Atmospheric dust loadings play a crucial role in the global climate system. Southern South America is a key dust source, however, dust deposition rates remain poorly quantified since the last glacial termination (~17 kyr ago), an important timeframe to anticipate future climate changes. Here we use isotope and element geochemistry in a peat archive from Tierra del Fuego, to reconstruct atmospheric dust fluxes and associated environmental and westerly wind changes for the past 16.2 kyr. Dust depositions were elevated during the Antarctic Cold Reversal (ACR) and second half of the Younger Dryas (YD) stadial, originating from the glacial Beagle Channel valley. This increase was most probably associated with a strengthening of the westerlies du...
The Puna-Altiplano plateau represents a regionally significant dust source, which is critically loca...
Downcore sediment grain-size records of mineral dust (2e10 mm) can provide key insights into changes...
I develop and interpret a late Holocene record of dust deposition from the West Antarctic Ice Sheet ...
Atmospheric dust loadings play a crucial role in the global climate system. Southern South America i...
The latitudinal displacement of the southern westerlies and associated climate systems is a key para...
Atmospheric mineral dust is intrinsically linked with climate. Although dust flux variability on gla...
Dust in the atmosphere plays a role in the transparency of the atmosphere1, the mineral nourishment ...
Patagonian dust is the darling of researchers of paleoclimatic variability of southern South America...
This paper presents the first detailed paleoclimate reconstruction of the latest Antarctic isotope m...
Antarctic ice preserves an ~800 kyr record of dust activity in the Southern Hemisphere. Major effort...
The source area of continental dust deposited at both Vostok and Dome C sites (East Antarctica) duri...
The strontium and neodymium isotopic signature of aeolian mineral particles archived in polar ice co...
The Puna-Altiplano plateau represents a regionally significant dust source, which is critically loca...
Downcore sediment grain-size records of mineral dust (2e10 mm) can provide key insights into changes...
I develop and interpret a late Holocene record of dust deposition from the West Antarctic Ice Sheet ...
Atmospheric dust loadings play a crucial role in the global climate system. Southern South America i...
The latitudinal displacement of the southern westerlies and associated climate systems is a key para...
Atmospheric mineral dust is intrinsically linked with climate. Although dust flux variability on gla...
Dust in the atmosphere plays a role in the transparency of the atmosphere1, the mineral nourishment ...
Patagonian dust is the darling of researchers of paleoclimatic variability of southern South America...
This paper presents the first detailed paleoclimate reconstruction of the latest Antarctic isotope m...
Antarctic ice preserves an ~800 kyr record of dust activity in the Southern Hemisphere. Major effort...
The source area of continental dust deposited at both Vostok and Dome C sites (East Antarctica) duri...
The strontium and neodymium isotopic signature of aeolian mineral particles archived in polar ice co...
The Puna-Altiplano plateau represents a regionally significant dust source, which is critically loca...
Downcore sediment grain-size records of mineral dust (2e10 mm) can provide key insights into changes...
I develop and interpret a late Holocene record of dust deposition from the West Antarctic Ice Sheet ...