Pollen stratigraphy of late pleistocene marine sediments at Nørre Lyngby and Skagen, North Denmark

Glaister, Christopher; Gibbard, Philip L.

doi:10.1016/s0277-3791(98)00021-3

Cited by 14 publications

(10 citation statements)

References 48 publications

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“…Jessen et al 1910; Knudsen 1984; Lykke‐Andersen 1987; Lykke‐Andersen & Knudsen 1991; Knudsen et al 1996; Kristensen et al 1998). This was later confirmed by pollen analysis and by absolute chronology (Glaister & Gibbard 1998; Kristensen et al 1998). The marine succession was previously thought to represent a continuous marine record (e.g.…”

Section: Rationale Behind the Stratigraphical Modelmentioning

confidence: 67%

Late Quaternary ice sheet, lake and sea history of southwest Scandinavia – a synthesis

Larsen¹,

Knudsen²,

Krohn³

et al. 2009

Boreas

101

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Section: Rationale Behind the Stratigraphical Modelmentioning

confidence: 67%

Late Quaternary ice sheet, lake and sea history of southwest Scandinavia – a synthesis

Larsen¹,

Knudsen²,

Krohn³

et al. 2009

Boreas

101

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“…1), have been reported as late Eemian (Glaister & Gibbard, 1998), tentatively late Eemian (C. G. Glaister, unpub. Ph.D. thesis, Univ.…”

Section: Ristinge Klint and Other Baltic Dinoflagellate Cyst Floras Cmentioning

confidence: 99%

Last Interglacial (Eemian) hydrographic conditions in the southwestern Baltic Sea based on dinoflagellate cysts from Ristinge Klint, Denmark

Head

2007

Geol. Mag.

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A dinoflagellate cyst record with strong Mediterranean/Lusitanian affinities is described from marine deposits of Eemian age (Last Interglacial; Late Pleistocene) at Ristinge Klint, Denmark, revealing new information about the hydrographic evolution of the southwestern Baltic Sea. A revised correlation of the pollen record at Ristinge Klint with that of the annually laminated site at Bispingen in northern Germany provides temporal control. Approximately the first quarter of Eemian time is represented. A marine ingression into a lake took place during the Quercus rise, about 300 years into the interglacial, and is marked by low (< c. 3 psu) salinities at the base of the Cyprina Clay that increased progressively. An abrupt and significant rise in the inflow of warm, saline waters from the North Sea occurred at about 750 years into the interglacial (the Corylus rise), and at about 1900 years into the interglacial, strongly stratified waters developed. Higher in the Cyprina Clay and continuing to its top, at nearly 3000 years into the interglacial, more open-marine waters are indicated, although fully marine conditions were not reached. The dinoflagellate record throughout the Cyprina Clay at Ristinge Klint is therefore one of increasing marine influence. Summer sea-surface temperatures approached, and may have exceeded, 26-28 • C during early Eemian time, indicating temperatures at least 5 • C warmer than at present. These warm conditions persisted to the top of the record at Ristinge Klint. No evidence exists at Ristinge Klint for the influence of Arctic watermasses, and the paucity of cold-water species throughout the section reflects mild winter temperatures in the southwestern Baltic Sea. The new species Spiniferites ristingensis is formally described, and the name Operculodinium centrocarpum var. cezare de Vernal, Goyette & Rodrigues, 1989 is validated.

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“…In order to obtain a core with 100% recovery through this interglacial unit, a new drilling (Nørre Lyngby 2) was carried out at almost the same location in 1993. Foraminifera, ostracods, macrofossils, diatoms (Kristensen et al 1998) and pollen (Glaister & Gibbard, 1998) indicate the presence of an interglacial unit between 70-61 m below present-day sea level in this core. The distribution of a few selected foraminiferal species and amino-acid ratios are shown in Figure 6.…”

Section: C Nørre Lyngbymentioning

confidence: 81%

“…Based on the interpretation of the foraminiferal assemblages and OSL datings, the interglacial deposit at Nørre Lyngby has been referred to the Eemian Interglacial and correlated with oxygen-isotope substage 5e (Seidenkrantz, Kristensen & Knudsen, 1995;Kristensen et al 1998). Pollen analytical data have been interpreted to support this conclusion (Glaister & Gibbard, 1998).…”

Section: C Nørre Lyngbymentioning

confidence: 99%

Geochronology and palaeoenvironment of marine Quaternary deposits in Denmark: new evidence from northern Jutland

Sejrup

Knudsen²

1999

Geol. Mag.

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The degree of isoleucine epimerization in the benthic foraminiferal species Elphidium excavatum and Bulimina marginata have been measured in four boreholes, penetrating marine interglacial beds, from northern Jutland. The results of these analyses are compiled with results obtained from other sites in Denmark and the North Sea region, and four aminozones (AZs) have been erected. AZ1 (aIle/Ile < 0.05) include the Late Weichselian and the Holocene part of the record. AZ2 (0.08-0.12

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Pollen stratigraphy of late pleistocene marine sediments at Nørre Lyngby and Skagen, North Denmark

Cited by 14 publications

References 48 publications

Late Quaternary ice sheet, lake and sea history of southwest Scandinavia – a synthesis

Late Quaternary ice sheet, lake and sea history of southwest Scandinavia – a synthesis

Last Interglacial (Eemian) hydrographic conditions in the southwestern Baltic Sea based on dinoflagellate cysts from Ristinge Klint, Denmark

Geochronology and palaeoenvironment of marine Quaternary deposits in Denmark: new evidence from northern Jutland

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