# Samonil - Zofinsky prales - ABAL - ITRDB CZEC003 #---------------------------------------------------- # 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/19260 # 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-19260.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/czec003-crn-noaa.txt # Data_Download_Description: Raw Measurements - NOAA Template File; czec003-crn-noaa.txt # # Related_Online_Resource: https://www.ncei.noaa.gov/pub/data/paleo/treering/chronologies/europe/czec003.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 - ABAL - ITRDB CZEC003 #-------------------- # 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: CZEC003 # First_Year: 1587 # Last_Year: 2010 # Time_Unit: CE # Core_Length_m: # Parameter_Keywords: ring width # Notes: #-------------------- # Species # Species_Name: Abies alba Mill. # Common_Name: silver fir # Tree_Species_Code: ABAL #-------------------- # 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 1587 1.203 1 1588 1.051 1 1589 1.706 1 1590 0.892 1 1591 0.942 1 1592 0.771 1 1593 1.436 1 1594 0.747 1 1595 0.976 1 1596 1.091 1 1597 0.763 1 1598 0.732 1 1599 0.675 1 1600 0.83 1 1601 0.813 1 1602 0.746 1 1603 0.671 1 1604 0.861 1 1605 1.383 1 1606 1.154 1 1607 1.564 1 1608 0.581 1 1609 0.747 1 1610 0.322 1 1611 0.485 1 1612 0.808 1 1613 0.698 1 1614 0.935 1 1615 0.743 1 1616 0.763 1 1617 0.86 1 1618 0.62 1 1619 0.998 1 1620 1.346 1 1621 1.515 1 1622 2.567 1 1623 1.635 1 1624 1.464 1 1625 1.574 1 1626 1.025 1 1627 1.193 1 1628 0.684 1 1629 0.91 1 1630 0.873 1 1631 0.836 1 1632 0.656 1 1633 0.819 1 1634 0.841 1 1635 1.112 1 1636 0.574 1 1637 1.646 1 1638 1.091 1 1639 1.238 1 1640 1.314 2 1641 1.251 2 1642 1.169 2 1643 0.789 2 1644 1.018 2 1645 0.873 2 1646 0.975 2 1647 0.822 2 1648 0.955 2 1649 0.771 2 1650 0.742 2 1651 1.095 2 1652 0.818 3 1653 0.728 3 1654 0.698 3 1655 1.121 4 1656 1.006 4 1657 1.059 4 1658 1.064 4 1659 0.951 4 1660 0.962 4 1661 0.861 4 1662 0.757 4 1663 0.984 4 1664 0.881 4 1665 0.955 4 1666 0.99 4 1667 0.977 4 1668 0.931 4 1669 0.838 4 1670 1.068 4 1671 0.998 4 1672 0.842 4 1673 1.028 4 1674 1.16 4 1675 1.226 4 1676 1.17 4 1677 1.183 4 1678 0.989 4 1679 0.848 4 1680 0.846 5 1681 1.074 5 1682 0.796 5 1683 0.876 5 1684 0.878 5 1685 0.866 5 1686 0.918 5 1687 0.998 5 1688 1.201 5 1689 1.252 5 1690 1.08 5 1691 1.042 5 1692 1.384 5 1693 1.118 5 1694 1.193 5 1695 0.946 6 1696 0.942 6 1697 1.05 6 1698 0.862 6 1699 1.065 6 1700 1.021 6 1701 0.801 6 1702 0.813 6 1703 0.95 6 1704 0.91 6 1705 0.788 6 1706 0.814 6 1707 0.807 6 1708 0.888 6 1709 0.958 6 1710 1.02 6 1711 0.843 6 1712 0.813 6 1713 0.959 6 1714 0.958 6 1715 1.051 7 1716 0.95 7 1717 0.938 7 1718 0.98 7 1719 0.874 7 1720 0.757 7 1721 0.943 7 1722 1.02 7 1723 1.318 7 1724 0.921 7 1725 1.012 7 1726 1.104 8 1727 1.044 8 1728 1.059 10 1729 1.133 10 1730 0.925 10 1731 1.087 10 1732 0.787 10 1733 0.905 11 1734 0.929 11 1735 0.949 12 1736 0.882 12 1737 1.01 12 1738 1.061 12 1739 0.998 13 1740 0.896 13 1741 1.047 13 1742 0.812 13 1743 0.687 13 1744 0.85 13 1745 0.737 13 1746 0.842 13 1747 0.86 13 1748 0.986 14 1749 0.916 14 1750 0.827 14 1751 0.92 14 1752 0.851 15 1753 0.755 15 1754 1.015 15 1755 1.057 15 1756 1.044 15 1757 1.12 15 1758 1.141 16 1759 1.2 16 1760 1.131 16 1761 1.255 16 1762 0.972 16 1763 1.153 16 1764 1.003 16 1765 1.006 16 1766 1.012 16 1767 0.944 16 1768 0.874 16 1769 1.004 16 1770 0.905 16 1771 0.992 17 1772 0.994 17 1773 0.899 17 1774 0.991 17 1775 0.925 18 1776 1.055 18 1777 1.087 18 1778 1.031 18 1779 0.919 18 1780 0.996 18 1781 0.888 18 1782 0.937 18 1783 1.01 18 1784 0.974 18 1785 0.977 18 1786 0.908 18 1787 0.817 18 1788 0.976 19 1789 0.988 19 1790 1.162 20 1791 0.905 20 1792 1.02 20 1793 1.086 20 1794 1.011 20 1795 1.006 20 1796 0.931 21 1797 0.991 22 1798 1.151 22 1799 0.917 22 1800 0.903 22 1801 0.778 23 1802 0.633 23 1803 0.805 23 1804 0.805 23 1805 0.724 23 1806 0.987 23 1807 1.029 23 1808 0.911 23 1809 1.114 23 1810 0.896 23 1811 0.861 23 1812 1.068 23 1813 0.937 23 1814 0.873 23 1815 0.989 23 1816 1.113 23 1817 1.115 23 1818 1.115 23 1819 1.046 23 1820 0.856 23 1821 0.991 23 1822 0.857 23 1823 0.816 23 1824 1.018 23 1825 1.037 23 1826 1.057 23 1827 1.193 23 1828 1.29 23 1829 1.006 23 1830 1.215 23 1831 1.232 23 1832 0.726 23 1833 1.102 23 1834 1.03 23 1835 0.958 23 1836 1.063 23 1837 0.772 23 1838 0.908 24 1839 0.869 24 1840 0.856 24 1841 0.86 24 1842 0.936 24 1843 0.903 24 1844 1.149 24 1845 0.975 25 1846 1.037 25 1847 1.14 26 1848 1.294 26 1849 0.897 26 1850 1.125 26 1851 1.111 26 1852 1.017 26 1853 1.118 26 1854 0.926 27 1855 1.004 27 1856 0.978 27 1857 0.986 27 1858 0.825 27 1859 0.945 28 1860 0.828 28 1861 0.948 28 1862 0.748 28 1863 0.905 28 1864 0.899 28 1865 1.151 28 1866 1.04 28 1867 0.73 28 1868 1.009 28 1869 1.028 28 1870 0.826 28 1871 0.707 28 1872 0.68 28 1873 1.008 28 1874 0.716 28 1875 1.143 28 1876 1.014 28 1877 0.933 28 1878 1.071 28 1879 0.931 28 1880 1.136 28 1881 1.064 28 1882 0.959 28 1883 1.15 28 1884 1.316 28 1885 1.182 28 1886 1.455 28 1887 1.205 28 1888 0.981 28 1889 0.988 28 1890 0.917 28 1891 0.89 28 1892 1.079 28 1893 0.932 28 1894 0.934 28 1895 0.912 28 1896 0.917 28 1897 0.948 28 1898 0.938 28 1899 1.035 28 1900 0.955 28 1901 0.955 28 1902 0.951 28 1903 0.762 28 1904 0.868 28 1905 1.071 28 1906 0.941 28 1907 0.917 28 1908 0.93 28 1909 0.9 28 1910 0.995 28 1911 0.925 28 1912 0.921 28 1913 1.082 28 1914 1.062 28 1915 0.948 28 1916 1.172 28 1917 0.929 28 1918 1.187 28 1919 0.99 28 1920 1.034 28 1921 1.096 28 1922 0.96 28 1923 0.916 28 1924 0.867 28 1925 1.082 28 1926 0.874 28 1927 0.99 28 1928 1.094 28 1929 1.094 28 1930 1.071 28 1931 0.692 28 1932 0.772 28 1933 0.771 28 1934 0.964 28 1935 1.008 28 1936 0.926 28 1937 0.881 28 1938 1.012 28 1939 1.034 28 1940 1.112 28 1941 1.191 28 1942 0.833 28 1943 0.92 28 1944 0.805 28 1945 1.012 28 1946 0.96 28 1947 1.063 28 1948 1.276 28 1949 1.206 28 1950 0.83 28 1951 1.018 28 1952 0.892 28 1953 1.066 28 1954 1.053 28 1955 1.299 28 1956 1.103 28 1957 1.131 28 1958 0.785 28 1959 0.737 28 1960 0.818 28 1961 0.968 28 1962 1.008 28 1963 1.311 28 1964 1.04 28 1965 1.12 28 1966 0.905 28 1967 0.961 28 1968 0.911 28 1969 0.911 28 1970 1.063 28 1971 1.255 28 1972 1.29 28 1973 1.146 28 1974 1.111 28 1975 1.117 28 1976 0.745 28 1977 0.708 28 1978 0.533 28 1979 0.588 28 1980 0.836 28 1981 0.598 28 1982 0.639 28 1983 0.605 28 1984 0.552 28 1985 0.9 28 1986 0.9 28 1987 0.825 28 1988 0.801 28 1989 0.892 28 1990 1.067 28 1991 1.112 28 1992 0.975 28 1993 0.926 28 1994 0.87 28 1995 0.862 28 1996 1.066 28 1997 1.103 28 1998 0.826 28 1999 1.345 28 2000 1.249 28 2001 1.262 28 2002 0.973 28 2003 1.218 28 2004 1.159 28 2005 0.889 28 2006 0.956 28 2007 0.866 28 2008 0.782 27 2009 1.057 25 2010 0.907 15