New PDF release: d - problem on weaklyq-convex domains
By Ho L. H.
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Extra info for d - problem on weaklyq-convex domains
Example text
Thus, two or more closely related species are likely to be combined into one species if they have strong gradient monognathic and weak dignathic heterodonty. Because of lumping, the number offossil speciesdescribed for selected shark and ray groups is much smaller than it should be. The Collector's Guide to Fossil Sharks and Rays from the Cretaceous of Texas 19 Shark and Ray Hard Parts Tooth Terminology The tooth terminology used throughout this book is defined and illustrated on the following pages.
We emphasize "in Texas" because many of the species illustrated in this book are found in Cretaceous deposits elsewhere in North America, and many of the larger species have worldwide distributions. The chronologic range and maximum tooth size can and do vary somewhat according to geographic location. The author and publication date of the genus and species are listed below the chronologic range. Junior synonyms (invalid names) are not given. Description: Significant tooth features and tooth histology.
Root types. , basal view. 22 The Collector's Guide to Fossil Sharks a n d Raysjiom the Cretaceous of Texas Tooth Histology Root Types The root structure and vascularization patterns found in shark and ray teeth were extensively studied by the Belgian paleontologist Edgar Casier. After surveying modem and fossil selachians, Casier (1947a-c) proposed four basic structural tooth types or stages that he defined mainly on the placement of foramina and attributes of the nutrient groove. Primitive Paleozoic and many Mesozoic selachians, including hybodonts and hexanchoids, have anaulacorhizous roots that are flattened or tabular, lack a nutrient groove and are very porous (Figure I).
d - problem on weaklyq-convex domains by Ho L. H.
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