Effect of topographic position on differential biotic and lithological responses to the late glacial–early Holocene climatic oscillations recorded in sediments of two landslide fens (the Outer Western Carpathians, S Poland)
The Holocene: A Major Interdisciplinary Journal Focusing on Recent Environmental Change
Published online on January 18, 2026
Abstract
The Holocene, Volume 36, Issue 4, Page 457-471, April 2026.
Landslide fens are characteristic landforms of the Beskid Makowski Mountains area in the Outer Western Carpathians (S Poland) and contain rarely occurring late glacial and Holocene organic-minerogenic sedimentary sequences. Multi-proxy study (radiocarbon ...
Landslide fens are characteristic landforms of the Beskid Makowski Mountains area in the Outer Western Carpathians (S Poland) and contain rarely occurring late glacial and Holocene organic-minerogenic sedimentary sequences. Multi-proxy study (radiocarbon ...