. Ordovician fossils of north China. Paleontology; Paleontology. (I) 46 Palxontologia Sinica Ser. B final endosheath is nearer the dorsal than the ventral side of the siphuncle (text fig. 6) as is shown by the two parallel sections (text figs. S and 0), taken essentially parallel. Fig. 6. Chilliiorrras nalhani. Restored longitudinal section, constructed from actual measurements along section a-b and c - d, and tlie exposed worn surface of the ventral side (lower dotted line), and with the aid of other specimens, x - y line of section shown in fig. 7. Two thirds natural size. cK-final sheath, o
. Ordovician fossils of north China. Paleontology; Paleontology. (I) 46 Palxontologia Sinica Ser. B final endosheath is nearer the dorsal than the ventral side of the siphuncle (text fig. 6) as is shown by the two parallel sections (text figs. S and 0), taken essentially parallel. Fig. 6. Chilliiorrras nalhani. Restored longitudinal section, constructed from actual measurements along section a-b and c - d, and tlie exposed worn surface of the ventral side (lower dotted line), and with the aid of other specimens, x - y line of section shown in fig. 7. Two thirds natural size. cK-final sheath, or endoconic lining; s/i-shcll- wall o{ siphuncle (ectosiphuncle). .sf-stereoplasmic filling of siphuncle; st-endosiphotube; ri-section of rock 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 Grabau, Amadeus W. (Amadeus William), 1870-1946. Peking, Published by the Geological Survey of China
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Keywords: ., bookcentury1900, bookdecade1920, booksubjectpaleont, bookyear1922
