Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 546 - Benachrichtigung über den Tod der Schwester

u.a.: Beschreibung der Stadt Hamburg;

Die letzten Tage von Pompeji : geschichtliche Schilderung aus dem Jahr 79 nach Chr. ; (frei nach E. L. Bulwer u. A.)

von J. A. Pflanz

Ms. lat. qu. 79 - De contractibus

Vorbesitzer: Benediktinerkloster St. Jakob in Mainz

Ms.Ff.F.Stoltze 3. 79 - Brief von Historisches Museum an Lydia Lerner-Stoltze

Stoltze-Gedächtnisausstellung

Ms.Ff.F.Stoltze 3. 546 - Brief von Friedrich Stoltze an Unbekannt

Frankfurter Latern, Zeichner, Honorar, Ende der Zusammenarbeit

Goethe im 79. Lebensjahre

Signatur des Originals: S 36/F04202

Goethe im 79. Lebensjahre

Signatur des Originals: S 36/F04203

Göthe im 79. Lebensjahre, von Stieler gemalt : Zur Erinnerung an Göthes 150 jähr. Geburtstag, 28. Aug. 1899

Signatur des Originals: S 36/F04204

Göthe im 79. Lebensjahre, von Stieler gemalt : Zur Erinnerung an Göthes 150 jähr. Geburtstag, 28. Aug. 1899

Signatur des Originals: S 36/F04205

Na 1 Nachlass Max Horkheimer, 546 - Korrespondenzen mit Leo Löwenthal (p. VI 18, 215-414)

135 Briefe zwischen Leo Löwenthal und Max Horkheimer; 2 Briefe von Max Horkheimer an S. Flowerman, 1945/1946; 2 Briefe zwischen John Slawson und Max Horkheimer, Februar 1946; 1 Brief von R. Nevitt Sanford an John Slawson, 31.01.1946; 1 Brief von Paul Lazarsfeld an Norbert K. Merton, 04.02.1946; 1 Brief von Paul Lazarsfeld an Theodore Abel, 05.02.1946; 2 Briefe zwischen Max Horkheimer und Dessie E. Kushell, Januar 1946; 3 Briefe von Max Horkheimer an Margaret Nicolson, Januar 1946;

Ms. lat. oct. 79 - Logica peripateticorum

Vorbesitzer: F M K O C

Oceanography during TYDEMAN cruise DCM (DeepChlorMax) to the Equatorial Atlantic

The cruise with RV Tydeman was devoted to study permanently stratified plankton systems in the (sub)tropical ocean, which are characterised by a deep chlorophyll peak between 80 and 150 m. To minimise lateral effects by horizontal transport of nutrients and organic matter from river outflow and upwelling regions, stations were selected in the middle of the North Atlantic Ocean between the continents of America and Africa. (5 - 35° N and 50 - 15° W). Here the vertical distributions of light and nutrients control the abundance and growth of autotrophic algae in the thermically stratified water column. This phytoplankton is numerically dominated by the prokaryotic picoplankters Synechococcus spp. and Prochlorococcus spp., which are smaller than 2 ?m. The productivity of the 100 to 150 m deep euphotic zone can be high, because a high heterotrophic/autotrophic biomass ratio induces a rapid regeneration of nutrients and inorganic carbon. Primary grazers are mainly micro-organisms such as heterotrophic nannoflagellates and ciliates, which feed on the small algae and on bacteria. Heterotrophic bacteria can outnumber the autotrophic algae, because their number is related to the substrate pools of dissolved and particulate dead organic matter. These DOC and detritus pools reach equilibrium at a concentration, where the rate of their production (proportional to algal biomass) equals their mineralisation and sinking rate (proportional to the concentration and weight of POC and detritus). At a relatively low value of the weight-specific loss rates, the equilibrium concentration of these carbon pools and their load of bacteria can be high. The bacterial productivity is proportional to the mineralisation rate, which in a steady state can never be higher than the rate of primary production. Hence the ratio in turnover rate of bacteria and autotrophs tends to be reciprocally proportional to their biomass ratio.