98 J. STANLEY-EROWN INDEX TO VOLUMES 21 TO 30 



Page 

 Fauna of the Tejoii .i^roiip in S.-iu Dic.^d ('oiiiity : Uoy E. Dii-korson . . . 27,173 



— , Recurrent Hamilton • 31, 287 



— , Tribes Hill or Lower Beekmantown and Bucks Bridge 26, 2S9 



— , Weaklen, Potomac, Kootenai. Bear liiver, Dakota. Sundance, and 



Washita invertebrate 26, -3-14-348 



Faunai. and stratigraphic relations of the later lOocene of the Pacific 



coast ; Harold Hannibal 26, 168 



Lincoln formation in Washin,;,'ton : (". K. Weaver 26.169 



— continuity, Evidence of 21, -'.>2, 297 



— geography of the Eocene of California ; II. E. Dickerson 26, 410 



— migrations and diastrophism 25, ■■!97-399 



— relations of the San Lorenzo Oligocene to the Eocene in California. 25,153 

 Upper Neocene in the Sargent oil fields, California; Bruce 



Martin 24, 129 



— studies in the Cretaceoiis of the Santa Ana Mountains of southci-n 



California ; Earl L. Packard . . .^ 27, 174 



— -succession of Chester Group in Illinois and Kentucky 27, 156 



— zones of Pliocene formations, Vertebrate 27, 172 



the Martinez Eocene of California : K. E. Dickerson 25, 154 



Oligocene ; B. L. Clark 39, 166 



San Pablo formation east of Walnut Creek, near ^Nlount 



Diablo, California ; John P. Buwalda 24, 130 



Faunas, Contemporaneity of 21, 294 



, — contrasted, ^Migration of species and shifting of 21, 290 



— , Fixed and fluctuating characters of 21, 293 



— , Hypothesis of recurrents and shifting of 21, 285 



— in the John Day region, Succession of Miocene 28, 215 



— (invertebrate). Correlation between those of California and ]Mexico 26,414 

 • — - — of the American Triassic : relations to those of Asia and F]urope 26,412 



— , Lithologic changes not sufficient to account for difference in 21, 289 



— , Magma and local speci.-il 21, 293 



— , Ocean water determined the shifting or migration of 21, 289 



■ — of California, Peview of the Miocene and Oligocene 26, 416 



Japan and western United States, Comparison of Cretaceous.... 26,414 



— ■ — the Eastitort quadrangle, JNIaine, Correlation of the Paleozoic... 23,8.5, 



349-352 



• problems suggested by a study of the 24. 377-397 



Girardeau and Edgewood limestone 24, 112, .358, 368 



— Morrison, Comparison with other non-marine invertebi'iite. . . . 26, ,344 



Pacific Coast region, Vertel)rate ; J. C. Merriam 26, 416 



Santa Ana Mountains, Cretaceous 26, 169 



— , On the derivation of Paleozoic 22, 96 



— , Ordovician and Silurian polar 22, 92 



— , Rare and dominant species 21, 293 



— , Recurrence of 21, 292 



— , Reversal of order in .succession of 21, 286 



^, Rochester shale, Edmunds species of the Gotland section, Bohemian 



E= and Podilian 24, .381-385 



