GEOLOGY AND PALEONTOLOGY OF CANAL ZONE 1918. Canu, Ferdinand, and Bassler, R. S., Bryozoa of the Canal Zone and related areas: Idem, p. 117-122, pl. 53. Two species from Emperador limestone [member of Culebra formation]. Reissued in complete volume, 1919. 1918. Rathbun, M. J., Decapod crustaceans from the Panama region: Idem, p. 123-184, pls. 54-66. Species from Caimito [misidentified as Culebra], Culebra, and Gatun formations, and Pleistocene strata. Reissued in complete volume, 1919. 1918. Pilsbry, H. A., Cirripedia from the Panama Canal Zone: Idem, p. 185-188, pl. 67. Five species from so-cllled Pliocene [Alhajuela sandstone member of Caimito formation], Gatun formation, and Pleistocene strata. Reissued in complete volume, 1919. 1919. Vaughan, T. W., Contributions to the geology and paleontology of the Canal Zone, Panama, and geologically related areas in Central America and the West Indies: U. S. Natl. Mus. Bull. 103, 612 p., 154 pls., 27 figs. Separate parts of this volume are listed in present bibliography as 1918 or 1919 items. 1919. Vaughan, T. W., Fossil corals from Central America, Cuba, and Porto Rico, with an account of the American Tertiary, Pleistocene, and Recent coral reefs: Idem, p. 189-524, pis. 68-152, figs. 4-25. Species front Caimito formation [misidentified as Culebra formation and Emperador limestone member], Culebra formation and Emperador limestone member, and La Boca marine member of Panamd formation [misidentified as Emperador limestone member of Culebra formation] are described, and species from Pleistocene strata are listed. 1919. MacDonald, D. F., The sedimentary formations of the Panama Canal Zone, with special reference to the stratigraphic relations of the fossiliferous beds: Idem, p. 525-545, pls. 153, 154, figs. 26, 27. The name "Ciagres sandstone" is proposed. Aside from that new name and slight changes in some age assignments, discussion of stratigraphy is essentially similar to that in MacDonald's 1915 account. Includes measured stratigraphic sections. 1919. Vaughan, T. W., The biologic character and geologic correlation of the sedimentary formations of Panama in their relation to the geologic history of Central America and the West Indies: Idem, p. 547-612. Paleontology, age, and correlation of formations in Canal Zone. 1919. Sears, J. D., Deposits of manganese ore near Boqueron River, Panama: U. S. Geol. Survey Bull. 710, p. 85-91, figs. 1-3. Manganese prospects near Rio Boquer6n. Southernnost prospect is shown on plate 1 of present report. 1921. Berry, E. W., A palm nut from the Miocene of the Cana Zone: U. S. Natl. Mus. Proc., v. 59, p. 21-22, 3 figs. Found in Gatun formation. 1921. Cooke, C. IV., Orthaulax, a Tertiary guide fossil: UT. S. Geol. Survey Prof. Paper 129, p. 23-37, pls. 2-5. Orthaulax gabbi is recorded from Caimito formation [not so specified] and Culebra formation. 1922. Olsson, A. A., The Miocene of northern Costa Rica:: Bull. Am. Paleontology, v. 9, no. 39, 309 p., 32 pis., Includes mollusks from Gatun formation of Canal I Zone and one species from Toro limestone member. of Chagres sandstone (Pecten macdonaldi). 1923. Vaughan, T. W., Studies of the larger Tertiary foraminifera from tropical and subtropical America: Natl. Acad. Sci. Proc., v. 9, p. 253-257. Includes Lepidocyclina miraflorensis from a incality, apparently now submerged, evidently representing La Boca marine member of Panamd formation. 1924. Hanna, G. D., Rectifications of nomenclature: Calif. Acad. Sci. Proc., 4th ser., v. 13, p. 151-186. Three new names are proposed for Canal Zone fossil mollusks. 1924. National Academy of Sciences, Report of the Committee of the National Academy of Sciences on Panama Canal Slides: Natl. Acad. Sci. M~em., v. 18, 84 p., 51 pls., 19 figs. Appendix B on geology, by MacDonald, includes structure sections of part of Gaillard Cut. Appendix C is a discussion of chemical and physical properties of Cucaracha formation. 1924. Vaughan, T. W., American and European Tertiary larger Foraminifera: Geol. Soc. America Bull., v. 35, p. 785-822, pls. 30-36, 6 figs. Includes Miogypsina cushmani, from Culebra formation, and M. panamensis from strata now referred to Caimito formation. 1924- Douvill6, Henri, Revision des Lcpidocyclines: Soc. G6l. 1925. France Mc6m., new ser., 956m. 2 (t. 2), 115 p., 7 pls., 83 figs. Includes Lepidocyclina canellei and L. chaperi, and a new species from upper valley of Rio Chagres, L. decorate, which has not been recognized ir later collections (see Cole, 1952, [1953], p. 3). 1925. Dali, W. H., Illustrations of unfigured types of shells in the collections of the United States Nacional Museum: U. S. Natl. TMus. Proc., v. 66, art. 17, 41 p., 36 pls. Includes a Pliocene species (Sthenorytis toroense) and two Pleistocene species (Corbula macdonaldi and Yoldia perprotracla) described by Dall in 1912. 1925. Maury, C. J., A further contribution to the paleontology of Trinidad (Miocene horizons): Bull. Am. Paleontology, v. 10, no. 42, 250 p., 43 pls. Includes a species froin Culebra formation (Scapharca balboai) and two from Gatun formation (Scapharca dariensis and Clementia dariena). 1926. Hodson, Floyd, Venezuelan and Caribbean Turritellas: Idem, v. 11, no. 45, 50 p., 30 pls. Turritella altilira is illustrated. 1926. Vaughan, T. W., The stratigraphic horizon of the beds containing Lepidocyclina chaperi on Haut Chagres, Panama: Natl. Acad. Sci. Proc., v. 12, p. 519-522. At type locality, San Juan de Pequenc in sipper Chagres valley (locality 3 of present report), Lepidocyclina chaperi is associated with ipper Eocene species. 1926. Woodring, W. P., American Tertiary mollusks of the genus Clementia: U. S. Geol. Survey Prof. Paper 147, p. 25-47, pls. 14-17, 1 fig. 8