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Article: Late Devensian and Holocene relative sea-level changes in northwestern Scotland: New data to test existing models

TitleLate Devensian and Holocene relative sea-level changes in northwestern Scotland: New data to test existing models
Authors
Issue Date1995
PublisherElsevier Ltd. The Journal's web site is located at http://www.elsevier.com/locate/quaint
Citation
Quaternary International, 1995, v. 26 C, p. 97-123 How to Cite?
AbstractPollen, diatom, lithostratigraphic and radiocarbon data from five sites in northwestern Scotland provide new data from an area previously devoid of reliable and precise information on Late Devensian and Holocene sea-level changes. The sites cover a range of palaeoenvironments, indicative of diversity in coastal evolution since deglaciation. For each site and palaeoenvironment the reference water (tide) level, indicative range, age and tendency of sea-level movement of all sea-level index points are quantified to enable correlation of the diverse coastal environments. The data record patterns of relative sea-level change and tendencies of sea-level movement from 12 ka BP to 1 ka BP. This is the longest and most comprehensive published record of relative sea-level change from the area. The information is used to test the accuracy of existing models of relative sea-level change. The results are only broadly consistent with a quantitative rebound model, and there is significant disagreement with empirical models during the Late Devensian and the early Holocene. © 1995.
Persistent Identifierhttp://hdl.handle.net/10722/150976
ISSN
2021 Impact Factor: 2.454
2020 SCImago Journal Rankings: 0.927

 

DC FieldValueLanguage
dc.contributor.authorShennan, Ien_US
dc.contributor.authorInnes, JBen_US
dc.contributor.authorLong, AJen_US
dc.contributor.authorZong, Yen_US
dc.date.accessioned2012-06-26T06:15:24Z-
dc.date.available2012-06-26T06:15:24Z-
dc.date.issued1995en_US
dc.identifier.citationQuaternary International, 1995, v. 26 C, p. 97-123en_US
dc.identifier.issn1040-6182en_US
dc.identifier.urihttp://hdl.handle.net/10722/150976-
dc.description.abstractPollen, diatom, lithostratigraphic and radiocarbon data from five sites in northwestern Scotland provide new data from an area previously devoid of reliable and precise information on Late Devensian and Holocene sea-level changes. The sites cover a range of palaeoenvironments, indicative of diversity in coastal evolution since deglaciation. For each site and palaeoenvironment the reference water (tide) level, indicative range, age and tendency of sea-level movement of all sea-level index points are quantified to enable correlation of the diverse coastal environments. The data record patterns of relative sea-level change and tendencies of sea-level movement from 12 ka BP to 1 ka BP. This is the longest and most comprehensive published record of relative sea-level change from the area. The information is used to test the accuracy of existing models of relative sea-level change. The results are only broadly consistent with a quantitative rebound model, and there is significant disagreement with empirical models during the Late Devensian and the early Holocene. © 1995.en_US
dc.languageengen_US
dc.publisherElsevier Ltd. The Journal's web site is located at http://www.elsevier.com/locate/quainten_US
dc.relation.ispartofQuaternary Internationalen_US
dc.titleLate Devensian and Holocene relative sea-level changes in northwestern Scotland: New data to test existing modelsen_US
dc.typeArticleen_US
dc.identifier.emailZong, Y:yqzong@hkucc.hku.hken_US
dc.identifier.authorityZong, Y=rp00846en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.scopuseid_2-s2.0-0029530268en_US
dc.identifier.volume26en_US
dc.identifier.issueCen_US
dc.identifier.spage97en_US
dc.identifier.epage123en_US
dc.publisher.placeUnited Kingdomen_US
dc.identifier.scopusauthoridShennan, I=7004126665en_US
dc.identifier.scopusauthoridInnes, JB=7102004815en_US
dc.identifier.scopusauthoridLong, AJ=7202417094en_US
dc.identifier.scopusauthoridZong, Y=7005203454en_US
dc.identifier.issnl1040-6182-

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