1941 0.807 156 1942 1.119 156 1943 0.846 156 1944 1.385 156 1945 1.026 156 1946 0.739 156 1947 0.986 156 1948 1.118 156 1949 0.868 156 1950 1.045 156 1951 0.849 156 1952 0.921 156 1953 0.849 156 1954 0.925 156 1955 1.116 156 1956 0.955 156 1957 0.943 156 1958 0.916 156 1959 1.281 156 1960 0.909 157 1961 1.084 157 1962 1.06 157 1963 0.782 157 1964 0.946 157 1965 1.117 158 1966 0.825 159 1967 1.083 161 1968 1.351 161 1969 0.861 162 1970 1.075 164 1971 1.007 167 1972 1.018 169 1973 0.978 169 1974 1.016 171 1975 1.14 171 1976 0.987 172 1977 0.76 173 1978 0.864 174 1979 0.689 174 1980 0.961 174 1981 0.999 174 1982 1.334 174 1983 1.073 174 1984 0.895 175 1985 0.83 176 1986 0.893 177 1987 0.906 177 1988 1.21 178 1989 1.107 178 1990 1.17 178 1991 0.977 178 1992 1.029 178 1993 1.005 178 1994 1.108 178 1995 0.849 178 1996 0.748 178 1997 1.104 178 1998 1.146 178 1999 0.977 178 2000 0.781 178 2001 1.047 178 2002 0.992 178 2003 0.881 178 2004 0.981 178 2005 0.886 178 2006 0.885 178 2007 1.08 168 2008 1.15 159 2009 1.202 85 2010 1.092 13