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Lateral Margins (lateral + margin)
Selected AbstractsDifferences of Hydrocarbon Enrichment between the Upper and the Lower Structural Layers in the Tazhong PaleoupliftACTA GEOLOGICA SINICA (ENGLISH EDITION), Issue 5 2010JIANG Zhenxue Abstract: The Tazhong paleouplift is divided into the upper and the lower structural layers, bounded by the unconformity surface at the top of the Ordovician carbonate rock. The reservoirs in the two layers from different parts vary in number, type and reserves, but the mechanism was rarely researched before. Therefore, an explanation of the mechanism will promote petroleum exploration in Tazhong paleouplift. After studying the evolution and reservoir distribution of the Tazhong paleouplift, it is concluded that the evolution in late Caledonian, late Hercynian and Himalayan periods resulted in the upper and the lower structural layers. It is also defined that in the upper structural layer, structural and stratigraphic overlap reservoirs are developed at the top and the upper part of the paleouplift, which are dominated by oil reservoirs, while for the lower structural layer, lithological reservoirs are developed in the lower part of the paleouplift, which are dominated by gas reservoirs, and more reserves are discovered in the lower structural layer than the upper. Through a comparative analysis of accumulation conditions of the upper and the lower structural layers, the mechanism of enrichment differences is clearly explained. The reservoir and seal conditions of the lower structural layer are better than those of the upper layer, which is the reason why more reservoirs have been found in the former. The differences in the carrier system types, trap types and charging periods between the upper and the lower structural layers lead to differences in the reservoir types and distribution. An accumulation model is established for the Tazhong paleouplift. For the upper structural layer, the structural reservoirs and the stratigraphic overlap reservoirs are formed at the upper part of the paleouplift, while for the lower structural layer, the weathering crust reservoirs are formed at the top, the reef-flat reservoirs are formed on the lateral margin, the karst and inside reservoirs are formed in the lower part of the paleouplift. [source] The braincase of the chondrichthyan Doliodus from the Lower Devonian Campbellton Formation of New Brunswick, CanadaACTA ZOOLOGICA, Issue 2009John Maisey Abstract The braincase of the late Lower Devonian (Emsian) chondrichthyan Doliodus is described for the first time. Its postorbital process is extended ventrally and probably enclosed part of the infraorbital sensory canal, as in some placoderms. Doliodus has a shark-like dentition, but its upper anterior tooth files were supported by the internasal cartilage of the braincase, not by the palatoquadrates. Modern selachian jaws and dentitions are not representative of primitive crown-group gnathostomes because they display a mixture of conserved and derived character states. Separation of the palatoquadrates by the internasal cartilage is probably a primitive condition for crown-group gnathostomes. Continuity of the upper dental arcade across the ethmoid region may represent a synapomorphy of chondrichthyans and some acanthodians (the condition is not found in placoderms or osteichthyans). Exclusion of the arcade from the ethmoid region is probably apomorphic within elasmobranchs. Doliodus has curious bar-like, paired subcranial ridges ending posteriorly at the hyomandibular articulation. These superficially resemble visceral arch infrapharyngohyals fused to the floor of the braincase, adding circumstantial palaeontological support to the old proposal that parts of visceral arches may be incorporated into the gnathostome braincase, although it seems more plausible that they formed in the lateral margins of the embryonic parachordal or hypotic lamina. [source] The apical ectodermal ridge in the pectoral fin of the Australian Lungfish (Neoceratodus forsteri): keeping the fin to limb transition in the foldACTA ZOOLOGICA, Issue 2009Verity S. Hodgkinson Abstract The apical ectodermal ridge (AER) in Neoceratodus develops after an initial period of mesenchymal proliferation and outgrowth of the fin bud and persists until chondrogenesis of the stylopod and zeugopod is initiated. At this time, the lateral margins of the AER convert to the fin fold leading to subsequent development of the dermal fin skeleton. Thorogood's (1991) fin fold model predicts that the AER should persist longer in Neoceratodus than it does in actinopterygians because of the comparatively extensive endochondral skeleton in lungfish. While the AER does persist into early chondrogenesis and is extended compared to actinopterygians (lost before fin radial chondrogenesis) it does not persist into further stages of chondrogenesis, providing partial support for Thorogood's model. Fgf8 appears in the lungfish fin epithelium during the initial period of fin outgrowth before a physical AER forms, when Fgf8 is restricted to the AER plus the preaxial and postaxial epithelium immediately adjacent to the AER. Fgf8 is no longer detected after the AER is replaced by a fin fold. Neoceratodus appears to provide a halfway point between ray fins and limbs during very early development as Thorogood proposed, but not precisely for the reasons his model suggests. [source] A new method of margin evaluation in breast conservation surgery using an adjustable mould during fixationHISTOPATHOLOGY, Issue 1 2001S Ichihara A new method of margin evaluation in breast conservation surgery using an adjustable mould during fixation Aims:,We have developed a new method of breast resection margin assessment in quadrantectomy using an adjustable mould to prevent the three-dimensional specimen from distorting during fixation. Methods and results:,The new method has been applied to 10 consecutive quadrantectomies (six invasive duct carcinomas, four duct carcinoma in situ with or without microinvasion). The precise configuration of the fixed specimen enabled pathologists to examine the side slices, the 5 mm thick slices cut parallel to the flat lateral margins of the specimen, permitting the separation of margin evaluation from tumour characterization. Eight cases with negative margins by our method would also be negative by assessment of inked margins since the margin widths were estimated to be from 5 to 30 mm (average 16.3 mm); two cases with positive margins would also be positive by inked margins. Conclusions:,Our new method was as reliable as the inked margins employing sequential slicing of the entire tissue, although it reduced the number of blocks by more than half in invasive carcinomas. A further advantage of this method is that the accuracy in margin evaluation is not influenced by the extent of tumour sampling. In addition, our system can pinpoint the positive margins facilitating re-excision to obtain tumour-free margins. [source] Evidence of a rheotactic component in the odour search behaviour of freshwater eelsJOURNAL OF FISH BIOLOGY, Issue 3 2003A. G. Carton The detection of food odour by the freshwater eels, Anguilla australis and Anguilla dieffenbachii released a behavioural response to flow that resulted in direct upstream movement toward the odour source. Changes in various orientation parameters were observed as eels neared the source. Eels had substantially lower swimming velocities and considerably more variable heading and course angles close to the odour source (,0·9 m) than further away (>0·9 m). Observed changes in orientation parameters were primarily due to changes in the behaviour of a searcher following odour loss. Cross-stream movements were initiated when the eel moved beyond the lateral margins of the odour plume. The behavioural switch from odour-conditioned rheotaxis to cross-stream casting following odour loss occurred more frequently close to the odour source where the plume was most narrow. Odour-conditioned rheotaxis enables the searcher to move quickly and efficiently toward the odour source without the need to extract directional information from a highly intermittent and complex chemical signal. [source] Circulating Angiotensin II Activates Neurones in Circumventricular Organs of the Lamina Terminalis That Project to the Bed Nucleus of the Stria TerminalisJOURNAL OF NEUROENDOCRINOLOGY, Issue 8 2003N. Sunn Abstract The aim of this study was to determine, in conscious rats, whether elevated concentrations of circulating angiotensin II activate neurones in both the subfornical organ and organum vasculosum of the lamina terminalis (OVLT) that project to the bed nucleus of the stria terminalis (BNST). The strategy employed was to colocalize retrogradely transported cholera toxin B subunit (CTB) from the BNST, with elevated levels of Fos protein in response to angiotensin II. Circulating angiotensin II concentrations were increased by either intravenous infusion of angiotensin II or subcutaneous injection of isoproterenol. Neurones exhibiting Fos in response to angiotensin II were present in the subfornical organ, predominantly in its central core but with some also seen in its peripheral aspect, the dorsal and lateral margins of the OVLT, the supraoptic nucleus and the parvo- and magnocellular divisions of the paraventricular nucleus. Fos-labelling was not apparent in control rats infused with isotonic saline intravenously or injected with either CTB or CTB conjugated to gold particles (CTB-gold) only. Of the neurones in the subfornical organ that were shown by retrograde labelling to project to BNST, approximately 50% expressed Fos in response to isoproterenol. This stimulus also increased Fos in 33% of neurones in the OVLT that project to BNST. Double-labelled neurones were concentrated in the central core of the subfornical organ and lateral margins of the OVLT in response to increased circulating angiotensin II resulting from isoproterenol treatment. These data support a role for circulating angiotensin II acting either directly or indirectly on neurones in subfornical organ and OVLT that project to the BNST and provide further evidence of functional regionalization within the subfornical organ and the OVLT. The function of these pathways is yet to be determined; however, a role in body fluid homeostasis is possible. [source] Geissleria gereckei sp. nov. (Bacillariophyta) from leaf-litter covered stones of very shaded carbonate mountain springs with extremely low dischargePHYCOLOGICAL RESEARCH, Issue 3 2009Marco Cantonati SUMMARY A new benthic freshwater diatom, Geissleria gereckei sp. nov., was identified from light and scanning electron micrographs. The most characteristic morphological features are the valve outline (elliptical, but with lateral margins that can range from slightly convex to slightly concave and also straight, and protracted, almost capitate ends), the size and length/width ratio, and the pattern of the striae around the central area. The new species was found to be epilithic, and characteristic of leaf-litter covered stones of very shaded carbonate mountain springs of the Italian Alps with extremely-low discharge (likely to be affected by seasonal desiccation). Very-low-discharge springs host a highly specialized diatom microflora, and are likely to increase in number in the near future due to the reduction of water, which is predicted to be caused by climate change in many regions. [source] Synaptic connections of cholinergic antennal lobe relay neurons innervating the lateral horn neuropile in the brain of Drosophila melanogasterTHE JOURNAL OF COMPARATIVE NEUROLOGY, Issue 3 2003Kouji Yasuyama Abstract Presumed cholinergic projection neurons (PNs) in the brain of the fruit fly Drosophila melanogaster, immunoreactive to choline acetyltransferase (ChAT), convey olfactory information between the primary sensory antennal lobe neuropile and the mushroom body calyces, and finally terminate in the lateral horn (LH) neuropile. The texture and synaptic connections of ChAT PNs in the LH and, comparatively, in the smaller mushroom body calyces were investigated by immuno light and electron microscopy. The ChAT PN fibers of the massive inner antennocerebral tract (iACT) extend into all portions of the LH, distributing in a nonrandom fashion. Immunoreactive boutons accumulate in the lateral margins of the LH, whereas the more proximal LH exhibits less intense immunolabeling. Boutons with divergent presynaptic sites, unlabeled as well as ChAT-immunoreactive, appear to be the preponderant mode of synaptic input throughout the LH. Synapses of ChAT-labeled fibers appear predominantly as divergent synaptic boutons (diameters 1,3 ,m), connected to unlabeled postsynaptic profiles, or alternatively as a minority of tiny postsynaptic spines (diameters 0.05,0.5 ,m) among unlabeled profiles. Together these spines encircle unidentified presynaptic boutons of interneurons which occupy large areas of the LH. Thus, synaptic circuits in the LH differ profoundly from those of the PNs in the mushroom body calyx, where ChAT spines have not been encountered. Synaptic contacts between LH ChAT elements were not observed. The synaptic LH neuropile may serve as an output area for terminals of the ChAT PNs, their presynaptic boutons providing input to noncholinergic relay neurons. The significance of the postsynaptic neurites of the ChAT PNs is discussed; either local or other interneurons might connect the ChAT PNs within the LH, or PNs might receive inputs arising from outside the LH. J. Comp. Neurol. 466:299,315, 2003. © 2003 Wiley-Liss, Inc. [source] Configuration and timing of Ungava Bay ice streams, Labrador,Ungava, CanadaBOREAS, Issue 1 2003KRISTER N. JANSSON The prominent Ungava Bay landform swarm (UBLS), covering an area of ,260000 km2 south of Ungava Bay, Canada, is defined by drumlins, crag-and-tails, horned crag-and-tails and flutes indicating convergent ice flow towards Ungava Bay. The UBLS has been difficult to interpret in terms of ice-sheet configuration, dynamics and age. Aerial photograph and satellite image interpretations of the Labrador-Ungava region reveal a previously unrecognized level of complexity within the UBLS consisting of several well-defined segments, most interpreted as representing discrete stream-flow events. Each of the segments is characterized by one or more of the criteria (convergent flow patterns at their heads, attenuated till lineations and abrupt lateral margins) previously suggested as diagnostic for formation by fast-flowing ice (ice streams). The UBLS reflects the most direct and probably fastest contact (in terms of sediment transport) between the Laurentide Ice Sheet interior and the ocean. It is therefore a prime candidate for abrupt changes in glacial-age northwest Atlantic seafloor sedimentation. [source] | ||||||||||||||||