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Record #125842:

Late Tertiary Antarctic paleoclimate and ice-sheet dynamics inferred from surficial deposits in Wright Valley / Brenda L. Hall, George H. Denton, Daniel R. Lux, James G. Bockheim.

Title: Late Tertiary Antarctic paleoclimate and ice-sheet dynamics inferred from surficial deposits in Wright Valley / Brenda L. Hall, George H. Denton, Daniel R. Lux, James G. Bockheim.
Author(s): Hall, Brenda L.
Denton, George H.
Lux, Daniel R.
Bockheim, James G.
Date: 1993.
In: Geografiska Annaler. Series A. Physical Geography. (1993.), Vol. 75A(4) (1993)
Abstract: Evidence from drift deposits shows neither Pliocene ice-sheet overriding of Transantarctic Mountains during last 3.8 Ma, nor warming sufficient to impose extensive melting margins on glaciers at sea level during past 3.7 Ma. Concludes that Pliocene collapse of east Antarctic ice sheet after 3.7 Ma is unlikely, and supports traditional view that ice sheet has remained relative stable since Middle Miocene.
Notes:

Geografiska Annaler. Series A. Physical Geography. Vol. 75A(4) :239-267 (1993).

Keywords: 551.33 -- Glacial geology.
551.332.2 -- Drift, glacial. Deposits.
551.336 -- Ice ages.
551.78 -- Tertiary.
551.782.2 -- Pliocene.
551.782.1 -- Miocene.
551.337 -- Chronology of the Pleistocene and recent periods.
551.583.7 -- Palaeoclimatology.
551.436.5 -- Dry valleys.
E7 -- Glaciology: glacial geology and ice ages.
(*7) -- Antarctic regions.
(*7.7) -- West Antarctica.
SPRI record no.: 125842

MARCXML

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035 ## ‡aSPRI-125842
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245 00 ‡aLate Tertiary Antarctic paleoclimate and ice-sheet dynamics inferred from surficial deposits in Wright Valley /‡cBrenda L. Hall, George H. Denton, Daniel R. Lux, James G. Bockheim.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1993.
300 ## ‡ap. 239-267 :‡bill., tables, maps.
500 ## ‡aGeografiska Annaler. Series A. Physical Geography. Vol. 75A(4) :239-267 (1993).
520 3# ‡aEvidence from drift deposits shows neither Pliocene ice-sheet overriding of Transantarctic Mountains during last 3.8 Ma, nor warming sufficient to impose extensive melting margins on glaciers at sea level during past 3.7 Ma. Concludes that Pliocene collapse of east Antarctic ice sheet after 3.7 Ma is unlikely, and supports traditional view that ice sheet has remained relative stable since Middle Miocene.
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.332.2 -- Drift, glacial. Deposits.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.78 -- Tertiary.‡2udc
650 07 ‡a551.782.2 -- Pliocene.‡2udc
650 07 ‡a551.782.1 -- Miocene.‡2udc
650 07 ‡a551.337 -- Chronology of the Pleistocene and recent periods.‡2udc
650 07 ‡a551.583.7 -- Palaeoclimatology.‡2udc
650 07 ‡a551.436.5 -- Dry valleys.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*7.7) -- West Antarctica.‡2udc
700 1# ‡aHall, Brenda L.
700 1# ‡aDenton, George H.
700 1# ‡aLux, Daniel R.
700 1# ‡aBockheim, James G.
773 0# ‡7nnas ‡tGeografiska Annaler. Series A. Physical Geography. ‡gVol. 75A(4) (1993) ‡wSPRI-40621
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221005