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Climate of the Past An interactive open-access journal of the European Geosciences Union
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CP | Articles | Volume 14, issue 1
Clim. Past, 14, 85–100, 2018
https://doi.org/10.5194/cp-14-85-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
Clim. Past, 14, 85–100, 2018
https://doi.org/10.5194/cp-14-85-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 25 Jan 2018

Research article | 25 Jan 2018

Dendrochronologically dated pine stumps document phase-wise bog expansion at a northwest German site between ca. 6700 and ca. 3400 BC

Inke Elisabeth Maike Achterberg et al.

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Subject: Vegetation Dynamics | Archive: Terrestrial Archives | Timescale: Holocene
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Cited articles

Achterberg, I., Bauerochse, A., Giesecke, T., Metzler, A., and Leuschner, H.: Contemporaneousness of Trackway construction and environmental change: a dendrochronological study in Northwest-German mires, IANSA, 6, 19–29, 2015. 
Achterberg, I., Frechen, M., Bauerochse, A., Eckstein, J., and Leuschner, H. H.: The Goettingen tree-ring chronologies of peat-preserved oaks and pines from northwest Germany, ZDGG – German Journal of Geosciences (German J. Geol.), 168, 9–19, 2017. 
Achterberg, I. E. M., Eckstein, J., Birkholz, B., Bauerochse, A., Leuschner, H. H.: Dendrochronological dates of subfossil pines (Pinus sylvestris L.), relative dates of floating chronology, and peat stratigraphy from site “TOMO_south” at Totes Moor, northwest Germany, PANGAEA, https://doi.pangaea.de/10.1594/PANGAEA.884249, 2017. 
Achterberg, I. E. M., Eckstein, J., Birkholz, B. et al.: Dendrochronological dates of subfossil pines (Pinus sylvestris L.) of site TOMO_south, https://doi.pangaea.de/10.1594/PANGAEA.884247, 2017. 
Achterberg, I. E. M., Eckstein, J., Birkholz, B. et al.: Peat stratigraphy of site TOMO_south, https://doi.pangaea.de/10.1594/PANGAEA.884212, 2017. 
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Short summary
At a bog site at Totes Moor in northwest Germany a layer of pine tree stumps at the fen–bog transition was exposed by peat mining. The lateral expansion of ombrotrophic bog between 6703 BC and 3403 BC was reconstructed using the locations and dendrochronological dates of the tree stumps. The spatial pattern relates to the elevation a.s.l. of the mineral base beneath the peat. The temporal distribution of bog expansion pulses relates to climatic variation.
At a bog site at Totes Moor in northwest Germany a layer of pine tree stumps at the fen–bog...
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