. Bulletins of American paleontology. . Lobocorallium trilobatum triiobatur L. trilobatum vaurealense Grewingkia haysii o 500 1000 cross-sectional area, mm^ 1500 Text-figure 38.—Relation between number of major septa In) and coral cross-sectional area in Lnhocorallium rrilnh<ititm irilobutum (Whit- eaves. 1895) from the Stony Mountain Formation, Stony Mountain, Manitoba; LohocitralHum Irilohaliim vuiircalensc (Twenhofel, 1928) from the Vaureal Formation, Anticosti Island, Quebec, and the Sienopuniu faunal zone of the White Head Formation, Perce, Quebec; Grewingkia haysii (Meek, 1865) from M
. Bulletins of American paleontology. . Lobocorallium trilobatum triiobatur L. trilobatum vaurealense Grewingkia haysii o 500 1000 cross-sectional area, mm^ 1500 Text-figure 38.—Relation between number of major septa In) and coral cross-sectional area in Lnhocorallium rrilnh<ititm irilobutum (Whit- eaves. 1895) from the Stony Mountain Formation, Stony Mountain, Manitoba; LohocitralHum Irilohaliim vuiircalensc (Twenhofel, 1928) from the Vaureal Formation, Anticosti Island, Quebec, and the Sienopuniu faunal zone of the White Head Formation, Perce, Quebec; Grewingkia haysii (Meek, 1865) from Manitoba, Northwest Territories, and northwestern Greenland (see Hlias, 1981, fig. lib).. 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 Paleontological Research Institution (Ithaca, N. Y. ); Columbia University. Ithaca, N. Y. , Paleontological Research Institution [etc. ]
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