Carte de la coste d'Arabie, Mer Rouge et Golfe de Perse: tirée de la Carte de l'Océan Oriental publiée en 1740 par Ordre de Mgr le Comte de Maurepas augmentée sur des remarques particulières et dressée sur des observations astronomiques = Kaart van de Kust van Arabië, de Roode-Zee en de Gulf van Persië Gemaakt na de Fransse-Kaart van den Ooster-Ocean uitgegeven A. 1740 op Bevel van den Hre Grave de Maurepas Vermeederd op byzondere Aanmerkingen, en geschikt volgens Sterrekundige-Waarnemingen

J. V. Schley.

A new map of the East India Isles: from the latest authorities

by John Cary.

Die Staaten von Südost=Europa: Rumänien, Serbien, Montenegro, Bulgarien, Kreta, Europ. Türkei, Griechenland

Redigiert v. Dr. K. Peucker ; Rudolph Maschek sculps ; Kartogr. Anst. v. Th. Bannwarth.

Das Kœnigreich Bosnien, und die Herzegovina (Rama) samt den angrœnzenden Provinzen von Croatien, Sclavonien, Temesvar, Servien, Albanien, Ragusa, und den Venetianischen Dalmatien

nach den militœrischen Handkarten des Prinzen Eugen der Grafen Khevenhüller, Marsigli und Pallavicini geographisch aufgetragen, und nach den zuverloessigsten Nachrichten, und Reisebeschreibungen berichtiget im Jahre 1788 von Herrn Maximilian Schimek ; J. Alberti Sculp. ; F. Müller Scrip.

The Turkish Empire in Europe, Asia, and Africa: dividid into all its governments, together with the other territories that are tributary to it, as also the dominions of ye Emperor of Marocco [sic] according to the newest and most exact observations

by H. Moll.

Karte der Kaukasus-Länder und der angränzenden Türkischen und Persischen Provinzen Armenien, Kurdistan, und Azerbeidjan

bearbeitet und gezeichnet von H. Kiepert.

General Charte der Laender Zwischen dem Schwarzen und Caspischen Meere: Circassien, Georgien, Armenien, Wüste von Astrachan und Caucasus hauptsoechlich die Grosse und Kleine Kabarda

Nach Russischen und and Handschriften entworsen Strasburg bey Joh. Georg Treuttel ; I. P. Kremer delin ; B. F. Leizelt sc.

Eastern Turkistan

specially prepared for the Foreign Department, from India ; published under direction of Colonel F. B. Longe, R. E., Surveyor General of India.

Fessae, et Marocchi Regna Africae celeberr

describebat Abrah. Ortelius.

Prof. C. Haussknecht's Routen im Orient 1865-1869: III. Kurdistan und Irak

nach dessen Originalskizzen redigirt von H. Kiepert.

Suspended matter on the meridional section in the Laptev Sea in August-September 1991

Suspended matter concentration along a meridian section from the Lena River delta to 78°N (~500 km) at ten stations from the surface to the bottom was studied with weight and optical (light attenuation index) techniques. At seven stations average residence time of suspended matter in surface waters was determined by the disequilibrium 234Th method. Average residence time of suspended matter in other depth intervals was calculated by regression dependence between the 234Th/238U ratio and suspended matter concentration. Differential and integral fluxes of suspended matter in the water column were also calculated. Nepheloid matter dominates in suspended matter composition in surface waters. Calculations indicate that, before being buried on the bottom, solid river run-off is resuspended 2.3 times (aver.). Redistribution of nepheloid suspended matter in the near-bottom layer results in formation of a strongly pronounced depocentre - an area of maximal discharge of solid river run-off within the Laptev Sea.

Raw data of SCADCP (self-contained Acoustic Doppler Current Profiler) from three moorings in the Eastern Weddell Sea, 2005-2008

The success of any efforts to determine the effects of climate change on marine ecosystems depends on understanding in the first instance the natural variations, which contemporarily occur on the interannual and shorter time scales. Here we present results on the environmental controls of zooplankton distribution patterns and behaviour in the eastern Weddell Sea, Southern Ocean. Zooplankton abundance and vertical migration are derived from the mean volume backscattering strength (MVBS) and the vertical velocity measured by moored acoustic Doppler current profilers (ADCPs), which were deployed simultaneously at 64°S, 66.5°S and 69°S along the Greenwich Meridian from February, 2005, until March, 2008. While these time series span a period of full three years they resolve hourly changes. A highly persistent behavioural pattern found at all three mooring locations is the synchronous diel vertical migration (DVM) of two distinct groups of zooplankton that migrate between a deep residence depth during daytime and a shallow depth during nighttime. The DVM was closely coupled to the astronomical daylight cycles. However, while the DVM was symmetric around local noon, the annual modulation of the DVM was clearly asymmetric around winter solstice or summer solstice, respectively, at all three mooring sites. DVM at our observation sites persisted throughout winter, even at the highest latitude exposed to the polar night. Since the magnitude as well as the relative rate of change of illumination is minimal at this time, we propose that the ultimate causes of DVM separated from the light-mediated proximal cue that coordinates it. In all three years, a marked change in the migration behaviour occurred in late spring (late October/early November), when DVM ceased. The complete suspension of DVM after early November is possibly caused by the combination of two factors: (1) increased availability of food in the surface mixed layer provided by the phytoplankton spring bloom, and (2) vanishing diurnal enhancement of the threat from visually oriented predators when the illumination is quasi-continuous during the polar and subpolar summer. Zooplankton abundance in the water column, estimated as the mean MVBS in the depth range 50-300 m, was highest end of summer and lowest mid to end winter on the average annual cycle. However, zooplankton abundance varied several-fold between years and between locations. Based on satellite and in situ data of chlorophyll and sea ice as well as on hydrographic measurements, the interannual and spatial variations of zooplankton mean abundance can be explained by differences in the magnitude of the phytoplankton spring bloom, which develops during the seasonal sea ice retreat. Whereas the vernal ice melt appears necessary to stimulate the blooming of phytoplankton, it is not the determinator of the blooms magnitude, its areal extent and duration. A possible explanation for the limitation of the phytoplankton bloom in some years is top-down control. We hypothesise that the phytoplankton spring development can be curbed by grazing when the zooplankton had attained high abundance by growth during the preceding summer.

A history of the Jewish people,

Includes bibliography.

Proceedings of the Geothermal Program Review VII, "DOE research and development for the geothermal marketplace" : March 21-23, 1989, San Francisco, CA /

"CONF-890352."

Geothermal innovative technologies catalog : submitted to the U.S. Department of Energy, San Francisco Operations Office /

"DOE/SF/16299-H1."