FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1987337564> ?p ?o ?g. }

• W1987337564 endingPage "1647" @default.
• W1987337564 startingPage "1625" @default.
• W1987337564 abstract "Sediment cores from two glacier-fed lakes are used to reconstruct a continuous record of glacier variations since about 10,000 cal. BP in the Smørstabbtinden massif of central Jotunheimen, southern Norway. Particular attention is paid to the century- to millennial-scale, pre-Little Ice Age glacial signal based on an estimated temporal resolution of ⩽55 and ⩽25 yr cm−1 for Bøvertunsvatnet and Dalsvatnet, respectively. Visible lithostratigraphic variations, organic content/loss-on-ignition, calcium carbonate content, magnetic susceptibility and grain-size fractions (especially the fine silt) are used as proxy indicators of glacier presence and extent in the lake catchments. Following deglaciation, the early Holocene was characterized by generally small glaciers until a major advance (the Finse Event) peaking at approximately 8200 cal. BP. From 7900 to at least 5300 cal. BP glaciers appear to have been absent from central Jotunheimen. There is evidence of glacier expansion between about 2400 and 1600 cal. BP (the Bøvertun I Event) and between about 1400 and 800 cal. BP (the Bøvertun II Event) before reduced glacier extent during the Mediaeval Warm Period. Finally, the most extensive Neoglacial maximum occurred during the Little Ice Age after 500 cal. BP. In addition to providing a record of the broad pattern of climatically forced Holocene glacier variations, periodicities at 110–140, 200–285 and about 500 yr have been identified. Uncertainties remain concerning the precise timing of events, glacierization and deglacierization detection thresholds, a possible mid- to late-Holocene (5300–2500 cal. BP) Neoglacial build-up of small glaciers, and shorter-term, decadal- to century-scale variations in glacier size, for which more proximal sites are required." @default.
• W1987337564 created "2016-06-24" @default.
• W1987337564 creator A5008916045 @default.
• W1987337564 creator A5012060068 @default.
• W1987337564 creator A5012122355 @default.
• W1987337564 creator A5015373929 @default.
• W1987337564 creator A5046156219 @default.
• W1987337564 date "2000-11-01" @default.
• W1987337564 modified "2023-10-14" @default.
• W1987337564 title "Holocene glacier variations in central Jotunheimen, southern Norway based on distal glaciolacustrine sediment cores" @default.
• W1987337564 cites W118646744 @default.
• W1987337564 cites W1541893073 @default.
• W1987337564 cites W1578359704 @default.
• W1987337564 cites W1604275499 @default.
• W1987337564 cites W1927648166 @default.
• W1987337564 cites W1964935748 @default.
• W1987337564 cites W1970550148 @default.
• W1987337564 cites W1974336339 @default.
• W1987337564 cites W1975655090 @default.
• W1987337564 cites W1975715178 @default.
• W1987337564 cites W1976871820 @default.
• W1987337564 cites W1977398233 @default.
• W1987337564 cites W1979818626 @default.
• W1987337564 cites W1982082363 @default.
• W1987337564 cites W1982112039 @default.
• W1987337564 cites W1986090479 @default.
• W1987337564 cites W1986624012 @default.
• W1987337564 cites W1988196896 @default.
• W1987337564 cites W1991881062 @default.
• W1987337564 cites W1993219186 @default.
• W1987337564 cites W1994291261 @default.
• W1987337564 cites W2005420354 @default.
• W1987337564 cites W2007448458 @default.
• W1987337564 cites W2008875043 @default.
• W1987337564 cites W2011062887 @default.
• W1987337564 cites W2013780180 @default.
• W1987337564 cites W2014688144 @default.
• W1987337564 cites W2019408839 @default.
• W1987337564 cites W2019658294 @default.
• W1987337564 cites W2019807079 @default.
• W1987337564 cites W2023113054 @default.
• W1987337564 cites W2023536122 @default.
• W1987337564 cites W2031305763 @default.
• W1987337564 cites W2036729924 @default.
• W1987337564 cites W2037550159 @default.
• W1987337564 cites W2037918186 @default.
• W1987337564 cites W2039917012 @default.
• W1987337564 cites W2040564336 @default.
• W1987337564 cites W2041006844 @default.
• W1987337564 cites W2044398360 @default.
• W1987337564 cites W2052003350 @default.
• W1987337564 cites W2053444911 @default.
• W1987337564 cites W2053873865 @default.
• W1987337564 cites W2055344560 @default.
• W1987337564 cites W2056653118 @default.
• W1987337564 cites W2057752671 @default.
• W1987337564 cites W2059241940 @default.
• W1987337564 cites W2059891162 @default.
• W1987337564 cites W2060303663 @default.
• W1987337564 cites W2061517952 @default.
• W1987337564 cites W2064618182 @default.
• W1987337564 cites W2065778182 @default.
• W1987337564 cites W2068090847 @default.
• W1987337564 cites W2071705746 @default.
• W1987337564 cites W2075780012 @default.
• W1987337564 cites W2075848460 @default.
• W1987337564 cites W2080042998 @default.
• W1987337564 cites W2084252592 @default.
• W1987337564 cites W2084850065 @default.
• W1987337564 cites W2086416727 @default.
• W1987337564 cites W2086972503 @default.
• W1987337564 cites W2087888479 @default.
• W1987337564 cites W2090033270 @default.
• W1987337564 cites W2093007305 @default.
• W1987337564 cites W2116153413 @default.
• W1987337564 cites W2116321811 @default.
• W1987337564 cites W2121841894 @default.
• W1987337564 cites W2142952299 @default.
• W1987337564 cites W2176359510 @default.
• W1987337564 cites W2184007054 @default.
• W1987337564 cites W2204289341 @default.
• W1987337564 cites W2273957027 @default.
• W1987337564 cites W2280624662 @default.
• W1987337564 cites W2315346895 @default.
• W1987337564 cites W231559496 @default.
• W1987337564 cites W2318991685 @default.
• W1987337564 cites W2324161166 @default.
• W1987337564 cites W2335457657 @default.
• W1987337564 cites W2336008680 @default.
• W1987337564 cites W236967408 @default.
• W1987337564 cites W2476752497 @default.
• W1987337564 cites W268430260 @default.
• W1987337564 cites W2767564617 @default.
• W1987337564 cites W2797540839 @default.
• W1987337564 cites W281218121 @default.
• W1987337564 cites W2954300830 @default.
• W1987337564 cites W423856055 @default.
• W1987337564 cites W594456457 @default.

• next