419 resultados para Valais shrew


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Edited by Oliver W. B. Peabody; based on Singer's edition, "carefully compared" with the folio of 1623; with the life by Dr. Symmons, revised, and "New facts" by Collier. The first critical American edition. cf. Preface and J. Sherzer, American editions of Shakespeare (Modern lang. assoc. Publ., v. 22, pp. 658-659)

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1. Tempest. Two gentlemen of Verona. Merry wives of Windsor. Measure for measure. Comedy of errors.--2. Much ado about nothing. Love's labour's lost. Midsummer night's dream. Merchant of Venice. As you like it.--3. Taming of the shrew. All's well that ends well. Twelfth Night. Winter's tale.--4. King John. King Richard II. King Henry IV. King Henry V.--5. King Henry VI. King Richard III. King Henry VIII.--6. Troilus and Cressida. Coriolanus. Titus Andronicus. Romeo and Juliet.--7. Timon of Athens. Julius Caesar. Macbeth. Hamlet. King Lear.--8. Othello. Antony and Cleopatra. Cymbeline. Pericles.--9. Songs, sonnets, poems. Index to first lines.

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v. 1. Life, etc. The tempest. The two gentlemen of Verona. The merry wives of Windsor. Measure for measure.--v. 2. The comedy of errors. Much ado about nothing. Love's labour's lost. A midsummer night's dream. The merchant of Venice.--v. 3. As you like it. The taming of the shrew. All's well that ends well. Twelfth-night. The winter's tale.--v. 4. King John. King Richard II. King Henry IV. Pts. I-II. King Henry V.--v. 5. King Henry VI. Pts. I-III. King Richard III. King Henry VIII.--v. 6. Triolus and Cressida. Coriolanus. Titus Andronicus. Romeo and Juliet. Timon of Athens. Julius Caesar.--v. 7. Macbeth. Hamlet. King Lear. Othello. Antony and Cleopatra. Cymbeline.--v. 8. Pericles. The two noble kinsmen. Venus and Adonis. Lucrece. Sonnets. A lover's complaint. The passionate pilgrim. The phoenix and turtle.--v. 9. Glossary.

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"The text ... from MacBeth [v. 31] onwards has been edited by Mr. Walter Raleigh" note in v. 38.

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Added title-pages, engraved (with vignette) : The plays of William Shakspeare, illustrated with engravings by George B. Ellis, from the designs of R. Smirk, R. A.

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At head of title: The Dr. Johnson edition.

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In the Salgesch forest in the Canton of Valais in Switzerland, the understory has been removed to test whether effects on pine tree vitality. The data set published here compromises 120 time series of 60 soil temperature and 60 volumetric water content (VWC) sensors (EC-TM and 5-TM) (Decagon Devices, WA, USA) at three soil depth levels (5, 30, 60 cm) employed in the direct vicinity of six control trees and six trees with the undergrowth removed. At the levels 5 and 60 cm, three replications were made whereas 4 replications were made at level 30 cm. Six loggers recorded hourly data since 2010 with 18% gaps or 11% when not considering winter months December, January and February. The figure attached to this repository shows the average VWC and temperature of all measurements within the same depth and treatment specific setting aggregated in a defined time interval and period. In addition to that, the standard deviations are plotted as transparent polygons. In case of insufficient values for calculating standard deviations, the setting specific mean standard deviation of the considered time period are inserted.

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Abundant material of turtles from the early Oligocene site of Boutersem-TGV (Boutersem, Belgium), is presented here. No information on the turtles found there was so far available. All the turtle specimens presented here are attributable to a single freshwater taxon that is identified as a member of Geoemydidae, Cuvierichelys. It is the first representative of the ‘Palaeochelys s. l.–Mauremys’ group recognized in the Belgian Paleogene record. This material, which allows to know all the elements of both the carapace and the plastron of the taxon, cannot be attributed to the only species of the genus Cuvierichelys so far identified in the Oligocene, the Spanish form Cuvierichelys iberica. The taxon from Boutersem is recognized as Cuvierichelys parisiensis. Thus, both the paleobiogeographic and the biostratigraphic distributions of Cuvierichelys parisiensis are extended, its presence being confirmed for the first time outside the French Eocene record. The validity of some European forms is refuted, and several characters previously proposed as different between Cuvierichelys iberica and Cuvierichelys parisiensis are recognized as subjected to intraspecific variability.

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Fossil associations from the middle and upper Eocene (Bartonian and Priabonian) sedimentary succession of the Pamplona Basin are described. This succession was accumulated in the western part of the South Pyrenean peripheral foreland basin and extends from deep-marine turbiditic (Ezkaba Sandstone Formation) to deltaic (Pamplona Marl, Ardanatz Sandstone and Ilundain Marl formations) and marginal marine deposits (Gendulain Formation). The micropalaeontological content is high. It is dominated by foraminifera, and common ostracods and other microfossils are also present. The fossil ichnoasssemblages include at least 23 ichnogenera and 28 ichnospecies indicative of Nereites, Cruziana, Glossifungites and ?Scoyenia-Mermia ichnofacies. Body macrofossils of 78 taxa corresponding to macroforaminifera, sponges, corals, bryozoans, brachiopods, annelids, molluscs, arthropods, echinoderms and vertebrates have been identified. Both the number of ichnotaxa and of species (e. g. bryozoans, molluscs and condrichthyans) may be considerably higher. Body fossil assemblages are comparable to those from the Eocene of the Nord Pyrenean area (Basque Coast), and also to those from the Eocene of the west-central and eastern part of South Pyrenean area (Aragon and Catalonia). At the European scale, the molluscs assemblages seem endemic from the Pyrenean area, although several Tethyan (Italy and Alps) and Northern elements (Paris basin and Normandy) have been recorded. Palaeontological data of studied sedimentary units fit well with the shallowing process that throughout the middle and late Eocene occurs in the area, according to the sedimentological and stratigraphical data.

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[EN] European island shrews are either relicts of the endemic Pleistocene fauna, e.g., Crocidura zimmermanni, or were introduced from continental source populations. In order to clarify the taxonomic status and the origin of the two shrew species from the Canary Islands, a 981 bp fragment of cytochrome b gene was investigated in all European Crocidura species and compared with the Canary shrew (Crocidura canariensis) and the Osorio shrew (Crocidura osorio). The first shares its karyotype with the Sicilian shrew Crocidura sicula (2N = 36), the second with the Greater white-toothed shrew Crocidura russula (2N = 42), suggesting possible sister species relationships.