Johann Heinrich Hottinger, Brustbild

Signatur des Originals: S 36/G04128

Carl Graumann als Heinrich Krey, Rollenbild, Brustbild, in: Carl Sternheim: Bürger Schippel

Signatur des Originals: S 36/G04573

Heinrich Henkel, Brustbild

Signatur des Originals: S 36/G04597

Friedrich Christian Heinrich Schönheit : Ein Lebensbild des thüringer Floristen zur Säkularfeier seines Geburtstages

Von Oskar Schmidt

Aus Briefen an Heinrich Voss

Bernhard Rudolf Abeken

Wohlverdienter Gedächtniß-Tempel : Welcher zu Ehren der in Gott zu Badrin den 28. Julij Seelig entschlaffenen Wohlgebohrnen Frauen, Frn. Johanna Rahel gebohrner Lämmelin, Des ... Herrn, Herr Heinrich Otto D'Egydi ... gewesener Eheliebsten, Bey Ihrer Beerdigung ... 4. Octob. 1696 ...

auffgerichtet worden Von M. Johann Weller

Briefe an Johann Heinrich Merck von Göthe, Herder, Wieland und andern bedeutenden Zeitgenossen : mit Merck's biographischer Skizze

herausgegeben von Karl Wagner

Briefe an und von Johann Heinrich Merck : eine selbständige Folge der im Jahr 1835 erschienenen Briefe an J. H. Merck ; mit Facsimilien der Handschriften von Göthe, Herder, Wieland ...

aus den Handschriften herausgegeben von Karl Wagner

Beck, Heinrich/Ismael Quiles (Editores) Entwicklung zur Menschlichkeit durch Begegnung westlicher und östlicher Kultur: Akten d. IV Interkontinentalen Kolloquiums zur Philos. In-sistenzanthropologie, 1 . - 6 . September 1986 an d. Univ. Bamberg, Frankfurt am Main; Bern; New York; París: Lang, 1988 (Schriften zur Tríadik und Ontodynamik; Band 1)

Fil: Matuschka, Daniel von.

La puerta trasera del Edén : acerca de la gracia en “Über das marionettentheater" de Heinrich von Kleist

El presente trabajo analiza la cuestión de la gracia en el breve relato kleistiano “Acerca del teatro de las marionetas". El problema filosófico que allí se presenta es el de la posibilidad de que un cuerpo artificial como el del muñeco articulado adquiera una gracia que el cuerpo propio del ser humano no podría alcanzar jamás, aun en el caso de los mejores bailarines. Nos proponemos entonces el desafío de pensar de qué modo debe ser pensada la relación entre los cuerpos y el conocimiento para que tal fenómeno sea posible. Sostendremos que la noción de gracia constituye en este texto el modo kleistiano de construir una línea de fuga frente a su interpretación de Kant.

Age determination and Heinrich Events in sediment cores SU90-08 and KET80-03

The Mediterranean Sea hydrology at the time of the Heinrich formation in the North Atlantic Ocean was analyzed by comparing sea surface temperatures (SSTs) and oxygen isotope composition of seawater (dw) changes during the past 75 kyr in two marine cores. These were compared to the palynological variations derived in the Mediterranean Sea core. During the last glacial the two oceanic SST records show similar and synchronous patterns, with several long-term cooling periods, ending by abrupt SST increases. At the time of the Heinrich events, cold SSTs and low salinity prevailed in the Mediterranean Sea. The freshwater budget was similar to the modern one, permitting the presence of a mixed forest on the Mediterranean borderlands. The post-Heinrich periods are marked by a freshwater budget decrease, limiting oak and fir tree growth in the Mediterranean region. Increase of precipitation or reduction of evaporation is observed before the Heinrich episode, and is associated with a well-developed mixed Mediterranean forest.

Abrupt shifts of the Sahara-Sahel boundary during Heinrich stadials demonstrated on a sediment core transect

Relict dune fields that are found as far south as 14° N in the modern-day African Sahel are testament to equatorward expansions of the Sahara desert during the Late Pleistocene. However, the discontinuous nature of dune records means that abrupt millennial-timescale climate events are not always resolved. High-resolution marine core studies have identified Heinrich stadials as the dustiest periods of the last glacial in West Africa although the spatial evolution of dust export on millennial timescales has so far not been investigated. We use the major-element composition of four high-resolution marine sediment cores to reconstruct the spatial extent of Saharan-dust versus river-sediment input to the continental margin from West Africa over the last 60 ka. This allows us to map the position of the sediment composition corresponding to the Sahara-Sahel boundary. Our records indicate that the Sahara-Sahel boundary reached its most southerly position (13° N) during Heinrich stadials and hence suggest that these were the periods when the sand dunes formed at 14° N on the continent. Heinrich stadials are associated with cold North Atlantic sea surface temperatures which appear to have triggered abrupt increases of aridity and wind strength in the Sahel. Our study illustrates the influence of the Atlantic meridional overturning circulation on the position of the Sahara-Sahel boundary and on global atmospheric dust loading.