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Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland.

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Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland. / Vosgerau, H.; Funder, S.; Kelly, M. et al.
In: Boreas, Vol. 23, No. 4, 1994, p. 398-411.

Research output: Contribution to Journal/Magazine › Journal article

Harvard

Vosgerau, H, Funder, S, Kelly, M, Knudsen, K-L, Kronborg, C, Madsen, HB & Sejrup, HP 1994, 'Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland.', Boreas, vol. 23, no. 4, pp. 398-411. https://doi.org/10.1111/j.1502-3885.1994.tb00608.x

APA

Vosgerau, H., Funder, S., Kelly, M., Knudsen, K-L., Kronborg, C., Madsen, H. B., & Sejrup, H. P. (1994). Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland. Boreas, 23(4), 398-411. https://doi.org/10.1111/j.1502-3885.1994.tb00608.x

Vancouver

Vosgerau H, Funder S, Kelly M, Knudsen K-L, Kronborg C, Madsen HB et al. Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland. Boreas. 1994;23(4):398-411. doi: 10.1111/j.1502-3885.1994.tb00608.x

Author

Vosgerau, H. ; Funder, S. ; Kelly, M. et al. / Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland. In: Boreas. 1994 ; Vol. 23, No. 4. pp. 398-411.

Bibtex

@article{ea2d854c2c7f4a6388fc5f6104517c7f,
title = "Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland.",
abstract = "Coastal cliffs and stream cut sections at Langelandselv on Jameson Land show a 22 m thick sedimentary succession reflecting the development of shallow marine and fluvial environments during the last interglaciation. The shallow marine sediments were deposited in upper shoreface, back-barrier, and delta environments during a rise in the relative sea level from 0 to 18 m. The interglacial succession ends with glaciotectonically dislocated fluvial sand, and is capped by alternating beds of lodgement till and fluvial sand, deposited during the Early Weichselian. The age is determined by palacoceanographic correlation of molluse and foraminifer faunas with isotopic substage 5e in the deep sea record, supported by luminescencs and U/Th dates and amino acid analysis.",
author = "H. Vosgerau and S. Funder and M. Kelly and K.-L. Knudsen and C. Kronborg and Madsen, {H. B.} and Sejrup, {H. P.}",
year = "1994",
doi = "10.1111/j.1502-3885.1994.tb00608.x",
language = "English",
volume = "23",
pages = "398--411",
journal = "Boreas",
issn = "1502-3885",
publisher = "Wiley-Blackwell",
number = "4",

}

RIS

TY - JOUR

T1 - Palaeoenvironments and changes in the relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland.

AU - Vosgerau, H.

AU - Funder, S.

AU - Kelly, M.

AU - Knudsen, K.-L.

AU - Kronborg, C.

AU - Madsen, H. B.

AU - Sejrup, H. P.

PY - 1994

Y1 - 1994

N2 - Coastal cliffs and stream cut sections at Langelandselv on Jameson Land show a 22 m thick sedimentary succession reflecting the development of shallow marine and fluvial environments during the last interglaciation. The shallow marine sediments were deposited in upper shoreface, back-barrier, and delta environments during a rise in the relative sea level from 0 to 18 m. The interglacial succession ends with glaciotectonically dislocated fluvial sand, and is capped by alternating beds of lodgement till and fluvial sand, deposited during the Early Weichselian. The age is determined by palacoceanographic correlation of molluse and foraminifer faunas with isotopic substage 5e in the deep sea record, supported by luminescencs and U/Th dates and amino acid analysis.

AB - Coastal cliffs and stream cut sections at Langelandselv on Jameson Land show a 22 m thick sedimentary succession reflecting the development of shallow marine and fluvial environments during the last interglaciation. The shallow marine sediments were deposited in upper shoreface, back-barrier, and delta environments during a rise in the relative sea level from 0 to 18 m. The interglacial succession ends with glaciotectonically dislocated fluvial sand, and is capped by alternating beds of lodgement till and fluvial sand, deposited during the Early Weichselian. The age is determined by palacoceanographic correlation of molluse and foraminifer faunas with isotopic substage 5e in the deep sea record, supported by luminescencs and U/Th dates and amino acid analysis.

U2 - 10.1111/j.1502-3885.1994.tb00608.x

DO - 10.1111/j.1502-3885.1994.tb00608.x

M3 - Journal article

VL - 23

SP - 398

EP - 411

JO - Boreas

JF - Boreas

SN - 1502-3885

IS - 4

ER -