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Record #117916:
- #117916
Main publication details
MARC record¹⁰Be peaks as time markers in polar ice cores / J. Beer, and 8 others.
| Title: | ¹⁰Be peaks as time markers in polar ice cores / J. Beer, and 8 others. |
| Author(s): | Beer, J. |
| Date: | 1992. |
| Publisher: | Berlin: Springer |
| In: | Last deglaciation : absolute and radiocarbon chronologies. (1992.), |
| Abstract: | ¹⁰Be concentration peaks observed in Antarctic ice cores from Vostok (35 and 60 ka BP) and Dome Circe (35 ka BP) offer possibility of synchronizing ice-core records from southern and northern hemispheres. 35 ka BP peak is clearly present in Byrd (Antarctic) core and probably in Camp Century (Greenland) core. Comparisons with δ¹⁸O and SO₄ suggest that peak is caused by higher production rate of cosmogenic radionuclides rather than by climatic effects. 60 ka BP peak could not be found in either core, perhaps due to inadequate sampling. |
| 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. (*747.6) -- Dome Circe region. (*772) -- Byrd Land. (*38) -- Greenland. |
| SPRI record no.: | 117916 |
LDR 01980naa#a2200000#a#4500 001 SPRI-117916 005 20230922095230.0 007 ta 008 230922s1992####gw#a###|#####|0||#0#eng#d 035 ## ‡aSPRI-117916 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aBeer, J. 245 10 ‡a¹⁰Be peaks as time markers in polar ice cores /‡cJ. Beer, and 8 others. 260 ## ‡aBerlin :‡bSpringer,‡c1992. 300 ## ‡ap. 141-153 :‡bdiags. 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# ‡a¹⁰Be concentration peaks observed in Antarctic ice cores from Vostok (35 and 60 ka BP) and Dome Circe (35 ka BP) offer possibility of synchronizing ice-core records from southern and northern hemispheres. 35 ka BP peak is clearly present in Byrd (Antarctic) core and probably in Camp Century (Greenland) core. Comparisons with δ¹⁸O and SO₄ suggest that peak is caused by higher production rate of cosmogenic radionuclides rather than by climatic effects. 60 ka BP peak could not be found in either core, perhaps due to inadequate sampling. 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 651 #7 ‡a(*747.6) -- Dome Circe region.‡2udc 651 #7 ‡a(*772) -- Byrd Land.‡2udc 651 #7 ‡a(*38) -- Greenland.‡2udc 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# ‡a20230922