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141.
Sten M Walther Mats J Johansson Torun Flateb? Anne Nicolaysen Gunnar Nicolaysen 《Journal of applied physiology》2005,99(3):909-914
The classic four-zone model of lung blood flow distribution has been questioned. We asked whether the effect of positive end-expiratory pressure (PEEP) is different between the prone and supine position for lung tissue in the same zonal condition. Anesthetized and mechanically ventilated prone (n = 6) and supine (n = 5) sheep were studied at 0, 10, and 20 cm H2O PEEP. Perfusion was measured with intravenous infusion of radiolabeled 15-microm microspheres. The right lung was dried at total lung capacity and diced into pieces (approximately 1.5 cm3), keeping track of the spatial location of each piece. Radioactivity per unit weight was determined and normalized to the mean value for each condition and animal. In the supine posture, perfusion to nondependent lung regions decreased with little relative perfusion in nondependent horizontal lung planes at 10 and 20 cm H2O PEEP. In the prone position, the effect of PEEP was markedly different with substantial perfusion remaining in nondependent lung regions and even increasing in these regions with 20 cm H2O PEEP. Vertical blood flow gradients in zone II lung were large in supine, but surprisingly absent in prone, animals. Isogravitational perfusion heterogeneity was smaller in prone than in supine animals at all PEEP levels. Redistribution of pulmonary perfusion by PEEP ventilation in supine was largely as predicted by the zonal model in marked contrast to the findings in prone. The differences between postures in blood flow distribution within zone II strongly indicate that factors in addition to pulmonary arterial, venous, and alveolar pressure play important roles in determining perfusion distribution in the in situ lung. We suggest that regional variation in lung volume through the effect on vascular resistance is one such factor and that chest wall conformation and thoracic contents determine regional lung volume. 相似文献
142.
Summary Incubation for Ca++-activated myosin ATPase reveals three types of muscle fibres in m. parietalis of the Atlantic hagfish (Myxine glutinosa), while m. craniovelaris and m. longitudinalis linguae both contain one type of muscle fibres.The fast twitch white fibres of m. longitudinalis linguae and m. parietalis show relatively high ATPase activity, while the intermediate fibres of m. parietalis show low activity. Despite of being slow non-twitch, the superficial red fibres of m. parietalis and the fibres of m. craniovelaris show an ATPase activity even higher than that of the fast twitch muscle fibres. 相似文献
143.
The localization, isolation and partial characterization of a collagenolytic enzyme from the land planarian Bipalium kewense is described. This enzyme can be obtained by direct extraction of the organism, and can be separated from non-collagenous proteolytic activity by (NH(4))(2)SO(4) precipitation and Sephadex-gel chromatography. Its mode of attack on collagen and sensitivity to a variety of inhibitors indicate that this enzyme differs from vertebrate collagenases and a previously described invertebrate collagenase. 相似文献
144.
Ultrastructure of four types of striated muscle fibers in the atlantic hagfish (Myxine glutinosa,L.)
Summary Four types of striated muscle fibers with distinctive ultrastructure were defined in the Atlantic hagfish (Myxine glutinosa, L.): white, intermediate, and red fibers of m. parietalis, and red fibers of m. craniovelaris.White fibers are thick, contain very few mitochondria and fat vacuoles, and possess distinct and separate myofibrils with thin Z-disks and distinct M-lines. Intermediate fibers are thinner, possess largely similar myofibrils that often are even better separated due to a higher content of fat vacuoles and especially mitochondria and glycogen granules. Red fibers of m. parietalis contain large amounts of mitochondria, fat vacuoles, and glycogen granules. Their myofibrils possess M-lines, and although branching more, the myofibrils of red fibers conform with a Fibrillenstruktur pattern like those of white and intermediate fibers. Red fibers of m. craniovelaris are very thin, possess many smaller fat vacuoles, and large amounts of mitochondria and glycogen granules. The myofibrils are significantly thinner than in m. parietalis fibers, run as quite independent well separated units, possess thicker Z-disks, and lack M-lines. Large amounts of myosatellite cells are associated with these red fibers.Triads are located near A/I-junctions in all four fiber types and occur irregularly, the density of triads being different in the various fiber types.We are indebted to Dr. Finn Walvig, Biological Station, University of Oslo, Drøbak, for supply of hagfishes, and we also wish to thank Dr. Jan K. S. Jansen, Institute of Physiology, University of Oslo, for valuable suggestions during this study. 相似文献
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Julius Pia 《Molecular & general genetics : MGG》1922,30(1):63-98
Ohne ZusammenfassungVergleiche: J. Pia: DieSiphoneae verticillatae vom Karbon bis zur Kreide. Abhandl. Zool.-bot. Ges. Wien. Bd. 11. Heft 2. 1920. Mit Literaturliste. Seit dem Erscheinen dieser Arbeit sind mir folgende wichtigere einschlägige Veröffentlichungen bekannt geworden:A. Andreae: Ein Beitrag zur Kenntnis des Elsässer Tertiärs. Abhandl. z. geol. Spezialk. v. Elsaß-Lotr. vol. 2. fasc. 3. Straßburg 1884.A. Baretti: Contributo allo studio delleSiphoneae Verticillatae del calcare di Villanova-Mondovi. Atti soc. Ital. sc. nat. vol. 58. Pavia 1919. p. 216.F. Börgesen: The Marine Algae of the Danish West Indies. Part. 1.Chlorophyceae. Dansk. Bot. Arkiv. vol. 1. No. 4. 1913.F. Börgesen: The Marine Algae of the Danish West Indies. III.Rhodophyceae with Addenda to theChlorophyceae, Phaeophyceae andRhodophyceae. Ebendort. vol. 3. No. 1a–f. 1917–20.S. v. Bubnoff: Die ladinische Fauna von Forno (Mezzovalle) bei Predazzo. Verhandl. Heidelb. Naturh.-mediz. Vereins 1920. N. F. Bd. 14. S. 257.E. Fossa-Mancini:Sifoneae verticillatae triasiche e liassiche dell' Appennino umbro-marchigiano. Pro. verb. soc. Tosc. sc. nat. vol. 30. 10. III. 1921.M. Gortani: La fauna permocarbonifera del Col Mezzodi presso Forni Avoltri. Pal. Ital. vol. 12. 1906. p. 1.J. Kiaer: Oversigt over Kalkalgefloraerna i Norges Ordovicium og Silur. Norsk Geol. Tidskr. vol. 6. 1921. p. 113.O. Lignier: Végétaux fossiles de Normandie. VI. — Flore jurassique de Mamers (Sarthe). Mém. soc. Linn. Normandie. vol. 24. 1911–13. fasc. 1. p. 1.O. Lignier: Végétaux fossiles de Normandie. VII. — Contribution à la flore jurassique. Ebendort fasc. 2. 1913. p. 67.L. Morellet: Deux Algues siphonées verticillées du Thanétien de Boncourt (Oise). Bull. soc. géol. France ser. 4. vol. 8. 1908. p. 96.L. Morellet et J. Morellet: Les Dasycladacées du Tertiaire Parisien. Mém. soc. géol. France, Paléontologie. vol. 21. fasc. 1. Mém. No. 47. 1913.L. Morellet: Note sur les algues siphonées. In H. Douvillé: Le crétacé et l'éocène du Tibet central. Pal. Indica, New Ser. vol. 5. Mém. No. 3. p. 47. 1916.Munier-Chalmas: Notes préliminaires pour servir à l'étude des terrains crétacées. Bull. soc. géol. France. ser. 3. vol. 25. 1897. p. 82.Ph. Négris: Roches cristallophylliennes et tectonique de la Grèce. 2e appendice. Athènes 1919.S. Squinabol: Di una specie fossile di Acetabularia. Atti e Mem. Acc. sc. Padova, n. s. vol. 18. 1902. p. 151.Mit Tafel 1. 相似文献
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