Global change over the last climatic cycle from the vostok ice core record (Antarctica)
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Cited by (19)
Late Quaternary terrigenous sediment supply in the Drake Passage in response to Patagonian and Antarctic ice dynamics
2023, Global and Planetary ChangeCitation Excerpt :Since the clay mineral assemblages reveal distinct temporal changes, we applied the ratios of smectite/(chlorite + illite) and quartz/feldspar to describe the mineralogical variations within the clay fraction (Fig. 6). During the full glacial stages MIS 6 and 2 (Jouzel et al., 1989), we find low smectite/(chlorite + illite), quartz/feldspar, Ti/Al, and Si/Al ratios associated with high χMSterr values, and Fe-rich chlorite, Ti/Ca and Fe/Ca ratios (Figs. 3, 4 and 6). These features are consistent with basic to intermediate and undifferentiated parent rocks in the southern South America and on the Antarctic Peninsula (Burton-Johnson and Riley, 2015; Diekmann et al., 2000; Hillenbrand et al., 2009; Marinoni et al., 2008).
Holocene climate variability from the lake sediment core in Schirmacher Oasis region, East Antarctica: Multiproxy approach
2016, Quaternary InternationalCitation Excerpt :Moreover, during the Holocene, the climate variation in both the hemisphere glacier retreat and re-advancement are neither strictly in the phase, nor out of phase as evidenced by the studies of glaciers retreat or readvancement in New Zealand records (Schaefer et al., 2009). The Antarctic climatic history reconstructed from long ice-cores is significant in improving our understanding of the atmosphere circulation and composition (Jouzel et al., 1989, 2007). Despite, the long ice-core studies which have been carried out to understand the long term glacial-interglacial climatic changes, the contribution of ice core studies within the Holocene from coastal areas of East Antarctica did not show promising results.
Soils and the Quaternary climate system
2003, Developments in Quaternary ScienceCitation Excerpt :Both terrestrial and marine evidence support the argument for multiple glaciations associated with water and temperature cycles through the Quaternary (Winograd et al., 1997). In some cases, moisture delivery to high latitudes increased preceding glacial maxima (Winograd, 2001) and decreased at maxima (Jouzel et al., 1989). During glacial periods, many pluvial lakes and inland seas expanded greatly due to shifts in moisture patterns and boundaries (Smith & Street-Perrot, 1983).
Quaternary paleoenvironmental change on the Tibetan Plateau and adjacent areas (Western China and Western Mongolia)
2000, Quaternary InternationalTropical South America during the Last Glacial Maximum: Evidence from glacial, periglacial and fluvial records
2000, Quaternary InternationalLate Quaternary environmental changes and the alluvial record in humid tropical environments
2000, Quaternary International