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Record #104137:
- #104137
Main publication details
MARC recordEvidence of environmental change since the last glacial maximum inferred from chemical analysis of an ice core from Law Dome, Antarctica (abstract) / Neal W. Young, M. de Angelis, D. Davies.
| Title: | Evidence of environmental change since the last glacial maximum inferred from chemical analysis of an ice core from Law Dome, Antarctica (abstract) / Neal W. Young, M. de Angelis, D. Davies. |
| Author(s): | Young, Neal W. Angelis, M. de. Davies, D. |
| Date: | 1990. |
| In: | Annals of Glaciology. (1990.), Vol. 14 (1990) |
| Abstract: | Concentration of major anions and cations measured on samples selected from ice core to give information on major environmental changes which have occurred from 26 to 6 ka BP. Chemical species can be divided into those from marine (Na and Mg) and continental (Al) sources. Methane sulphonic acid also determined; this has marine biogenic source and exhibits pattern which is generally unrelated to variations in main divisions. Oxygen isotope ratios provide additional data source. |
| Notes: | Annals of Glaciology. Vol. 14 :365 (1990). |
| Keywords: | 551.324.29 -- Land ice, miscellaneous forms. 551.324.84 -- Land ice, impurities. 551.32 -- Glaciology. 551.324 -- Land ice. 54 -- Chemistry. 539.155.2 -- Isotopic analysis. 551.583 -- Climatic changes. E5 -- Glaciology: land ice. (*7) -- Antarctic regions. (*747.3) -- Budd Coast. |
| SPRI record no.: | 104137 |
LDR 01592naa#a2200000#a#4500 001 SPRI-104137 005 20231211191441.0 007 ta 008 231211s1990####xx####|##|###|0||#0|eng#d 035 ## ‡aSPRI-104137 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aYoung, Neal W. 245 10 ‡aEvidence of environmental change since the last glacial maximum inferred from chemical analysis of an ice core from Law Dome, Antarctica (abstract) /‡cNeal W. Young, M. de Angelis, D. Davies. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1990. 300 ## ‡ap. 365. 500 ## ‡aAnnals of Glaciology. Vol. 14 :365 (1990). 520 3# ‡aConcentration of major anions and cations measured on samples selected from ice core to give information on major environmental changes which have occurred from 26 to 6 ka BP. Chemical species can be divided into those from marine (Na and Mg) and continental (Al) sources. Methane sulphonic acid also determined; this has marine biogenic source and exhibits pattern which is generally unrelated to variations in main divisions. Oxygen isotope ratios provide additional data source. 650 07 ‡a551.324.29 -- Land ice, miscellaneous forms.‡2udc 650 07 ‡a551.324.84 -- Land ice, impurities.‡2udc 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a54 -- Chemistry.‡2udc 650 07 ‡a539.155.2 -- Isotopic analysis.‡2udc 650 07 ‡a551.583 -- Climatic changes.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 651 #7 ‡a(*747.3) -- Budd Coast.‡2udc 700 1# ‡aAngelis, M. de. 700 1# ‡aDavies, D. 773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 14 (1990) ‡wSPRI-60773 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231211