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Biscaye PE, Grousset FE, Revel M, Van der Gaast S, Zielinski GA, Vaars A et al (1997) Asian
provenance of glacial dust (stage 2) in the Greenland Ice Sheet Project 2 Ice Core, Summit,
Greenland. J Geophys Res 102:26765-26781
Bory AJ-M, Biscaye PE, Svensson A, Grousset FE (2002) Seasonal variability in the origin of
recent atmospheric mineral dust at NorthGRIP, Greenland. Earth Planet Sci Lett 196:123-134
Bory A, Wolff E, Mulvaney R, Jagoutz E, Wegner A, Ruth U et al (2010) Multiple sources supply
eolian mineral dust to the Atlantic sector of coastal Antarctica: Evidence from recent snow
layers at the top of Berkner Island ice sheet. Earth Planet Sci Lett 291:138-148
Burton GR, Rosman KJR, Candelone J-P, Burn LJ, Boutron CF, Hong S (2007) The impact of
climatic conditions on Pb and Sr isotopic ratios found in Greenland ice, 7-150 ky BP. Earth
Planet Sci Lett 259:557-566
Chen J, Li G, Yang J, Rao W, Lu H, Balsam W et al (2007) Nd and Sr isotopic characteristics of
Chinese deserts: implications for the provenances of Asian dust. Geochim Cosmochim Acta
71:3904-3914
Dansgaard W, Johnsen SJ, Møller J, Langway CC Jr (1969) One thousand centuries of climatic
record from Camp Century on the Greenland ice sheet. Science 166:377-381
De Angelis M, Legrand M, Petit JR, Barkov NI, Korotkevitch YS, Kotlyakov VM (1984)
Soluble and insoluble impurities along the 950 m deep Vostok ice core (Antarctica) - climatic
implications. J Atmos Chem 1:215-239
De Angelis M, Barkov NI, Petrov VN (1987) Aerosol concentrations over the last climatic cycle
(160 kyr) from an Antarctic ice core. Nature 325:318-321
De Deckker P, Norman M, Goodwin ID, Wain A, Gingele FX (2010) Lead isotopic evidence for an
Australian source of aeolian dust to Antarctica at times over the last 170,000 years. Palaeogeogr
Palaeoclimatol Palaeoecol 285:205-223
Delmonte B, Petit J-R, Maggi V (2002a) Glacial to Holocene implications of the new 27000-year
dust record from the EPICA Dome C (East Antarctica) ice core. Clim Dyn 18:647-660
Delmonte B, Petit J-R, Maggi V (2002b) LGM-Holocene changes and Holocene millennial-scale
oscillations of dust particles in the EPICA Dome C ice core, East Antarctica. Ann Glaciol
35:306-312
Delmonte B, Basile-Doelsch I, Petit J-R, Maggi V, Revel-Rolland M, Michard A et al (2004a)
Comparing the EPICA and Vostok dust records during the last 220,000 years: stratigraphic
correlation and provenance in glacial periods. Earth-Sci Rev 66:63-87
Delmonte B, Petit JR, Andersen KK, Basile-Doelsch I, Maggi V, Ya Lipenkov V (2004b) Dust size
evidence for opposite regional atmospheric circulation changes over east Antarctica during the
last climatic transition. Clim Dyn 23:427-438
Delmonte B, Petit JR, Basile-Doelsch I, Jagoutz E, Maggi V (2007) Late quaternary interglacials in
East Antarctica from ice core dust records. In: Sirocko F, Litt T, Claussen M (eds) The climate
of past interglacials, vol 7. Elsevier, Amsterdam, pp 53-73
Delmonte B, Baroni C, Andersson PS, Schoberg H, Hansson M, Aciego S et al (2010) Aeolian
dust in the Talos Dome ice core (East Antarctica, Pacific/Ross Sea sector): Victoria Land versus
remote sources over the last two climate cycles. J Quat Sci 25:1327-1337
Drab E, Gaudichet A, Jaffrezo JL, Colin JL (2002) Mineral particles content in recent snow at
Summit (Greenland). Atmos Environ 36:5365-5376
Edwards R, Sedwick P, Morgan V, Boutron C (2006) Iron in ice cores from Law Dome: a record of
atmospheric iron deposition for maritime East Antarctica during the Holocene and Last Glacial
Maximum. Geochem Geophys Geosyst 7(12):Q12Q01. doi:
10.1029/2006GC001307
Faria SH, Freitag J, Kipfstuhl S (2010) Polar ice structure and the integrity of ice-core paleoclimate
records. Quat Sci Rev 29:338-351
Fattori I, Becagli S, Bellandi S, Castellano E, Innocenti M, Mannini A et al (2005) Chemical
composition and physical features of summer aerosol at Terra Nova Bay and Dome C,
Antarctica. J Environ Monit 7:1265-1274
Feng J-L, Hu Z-G, Ju J-T, Zhu L-P (2011) Variations in trace element (including rare earth element)
concentrations with grain sizes in loess and their implications for tracing the provenance of
eolian deposits. Quat Int 236:116-126
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