Klaus Dittmers
Alfred Wegener Institute for Polar and Marine Research
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Publication
Featured researches published by Klaus Dittmers.
Polar Research | 2002
Ruediger Stein; Frank Niessen; Klaus Dittmers; Michael Levitan; F. Schoster; Johannes Simstich; Tatjana Steinke; O. Stepanets
The extent of the Barents-Kara Ice Sheet during the eastern Last Glacial Maximum (LGM) is not yet fully known. A detailed echo-sounding survey performed during the Boris Petrov Expedition 2001 permitted the detailed mapping of part of it. Based on the profiling results, a southern connection between the LGM Barents-Kara Ice Sheet and a local ice sheet on Taymyr Peninsula appears to be unlikely. Based on sediment core data and profiling results, most of the terrigenous river-derived material accumulated in the estuaries during late Holocene times, whereas during early Holocene times of lowered sea level major amounts were transported further offshore and accumulated on the shelf. During the post-glacial sea level rise, the main depocentre migrated southward, reaching its present position no earlier than about 6 cal. Ky BP (or 5.2 Kya). Future studies of accelerator mass spectrometry (AMS) 14C-dated sediment cores will allow a detailed reconstruction of the variability of fluvial sediment discharge and the history of glaciation in the Kara Sea during late Quaternary times.
Quaternary Science Reviews | 2004
Rüdiger Stein; Klaus Dittmers; Kirsten Fahl; M. Kraus; Jens Matthiessen; Frank Niessen; Martina Pirrung; Yelena I. Polyakova; F. Schoster; Tatjana Steinke; Dieter K Fütterer
EPIC3Proceedings in Marine Sciences, Vol. 6, Elsevier Amsterdam, p., pp. 401-434 | 2003
Rüdiger Stein; Kirsten Fahl; Klaus Dittmers; Frank Niessen; O. Stepanets
Global and Planetary Change | 2008
Klaus Dittmers; Frank Niessen; Rüdiger Stein
Marine Geology | 2008
Klaus Dittmers; Frank Niessen; Rüdiger Stein
EPIC3Berichte zur Polar- und Meeresforschung, 419, pp. 64-74 | 2002
Frank Niessen; Klaus Dittmers
Supplement to: Stein, R et al. (2003): Holocene siliciclastic and organic carbon fluxes in the Ob and Yenisei estuaries and the adjacent inner Kara Sea: Quantification, variability, and paleoenvironmental implications. In: Stein, R; Fahl, K; Fütterer, D K; Galimov, E M & Stepanets, O V (eds.), Siberian River Run-off in the Kara Sea: Characterisation, Quantification, Variability, and Environmental Significance, 488 pp. Proceedings in Marine Sciences, Elsevier, Amsterdam, 6, 401-432 | 2013
Ruediger Stein; Kirsten Fahl; Klaus Dittmers; Frank Niessen; O. Stepanets
EPIC3European Geosciences Union First General Assembly, Nice (F)April 2004., 25 | 2004
Klaus Dittmers; F. Niesen; Rüdiger Stein
In supplement to: Stein, R et al. (2003): Holocene siliciclastic and organic carbon fluxes in the Ob and Yenisei estuaries and the adjacent inner Kara Sea: Quantification, variability, and paleoenvironmental implications. In: Stein, R; Fahl, K; Fütterer, D K; Galimov, E M & Stepanets, O V (eds.), Siberian River Run-off in the Kara Sea: Characterisation, Quantification, Variability, and Environmental Significance, 488 pp. Proceedings in Marine Sciences, Elsevier, Amsterdam, 6, 401-432 | 2013
Ruediger Stein; Kirsten Fahl; Klaus Dittmers; Frank Niessen; O. Stepanets
Supplement to: Dittmers, KH et al. (2008): Late Weichselian Fluvial Evolution on the Southern Kara Sea Shelf, North Siberia. Global and Planetary Change, 60(3-4), 327-350, https://doi.org/10.1016/j.gloplacha.2006.12.006 | 2008
Klaus Dittmers; Frank Niessen; Ruediger Stein
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