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Rapeseed cultivars exhibit a wide range of oil content in the mature seeds. Little is known about the relationship between the oilbody structures and the differences in oil contents of Brassica napus cultivars. In the present study, the oilbody morphology and its fate during the embryo development and seedling growth in several cultivars with oil contents ranging from 33.4 to 49.8% were studied. Cultivars with low oil contents (LO), some of the oilbodies were in similar size to those in cultivars with high oil content (HO), while some oilbodies in the LO cultivars were several times bigger (over 5.0 microm). These are much larger than the average size of B. napus seed oilbodies that were previously reported (Mantese et al. Ann Bot 97:999-1010, 2006). The oleosin protein levels and oleosin1 gene transcript abundances in the HO cultivars were clearly higher than in the LO cultivars. The shapes of oilbodies were similar during early stages of embryo development in both HO and LO cultivars, while as the embryos matured, the unusually large oilbodies were generated in the LO cells. After germination, the oilbodies in LO cultivars were consumed more slowly than in HO, and the seed germination rates of LO cultivars were less than those of HO cultivars. The low accumulation of oleosins results in the forming of unusually large oilbodies in LO cultivars.

Abstract. The 1951The -2009 drought history of China is reconstructed using daily soil moisture values generated by the Variable Infiltration Capacity (VIC) land surface macroscale hydrology model. VIC is applied over a grid of 10 458 points with a spatial resolution of 30 km × 30 km, and is driven by observed daily maximum and minimum air temperature and precipitation from 624 long-term meteorological stations. The VIC soil moisture is used to calculate the Soil Moisture Anomaly Percentage Index (SMAPI), which can be used as a measure of the severity of agricultural drought on a global basis. We have developed a SMAPI-based drought identification procedure for practical uses in the identification of both grid point and regional drought events. As a result, a total of 325 regional drought events varying in time and strength are identified from China's nine drought study regions. These drought events can thus be assessed quantitatively at different spatial and temporal scales. The result shows that the severe drought events of 1978, 2000 and 2006 are well reconstructed, which indicates that the SMAPI is capable of identifying the onset of a drought event, its progression, as well as its termination. Spatial and temporal variations of droughts in China's nine drought study regions are studied. Our result shows that on average, up to 30 % of the total area of China is prone to drought. Regionally, an upward trend in drought-affected areas has been detected in three regions (Inner Mongolia, Northeast and North) from 1951-2009. However, the decadal variability of droughts has been weak in the rest of the five regions (South, Southwest, Correspondence to: Z. Y. Wu (wzyhhu@gmail.com) East, Northwest, and Tibet). Xinjiang has even been showing steadily wetter since the 1950s. Two regional dry centres are discovered in China as the result of a combined analysis on the occurrence of drought events from both grid points and drought study regions. The first centre is located in the area partially covered by the North and the Northwest, which extends to the southeastern portion of Inner Mongolia and the southwest part of Northeast. The second one is found on the central to southern portion of the South. Our study demonstrates the applicability and the value of using modeled soil moisture for reconstructing drought histories, and the SMAPI is useful for analyzing drought at different spatial and temporal scales.