0000000000305969

AUTHOR

Wim Kuijper

showing 3 related works from this author

Fires at Neumark-Nord 2, Germany: An analysis of fire proxies from a Last Interglacial Middle Palaeolithic basin site

2016

Few sites with evidence for fire use are known from the Last Interglacial in Europe. Hearth features are rarely preserved, probably as a result of post-depositional processes. The small postglacial basins (

010506 paleontologyArcheologyHearthEemianStructural basinHeated flint01 natural sciencesLast InterglacialBurned bone0601 history and archaeologyCharcoalheated flint0105 earth and related environmental sciencesFire usegeographyEemiangeography.geographical_feature_category060102 archaeology06 humanities and the artsSedimentary basinArchaeologysedimentary basinsburned bonevisual_artCharcoalInterglacialvisual_art.visual_art_mediumGeologycharcoal
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Environmental conditions at the Last Interglacial (Eemian) site Neumark‐Nord 2, Germany inferred from stable isotope analysis of freshwater mollusc o…

2020

Acknowledgements The authors acknowledge the two anonymous reviewers for their useful comments that improved the manuscript. Financial support for the excavations in Neumark‐Nord 2 was provided by the Lausitzer Mitteldeutsche Braunkohlengesellschaft mbH, the Landesamt fur Denkmalpflege und Archaologie Sachsen‐Anhalt (Harald Meller, Susanne Friederich), the Romisch‐Germanisches Zentralmuseum Mainz, the Leids Universiteits Fonds ‘Campagne voor Leiden’ program and the Netherlands Organization for Scientific Research (N.W.O.).

Supplementary dataArcheologyEemianbiologyδ18OGeologybiology.organism_classificationArchaeologyBithynia tentaculataInterglacialEcology Evolution Behavior and SystematicsGeologyFreshwater molluscIsotope analysisBoreas
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Direct terrestrial–marine correlation demonstrates surprisingly late onset of the last interglacial in central Europe

2011

AbstractAn interdisciplinary study of a small sedimentary basin at Neumark Nord 2 (NN2), Germany, has yielded a high-resolution record of the palaeomagnetic Blake Event, which we are able to place at the early part of the last interglacial pollen sequence documented from the same section. We use this data to calculate the duration of this stratigraphically important event at 3400 ± 350 yr. More importantly, the Neumark Nord 2 data enables precise terrestrial–marine correlation for the Eemian stage in central Europe. This shows a remarkably large time lag of ca. 5000 yr between the MIS 5e ‘peak’ in the marine record and the start of the last interglacial in this region.

010506 paleontologyEemiangeographyPaleomagnetismgeography.geographical_feature_category010504 meteorology & atmospheric sciencesAardwetenschappenBlake EventMIS 5ePalaeomagnetismLast interglacialTime lagLate onsetEemianSedimentary basin01 natural sciencesSequence (geology)PaleontologyArts and Humanities (miscellaneous)InterglacialShort PaperGeneral Earth and Planetary SciencesGeology0105 earth and related environmental sciencesEarth-Surface ProcessesQuaternary Research
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