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Record #149182:

Changes in climate, ocean and ice-sheet conditions in the Ross embayment, Antarctica, at 6 ka / Eric J. Steig, Charles P. Hart, James W.C. White, Wendy L. Cunningham, Matthew D. Davis, Eric S. Saltzman.

Title: Changes in climate, ocean and ice-sheet conditions in the Ross embayment, Antarctica, at 6 ka / Eric J. Steig, Charles P. Hart, James W.C. White, Wendy L. Cunningham, Matthew D. Davis, Eric S. Saltzman.
Author(s): Steig, Eric J.
Hart, Charles P.
White, James W. C.
Cunningham, Wendy L.
Davis, Matthew D.
Saltzman, Eric S.
Date: 1998.
In: Annals of Glaciology. (1998.), Vol. 27 (1998)
Abstract: Data from Taylor Dome, East Antarctica and sediment cores from western Ross Sea suggest abrupt cooling and concomitant increase in sea-ice cover about 6000 BP. Radiocarbon dates from raised beach deposits indicate retreat of ice shelves in Ross embayment ceased about 6 ka, coinciding with other environmental changes inferred. Climate seems to be important in controlling evolution of ice-shelf margins following end of last glaciation.
Notes:

Annals of Glaciology. Vol. 27 :305-310 (1998).

International Symposium on Antarctica and Global Change: Interactions and Impacts, W.F. Budd (Editor), 13--18 July 1997, Hobart, Tasmania, Australia.

Keywords: 551.583 -- Climatic changes.
551.583.3 -- Climatic changes, Quaternary.
550.93 -- Geochronology.
539.16 -- Radio-carbon dating.
551.32 -- Glaciology.
551.324 -- Land ice.
551.324.24 -- Ice sheets and caps.
551.326 -- Floating ice.
551.326.7 -- Sea ice.
E7 -- Glaciology: glacial geology and ice ages.
(*7) -- Antarctic regions.
(*881) -- Ross Sea.
SPRI record no.: 149182

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245 00 ‡aChanges in climate, ocean and ice-sheet conditions in the Ross embayment, Antarctica, at 6 ka /‡cEric J. Steig, Charles P. Hart, James W.C. White, Wendy L. Cunningham, Matthew D. Davis, Eric S. Saltzman.
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520 3# ‡aData from Taylor Dome, East Antarctica and sediment cores from western Ross Sea suggest abrupt cooling and concomitant increase in sea-ice cover about 6000 BP. Radiocarbon dates from raised beach deposits indicate retreat of ice shelves in Ross embayment ceased about 6 ka, coinciding with other environmental changes inferred. Climate seems to be important in controlling evolution of ice-shelf margins following end of last glaciation.
650 07 ‡a551.583 -- Climatic changes.‡2udc
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650 07 ‡a550.93 -- Geochronology.‡2udc
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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 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*881) -- Ross Sea.‡2udc
700 1# ‡aSteig, Eric J.
700 1# ‡aHart, Charles P.
700 1# ‡aWhite, James W. C.
700 1# ‡aCunningham, Wendy L.
700 1# ‡aDavis, Matthew D.
700 1# ‡aSaltzman, Eric S.
773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 27 (1998) ‡wSPRI-60773
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