Global sea-level fluctuations during the Last Interglaciation (MIS 5e)

The geomorphology and morphostratigraphy of numerous worldwide sites reveal the relative movements of sea level during the peak of the Last Interglaciation (Marine Isotope Stage (MIS) 5e, assumed average duration between 130±2 and 119±2 ka). Because sea

Bibliographic Details
Published in:Quaternary Science Reviews
Main Authors: Hearty, Paul J, Hollin, John T, Neumann, A.Conrad, O'Leary, Michael John, McCulloch, Malcolm
Format: Article in Journal/Newspaper
Language:unknown
Published: Pergamon-Elsevier Ltd
Subjects:
Keywords: Climate change
Geomorphology
Glacial geology
Reefs
Sea ice
Stratigraphy
Diagenesis
Hydro-isostatic effects
Morphostratigraphy
Racemization
Sea level
climate change
coast
GIS
ice sheet
Last Interglacial
sea level change
sedi
Ice Sheet
Online Access:http://hdl.handle.net/1885/37305
https://doi.org/10.1016/j.quascirev.2007.06.019
https://openresearch-repository.anu.edu.au/bitstream/1885/37305/5/%255B224%255D_2007_Hearty_et_al._Global_sea-level%253Bfluctuations.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/37305/7/01_Hearty_Global_sea-level_fluctuations_2007.pdf.jpg
Description
Summary:The geomorphology and morphostratigraphy of numerous worldwide sites reveal the relative movements of sea level during the peak of the Last Interglaciation (Marine Isotope Stage (MIS) 5e, assumed average duration between 130±2 and 119±2 ka). Because sea

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