King Horn, with fragments of Floriz and Blauncheflur, and of the Assumption of Our Lady, from a ms. (G G.4.27.2.) in the Cambridge University Library. Also, from mss. in the British Museum, the Assumption of Our Lady (add. mss. 10036), and fragments of the Floyres and Blancheflur (Cotton Vitellius D. III)

This number was re-edited from the manuscript in 1901 by George H. McKnight.

Treaty of peace between His imperial and Catholick Majesty Charles VI, and His royal Catholic Majesty Philip V, concluded at Vienna the 30th of April 1725. Treaty of Commerce between His imperial and Catholick Majesty Charles VI, and His royal Catholick Majesty Philip V, concluded at Vienna, May 1, 1725. Treaty between the King of Great Britain, the most Christian King, and the King of Prussia, made at Hanover the 3rd of September, 1725 [microform].

Text in English and Latin, and English and French, in parallel columns.

Peftjauawybast, king of Nen-nesut : genealogy, art history, and the chronology of late libyan Egypt

This paper argues in detail for the identification of Peftjauawybast, King of Nen-nesut (fl. 728/720 BC ), with Peftjauawybast, High Priest of Ptah in Memphis (fl. c. 790–780 BC2), known from the Apis stela of year 28 of Shoshenq III. This identification ties in with a significant lowering of the accepted dates for the kings from Shoshenq III, Osorkon III and Takeloth III to Shoshenq V, and the material culture associated with them. Such a shift seems to be supported by stylistic and genealogical evidence. As a consequence, it is further suggested that the Master of Shipping at Nen-nesut, Pediese i, was perhaps related by descent and marriage to the family of the High Priests of Memphis and King Peftjauawybast.

Late Quaternary history of North Eurasian Norway spruce ( Picea abies ) and Siberian spruce ( Picea obovata ) inferred from macrofossils, pollen and cytoplasmic DNA variation

Aim We used combined palaeobotanical and genetic data to assess whether Norway spruce (Picea abies) and Siberian spruce (Picea obovata), two major components of the Eurasian boreal forests, occupied separate glacial refugia, and to test previous hypotheses on their distinction, geographical delimitation and introgression. Location The range of Norway spruce in northern Europe and Siberian spruce in northern Asia. Methods Pollen data and recently compiled macrofossil records were summarized for the Last Glacial Maximum (LGM), late glacial and Holocene. Genetic variation was assessed in 50 populations using one maternally (mitochondrial nad1) and one paternally (chloroplast trnT–trnL) inherited marker and analysed using spatial analyses of molecular variance (SAMOVA). Results Macrofossils showed that spruce was present in both northern Europe and Siberia at the LGM. Congruent macrofossil and pollen data from the late glacial suggested widespread expansions of spruce in the East European Plain, West Siberian Plain, southern Siberian mountains and the Baikal region. Colonization was largely completed during the early Holocene, except in the formerly glaciated area of northern Europe. Both DNA markers distinguished two highly differentiated groups that correspond to Norway spruce and Siberian spruce and coincide spatially with separate LGM spruce occurrences. The division of the mtDNA variation was geographically well defined and occurred to the east of the Ural Mountains along the Ob River, whereas the cpDNA variation showed widespread admixture. Genetic diversity of both DNA markers was higher in western than in eastern populations. Main conclusions North Eurasian Norway spruce and Siberian spruce are genetically distinct and occupied separate LGM refugia, Norway spruce on the East European Plain and Siberian spruce in southern Siberia, where they were already widespread during the late glacial. They came into contact in the basin of the Ob River and probably hybridized. The lower genetic diversity in the eastern populations may indicate that Siberian spruce suffered more from past climatic fluctuations than Norway spruce.

Jesus of Nazareth in the light of Jewish and Christian thought and history : a sunday lecture delivered January 10, 1926

by Samuel H. Goldenson

Age determination and grwoth rates of stalagmites and stalactites from the Okshola cave, Fauske, northern Norway

The sensitivity of terrestrial environments to past changes in heat transport is expected to be manifested in Holocene climate proxy records on millennial to seasonal timescales. Stalagmite formation in the Okshola cave near Fauske (northern Norway) began at about 10.4 ka, soon after the valley was deglaciated. Past monitoring of the cave and surface has revealed stable modern conditions with uniform drip rates, relative humidity and temperature. Stable isotope records from two stalagmites provide time-series spanning from c. 10380 yr to AD 1997; a banded, multi-coloured stalagmite (Oks82) was formed between 10380 yr and 5050 yr, whereas a pristine, white stalagmite (FM3) covers the period from ~7500 yr to the present. The stable oxygen isotope (delta18Oc), stable carbon isotope (delta13Cc), and growth rate records are interpreted as showing i) a negative correlation between cave/surface temperature and delta18Oc, ii) a positive correlation between wetness and delta13Cc, and iii) a positive correlation between temperature and growth rate. Following this, the data from Okshola show that the Holocene was characterised by high-variability climate in the early part, low-variability climate in the middle part, and high-variability climate and shifts between two distinct modes in the late part. A total of nine Scandinavian stalagmite delta18Oc records of comparable dating precision are now available for parts or most of the Holocene. None of them show a clear Holocene thermal optimum, suggesting that they are influenced by annual mean temperature (cave temperature) rather than seasonal temperature. For the last 1000 years, delta18Oc values display a depletion-enrichment-depletion pattern commonly interpreted as reflecting the conventional view on climate development for the last millennium. Although the delta18Oc records show similar patterns and amplitudes of change, the main challenges for utilising high-latitude stalagmites as palaeoclimate archives are i) the accuracy of the age models, ii) the ambiguity of the proxy signals, and iii) calibration with monitoring data.

Letters of William III. and Louis XIV. and their ministers; illustrative of the domestic and foreign politics of England, from the peace of Ryswick to the accession of Philip V. of Spain, 1697 to 1700.

With appendix of treaties and documents.

Memoirs of the life and reign of King George the Third /

Mode of access: Internet.

[The] most important transactions of the sixth session of the First Parliament of His Majesty King George II. anno domini, MDCCXXXIII : containing ... also in this pamphlet are inserted, The Lords protests in the said session of Parliament : and a compleat list of all those gentlemen of the House of Commons as voted for or against the late excise-bill ... .

Goldsmiths'-Kress no. 07160.0-4.

Memoirs of King Richard the Third and some of his contemporaries, with an historical drama on the battle of Bosworth.

Mode of access: Internet.

The troublesome raigne of John, king of England. The first quarto, 1591, which Shakspere rewrote (about 1595) as his "Life and death of King John"...

"Forewords" to pt. II contain extracts from the sources of the play(Hall's and Holinshed's chronicles) : p. iii-xxxviii.

The autobiography and correspondence of Mary Granville, Mrs. Delany : with interesting reminiscences of King George the Third and Queen Charlotte /

Mode of access: Internet.

The autobiography and correspondence of Mary Granville, Mrs. Delany : with interesting reminiscences of King George the Third and Queen Charlotte /

Mode of access: Internet.

Travels in Denmark, Sweden, and Norway.

Mode of access: Internet.

The tragedie of King Richard the third : contayning his treacherous plots against his brother Clarence: the pittifull murder of his innocent nephewes: his tyrannicall vsurpation: with the whole course of his detested life, and most deserued death. As it hath been lately acted by the kings maiesties seruants /

Mode of access: Internet.