Natural parthenogenesis,larval and juvenile development,and geographical distribution of the coral reef asteroid Ophidiaster granifer

Ophidiaster granifer Lütken is a small cryptic coral reef asteroid found in the Indo-West Pacific. Its mode of reproduction, shown by aquarium observations and gonad histology, is parthenogenetic. This is the first confirmation of natural parthenogenesis in the phylum Echinodermata, despite many studies showing artificial parthenogenesis in echinoderms. Populations of O. granifer from Micronesia, New Guinea and the Great Barrier Reef consisted only of females: no testes or spermatogenesis were found in any individual at any stage of gonad development of ca 400 individuals. Regular year-round population censuses at Guam, Micronesia, revealed a distinct 0-year class which grew to sexual maturity in two years. There was an annual reproductive cycle with apparently-synchronous spawning in early winter. The large eggs, ca 0.6 mm diameter, develop into lecithotrophic larvae. Some larvae are planktonic, while some remain attached under the rocks. The latter develop through metamorphosis in situ. Parthenogenetic reproduction leading to both stationary and dispersed larvae may be related to the low fecundity and low population densities of this small asteroid.     

Characterizing kinetics of transport and transformation of selenium in water-sediment microcosm free from selenium contamination using a simple mathematical model

This study developed a seven-compartment model for predicting the fate of selenium (Se) in an aquatic environment containing a water-sediment boundary. Speciation of Se in water-sediment microcosms under microaerobic conditions was measured to evaluate first-order kinetics of Se transportation and transformation. The microcosm consisted of a 10-ml solution containing 1mM soluble Se as selenate (Se6+) or selenite (Se4+) and 8 g wet sediment that was free from Se contamination, sampled from the Senri, Yamato, or Yodo Rivers in Osaka, Japan. Stepwise reaction coefficients describing transportation and transformation were determined using an inverse method on this model which includes: selenate (Se(W)6+) and selenite (Se(W)4+) in ponded water; selenate (Se(S)6+) and selenite (Se(S)4+), elemental Se (Se0), organic Se (Se2-) in sediment; and gaseous Se (DMSe). During this 1-month experiment, soluble Se was transported from ponded water to the sediment and Se was transformed sequentially to other Se species through biochemical reactions. Experimental and kinetic analyses indicated quantitatively that the Yamato River microcosm, with its high organic matter content, had a high adsorption rate of soluble Se. The Yodo River microcosm had a low adsorption rate for Se6+ and a low Se reduction rate. The Senri River microcosm had an apparent high volatilization rate of DMSe. The model developed in this study is extremely useful for predicting fate of Se in aquatic environment in the field.     

Shell structure and behaviour related to cementation in oysters

Shell microstructure and mantle behaviour relating to shell cementation was studied on adult oysters,Crassostrea gigas, Saccostrea mordax, andS. kegaki (collected from Shirahama, Wakayama Prefecture, Japan, in 1989 and 1990). At the place of cementation, the prismatic structure of the outermost shell layer is modified to a significant structure. This structure, named the ridge-and-furrow structure, consists of calcified ridges a few microns wide separated by furrows, both arranged parallel to the shell growth direction. The furrows are ultimately filled by shell material. The prismatic and ridge-and-furrow structures gradually merge in a transitional area where an intermediate type of the two structures occurs. The small size of the crystal units of the ridges and furrows is due to the close distribution of crystal seeds, especially close to pre-existing ridges. This is the basis of the difference between the ridge-and-furrow and the prismatic structures and also makes the former structure functional for cementation, in contrast to the latter. At the site of ongoing shell cementation, the mantle margin adpresses the shell margin onto the substrate. Experiments show that this pressing action is essential for cementation and probably also for the formation of the ridge-and-furrow structure. Even the right valve, which oysters nerve use to cement in natural conditions, forms the ridge-and-furrow structure and cements to the substrate if the pressing action of its mantle margin is induced under artificial conditions. Behavioural changes probably led oysters to switch from byssal attachment to cementation within a short time span when they acquired their cementing habit.     

Purification and immunolocalization of a vitellin-like protein from the Pacific oyster Crassostrea gigas

A female-specific protein from the hemolymph, and a related ovarian protein were identified in the Pacific oyster Crassostrea gigas using immunological procedures. The latter protein was isolated from ovarian extract by a combination of precipitation in distilled water, ammonium sulfate fractionation, hydroxylapatite chromatography and gel filtration on a Sepharose 6B column, and was identified as a macromolecular glycolipoprotein of 500 kD; sodium dodecylsulfate polyacrylamide gel electrophoresis, under reducing conditions, revealed seven heterogeneous polypeptides. Using a specific antiserum against purified protein, we also examined the immunohistochemical distribution of the protein at light- and electron-microscopic levels. Light microscopy revealed its presence in the oocytes, and electron microscopy identified it in yolk granules and the vitelline coat of the oocytes. These results indicate that the purified protein is a vitellin-like protein. Since no organ other than the ovary reacted with the antiserum, it is probable that the protein is produced inside the ovary, probably autosynthetically by oocytes.     

Using remote sensing and GIS to detect and monitor land use and land cover change in Dhaka Metropolitan of Bangladesh during 1960–2005

This paper illustrates the result of land use/cover change in Dhaka Metropolitan of Bangladesh using topographic maps and multi-temporal remotely sensed data from 1960 to 2005. The Maximum likelihood supervised classification technique was used to extract information from satellite data, and post-classification change detection method was employed to detect and monitor land use/cover change. Derived land use/cover maps were further validated by using high resolution images such as SPOT, IRS, IKONOS and field data. The overall accuracy of land cover change maps, generated from Landsat and IRS-1D data, ranged from 85% to 90%. The analysis indicated that the urban expansion of Dhaka Metropolitan resulted in the considerable reduction of wetlands, cultivated land, vegetation and water bodies. The maps showed that between 1960 and 2005 built-up areas increased approximately 15,924 ha, while agricultural land decreased 7,614 ha, vegetation decreased 2,336 ha, wetland/lowland decreased 6,385 ha, and water bodies decreased about 864 ha. The amount of urban land increased from 11% (in 1960) to 344% in 2005. Similarly, the growth of landfill/bare soils category was about 256% in the same period. Much of the city's rapid growth in population has been accommodated in informal settlements with little attempt being made to limit the risk of environmental impairments. The study quantified the patterns of land use/cover change for the last 45 years for Dhaka Metropolitan that forms valuable resources for urban planners and decision makers to devise sustainable land use and environmental planning.     

Community-scale analysis of the farmland abandonment occurrence process in the mountain region of Ladakh,India

Farmland abandonment has been a significant issue in mountain regions. Thus, many studies have attempted to uncover its driving factors. Most existing studies take a large- or meso-scale view of mountain regions, and there are a few studies that provide community-level analysis. Therefore, it is unclear how ecological and sociopolitical factors are actually combined to influence farmland abandonment at a community level. Thus, we conducted a field survey in the mountain village of Ladakh, northern India, beginning in 2009 and tried to understand the farmland abandonment occurrence process from the viewpoint of traditional altitudinal models of land use. Using data collected during the survey, a relationship between altitude and farmland abandonment was established. However, this relationship was complex, combining traditional forms of land use system in the village. The altitudinal model of land use was very common in mountain regions; thus, discussions of current land use issues should be based on an understanding of such traditional altitudinal systems.