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Record #117915:

¹⁰Be deposition at Vostok, Antarctica during the last 50,000 years and its relationship to possible cosmogenic production variations during this period / G.M. Raisbeck, F. Yiou, Jean Jouzel, J.R. Petit, N.I. Barkov, Edouard Bard.

Title: ¹⁰Be deposition at Vostok, Antarctica during the last 50,000 years and its relationship to possible cosmogenic production variations during this period / G.M. Raisbeck, F. Yiou, Jean Jouzel, J.R. Petit, N.I. Barkov, Edouard Bard.
Author(s): Raisbeck, G. M.
Yiou, F.
Jouzel, Jean.
Petit, J. R.
Barkov, N. I.
Bard, Edouard.
Date: 1992.
Publisher: Berlin: Springer
In: Last deglaciation : absolute and radiocarbon chronologies. (1992.),
Abstract: Calculated ¹⁰Be deposition rate is approximately constant over past 50 ka, thus giving no evidence for any large (>20%) variation in cosmogenic production during this period, except for 1 to 2 ka interval 35 ka BP, when it increased by factor of 2.
Notes:

In: The last deglaciation : absolute and radiocarbon chronologies / Edouard Bard, Wallace S. Broecker, eds.

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.24 -- Ice sheets and caps.
551.324.84 -- Land ice, impurities.
54.027 -- Isotope analysis.
524.1 -- Cosmic rays.
551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.
622.14 -- Core sampling, ice and snow.
E5 -- Glaciology: land ice.
(*7) -- Antarctic regions.
(*74) -- Australian Antarctic Territory.
(*747.5) -- Vostok region.
SPRI record no.: 117915

MARCXML

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245 00 ‡a¹⁰Be deposition at Vostok, Antarctica during the last 50,000 years and its relationship to possible cosmogenic production variations during this period /‡cG.M. Raisbeck, F. Yiou, Jean Jouzel, J.R. Petit, N.I. Barkov, Edouard Bard.
260 ## ‡aBerlin :‡bSpringer,‡c1992.
300 ## ‡ap. 127-139 :‡bdiag.
490 0# ‡aNATO ASI Series. Series I: Global Environmental Change ;‡v2
500 ## ‡aIn: The last deglaciation : absolute and radiocarbon chronologies / Edouard Bard, Wallace S. Broecker, eds.
520 3# ‡aCalculated ¹⁰Be deposition rate is approximately constant over past 50 ka, thus giving no evidence for any large (>20%) variation in cosmogenic production during this period, except for 1 to 2 ka interval 35 ka BP, when it increased by factor of 2.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.24 -- Ice sheets and caps.‡2udc
650 07 ‡a551.324.84 -- Land ice, impurities.‡2udc
650 07 ‡a54.027 -- Isotope analysis.‡2udc
650 07 ‡a524.1 -- Cosmic rays.‡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 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*74) -- Australian Antarctic Territory.‡2udc
651 #7 ‡a(*747.5) -- Vostok region.‡2udc
700 1# ‡aRaisbeck, G. M.
700 1# ‡aYiou, F.
700 1# ‡aJouzel, Jean.
700 1# ‡aPetit, J. R.
700 1# ‡aBarkov, N. I.
700 1# ‡aBard, Edouard.
773 0# ‡7nnam ‡aEdouard Bard, Wallace S. Broecker, eds. ‡tLast deglaciation : absolute and radiocarbon chronologies. ‡dBerlin : Springer, 1992. ‡wSPRI-117909
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221004