319 resultados para Aristichthys nobilis
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Marca tip. del editor en v6r (Kristeller. It.B., 281)
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Sign.: A-S8, T6
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Pie de imp. tomado del colofón en 2K2r
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Marca tip. en A7v
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Pie de imp. tomado del colofón
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Pie de imp. tomado del colofón
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Pie de imp. tomado del colofón
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Capitulares grab. xil.
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Sign.: A4
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This layer is a georeferenced raster image of the historic paper map entitled: Gandavum amplissima Flandriae urbs à Julio Caesare condita, et à suo nomine Caio ut chronici Brabantini loquuntur dicta, fluminibus nobilis amoena, ampla, spaciosa, nunque conclusa, nusque suffocata. It was published by J. Janssonius in 1657. Scale [ca. 1:9,000]. Covers a portion of Gent, Belgium. Map in Latin. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Belgian Lambert 1972 coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads, drainage, built-up areas and selected buildings, fortifications, ground cover, and more. Includes also text and index.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.
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Six sites (759-764) were drilled on the Exmouth Plateau during Ocean Drilling Program Leg 122. Nannofossilrich Cenozoic sediments were recovered at all six sites, reflecting the open-ocean conditions that prevailed over the Exmouth Plateau during the Cenozoic. Calcareous nannofossils are abundant, diverse (250 different species identified), and generally well preserved throughout the composite lower Paleocene to Quaternary section. The diversity and preservation of nannofossils permits a high degree of stratigraphic resolution at each site. Site 762 on the central part of the Exmouth Plateau contains an almost unbroken Cenozoic record (only Miocene Zones NN3, NN8, and NN10 are missing). This site may prove to be a useful Cenozoic biostratigraphic and biomagnetochronologic reference section for the eastern Indian Ocean.