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Full-Text Articles in Life Sciences
Increased Dust Deposition In New Zealand Related To Twentieth Century Australian Land Use, Janice Brahney, Ashley P. Ballantyne, Marcus Vandergoes, Troy Baisden, Jason C. Neff
Increased Dust Deposition In New Zealand Related To Twentieth Century Australian Land Use, Janice Brahney, Ashley P. Ballantyne, Marcus Vandergoes, Troy Baisden, Jason C. Neff
Watershed Sciences Faculty Publications
Mineral aerosols (dust) generated in the dryland regions of Australia have the potential to reach New Zealand through atmospheric transport. Although a large portion of dust in New Zealand originates in Australia, little is known about how dust deposition has varied over time in New Zealand or what may have caused this variation. We used geochemical dust proxies to examine the recent history of dust deposition to two alpine lakes in Kahurangi National Park, South Island, New Zealand. Geochemical indicators suggest that dust deposition began to increase around 1900, with the greatest deposition rates occurring from ~1920 to ~1990. In …
Microbial Fe(Iii) Reduction As A Potential Iron Source From Holocene Sediments Beneath Larsen Ice Shelf, Jaewoo Jung, Kyu-Cheul Yoo, Brad E. Rosenheim, Tim M. Conway, Jae Il Lee, Ho Il Yoon, Chung Yeon Hwang, Kiho Yang, Christina Subt, Jinwook Kim
Microbial Fe(Iii) Reduction As A Potential Iron Source From Holocene Sediments Beneath Larsen Ice Shelf, Jaewoo Jung, Kyu-Cheul Yoo, Brad E. Rosenheim, Tim M. Conway, Jae Il Lee, Ho Il Yoon, Chung Yeon Hwang, Kiho Yang, Christina Subt, Jinwook Kim
Marine Science Faculty Publications
Recent recession of the Larsen Ice Shelf C has revealed microbial alterations of illite in marine sediments, a process typically thought to occur during low-grade metamorphism. In situ breakdown of illite provides a previously-unobserved pathway for the release of dissolved Fe2+ to porewaters, thus enhancing clay-rich Antarctic sub-ice shelf sediments as an important source of Fe to Fe-limited surface Southern Ocean waters during ice shelf retreat after the Last Glacial Maximum. When sediments are underneath the ice shelf, Fe2+ from microbial reductive dissolution of illite/Fe-oxides may be exported to the water column. However, the initiation of an oxygenated, …