FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3213773670> ?p ?o ?g. }

• W3213773670 endingPage "107271" @default.
• W3213773670 startingPage "107271" @default.
• W3213773670 abstract "Compositions of mineral dust in ice cores serve as tracers of paleo-atmospheric circulation patterns, providing linkages between sources and sinks. Here we document the geochemical makeup of dust reaching continental West Antarctica, on late Holocene samples from the Siple Dome A ice core (spanning ∼1030–1800 C.E). The Nd–Sr isotope signature is unusual for Antarctic ice core dust samples. Siple Dome data are characterized by low Nd isotope ratios (as low as εNd = −16.3) along with low Sr isotope ratios (highest 87Sr/86Sr = 0.7102) compared with other Antarctic dust signatures. A well-defined inverse correlation between Sr–Nd isotope ratios indicates two primary mixing sources. The low εNd-values indicate involvement of ancient (Archean-to-early Proterozoic) continental crust, as either the direct source or as a precursor of the source, and the low Sr-values require low Rb/Sr ratios that often reflect high-grade metamorphism. The known Antarctic terrane with these characteristics is parts of Enderby Land, nearly at the opposite end of Antarctica. The isotopic signature of the second end-member is compatible with West Antarctic volcanoes or Patagonia in South America. The Sr–Nd isotopes and trace element abundances are also chemically compatible with mixing between volcanic material from Gaussberg, a small lamproite volcano in Kaiser Wilhelm II Land in coastal East Antarctica whose source is ancient lithospheric mantle, with dust from Patagonia or material from West Antarctic volcanoes. We assess these potential mixing scenarios and conclude that Siple Dome's unusual geochemical signature can best be explained by a mixture of Patagonian dust and a Gaussberg-like source, with additional minor contributions from old eroded Archean-to-early Proterozoic bedrock sources such as those in Enderby Land. Moreover, Siple Dome dust compositions are distinct from dust deposited on Taylor and Clark Glaciers in the McMurdo Dry Valleys of the western Ross Sea, precluding the Dry Valleys as a late Holocene dust source to this region of the eastern Ross Sea." @default.
• W3213773670 created "2021-11-22" @default.
• W3213773670 creator A5000571500 @default.
• W3213773670 creator A5001784726 @default.
• W3213773670 creator A5013299024 @default.
• W3213773670 creator A5027992695 @default.
• W3213773670 creator A5042537454 @default.
• W3213773670 creator A5052477206 @default.
• W3213773670 creator A5067690055 @default.
• W3213773670 creator A5091285519 @default.
• W3213773670 date "2021-12-01" @default.
• W3213773670 modified "2023-10-16" @default.
• W3213773670 title "Late Holocene dust provenance at Siple Dome, Antarctica" @default.
• W3213773670 cites W1556220029 @default.
• W3213773670 cites W1602475393 @default.
• W3213773670 cites W1897631106 @default.
• W3213773670 cites W1963895982 @default.
• W3213773670 cites W1963960391 @default.
• W3213773670 cites W1965841742 @default.
• W3213773670 cites W1967248360 @default.
• W3213773670 cites W1970805999 @default.
• W3213773670 cites W1972456376 @default.
• W3213773670 cites W1973752938 @default.
• W3213773670 cites W1977533161 @default.
• W3213773670 cites W1978002563 @default.
• W3213773670 cites W1985378157 @default.
• W3213773670 cites W1986045371 @default.
• W3213773670 cites W1990432890 @default.
• W3213773670 cites W1996055672 @default.
• W3213773670 cites W2008976923 @default.
• W3213773670 cites W2010154362 @default.
• W3213773670 cites W2010544255 @default.
• W3213773670 cites W2015226467 @default.
• W3213773670 cites W2017976235 @default.
• W3213773670 cites W2021949139 @default.
• W3213773670 cites W2024863878 @default.
• W3213773670 cites W2026207505 @default.
• W3213773670 cites W2029276637 @default.
• W3213773670 cites W2031531057 @default.
• W3213773670 cites W2037099081 @default.
• W3213773670 cites W2041718718 @default.
• W3213773670 cites W2048872829 @default.
• W3213773670 cites W2060683567 @default.
• W3213773670 cites W2060706280 @default.
• W3213773670 cites W2060768492 @default.
• W3213773670 cites W2062927038 @default.
• W3213773670 cites W2067413419 @default.
• W3213773670 cites W2067661300 @default.
• W3213773670 cites W2068527782 @default.
• W3213773670 cites W2076566162 @default.
• W3213773670 cites W2078689557 @default.
• W3213773670 cites W2079240477 @default.
• W3213773670 cites W2086583469 @default.
• W3213773670 cites W2086613968 @default.
• W3213773670 cites W2099800029 @default.
• W3213773670 cites W2103193636 @default.
• W3213773670 cites W2116215375 @default.
• W3213773670 cites W2121596339 @default.
• W3213773670 cites W2122295209 @default.
• W3213773670 cites W2131914340 @default.
• W3213773670 cites W2139551431 @default.
• W3213773670 cites W2140223027 @default.
• W3213773670 cites W2145624078 @default.
• W3213773670 cites W2146511959 @default.
• W3213773670 cites W2166681005 @default.
• W3213773670 cites W2239335096 @default.
• W3213773670 cites W2300257555 @default.
• W3213773670 cites W2318104397 @default.
• W3213773670 cites W2330691297 @default.
• W3213773670 cites W2336125544 @default.
• W3213773670 cites W2392209212 @default.
• W3213773670 cites W2512772252 @default.
• W3213773670 cites W2593546597 @default.
• W3213773670 cites W2609433094 @default.
• W3213773670 cites W2801782637 @default.
• W3213773670 cites W2890759032 @default.
• W3213773670 cites W2897707284 @default.
• W3213773670 cites W2911391578 @default.
• W3213773670 cites W2968871162 @default.
• W3213773670 cites W2972568455 @default.
• W3213773670 cites W3044141773 @default.
• W3213773670 cites W3108104645 @default.
• W3213773670 doi "https://doi.org/10.1016/j.quascirev.2021.107271" @default.
• W3213773670 hasPublicationYear "2021" @default.
• W3213773670 type Work @default.
• W3213773670 sameAs 3213773670 @default.
• W3213773670 citedByCount "3" @default.
• W3213773670 countsByYear W32137736702022 @default.
• W3213773670 countsByYear W32137736702023 @default.
• W3213773670 crossrefType "journal-article" @default.
• W3213773670 hasAuthorship W3213773670A5000571500 @default.
• W3213773670 hasAuthorship W3213773670A5001784726 @default.
• W3213773670 hasAuthorship W3213773670A5013299024 @default.
• W3213773670 hasAuthorship W3213773670A5027992695 @default.
• W3213773670 hasAuthorship W3213773670A5042537454 @default.
• W3213773670 hasAuthorship W3213773670A5052477206 @default.
• W3213773670 hasAuthorship W3213773670A5067690055 @default.
• W3213773670 hasAuthorship W3213773670A5091285519 @default.

• next