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• W2277910421 endingPage "397" @default.
• W2277910421 startingPage "381" @default.
• W2277910421 abstract "In order to document changes in Holocene glacier extent and activity in NE Greenland (~73° N) we study marine sediment records that extend from the fjords ( PS 2631 and PS 2640), across the shelf ( PS 2623 and PS 2641), to the Greenland Sea ( JM 07‐174 GC ). The primary bedrock geology of the source areas is the Caledonian sediment outcrop, including Devonian red beds, plus early Neoproterozoic gneisses and early Tertiary volcanics. We examine the variations in colour ( CIE *), grain size, and bulk mineralogy (from X‐ray diffraction of the <2 mm sediment fraction). Fjord core PS 2640 in Sofia Sund, with a marked red hue, is distinct in grain size, colour and mineralogy from the other fjord and shelf cores. Five distinct grain‐size modes are distinguished of which only one is associated with a coarse ice‐rafting signal – this mode is rare in the mid‐ and late Holocene. A sediment unmixing program (SedUnMix MC ) is used to characterize down‐core changes in sediment composition based on the upper late Holocene sediments from cores PS 2640 (Sofia Sund), PS 2631 (Kaiser Franz Joseph Fjord) and PS 2623 (south of Shannon Is), and surface samples from the Kara Sea (as an indicator of transport from the Russian Arctic shelves). Major changes in mineral composition are noted in all cores with possible coeval shifts centred c . 2.5, 4.5 and 7.5 cal. ka BP (±0.5 ka) but are rarely linked with changes in the grain‐size spectra. Coarse IRD (>2 mm) and IRD ‐grain‐size spectra are rare in the last 9–10 cal. ka BP and, in contrast with areas farther south (~68° N), there is no distinct IRD signal at the onset of neoglaciation. Our paper demonstrates the importance of the quantitative analysis of sediment properties in clarifying source to sink changes in glacial marine environments." @default.
• W2277910421 created "2016-06-24" @default.
• W2277910421 creator A5020163951 @default.
• W2277910421 creator A5020584402 @default.
• W2277910421 creator A5044728558 @default.
• W2277910421 creator A5051620437 @default.
• W2277910421 date "2016-02-18" @default.
• W2277910421 modified "2023-09-27" @default.
• W2277910421 title "Late Quaternary changes in sediment composition on the <scp>NE</scp> Greenland margin (~73° N) with a focus on the fjords and shelf" @default.
• W2277910421 cites W1593626476 @default.
• W2277910421 cites W1598942597 @default.
• W2277910421 cites W1901383371 @default.
• W2277910421 cites W1946452910 @default.
• W2277910421 cites W1971250306 @default.
• W2277910421 cites W1972862806 @default.
• W2277910421 cites W1975531084 @default.
• W2277910421 cites W1976840776 @default.
• W2277910421 cites W1978912155 @default.
• W2277910421 cites W1985167833 @default.
• W2277910421 cites W1986082069 @default.
• W2277910421 cites W1987695312 @default.
• W2277910421 cites W1990899433 @default.
• W2277910421 cites W1995889939 @default.
• W2277910421 cites W1996792740 @default.
• W2277910421 cites W1997271253 @default.
• W2277910421 cites W2006778670 @default.
• W2277910421 cites W2016349369 @default.
• W2277910421 cites W2026964656 @default.
• W2277910421 cites W2029650043 @default.
• W2277910421 cites W2040992031 @default.
• W2277910421 cites W2041455370 @default.
• W2277910421 cites W2043336799 @default.
• W2277910421 cites W2044075909 @default.
• W2277910421 cites W2048434240 @default.
• W2277910421 cites W2048891927 @default.
• W2277910421 cites W2051559013 @default.
• W2277910421 cites W2053834492 @default.
• W2277910421 cites W2056535082 @default.
• W2277910421 cites W2058348604 @default.
• W2277910421 cites W2059648873 @default.
• W2277910421 cites W2059864317 @default.
• W2277910421 cites W2060168689 @default.
• W2277910421 cites W2061372308 @default.
• W2277910421 cites W2063685813 @default.
• W2277910421 cites W2064311963 @default.
• W2277910421 cites W2070753499 @default.
• W2277910421 cites W2072340496 @default.
• W2277910421 cites W2075604832 @default.
• W2277910421 cites W2076596567 @default.
• W2277910421 cites W2077267127 @default.
• W2277910421 cites W2084812846 @default.
• W2277910421 cites W2087589292 @default.
• W2277910421 cites W2089567504 @default.
• W2277910421 cites W2094229142 @default.
• W2277910421 cites W2096819901 @default.
• W2277910421 cites W2097485826 @default.
• W2277910421 cites W2101137098 @default.
• W2277910421 cites W2102082702 @default.
• W2277910421 cites W2106585957 @default.
• W2277910421 cites W2106589325 @default.
• W2277910421 cites W2107422206 @default.
• W2277910421 cites W2112191269 @default.
• W2277910421 cites W2121138676 @default.
• W2277910421 cites W2121852866 @default.
• W2277910421 cites W2122431669 @default.
• W2277910421 cites W2126292839 @default.
• W2277910421 cites W2126580316 @default.
• W2277910421 cites W2128614169 @default.
• W2277910421 cites W2133476460 @default.
• W2277910421 cites W2134577449 @default.
• W2277910421 cites W2135623743 @default.
• W2277910421 cites W2138310068 @default.
• W2277910421 cites W2143723805 @default.
• W2277910421 cites W2146896381 @default.
• W2277910421 cites W2148858284 @default.
• W2277910421 cites W2149828813 @default.
• W2277910421 cites W2150480637 @default.
• W2277910421 cites W2152540970 @default.
• W2277910421 cites W2153358054 @default.
• W2277910421 cites W2154957968 @default.
• W2277910421 cites W2160499563 @default.
• W2277910421 cites W2160918514 @default.
• W2277910421 cites W2168439910 @default.
• W2277910421 cites W2168902415 @default.
• W2277910421 cites W2175115291 @default.
• W2277910421 cites W2287480482 @default.
• W2277910421 cites W2320874953 @default.
• W2277910421 cites W2328843157 @default.
• W2277910421 cites W2336705766 @default.
• W2277910421 cites W2505371321 @default.
• W2277910421 cites W2515608062 @default.
• W2277910421 cites W351969517 @default.
• W2277910421 cites W4211135859 @default.
• W2277910421 cites W4246911884 @default.
• W2277910421 cites W4299542564 @default.
• W2277910421 cites W644494263 @default.
• W2277910421 doi "https://doi.org/10.1111/bor.12169" @default.
• W2277910421 hasPublicationYear "2016" @default.

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