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Date: 2011-05-06 05:45:41 James Ross Island group Graham Land Sobral Formation Seymour Island Bertodano Bay Lopez de Bertodano Formation Maastrichtian Sobral Concretion Geography of Antarctica Geologic time scale Phanerozoic		Bookman Old Style Negreta cursiva Add to Reading List Source URL: s3.amazonaws.com Download Document from Source Website File Size: 4,01 MB Share Document on Facebook

	Tertiary boundary. Over much of this section it was possible to collect at 1.5-meter intervals; for most of the remainder, we could collect at 3-meter intervals. Cretaceous strata (Lopez de Bertodano Formation) cropping DocID: 158XU - View Document
	Recent advances in the systematics and distribution of fossil lobsters from the Cretaceous and Paleocene of James Ross Basin, Antarctica - DocID: 14zWP - View Document
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	Changes in the macrofossil faunas at the end of the cretaceous on Seymour Island, Antarctic Peninsula I DocID: 14iWG - View Document
	include bivalves, gastropods, echinoderm spines, and abundant wood. This work was supported by National Science Foundation grant DPPReferences Andersson, J. Con the geology of Graham Land. Bulletin of DocID: 14iCu - View Document