Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Susanne Heier-Nielsen"'
Publikováno v:
Knudsen, K L, Conradsen, K, Heier-Nielsen, S & Seidenkrantz, M-S 1996, ' Palaeoenvironments in the Skagerrak-Kattegat basin in the eastern North Sea during the last deglaciation ', Boreas, vol. 25, no. 2, pp. 65-77 . https://doi.org/10.1111/j.1502-3885.1996.tb00836.x
The study of a c. 18 m thick Late Weichselian- Early Holocene (isotope stage 2/1) marine succession (original water depth 100–150 m) from the Skagen 3 borehole, northern Denmark, has led to a better understanding of the palaeoenvironmental changes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d31ee20e4175af4eb02a1987387951a8
https://doi.org/10.1111/j.1502-3885.1996.tb00836.x
https://doi.org/10.1111/j.1502-3885.1996.tb00836.x
Publikováno v:
ResearcherID
Knudsen, K L, Conradsen, K, Heier-Nielsen, S & Seidenkrantz, M-S 1996, ' Quaternary palaeoceanography and palaeogeography in northern Denmark, a review of results from the Skagen cores ', Bulletin of the Geological Society of Denmark, vol. 43, no. 3, pp. 22-33 .
Knudsen, K L, Conradsen, K, Heier-Nielsen, S & Seidenkrantz, M-S 1996, ' Quaternary palaeoceanography and palaeogeography in northern Denmark, a review of results from the Skagen cores ', Bulletin of the Geological Society of Denmark, vol. 43, no. 3, pp. 22-33 .
Palaeoenvironmental reconstructions from the Skagen record contribute to the understanding of Late Quatemary climatic changes and variations in the oceanographic circulation pattem in the entire North Atlantic region. The Skagen cores penetrated c. 1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9a1c5167bf74431285bd6f76e5cc8d43
https://doi.org/10.37570/bgsd-1996-43-03
https://doi.org/10.37570/bgsd-1996-43-03
Publikováno v:
The Holocene. 5:313-322
Cores from the central part of the Limfjord, Denmark, have been investigated with respect to content of foraminifera, Ostracoda, macrofauna, and aquatic flora. The observed shifts in faunal composition are mainly due to changing salinity conditions c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::11c01068d6e56130191b5632eb457d65
https://doi.org/10.1177/095968369500500306
https://doi.org/10.1177/095968369500500306
Autor:
Susanne Heier-Nielsen, Keld Conradsen
Publikováno v:
Paleoceanography. 10:801-813
Paleoceanographic and paleoenvironmental interpretations based on foraminifera, sedimentary data, radiocarbon dates, and stable isotope measurements were derived from two sections in the Skagerrak: a 115-m-thick Holocene marine section drilled onshor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::359f03734cec1205da90927af02cb4bf
https://doi.org/10.1029/95pa01142
https://doi.org/10.1029/95pa01142
Autor:
Arny E. Sveinbjörnsdottir, Keld Conradsen, N. Rud, Jan Heinemeier, Susanne Heier-Nielsen, K.L. Knudsen, H.L. Nielsen
Publikováno v:
Radiocarbon. 37:119-130
We report on 69 radiocarbon dates of mollusk shells and benthic foraminifera from the upper 132 m of the marine shelf sediments of the Skagen Core (220 m total length). The dated sequence covers the Late Glacial and the Holocene (from 15 ka bp to Rec
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9909e6d4e4fb8b206e84fe719915aac4
https://doi.org/10.1017/s0033822200030551
https://doi.org/10.1017/s0033822200030551
Publikováno v:
Radiocarbon. 37:875-882
AMS 14C dates were measured for 28 mollusk shells collected live in Danish waters over the period ad 1885 to 1945. Fourteen samples were from fjords and 14 were marine samples from the Danish Skagerrak-Kattegat coastal area and from the Belts. Reserv
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3a78cabed9590be7ebdae2190f75bd17
https://doi.org/10.1017/s0033822200014958
https://doi.org/10.1017/s0033822200014958