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Record #156117:
- #156117
Main publication details
MARC recordChronology and palaeoenvironments during the late Weichselian deglaciation of the south-west Iceland shelf / Anne Jennings, and 7 others.
| Title: | Chronology and palaeoenvironments during the late Weichselian deglaciation of the south-west Iceland shelf / Anne Jennings, and 7 others. |
| Author(s): | Jennings, Anne. |
| Date: | 2000. |
| In: | Boreas. (2000.), Vol. 29(3) (2000) |
| Abstract: | Foraminifera, sediments and tephra geochemistry in core from SW Iceland shelf were used to reconstruct palaeoenvironments between 12 700 and 9 400 yrs. ¹⁴C BP. Seismic-reflection profiles place core in sediments within one metre of underlying glacial till. Foraminifera in earliest sediments provide record of ice-distal conditions and immigration of slope species onto shelf in association with warm Atlantic water. Arctic conditions began by 11 140 BP with abrupt increase in meltwater and near exclusion of boreal fauna. Other notable swings include inferred jökulhlaup. |
| Notes: | Boreas. Vol. 29(3) :167-183 (2000). |
| Keywords: | 551.33 -- Glacial geology. 551.463 -- Sea water, physical properties. 551.583.7 -- Palaeoclimatology. D -- Atmospheric sciences. (*3) -- Arctic regions. (*616) -- Iceland waters. |
| SPRI record no.: | 156117 |
LDR 01439naa#a2200000#a#4500 001 SPRI-156117 005 20231207161511.0 007 ta 008 231207s2000####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-156117 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aJennings, Anne. 245 10 ‡aChronology and palaeoenvironments during the late Weichselian deglaciation of the south-west Iceland shelf /‡cAnne Jennings, and 7 others. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2000. 300 ## ‡ap. 167-183 :‡bdiags., tables, maps. 500 ## ‡aBoreas. Vol. 29(3) :167-183 (2000). 520 3# ‡aForaminifera, sediments and tephra geochemistry in core from SW Iceland shelf were used to reconstruct palaeoenvironments between 12 700 and 9 400 yrs. ¹⁴C BP. Seismic-reflection profiles place core in sediments within one metre of underlying glacial till. Foraminifera in earliest sediments provide record of ice-distal conditions and immigration of slope species onto shelf in association with warm Atlantic water. Arctic conditions began by 11 140 BP with abrupt increase in meltwater and near exclusion of boreal fauna. Other notable swings include inferred jökulhlaup. 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.463 -- Sea water, physical properties.‡2udc 650 07 ‡a551.583.7 -- Palaeoclimatology.‡2udc 650 07 ‡aD -- Atmospheric sciences.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*616) -- Iceland waters.‡2udc 773 0# ‡7nnas ‡tBoreas. ‡gVol. 29(3) (2000) ‡wSPRI-56035 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231207