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Quaternary stratigraphy of Norden, a proposal for terminology and classification

Jan Mangerud, +3 more
- 16 Jan 2008 - 
- Vol. 3, Iss: 3, pp 109-126
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TLDR
In this paper, a proposal for a common chronostratigraphical classification of the Quaternary in Norden (and partly continental NW Europe) is made, based on the sequence of glacials/interglacials.
Abstract
Principles and terminology for classification of the Quaternary are discussed, including lithostratigraphy, biostratigraphy. morphostratigraphy, climatostratigraphy and chronostratigraphy. The main conclusion is a proposal for a common chronostratigraphical classification of the Quaternary in Norden (and partly continental NW Europe). The Quaternary is subdivided into the Pleistocene and the Holocene Series. The Pleistocene is further subdivided into several provisional stages (Weichselian, Eemian, etc.), based on the sequence of glacials/interglacials. but with the boundaries preferably defined by stratotypes. The Late Weichselian and the Flandrian (Holocene) are subdivided into chronozoncs (Bolling, Older Dryas, Allerod, Younger Dryas, Preboreal, Boreal, Atlantic, Subboreal, Subatlantic) with the boundaries dcfined in conventional radiocarbon years.

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Journal Article

The early Holocene climate and sea-level changes in Lofoten and Vesterålen, North Norway

TL;DR: A submarine peat at Petvik in western Lofoten has been pollen-analysed and 14C-dated as discussed by the authors, and some additional data from Ramsa in northern Vesteralen, indicate that the sea leve) at the 7...S m Main shoreline isobase sank below present mean sea level around 9900 B.P.
Journal ArticleDOI

Where are the Missing Boats? The Pioneer Settlement of Norway as Long-Term History

TL;DR: In this paper, the authors address the process of colonization from a perspective of long-term history, analysing the record in an archaeological retrospective perspective, and discuss some of the presumptions giving an implicit framework to the current state of knowledge.

Submarine push moraine formation during the early Fennoscandian Ice Sheet deglaciation

TL;DR: In this paper, the authors analyzed the glacial history in the topographically confined paleo-ice stream drainage route of Vestfjorden, North Norway, based on bathymetric data, high-resolution seismology and 14C AMS-dated gravity cores.
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Deglaciation and Human Colonization of Northern Europe

TL;DR: A detailed review of existing archaeological and paleoecological evidence pertaining to the Late Upper Paleolithic of northern Europe, and theoretical observations on human colonization models and ecological responses to large-scale stadial and interstadial events is provided in this paper.
References
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Journal ArticleDOI

Half-life of Radiocarbon

TL;DR: The Fifth Radiocarbon Dating Conference, meeting at Cambridge (see p. 943 of this issue of Nature), adopted the following resolution as discussed by the authors, which determined the 1.1 − 3 of the half-life of carbon-14.
Journal Article

Late Quaternary foraminifera from Vendsyssel, Denmark and Sandnes, Norway

Abstract: Rolf W. Feyling-Hanssen: Weichselian interstadial Foraminifera from the Sandnes-Jæren area. Five shallow borings in the town of Sandnes, south of Stavanger, revealed clay deposits with marine fossils under a cover of sandy till with large blocks of Archaen rocks. This clay is called the Sandnes Clay. It is stiff and pre-consolidated, and disturbed only in the uppermost part. Four foraminiferal zones were distinguished, 1) the labradoricum-norcrossi assemblage, 2) the upper zone with scattered specimens, 3) the asklundi-bartletti assemblage, 4) the lower zone with scattered specimens. The assemblages are usually dominated by Elphidium clavatum and Cassidulina crassa, and turn out to be of Middle Weichselian (Middle Wisconsin) interstadial age. Deposits of corresponding age were found in the district of Jæren and on the island of Karmøy.
Journal ArticleDOI

Radiocarbon dating of marine shells, including a discussion of apparent age of Recent shells from Norway

Jan Mangerud
- 16 Jan 2008 - 
TL;DR: In this paper, the authors concluded that shell dates are reliable when handled carefully and gave apparent ages from 340±75 to 550±80 years, indicating that apparent age is not a significant problem in dating of Norwegian shells.

Late-glacial flora and periglacial phenomena in the Netherlands

TL;DR: In the East of Holland, in the Province of Overijssel, there is a region that, from the point of view of landscape, is one of the most beautiful and the most interesting we know in this country as discussed by the authors.
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