Palaeoenvironments and changes in relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland
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Palaeoenvironments and changes in relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland. / Vosgerau, H.; Funder, Svend Visby; Kelly, M.; Knudsen, K.L.; Kronborg, C.; Madsen, H.B.; Sejrup, H.-P.
In: Boreas, 1994, p. 398-412.Research output: Contribution to journal › Journal article › Research › peer-review
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TY - JOUR
T1 - Palaeoenvironments and changes in relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland
AU - Vosgerau, H.
AU - Funder, Svend Visby
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.
M3 - Journal article
SP - 398
EP - 412
JO - Boreas
JF - Boreas
SN - 0300-9483
ER -
ID: 35221660