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Titlebook: Sea Surface Studies; A Global View R. J. N. Devoy Book 1987 R.J.N. Devoy 1987 Arctic Ocean.Coast.ocean.oceanography.sea level.stratigraphy

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The Impact and Application of Sea-surface Changes or long-term flooding and coastal submergence (Hoffman, 1985; Barth and Titus, 1984; Devoy, 1980). It is important, therefore, that consideration is given in this book to the factors responsible for coastal change and to the problems facing Man’s habitation of this dynamic environment.
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Ocean Volume Change and the History of Sea Waterase through geological time to that of essential constancy since condensation of the primeval atmosphere. Composition of the oceans through time also was the subject of a similar range of different views.
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Quaternary Sea-level Changes: Southern Hemisphere Data65; Veeh, 1966; Mesolella .., 1969). Some of the most important on-land sequences of coral terraces are in the Southern Hemisphere, with the majority in the Australasian region (Fig. 9.1). Consequently, this chapter will focus on this area, particularly for the analysis of sea-level variations in the last 160,000 years.
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Introduction: First Principles and the Scope of Sea-surface Studiesricus Erici (1625), who noted (in translation), ‘the water has been lowered in many places so that skerries and rocks that had been covered before, and no man had known the existence of, now are visible and appear high above the water’.
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Ocean Volume Change and the History of Sea Waterture should generally be good for the later Phanerozoic, where sea-floor spreading data provide a basis for estimating ocean volume changes, stratigraphic evidence for sea-level changes is quite widespread and marine evaporites and other deposits are indicators of ocean composition. However, reachin
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