Identification of polypeptides specific to rachis abscission zone cells of Sambucus nigra

Specific polypeptides and antigenic determinants in abscission zone cells of the leaf rachis of Sambucus nigra L. (elderberry) were identified. Extracts from abscission zone tissue (OZ) and from ethylene-treated abscission zone tissue after separation (Zone) were probed, using sodium dodecyl sulphate-polyacrylamide gel electrophoresis (SDS-PAGE) and immunological techniques, for unique peptide components absent from neighbouring non-zone mid-rachis tissue (MR). Ouchterlony immuno-diffusion revealed differences in the spectrum of antigenic determinants possessed by each tissue type when challenged with antiserum raised against OZ. Immuno-electrophoresis showed a basic polypeptide which is expressed preferentially in the abscission zone.
Immune-competition of OZ, MR and Zone extracts using immuno-affinity column chromatography has identified polypeptides of ca 34, ca 32, and ca 28 kDa which are (up to the limits of detection) abscission-cell specific. An antibody raised against the ca 34 kDa polypeptide recognises a peptide of ca 34 kDa present in OZ and Zone. This peptide is absent from MR.
These results suggest that the specific positional differentiation of ethylene-responsive target cells which constitute the leaf rachis abscission zone in S. nigra is accompanied by the expression of zone-cell-specific antigenic determinants which are not expressed by non-target neighbouring tissue.     

Fine structure and its functional properties of the endostyle of Ascidians,Ciona intestinalis

Summary For the purpose used in understanding thyroid phylogenesis, the fine structure and the iodine metabolism of the endostyle of Ascidians,Ciona intestinalis, was studied by electron microscopy and electron microscopic autoradiography. There are 8 kinds of zones in the endostyle.Zone 1, 3, and 5 cells, especially zone 1 cells, are characterized by numerous long cilia. These cells which show no indications of protein-secretion but numerous small vesicles and cytoplasmic filaments might play a role in catching and transporting food, absorption of liquid and supporting the endostylar construction.Zone 2, 4, and 6 cells are large and characterized by well developed rough endoplasmic reticulum and numerous electron-dense secretory granules which are considered to be synthesized in the rough endoplasmic reticulum and transported to the Golgi apparatus to mature. They, which are somewhat similar to the pancreatic exocrine cells in fine structure, are believed to secrete the proteinous or mucoproteinous substances which might be related to the digestion of food.Zone 7 and 8 cells which might be homologous to the thyroid cell of the higher vertebrate contains poorly developed rough endoplasmic reticulum, small Golgi apparatus, a few multivesicular bodies, a few lysosomes, and numerous small vesicles. In addition zone 8 cells bear cilia on their apical surface. The cytoplasmic characteristics of these cell types, especially of zone 8 cells, are fairly similar to those of type 2C and type 3 cells of the endostyle of a larval lamprey, though the rough endoplasmic reticulum is not so well developed. By electron microscopic autoradiography numerous silver grains were observed on the apical cell membrane region of zone 7 and 8 cells, especially of zone 8 cells, 1, 4, 6, 16 and 24 hours after immersion in sea water containing¹²⁵I. This fact suggests that the iodination takes place in the apical cell membrane region of these cells. The materials in the endostylar lumen is washed away during the fixation and dehydrating processes of the tissue. Therefore, the possibility of iodination of thyroglobulin-like substances taking place within the endostylar lumen cannot be ruled out. Grains were also found in the multivesicular bodies and lysosomes after 4, 6, 16 and 24 hours, especially 16 and 24 hours. It seems that the organic iodine might be reabsorbed into the cytoplasm of these cells.This investigation was supported by research grant from Dr. Henry C. Buswell Research Fellowship.On leave from Department of Anatomy, Hiroshima University, School of Medicine, as a Visiting Research Professor. The authors wish to express their hearty thanks to Dr. Oliver P. Jones for his valuable criticism.     

Fractionation of nuclei from brain by zonal centrifugation and a study of the ribonucleic acid polymerase activity in the various classes of nuclei

1. The nuclei of the cells of the whole rat brain have been fractionated in a B-XIV zonal rotor with a discontinuous gradient of sucrose. Five fractions were obtained. Zone (I) contained neuronal nuclei (70%) and astrocytic nuclei (23%). Zone (II) contained astrocytic nuclei (81%) and neuronal nuclei (15%). Zone (III) contained astrocytic nuclei (84%) and oligodendrocytic nuclei (15%). Zone (IV) contained oligodendrocytic nuclei (92%) and zone (V) contained only oligodendrocytic nuclei. 2. The content of DNA, RNA and protein per nucleus was determined for each zone. Although the amount of DNA per nucleus is constant (7pg) the RNA varies from 4.5 to 2.5pg/nucleus and the protein from 38 to 17.6pg/nucleus. The neuronal nuclei have the greatest amounts of protein. The oligodendrocytic nuclei have the least content of RNA and protein. 3. The effects of pH, ionic strength, and Mg(2+) and Mn(2+) concentration on the activity of the nuclear system for synthesis in vitro of RNA have been investigated for unfractionated nuclei. From these studies a standard set of conditions for the assay of nuclear RNA polymerase has been established. 4. The activity of the RNA polymerase in each of the zonal fractions has been determined in the presence and in the absence of alpha-amanitin. Zone (II) is the most active, followed by zone (I). The nuclei of zones (IV) and (V) have comparable activity, which is 40% of that of zone (II). 5. The extent of incorporation of each of the four labelled nucleoside triphosphates by the nuclei from each zone has been measured. These values have been used to calculate the base composition of the RNA synthesized in vitro in each class of nucleus. 6. The effect of changes in the condition of assay of RNA polymerase in the different classes of nuclei has been investigated. Significant differences in the response to concentrations of metal ions and ammonium sulphate have been observed. 7. Homopolymer formation in each zone of brain nuclei has been determined. The extent of formation of the four homopolymers roughly parallels the RNA polymerase activity.     

Health risk assessment in children living in an urban area with hydrofluorosis: San Luis Potosí Mexico case study

BackgroundFluoride is an inorganic element, which can be found in high concentrations in groundwater. Its consumption and exposure have consequences on human health. The objective of this study was to evaluate fluoride exposure and develop a health risk assessment in children from an urban area with hydrofluorosis in Mexico.MethodsWater fluoride levels in active wells were provided by the Water State Agency and divided into three zones: agriculture zone (Zone A), metallurgical zone (Zone B), and industrial zone (Zone C). Urinary fluoride levels were determined by potentiometric method using an ion-selective electrode. Health risk assessment was performed through Monte Carlo model analysis and hazard quotient was calculated.ResultsAccording to fluoride well concentration, all zones have high concentration especially Zone B (2.55 ± 0.98 mg/L). Urinary fluoride concentrations were highest in children in Zone B (1.42 ± 0.8 mg/L). The estimated median daily intake dose of fluoride was 0.084 mg/Kg-day for the children living in zone B. The highest mean HQ value was to Zone B (1.400 ± 0.980), followed by Zone C (0.626 ± 0.443).ConclusionThe levels of fluoride exposure registered are a potential risk to generate adverse health effects in children in the San Luis Potosi metropolitan area.     

Lymphocyte positions in the dome epithelium of the rabbit appendix

The apico-basal distribution of lymphocytes within the epithelium covering the domes of lymphatic tissue in the wall of the rabbit appendix was investigated in single and serial sections stained either for general histology, for cytoplasmic basophilia and acidophilia, or for nonspecific esterase activity. From the base to the summit of a dome, four zones numbered proximo-distally 1-4 were distinguished. Epithelial cells migrate from base to summit, as indicated by mitotic figures in zone 1, the gradual change from cytoplasmic basophilia to acidophilia in zones 2 to 4, and visible extrusion of cells from zone 4 at the summit. Zone 1 was free of lymphocytes. Most of the lymphocytes in zone 2 were intercellular and randomly arranged, but a few in this zone were within tapered epithelial cells modified by a process extending basally to the basement membrane. Small numbers of these tapered epithelial cells also occurred in zone 3. The large clusters of ten to 12 lymphocytes that characterized zone 3 were intercellular and impinged the apical regions of epithelial cells. Serial sections at the level of the distal cluster of zone 3 showed lymphocytes located also more basally, and some of these lymphocytes appeared to be passing through the basement membrane back into the lymphoid tissue of the dome. Epithelium of zone 4 over the distal surface of a dome was largely free of lymphocytes. Apparently most infiltrating lymphocytes form intercellular clusters and then return to the subepithelial lymphatic tissue.     

新疆准噶尔盆地西北缘洪古勒楞组时代的新认识

标准地点的洪古勒楞组长期以来一直被认为是准噶尔盆地西北缘,乃至整个新疆北部以海相为主的层位上最高的晚泥盆世晚期的沉积。然而牙形类和微体脊椎动物的研究证实,该组跨弗拉阶－法门阶（Ｆ－Ｆ）界线,它至少包括了一小部分弗拉晚期和主体部分为法门早期的沉积。两个牙形类带ＬａｔｅｒｈｅｎａｎａＺｏｎｅ和ＭｉｄｄｌｅｃｒｅｐｉｄａＺｏｎｅ被识别出,它们在Ｆ－Ｆ界线附近,并分别在大绝灭事件（在ｌｉｎｇｕｉｆｏｒｍｉｓＺｏｎｅ内）之前后。另一个层位更高的牙形类带ＬａｔｅｃｒｅｐｉｄａＺｏｎｅ也可能存在。同时还证实,长期以来一直被认为“正常层序”的标准地点的洪古勒楞组的层序是倒转的。由此,含植物大化石Ｌｅｐｔｏｐｈｌｏｅｕｍｒｈｏｂｉｃｕｍ等的陆相层在下（此层可能归于该组下伏的朱鲁木特组）,而产牙形类和其它丰富的无脊椎动物的海相层在上。按牙形类年代带的年代地层时间表（Ｆｏｒｄｈａｍ,１９９２）,该组距今约３６８－３６４百万年。至于它和邻近地区和布克河组的关系,由于后者发现了更高层位的牙形类,两者还不能完全对比。     

Neural stem cell lineages are regionally specified, but not committed, within distinct compartments of the developing brain.

Regional patterning in the developing mammalian brain is partially regulated by restricted gene expression patterns within the germinal zone, which is composed of stem cells and their progenitor cell progeny. Whether or not neural stem cells, which are considered at the top of the neural lineage hierarchy, are regionally specified remains unknown. Here we show that the cardinal properties of neural stem cells (self-renewal and multipotentiality) are conserved among embryonic cortex, ganglionic eminence and midbrain/hindbrain, but that these different stem cells express separate molecular markers of regional identity in vitro, even after passaging. Neural stem cell progeny derived from ganglionic eminence but not from other regions are specified to respond to local environmental cues to migrate ventrolaterally, when initially deposited on the germinal layer of ganglionic eminence in organotypic slice cultures. Cues exclusively from the ventral forebrain in a 5 day co-culture paradigm could induce both early onset and late onset marker gene expression of regional identity in neural stem cell colonies derived from both the dorsal and ventral forebrain as well as from the midbrain/hindbrain. Thus, neural stem cells and their progeny are regionally specified in the developing brain, but this regional identity can be altered by local inductive cues.     

Seed coat development, anatomy and scanning electron microscopy of Harpagophytum procumbens (Devil's Claw), Pedaliaceae

Seed coat development of Harpagophytum procumbens (Devil's Claw) and the possible role of the mature seed coat in seed dormancy were studied by light microscopy (LM), transmission electron microscopy (TEM) and environmental scanning electron microscopy (ESEM). Very young ovules of H. procumbens have a single thick integument consisting of densely packed thin-walled parenchyma cells that are uniform in shape and size. During later developmental stages the parenchyma cells differentiate into 4 different zones. Zone 1 is the multi-layered inner epidermis of the single integument that eventually develops into a tough impenetrable covering that tightly encloses the embryo. The inner epidermis is delineated on the inside by a few layers of collapsed remnant endosperm cell wall layers and on the outside by remnant cell wall layers of zone 2, also called the middle layer. Together with the inner epidermis these remnant cell wall layers from collapsed cells may contribute towards seed coat impermeability. Zone 2 underneath the inner epidermis consists of large thin-walled parenchyma cells. Zone 3 is the sub-epidermal layers underneath the outer epidermis referred to as a hypodermis and zone 4 is the single outer seed coat epidermal layer. Both zones 3 and 4 develop unusual secondary wall thickenings. The primary cell walls of the outer epidermis and hypodermis disintegrated during the final stages of seed maturation, leaving only a scaffold of these secondary cell wall thickenings. In the mature seed coat the outer fibrillar seed coat consists of the outer epidermis and hypodermis and separates easily to reveal the dense, smooth inner epidermis of the seed coat. Outer epidermal and hypodermal wall thickenings develop over primary pit fields and arise from the deposition of secondary cell wall material in the form of alternative electron dense and electron lucent layers. ESEM studies showed that the outer epidermal and hypodermal seed coat layers are exceptionally hygroscopic. At 100% relative humidity within the ESEM chamber, drops of water readily condense on the seed surface and react in various ways with the seed coat components, resulting in the swelling and expansion of the wall thickenings. The flexible fibrous outer seed coat epidermis and hypodermis may enhance soil seed contact and retention of water, while the inner seed coat epidermis maintains structural and perhaps chemical seed dormancy due to the possible presence of inhibitors.     

Biotic zonation on rocky shores of Heard Island

Summary The zonation of rocky shore biota on Heard Island is described for the first time, related to a universal zonation scheme and compared with that recorded for other sub-Antarctic localities. The Kelp Zone of holdfasts of the giant kelp, Durvillea antarctica (Chamisso) Hariot (one of the characteristic features of these regions) is confirmed as a sublittoral fringe. The occurrence of a Bare Zone within the littoral zone on sub-Antarctic shores is discussed. The possible roles of submersion, spray, freezing and predation by gulls in influencing the extent and composition of zones are discussed.     

Primary production of the periphyton in the littoral of the Danube

Summary The gross primary production of periphyton, grown on artificial substrata in the littoral of the Danube, was measured by the light and dark bottle method from April 1970 to March 1971. The periphyton used for the measurements was sampled from various depths, in order to cover the production of the whole littoral. In connection with this, the littoral area was divided into four zones limited by the heights 600 to 200 cm, according to the local water level gauge. The highest localized zone A (500–600 cm) was inundated only at maximum water levels for rather short period of time, the deepest zone D (200–300 cm) was permanently flooded.The zone A showed an average periphyton primary production of 22.5, the zone B of 54.8, the zone C of 28.9 and the zone D of 9.1 mg O₂/dm²/day. When recalculated to periods when the individual zones were inundated, the annual production was as follows: in zone A: 0.94, zone B: 9.20, zone C: 7.29 and zone D: 3.06g O₂/dm². The highest primary production was always found in the zone just below the water level. Exceptions occurred only when this zone was inundated for a short time as a result of a temporary rise of the water level and the periphyton was insufficiently developed.In order to compare the values of primary production of periphyton obtained from shallower rivers, where the whole bottom is well illuminated, or from rivers that do not exhibit such frequent and extensive level oscillations as the Danube, average value calculated from results obtained from the zone closest to the water level at the time of measurements, were always used. These results represent a special zone following the water level changes which is called surface zone. Primary periphytic production in the surface zone was 43.8 mg O₂/dm²/day. For the annual period it corresponds to the value of 14.74 g O₂/dm². Efficiently of gross photosynthesis in this zone was on the average 1.72%.The height of the water level and the water temperature were higly correlated with gross periphytic production. Close relationships between chlorophyll a concent, biomass and gross primary production of periphyton were found.

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Zusammenfassung Die Bruttoprimärproduktion des auf künstlichem Substrat im litoralen Bereich der Donau wachsenden Periphytons, wurde vom April 1970 bis zum März 1971, mit Hilfe der Hell-Dunkelflaschenmethode, gemessen. Das für die Messung herangezogene Periphyton wurde aus verschiedenen Tiefenzonen entnommen, um die Produktion der gesamten Uferzone festzuhalten. Im Zusammenhang damit wurde der litorale Bereich der Donau in 4 Zonen gegliedert, welche ihre Grenzen bei einem Pegelstand von 600–200 cm des Ortspegels hatten. Die höchste Zone A (500–600 cm) wurde nur bei den höchsten Wasserstanden und nur für kurze Zeit vom Wasser überflutet, die tiefste Zone D (200–300 cm) war dauernd unter Wasser.In der Zone A war die durchschnittliche Produktion des Periphytons 22,5 mg O₂/dm²/Tag, in Zone B 54,8 mg, in Zone C 28,9 mg und in Zone D 9.1 mg. Nach Berechnung für die Zeit, in der die einzelnen Zonen vom Wasser bedeckt waren war folgende Produktion in den einzelnen Zonen festzustellen: in Zone A 0,94 g O₂/dm², in Zone B 9,20 g, in Zone C 7,29 g und in Zone D 3,06 g. Die höchste Periphytonproduktion wurde jeweils in der Zone festgestellt, welche dem Wasserspiegel am nächsten war. Eine Ausnahme bildeten nur jene Fälle, in denen these Zone nach vorübergehender Erhöhung des Wasserspiegels erst kurze Zeit vom Wasser bedeckt war und das Periphyton ungenügend entwickelt war.Zum Vergleich mit den Werten der Primärproduktion des Aufwuchses aus seichteren Gewässern mit gut belichteter Sohle, oder aus Flüssen welche nicht so häufige und weitreichende Spiegelschwankungen aufweisen wie die Donau, wird in der vorgelegten Arbeit der Durchschnittswert aus den Ergebnissen der Zone verwendet, welche zur Zeit der Messungen dem Wasserspiegel am nächsten war. Diese Ergebnisse repräsentieren eine besondere Zone, welche den Schwankungen des Wasserspiegels folgt und von den Autoren durch den Begriff Oberflachenzone bezeichnet wird. Die Primärproduktion des Periphytons in dieser Oberflächenzone war 43,8 mg O₂/dm²/Tag. Dem entspricht im Jahresverlauf ein Wert von 14,74 g O₂/dm². Die Ausnützung der Sonnenenergie war in dieser Zone im Durchschnitt 1,72%.Von den Umweltfaktoren zeigt die Höhe des Wasserspiegels und die Wassertemperatur den engsten Zusammenhang mit der Höhe der Bruttoprimärproduktion des Periphytons. In kürzeren Zeitabschnitten, in denen es zu keinen raschen ausgeprägten Schwankungen des Wasserspiegels des Flusses kommt, wurde eine enge Abhängigkeit zwischen den Werten der Primärproduktion und dem a-Chlorophylgehalt und auch der Biomasse festgestellt.

     

The Furongian (upper Cambrian) Alum Shale of Scandinavia: revision of zonation

The zonation of the Furongian Alum Shale in Scandinavia, based on olenid trilobites, is reviewed and revised. The current scheme is rooted in a detailed zonation introduced in the late 1950s with subzones that subsequently have been elevated to zonal rank. Ten of these zones are difficult to recognize in all Alum Shale districts, and a revised zonation is proposed, focused on unambiguous identification throughout Scandinavia. The difficulties in recognizing zones in some districts mostly relate to biofacies differentiation. Representatives of Ctenopyge are, for instance, common in palaeo-offshore areas, whereas pelturines are rare in these settings and vice versa in palaeo-inboard settings. The following modifications of the olenid zonation are proposed: the Olenus scanicus Zone is renamed the O. scanicus–O. rotundatus Zone; the Ctenopyge similis and Ctenopyge spectabilis zones are replaced by the Sphaerophthalmus modestus–Sphaerophthalmus angustus Zone; the Ctenopyge tumida Zone is renamed the Peltura acutidens–Ctenopyge tumida Zone; the Peltura scarabaeoides Subzone is restored (as a zone) and replaces the Ctenopyge bisulcata and Ctenopyge linnarssoni zones. The Parabolina heres megalops (Sub)Zone is reinstated and replaces the Peltura paradoxa Zone; the Acerocarina granulata and P. costata zones are combined as the Acerocarina granulata–Peltura costata Zone. In addition, the name Proceratopyge nathorsti–Simulolenus alpha Zone is suggested for the polymerid zone corresponding to the upper Miaolingian Agnostus pisiformis Zone. The proposed changes reduce the number of Furongian Zones to 23, allocated to six superzones. No subzones are recognized, but some zones can potentially be subdivided for improved local correlation. The stratigraphical ranges of all Furongian olenid trilobites and agnostoids described from Scandinavia are summarized.     

Dissociation and reassembly of Limulus polyphemus hemocyanin.

Limulus polyphemus hemocyanin is a 3.3 x 10(6)-Mr protein containing 48 subunits in an assemblage of eight hexamers. The molecule can be dissociated into monomers and dimers at pH 8.9 in the presence of 0.01 M EDTA. These subunits are heterogeneous and can be separated into five zones (I--V) by DEAE-Sephadex chromatography. Reassembly experiments were carried out with varied subunit mixtures, based on different combinations of the five chromatographic zones, in order to study the structural role of the diverse subunits in the eight-hexamer molecule. The reassembly products were analysed by electron microscopy and ultracentrifugation. No structural role for zone I could be found. Zone V and possibly zone II are needed to form structures larger than hexamers. Absence of zone III causes irregular aggregation of hexamers. Zone IV and perhaps zone II are needed to make eight-hexamer molecules from four-hexamer molecules. From these results we conclude that there is a high degree of subunit specificity in the inter-subunit contacts in the native Limulus hemocyanin molecule.     

Fundamental biogeographic patterns across the Mexican Transition Zone: an evolutionary approach

Transition zones, located at the boundaries between biogeographic regions, represent events of biotic hybridization, promoted by historical and ecological changes. They deserve special attention, because they represent areas of intense biotic interaction. In its more general sense, the Mexican Transition Zone is a complex and varied area where Neotropical and Nearctic biotas overlap, from southwestern USA to Mexico and part of Central America, extending south to the Nicaraguan lowlands. In recent years, panbiogeographic analyses have led to restriction of the Mexican Transition Zone to the montane areas of Mexico and to recognize five smaller biotic components within it. A cladistic biogeographic analysis challenged the hypothesis that this transition zone is biogeographically divided along a north‐south axis at the Transmexican Volcanic Belt, as the two major clades found divided Mexico in an east‐west axis. This implies that early Tertiary geological events leading to the convergence of Neotropical and Nearctic elements may be younger (Miocene) than those that led to the east‐west pattern (Paleocene). The Mexican Transition Zone consists of five biogeographic provinces: Sierra Madre Occidental, Sierra Madre Oriental, Transmexican Volcanic Belt, Sierra Madre del Sur, and Chiapas. Within this transition zone, at least four cenocrons have been identified: Paleoamerican, Nearctic, Montane Mesoamerican, and Tropical Mesoamerican. Future studies should continue refining the identification of cenocrons and the reconstruction of a geobiotic scenario, as well as integrating ecological biogeographic studies, to allow a more complete understanding of the patterns and processes that have caused the biotic complexity of this transition zone.     

Observations on the biogeography of the Amotape-Huancabamba Zone in northern Peru

Some scientists have suggested that the Huancabamba Depression in northern Peru—i.e., the partial interruption of the Andean chain by the Rio Chamaya drainage system—represents a major biogeographical barrier to montane taxa. Others have suggested that the Amotape-Huancabamba Zone in the Andes of northern Peru and the extreme south of Ecuador is an area of particular biological diversity and possibly a phytogeographical zone in its own right. The phytogeography of this area is investigated here with data mainly from the Loasaceae, supplemented by data on other plant and animal groups and by some new data fromPassiflora L. (Passifloraceae) andRibes L. (Grossulariaceae). The Huancabamba Depression itself does not seem to have been a major dispersal barrier for these groups. However, a phytogeographical zone—the Amotape-Huancabamba Zone—between the Río Jubones system in Ecuador and the Río Chamaya system in Peru can be recognized from the available data. This zone seems to be home to numerous endemic species and species groups and has a high level of diversity (6–8 times as high as adjacent areas to the north and to the south in the groups studied). The species of this area show narrow endemicity and often strikingly aberrant morphological characters, compared with representatives of the same groups from other areas. The overlap between northern and southern groups in the area, the mosaic nature of its habitats (geology, geography, and climate), and a varied geological history (habitat fragmentation, secondary contact) seem to be the three most important factors contributing to these patterns of diversification. At least some phylogenetically old taxa appear to have survived in the Amotape-Huancabamba Zone. The region thus seems to be home to a high number of both neoendemics and paleoendemics.     

Early Cambrian biogeography in the North Atlantic region

A model of Early Cambrian trilobite biogeography in the North Atlantic region (Theokritoff 1979. Lethaia 12 , 281–295) is reviewed and modified in the light of new data. The presence of Wanneria in conglomerates bearing the Elliptocephala asaphoides fauna strengthens correlation of the E. asaphoides fauna as well as, by implication, the upper part of the Calluvia Zone with the middle part of the Bonnia-Olenellus Zone. The faunas of the Bastion Formation of East Greenland and of the Devil's Cove Limestone of northern Newfoundland are reinterpreted as shelf faunas. Additional occurrences of Archaeocyatha are noted in Spain and northwest Scotland but reports of Archaeocyatha in northern Norway and East Germany are not authenticated. Neither Salterella nor 'Volborthella' are now recognized as characteristic of any trilobite province. Although Ordovician acritarch provinces show congruence with trilobite provinces, available data on Early Cambrian plankton are not sufficient to support algal provincialism. Interpretation of the geological record suggests that the Early Cambrian lapetus Ocean was stratified with a well-mixed oxygenated zone overlying a phosphate-rich oxygen minimum zone and that the Elliptocephala asaphoides fauna should be reinterpreted as a warm-water fauna.     

Separation and analysis of the major forms of plasma fibronectin

Human plasma fibronectin exists in circulation in multiple molecular forms that are distinguishable by SDS-polyacrylamide gel electrophoresis (zone I, approx. 450 kDa dimers; zone II, 190-235 kDa; Zone III, 146-175 kDa). (Chen, A.B., Amrani, D.L. and Mosesson, M.W. (1977) Biochim. Biophys. Acta 493, 310-322). We report here on investigations of plasma fibronectin that had been purified from the 'heparin-precipitable fraction' of plasma by DEAE-cellulose chromatography using buffers containing a chaotropic salt (KSCN). Zone I fibronectin and zone II fibronectin were subsequently separated by Sepharose CL-6B chromatography in the presence of 0.3 M KSCN. Electrophoresis of reduced zone I fibronectin dimers showed the presence of three types of subunits (i.e., 220 kDa, 215 kDa, 207 kDa), evidently all having the same NH2-terminal sequence. Subunits of this size were also found in reduced zone II fibronectin, as well as another polypeptide of 190 kDa, the latter amounting to under 5% of the total. Unreduced zone I fibronectin was resolved by gel electrophoresis into a doublet. The upper component amounted to approx. 90% of the total and was comprised of 220 kDa and/or 215 kDa subunits; the lower component contained 207 kDa plus a 220 kDa or 215 kDa subunit. Scanning transmission electron microscopy indicated that under physiologic conditions zone II fibronectin molecules, like those in zone I, exist as pleiomorphic, loosely folded structures (approx. 16 X 8-12 nm) that are somewhat smaller than dimeric zone I molecules (approx. 24 X 16 nm). Circular dichroic spectral analyses suggests that both types have similarly folded local domains. Affinity chromatography experiments revealed a relative decrease in the binding of zone II fibronectin to gelatin but no difference from zone I fibronectin with respect to heparin or fibrin binding.     

下扬子区奥陶纪牙形刺多样性演变初探

根据前人和作者现有资料,对下扬子地区,特别是宁镇地区奥陶纪已经报道的牙形刺属种进行厘定,并按牙形刺带逐带进行多样性统计分析,初步编制出该地区奥陶纪牙形刺属种的地层延限表.研究表明;下扬子区牙形刺在奥陶纪的宏演化经历了3次较明显的辐射事件,分别发生在特马豆克期晚期-弗洛期早期(Serratognathus diversua带)、大坪期早期(Baltoniodus triangularis带)、达瑞威尔期晚期(Eoplacognathus suecicus带);此外,还经历了2次快速增长期,分别发生在达瑞威尔期早期(Lenodus antivariabilis带)、桑比期晚期至凯迪期早期(Hamarodus europaeus带),后者可能与局部环境变化有关.研究表明:华南海平面升降对下扬子区牙形刺宏演化趋势有重要影响.