Lopez de Bertodano Formation

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1Tertiary 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

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

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Language: English - Date: 2011-05-06 05:46:01
2Recent advances in the systematics and distribution of fossil lobsters from the Cretaceous and Paleocene of James Ross Basin, Antarctica  -

Recent advances in the systematics and distribution of fossil lobsters from the Cretaceous and Paleocene of James Ross Basin, Antarctica -

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Language: English - Date: 2011-05-06 07:06:46
3Bookman Old Style Negreta cursiva

Bookman Old Style Negreta cursiva

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Language: English - Date: 2011-05-06 05:45:41
4Changes in the macrofossil faunas at the end of the cretaceous on Seymour Island, Antarctic Peninsula I

Changes in the macrofossil faunas at the end of the cretaceous on Seymour Island, Antarctic Peninsula I

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Language: English - Date: 2011-05-06 05:14:24
5include 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

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

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Language: English - Date: 2011-05-06 05:45:54
6Decapod crustaceans from James Ross Island, Antarctica JAMES ROSS	  RODNEY M. FELDMAN

Decapod crustaceans from James Ross Island, Antarctica JAMES ROSS RODNEY M. FELDMAN

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Language: English - Date: 2011-05-06 21:18:10
7Alvarez, W., L.W. Alvarez, F. Asaro, and H.V. MichelThe end of the Cretaceous: Sharp boundary or gradual transition? Science, 223, Bohor, B.F., E.E. Foord, P.J. Modreski, and D.M. TriplehornMin

Alvarez, W., L.W. Alvarez, F. Asaro, and H.V. MichelThe end of the Cretaceous: Sharp boundary or gradual transition? Science, 223, Bohor, B.F., E.E. Foord, P.J. Modreski, and D.M. TriplehornMin

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Language: English - Date: 2011-05-06 22:21:46
8stranding event. The only published accounts of extensive accumulations are limited to (1) Iredalewho reported observing over 100 broken shells on a beach near Cape Bedford, North Queensland; (2) Hamadain

stranding event. The only published accounts of extensive accumulations are limited to (1) Iredalewho reported observing over 100 broken shells on a beach near Cape Bedford, North Queensland; (2) Hamadain

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Language: English - Date: 2011-05-06 22:21:51
9Feldmann, R.M., and W.J. ZinsmeisterFossil crabs (Decapoda: Brachyura) from the La Meseta Formation (Eocene) of Antarctica: Paleoecological and biogeographic implications. Journal of Paleontology, 58(4),

Feldmann, R.M., and W.J. ZinsmeisterFossil crabs (Decapoda: Brachyura) from the La Meseta Formation (Eocene) of Antarctica: Paleoecological and biogeographic implications. Journal of Paleontology, 58(4),

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Language: English - Date: 2011-05-06 07:41:06
10____  Figure 2. Cockburn Island, Antarctic Peninsula. Seymour Island in background. View to the southeast.  sequence exposed along one of the small gullies at the south end

____ Figure 2. Cockburn Island, Antarctic Peninsula. Seymour Island in background. View to the southeast. sequence exposed along one of the small gullies at the south end

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Language: English - Date: 2011-05-06 15:40:53