. "1"^^ . . . "Kru\u0161n\u00E9 hory - hornictv\u00ED a \u017Eivotn\u00ED prost\u0159ed\u00ED. Das Erzgebirge - Umwelt und Bergbau" . "St\u0159\u00EDbrn\u00E1 hore\u010Dka a vol\u00E1n\u00ED hor. Archeologie st\u0159edov\u011Bk\u00E9ho hornictv\u00ED v Sasku a \u010Cech\u00E1ch. Silberrauch und Berggeschrey. Arch\u00E4ologie des mittelalterlichen Bergbaus in Sachsen und B\u00F6hmen" . "1"^^ . "Ore Mts, palynology, stratigraphy, Quaternary, human impact, environment, climate"@en . . "S\u00E4chsisches Landesamt f\u00FCr Arch\u00E4ologie Dresden" . . . "Dresden" . . . "Kru\u0161n\u00E9 hory - hornictv\u00ED a \u017Eivotn\u00ED prost\u0159ed\u00ED. Das Erzgebirge - Umwelt und Bergbau"@cs . "Kru\u0161n\u00E9 hory - hornictv\u00ED a \u017Eivotn\u00ED prost\u0159ed\u00ED. Das Erzgebirge - Umwelt und Bergbau"@cs . "I" . "Kru\u0161n\u00E9 hory jsou z hlediska Evropy v\u00FDznamnou oblast\u00ED hornictv\u00ED a zpracov\u00E1n\u00ED rud a vedle \u0160umavy i druh\u00FDm nejbohat\u0161\u00EDm \u00FAzem\u00EDm na ra\u0161eli\u0161tn\u00ED komplexy v \u010Cesk\u00E9 republice. Pylov\u00E1 anal\u00FDza sediment\u016F byla provedena na Lokalit\u011B Bo\u017E\u00ED Dar - V rezervaci a Bo\u017E\u00ED Dar. Mocnost analyzovan\u00FDch sediment\u016F u prvn\u00EDho profilu byla 2,9 (3) m a druh\u00E9ho ca 1 m. Palynologick\u00E1 a stratigrafick\u00E1 anal\u00FDza profilu B. Dar - V rezervaci dokl\u00E1d\u00E1, \u017Ee sediment se za\u010Dal ukl\u00E1dat v pozdnoglaci\u00E1ln\u00ED dob\u011B podle klasifikace Firbase (1949, 1952)v dob\u011B nejstar\u0161\u00ED dryas - B\u00F6lling - mlad\u0161\u00ED dryas (anorganick\u00E9 sedimenty nebyly palynologicky analyzov\u00E1ny. Pylov\u00E1 anal\u00FDza ukazuje negativn\u00ED vliv \u010Dlov\u011Bka na ekosyst\u00E9my Kru\u0161n\u00FDch hor od po\u010D\u00E1tku 19. stolet\u00ED. Dokl\u00E1d\u00E1 to pokles pylov\u00FDch zrn smrku, buku, jedle (ty jsou typick\u00E9 pro nemlad\u0161\u00ED subatlatick\u00E9 obdob\u00ED), b\u0159\u00EDzy, ol\u0161e a n\u00E1stup zrn borovice. Pylov\u00E9 spektrum dokl\u00E1d\u00E1 trv\u00E1n\u00ED ra\u0161elini\u0161\u0165 v t\u00E9to oblasti od pozdn\u00EDho glaci\u00E1lu vpodstat\u011B dodnes."@cs . . "[07FDC941EA6C]" . . . "Kru\u0161n\u00E9 hory jsou z hlediska Evropy v\u00FDznamnou oblast\u00ED hornictv\u00ED a zpracov\u00E1n\u00ED rud a vedle \u0160umavy i druh\u00FDm nejbohat\u0161\u00EDm \u00FAzem\u00EDm na ra\u0161eli\u0161tn\u00ED komplexy v \u010Cesk\u00E9 republice. Pylov\u00E1 anal\u00FDza sediment\u016F byla provedena na Lokalit\u011B Bo\u017E\u00ED Dar - V rezervaci a Bo\u017E\u00ED Dar. Mocnost analyzovan\u00FDch sediment\u016F u prvn\u00EDho profilu byla 2,9 (3) m a druh\u00E9ho ca 1 m. Palynologick\u00E1 a stratigrafick\u00E1 anal\u00FDza profilu B. Dar - V rezervaci dokl\u00E1d\u00E1, \u017Ee sediment se za\u010Dal ukl\u00E1dat v pozdnoglaci\u00E1ln\u00ED dob\u011B podle klasifikace Firbase (1949, 1952)v dob\u011B nejstar\u0161\u00ED dryas - B\u00F6lling - mlad\u0161\u00ED dryas (anorganick\u00E9 sedimenty nebyly palynologicky analyzov\u00E1ny. Pylov\u00E1 anal\u00FDza ukazuje negativn\u00ED vliv \u010Dlov\u011Bka na ekosyst\u00E9my Kru\u0161n\u00FDch hor od po\u010D\u00E1tku 19. stolet\u00ED. Dokl\u00E1d\u00E1 to pokles pylov\u00FDch zrn smrku, buku, jedle (ty jsou typick\u00E9 pro nemlad\u0161\u00ED subatlatick\u00E9 obdob\u00ED), b\u0159\u00EDzy, ol\u0161e a n\u00E1stup zrn borovice. Pylov\u00E9 spektrum dokl\u00E1d\u00E1 trv\u00E1n\u00ED ra\u0161elini\u0161\u0165 v t\u00E9to oblasti od pozdn\u00EDho glaci\u00E1lu vpodstat\u011B dodnes." . "B\u0159\u00EDzov\u00E1, Eva" . "978-3-941171-99-2" . "RIV/00025798:_____/14:00000460!RIV15-MSM-00025798" . "8"^^ . . "25227" . . "Ore Mts - Mining and environment"@en . . "296"^^ . "Kru\u0161n\u00E9 hory - hornictv\u00ED a \u017Eivotn\u00ED prost\u0159ed\u00ED. Das Erzgebirge - Umwelt und Bergbau" . . "Ore Mts - Mining and environment"@en . . . . "RIV/00025798:_____/14:00000460" . "Ore Mts are the important area of mining and like \u0160umava Mts (Bohemian Forest)are the second riche area of the peat complexes in the Czech Republic. Pollen analysis of their sediments was carried out at the localities of Bo\u017E\u00ED Dar-V rezervaci ('In the reserve') and of Bo\u017E\u00ED Dar. The thickness of the first analysed section was c. 2.90 (3) m and that of the second c. 1 m. Palynological and stratigraphical analysis of the Bo\u017E\u00ED Dar-V rezervaci section clearly shows the peat bog to have started forming in the late glacial period (thickness of the sediment c. 0.5 m), according to the classification of Firbas (1949, 1952) in the I. oldest Dryas-B\u00F6lling-older Dryas period (the inorganic sandy sediments are not analysed palynologically. The pollen analysis shows an obviously negative impact of man on the Kru\u0161n\u00E9 hory ecosystems roughly from the early 19th century. The pollen spectrum has recorded an abrupt fall of pollen grains of some trees such as spruce (Picea), beech (Fagus), fir (Abies), birch (Betula), alder (Alnus) and an increase in number of grains of pine (Pinus), which is typical for the younger sub-Atlantic period. The peat bog at Bo\u017E\u00ED Dar is an example of an upland bog and both analysed sections represent a continuous vegetational evolution from the late glacial period up to the present day."@en .