1 |
Zooplankton community structure in Southampton Water and its potential response to estuary chronic oil pollutionZinger, Irene January 1989 (has links)
No description available.
|
2 |
The local port book of Southampton for 1439-40 /Cobb, Henry Stephen, January 1961 (has links)
Texte remanié de: Th.--Master of arts--University of London, 1957. / Contient le texte des registres du port de Southampton de 1439 à 1440 (manuscrit conservé aux Archives de Southampton). Bibliogr. p. 112-115. Glossaire. Index.
|
3 |
Slave insurrections in Virginia (1830-1865)Drewry, William Sidney, January 1900 (has links)
Thesis (Ph. D.)--Johns Hopkins University, 1900. / Vita. Lettered on cover: The Southampton insurrection.
|
4 |
Slave insurrections in Virginia (1830-1865)Drewry, William Sidney, January 1900 (has links)
Thesis (Ph. D.)--Johns Hopkins University, 1900. / Vita. Lettered on cover: The Southampton insurrection.
|
5 |
Carbonate Sedimentology and Diagenesis of an Upper Ordovician Sponge-microbe-cement Mound on Southampton Island, Nunavut, CanadaCastagner, Ariane January 2016 (has links)
The Hudson Bay Basin is the largest intracratonic basin in North America, but remains a frontier area for our knowledge of its stratigraphy and sedimentology and its hydrocarbon potential. Large domal reefs (up to 10 m thick and 500 m wide) in the Upper Ordovician Red Head Rapids Formation on Southampton Island developed on the margin of this shallow-marine evaporitic basin in which physical and chemical seawater parameters were distinct from the open ocean and in which a diverse community of reef-building and dwelling metazoans was unable to flourish.
The main reef facies comprise boundstone and cementstone composed of various proportions of early-calcified sponge tissues, microbial encrusters, synsedimentary cement and small colonial metazoans. The accretionary mechanisms of the Red Head Rapids reefs were mainly the result of framebuilding by early-calcified sponges and small colonial corals and binding by calcimicrobial elements for the boundstone facies, and of massive aragonitic cement precipitation near the seafloor for the cementstone facies. These Upper Ordovician reefs, in which microbialites dominate but coexist with metazoans, were more widespread in the Early Ordovician
immediately prior to the Middle to Late Ordovician expansion of skeletal-dominant reefs. The Upper Ordovician reefs on Southampton Island, porous and locally bitumen impregnated, underwent early marine, near-surface and progressive burial diagenesis; reducing its primary porosity but significantly increasing its secondary porosity. They represent one of the major untested petroleum play types identified in the Hudson Bay Basin.
|
6 |
The french-speaking reformed community and their church in Southampton : 1567-c.1620 /Spicer, Andrew Paul. January 1997 (has links)
Texte remanié de: Doctoral thesis--Southampton--University, 1994.
|
7 |
Town defences in early modern EnglandDawson, Keith January 1995 (has links)
No description available.
|
8 |
Nat Turner's slave rebellion Together with the full text of the so-called "confessions" of Nat Turner made in prison in 1831.Aptheker, Herbert, January 1900 (has links)
Thesis (M.A.)--Columbia University. / Bibliography: p. 111-125.
|
9 |
Nat Turner's slave rebellion Together with the full text of the so-called "confessions" of Nat Turner made in prison in 1831.Aptheker, Herbert, January 1900 (has links)
Thesis (M.A.)--Columbia University. / Bibliography: p. 111-125.
|
10 |
Remembering Nat Turner : the rebellious slave in American thought, 1831 to present /French, Scot Andrew. January 2000 (has links)
Thesis (Ph. D.)--University of Virginia, 2000. / Includes bibliographical references (leaves 565-602). Also available online through Digital Dissertations.
|
Page generated in 0.0348 seconds