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Multicore Study of Upper Holocene Mire Development in West-Frisia, Northern Netherlands

Ecological and Archaeological Aspects

Datos Bibliográficos

ID15801814
AutoresBas Van Geel (0000-0003-4432-320X, University of Amsterdam, autor de correspondencia), Otto Brinkkemper (0000-0003-3126-8459, Cultural Heritage Agency of Netherlands), Guido B A van Reenen (Institute for Biodiversity and Ecosystem Dynamics, University of Amsterdam, Science Park 904, 1098 XH Amsterdam, The Netherlands), Nathalie Van der Putten (0000-0002-0271-9321, Vrije Universiteit Amsterdam), Nathalie N L Van der Putten (Vrije Universiteit Amsterdam), Jasmijn E Sybenga (University of Amsterdam), C M Soonius (Archeologisch Diensten Centrum (Netherlands)), Carla Soonius (Archeologie West-Friesland, P.O. Box 603, 1620 AR Hoorn, The Netherlands), A M Kooijman (0000-0001-9177-632X, University of Amsterdam), Tom Hakbijl (Naturalis Biodiversity Center), William D Gosling (0000-0001-9903-8401, University of Amsterdam)
Año2020
Volumen3
Número2
Páginas12-12
Fecha de publicación2020-05-07
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaQuaternary (JOURNAL)
Identificadores de la revistaISSN: 2571-550X • E-ISSN: 2571-550X
EditorialMultidisciplinary Digital Publishing Institute (PUBLISHER • CH)
DOI10.3390/quat3020012
OpenAlexW3023530816
IdiomaEN
Referencias citadas31

We studied twelve late Holocene organic deposits in West-Frisia, The Netherlands. Pollen, spores, non-pollen palynomorphs, mosses, other botanical macrofossils and insect remains were recorded for reconstructions of changing environmental conditions. Eastern West-Frisia was a cultivated landscape during the Bronze Age, but it became a freshwater wetland in the Late Bronze Age. In most of our sites, radiocarbon dates show that time transgressive inundation of soils preceded the climate shift at 850 cal BC for several centuries. We suggest that solar forcing of climate change may have delivered the final push to the inundation and depopulation of West-Frisia, which had already commenced several centuries before, due to sealevel rise. We did not find evidence for significant Bronze Age tree growth in West-Frisia before the inundations. Vegetation successions in the new wetlands developed from shallow mineral-rich freshwater to rich-fen vegetation. Subsequently poor fen vegetation with birch and pine developed, and the natural succession led to ombrotrophic raised bog vegetation. Complete successions from shallow, mineral-rich lakes to raised bog lasted between 1000 and 1500 calendar years. We hypothesize that medieval drainage and reclamation became possible only when the mires of West-Frisia had reached the raised bog stage. Reclamation of raised bogs by medieval farmers (drainage, eutrophication, peat digging) caused compaction, oxidation and loss of the upper part of the peat deposit. Seeds of salt-tolerant and salt-demanding plant species indicate that the medieval sites were inundated during storm surges with brackish or salt water, which triggered the farmers to build artificial mounds and, later, dikes. Under mounds and dikes, peat deposits remained protected against further decay. With our data we deliver a long-term perspective on contemporary ecosystem dynamics of freshwater wetlands, relevant for nature conservation and future climate change

Archaeology · Bog · Geography · Holocene · Macrofossil · Midden · Mire · Ombrotrophic · Peat · Physical geography · Vegetation (pathology · Wetland · Aeolian processes and effects · Geology and Paleoclimatology Research · Ecology · Geology · Oceanography · Paleontology

  • What Is Natural? The Need for a Long-Term Perspective in Biodiversity Conservation

    Open Access•Katherine J Willis, H J B Birks•Science•2006

  • Paleoecological studies in the Klokkeweel bog near hoogkarspel (prov. of Noord-Holland)

    Open Access•J P Pals, Bas Van Geel et al.•Review of Palaeobotany and…•1980

  • Fossil ascomycetes in Quaternary deposits

    Bas Van Geel, André Aptroot•Nova Hedwigia•2006

  • Palaeoecology and stratigraphy of the lateglacial type section at Usselo (the Netherlands)

    Open Access•Bas Van Geel, G Russell Coope et al.•Review of Palaeobotany and…•1989

  • A palaeoecological study of an upper late glacial and holocene sequence from “de borchert”, The Netherlands

    Open Access•Bas Van Geel, S J P Bohncke et al.•Review of Palaeobotany and…•1980

  • A late holocene deposit under the Westfriese Zeedijk near Enkhuizen (Prov. of Noord-Holland, The Netherlands)

    Open Access•Bas Van Geel, D P Hallewas et al.•Review of Palaeobotany and…•1983

  • A palaeoecological study of holocene peat bog sections in Germany and The Netherlands, based on the analysis of pollen, spores and macro- and microscopic remains of fungi, algae, cormophytes and animals

    Open Access•Bas Van Geel•Review of Palaeobotany and…•1978

  • Bog burst in the eastern Netherlands triggered by the 2.8 kyr BP climate event

    Open Access•Bas Van Geel, Henk Heijnis et al.•The Holocene•2014

  • All’s well? Comparing on- and off-site pollen samples and exploring the potential of pollen from man-made contexts

    Open Access•Yvonne F van Amerongen•Vegetation History and…•2019

  • Environmental reconstruction of a Roman Period settlement site in Uitgeest (The Netherlands), with special reference to coprophilous fungi

    Open Access•Bas Van Geel, Janneke Buurman et al.•Journal of Archaeological Science•2003

  • IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP

    Open Access•Paula J Reimer, Edouard Bard et al.•Radiocarbon•2013

  • The Sharp Rise of Δ 14 C ca . 800 cal BC

    Open Access•Bas Van Geel, Johannes Van Der Plicht et al.•Radiocarbon•1997

  • No Country for Men

    Open Access•Yftinus Van Popta•European Journal of Archaeology•2019

  • Maritime Culture in the Netherlands

    Open Access•Yftinus Van Popta, Christer Westerdahl et al.•The International Journal of…•2018

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