{"refrec":{"BRefID":242046,"RR":"<b>Shennan, I.; Hamilton, S.; Hillier, C.; Woodroffe, S.</b> (2005). A 16 000-year record of near-field relative sea-level changes, northwest Scotland, United Kingdom. <i>Quaternary International 133-134</i>: 95-106. <a href=\"http://dx.doi.org/10.1016/j.quaint.2004.10.015\" target=\"_blank\">http://dx.doi.org/10.1016/j.quaint.2004.10.015</a>","BEntID":233745,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Quaternary International 133-134</i>: 95-106. <a href=\"http://dx.doi.org/10.1016/j.quaint.2004.10.015\" target=\"_blank\">http://dx.doi.org/10.1016/j.quaint.2004.10.015</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Shennan, I.; Hamilton, S.; Hillier, C.; Woodroffe, S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Shennan, I. <i>et al.</i>","Englishabstract":"Isolation basins, raised tidal marshes, coastal wetlands and dune systems around Arisaig in northwest Scotland produce a ~16 000-year record of relative sea-level (RSL) change from the time of local deglaciation following the Last Glacial Maximum (LGM) to the present. New sea-level index points from Mointeach Mhor North define the culmination of the mid-Holocene RSL highstand to ~7600–7400 cal yr BP and 6.74±0.2 m above present. Numerous sea-level index points indicate that the RSL highstand persisted more than 1000 years before the onset of any significant RSL fall. This points to a gradual cessation of melting of the Laurentide and Antarctic ice sheets, rather than an abrupt termination. Isolation basin evidence, from a marine limit ~34 to 38 m above present down to sites close to current sea level, constrain the acceleration of eustatic sea-level rise during meltwater pulse 1a to ~30 mm yr-1 or ~11 km3 yr-1 meltwater discharge. Comparison of RSL observations with glacial isostatic adjustment (GIA) model predictions show differences in the pattern of residuals dependent upon the GIA model used. Changes to the far-field ice model components can partly explain the patterns of residuals.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"A 16 000-year record of near-field relative sea-level changes, northwest Scotland, United Kingdom","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:01.897972","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2005,"MonPub":null,"DateUpdate":"2014-10-14","DateCreate":"2014-10-14","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000227576900008","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.quaint.2004.10.015"},"refs":null,"anarec":{"AnaID":242046,"PubliDate":2005,"Pagination":"95-106","XtraPublOfAnaID":null,"ISBN":null,"Volume":"133-134","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45654,"SerRR":"Quaternary International. 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