...Christopher Smart.

The author's "A song to David".

A song to David, 1763.

"Facsimile printed from type", with reproduction of original t.-p.: A song to David. By Christopher Smart ... London, Printed for the author; and sold by Mr. Fletcher ... 1763.

Transactions.

Includes bibliographies: A bibliography of John Evelyn, by H. B. Wheatley: v.1, 77-90 -- Incunabula Virgiliana, comp. by W. A. Copinger: v.2, p.[123]-226. A list of books and papers on printers and printing, under the countries and towns to which they refer. Comp. by T. B. Reed: v.3, p.[81]-152 -- List of manuscripts and examples of metal and ivory bindings from the Bibliotheca Lindesiana: v.4. p.[213]-232 -- Bibliography of printing in Sicily, by R. S. Faber: v.5, p.209-211 -- A bibliography of the writings of Christopher Smart, with biographical references. By G. J. Gray: v.6, p.[269]-303 -- List of lace books, by E. F. Strange: v.7, p.219-246 -- Handlist of books in the library of the Bibliographical society: v.8, li p -- A bibliography of the Thoughts of Marcus Aurelius Antoninus, by J. W. Legg: v.10, p.[15]-81 -- The bibliography of Petronius, by S. Gaselee, with a Short-title handlist: v.10, p.[141]-233 -- A list of bibliographical books published since 1893. Comp. by R. A. Peddie: v.10, p.[235]-311 -- Richard Schilders and the English Puritans, by J. D. Wilson: v.11, p.[65]-134 -- The Schotts of Strassburg and their press, by S. H. Scott: v.11, p.[165]-188 -- Notes on English books printed abroad, 1525-48, by R. Steele: v.11, p.[189]-236 -- The romance of Amadis of Gaul, by H. Thomas: v.11, p.[251]-297 -- Notes on the bibliography of Pope, by G. A. Aitken: v.12, p.[113]-143 -- Road-books and itineraries bibliographically considered, by Sir H. G. Fordham: v.13, p.[29]-68 -- The Palmerin romances, by H. Thomas: v.13, p.[97]-144 -- Books on accountancy, 1494-1600, by C. Gordon: v.13, p.[145]-170 -- An agreement for bringing out the second Quignon breviary. Ed. by J.W. Legg: v. 13, p. [323]-348 -- Notes on the bibliography of Matthew Prior, by G. A. Aitken: v.14, p.[39]-68 -- The City printers [with partial list of titles of City official literature] by C. Welch: v.14, p.[175]-241.

The works of Horace : translated literally into English prose : for the use of those who are desirous of acquiring or recovering a competent knowledge of the Latin language /

Mode of access: Internet.

The works of Horace,

CBEL II.

The works of Horace /

Mode of access: Internet.

Om medel til saltpettersjuderiernes förbättring och upkomst i riket

Invocatio: M.G.H.

Strödde chemiske anmärkningar, til uplysning i svenska lagfarenheten

Invocatio: M.G.H.

Om bränwinets beskaffenhet, och medel at tilwärka det med sädens mästa besparing

Errata.

Strödde chemiske anmärkningar, i jurisprudentia opificiaria

Invocatio: I.G.N.

Om orsaker til Cumå krono lax och sik fiskets förminskning

Invocatio: I.G.V.N.

Totuus jumalisuteen yxikertaisesa ja perustetusa d. Lutheruxen Wähäisen catechismuxen selityxesä. Doctorilda E. Pontoppidanilda. Suomexi käätty. Ruotzin kielisestä toisesta ylöspanosta

Arkit: A-K8 L4.

Distribution of planktonic foraminifera in Pleistocene sediments of the New Jersey margin, NW Atlantic Ocean

Abundance records of planktonic foraminifera (>150 µm) from the upper 520 m of ODP Site 1073 (Hole 1073A, Leg 174A, 639 m water depth) have been integrated with SPECMAP-derived isotope stratigraphy, percentage of calcium carbonate, and coarse sediment fraction data in order to investigate the Pleistocene climatic history of the New Jersey margin. Six planktonic taxonomic groups dominate the foraminiferal assemblage at Site 1073: Neogloboquadrina pachyderma (d) (mean 33.8%), Turborotalita quinqueloba (18.5%), N. pachyderma (s) (18.4%), Globigerina bulloides group (11.4%), Globorotalia inflata group (9.4%), and Globigerinita glutinata (4.1%). Based on the distributions of these six foraminiferal groups, the Pleistocene section can be divided into three paleoclimatic intervals: Interval I (intermediate) corresponds to the Quaternary sediments from sequence boundary pp1 to the seafloor (79.5-0 mbsf; Emiliania huxleyi acme [85 ka] at 72 mbsf); Interval II (warm) occurs between sequence boundaries pp3 and pp1 (325-79.5 mbsf; last occurrence of Pseudoemiliania lacunosa [460 ka] at 330 mbsf); and Interval III (coldest) occurs between sequence boundaries pp4 and pp3 (520-325 mbsf; Calcareous nannofossils and dinocysts in proximity to pp4 indicate that the sedimentary record for 0.9-1.7 Ma is either missing altogether or highly condensed within the basal few meters of the section). Neogloboquadrina pachyderma (d) displays eight peaks of abundance which correlate, for the most part, with depleted delta18O values, increases in calcium carbonate percentages, low coarse fraction percentages, increased planktonic fragmentation (greater dissolution), and low N. pachyderma (s) abundances. These intervals are interpreted as representing warmer/interglacial conditions. Neogloboquadrina pachyderma (s) displays seven peaks of abundance which correlate, for the most part, with delta18O increases, decreases in calcium carbonate percentages, increases in coarse fraction percentages, and low N. pachyderma (d) abundances. These intervals are interpreted as representing cooler/glacial conditions. In Interval III, a faunal response to relative changes in sea-surface temperature is reflected by abundance peaks in Neogloboquadrina pachyderma (d), followed by Turborotalita quinqueloba and then N. pachyderma (s) (proceeding from warmest to coolest, respectively). This tripartite response is consistent with the oxygen isotope record and, although not as clear, also occurs in Intervals I and II. Six peaks/peak intervals of Globigerina bulloides abundance are closely matched by peaks in Globigerinita glutinata and occur within oxygen isotope stage (OIS) 2 (latter part) 3, 4, 5, 8, 9, 13(?), 14(?), and 15(?). We speculate that these intervals reflect increased upwelling and nutrient levels during both glacials and interglacials. Eight peak intervals of Globorotalia inflata show a general inverse correlation with G. bulloides and may reflect lowered nutrient and warmer surface waters.

Oxygen and carbon isotope data for benthic foraminifera from DSDP Site 94-608 and ODP Site 208-1264

Small biserial foraminifera were abundant in the early Miocene (ca. 18.9-17.2 Ma) in the eastern Atlantic and western Indian Oceans, but absent in the western equatorial Atlantic Ocean, Weddell Sea, eastern Indian Ocean, and equatorial Pacific Ocean. They have been assigned to the benthic genus Bolivina, but their high abundances in sediments without evidence for dysoxia could not be explained. Apertural morphology, accumulation rates, and isotopic composition show that they were planktic (genus Streptochilus). Living Streptochilus are common in productive waters with intermittent upwelling. The widespread early Miocene high Streptochilus abundances may reflect vigorous but intermittent upwelling, inducing high phytoplankton growth rates. However, export production (estimated from benthic foraminiferal accumulation rates) was low, possibly due to high regeneration rates in a deep thermocline. The upwelled waters may have been an analog to Subantarctic Mode Waters, carrying nutrients into the eastern Atlantic and western Indian Oceans as the result of the initiation of a deep-reaching Antarctic Circumpolar Current, active Agulhas Leakage, and vigorous vertical mixing in the Southern Oceans.