# 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/czec003r-crn-noaa.txt # Data_Download_Description: Raw Measurements - NOAA Template File; czec003r-crn-noaa.txt # # Related_Online_Resource: https://www.ncei.noaa.gov/pub/data/paleo/treering/chronologies/europe/czec003r.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 1591 0.908 1 1592 0.846 1 1593 1.592 1 1594 0.548 1 1595 1.017 1 1596 1.135 1 1597 0.732 1 1598 0.808 1 1599 0.833 1 1600 1.011 1 1601 0.901 1 1602 0.816 1 1603 0.781 1 1604 1.025 1 1605 1.461 1 1606 0.944 1 1607 1.399 1 1608 0.288 1 1609 0.902 1 1610 0.534 1 1611 0.859 1 1612 1.1 1 1613 0.801 1 1614 1.025 1 1615 0.761 1 1616 0.86 1 1617 0.978 1 1618 0.694 1 1619 1.164 1 1620 1.367 1 1621 1.31 1 1622 2.235 1 1623 0.814 1 1624 0.986 1 1625 1.372 1 1626 0.819 1 1627 1.164 1 1628 0.642 1 1629 1.072 1 1630 0.963 1 1631 0.9 1 1632 0.718 1 1633 0.987 1 1634 0.95 1 1635 1.177 1 1636 0.499 1 1637 1.809 1 1638 0.822 1 1639 1.085 1 1640 1.266 2 1641 1.352 2 1642 1.006 2 1643 0.676 2 1644 1.119 2 1645 0.897 2 1646 1.023 2 1647 0.828 2 1648 1.023 2 1649 0.802 2 1650 0.851 2 1651 1.229 2 1652 0.811 3 1653 0.762 3 1654 0.801 3 1655 1.154 4 1656 1.173 4 1657 0.943 4 1658 0.856 4 1659 0.933 4 1660 1.014 4 1661 0.825 4 1662 0.759 4 1663 1.12 4 1664 0.851 4 1665 1.016 4 1666 1.063 4 1667 0.977 4 1668 0.999 4 1669 0.914 4 1670 1.363 4 1671 0.825 4 1672 0.761 4 1673 0.988 4 1674 1.124 4 1675 1.082 4 1676 1.005 4 1677 1.053 4 1678 0.9 4 1679 0.834 4 1680 0.843 5 1681 1.168 5 1682 0.752 5 1683 0.922 5 1684 0.995 5 1685 0.893 5 1686 0.964 5 1687 1.003 5 1688 1.128 5 1689 1.122 5 1690 0.839 5 1691 1.069 5 1692 1.36 5 1693 0.877 5 1694 0.909 5 1695 0.888 6 1696 1 6 1697 1.103 6 1698 0.951 6 1699 1.07 6 1700 0.967 6 1701 0.744 6 1702 0.857 6 1703 1.052 6 1704 0.952 6 1705 0.87 6 1706 0.823 6 1707 0.84 6 1708 1.083 6 1709 1.007 6 1710 0.978 6 1711 1.042 6 1712 0.803 6 1713 1.159 6 1714 0.98 6 1715 0.751 7 1716 0.973 7 1717 1.078 7 1718 0.941 7 1719 0.861 7 1720 0.919 7 1721 1.047 7 1722 1.13 7 1723 1.284 7 1724 0.8 7 1725 0.92 7 1726 1.167 8 1727 1.045 8 1728 1.051 10 1729 1.05 10 1730 0.804 10 1731 1.062 10 1732 0.723 10 1733 0.881 11 1734 0.961 11 1735 0.946 12 1736 0.946 12 1737 0.999 12 1738 1.109 12 1739 1.061 13 1740 0.802 13 1741 1.034 13 1742 0.835 13 1743 0.808 13 1744 1.055 13 1745 0.88 13 1746 0.948 13 1747 0.972 13 1748 1.032 14 1749 0.918 14 1750 0.856 14 1751 0.987 14 1752 0.854 15 1753 0.855 15 1754 1.069 15 1755 1.144 15 1756 1.016 15 1757 1.088 15 1758 1.19 16 1759 0.984 16 1760 0.974 16 1761 1.152 16 1762 0.831 16 1763 1.108 16 1764 0.916 16 1765 0.989 16 1766 0.979 16 1767 0.956 16 1768 0.857 16 1769 1.03 16 1770 0.949 16 1771 1.004 17 1772 0.99 17 1773 0.92 17 1774 1.106 17 1775 0.9 18 1776 1.101 18 1777 1.062 18 1778 0.907 18 1779 0.91 18 1780 1.047 18 1781 0.931 18 1782 1.013 18 1783 1.028 18 1784 0.95 18 1785 0.998 18 1786 0.919 18 1787 0.847 18 1788 1.082 19 1789 1.054 19 1790 1.145 20 1791 0.851 20 1792 1.031 20 1793 1.071 20 1794 0.95 20 1795 0.995 20 1796 0.871 21 1797 0.98 22 1798 1.083 22 1799 0.851 22 1800 0.94 22 1801 0.822 23 1802 0.738 23 1803 0.98 23 1804 0.942 23 1805 0.81 23 1806 1.082 23 1807 1.027 23 1808 0.869 23 1809 1.126 23 1810 0.814 23 1811 0.876 23 1812 1.12 23 1813 0.912 23 1814 0.87 23 1815 1.006 23 1816 1.126 23 1817 1.039 23 1818 1.011 23 1819 0.96 23 1820 0.827 23 1821 1.075 23 1822 0.884 23 1823 0.878 23 1824 1.125 23 1825 1.027 23 1826 1.04 23 1827 1.127 23 1828 1.199 23 1829 0.867 23 1830 1.148 23 1831 1.088 23 1832 0.582 23 1833 1.212 23 1834 1.029 23 1835 0.984 23 1836 1.014 23 1837 0.734 23 1838 1 24 1839 0.917 24 1840 0.904 24 1841 0.957 24 1842 1.01 24 1843 0.946 24 1844 1.177 24 1845 0.877 25 1846 0.99 25 1847 1.079 26 1848 1.24 26 1849 0.717 26 1850 1.126 26 1851 1.08 26 1852 0.962 26 1853 1.096 26 1854 0.878 27 1855 1.011 27 1856 0.984 27 1857 0.979 27 1858 0.835 27 1859 1.039 28 1860 0.861 28 1861 1.034 28 1862 0.787 28 1863 1.03 28 1864 0.99 28 1865 1.175 28 1866 0.932 28 1867 0.682 28 1868 1.13 28 1869 1.053 28 1870 0.795 28 1871 0.773 28 1872 0.844 28 1873 1.184 28 1874 0.727 28 1875 1.273 28 1876 0.931 28 1877 0.884 28 1878 1.063 28 1879 0.877 28 1880 1.148 28 1881 0.983 28 1882 0.879 28 1883 1.145 28 1884 1.22 28 1885 0.997 28 1886 1.315 28 1887 0.935 28 1888 0.84 28 1889 0.964 28 1890 0.929 28 1891 0.936 28 1892 1.132 28 1893 0.883 28 1894 0.956 28 1895 0.956 28 1896 0.963 28 1897 0.981 28 1898 0.975 28 1899 1.086 28 1900 0.921 28 1901 0.972 28 1902 0.973 28 1903 0.799 28 1904 0.993 28 1905 1.136 28 1906 0.916 28 1907 0.912 28 1908 0.967 28 1909 0.922 28 1910 1.042 28 1911 0.921 28 1912 0.937 28 1913 1.09 28 1914 1.026 28 1915 0.905 28 1916 1.188 28 1917 0.846 28 1918 1.163 28 1919 0.889 28 1920 1.014 28 1921 1.076 28 1922 0.887 28 1923 0.922 28 1924 0.894 28 1925 1.153 28 1926 0.824 28 1927 1.004 28 1928 1.102 28 1929 1.048 28 1930 0.989 28 1931 0.656 28 1932 0.915 28 1933 0.922 28 1934 1.119 28 1935 0.997 28 1936 0.916 28 1937 0.919 28 1938 1.054 28 1939 1.023 28 1940 1.064 28 1941 1.11 28 1942 0.728 28 1943 0.986 28 1944 0.869 28 1945 1.105 28 1946 0.948 28 1947 1.055 28 1948 1.227 28 1949 1.074 28 1950 0.688 28 1951 1.068 28 1952 0.904 28 1953 1.086 28 1954 1.011 28 1955 1.254 28 1956 0.922 28 1957 1.047 28 1958 0.732 28 1959 0.847 28 1960 0.959 28 1961 1.095 28 1962 0.995 28 1963 1.273 28 1964 0.87 28 1965 1.043 28 1966 0.822 28 1967 0.993 28 1968 0.932 28 1969 0.944 28 1970 1.093 28 1971 1.209 28 1972 1.13 28 1973 0.948 28 1974 0.975 28 1975 1.024 28 1976 0.68 28 1977 0.855 28 1978 0.71 28 1979 0.879 28 1980 1.084 28 1981 0.714 28 1982 0.847 28 1983 0.831 28 1984 0.802 28 1985 1.152 28 1986 0.956 28 1987 0.869 28 1988 0.846 28 1989 0.983 28 1990 1.12 28 1991 1.039 28 1992 0.879 28 1993 0.902 28 1994 0.892 28 1995 0.915 28 1996 1.13 28 1997 1.051 28 1998 0.719 28 1999 1.386 28 2000 1.087 28 2001 1.049 28 2002 0.776 28 2003 1.179 28 2004 1.034 28 2005 0.821 28 2006 0.988 28 2007 0.913 28 2008 0.843 27 2009 1.171 25 2010 0.877 15