Abstract

Beavers have lived in the territory of Poland since the beginning of the Holocene, as testified by bone remains found in archaeological sites of different ages. The area inhabited by these animals has experienced continuing transformations of terrain relief, geological structure, hydrology and plant cover. In Poland, beavers are partially protected and their population has spread in virtually every part of the country (except in the highest mountain ranges). The authors of this paper wish to present the results of field works carried out since 2006 in the Tuchola Forest (Polish Plain). This paper aims to identify the potential sediments of relict beaver ponds and their sedimentological features. The studies are also backed up with a description of radiocarbon dating of samples. The results indicate that beavers used to live in the Tuchola Forest in the Middle Ages, as shown by the radiocarbon dates and sequences of mineral–organic deposits found in exposures and geological boreholes. The spatial distribution of organic and mineral deposits in wider sections of river valleys can be explained by the avulsion of the riverbed downstream of the pond and by the distribution of ponds in the Gołyjonka valley. The discovery of relict beaver pond sediments suggests that the activity of these mammals in the Middle Ages played a major part in shaping the landscape of the valley. The results of studies clearly indicate that analyses of the valley sediment facies of small watercourses should take into account the role beavers played in the past in shaping the landscape of the analysed valley. This highlights the insufficiency of studies concerning the activity of beavers in river valleys.

Highlights

  • The area of the Polish Plain is situated in a temperate forest zone

  • This paper aims to provide an outline of studies carried out so far in the area of the Tuchola Forest (Polish Plain) that were oriented at exploring relict beaver ponds

  • In the valley suspended over the headwater recess, wood with beaver cuts extracted from sediments of the relict beaver pond was dated 1265 ± 40 BP (663–779 cal AD) [22]

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Summary

Introduction

The area of the Polish Plain is situated in a temperate forest zone. Beavers appeared in this territory immediately after the last deglaciation when the formation of a forest biome commenced [1,2,3,4]. Few studies carried out in valleys in Poland documented the presence of beaver pond sediments within Holocene alluvia [4,22,62]. The results of studies carried out in small river valleys in the Tuchola Forest indicate that it is necessary to verify the hypotheses on the origin of numerous deposits accumulated on alluvial plains in the Holocene and popularize claims formulated by many researchers about the considerable share of relict beaver pond sediments in materials building the bottoms of river valleys [27,28,29,30,31]. QQuuaalliittaattiivvee aannaallyysseess ooff mmaaccrroo--rreemmaaiinnss wweerree ccaarrrriieedd oouutt aanndd tthhee ccoonntteenntt ooff oorrggaanniicc mmaatttteerr wwaass tteesstteedd ffoorr oorrggaanniicc ddeeppoossiittss. Cat1i4ngdsatwinegres wcaelirbercaatleidbrwatiethd wthiethOtxhCeaOl 4x.C4a(lO4x.4fo(rOdxRfoadrdioRcardbioncaArbcocneleArcactoelreUrantoitr, OUxnfiot,rdO,xUfoKr)d[,7U3]Kp)r[o7g3r]apmromgeraumsimnge uthseincgaltihberactaiolinbrcautirovne cInutrCvaelI2n0tC[7a4l]2.0 [74]

Study Area
Sand Separating Layers of Peat
Wood in Peat and Sand
Findings
Discussion
Full Text
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