Dendrochronologische Befunde zur jüngeren Flußgeschichte von Main, Fulda, Lahn und Oker

Delorme, Axel; Leuschner, Hanns Hubert

doi:10.3285/eg.33.1.05

Cited by 3 publications

(1 citation statement)

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“…Indeed, some regional studies carried out in central Europe have diagnosed fluctuations in watercourses during the Early Holocene based on morphodynamic and sedimentary criteria: Kalicki (2006) in Poland and Bielorussia, Becker and Schirmer (1977) as well as Delorme and Leuschner (1983), through the study of sub-fossil oak trunks deposited in Holocene valley fills in south-west Germany. Recently, quantitative studies carried out using cumulative probability distribution functions (CPDF) of 14 C ages pinpointed the major Holocene hydrological events in large areas or countries, especially for the mid-Holocene (Great Britain, Germany, Poland, Tunisia) (Starkel et al, 2006;Hoffmann et al, 2008;Zielhofer and Faust, 2008;Macklin et al, 2010).…”

Section: Introductionmentioning

confidence: 99%

A fluvial record of the mid-Holocene rapid climatic changes in the middle Rhone valley (Espeluche-Lalo, France) and of their impact on Late Mesolithic and Early Neolithic societies

Berger

Delhon

Magnin

et al. 2016

Quaternary Science Reviews

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Section: Introductionmentioning

confidence: 99%

A fluvial record of the mid-Holocene rapid climatic changes in the middle Rhone valley (Espeluche-Lalo, France) and of their impact on Late Mesolithic and Early Neolithic societies

Berger

Delhon

Magnin

et al. 2016

Quaternary Science Reviews

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Eichenstammlagen in Mooren und Talauen und die Klimaverschlechterung im Subboreal

Leuschner¹,

Delorme²,

Tüxen³

et al. 1985

Flora

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Progress in the holocene chrono-climatostratigraphy of Polish territory

Starkel

Michczyńska

Krąpiec³

et al. 2012

Geochronometria

159

123

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Abstract:The Holocene delivers a unique possibility to establish climatic stratigraphic boundaries based on detailed chronostratigraphy reflected in various facies of continental sediments, in their lithological parameters and organic remains. These sediments are dated by the 14 C method in the case of organic remains, by counting annual laminations in lacustrine facies, and by dendrochronological method in the case of fluvial sediments. The existence of well dated profiles enables to reconstruct various climatic parameters like amplitudes of seasonal temperatures, types and frequency of extreme rainfalls and floods and, finally, to distinguish rare rapid changes and most frequent gradual ones. This reconstruction is based on the analogous effects of various types of present-day rainfalls. The current authors present a critical review of existing chronostratigraphic divisions starting from simple millennial division by Mangerud based on Scandinavian palynological stratigraphy of peatbogs and Starkel's concept based on fluctuations in rainfall and runoff regime reflected in fluvial and other facies of continental deposits. In the last decades, the calibration of 14 C dates allowed a new approach to be used for the construction of the probability distribution function of these dates in various facies or types of sediments, which formed a background for distinguishing and correlating climatic phases and defining boundaries between them. These approaches have been creating new opportunities for revision of the existing chronostratigraphy. The aim of this paper is to present a revised version of chronostratigraphic division based on climatic fluctuations reflected in various facies of sediments on the territory of Poland and discuss their correlation with other European regions and global climatic changes.

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Dendrochronologische Befunde zur jüngeren Flußgeschichte von Main, Fulda, Lahn und Oker

Cited by 3 publications

References 0 publications

A fluvial record of the mid-Holocene rapid climatic changes in the middle Rhone valley (Espeluche-Lalo, France) and of their impact on Late Mesolithic and Early Neolithic societies

A fluvial record of the mid-Holocene rapid climatic changes in the middle Rhone valley (Espeluche-Lalo, France) and of their impact on Late Mesolithic and Early Neolithic societies

Eichenstammlagen in Mooren und Talauen und die Klimaverschlechterung im Subboreal

Progress in the holocene chrono-climatostratigraphy of Polish territory

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