Grimm k i (28 Ergebnisse)

10 S., 5 Abb., Sprache: Deutsch Gewicht in Gramm: 500.

hardcover. Zustand: Very Good.

Softcover. 38 x 27,5 cm. Ungeklammerte Original-Zeitschrift mit 12 unpaginierten Seiten, vielen s/w Fotos und einigen einfarbigen Illustrationen. Sauber und gut erhalten. die Abkürzung H.H. stand für das Archiv des Berliner Presse- und Bilderdienstes Heinrich Hoffmann (der offizielle 'Leibfotograf' Adolf Hitlers) / PK: Propandakompanie, spezielle Truppengattung der deutschen Wehrmacht und der Waffen-SS, in ihr waren Fotografen, Filmer und Schreiber als Soldaten organisiert, zur Lieferung von Material für die Kriegspropaganda -- Bitte Portokosten außerhalb EU erfragen! / Please ask for postage costs outside EU! / S ' il vous plait demander des frais de port en dehors de l ' UE! // Bitte beachten Sie auch unsere Fotos! / Please also note our photos! / Veuillez noter nos photos -- Genießen Sie den goldenen Herbst! Machen Sie es sich gemütlich , bei uns finden Sie sicher die passende Lektüre! -- Wir kaufen Ihre werthaltigen Bücher! K08233-438948. …

11 pp., 3 plates, gr. 8.

The wall structure of some foraminifers from the Rupeliam of the Mainz Basin, formerly referred to Spiroplectammina Cushman 1927, is examined. They are classified as Spiroplectinella Kisel?man 1972 because of the occurrence of pseudopores. The genus neither belong to the Spiroplectamminacea nor to the Textulariacea. The proposition of Hottinger et al. (1990) to separate it from these superfamilies is confirmed. 6 pp., 4 figs, gr. 8.…

The tintinnid Pseudarcella rhumbleri Spandel, 1909 from the Rupelian (Oligocene) of the Mainz Basin, is redescribed based on a neotype. Even though Tappan & Loeblich showed as early as 1968 that Pseudarcella is a tintinnid, more recent works of the Mainz Basin have still refered to it as being a foraminifera. 5 pp., 1 fig., gr. 8.…

5 pp., 1 fig., 4.

Valves of 20 Oligocene pelecypods from the Mainz Basin and 14 recent valves were examined for growth patterns. Whereas the microgrowth increments of the Rupelian samples indicate fortnightly tidal intervals, the Chattian specimens show annual (seasonal) variations in growth. 10 pp., 5 figs, gr. 8.

6 pp., 3 figs, 4.

Specimens of Discorbinoides patelliformis (Brady, 1884) are frequently fused at their apertural openings. This species is briefly described and the origin of this phenomenon is discussed. 6 pp., 1 fig., 8.

Hollow approx. 200 ?m diameter spheres have been frequently found in the Rupelian Fischschiefer of the Mainz Baisin. Spandel (1909) first described them as Orbulina bituminosa and interpreted them as foraminifera. The prefered interpretation of the spheres is that they are Crustacean eggs because of similarities both in terms of size and internal structure. 6 pp., 3 figs, gr. 8.…

18 pp., 4 figs, gr. 8.

The Lower Rupelian Clay and the Lower Meeressand of the Mainz Basin are subdivided using foraminifera. Based on this subdivision, the coastal facies, the Lower Meeressand, is correlated with the basin facies of the Rupelian Clay in the Mainz Basin. 11 pp., 4 figs, 8.

4 pp., 1 plate, gr. 8.

Close spaced sampling of 5 clay quarries in the Rupel area of Belgium and of 8 outcrop and 40 borehole sections in the Mainz Basin has led to an almost continuous foraminiferal record throughout the Middle Rupelian of the southern North Sea Basin. The distribution of foraminifera in the Boom Clay Formation is rather complex and directly related to its paleobathymetric evolution and its burial history. The exposed Boom Clay section studied here (Beds 1 to 55) can be subdivided in four major intervals, in which nine foraminiferal biofacies can be identified. Comparison with the foraminifera of the Rupelton in the Mainz Basin allows to equate the boundary between the Foraminiferenmergel (FM) and the Fischschiefer (FS) with the Terhagen Clay/Putte Clay boundary, the FM 2/FM 3 boundary with the base of pink layer Bed 21 and the FS A/FS B boundary with the base of the double band (Bed 39). The major changes in lithofacies and in foraminiferal associations reflect substantial changes in circulation in the southern North Sea Basin, due to eustatic sea-level changes and to the closure of marine pathways, related to uplift in the Alpine Foldbelt. 12 pp., 5 figs, 4.…

8 pp., 5 figs, gr. 8.

4 pp., 1 fig., 8.

4 pp., gr. 8.

4 pp., 2 figs, 4.

Studies on the foraminiferal fauna of five Rupelial sections in the Bavarian molasse and in the Inntalterti?r and also on material housed in the collection of the Bavarian Staatssammlung were made. The foraminiferal fauna was compared to those of the Mainz Basin and Upper Rhine Graben. Apart from the occurence of endemic and cosmopolitan foraminifers, species were identified which occur in the North Sea and Molasse basin only, but not in the Upper Thine Graben and Mainz Basin. Foraminifers, which existed only in the southern Rhine Graben and in the Molasse Basin, could not be identified in the investigated period. The results demonstrate that during the Rupelian a seaway connection, suitable for foraminifers, between the Bavarian Molasse, the Inntal-Tertiary, the Upper Rhine Graben and the Mainz Basin did not exist. 17 pp., 5 figs, 8.…

18 pp., 2 figs, gr. 8.

20 pp., 5 figs, 3 plates, gr. 8.

28 pp., 2 figs, 1 plate, br. 4 [+CD].

158 pp. + 3 pls, 14 figs, 4 tabs, br. 4.

Sonne, V.: Karlheinz Rothausen zum 70. Geburtstag. Grimm, K.I.: Schriften von Karlheinz Rothausen. Farsan, N.M.: Das Etroeungtium (Ober-Devon VI, Strunium) und die letzten Phacopinae (Trilobita) im westlichen Zentral- und West-Afghanistan. Grimm, M.C.: Orthocone Cephalopoden als sekund?re Hartgrundsubstrate in Black Shales des Oos-Plattenkalks (Frasniums der B?desheimer Mulde, Eifel, Deutschland). Stapf, K.R.G.: Erhaltung zarter Cyanobakterien-Strukturen in lakustrinen Kalksteinen durch schnelle Tuff-?berdeckung und anschlie?ende fr?hdiagenetische Silifizierung (Jakobsweiler Kalkstein, Nahe-Gruppe, Rotliegend, Saar-Nahe-Becken, SW-Deutschland). Schwarz, J. & Griessemer, T.W.: Eine neue Charophyten-Art aus dem Lutetium (Mitteleoz?n) des Oberrheingrabens bei Albersweiler (Rheinland-Pfalz, SW-Deutschland): Chara rothauseni sp. n. Hottenrott, M.: Eine eoz?ne Mikroflora aus dem Eisberger Becken (Nordpfalz, Deutschland). Martini, E.: Eine neue Trochaster-Art (Nannoplankton) mit Leitcharakter in den Mittleren Pechelbronn-Schichten (Unter-Oligoz?n). Mehrnusch, M.: Die Bolivinen (Foraminifera) des Melanientons (Oligoz?n der Hessischen Senke, Deutschland). Grimm, K.I.: Karreria rhenana (Spandel 1909), eine fixosessile Foraminifere von der Neum?hle (Oligoz?n, Mainzer Becken, Deutschland). G?rs, K.: Kleinturriden der Mangeliinae und Daphnellinae (Mollusca, Gastropoda) aus dem Unteren Meersand (Rupelium, Oligoz?n) des Mainzer Beckens. Sch?fer, P. & Kadolsky, D.: Zur Gliederung eines Terti?rprofils von Budenheim bei Mainz, insbesondere zur stratigraphischen Stellung und Genese der Milchquarzschotter (Oberoligoz?n) im nordwestlichen Rheinhessen (Mainzer Becken) . M?dden, C.: Eomyiden (Rodentia, Mammalia) aus dem Steinbruch Fl?rsheim (Unter-Mioz?n, Mainzer Becken, Deutschland). Heizmann, E.P.J. & Morlo, M.: Die semiaquatische Lartetictis dubia (Mustelinae, Carnivora, Mammalia) vom Goldberg/Ries (Baden-W?rttemberg). H?nermann, K.A.: Das Nashornkalb (Rhinocerotidae, Mammalia) vom H?wenegg (Obermioz?n, SW-Deutschland). Fordyce, R.E. & Watson, A.G.: Vertebral pathology in an Early Oligocene whale (Cetacea, ?Mysticeti) from Wharekuri, North Otago, New Zealand. Bopp, A. & Frauendorf, E.: Cribra orbitalia - Pathologische Befunde aus der Skelettsammlung im Beinhaus Oppenheim am Rhein. 186 pp., num. figs, br. 4.…

24 pp., 16 figs, gr. 8.

28 pp., 10 figs, gr. 8.

4°. 200 S. mit 92 Fotos (zumeist in Farbe) und 33 Zeichnungen. ill. OLn mit OUmschl. tadellos. EA.