Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Emma Sellén"'
Publikováno v:
Polar Research, Vol 33, Iss 0, Pp 1-12 (2014)
Sea ice and icebergs are the dominant transport agents for sand-sized material to the central Arctic Ocean. However, few studies have investigated concurrent changes in the silt-sized fraction of Arctic sediments. Here we present an analysis of the c
Externí odkaz:
https://doaj.org/article/d4681a33f2ce4b8ba3380c9fe879a6f2
Autor:
Emma Sellén, Svante Björck, Jan Backman, Eliana Fornaciari, Daniela Hanslik, Göran Skog, Matt O'Regan, Martin Jakobsson
Publikováno v:
Quaternary Science Reviews. 29:3430-3441
A short sediment core from a local depression forming an intra basin on the Lomonosov Ridge, was retrieved during the Healy-Oden Trans-Arctic Expedition 2005 (HOTRAX). It contains a record of the Marine Isotope Stages (MIS) 1-3 showing exceptionally
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::69c640394c723d7671f4ee353be48776
https://doi.org/10.1016/j.quascirev.2010.06.011
https://doi.org/10.1016/j.quascirev.2010.06.011
Autor:
Christian Marcussen, Björn Eriksson, Timothy Janzen, Benjamin Hell, Dennis Antony, Sara Jutterström, Ludvig Löwemark, Bert Rudels, Emma Sellén, K. Anders Olsson, Johanna Linders, Morten Sölvsten, Martin Jakobsson, Göran Björk, Patrick B. Eriksson, Leif G. Anderson, Sofia Hjalmarsson
Publikováno v:
Deep Sea Research Part I: Oceanographic Research Papers. 57:577-586
The LOMROG 2007 expedition targeted the previously unexplored southern part of the Lomonosov Ridge north of Greenland together with a section from the Morris Jesup Rise to Gakkel Ridge. The oceanog ...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5e1c26044aa65b0228f3aed206ccd5f1
https://doi.org/10.1016/j.dsr.2010.01.006
https://doi.org/10.1016/j.dsr.2010.01.006
Publikováno v:
Global and Planetary Change. 68:38-47
Neogene marine sediments can be dated via decay of the cosmogenic radionuclide Be-10. Two cores from the Alpha and Mendeleev Ridges in the Arctic Ocean have been analyzed for seawater-derived beryllium (Be) isotopes in order to date the sediments and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2c58b67415429c53c8d62609c78627e2
https://doi.org/10.1016/j.gloplacha.2009.03.024
https://doi.org/10.1016/j.gloplacha.2009.03.024
Publikováno v:
Global and Planetary Change. 61:275-284
A standard lithostratigraphic model based on cores retrieved 1963–1973 from the ice island T-3 was developed by Clark et al. (1980) for the Amerasian Basin of the Arctic Ocean. We have investigated ...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::43e81d4d5717a3283c470950c8fd4553
https://doi.org/10.1016/j.gloplacha.2007.10.007
https://doi.org/10.1016/j.gloplacha.2007.10.007
Publikováno v:
Polar Research; Vol 33 (2014) incl supplements
Polar Research, Vol 33, Iss 0, Pp 1-12 (2014)
Polar Research, Vol 33, Iss 0, Pp 1-12 (2014)
Sea ice and icebergs are the dominant transport agents for sand-sized material to the central Arctic Ocean. However, few studies have investigated concurrent changes in the silt-sized fraction of Arctic sediments. Here we present an analysis of the c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::455df2cec6fa4cf9801df51cb5fd3644
http://www.polarresearch.net/index.php/polar/article/view/23672
http://www.polarresearch.net/index.php/polar/article/view/23672
Autor:
Jan Backman, Christian Marcussen, Benjamin Hell, Johan Nilsson, Göran Björk, Björn Eriksson, Åsa Wallin, Florence Colleoni, Leonid Polyak, Matt O'Regan, Emma Sellén, Dennis A. Darby, Ludvig Löwemark, Martin Jakobsson, Daniela Hanslik, Larry A. Mayer, Leif G. Anderson, Julian A. Dowdeswell
Publikováno v:
Quaternary Science Reviews
Quaternary Science Reviews, Elsevier, 2010, 29 (25-26), pp.3505-3517. ⟨10.1016/j.quascirev.2010.03.015⟩
Quaternary Science Reviews, Elsevier, 2010, 29 (25-26), pp.3505-3517. ⟨10.1016/j.quascirev.2010.03.015⟩
International audience; The hypothesis of floating ice shelves covering the Arctic Ocean during glacial periods was developed in the 1970s. In its most extreme form, this theory involved a 1000 m thick continuous ice shelf covering the Arctic Ocean d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::dabdb3fac620e182ceb23255055b809c
https://hal-insu.archives-ouvertes.fr/insu-00653315
https://hal-insu.archives-ouvertes.fr/insu-00653315
Sediment physical properties measured in cores from all the major ridges and plateaus in the central Arctic Ocean were studied in order to analyze the spatial and temporal consistency of sediment depositional regimes during the Quaternary. In total,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c75966b0299781aab8f11a2f226b38c6
http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-30894
http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-30894
Autor:
Emma Sellén, Riko Noormets, Benjamin Hell, Jan Backman, Morten Sölvsten, Jeffrey Evans, Martin Jakobsson, Colm Ó Cofaigh, Julian A. Dowdeswell, Christian Marcussen, Ludvig Löwemark, Matt O'Regan, Kelly A. Hogan
High-resolution geophysical evidence on the seafloor morphology and acoustic stratigraphy of the Yermak Plateau and northern Svalbard margin between 79°20′ and 81°30′N and 5° and 22°E is presented. Geophysical datasets are derived from swath
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a2c135a27fba6e4182914c2df14bdccf
http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-47298
http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-47298