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• W2027001806 abstract "Research Article| October 01, 2000 COMBINED FORAMINIFERAL AND THECAMOEBIAN ENVIRONMENTAL RECONSTRUCTION FROM AN ISOLATION BASIN IN NW SCOTLAND: IMPLICATIONS FOR SEA-LEVEL STUDIES Jeremy Lloyd Jeremy Lloyd Department of Geography, Science Laboratories, University of Durham, South Road, Durham, DH1 3LE, UK Search for other works by this author on: GSW Google Scholar Author and Article Information Jeremy Lloyd Department of Geography, Science Laboratories, University of Durham, South Road, Durham, DH1 3LE, UK Publisher: Cushman Foundation for Foraminiferal Research Received: 08 Jun 1999 Accepted: 17 Apr 2000 First Online: 03 Mar 2017 Online ISSN: 1943-264X Print ISSN: 0096-1191 © 2000 Journal of Foraminiferal Research Journal of Foraminiferal Research (2000) 30 (4): 294–305. https://doi.org/10.2113/0300294 Article history Received: 08 Jun 1999 Accepted: 17 Apr 2000 First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Jeremy Lloyd; COMBINED FORAMINIFERAL AND THECAMOEBIAN ENVIRONMENTAL RECONSTRUCTION FROM AN ISOLATION BASIN IN NW SCOTLAND: IMPLICATIONS FOR SEA-LEVEL STUDIES. Journal of Foraminiferal Research 2000;; 30 (4): 294–305. doi: https://doi.org/10.2113/0300294 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyJournal of Foraminiferal Research Search Advanced Search Abstract The sedimentary sequence preserved in the isolation basin at Loch nan Corr (NW Scotland) represents a high resolution record of environmental changes over the last 9.5 ka (virtually the entire Holocene). The final isolation of the basin from the sea is recorded over a 6 m sediment sequence lasting c. 7000 years as the rock sill of the basin passes through the intertidal zone. This isolation is due to relative sea-level fall associated with isostatic rebound from the melting of the Last Glacial Maximum ice sheet. Combining faunal counts of foraminifera and thecamoebians from the same sample preparations allows an accurate reconstruction of sea-level and environmental changes at this site over the Holocene. This study shows the potential for isolation basins in mesotidal areas to provide a series of sea-level index points from a single isolation contact thus improving the ease and accuracy of sea-level reconstructions. Biostratigraphic data improve our understanding of the ecology of foraminifera in these relatively unstudied rock-enclosed lagoonal ecosystems. It seems likely that Miliammina fusca can tolerate the generally low and highly variable salinities in these lagoonal settings more readily than any other foraminiferal species. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2027001806 title "COMBINED FORAMINIFERAL AND THECAMOEBIAN ENVIRONMENTAL RECONSTRUCTION FROM AN ISOLATION BASIN IN NW SCOTLAND: IMPLICATIONS FOR SEA-LEVEL STUDIES" @default.
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