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Record #127812:
Late Quaternary stable isotopic stratigraphy of Hole 910A, Yermak Plateau, Arctic Ocean: relations with Svalbard/Barents Sea ice sheet history / Benjamin P. Flower.
Title: | Late Quaternary stable isotopic stratigraphy of Hole 910A, Yermak Plateau, Arctic Ocean: relations with Svalbard/Barents Sea ice sheet history / Benjamin P. Flower. |
Author(s): | Flower, Benjamin P. |
Date: | 1993. |
In: | Ocean Drilling Program. Proceedings. Scientific Results. (1993.), Vol. 151(26) (1993) |
Abstract: | Hole at 552 m water depth provides early opportunity for high resolution studies of Quaternary Arctic Ocean climates. Oxygen and carbon isotopic data based on Neogloboquadrina pachyderma from top 24.5 m provide both stratigraphic age control and history of latter Quaternary surface water environments. Isotope values can be explained by 1) episodic grounding of marine based ice sheet and/or 2) coarser grained glacial sedimentation. Major change in Svalbard/Barents Sea ice sheet is suggest by oxygen isotopic stratigraphy near Stage 17/16 boundary (670 ka) |
Notes: | Ocean Drilling Program. Proceedings. Scientific Results. Vol. 151(26) :445-454 (1993). |
Keywords: | 54.027 -- Isotope analysis. 551.326.7 -- Sea ice. 551.461.8 -- Palaeo-oceanography. 551.583.3 -- Climatic changes, Quaternary. 551.79 -- Quaternary. 91(08) -- Expeditions: 1993 JOIDES Resolution. C -- Oceanography, hydrography and hydrology. (*3) -- Arctic regions. (*60) -- Arctic Ocean and adjacent waters. |
SPRI record no.: | 127812 |
LDR 01731naa#a2200000#a#4500 001 SPRI-127812 005 20240328123902.0 007 ta 008 240328s1993####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-127812 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aFlower, Benjamin P. 245 10 ‡aLate Quaternary stable isotopic stratigraphy of Hole 910A, Yermak Plateau, Arctic Ocean :‡brelations with Svalbard/Barents Sea ice sheet history /‡cBenjamin P. Flower. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1993. 300 ## ‡ap. 445-454 :‡bdiags., tables, map. 500 ## ‡aOcean Drilling Program. Proceedings. Scientific Results. Vol. 151(26) :445-454 (1993). 520 3# ‡aHole at 552 m water depth provides early opportunity for high resolution studies of Quaternary Arctic Ocean climates. Oxygen and carbon isotopic data based on Neogloboquadrina pachyderma from top 24.5 m provide both stratigraphic age control and history of latter Quaternary surface water environments. Isotope values can be explained by 1) episodic grounding of marine based ice sheet and/or 2) coarser grained glacial sedimentation. Major change in Svalbard/Barents Sea ice sheet is suggest by oxygen isotopic stratigraphy near Stage 17/16 boundary (670 ka) 650 07 ‡a54.027 -- Isotope analysis.‡2udc 650 07 ‡a551.326.7 -- Sea ice.‡2udc 650 07 ‡a551.461.8 -- Palaeo-oceanography.‡2udc 650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc 650 07 ‡a551.79 -- Quaternary.‡2udc 650 07 ‡a91(08) -- Expeditions: 1993 JOIDES Resolution.‡2udc 650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 773 0# ‡7nnas ‡tOcean Drilling Program. Proceedings. Scientific Results. ‡gVol. 151(26) (1993) ‡wSPRI-96524 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240328