(1) Cephalopods from the Lower Part of the Cody Shale of Oregon Basin, Wyoming. pp. 1–19, pl. i–viii. Prof. Paper 150—A. - (2) The Scaphites, An Upper Cretaceous Ammonite Group. pp. 21–40, pl. ix–xi. Prof. Paper 150—B. - (3) The Cephalopods of the Eagle Sandston and Related Formations in the Western Interior of the United States. pp. 1–87, pl. i–xlv. Prof. Paper 151.

A. G. B.

doi:10.1017/S0016756800107769

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(1) Cephalopods from the Lower Part of the Cody Shale of Oregon Basin, Wyoming. pp. 1–19, pl. i–viii. Prof. Paper 150—A. - (2) The Scaphites, An Upper Cretaceous Ammonite Group. pp. 21–40, pl. ix–xi. Prof. Paper 150—B. - (3) The Cephalopods of the Eagle Sandston and Related Formations in the Western Interior of the United States. pp. 1–87, pl. i–xlv. Prof. Paper 151.

Volume 65, Issue 6
A. G. B.
DOI: https://doi.org/10.1017/S0016756800107769

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(1) Cephalopods from the Lower Part of the Cody Shale of Oregon Basin, Wyoming. pp. 1–19, pl. i–viii. Prof. Paper 150—A. - (2) The Scaphites, An Upper Cretaceous Ammonite Group. pp. 21–40, pl. ix–xi. Prof. Paper 150—B. - (3) The Cephalopods of the Eagle Sandston and Related Formations in the Western Interior of the United States. pp. 1–87, pl. i–xlv. Prof. Paper 151.

Volume 65, Issue 6
A. G. B.
DOI: https://doi.org/10.1017/S0016756800107769

To save this article to your Google Drive account, please select one or more formats and confirm that you agree to abide by our usage policies. If this is the first time you used this feature, you will be asked to authorise Cambridge Core to connect with your Google Drive account. Find out more about saving content to Google Drive.

(1) Cephalopods from the Lower Part of the Cody Shale of Oregon Basin, Wyoming. pp. 1–19, pl. i–viii. Prof. Paper 150—A. - (2) The Scaphites, An Upper Cretaceous Ammonite Group. pp. 21–40, pl. ix–xi. Prof. Paper 150—B. - (3) The Cephalopods of the Eagle Sandston and Related Formations in the Western Interior of the United States. pp. 1–87, pl. i–xlv. Prof. Paper 151.

Volume 65, Issue 6
A. G. B.
DOI: https://doi.org/10.1017/S0016756800107769

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