Books on the topic 'Fossil Victoria'

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1

Flannery, Tim F. The Macropodoidea (Marsupialia) of the early Pliocene Hamilton local fauna, Victoria, Australia. Chicago, Ill: Field Museum of Natural History, 1992.

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2

International Echinoderm Conference (6th 1987 Victoria, B.C.). Echinoderm biology: Proceedings of the sixth International Echinoderm Conference, Victoria, 23-28 August 1987. Brookfield, The Netherlands: A.A. Balkema, 1988.

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3

Wellington), International Bryozoology Conference (10th 1995 Victoria University of. Bryozoans in space and time: Proceedings of the 10th International Bryozoology Conference, Victoria University of Wellington, Wellington, New Zealand, 1995. Wellington, N.Z: NIWA, 1996.

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4

International Symposium on Ostracoda. (11th 1991 Warrnambool, Victoria). Ostracoda in the earth and life sciences: Proceedings of the 11th International Symposium on Ostracoda : Warrnambook, Victoria, Australia, 8-12, July 1991. Rotterdam: A.A. Balkema, 1993.

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5

S, Sarjeant William Antony, ed. The tracks of Triassic vertebrates: Fossil evidence from North-West England. London: The Stationery Office, 1997.

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6

Congress of the International Council for Archaeozoology. (8th 1998 Victoria, Canada). Dogs through time: An archaeological perspective : proceedings of the 1st ICAZ Symposium on the History of the Domestic Dog : eighth congress of the International Council for Archaeozoology (ICAZ98), August 23-29, 1998, Victoria, B.C., Canada. Oxford: Archeopress, 2000.

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7

J, Crockford Susan, and International Council for Archaeozoology. Congress, eds. Dogs through time: An archaeological perspective ; proceedings of the 1st ICAZ Symposium on the History of the Domestic Dog ; Eighth Congress of the International Council for Archaeozoology (ICAZ98), August 23-29, 1998, Victoria, B.C., Canada. Oxford: Archaeopress, 2000.

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8

Men among the mammoths: Victorian science and the discovery of human prehistory. Chicago: University of Chicago Press, 1993.

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9

Stephen, McLoughlin, ed. Early Cretaceous (Neocomian) flora and fauna of the Lower Strzelecki Group, Gippsland Basin, Victoria. Canberra: Association of Australasian Palaeontologists, 2002.

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10

Lambert, P., Ross David Burke, and P. V. Mladenov. Echinoderm Biology: Proceedings of the Sixth International Echinoderm Conference, Victoria, 23-28 August 1987. Aa Balkema, 1988.

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11

Bryozoans in space and time: Proceedings of the 10th International Bryozoology Conference, Victoria University of Wellington, Wellington, New Zealand, 1995. NIWA, 1996.

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12

Murdoch, John, Victoria and Albert museum., and Geoffrey Tresise. Seventeenth-century English Miniatures in the Collection of the Victoria and Albert Museum. Stationery Office Books (TSO), 1997.

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13

Murdoch, John, Victoria and Albert museum, and Geoffrey Tresise. Seventeenth-century English Miniatures in the Collection of the Victoria and Albert Museum. Stationery Office Books (TSO), 1997.

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14

A, Jell P., Roberts J, and Association of Australasian Palaeontologists, eds. Plants and invertebrates from the Lower Cretaceous Koonwarra Fossil Bed, South Gippsland, Victoria. Sydney, Australia: Association of Australasian Palaeontologists, 1986.

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15

Jones, Chris. Fossil Poetry. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198824527.001.0001.

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Fossil Poetry provides the first book-length overview of the place of Anglo-Saxon in nineteenth-century poetry in English. It addresses the use of Anglo-Saxon as a resource by Romantic and Victorian poets in their own compositions, as well as the construction and ‘invention’ of Anglo-Saxon in and by nineteenth-century poetry. Fossil Poetry takes its title from a famous passage on ‘early’ language in the essays of Ralph Waldo Emerson, and uses the metaphor of the fossil to contextualize poetic Anglo-Saxonism within the developments that had been taking place in the fields of geology, palaeontology, and the evolutionary life sciences since James Hutton’s apprehension of ‘deep time’ in his 1788 Theory of the Earth. Fossil Poetry argues that two phases of poetic Anglo-Saxonism took place over the course of the nineteenth century: firstly, a phase of ‘constant roots’ whereby Anglo-Saxon is constructed to resemble, and so aetiologically to legitimize, a tradition of English Romanticism conceived as essential and unchanging; secondly, a phase in which the strangeness of many of the ‘extinct’ philological forms of early English is acknowledged, and becomes concurrent with a desire to recover and recuperate the fossils of Anglo-Saxon within contemporary English poetry. A wide range of eighteenth- and nineteenth-century works of antiquarianism, philology, and Anglo-Saxon scholarship forms the evidential base that underpins the advancement of these two models for understanding the place of Anglo-Saxon in nineteenth-century poetry. New archival research and readings of unpublished papers by Tennyson, Whitman, and Morris is also presented here for the first time.
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16

Desmond, Adrian. Archetypes and Ancestors: Palaeontology in Victorian London, 1850-1875. University Of Chicago Press, 1986.

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17

Beerling, David. The Emerald Planet. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780192806024.001.0001.

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Global warming is contentious and difficult to measure, even among the majority of scientists who agree that it is taking place. Will temperatures rise by 2ºC or 8ºC over the next hundred years? Will sea levels rise by 2 or 30 feet? The only way that we can accurately answer questions like these is by looking into the distant past, for a comparison with the world long before the rise of mankind. We may currently believe that atmospheric shifts, like global warming, result from our impact on the planet, but the earth's atmosphere has been dramatically shifting since its creation. This book reveals the crucial role that plants have played in determining atmospheric change - and hence the conditions on the planet we know today. Along the way a number of fascinating puzzles arise: Why did plants evolve leaves? When and how did forests once grow on Antarctica? How did prehistoric insects manage to grow so large? The answers show the extraordinary amount plants can tell us about the history of the planet -- something that has often been overlooked amongst the preoccuputations with dinosaur bones and animal fossils. David Beerling's surprising conclusions are teased out from various lines of scientific enquiry, with evidence being brought to bear from fossil plants and animals, computer models of the atmosphere, and experimental studies. Intimately bound up with the narrative describing the dynamic evolution of climate and life through Earth's history, we find Victorian fossil hunters, intrepid polar explorers and pioneering chemists, alongside wallowing hippos, belching volcanoes, and restless landmasses.
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