Anna Amalia, Brustbild

Signatur des Originals: S 36/G02716

Anna Bishop, Kniestück

Signatur des Originals: S 36/G02820

Anna Euphrosina Krauß, Kniestück

Signatur des Originals: S 36/G03237

Pauline Anna Milder-Hauptmann, Brustbild

Signatur des Originals: S 36/G03396

Pauline Anna Milder-Hauptmann, Brustbild

Signatur des Originals: S 36/G03397

Pauline Anna Milder-Hauptmann, Rollenbild, Hüftbild

Signatur des Originals: S 36/G03398

Anna Schechner, Brustbild

Signatur des Originals: S 36/G03611

Maria Anna Lager, Brustbild

Signatur des Originals: S 36/G04163

Giuditta Pasta als Anna Bolena, Rollenbild, Kniestück, in: Gaetano Donizetti: Anna Bolena

Signatur des Originals: S 36/G14295

Anna Barbara von Röbel, Rollenbild

Signatur des Originals: S 36/G04336

Valère als Anna, Rollenbild, in: Carl Maria von Weber: Der Freischütz

Signatur des Originals: S 36/G04430

Zum Gedächtnis an Dr. Meier Appel : Stadt- und Konferenzrabbiner in Karlsruhe, gest. 8. Februar 1919 und seine Gattin Anna Appel, geb. Willstätter, gest. 31. Dez. 1918

Digitalisiert in Kooperation mit dem YIVO Institute for Jewish Research am Center for Jewish History, NY

Interview with Anna Steinberger

An oral interview with Dr. Anna Steinberger, who taught and conducted basic research in Reproductive Biology and served as Assistant Dean for Faculty Affairs at UT Medical School-Houston. Her research yielded over 250 scientific articles, books, and book chapters for which she received numerous awards and recognitions in the USA and abroad.

Clay minerals in bottom sediments of the St. Anna Trough

This paper is devoted to studies of clay minerals from two cores collected in the northern and central regions of the St. Anna Trough, the largest trough of the Kara Sea. Upper Quaternary glacial, glaciomarine, and marine deposits are characterized by various contents of kaolinite, chlorite, illite, and smectite. It is established that, from older to younger deposits, amounts of kaolinite and chlorite generally decrease, while those of illite and smectite, on the contrary, increase. A joint analysis of distributions of clay and heavy minerals over the section allowed us to refine position of sources for terrigenous matter and their temporal variability. It is shown changes in sources of supply were directly related to climate changes that occurred when passing from glacial to marine sedimentation environments.