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Record #104102:
- #104102
Main publication details
MARC recordAtmospheric chemistry changes over the last climatic cycle (180 000 years) inferred from the Vostok (Antarctica) ice-core study (abstract) / M. Legrand, C. Feniet-Saigne, J.R. Petit.
| Title: | Atmospheric chemistry changes over the last climatic cycle (180 000 years) inferred from the Vostok (Antarctica) ice-core study (abstract) / M. Legrand, C. Feniet-Saigne, J.R. Petit. |
| Author(s): | Legrand, M. Feniet-Saigne, C. Petit, J. R. |
| Date: | 1990. |
| In: | Annals of Glaciology. (1990.), Vol. 14 (1990) |
| Abstract: | Isotopic composition of ice in 2200 m ice core identifies series of ions originating from impurities in atmosphere deposited over whole last climatic cycle. Large variations of marine and terrestrial aerosols reflect global (source strength and transport efficiency) and local (deposition) changes. Secondary aerosols or gases exhibit more moderate variations. Discusses significance of several specific periodicities. |
| Notes: | Annals of Glaciology. Vol. 14 :344 (1990). |
| Keywords: | 551.32 -- Glaciology. 551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc. 622.14 -- Core sampling, ice and snow. 551.324.84 -- Land ice, impurities. 551.324 -- Land ice. 539.155.2 -- Isotopic analysis. 551.510.42 -- Atmospheric impurities, dust and aerosols. E5 -- Glaciology: land ice. (*7) -- Antarctic regions. (*747.5) -- Vostok region. |
| SPRI record no.: | 104102 |
LDR 01605naa#a2200000#a#4500 001 SPRI-104102 005 20230325044322.0 007 ta 008 230325s1990####xx####|##|###|0||#0|eng#d 035 ## ‡aSPRI-104102 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aLegrand, M. 245 10 ‡aAtmospheric chemistry changes over the last climatic cycle (180 000 years) inferred from the Vostok (Antarctica) ice-core study (abstract) /‡cM. Legrand, C. Feniet-Saigne, J.R. Petit. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1990. 300 ## ‡ap. 344. 500 ## ‡aAnnals of Glaciology. Vol. 14 :344 (1990). 520 3# ‡aIsotopic composition of ice in 2200 m ice core identifies series of ions originating from impurities in atmosphere deposited over whole last climatic cycle. Large variations of marine and terrestrial aerosols reflect global (source strength and transport efficiency) and local (deposition) changes. Secondary aerosols or gases exhibit more moderate variations. Discusses significance of several specific periodicities. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.‡2udc 650 07 ‡a622.14 -- Core sampling, ice and snow.‡2udc 650 07 ‡a551.324.84 -- Land ice, impurities.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a539.155.2 -- Isotopic analysis.‡2udc 650 07 ‡a551.510.42 -- Atmospheric impurities, dust and aerosols.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 651 #7 ‡a(*747.5) -- Vostok region.‡2udc 700 1# ‡aFeniet-Saigne, C. 700 1# ‡aPetit, J. R. 773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 14 (1990) ‡wSPRI-60773 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230325