Gilgal : ein Beitrag zur Geschichte der Einwanderung Israels in Palästina

von Ernst Sellin

Das Vater Unser eines Unterwaldners

erfunden von Johann Martin Usteri in Zürich, ausgef. und in Tuschmanier geäzt von Marquard Wocher

Na 1 Nachlass Max Horkheimer, 563 - Korrespondenzen u.a. mit Alice H. Maier und Leo Löwenthal (p. VI 27, 1-253)

Briefwechsel zwischen Max Horkheimer und Alice H. Maier; 5 Briefe an Maurice und Carolyn Tumarkin von Max Horkheimer, 1957/1964; 1 Brief von Max Horkheimer an Charles Gorman, 27.04.1957; 1 Brief von Alice H. Maier an die Marquis Company (Chicago), 06.05.1957; 2 Briefe an H. P. Edelman von Max Horkheimer, 1964; 3 Briefe zwischen Alice H. Maier und H. P. Edelman, 1957/1963; 1 Brief von Margot von Mendelssohn an Alice H. Maier, 01.04.1957; 1 Brief an Richard Corwine Stevenson von Max Horkheimer, 16.03.1957; 1 Brief von Max Horkheimer an Inge Aicher-Scholl, 26.02.1957; 1 Brief an Herman Strasburger von Max Horkheimer, 21.01.1957; 1 Brief von Elisabeth Richter an Alice H. Maier, [1957]; 1 Brief an den Director of International Operations (Washington) von Chauncy D. Harris, 05.02.1957; 1 Brief von Alice H. Maier an Comptroller of Customs (New York), 11.01.1957; 1 Brief an Herbert Marcuse von Alice H. Maier, 14.01.1957; 2 Briefe zwischen Alice H. Maier und The Saturday Evening Post (Philadelphia), Oktober 1956; 1 Brief an die Staats-Herold Corporation (Woodside) von Alice H. Maier, 24.09.1956; 2 Briefe zwischen Alice H. Maier und Werner Thönnessen, 1956; 2 Briefe zwischen dem National Better Business Bureau (New York) und Alice H. Maier, 1956; 2 Briefe zwischen Alice H. Maier und Herman L. Filene, Januar 1956; 5 Briefe zwischen Max Horkheimer und Edwin J. Lukas, 1962 - 1963; 7 Briefe zwischen Monroe Karasik und Max Horkheimer, 1963; 1 Brief von Max Horkheimer an James Conant, 30.05.1963; 1 Brief an John J. McCloy von Max Horkheimer, 30.05.1963; 3 Briefe an Herman S. Klein von Alice H. Maier, 1960/1963; 1 Brief von Max Horkheimer an Hartley Chemists (New York), 06.02.1962; 1 Brief an Columbia Chemists (New York) von Max Horkheimer, 06.02.1962; 1 Brief von Max Horkheimer an A. P. Bersohn, 06.06.1962; 1 Brief an A. P. Bersohn von Alice H. Maier, 20.04.1962; 1 Brief an Alice H. Maier von Paul Kind, 22.05.1962; 1 Brief an Cyrus C. Hoffman von Alice H. Maier, 23.03.1961; 2 Briefe von Alice H. Maier an Friedrich Pollock, 1960/1966;

(Table S1) Age determination of Emperor Seamounts basement

The Hawaiian-Emperor hotspot track has a prominent bend, which has served as the basis for the theory that the Hawaiian hotspot, fixed in the deep mantle, traced a change in plate motion. However, paleomagnetic and radiometric age data from samples recovered by ocean drilling define an age-progressive paleolatitude history, indicating that the Emperor Seamount trend was principally formed by the rapid motion (over 40 millimeters per year) of the Hawaiian hotspot plume during Late Cretaceous to early-Tertiary times (81 to 47 million years ago). Evidence for motion of the Hawaiian plume affects models of mantle convection and plate tectonics, changing our understanding of terrestrial dynamics.

Nannofossil bioevents and biozones of ODP Holes 197-1203A and 197-1204A on Detroit Seamount

Calcareous nannofossils were studied in sedimentary successions recovered from two holes on the Detroit Seamount in the northwestern Pacific Ocean. Preservation of calcareous nannoflora assemblages varies from poor to good throughout the sediments recovered from both Holes 1203A and 1204A. Biostratigraphic investigation allowed the identification of 19 nannofossil zones in Hole 1203A and 7 in Hole 1204A. The sedimentary cover in Hole 1203A ranges from lower Eocene (Zone NP12) to upper Miocene (Zone NN9). The sedimentary interval investigated directly overlying the basalt recovered at Hole 1204A is late Campanian in age (Zones CC22-CC23), and the top of the section is middle Eocene (Zone NP15) in age. Major unconformities were observed in Hole 1204A between upper Campanian (Zones CC22-CC23) and lower Thanetian (Zone NP7) sediments and between upper Thanetian (Zone NP8) and upper Ypresian (Zone NP12) sediments.

Stable Water Isotopologue data collected during HCCT-2010

Cloud samples for the isotopic analysis were collected in the framework of the Hill Cap Cloud Thuringia 2010 (HCCT-2010) campaign on Schmücke (50° 39'N/ 10° 46'E, 937 m a.s.l.; Germany) in September and October 2010 with a three-stage Caltech Active Strand Cloudwater Collector (CASCC) during 13 different cloud events with a temporal resolution of 1 to 3 hours. In a first step, we ensured that no additional fractionation occurred during sampling with the CASCC. The d values of the three sizes classes of the CASCC (4 µm to 16 µm, 16 µm to 22 µm and >22 µm) did not differ significantly, revealing that the cloud droplets of different sizes quickly equilibrate their delta value with the one of the surrounding vapor. delta values in the cloud droplets varied from -77 per mil to -15 per mil in d2H and from -12.1 per mil to -3.9 per mil in d18O and were fitted by d2H =7.8*d18O +13*10**-3. delta values decreased with temperature as well as towards the end of the campaign, representing a seasonal trend which is known from d values in precipitation. The deuterium excess of the cloud samples was generally higher than the Local Meteoric Water Line of the closest GNIP (Global Network of Isotopes in Precipitation) station. Rain decreases its deuterium excess during falling through an unsaturated air column, while the cloud droplets conserve the deuterium excess of the initial evaporation and thus have been found to be a good indicator for the airmass source region: higher deuterium excess was measured for polar air masses and lower deuterium excess for Mediterranean air masses. Changes in d values during one cloud event were up to 3.6 per mil (d2H) and 0.23 per mil (d18O), except for frontal passages, which were associated with increases of ~6 per mil per hour (d2H) and ~0.6 per mil per hour (d18O). Using a box model, we showed that the influence of condensation only was able to explain the variation in the isotope signal of two cloud passages. Consequently, we deduced that the water vapor "feeding" the cloud advected the measured changes. A trajectory analysis and moisture source diagnostic revealed that it is very likely that the variations were either related to rain out along the trajectories or to meteorological changes in the moisture source region. This was the first study using stable water isotopologues in cloud water manifesting their potential in the context of atmospheric water vapor circulation.