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• W1858277493 endingPage "40" @default.
• W1858277493 startingPage "26" @default.
• W1858277493 abstract "Global sea level during the Last Interglacial (LIG, Marine Isotope Sub-stage 5e) peaked between c. 5.5 and 9 m above present, implying significant melt from Greenland and Antarctica. Relative sea level (RSL) observations from several far- and intermediate-field sites suggest abrupt fluctuations or jumps in RSL during the LIG highstand that require one or more episodes of ice-sheet collapse and regrowth. Such events should be manifest as unique sea-level fingerprints, recorded in far-, intermediate- and near-field sites depending on the source(s) of ice-mass change involved. To date, though, no coherent evidence of such fluctuations has been reported from near-field RSL studies in northwest Europe. This is an important problem because RSL fluctuations during the LIG are portrayed as warning signs for how polar ice sheets may behave in a future, warmer than present, world. Here we review the evidence for RSL change during the LIG using stratigraphic data from the best resolved highstand records that exist in the near-field of northwest Europe, from a range of settings that include lagoonal, shallow marine, tidal flat, salt marsh and brackish-water fluviatile environments. Consideration of previously published stratigraphic records from two sites in the Eemian coastal-marine embayment that existed in the central Netherlands, yields no clear indications for abrupt RSL change during the attainment of the near-field highstand. Nor do we find any such indications common to other records from countries bordering the North Sea, the Baltic Sea and the White Sea. Two modelling experiments that explore the global signal of hypothetical sea-level oscillations caused by partial collapse and regrowth of either the Greenland or Antarctic LIG ice-sheet, show that the North Sea region is relatively insensitive to mass changes sourced from Greenland but should clearly register events with an Antarctic origin, especially those that occur late in the LIG. The lack of evidence for abrupt sea-level fluctuations at this time in northwest Europe concurs with a lack of clear near-field evidence for ice sheet collapse." @default.
• W1858277493 created "2016-06-24" @default.
• W1858277493 creator A5001929892 @default.
• W1858277493 creator A5049669987 @default.
• W1858277493 creator A5050212307 @default.
• W1858277493 creator A5061982273 @default.
• W1858277493 creator A5070386432 @default.
• W1858277493 creator A5083387810 @default.
• W1858277493 date "2015-10-01" @default.
• W1858277493 modified "2023-10-14" @default.
• W1858277493 title "Near-field sea-level variability in northwest Europe and ice sheet stability during the last interglacial" @default.
• W1858277493 cites W1486733610 @default.
• W1858277493 cites W1540946605 @default.
• W1858277493 cites W1588926584 @default.
• W1858277493 cites W1603555063 @default.
• W1858277493 cites W1815495402 @default.
• W1858277493 cites W1822513039 @default.
• W1858277493 cites W1857847771 @default.
• W1858277493 cites W1945899484 @default.
• W1858277493 cites W1964694269 @default.
• W1858277493 cites W1965275464 @default.
• W1858277493 cites W1965946820 @default.
• W1858277493 cites W1966210598 @default.
• W1858277493 cites W1966265779 @default.
• W1858277493 cites W1966282214 @default.
• W1858277493 cites W1969303183 @default.
• W1858277493 cites W1973540896 @default.
• W1858277493 cites W1974194861 @default.
• W1858277493 cites W1974258673 @default.
• W1858277493 cites W1975258366 @default.
• W1858277493 cites W1977298633 @default.
• W1858277493 cites W1980003546 @default.
• W1858277493 cites W1981102897 @default.
• W1858277493 cites W1981304827 @default.
• W1858277493 cites W1981500141 @default.
• W1858277493 cites W1984175161 @default.
• W1858277493 cites W1984682253 @default.
• W1858277493 cites W1986254615 @default.
• W1858277493 cites W1990393337 @default.
• W1858277493 cites W1990811231 @default.
• W1858277493 cites W1993178991 @default.
• W1858277493 cites W1994155113 @default.
• W1858277493 cites W1995637978 @default.
• W1858277493 cites W1995764097 @default.
• W1858277493 cites W1999675026 @default.
• W1858277493 cites W2002131871 @default.
• W1858277493 cites W2013136201 @default.
• W1858277493 cites W2014169468 @default.
• W1858277493 cites W2015573300 @default.
• W1858277493 cites W2017191372 @default.
• W1858277493 cites W2017202038 @default.
• W1858277493 cites W2019123587 @default.
• W1858277493 cites W2021124392 @default.
• W1858277493 cites W2022898066 @default.
• W1858277493 cites W2023053811 @default.
• W1858277493 cites W2024872505 @default.
• W1858277493 cites W2025427502 @default.
• W1858277493 cites W2026037965 @default.
• W1858277493 cites W2026261450 @default.
• W1858277493 cites W2026391369 @default.
• W1858277493 cites W2028200333 @default.
• W1858277493 cites W2028491985 @default.
• W1858277493 cites W2033818786 @default.
• W1858277493 cites W2035927985 @default.
• W1858277493 cites W2037528981 @default.
• W1858277493 cites W2037648824 @default.
• W1858277493 cites W2038706413 @default.
• W1858277493 cites W2042795871 @default.
• W1858277493 cites W2045798746 @default.
• W1858277493 cites W2047554914 @default.
• W1858277493 cites W2053074196 @default.
• W1858277493 cites W2053613265 @default.
• W1858277493 cites W2053887324 @default.
• W1858277493 cites W2057199947 @default.
• W1858277493 cites W2061993062 @default.
• W1858277493 cites W2064343147 @default.
• W1858277493 cites W2066248944 @default.
• W1858277493 cites W2066361114 @default.
• W1858277493 cites W2066878985 @default.
• W1858277493 cites W2068602401 @default.
• W1858277493 cites W2073219930 @default.
• W1858277493 cites W2076238280 @default.
• W1858277493 cites W2076517688 @default.
• W1858277493 cites W2079672199 @default.
• W1858277493 cites W2080407912 @default.
• W1858277493 cites W2080912283 @default.
• W1858277493 cites W2080940309 @default.
• W1858277493 cites W2087567020 @default.
• W1858277493 cites W2088543940 @default.
• W1858277493 cites W2088919365 @default.
• W1858277493 cites W2089225402 @default.
• W1858277493 cites W2090197982 @default.
• W1858277493 cites W2092578341 @default.
• W1858277493 cites W2099550415 @default.
• W1858277493 cites W2101516930 @default.
• W1858277493 cites W2111356440 @default.
• W1858277493 cites W2112363056 @default.
• W1858277493 cites W2114200946 @default.

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