By Spencer Lucas
There seems a fly-over tone and caliber to this publication. It lacks move and solidarity. The photograph caliber is certainly terrible. Lucas additionally mis-cites Henry Fairfield Osborn's theorizing -- the quotation will be to Osborn's article in technological know-how (April thirteen, 1900), fairly at p. 567, no longer his later 1910 booklet book. As to recounting the primary Asiatic Expeditions, the therapy is asymmetric and a little speculative. additionally, a few spellings are inconsistent: eg., "Granter" (caption determine 2-10) vs. "Granger" (text, p. 24), and nor is present in the Index; "William Morris" (p. 24) truly was once "Frederick B. Morris," and, back, nor is present in the Index; the day trip series on p. 24 is muddled (incorrect use of "First," "Second," etc.) and likewise ignores these made in China starting in 1921; and and so forth.
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Additional resources for Chinese Fossil Vertebrates
Book Page 26 Wednesday, October 31, 2001 10:26 AM 26 HISTORY OF VERTEBRATE PALEONTOLOGICAL STUDIES life in China, studying its stratigraphy and fossil invertebrates, training Chinese geologists, and interacting extensively with Andersson, Andrews, Black and the other foreign vertebrate paleontologists working in China (Johnson 1985). In 1915, Emile Licent, a French Jesuit priest and entomologist, went to Tianjin, where he established a natural history museum at the Jesuit college. Licent collected fossil mammals, primarily Neogene horses from Gansu, and in 1923 was joined by a trained paleontologist and fellow French Jesuit, Pierre Teilhard de Chardin (1881–1955).
The vertebrate biochronology proposed here for the Chinese Silurian thus is coarse, but has the potential for further development as a useful tool for correlation. Silurian Vertebrate Paleobiogeography China’s Silurian vertebrate fossils are essentially confined to the south China block (see figure 3-2), so the biogeographical affinities of these vertebrates should parallel the paleogeographic affinities of this microplate. During the Silurian, south China was an isolated microplate (see figure 3-1).
The oldest fossil vertebrates known are Early Cambrian agnathans from China. Silurian Vertebrate Biochronology The text above identified four biochrons that correspond to the time represented by the Chinese Silurian vertebrate fossil assemblages (see figure 3-3). Further refinement of this scheme is desirable; each biochron is equal to about one epoch of the Silurian, or about 5 to 10 million years on the Harland et al. (1990) numerical time scale. The vertebrate biochronology proposed here for the Chinese Silurian thus is coarse, but has the potential for further development as a useful tool for correlation.
Chinese Fossil Vertebrates by Spencer Lucas