Atmospheric circulation and the differentiation of precipitation sources during the Holocene inferred from five stalagmite records from Demänová Cave System (Central Europe)
Atmospheric circulation and the differentiation of precipitation sources during the Holocene inferred from five stalagmite records from Demänová Cave System (Central Europe)
Atmospheric circulation and the differentiation of precipitation sources during the Holocene inferred from five stalagmite records from Demänová Cave System (Central Europe)
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dc.type
JournalArticle
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dc.description.physical
834-846
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dc.description.additional
Bibliogr. s. 845-846
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dc.subject.en
local factors
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dc.subject.en
Low Tatra Mountains
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dc.subject.en
paleoclimate
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dc.subject.en
Slovakia
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dc.subject.en
speleothem
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dc.subject.en
stable carbon isotopes
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dc.subject.en
stable oxygen isotopes
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dc.description.volume
30
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dc.description.number
6
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dc.description.publication
2,1
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dc.identifier.doi
10.1177/0959683620902224
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dc.identifier.eissn
1477-0911
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dc.title.journal
Holocene
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dc.language.container
eng
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dc.affiliation
Wydział Geografii i Geologii : Instytut Nauk Geologicznych