Histoire romaine depuis la fondation de Rome ... /

Mode of access: Internet.

D. Phlippi Parentii ... De rebus ad Ambianum principale Picardiae oppidum gestis anno 1597, missa ad Patricium Sellensem ...

Mode of access: Internet.

Rudimentos, formaciones y evoluciones de las Armadas, ó sea, Táctica naval /

Mode of access: Internet.

Cantique des cantiques /

Mode of access: Internet.

Refutatio elenchi calendarii gregoriani a Setho Calvisio conscripti : et opera Dauidis Origani editi: qua libris quatuor Calendarium Gregorianum vere Ecclesiasticum /

Mode of access: Internet.

Opus morale in praecepta decalogi /

Explicatio mandati secundi decalogi / per patrem Thomas Sanchez ..., p. 605-1287, con port. propia siendo el pie de imp.: Madriti : praelo [et] expensis Ludouici Sanchez ..., 1613.

Management and program audit of the Parents Too Soon Program.

"August 1990."

Emilius; or, A treatise of education. /

Includes index.

The angler; : a poem, in ten cantos. Comprising proper instructions in the art, with rules to choose fishing rods, lines, hooks, floats, baits, and to make artificial flies; receipts for pastes, &c. &c. Embellished with upwards of twenty beautiful wood-cuts. /

References: Westwood, T. Bibliotheca piscatoria, p. 131.

Anecdotes du sejour du roi de Suede a Bender, ou, Lettres de Mr. le baron de Fabrice pour servir d'eclaircissement a l'histoire de Charles XII.

Signatures: *⁴ A-D⁸ E⁸(E2 unsigned, E5 signed E4) F-X⁸ Y⁴

R.P. Jacobi Tirini ... In universam Sacram Scripturam commentarius.

Mode of access: Internet.

Informe anual

Report year ends June 30, 1905

Uebersetzung des Buchs Massoreth Hammassoreth

unter Aufsicht und mit Anmerkungen D. Joh. Salomo Semlers ; [Verfasser: Elias Levita ben Asher ; Übersetzer: Christian Gottlob Meyer]

Quarternary tephra layers in sediment cores from the Bellingshausen Sea and Scotia Sea

The Southern Ocean is a region of the world's ocean which is fundamental to the generation of cold deep ocean water which drives the global therrno-haline circulation. Previous investigations of deep-sea sediments south of the Polar Front have been significantly constrained by the lack of a suitable correlation and dating technique. In this study, deep-sea sediment cores from the Bellingshausen, Scotia and Weddell seas have been investigated for the presence of tephra layers. The major oxide and trace element composition of glass shards have been used to correlate tephra isochrons over distances in excess of 600 km. The source volcanoes for individual tephra layers have been identified. Atmospheric transport distances greater than 1500 km for >32 pm shards are reported. One megascopic tephra is identified and correlated across 7 sediment drifts on the continental rise in the Bellingshausen Sea. Its occurrence in a sedimentary unit that has been biostratigraphically dated to delta 18O substage 5e identifies it as a key regional marker horizon for that stage. An unusual bimodal megascopic ash layer erupted from Deception Island, South Shetland Islands, has been correlated between 6 sediment cores which form a 600 km NE-SW transect from the central Scotia Sea to Jane Basin. This megascopic ash layer has been 14C dated at c. 10,670 years BP. It represents the last significant input of tephra into the Scotia Sea or Jane Basin from that volcano and forms an important early Holocene marker horizon for the region. Five disseminated tephras can be correlated to varying extents across the central Scotia Sea cores. Together with the megascopic tephra they form a tephrostratigraphic framework that will greatly aid palaeoclimatic, palaeoenvironrnental and palaeoceanographic investigations in the region.

(Table 1) Radiocarbon ages of core AB01/94 obtained in the Tromper Wiek, western Baltic Sea

In the Tromper Wiek northeast of Rügen, acoustical investigations using Air Gun, Boomer, Chirp Sonar and Sediment-Echosounder were carried out. Together with sediment core information, it allowed the identification of five seismostratigraphic units (E1 to E5). Conventional and AMS-14C-datings supported their chronostratigraphical classification. The uppermost till (E1) was incised by late glacial channels filled with glaciolacustrine sediments (E2) of the early Baltic Ice Lake stages. These were regionally overlain with a sharp unconformity by a thick (locally >20 m) sedimentary complex (E3) of acoustically laminated silts of freshwater origin. This lower part of the E3-complex (E3a) is overlain by fluvial to coastal silty fine sands (E3b) deeper towards the Arkona Basin. Fine plant debris in the uppermost part of sub-unit E3a yielded ages of 10,100 and 10,500 14C-years B.P., representing the final phase of the Baltic Ice Lake. The fine sands of sub-unit E3b were deposited after the final drainage of the Baltic Ice Lake. In the shallower central part of the bay, the silts of sub-unit E3a were covered by a younger unit (E4) of fine sand with plant debris. A sedge peat occurring at the basis of unit E4 yielded an age of 9,590 14C-years B.P. The fine sands overlying the unit E3 in the central part of Tromper Wiek were deposited in the Ancylus Lake. Their position at about 20 m below present sea level (b.s.l.) reflects the maximum highstand in this area. The character and distribution of the Early Holocene deposits at greater depth suggest a lake water level at about 30 m b.s.l. after this highstand. Below 25 m b.s.l. muddy Littorina Sea sediments are observed. The thickness of these muds and sandy muds increases gradually towards the Arkona Basin. Locally, they are found in a channel-like structure immediately north of Jasmund.