Ecology and fluvial dynamics of an Early Holocene medium-sized European lowland river valley (Upper Scheldt, northern Belgium)

The fluvial environment of Early Holocene small- to middle-sized lowland rivers in northwest Europe is mostly unstudied due to a lack of preserved and accessible deposits. A rescue excavation in the Scheldt valley in northern Belgium offered the opportunity to study a Boreal alluvial succession in d...

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Bibliographic Details
Published in:Boreas
Main Authors: Storme, Annelies, Bastiaens, Jan, Crombé, Philippe, Debruyne, Sofie, Louwye, Stephen, Deforce, Koen
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Earth and Environmental Sciences
Archaeology
Geology
Ecology
Evolution
Behavior and Systematics
DIJLE CATCHMENT
ICE-CORE
SEDIMENTATION
SUCCESSION
STRATIGRAPHY
FLOODPLAINS
ENVIRONMENT
DEPOSITS
RECORDS
ice core
Online Access:https://biblio.ugent.be/publication/8621599
http://hdl.handle.net/1854/LU-8621599
https://doi.org/10.1111/bor.12362
https://biblio.ugent.be/publication/8621599/file/8621600
Description
Summary:The fluvial environment of Early Holocene small- to middle-sized lowland rivers in northwest Europe is mostly unstudied due to a lack of preserved and accessible deposits. A rescue excavation in the Scheldt valley in northern Belgium offered the opportunity to study a Boreal alluvial succession in detail. The results of palaeoecological and sedimentological analyses (diatoms, pollen, botanical macro-remains, molluscs, grain size) characterize the biotic and physical environment in the middle reach of this medium-sized river system. Although the Early Holocene in the Scheldt Basin has often been portrayed as a period of fluvial stability with marshy conditions and diffuse discharge, this study showed evidence of point bar formation by a small, low-energy meandering river between similar to 9.5 and similar to 8.8cal. ka BP. The point bar was at least temporarily vegetated and shows a shift from herbaceous riparian vegetation to an open willow-dominated alluvial forest. This evidence points to a more open vegetation and a more energetic environment than traditionally described for rivers of this size and age. A link to the 9.3 ka BP cooling event is suggested and possible reasons for the scarcity of records of this type of deposits are discussed.

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