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Mid-Holocene humid periods reconstructed from calcite varves of the Lake Woserin sediment record (north-eastern Germany)

Dados Bibliográficos

ID12267453
AutoresMarkus Czymzik (0000-0003-1599-7643, Lund University, autor correspondente), Stefan Dreibrodt (0000-0003-4812-0258, Institute for Ecosystem Research, Christian-Albrechts University Kiel, Germany), Ingo Feeser (0000-0002-9618-5139, Institute for Pre- and Protohistory, Christian-Albrechts University Kiel, Germany), Florian Adolphi (0000-0003-0014-8753, Lund University), Achim Brauer (0000-0002-6655-9451, Section 5.2 Climate Dynamics and Landscape Evolution, GFZ German Research Centre for Geosciences, Germany)
Ano2016
Volume26
Fascículo6
Páginas935-946
Data de publicação2016-01-18
Peer ReviewedSim
Open AccessSim
TipoARTICLE
PeriódicoThe Holocene (JOURNAL)
Identificadores do periódicoISSN: 0959-6836 • E-ISSN: 1477-0911
EditoraSAGE Publishing (PUBLISHER • US)
DOI10.1177/0959683615622549
OpenAlexW2344970556
IdiomaEN
Citações recebidas4
Referências citadas35

Time-series of varve properties and geochemistry were established from varved sediments of Lake Woserin (north-eastern Germany) covering the recent period AD 2010–1923 and the mid-Holocene time-window 6400–4950 varve years before present (vyr BP) using microfacies analyses, x-ray fluorescence (μ-XRF) scanning, microscopic varve chronology, and 14 C dating. The microscopic varve chronology was compared with a macroscopic varve chronology for the same sediment interval. Calcite layer thickness during the recent period is significantly correlated to increases in local annual precipitation ( r = 0.46, p = 0.03) and reduced air-pressure ( r = −0.72, p 1 standard deviation calcite layer thickness depicts a negative wave train air-pressure anomaly centered over southern Europe, with north-eastern Germany at its northern frontal zone. Three centennial-scale intervals of thicker calcite layers around the mid-Holocene periods 6200–5900, 5750–5400, and 5300–4950 vyr BP might reflect humid conditions favoring calcite precipitation through the transport of Ca 2+ ions into Lake Woserin, synchronous to wetter conditions in Europe. Calcite layer thickness oscillations of about 88 and 208 years resemble the solar Gleissberg and Suess cycles suggesting that the recorded hydroclimate changes in north-eastern Germany are modified by solar influences on synoptic-scale atmospheric circulation. However, parts of the periods of thicker calcite layers around 5750–5400 and 5200 vyr BP also coincide with enhanced human catchment activity at Lake Woserin. Therefore, calcite precipitation during these time-windows might have further been favored by anthropogenic deforestation mobilizing Ca 2+ ions and/or lake eutrophication

Calcite · Chronology · Climatology · Geochemistry · Geography · Geomorphology · Holocene · Precipitation · Sediment · Varve · earthquake and tectonic studies · Geological formations and processes · Geology and Paleoclimatology Research · Geology · Oceanography · Paleontology

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Obras citantes distintas4
Citações por ano0,4
Intervalo de citações2016 - 2024 (9)
Velocidade de citaçãorecent
Altamente citadoNão
Tipos de citaçãoNeutras: 3
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