Late Glacial Sea Level Minima in the Western British Isles
Lead Research Organisation:
University of Ulster
Department Name: Sch of Environmental Sciences
Abstract
Relative sea level (RSL) change reflects the interplay between a large number of variables operating at scales from global to local. Changes in RSL around the British Isles (BI) since the height of the last glaciation (ca. 24 000 years ago), are dominated by two key variables (i) the rise of ocean levels caused by climate warming and the melting of land-based ice; and (ii) the vertical adjustment of the Earth's surface due to the redistribution of this mass (unloading of formerly glaciated regions and loading of the ocean basins and margins). As a consequence RSL histories vary considerably across the region once covered by the British-Irish Ice Sheet (BIIS). The variable RSL history means that the BI is a globally important location for studying the interactions between land, ice and the ocean during the profound and rapid changes that followed the last glacial maximum. The BI RSL record is an important yardstick for testing global models of land-ice-ocean interactions and this in turn is important for understanding future climate and sea level scenarios. At present, the observational record of RSL change in the British Isles is limited to shallow water areas because of accessibility and only the later part of the RSL curve is well studied. In Northern Britain, where the land has been rising most, RSL indicators are close to or above present sea level and the RSL record is most complete. In southern locations, where uplift has been less, sea level was below the present for long periods of time but there is very little data on RSL position. There are varying levels of agreement between models and existing field data and we cannot be certain of model projections of former low sea levels. Getting the models right is important for understanding the whole global pattern of land-ice-ocean interactions in the past and into the future. To gather the missing data and thus improve the utility of the British RSL curves for testing earth-ice-ocean models, we will employ a specialised, interdisciplinary approach that brings together a unique team of experts in a multidisciplinary team. We have carefully selected sites where there is evidence of former sea levels is definitely preserved and we will use existing seabed geological data in British and Irish archives to plan our investigations. The first step is marine geophysical profiling of submerged seabed sediments and mapping of surface geomorphological features on the seabed. These features include the (usually) erosional surface (unconformity) produced by the rise in sea level, and surface geomorphological features that indicate former shorelines (submerged beaches, barriers and deltas). These allow us to identify the position (but not the age) of lower than present sea levels. The second step is to use this stratigraphic and geomorphological information to identify sites where we will take cores to acquire sediments and organic material from low sea-level deposits. We will analyse the sediments and fossil content of the cores to find material that can be closely related to former sea levels and radiocarbon dated. The third step in our approach is to extend the observed RSL curves using our new data and compare this to model predictions of RSL. We can then modify the parameters in the model to obtain better agreement with observations and thus better understand the earth-ice-ocean interactions. These data are also important for understanding the palaeogeography of the British Isles. Our data will allow a first order reconstruction of former coastlines, based upon the modern bathymetry, for different time periods during the deglaciation. This is of particular importance to the presence or absence of potential landbridges that might have enabled immigration to Ireland of humans and animals. They will also allow us to identify former land surfaces on the seabed. The palaeogeography is crucial to understanding the evolving oceanographic circulation of the Irish Sea.
Organisations
Publications
Biausque M
(2020)
Multiple intertidal bars on beaches: A review
in Earth-Science Reviews
Hamon-Kerivel K
(2020)
Shoreface mesoscale morphodynamics: A review
in Earth-Science Reviews
Plets R
(2019)
Late Quaternary sea-level change and evolution of Belfast Lough, Northern Ireland: new offshore evidence and implications for sea-level reconstruction
in Journal of Quaternary Science
Pretorius L
(2016)
Submerged shoreline preservation and ravinement during rapid postglacial sea-level rise and subsequent "slowstand"
in Geological Society of America Bulletin
Plets R
(2015)
Late Quaternary evolution and sea-level history of a glaciated marine embayment, Bantry Bay, SW Ireland
in Marine Geology
Plets Ruth
(2014)
Deglacial and post-glacial sea-level history for Bantry Bay (SW Ireland) based on offshore evidence
in EGU General Assembly Conference Abstracts
Cooper J. Andrew
(2014)
New observations on lower than present relative sea-levels since the late Glacial from the British Isles
in EGU General Assembly Conference Abstracts
Callard S. Louise
(2014)
Offshore evidence of postglacial relative sea-level change from eastern Ireland.
in EGU General Assembly Conference Abstracts
Plets R. M.
(2013)
Post-glacial sea-level history for SW Ireland (Bantry Bay) based on offshore evidence
in AGU Fall Meeting Abstracts
Cooper J. A.
(2013)
New observations on relative sea-level change since the late Glacial from the British and Irish continental shelf and their implications for understanding earth-ice-ocean interactions
in AGU Fall Meeting Abstracts
Quinn R.
(2013)
Post-glacial sea-level history for NE Ireland (Belfast Lough) based on offshore evidence
in AGU Fall Meeting Abstracts
James Cooper (Author)
(2012)
SUBMERGED SHORELINES IN THE IRISH SEA: SPATIAL VARIABILITY IN FORM AND PRESERVATION
James Cooper (Author)
(2012)
Topographic and stratigraphic expression of submerged shorelines in the Irish Sea
James Cooper (Author)
(2011)
Late glacial sea level minima in the Western British Isles: observed and modelled.
Description | We have constrained the late glacial sea levels at several sites around the Irish Sea. This is providing a baseline for modelling investigations of earth-ice-ocean interactions. In addition, we have examined the relationship between sea level change and coastal evolution in several paraglacial environments (marine embayments, open sedimentary coast, open rocky coast and estuaries). |
Exploitation Route | Further refinement of sea level curves |
Sectors | Education Energy Environment Culture Heritage Museums and Collections |
Description | We have created a display in the Titanic Belfast education centre, Northern Ireland's biggest indoor visitor attraction. This highlights our findings to a non-technical audience and describes the work of marine geologists. |
First Year Of Impact | 2015 |
Sector | Education,Culture, Heritage, Museums and Collections |
Impact Types | Cultural Societal |
Description | Coastal Geography Day Course for Geography Teachers, March 2011 |
Form Of Engagement Activity | A formal working group, expert panel or dialogue |
Part Of Official Scheme? | Yes |
Geographic Reach | Regional |
Primary Audience | Professional Practitioners |
Results and Impact | The teachers acquired case studies that can be used in class. A question and discussion session was included in the programme. The teachers were overwhelmingly positive in their appraisal. After the engagement we were asked to make presentations at several schools' conferences |
Year(s) Of Engagement Activity | 2009 |
Description | Session Organisation: Sea level in interglacials and the last deglaciation (including Milutin Milankovic Medal Lecture) |
Form Of Engagement Activity | A talk or presentation |
Part Of Official Scheme? | Yes |
Geographic Reach | International |
Primary Audience | Other academic audiences (collaborators, peers etc.) |
Results and Impact | The collection of talks encouraged discussion with other groups It was agreed to co-convene a similar session in subsequent years |
Year(s) Of Engagement Activity | 2014 |