. A descriptive catalogue of the marine reptiles of the Oxford clay. Based on the Leeds Collection in the British Museum (Natural History), London ... Reptiles, Fossil. 154 MARINE REPTILES OE THE OXFORD CLAY. whether this is formed by a median parasphenoid element or by the elevation of the pterygoids along a median line of symphysis. Mr. Leeds points out that Deslong- ehamps figures a similar ridge in Pelagosaurvs, but it does not seem to be present in Steneosaurvs. At its hinder end the vomer (parasphenoidj is concealed ventrally. Please note that these images are extracted from scanned page
. A descriptive catalogue of the marine reptiles of the Oxford clay. Based on the Leeds Collection in the British Museum (Natural History), London ... Reptiles, Fossil. 154 MARINE REPTILES OE THE OXFORD CLAY. whether this is formed by a median parasphenoid element or by the elevation of the pterygoids along a median line of symphysis. Mr. Leeds points out that Deslong- ehamps figures a similar ridge in Pelagosaurvs, but it does not seem to be present in Steneosaurvs. At its hinder end the vomer (parasphenoidj is concealed ventrally. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original British Museum (Natural History). Dept. of Geology; Andrews, Charles William, 1866-1924. London, Printed by order of the Trustees
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Keywords: ., bookcentury1900, bookdecade1910, booksubjectreptile, bookyear1910