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Record #113474:

The paleoclimatic setting of the Late Paleozoic marine ice sheet in the Karoo Basin of southern Africa / Johan N.J. Visser.

Title: The paleoclimatic setting of the Late Paleozoic marine ice sheet in the Karoo Basin of southern Africa / Johan N.J. Visser.
Author(s): Visser, Johan N. J.
Date: 1991.
Publisher: Boulder, CO: Geological Society of America
In: Glacial marine sedimentation; paleoclimatic significance. (1991.),
Abstract: Evidence exists for continuum of polar to temperate climatic settings during Permo-Carboniferous glaciation in Dwyka Basin. Ancient glaciomarine sequences cannot be defined simply as having polar, subpolar or temperate settings. In terms of sediment volume, Dwyka Formation was deposited during warmer subpolar spells, related to high sea levels, alternating with severe polar conditions.
Notes:

In: Glacial marine sedimentation; paleoclimatic significance / John B. Anderson, Gail M. Ashley, eds.

Keywords: 551.33 -- Glacial geology.
551.332.25 -- Glacio-marine deposits.
551.336 -- Ice ages.
551.73 -- Palaeozoic.
551.583.7 -- Palaeoclimatology.
E7 -- Glaciology: glacial geology and ice ages.
(68) -- States and territories of southern Africa.
SPRI record no.: 113474

MARCXML

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007 ta
008 240329s1991####couab##|#####|0||#0#eng#d
035 ## ‡aSPRI-113474
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aVisser, Johan N. J.
245 14 ‡aThe paleoclimatic setting of the Late Paleozoic marine ice sheet in the Karoo Basin of southern Africa /‡cJohan N.J. Visser.
260 ## ‡aBoulder, CO :‡bGeological Society of America,‡c1991.
300 ## ‡ap. 181-189 :‡bill., diags., maps.
490 0# ‡aGeological Society of America Special ;‡vPaper 261
500 ## ‡aIn: Glacial marine sedimentation; paleoclimatic significance / John B. Anderson, Gail M. Ashley, eds.
520 3# ‡aEvidence exists for continuum of polar to temperate climatic settings during Permo-Carboniferous glaciation in Dwyka Basin. Ancient glaciomarine sequences cannot be defined simply as having polar, subpolar or temperate settings. In terms of sediment volume, Dwyka Formation was deposited during warmer subpolar spells, related to high sea levels, alternating with severe polar conditions.
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.332.25 -- Glacio-marine deposits.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.73 -- Palaeozoic.‡2udc
650 07 ‡a551.583.7 -- Palaeoclimatology.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(68) -- States and territories of southern Africa.‡2udc
773 0# ‡7nnam ‡aJohn B. Anderson, Gail M. Ashley, eds. ‡tGlacial marine sedimentation; paleoclimatic significance. ‡dBoulder, CO : Geological Society of America, 1991. ‡wSPRI-113463
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240329