DOI: 10.1016/j.quascirev.2015.09.017
Scopus记录号: 2-s2.0-84989913818
论文题名: Provenance analysis of central Arctic Ocean sediments: Implications for circum-Arctic ice sheet dynamics and ocean circulation during Late Pleistocene
作者: Kaparulina E. ; Strand K. ; Lunkka J.P.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2016
卷: 147 起始页码: 210
结束页码: 220
语种: 英语
英文关键词: Circulation
; Circum-Arctic
; Heavy minerals
; Ice sheet
; Late Pleistocene
; Lomonosov ridge
; Paleoclimate
; Provenance
Scopus关键词: Boiler circulation
; Glacial geology
; Glaciers
; Minerals
; Oceanography
; Sea ice
; Sediments
; Circum-Arctic
; Heavy minerals
; Ice sheet
; Late Pleistocene
; Lomonosov ridges
; Paleoclimates
; Provenance
; Ice
英文摘要: Mineralogical and geochemical data generated from the well referred shallow core 96/12-1pc on the Lomonosov Ridge, central Arctic Ocean was used to evaluate ice transport from the circum-Arctic sources and variability in sediment drainage and provenance changes. In this study heavy minerals in central Arctic sediments were used to determine those most prominent provenance areas and their changes related to the Late Pleistocene history of glaciations in the Arctic. Provenance changes were then used to infer variations in the paleoceanographic environment of the central Arctic Ocean, such as variations in the distribution of sea ice, icebergs controlled by the Arctic Ocean circulation. Four critical end-members including Victoria and Banks Islands, the Putorana Plateau, the Anabar Shield, and the Verkhoyansk Fold Belt were identified from the Amerasian and Eurasian source areas, and their proportional contributions were estimated in relation to Late Pleistocene ice sheet dynamics and ocean circulation. The results show changes in transport pathways and source areas within two examined transitions MIS6-5 and MIS4-3. The main source for material during MIS6-5 transition was Amerasian margin due to the high dolomite content in the studied section of sediments inferring strong Beaufort Gyre (BG) and Transpolar Drift (TPD) transport for this material. IRD material during late the MIS6 to 5 deglacial event was from terrigenous input through from the MacKenzie route Banks/Victoria Islands then transported as far as the Lomonosov Ridge area. The transition, MIS4-3 in comparison with MIS6-5, shows a clear shift in source areas, reflected in a different mineralogical composition of sediments, supplied from the Eurasian margin, such as the Anabar Shield, the Putorana Plateau and the Verkhoyansk Fold Belt during active decay of the Barents-Kara Ice Sheet presumable associated with an ice-dammed lake outburst then triggered by a strong TPD over the central Arctic. These two studied deglaciations suggest that contributions of different circum-Arctic sediment sources are related to interaction between ice sheet decay, sea ice production and circulation. © 2015 Elsevier Ltd Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/59503
Appears in Collections: 过去全球变化的重建
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作者单位: Thule Institute, University of Oulu, PO Box 7300, Oulu, Finland; Oulu Mining School, University of Oulu, PO Box 3000, Oulu, Finland
Recommended Citation:
Kaparulina E.,Strand K.,Lunkka J.P.. Provenance analysis of central Arctic Ocean sediments: Implications for circum-Arctic ice sheet dynamics and ocean circulation during Late Pleistocene[J]. Quaternary Science Reviews,2016-01-01,147