Effects of Point Pattern Shape on Home-Range Estimates

Abstract: Home-range estimators are commonly tested with simulated animal locational data in the laboratory before the estimators are used in practice. Although kernel density estimation (KDE) has performed well as a home-range estimator for simulated data, several recent studies have reported its poor performance when used with data collected in the field. This difference may be because KDE and other home-range estimators are generally tested with simulated point locations that follow known statistical distributions, such as bivariate normal mixtures, which may not represent well the space-use patterns of all wildlife species. We used simulated animal locational data of 5 point pattern shapes that represent a range of wildlife utilization distributions to test 4 methods of home-range estimation: 1) KDE with reference bandwidths, 2) KDE with least-squares cross-validation, 3) KDE with plug-in bandwidths, and 4) minimum convex polygon (MCP). For the point patterns we simulated, MCP tended to produce more accurate area estimates than KDE methods. However, MCP estimates were markedly unstable, with bias varying widely with both sample size and point pattern shape. The KDE methods performed best for concave distributions, which are similar to bivariate normal mixtures, but still overestimated home ranges by about 40–50% even in the best cases. For convex, linear, perforated, and disjoint point patterns, KDE methods overestimated home-range sizes by 50–300%, depending on sample size and method of bandwidth selection. These results indicate that KDE does not produce home-range estimates that are as accurate as the literature suggests, and we recommend exploring other techniques of home-range estimation.     

Palaeohistology of the bones of pterosaurs (Reptilia: Archosauria): anatomy, ontogeny, and biomechanical implications

Thin sections from long bones of specimens representing pterosaurs ranging from the Early Jurassic to the latest Cretaceous provide a profile of bone histology across a range of sizes, skeletal elements, growth stages, and phylogenetic positions. Most pterosaur bone is fibro-lamellar, organized in an unusual way that suggests high growth rates through ontogeny. Fibro-lamellar deposits are finished by a relatively abrupt deceleration or cessation of growth represented by lamellar, poorly vascularized subperiosteal bone in what appear to be adults. Pterosaurs had the thinnest bone walls of any tetrapods; they complemented high rates of periosteal deposition with almost equally high rates of endosteal erosion. Pterosaurs show a great variety of histologic features that include articular calcified cartilage, sub-chondral bone plates, trabecular bone struts and related internal supports, and secondary deposition and remodeling of bone. They remodeled their bones internally by (1) depositing endosteal bone coatings on the inner cortex and over struts of pre-existing internal bone, (2) secondarily filling bone spaces, and (3) Haversian reworking. The construction of these struts reflects both developmental patterns of bone construction and biomechanical function. Alternating plywood-like layers of bone, heretofore undescribed in tetrapods, provided strength, as did the obliquely oriented system of reticular blood vessels in the bones. The distribution and ontogenetic features of pterosaur bone tissues, when combined with other evidence, suggest generally high growth rates, high metabolic levels, altricial birth, and extended parental care.     

Pollen Dimorphism--Origin and Significance in Pollen Plant Formation by Anther Culture

Pollen dimorphism during the ripening of Nicotiana tabacum antherstakes the form of differentiation at the binucleate pollen stageinto normal (N) grains, characterized by their high frequency,larger size, densely–staining cytoplasm and high starchcontent and into smaller (S) grains characterized by their variableand low frequency and weakly–staining cytoplasm. Mostof the S grains show distinctive vegetative and generative nuclei(A grains); a small number have two vegetative–type nuclei(B grains). Evidence is presented that when excised anthersare cultured, pollen plants arise only from S grains. It issuggested that the differentiation into N and S grains arisesby an abnormal second meiotic division in the pollen mothercells. Nicotiana tabacum, tobacco, pollen dimorphism, anther culture     

Effect of Water Activity on Heat Survival of Staphylococcus aureus, Salmonella typhimurium and Salm. senftenberg

The viability of Staphylococcus aureus heated at 55° in phosphate buffer was determined on recovery media of different water activity ( a_w ) levels. The basal recovery medium, tryptone–soya agar ( a_w 0.997) was adjusted to lower a_w levels by the addition of NaCl, glycerol or sucrose. Maximum survival occurred at a_w 0.997. Viability was reduced to 1/10 of the maximum at a_w 0.98 when a_w , was controlled by sucrose or NaCl but not until a_w 0.93 with glycerol. To eliminate effects such as incomplete mixing or post-heating dilution and in order to use conditions comparable to those occurring in foods, a solid medium heating/recovery method was also used. This involved heating, by immersion, of surface-inoculated agar plates and recovery of survivors in situ . Heat resistance studies could thus only be carried out at a_w levels permitting growth on the heating/recovery medium. Staphylococcus aureus, Salmonella typhimurium and Salm. senftenberg 775W were heated at 55° and recovered in situ on tryptone-soya agar adjusted to lower a_w levels as above. Maximum survival of Staph. aureus occurred at a higher a_w with glycerol ( a_w 0.965) than with NaCl (0.92) or sucrose (0.90). The maximum survival of both Salm. typhimurium and Staph. aureus heated at 55° occurred at the same a_w (0.965) with glycerol. This maximum was not affected by the duration of heating. As a contrast, heat resistance of Salm. senftenberg 775W was virtually unaffected by reduction in the a_w of the heating/recovery medium.     

Calcium Oxalate Raphide Crystals and Crystalliferous Idioblasts in the Carpels of Ornithogalum caudatum

Crystalliferous idioblasts commonly are found in groups of twoor three cells in the peripheral region of the carpels Crystals,composed of calcium oxalate, usually are m well-organized bundleswhich develop within a matrix of protein and carbohydrate inthe vacuole of each idioblast The matrix occurs around and betweenindividual crystal chambers and contains spheres and tubules5.4 nm in diameter The matrix changes in character and locationwith age Crystals form within their own individual chambers,each comprised of a series of lamellae The number of lamellaeis variable The innermost lamella is different from the othersin that it is apparently continuous The other lamellae are platelikeand superficially resemble successive periderms. The lamellaemay begin and/or terminate abruptly or they may anastamose Eachlamella is composed of chains of spheres about 6 1 nm in diameterand is separated from adjacent lamellae by tubules 5.4 nm indiameter Both the crystals and slime body are absorbed duringlater stages of carpel maturation. Ornithogalum caudatum Ait carpel, calcium oxalate, idioblasts, ultrastructure