What is new in the pathology of pancreatic neuroendocrine tumors?

The diagnostics of pancreatic neuroendocrine tumors (PanNEN) have changed in recent years especially concerning the World Health Organization (WHO) classification, TNM staging and grading. Furthermore, some new prognostic and predictive immunohistochemical markers have been introduced. Most progress, however, has been made in the molecular pathogenesis of these neoplasms. Using next generation sequencing techniques, the mammalian target of rapamycin (mTOR) pathway, hypoxia and epigenetic changes were identified as key players in tumorigenesis. In this article the most important developments of morphological as well as immunohistochemical diagnostics together with the molecular background of PanNEN are summarized.

The Forgotten Archduke: The Funeral Monument for Ernest of Austria in Brussels

Archduke Ernest of Austria (1553–1595), second son of Emperor Maximilian II and younger brother of Emperor Rudolf II, was in his youth a possible candidate for the thrones of the Empire or the Spanish Kingdom. Instead, he became Governor-General of the Netherlands in 1593 and relocated to Brussels in 1594 where he was welcomed with lavish festivities as the bearer of hope and prosperity. Unfortunately, Ernest died only thirteen months later without having achieved any political success. His brother and successor Albert of Austria commissioned the funeral monument for Ernest in 1600 after it was settled that he would be buried in Brussels and not Vienna. Focusing on this monument, which draws stylistically from various dynasty-related models, it will be shown that Albert intended to use this monument – and thus his brother’s memoria – to make the Brussels Cathedral the primary location of Habsburg dynastic memory in the Low Countries.

Po Beerez [Musikdruck] : ("Im Lande der Väter")

Arno Nadel

Na 1 Nachlass Max Horkheimer, 24 - Korrespondenzen u.a. mit Stefan Jacobwicz (p. I 12, 176-330)

1 Brief an Ernst Jacob von Max Horkheimer; 31 Briefe zwischen Stefan Jacobwicz und Max Horkheimer, 1936-1945; 1 Brief an die American Consul Lisabon von Max Horkheimer; 23 Briefe zwischen Heinz Jacoby, Lilli Jacoby und Max Horkheimer, 1936-1943; 1 Brief von Max Horkheimer an John B. Norman, 29.06.1942; 1 Brief von Max Horkheimer an George L. Warren; 1 Brief vom Service Social d'Aide aux Emigrants Paris an Heinz Jacobi, 18.01.1940; 1 Brief von Max Horkheimer an Jaeger , 29.09.1937; 5 Brief zwischen Philip C. Jessup und Max Horkheimer, 15.10.1940-1941; 3 Briefe an die Jewish National and University Library Jerusalem von Max Horkheimer, 1943, 1949; 5 Briefe zwischen der Jewish Telegraphic Agency New York und Max Horkheimer, 1940; 2 Briefe zwischen Ernest Jones und Max Horkheimer, 29.04.1938, 11.05.1938; 14 Briefe zwischen der Journal of Criminal Psychopathology, Woodbourne und Max Horkheimer,1940-1941; 1 Brief vom Journal of Philosophy and Phenomenological Research Bufallo N.Y. an Max Horkheimer, 19.11.1940; 1 Brief an das Jüdisches Schwesternheim Stuttgart an Max Horkheimer, 29.12.1937; 1 Brief von Jean Juget an Max Horkheimer, 25.11.1935; 2 Briefe zwischen der Juilliard School of Music New York und Theodor W. Adorno, 17.07.1940, 18.07.1940; 2 Briefe zwischen Gustave S. Juliber und Max Horkheimer, 09.10.1938, 01.11.1938;

Na 1 Nachlass Max Horkheimer, 543 - Korrespondenzen u.a. mit Leo Löwenthal und Henryk Grossmann (p. VI 17, 1 - 156)

106 Briefe zwischen Max Horkheimer und Leo Löwenthal; 5 Briefe zwischen Paul Massing und Max Horkheimer, 1944; 1 Brief von Max Horkheimer an Philip Klein, 24.07.1944; 1 Brief von Max Horkheimer an Gerhard H. Seger, 22.07.1944; 1 Brief von Frederick Pollock an Elliot Cohen, 23.06.1944; 1 Brief von Frederick Pollock an Henryk Grossman, 21.04.1944; 1 Brief von Max Horkheimer an Henryk Grossman, 03.07.1944; 2 Briefe zwischen Frederick Pollock und Leo Löwenthal, April u. September 1944; 1 Brief von Leo Löwenthal an H. Schickel, 07.04.1944; 2 Briefe von der Biographical Encyclopedia of the World (New York) an Max Horkheimer, 1944; 1 Brief von dem Office of War Information (Washington D.C.) an Leo Löwenthal, 17.01.1944;

Geochemistry and age determination of zircons in Cretaceous to Quaternary sediments

In central Antarctica, drainage today and earlier back to the Paleozoic radiates from the Gamburtsev Subglacial Mountains (GSM). Proximal to the GSM past the Permian-Triassic fluvial sandstones in the Prince Charles Mountains (PCM) are Cretaceous, Eocene, and Pleistocene sediment in Prydz Bay (ODP741, 1166, and 1167) and pre-Holocene sediment in AM04 beneath the Amery Ice Shelf. We analysed detrital zircons for U-Pb ages, Hf-isotope compositions, and trace elements to determine the age, rock type, source of the host magma, and "crustal" model age (T(C)DM). These samples, together with others downslope from the GSM and the Vostok Subglacial Highlands (VSH), define major clusters of detrital zircons interpreted as coming from (1) 700 to 460 Ma mafic granitoids and alkaline rock, epsilon-Hf 9 to -28, signifying derivation 2.5 to 1.3 Ga from fertile and recycled crust, and (2) 1200-900 Ma mafic granitoids and alkaline rock, epsilon-Hf 11 to -28, signifying derivation 1.8 to 1.3 Ga from fertile and recycled crust. Minor clusters extend to 3350 Ma. Similar detrital zircons in Permian-Triassic, Ordovician, Cambrian, and Neoproterozoic sandstones located along the PaleoPacific margin of East Antarctica and southeast Australia further downslope from central Antarctica reflect the upslope GSM-VSH nucleus of the central Antarctic provenance as a complex of 1200-900 Ma (Grenville) mafic granitoids and alkaline rocks and older rocks embedded in 700-460 Ma (Pan-Gondwanaland) fold belts. The wider central Antarctic provenance (CAP) is tentatively divided into a central sector with negative ?Hf in its 1200-900 Ma rocks bounded on either side by positive epsilon-Hf. The high ground of the GSM-VSH in the Permian and later to the present day is attributed to crustal shortening by far-field stress during the 320 Ma mid-Carboniferous collision of Gondwanaland and Laurussia. Earlier uplifts in the ~500 Ma Cambrian possibly followed the 700-500 Ma assembly of Gondwanaland, and in the Neoproterozoic the 1000-900 Ma collisional events in the Eastern Ghats-Rayner Province at the end of the 1300-1000 Ma assembly of Rodinia.