The timing of last‐glacial periglacial and aeolian events, Twente, eastern Netherlands

Bateman, Mark D.; Huissteden, J. van

doi:10.1002/(sici)1099-1417(199905)14:3<277::aid-jqs460>3.0.co;2-w

Cited by 84 publications

(69 citation statements)

References 15 publications

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“…The consequence for the luminescence age calculation will be of the same magnitude as the values for the dose rate but with opposite sign. Bateman & van Huissteden (1999) and Frechen et al (2001a). The Beuningen gravel bed is defined as a deflation horizon between Older Coversand I and II.…”

Section: Moisturesupporting

confidence: 83%

“…The IRSL results are within the standard deviation in agreement with geological age estimates for most of the samples (Bateman & van Huissteden, 1999;Frechen et al, 2001a). However, additional combined dating approaches are required on different dating material from the same section, for example radiocarbon dating on organic matter and luminescence on quartz and potassium-rich feldspar.…”

Section: Discussionmentioning

confidence: 89%

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The coversands and timing of Late Quaternary earthquake events along the Peel Boundary Fault in the Netherlands

Frechen

Berg²

2002

Netherlands Journal of Geosciences

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The coversands along the Peel Boundary Fault in die Netherlands were investigated by a luminescence dating approach combining Infrared Optically Stimulated Luminescence (IRSL) andThermoluminescence (TL) methods. At the Neer trench, ten samples were collected and investigated in order to set up an independent chronological framework for the deposition history of the fluvio-aeolian and aeolian sediments and hence the timing of Late Weichselian and Holocene earthquake events. Five sedimentary units could be distinguished by this chronological approach. The oldest fluvio-aeolian unit yielded a mean deposition age of 35.9±0.4 ka and is designated to correlate with the Middle Weichselian. An IRSL age estimate of 20.1 ±2.9 ka was determined for the sediment that most likely represents the Older Coversands I, and a mean luminescence age of 15.1±1.2 ka for deposits just below the Beuningen gravel bed.The aeolian sediment from above the Beuningen horizon yielded an IRSL age estimate of 9.4±1.0 ka. The youngest deposits from the colluvial wedge yielded <6.9±0.7 ka BP, and so an earthquake event was likely to occur during the Middle or Late Holocene, as evidenced by the luminescence age estimates.

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Section: Moisturesupporting

confidence: 83%

Section: Discussionmentioning

confidence: 89%

The coversands and timing of Late Quaternary earthquake events along the Peel Boundary Fault in the Netherlands

Frechen

Berg²

2002

Netherlands Journal of Geosciences

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“…BP (Van Geel et al, 1989). Hence, this provides a minimum age for the Beuningen Complex of about 14.8-14.3 ka cal.BP, which is in good correspondence with the recent OSL dates by Bateman & Van Huissteden (1999). Between 14.1 and 14.0 ka cal.…”

Section: Aeolian Activitymentioning

confidence: 99%

Climatic and environmental events over the Last Termination, as recorded in The Netherlands: a review

Hoek¹,

Bohncke²

2002

Netherlands Journal of Geosciences

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The Last Termination, orWeichselian Lateglacial (ca 15-10 ka cal. BP), is a time period with rapid changes in climate and environment. The oxygen-isotope records of the Greenland ice-cores are regarded as the most complete climate proxy for the North Atlantic region. In The Netherlands several other proxies have been investigated and dated in great detail over the last few decades. However, changes registered in the different records are not by definition causally related to climate changes. Comparison of the different records on a common time-scale permits evaluation of the interrelationships and correlations to the Greenland ice-cores. Some events are the result of the complex interplay of different environmental variables and have no causal relationship with climate changes at all. By comparing the different records on a common time-scale and examining spatial patterns, the links between the proxies become evident.

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“…More recently it has become possible to date aeolian sediments reliably with optically stimulated luminescence (OSL) dating (e.g. Bateman, 1995Bateman, , 1998Radtke and Janotta, 1998;Bateman and Van Huissteden, 1999;Vandenberghe et al, 2004;Koster, 2005). However, many uncertainties about the nature of LP surface winds remain.…”

Section: Introductionmentioning

confidence: 99%

Weichselian Late Pleniglacial surface winds over northwest and central Europe: a model–data comparison

Renssen

Kasse

Vandenberghe

et al. 2007

J Quaternary Science

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2006. Weichselian Late Pleniglacial surface winds over northwest and central Europe: a model-data comparison.ABSTRACT: Reconstructions of the Weichselian Late Pleniglacial wind direction in northwest and central Europe are reviewed and compared with palaeoclimate simulations performed with an atmospheric general circulation model. These reconstructions are based on proxy data containing information on former wind directions, such as relic dune forms, sediments and wind-polished rock surfaces. The objective is to investigate whether: (1) the proxy information is internally consistent; and (2) in agreement with the model simulations. We find a general consensus in the proxy-based reconstructions, indicating a dominant westerly to northwesterly wind in winter during the Late Pleniglacial. The model results indicate over the study area an atmospheric circulation in winter that is dominated by southwesterly to west-northwesterly winds, which are stronger than the southwesterly winds in the present-day climate. The main driving factors behind the anomalous atmospheric circulation in the Late Pleniglacial are the Laurentide Ice Sheet and a colder North Atlantic Ocean with a relatively extensive sea-ice cover, leading to an eastward relocation of the Icelandic Low and an enhanced pressure gradient over northwest Europe. The minor difference in Late Pleniglacial wind direction between the reconstructions and model can be explained by a combination of uncertainties in the proxy data and the relatively low spatial resolution of the applied climate model.

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The timing of last‐glacial periglacial and aeolian events, Twente, eastern Netherlands

Cited by 84 publications

References 15 publications

The coversands and timing of Late Quaternary earthquake events along the Peel Boundary Fault in the Netherlands

The coversands and timing of Late Quaternary earthquake events along the Peel Boundary Fault in the Netherlands

Climatic and environmental events over the Last Termination, as recorded in The Netherlands: a review

Weichselian Late Pleniglacial surface winds over northwest and central Europe: a model–data comparison

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