Postglacial relative sea-level changes in northwest Iceland: Evidence from isolation basins, coastal lowlands and raised shorelines

QUATERNARY SCIENCE REVIEWS

卷:169

Article

Brader, Martin D.¹  Lloyd, Jeremy M.¹  Barlow, Natasha L. M.^1,2  Norodahl, Hreggviour³  Bentley, Michael J.¹  Newton, Anthony J.⁴ 

[1] Univ Durham, Dept Geog, South Rd, Durham DH1 3LE, England

[2] Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England

[3] Univ Iceland, Fac Earth Sci, Sch Engn & Nat Sci, Reykjavik, Iceland

[4] Univ Edinburgh, Inst Geog, Sch GeoSci, Edinburgh EH8 9XP, Midlothian, Scotland

关键词: Holocene;    Sea level changes;    Europe;    Micropalaeontology;    Diatoms;    Isolation basin;    Iceland;   

DOI  :  10.1016/j.quascirev.2017.05.022

来源: Elsevier

【 摘 要 】

Relative sea-level (RSL) data provide constraints on land uplift associated with former ice loading and can be used to differentiate between contrasting ice unloading scenarios. Isolation basin, coastal lowland and geomorphological evidence is employed to reconstruct RSL changes in northwest (NW) Iceland, which may have experienced contrasting uplift patterns. Under local (NW) uplift, highest RSL would be expected in central Vestfirair, whereas highest RSL would be closest to the main ice loading centre under regional (central Iceland) uplift. Four new RSL records are presented based on 16 sea-level index points and 4 limiting ages froth sites principally focussed along a transect away from central Iceland. The new RSL records highlight spatial variability of Holocene RSL changes and provide constraints on deglaciation. There is an increase in marine limit elevation with proximity to the proposed principal ice loading centre in central Iceland. Highest recorded marine limit shorelines are found in HrtitafjOrour-Heggstabanes (southeast), the lowest in Hloouvik and Rekavik bak Larum (north), and at an intermediate elevation in Reylcjanes-Laugardalur (central Vestfiroir). Evidence from Breioavik-Latrar records early rapid deglaciation in Breioafjorour or a complex interplay of multiple uplift centres. RSL fell rapidly following deglaciation in several locations as a result of the quick response of the Icelandic lithosphere to unloading. The RSL data along the transect show an uplift pattern consistent with extensive regional glaciation emanating from central Iceland, which could have implications for ice sheet configuration and patterns of deglaciation, glacio-isostatic adjustment modelling and the volume of meltwater input into the North Atlantic. (C) 2017 The Authors. Published by Elsevier Ltd.

【 授权许可】

Free