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- Additional file 7: of Transcriptional profiling of human bronchial epithelial cell BEAS-2B exposed to diesel and biomass ultrafine particlesTable S4. Fold change of genes differentially expressed by the exposure to both diesel and biomass UFP. (XLS 67Â kb)
- FIG. 9 in Maerl-bed mapping and carbonate quantification on submerged terraces offshore the Cilento peninsula (Tyrrhenian Sea, Italy)FIG. 9. — Distribution of morpho-acoustic facies mapped in the areas investigated. The size of these areas are indicated in m2.
- (Table 4) Relative abundance of selected calcareous nannofossils species in sediment core UM94PC31geoscientificInformation
- CCDC 710224: Experimental Crystal Structure DeterminationAn entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
- CCDC 728554: Experimental Crystal Structure DeterminationRelated Article: R.D.Pergola, A.Sironi, C.Manassero, M.Manassero|2009|Eur.J.Inorg.Chem.||4618|doi:10.1002/ejic.200900580
- (Figure 4 and 5) Age and Calcium/Titanium ratio of sediment core DP30PCgeoscientificInformation
- (Table 1) 39Ar-40Ar age determinations for minerals from ODP Hole 210-1277geoscientificInformation
- Deuterium data from EPICA Dome C ice core EDC, 6.6-3140.5 metresgeoscientificInformation
- Linking catchment hydrology and ocean circulation in Late Holocene southernmost AfricaDue to the high sensitivity of southern Africa to climate change, a reliable understanding of its hydrological system is crucial. Recent studies of the regional climatic system have revealed a highly complex interplay of forcing factors on precipitation regimes. This includes the influence of the tropical easterlies, the strength of the southern hemispheric westerlies as well as sea surface temperatures along the coast of the subcontinent. However, very few marine records have been available in order to study the coupling of marine and atmospheric circulation systems. Here we present results from a marine sediment core, recovered in shallow waters off the Gouritz River mouth on the south coast of South Africa. Core GeoB18308-1 allows a closer view of the last ~ 4 kyr. Climate sensitive organic proxies, like the distribution and isotopic composition of plant-wax lipids as well as indicators for sea surface temperatures and soil input, give information on oceanographic and hydrologic changes during the recorded time period. Moreover, the micropaleontology, mineralogical and elemental composition of the sediments reflect the variability of the terrigenous input to the core site. The combination of down-core sediment signatures and a catchment-wide provenance study indicate that the Little Ice Age (~ 300-650 cal yr BP) was characterized by climatic conditions favorable to torrential flood events. The Medieval Climate Anomaly (~ 950-650 cal yr BP) is expressed by lower sea surface temperatures in the Mossel Bay area and humid conditions in the Gouritz River catchment. These new results suggest that the coincidence of humid conditions and cooler sea surface temperatures along the south coast of South Africa resulted from a strengthened and more southerly anticyclonic circulation. Most probably, the transport of moisture from the Indian Ocean by strong subtropical easterlies was coupled with Agulhas Bank upwelling pulses, which were initiated by an increase in Agulhas Current strength.
- McMurdo Sound dust Sr and Nd isotopic data
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