"Biologia" . "5"^^ . . . "Cladocera; palaeolimnology; climate change"@en . . . . . . . "13"^^ . . . "The long-term succession of cladoceran fauna and palaeoclimate forcing: A 14,600\u2013year record from Ple\u0161n\u00E9 Lake, the Bohemian Forest"@en . "[26354D57C114]" . "Pra\u017E\u00E1kov\u00E1, M." . . . "Zbytky perloo\u010Dek byly analyzov\u00E1ny v 543 cm dlouh\u00E9m vzorku sedimentu z Ple\u0161n\u00E9ho jezera na \u0160umav\u011B. Tento sediment pokr\u00FDv\u00E1 obdob\u00ED 11600 let od konce posledn\u00EDho zaledn\u011Bn\u00ED a\u017E po sou\u010Dasnost. Nejv\u00FDznamn\u011Bj\u0161\u00ED zm\u011Bny ve faun\u011B perloo\u010Dek nastaly 10500 let BP a vyvrcholily cca 10300 let BP s rozvojem lesa v povod\u00ED. Sou\u010Dasn\u00E9 ochuzen\u00ED fauny perloo\u010Dek bylo zp\u016Fsobeno kyselou depozic\u00ED ve 20. stolet\u00ED."@cs . . "Suppl. 20" . . "Dlouhodob\u00E1 sukcese fauny perloo\u010Dek a palaeoklimatick\u00E9 vlivy: 14600 let dlouh\u00FD z\u00E1znam z Ple\u0161n\u00E9ho jezera na \u0160umav\u011B"@cs . "Vesel\u00FD, J." . "A sediment record of cladoceran remains was analysed in a 543 cm long core from Ple\u0161n\u00E9 Lake, covering the time period from the Oldest Dryas to the present (11,600-yr period). The most important change in cladoceran fauna occurred at 10.5 kyr BP and culminated with forestation of the catchment around 10.3 kyr BP. The recent impoverishment of aquatic fauna was caused by acid deposition in the 20th century." . "Majer, V." . "S387;S399" . "RIV/60077344:_____/06:00080158!RIV07-AV0-60077344" . "483626" . . "The long-term succession of cladoceran fauna and palaeoclimate forcing: A 14,600\u2013year record from Ple\u0161n\u00E9 Lake, the Bohemian Forest"@en . "The long-term succession of cladoceran fauna and palaeoclimate forcing: A 14,600\u2013year record from Ple\u0161n\u00E9 Lake, the Bohemian Forest" . "Fott, J." . "A sediment record of cladoceran remains was analysed in a 543 cm long core from Ple\u0161n\u00E9 Lake, covering the time period from the Oldest Dryas to the present (11,600-yr period). The most important change in cladoceran fauna occurred at 10.5 kyr BP and culminated with forestation of the catchment around 10.3 kyr BP. The recent impoverishment of aquatic fauna was caused by acid deposition in the 20th century."@en . . . "1"^^ . "P(GA206/00/0063), Z(AV0Z60170517), Z(MSM0021620828), Z(MZP0002579801)" . "Dlouhodob\u00E1 sukcese fauny perloo\u010Dek a palaeoklimatick\u00E9 vlivy: 14600 let dlouh\u00FD z\u00E1znam z Ple\u0161n\u00E9ho jezera na \u0160umav\u011B"@cs . . "0006-3088" . "61" . "Kop\u00E1\u010Dek, Ji\u0159\u00ED" . "SK - Slovensk\u00E1 republika" . "The long-term succession of cladoceran fauna and palaeoclimate forcing: A 14,600\u2013year record from Ple\u0161n\u00E9 Lake, the Bohemian Forest" . . "RIV/60077344:_____/06:00080158" .