Fuli Wu

Abstract Windblown mineral dust is a nutrient source to the ocean, influencing global ocean productivity, ocean carbon uptake and climate. In this Review, we examine how dust emission fluxes, sources and compositions have changed over the past 7 Myr and consider the implications for ocean productivity.

Abstract Reorganization of the Asian climate from one dominated by global planetary wind systems to a regional monsoon climate is closely related to the surface uplift of the Tibetan Plateau (TP). However, evaluating this climatic reorganization is limited by difficulty in constraining the complex, multistaged uplift of the TP and contradictory evidence regarding Asian Monsoon onset.

Although there are few reports about H S-negative Salmonella, the incidence of H S-negative strains is on the rise lately. To the best of our knowledge, 100 H S-negative Salmonella isolates of 13 serovars have been reported [6–12]. Moreover, 17 H S-negative S. Senftenberg isolates, 19 H S-negative S. Choleraesuis isolates, and seven H S-negative S. Aberdeen isolates were reported in our previous studies [13–15].