Vývoj přírodního prostředí Českého krasu v holocénu na podkladě malakostratigrafických analýz
Holocene environmental history of the Czech Karst on the basis of malacostratigraphic analyses
dissertation thesis (DEFENDED)
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http://hdl.handle.net/20.500.11956/95054Identifiers
Study Information System: 198282
Collections
- Kvalifikační práce [19062]
Author
Advisor
Referee
Juřičková, Lucie
Kovanda, Jiří
Faculty / Institute
Faculty of Science
Discipline
Geology with Specialisation
Department
Institute of Geology and Paleontology
Date of defense
19. 6. 2006
Publisher
Univerzita Karlova, Přírodovědecká fakultaLanguage
Czech
Grade
Pass
Introduction The faunal response to crimatic- and vegetal change during the HolocenelPostglacial) is known in far. r.t. a.ti'r,' although the information issufficient ťor certain amongst invertebrates f::'lť ^* ."*uT' regions. Molluscs are unusual potentrally be ","o t3"'i3;.::"'::;:.T *;:Í..Ti:,T$#T:j, ""*Ípalaeoenvironmental questions. rne mosi vatuable sequeň",?i^oliiou,rythose that are continuous' cover long periods of time and furnish fossilassemblages that faithfulty reflect tn.li"i"g ""mmunities, from whicrr trrey''r ere derived. Relatively few deposits "onřuini.'g molluscs fulfill all these :HÍ:^ but calcareous tufa áeposits ;;;^ thes. ..qui,"-.n;; ]; i".g" The czech Karst' formed by pareozoic limestone and rocated in the centrarpart of Bohemia between |.tl ana zaliě, is an area with numerousieposits of calcareous tufa. In this karst area about 70 localities are know "rhere calcareous tufa precipitates or was deposited in the past. (Kovanda]971: Ložek 1992;Kaď1ecoia a Žat, rqďsl. '"" Purpose of dissertation The purpose of submitted work is to give the characteristicpaleoenvironmental development of selected io"uiiti", in the Czech řarst'and to complete existing- knowledge utout it. environmentar developmentrn this karst area during Holocene p"eriod- --'- rnls worl( comes from data acquired from a...
Introduction The faunal response to crimatic- and vegetal change during the HolocenelPostglacial) is known in far. r.t. a.ti'r,' although the information issufficient ťor certain amongst invertebrates f::'lť ^* ."*uT' regions. Molluscs are unusual potentrally be ","o t3"'i3;.::"'::;:.T *;:Í..Ti:,T$#T:j, ""*Ípalaeoenvironmental questions. rne mosi vatuable sequeň",?i^oliiou,rythose that are continuous' cover long periods of time and furnish fossilassemblages that faithfulty reflect tn.li"i"g ""mmunities, from whicrr trrey''r ere derived. Relatively few deposits "onřuini.'g molluscs fulfill all these :HÍ:^ but calcareous tufa áeposits ;;;^ thes. ..qui,"-.n;; ]; i".g" The czech Karst' formed by pareozoic limestone and rocated in the centrarpart of Bohemia between |.tl ana zaliě, is an area with numerousieposits of calcareous tufa. In this karst area about 70 localities are know "rhere calcareous tufa precipitates or was deposited in the past. (Kovanda]971: Ložek 1992;Kaď1ecoia a Žat, rqďsl. '"" Purpose of dissertation The purpose of submitted work is to give the characteristicpaleoenvironmental development of selected io"uiiti", in the Czech řarst'and to complete existing- knowledge utout it. environmentar developmentrn this karst area during Holocene p"eriod- --'- rnls worl( comes from data acquired from a...