Ms.Ff.F.Stoltze 3. 204 - Brief von Martin Ochs an Friedrich Stoltze

Bernhard Schnapper, Frankfurter Latern, Krebbelzeitungen, Nizza

Inc. hebr. 61 - Perush seder ha-tefilot

Vorbesitzer: Abraham Merzbacher (?)

Fragm. lat. VII 61 - Kanonistischer Text

Trägerband: Inc. qu. 873; Vorbesitzer: Dominikanerkloster Frankfurt am Main

Na 1 Nachlass Max Horkheimer, 577 - Korrespondenzen mit Friedrich (Frederick) Pollock (p. VI 32, 204-409)

1 Brief von Max Horkheimer an Edwin S. Bingham, 03.05.1942; 1 Brief von Frederick Pollock an A. P. Bersohn, 12.03.1942; 1 Brief von Austin P. Evans an Frederick Pollock, 26.02.1942; 1 Brief von Alice H. Maier an Max Horkheimer, 10.02.1942; 1 Brief von Franz Neumann an Frederick Pollock, 02.02.1942; 1 Brief von Frederick Pollock an Moritz Bonn, [1942];

Ms. lat. oct. 61 - Directorium Moguntinum ad usum ecclesiae S. Bartholomaei Francfordensis

Die tatsächliche Blattzahl weicht von den Angaben des Kataloges ab.

Ausst. 204 - Beschreibu[n]g des heyligen Bischoffs Eusebij: der ain junger vn[d] discipel deß heyligen Sancti Hieronymi gewest ist zu dem Bischoff Damaso vn[d] dem Römer Theodosio von dem leben vn[d] sterben desselben heyligsten Hieronymi. Welche beschreybung sonnst Sannt Hieronymus geschefft oder Testament genannt wirdet mit vil gezierten götliche[n] vn[d] Cristenlichen leern vermenget durch ainen sondern liebhaber Sancti Hieronymi auß dem Latein in das tewtsch gezogen

Vorbesitzer: Heinrich Anton Cornill-d'Orville (Exlibris im Vorderdeckel)

Fragm. lat. I 18 - Micrologus (c. 23, 46 - 49, 51 - 61)

Trägerbände: Ms. Barth. 13; Ms. Barth. 18; Ms. Barth. 29; Ms. Barth. 41; Vorbesitzer: Bartholomaeusstift Frankfurt am Main

Ms. lat. oct. 204 - La Cortona convertita

Vorbesitzer: Michelangelo Gualandi;

Sonate pour le pianoforte et flûte oeuv. 61

par F. Schneider

Isotope ratios of basalts from ODP Leg 115 holes (Table 1)

Strontium, neodymium, and lead isotope ratios are reported for 13 Leg 115 basalts as well as 3 basalts from Texaco drill hole SM-1 on the Mascarene Plateau. The 87Sr/86Sr ratios and eNd range from 0.70330 to 0.70439 and 5.5 to 7.4, respectively, although 87Sr/86Sr ratios higher than 0.70383 are found only in SM-1 basalts. The high 87Sr/86Sr values are thought to reflect seawater Sr in secondary phases, although all samples were strongly leached in HC1 before analysis. 206Pb/204Pb ratios range from 18.53 to 18.80, and sho high 207Pb/204Pb and 208Pb/204Pb ratios relative to 206Pb/204Pb ratios, typical of Indian Ocean mid-ocean ridge (MORB) and oceanic-island basalts (OIB). Isotopic compositions of Leg 115 basalts generally fall between fields for MORB and Reunion Island basalts, consistent with the conclusion drawn from geochronological studies that Deccan flood basalt volcanism, the Chagos-Laccadive Ridge, and the Mascarene Plateau are all products of the Reunion mantle plume. Isotopic compositions of magmas produced by this plume have varied systematically with time in the direction of less "depleted," less MORB-like isotopic signatures. This compositional change has been accompanied by a decrease in eruption rate. We interpret Deccan volcanism as the voluminous beginning of the plume. Reduced entrainment of asthenosphere following melting of the plume head resulted in less MORB-like isotope ratios in magmas and a decrease in eruptive activity with time.

Physical oceanography from the TRACTOR project

Primary Objectives - Describe and quantify the present strength and variability of the circulation and oceanic processes of the Nordic Seas regions using primarily observations of the long term spread of a tracer purposefully released into the Greenland Sea Gyre in 1996. - Improve our understanding of ocean processes critical to the thermaholine circulation in the Nordic Seas regions so as to be able to predict how this region may respond to climate change. - Assess the role of mixing and ageing of water masses on the carbon transport and the role of the thermohaline circulation in carbon storage using water transports and mixing coefficients derived from the tracer distribution. Specific Objectives Perform annual hydrographic, chemical and SF6 tracer surveys into the Nordic regions in order to: - Measure lateral and diapycnal mixing rates in the Greenland Sea Gyre and in the surrounding regions. - Document the depth and rates of convective mixing in the Greenland Sea using the SF6 and the water masses characteristics. - Measure the transit time and transport of water from the Greenland Sea to surrounding seas and outflows. Document processes of water mass transformation and entrainment occurring to water emanating from the central Greenland Sea. - Measure diapycnal mixing rates in the bottom and margins of the Greenland Sea basin using the SF6 signal observed there. Quantify the potential role of bottom boundary-layer mixing in the ventilation of the Greenland Sea Deep Water in absence of deep convection. Monitor the variability of the entrainment of water from the Greenland Sea using time series auto-sampler moorings at strategic positions i.e., sill of the Denmark Strait, Labrador Sea, Jan Mayen fracture zone and Fram Strait. Relate the observed variability of the tracer signal in the outflows to convection events in the Greenland Sea and local wind stress events. Obtain a better description of deepwater overflow and entrainment processes in the Denmark Strait and Faeroe Bank Channel overflows and use these to improve modelling of deepwater overflows. Monitor the tracer invasion into the North Atlantic using opportunistic SF6 measurements from other cruises: we anticipate that a number of oceanographic cruises will take place in the north-east Atlantic and the Labrador Sea. It should be possible to get samples from some cruises for SF6 measurements. Use process models to describe the spread of the tracer to achieve better parameterisation for three-dimensional models. One reason that these are so resistant to prediction is that our best ocean models are as yet some distance from being good enough, to predict climate and climate change.