Serena Tarlati
Final deglaciation of the Malin Sea through meltwater release and calving events
Tarlati, Serena; Benetti, S.; Callard, S.L.; Ó Cofaigh, C.; Dunlop, P.; Georgiopoulou, A.; Edwards, R.; Van Landeghem, K.; Saher, M.; Chiverrell, R.; Fabel, D.; Moreton, S.; Morgan, S.; Clark, C.D.
Authors
S. Benetti
S.L. Callard
Professor Colm O'Cofaigh colm.ocofaigh@durham.ac.uk
Head Of Department
P. Dunlop
A. Georgiopoulou
R. Edwards
K. Van Landeghem
M. Saher
R. Chiverrell
D. Fabel
S. Moreton
S. Morgan
C.D. Clark
Abstract
During the last glacial maximum, the British–Irish Ice Sheet (BIIS) extended to the shelf edge in the Malin Sea between Ireland and Scotland, delivering sediments to the Donegal Barra Fan (DBF). Analysis of well-preserved, glacially derived sediment in the DBF provides new insights on the character of the BIIS final deglaciation and palaeoenvironmental conditions at the Younger Dryas. Chaotic/laminated muds, ice-rafted debris (IRD)-rich layers and laminated sand–mud couplets are interpreted as respectively mass transport deposits, plumites and turbidites of BIIS-transported sediments. Peaks in IRD, constrained by radiocarbon dating to after 18 cal ka BP, indicate discrete intervals of iceberg calving during the last stages of deglaciation. Glacially derived sedimentation on the slope occurred until c. 16.9 cal ka BP. This is interpreted as the last time the ice sheet was present on to the shelf, allowing glacial meltwater to reach the fan. Bioturbated and foraminifera-rich muds above glaciomarine sediments are interpreted as interglacial hemipelagites and contourites, with the presence of Zoophycos suggesting restoration of bottom currents at the transition between stadial and interstadial conditions. During the Younger Dryas, Neogloboquadrina pachyderma sinistral abundances and an isolated peak in IRD indicate the temporary restoration of cold conditions and the presence of icebergs in the region.
Citation
Tarlati, S., Benetti, S., Callard, S., Ó Cofaigh, C., Dunlop, P., Georgiopoulou, A., Edwards, R., Van Landeghem, K., Saher, M., Chiverrell, R., Fabel, D., Moreton, S., Morgan, S., & Clark, C. (2020). Final deglaciation of the Malin Sea through meltwater release and calving events. Scottish Journal of Geology, 56(2), 117-133. https://doi.org/10.1144/sjg2019-010
Journal Article Type | Article |
---|---|
Acceptance Date | Mar 30, 2020 |
Online Publication Date | May 6, 2020 |
Publication Date | Jan 1, 2020 |
Deposit Date | May 11, 2020 |
Publicly Available Date | May 6, 2021 |
Journal | Scottish Journal of Geology |
Print ISSN | 0036-9276 |
Electronic ISSN | 2041-4951 |
Publisher | The Geological Society |
Peer Reviewed | Peer Reviewed |
Volume | 56 |
Issue | 2 |
Pages | 117-133 |
DOI | https://doi.org/10.1144/sjg2019-010 |
Public URL | https://durham-repository.worktribe.com/output/1302507 |
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Copyright Statement
Scottish journal of geology 2020. https://doi.org/10.1144/sjg2019-010. © Geological Society of London 2020.
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