id:"swepub:oai:lup.lub.lu.se:4f52a78f-668f-4af1-972e-cc071bf6901b"
Search: id:"swepub:oai:lup.lub.lu.se:4f52a78f-668f-4af1-972e-cc071bf6901b" > Glacial and palaeo-...
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| Fältnamn | Indikatorer | Metadata |
|---|---|---|
| 000 | 03391naa a2200409 4500 | |
| 001 | oai:lup.lub.lu.se:4f52a78f-668f-4af1-972e-cc071bf6901b | |
| 003 | SwePub | |
| 008 | 160401s2008 | |||||||||||000 ||eng| | |
| 024 | 7 | a https://lup.lub.lu.se/record/9961002 URI |
| 024 | 7 | a https://doi.org/10.1111/j.1751-8369.2008.00066.x2 DOI |
| 040 | a (SwePub)lu | |
| 041 | a engb eng | |
| 042 | 9 SwePub | |
| 072 | 7 | a art2 swepub-publicationtype |
| 072 | 7 | a ref2 swepub-contenttype |
| 100 | 1 | a Möller, Peru Lund University,Lunds universitet,Kvartärgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Quaternary Sciences,Department of Geology,Faculty of Science4 aut0 (Swepub:lu)geol-pmo |
| 245 | 1 0 | a Glacial and palaeo-environmental history of the Cape Chelyuskin area, Arctic Russia |
| 264 | c 2016-12-16 | |
| 264 | 1 | b Norwegian Polar Institute,c 2008 |
| 520 | a Quaternary glacial stratigraphy and relative sea-level changes reveal at least two glacial expansions over the Chelyuskin Peninsula, bordering the Kara Sea at about 77°N in the Russian Arctic, as indicated from tills interbedded with marine sediments, exposed in stratigraphic superposition, and from raised beach sequences mapped to altitudes of at least up to ca. 80 m a.s.l. Chronological control is provided by accelerator mass spectrometry 14C dating, electron-spin resonance and optically stimulated luminescence geochronology. Major glaciations, followed by deglaciation and marine inundation, occurred during marine oxygen isotope stages 6–5e (MIS 6–5e) and stages MIS 5d–5c. These glacial sediments overlie marine sediments of Pliocene age, which are draped by fluvial sediment of a pre-Saalian age, thereby forming palaeovalley/basin fills in the post-Cretaceous topography. Till fabrics and glacial Tectonics record expansions of local ice caps exclusively, suggesting wet-based ice cap advance, followed by cold-based regional ice-sheet expansion. Local ice caps over highland sites along the perimeter of the shallow Kara Sea, including the Byrranga Mountains and the Severnaya Zemlya archipelago, appear to have repeatedly fostered initiation of a large Kara Sea ice sheet, with the exception of the Last Glacial Maximum (MIS 2), when Kara Sea ice neither impacted the Chelyuskin Peninsula nor Severnaya Zemlya, and barely touched the northern coastal areas of the Taymyr Peninsula. | |
| 650 | 7 | a NATURVETENSKAPx Geovetenskap och miljövetenskapx Geologi0 (SwePub)105042 hsv//swe |
| 650 | 7 | a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Geology0 (SwePub)105042 hsv//eng |
| 653 | a glacial geology | |
| 653 | a Eemian | |
| 653 | a glacial stratigraphy | |
| 653 | a Siberia | |
| 653 | a Kara Sea ice sheet | |
| 700 | 1 | a Federov, G4 aut |
| 700 | 1 | a Pavlov, M4 aut |
| 700 | 1 | a Seidenkrantz, M.-S.4 aut |
| 700 | 1 | a Sparrenbom, Charlotteu Swedish Geotech Inst4 aut0 (Swepub:lu)geol-cjo |
| 710 | 2 | a Kvartärgeologib Geologiska institutionen4 org |
| 773 | 0 | t Polar Researchd : Norwegian Polar Instituteg 27:2, s. 222-248q 27:2<222-248x 0800-0395x 1751-8369 |
| 856 | 4 | u http://www.polarresearch.net/index.php/polar/article/view/6178x freey FULLTEXT |
| 856 | 4 | u http://dx.doi.org/10.1111/j.1751-8369.2008.00066.xx freey FULLTEXT |
| 856 | 4 8 | u https://lup.lub.lu.se/record/996100 |
| 856 | 4 8 | u https://doi.org/10.1111/j.1751-8369.2008.00066.x |
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