Revised Upper Cenozoic stratigraphy of the Dutch sector of the North Sea Basin: towards an integrated lithostratigraphic, seismostratigraphic and allostratigraphic approach

Rijsdijk, Kenneth F.; Passchier, Sandra; Weerts, H.J.T.; Laban, C.; Leeuwen, R.J.W. van; Ebbing, Jan H.J.

doi:10.1017/s0016774600023015

Cited by 36 publications

(87 citation statements)

References 12 publications

(32 reference statements)

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“…Doppert et al, 1975;van Adrichem Boogaert & Kouwe, 1993;Bowen, 1999;Gullentops et al, 2001;Laga et al, 2001;McMillan, 2002McMillan, , 2005Ebbing et al, 2003;Westerhoff et al, 2003;Rijsdijk et al, 2005;Weerts et al, 2005). Differences between these schemes exist for various reasons.…”

Section: Lithostratigraphic Division Schemesmentioning

confidence: 99%

North Sea palaeogeographical reconstructions for the last 1 Ma

Cohen

Gibbard

Weerts

2014

Netherlands Journal of Geosciences

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The landscape evolution of the southern North Sea basin is complex and has left a geographically varying record of marine, lacustrine, fluvial and glacial sedimentation and erosion. Quaternary climatic history, which importantly included glaciation, combined with tectonics gave rise to cyclic and non-cyclic changes of sedimentation and erosion patterns. Large-scale landscape reorganisations left strong imprints in the preserved record, and are important for the detail that palaeogeographical reconstructions for the North Sea area can achieve. In the spirit of the North Sea Prehistory Sea. It summarises current stratigraphical and chronological frameworks and provides an overview of sedimentary environments. As we go back in time, the understanding of Quaternary palaeo-environmental evolution in the North Sea basin during the last 1 million years becomes decreasingly accurate, with degree of preservation and accuracy of age control equally important controls. Comparing palaeogeographical reconstructions for the Middle Pleistocene, the last interglacial-glacial cycle and the period following the Last Glacial Maximum illustrates this. More importantly, a series of palaeogeographical maps provide an account of basin-scale landscape change, which provides an overall framework for comparing landscape situations through time.

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Section: Lithostratigraphic Division Schemesmentioning

confidence: 99%

North Sea palaeogeographical reconstructions for the last 1 Ma

Cohen

Gibbard

Weerts

2014

Netherlands Journal of Geosciences

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“…Hybridised versions of these stratigraphic approaches are now widely applied to many onshore and offshore Quaternary successions in northern Europe (Larsen and Andersen, 2005;McMillan, 2005;Rijsdijk et al, 2005;Sejrup et al, 2005;Weerts et al, 2005;Rose, 2009;Stoker et al, 2009;Hughes, 2010;Lüthgens et al, 2010).…”

Section: Lithostratigraphy -Important Conceptsmentioning

confidence: 99%

Quaternary glaciations of northern Europe

Böse

Lüthgens

Lee

et al. 2012

Quaternary Science Reviews

124

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This paper presents the outcome of a workshop, held in Berlin in February 2009, concerned with current research on the glacial history of northern Europe, including the British Isles. The methodologies presently used to resolve this topic are outlined. Particular attention is given to new analytical methods deriving from high resolution remote imaging of glacial terrain both on land and on the sea-bed, key new stratigraphic sections, higher resolution results from conventional geochronological methods like radiocarbon and more recently developed technologies such as luminescence and cosmogenic radionuclide dating. The relationships between the results derived from these two methods are discussed in further detail along with possible explanations for these differences. An outline of a 'most likely' glacial history of the Scandinavian and British and Irish Ice Sheets is presented along with possible links to global climate change as represented by the marine isotope (MIS) record. Tentative evidence for glaciation is identified in MIS 22, 16, 12, 10, 8, 6, 4 and 2 and correlations of 'phases' within the Last Glaciation are also explored for both the Scandinavian and British and Irish Ice Sheets. The results show that the character and extent of glaciation in different parts of the region are not synchronous and much more geochronological work is required before regional correlations can be established with confidence. Keywords: glaciation, marine isotope stages (MIS), Scandinavian Ice Sheet (SIS), British and Irish Ice Sheet (BIIS), Last Glacial Maximum Introduction and objectivesThe glaciation of northern Europe has been a subject of interest and debate for over 200 years and today, at a time of greater awareness to the consequences of climate change, the subject retains its relevance to science and society. With the development of new methodologies for dating glacial deposits and important new findings for modelling glacier response to climate change this subject requires re-evaluation and re-interpretation. Likewise it has been possible to identify critical issues that should be the focus for future research. Consequently, in February 2009 an exploratory workshop was held at the Freie Universität Berlin to examine the frequency and timing of glaciations in northern Europe (including Britain) during the Middle and Late Pleistocene. The workshop was funded by the DFG (Deutsche Forschungsgmeinschaft/ German Research Foundation) and involved 24 participants. This issue of Quaternary Science Reviews includes a number of the contributions presented and discussed at the meeting along with certain invited papers that present new findings on the topic of the special issue. This paper will begin by briefly reviewing the contents of the issue giving particular attention to new and important findings. This will be followed by a section that will evaluate the methodologies currently being applied to understand the glaciations of northern Europe. Some of these methodologies, such as lithostratigraphy and morphostratig...

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“…The only work with which we are familiar that combines lithostratigraphic and allostratigraphic approaches is that of Rijsdijk et al (2005), who covers the Neogene and Quaternary deposits of the Netherlands. Here the broadly defined lithostratigraphic formations of Weerts and Westerhoff (2007) are included within allostratigraphic formations.…”

Section: Allostratigraphy In Quaternary Depositsmentioning

confidence: 99%

A shift from lithostratigraphic to allostratigraphic classification of Quaternary glacial deposits

Räsänen

Auri²,

Huitti³

et al. 2009

Gsa Today

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The bedrock of the northern halves of North America and Europe is covered by Quaternary glacial deposits, forming a surficial overburden that is relatively thin, nonlithified, lithologically variable on a small scale (in terms of grain-size, mineralogy, texture, fabric, structure, and color), and often has a well-preserved depositional topography. These geologically unique characteristics and the fact that the glacial overburden was long considered to be of only restricted economic value have caused it to be treated differently in geological research from the older, regularly lithified strata. Due to the striking geomorphology of these glacial deposits, their investigation has also been incorporated into physical geography research. Thus, the segregation of the Quaternary research community into different schools of geology and geography has created multiple classification approaches and has caused the formal stratigraphic classifications successfully applied in pre-Quaternary geology to be applied less regularly to Quaternary glacial strata. This has led to inefficient use of Quaternary geological data for scientific and socio-economic purposes.The few currently existing national Quaternary stratigraphic frameworks are based on lithostratigraphy. These are poorly suited for describing deposits in glaciated shield areas in particular; we propose a classification for such areas based on the combined use of allostratigraphic and lithostratigraphic data, with alloformations as the fundamental units and lithostratigraphic units filling out the framework where appropriate. This classification would provide a hierarchical framework for glaciogenic deposits that could potentially support stratigraphic information systems, databases, and digital spatial models more effectively than the traditional lithostratigraphic frameworks.

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Revised Upper Cenozoic stratigraphy of the Dutch sector of the North Sea Basin: towards an integrated lithostratigraphic, seismostratigraphic and allostratigraphic approach

Cited by 36 publications

References 12 publications

North Sea palaeogeographical reconstructions for the last 1 Ma

North Sea palaeogeographical reconstructions for the last 1 Ma

Quaternary glaciations of northern Europe

A shift from lithostratigraphic to allostratigraphic classification of Quaternary glacial deposits

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