The influence of summer and winter stress and water relationships on the distribution of Quercus ilex L.

Several aspects of plant-water relationships and canopy behaviour have been studied over several years in two experimental areas of Quercus ilex L. forests in the northeastern Iberian Peninsula. Water requirements, water status limits necessary for a positive carbon budget and the functional canopy behaviour in the face of abiotic stress were evaluated, in order to determine which factors influence the geographical range of these forests.The results showed that holm oak has a conservative water use, a low cuticular transpiration, a high capacity for osmotic adjustement and xerophytic characteristics in leaf morphology and canopy arrangement. More than 440 mm of annual rainfall are required for these forests to persist. Summer drought and winter cold are thus important abiotic factors limiting the distribution of Quercus ilex. In both cases, drought stress is involved.     

Siberian species of the riihimakiensis-group in the genusChironomus (Diptera,Chironomidae). 1. Karyotypes and morphology

Karyotypes and morphology of three species with close relations toC. riihimakiensis Wülker 1971 are described from material of Tuva and Altai in Siberia. Only one of them could be reared to the male adult and was namedC. tuvanicus n.sp.     

On the precision and accuracy achieved by Escherichia coli cells at fission about their middle

Length and width of each of the prospective siblings of constricted Escherichia coli cells from different strains and culture conditions were measured from electron micrographs. The data were statistically analyzed to investigate how equally the length and volume of one cell was divided into two. The analysis showed that, for all cultures, bipartition is unbiased or very nearly so, i.e. sibling cells were on the average equally long and large. The precision of bipartition attained by the cells was usually high; it was related to the average cell shape (length/width): slender E. coli cells divided into two less precisely than squat cells. Absolute size, growth rate and strain specificity affected the precision of bipartition only indirectly, i.e. in as much as they influenced cell shape.     

The relationship between split-line orientation and in vivo bone strain in galago (G. crassicaudatus) and macaque (Macaca mulatta and M. fascicularis) Mandibles

There is still disagreement concerning the functional significance of split-line patterns in bone. This study was undertaken to reexamine the mechanical forces hypothesis for split-line formation by comparing split-line patterns with in vivo mandibular bone strain patterns. The relationship between split-line orientation and in vivo stress and strain patterns on macaque and galago mandibles was examined during jaw opening and the power stroke of mastication and incision. An attempt was made to relate split-line orientation to the direction of tensile stress and strain along the primate mandible. In addition, we also investigated the alternative possibility that split-line orientation is related to the direction of low stresses (and strains) on the primate mandible. The results of this study showed that there was no consistent relationship between split-line orientation and the principal strains or stresses. Thus, split-lines did not run consistently in the direction of high or low stress and strain. Therefore, we have concluded that split-line orientation provides little useful information for inferring patterns of stress and strain in bone.     

Δ1-11-oxa-11-deoxycortisol: A new antiglucocorticoid with activity in vivo

A new steroid-like compound, Δ¹-11-oxa-11-deoxycortisol, was tested in a one-week growth suppression, thymus suppression and adrenal weight suppression bioassay for possible glucocorticoid antagonist activity in $\text{vivo}$. We hypothesized that this compound would have antiglucocorticoid activity based on previous studies of 11-deoxycortisol and Δ^1,9(11)-11-deoxycortisol, which were optimal glucocorticoid antagonists $\text{in vivo}$ in adrenalectomized rats, but which lost antiglucocorticoid activity in intact animals, apparently due to adrenal 11β-hydroxylation. Thus, Δ¹-11-oxa-11-deoxycortisol, a compound which cannot undergo llβ-hydroxylation, was synthesized and tested as an antiglucocorticoid. This analog had an affinity for the rat thymus glucocorticoid receptor similar to that of its parent compounds (Ki 0.9-3.1×10^?7M). A dose of 1 $\text{mg}\text{rat}$ antagonized the effect of 15μg of dexamethasone in the growth suppression assay (p<0.05) and in the thymus suppression assay (p<0.06), but did not antagonize dexamethasone-induced adrenal weight suppression. Δ¹-11-oxa-11-deoxycortisol did not exhibit glucocorticoid activity in any of the three assays. These data suggest that Δ¹-11-oxa-11-deoxycortisol may be a pure competitive antagonist of dexamethasone.     

Description of Meloidogyne nataliei n. sp. (Nematoda: Meloidogynidae) from Grape (Vitis labrusca) in Michigan,with SEM Observations

Meloidogyne nataliei n. sp. is described and illustrated from grape (Vitis labrusca) in a declining vineyard at Mattawan, Michigan, USA. Infected grape roots exhibit no hyperplastic symptoms. Females protrude from the roots and are surrounded by a massive egg sac containing many eggs. This new species is distinguishable from other species of the genus especially by its large, striking perineal pattern with, usually, two ropelike separated striae on each side extending laterally from the vulval and anal areas. Among other diagnostic characters are the location of the female excretory pore adjacent to or near the base of the head and the heavy larval stylet averaging about 22 μm in length. Examination of males, females, and larvae with the scanning electron microscope confirmed observations made by optical microscopy and revealed diagnostic and other structures in greater detail. Of particular significance was the nature of the male head, with a massive circular labial disc on which is located a rectangular structure surrounding the oral opening, and the six distinct lips appearing as a rosette in en face view. The known distribution of this new species is presently limited to its original location in Michigan.     

Description and SEM Observations of Meloidogyne chitwoodi n. sp. (Meloidogynidae), a Root-knot Nematode on Potato in the Pacific Northwest

Meloidogyne chitwoodi n. sp. is described and illustrated from potato (Solanum tuberosum) originally collected from Quincy, Washington, USA. This new species resembles M. hapla, but its perineal pattern is basically round to oval with distinctive and broken, curled, or twisted striae around and above the anal area. The vulva is in a sunken area devoid of striae. Vesicles or vesicle-like structures are present in the median bulb of females. The larva tail, being short and blunt with a hyaline tail terminal having little or no taper to its rounded terminus, is distinctively different from M. hapla. SEM observations revealed the nature of the perineal pattern and details of the head of larvae and males, and showed the spicules to have dentate tips ventrally. Hosts for M. chitwoodi n. sp. include potato, tomato, corn, and wheat but not strawberry, pepper, or peanut. The latter three crops are excellent hosts for M. hapla. The known distribntion of this new root-knot species presently involves certain areas of Idaho, Washington, and Oregon. The common name "Columbia root-knot nematode" is proposed for M. chitwoodi n. sp.     

Rhyncholites and conchorhynchs as calcified jaw elements in some late Cretaceous ammonites

Conspicuous calcareous coverings are present in the anterior region of 17 fossil jaws from late Cretaceous rocks of Hokkaido (Japan) and Sakhalin (U.S.S.R.). The jaws were preserved in calcareous nodules either in situ in body chambers of ammonites or in close association with identifiable ammonite conch remains. From the morphologic similarity between in situ and isolated jaws, they may be attributed to Tetragonites glabrus, Gaudryceras tenuiliratum, G. denseplicatum, G. sp., and Neophylloceras subramosum. The jaw apparatus of these species is composed of two three-dimensional black walls of carbonate apatite, which might be a diagenetic replacement of chitinous material. The calcareous coverings in both upper and lower jaws closely resemble those of upper (rhyncholite) and lower (conchorhynch) jaws of modern Nautilus as well as rhyncholite and conchorhynch fossils in their gross morphology, microstructure, and chemical composition. Calcified remains of cephalopod jaws known as rhyncholites and conchorhynchs have been reported from late Paleozoic to Recent. The present discovery of ammonoid rhyncholites and conchorhynchs suggests that at least some previously known late Paleozoic and Mesozoic counterparts belong to the Ammonoidea. The essential similarity of jaw elements of some Late Cretaceous ammonites and modern Nautilus gives reliable information on the feeding habits of the former. The sharp and thick ammonoid rhyncholites and conchorhynchs may have had a special function for cutting up food, similar to those of Nautilus.     

An integumental anatomy for the butterfly Glaucopsyche lygdamus (Lepidoptera:Lycaenidae):a morphological terminology and homology

An integumental anatomy for the lycaenid butterfly Glaucopsyche lygdamus is presented. Comparisons with other lepidopteran taxa are made to rectify the homology of parts and contrast anatomical divergences within the Lycaenidae. A general terminology based on Snodgrass is given, to replace many of the specialized and often synonymous terms restricted to the Lepidoptera. Many common anatomical svnonyms are also given. Several reinterpretations of the anatomy and homology of various integumental regions are discussed. A previously unreported cuticular anomaly on abdominal tergum 2 of male Polyommatinae (Downey's area) is described. The following new or newly combined terms are used:postgenal-occipital area, postgenal-occipital protuberance, dorsal temporal sulci, postantennal projections, pronotal projection, infraepisternal-basisternal plate, paracoxal-marginopleural sulci, dorsal epimeral sulci, ventral epimeral sulci, secondary coxal sulci, ventral subcostal-radial process, lateral secondary sclerite and Downey's area.