Karoli Magni et Lvdovici pii christianiss. regvm et impr. Francorum capitvla sive leges ecclesiasticae et civiles ab Ansegiso ... & Benedicto Leuita collecte libris septem ...

Mode of access: Internet.

Concilium Aschaimense sub Tassilone II., Duce Bajoariae, anno reparatae salutis DCCLXIII. celebratum. ...

Mode of access: Internet.

Williram's Uebersetzung und Auslegung des Hohenliedes,

Codex vratislaviensis and Codex lugdunensis on opposite pages numbered in duplicate vi-lxxviii and 6-78.

Éloge de Suger, abbé de Saint-Denis, ministre d'Etat, et régent du royaume, sous le règne de Louis le jeune : discours qui a remporté le prix au jugement de l'Académie françoise en 1779 /

With: Suger, moine de Saint-Denis. [S.l. : s.n., 1779].

Miscellanies, relating to Lancashire and Cheshire.

Includes index.

Gesta abbatum fontanellensium.

Also published under title: Chronicon fontanellensis abbatiae.

Die angelsächsischen prosabearbeitungen der Benedictiner-regel.

Translation attributed to St. Æthelwold, bishop of Winchester.

Chronica Jocelini de Brakelond, de rebus gestis Samsonis abbatis monasterii Sancti Edmundi.

"Genealogia de Cokefield": p. 144-145.

Un traité de la vie solitaire. Epistola ad fratres de Monte-Dei.

Attributed to Bernard de Clairvauv, Peter Cellensis and Guigues du Chastel.

De corpore et sanguine dominii : cum appendice epistola ad fredugardum /

Mode of access: Internet.

Sedimentological investigations and age constraints of sediment cores from the outer Abbot trough, Amundsen Sea shelf

Knowing the extent of the West Antarctic Ice Sheet (WAIS) at the Last Glacial Maximum (LGM) is crucial for initiating and calibrating numerical ice sheet models that can predict future ice-sheet change and contributions to sea level. However, empirical data are lacking for key areas of outer continental shelves, where the LGM-WAIS must have terminated. We present detailed marine geophysical and geological data documenting an up to ~12 m-thick sequence of glaciomarine sediments within a relict glacial trough in the outer parts of the Amundsen Sea Embayment. Continuous deposition must have persisted here since at least >40 ka BP, pre-dating the established LGM by >13,000 years. Observations constrain the LGM grounding line to a distinct grounding-zone wedge ~100 km inland from the continental shelf edge. Thus, a substantial shelf area (~6000 km**2) remained ice free through the last glacial cycle.