The Anglican Eucharist 1900-1967: an historical survey of the theological and liturgical developments during this period with particular reference to the catholic and evangelical wings of the Church of England

An historical survey of the theological and liturgical developments in this field in the Church of England with particular reference to the catholic and evangelical wings of the Church. Theories concerning Eucharistic Sacrifice are considered particularly those of the 'Heavenly Session' school of thought, Spens, Hicks, Mascall, and the conservative evangelicals together with the modifications of Lampe and C.F.D. Moule. Various semi-official doctrinal statements of the Church of England are also noted. Theories of Eucharistic Presence are also presented including those of O.C. Quick and William Temple in addition to those which could be more clearly distinguished as 'catholic' or 'evangelical'; an appendix relates all these theories to the practice of Reservation and Extra-liturgical Devotions. The theology of the Body of Christ, the Church, is considered in relationship to the Eucharist and with this the emerging theology of the laity. The rediscovery of the cosmic significance of the Eucharist is particularly noted in its relationship to current Roman Catholic and Orthodox thought. There is a survey of the Liturgical revision in the Church of England throughout this century with special reference to the question of Reservation, the 1927/8 Prayer Book debates and the emergence of Series II. Reference is made to the Liturgy of the Church of South India and revision throughout the Anglican Communion as a whole. These liturgical revisions are then placed in their background of the European Liturgical movement and the development of the Parish Communion Movement in the Church of England. Finally liturgy and theology are seen in relationship to ecclesiastical architecture, which is shown to have changed considerably to embody the new understanding of the Eucharist as corporate action and the Liturgy which has been designed to translate this into terms of worship

Compositional variations in calciturbidites and calcidebrites in response to sea-level fluctuations (Exuma Sound, Bahamas)

compositional variation of Pleistocene carbonate gravity deposits from the Exuma Sound Basin, Bahamas, was determined. Two types of gravity deposit were present in the cores of ODP Leg 101, Site 632A, i.e., calciturbidites and calcidebrites. In analogy with earlier studies, the compositional variations in the calciturbidites could be linked to different sources on the carbonate margin, i.e., platform interior, platform edge, and platform slope. Calciturbidites deposited during interglacial, sea-level highstands show a dominance of non-skeletal grains, largely derived from the platform interior, while calciturbidites of glacial, sea-level lowstands, show a dominance of skeletal platform-edge to platform-slope-derived grains. Thus, the calciturbidite composition can be used to reconstruct the position of absolute sea level. In addition, the mud content of the calciturbidites increased after Marine Isotope Stage 11. In contrast, the composition of the calcidebrites remained unaltered through time and showed a clear dominance of platform-edge-derived sediments during varying sea-level positions. The Bahamian carbonate platform is located in a tectonically stable passive-margin setting and the gravity-flow deposits were laid down in an environment exclusively controlled by eustatic sea-level fluctuations. This study shows that all types of gravity-induced carbonate deposits, calciturbidites, and calcidebrites, were deposited in response to global eustatic sea-level variations. The sediment composition could be linked directly to sediment input from specific facies realms along the carbonate platform margin. Hence, sediment composition analysis is a strong tool that may be used to discriminate between gravity-induced deposition triggered by eustatic sea-level changes and that related to tectonic events, when analyzing resedimentation processes in sedimentary basins.Geoscience & EngineeringCivil Engineering and Geoscience