Maryland Geological Survey 6, pt. 1
Maryland Geological Survey 6, pt. 1
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Occurrence. — Monmouth Formation. Brightseat, Prince George's County.
Collection. — Maryland Geological Survey.
Genus LIOPEPLUM Dall [Trans. Wagner Free Inst. Sci., Phlla., vol. iii, pt. i, 1890, p. 73] Type. — Liopeplum lioderma Conrad.
" Liopeplum is of smaller size than the two preceding groups. It is characterized by a minute trochoid nucleus, ribbed early whorls and Etymology: Xctof, smooth; WirXo;. an upper garment.
28 Digitized by GooqIc 430 Systematic Paleontology smooth body-whorl in t...he adult, all covered with a most elegant and polished glaze ; also by its habit of depositing a band of callus above the suture on the periphery of the preceding whorl. The pillar is stout and slightly curved, and the plaits are three or more, weak and rather variable, somewhat as in Volutolithes. The sinus at the suture is notable but not very wide. The plaits are preceded on the pillar by a thin mass of glaze which extends over the well-marked siphonal f asciole, somewhat as in some OlivcB, but with less defined boundaries.
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To quickly assess the difficulty of the text, read a short excerpt:
Occurrence. — Monmouth Formation. Brightseat, Prince George's County.
Collection. — Maryland Geological Survey.
Genus LIOPEPLUM Dall [Trans. Wagner Free Inst. Sci., Phlla., vol. iii, pt. i, 1890, p. 73] Type. — Liopeplum lioderma Conrad.
" Liopeplum is of smaller size than the two preceding groups. It is characterized by a minute trochoid nucleus, ribbed early whorls and Etymology: Xctof, smooth; WirXo;. an upper garment.
28 Digitized by GooqIc 430 Systematic Paleontology smooth body-whorl in t...he adult, all covered with a most elegant and polished glaze ; also by its habit of depositing a band of callus above the suture on the periphery of the preceding whorl. The pillar is stout and slightly curved, and the plaits are three or more, weak and rather variable, somewhat as in Volutolithes. The sinus at the suture is notable but not very wide. The plaits are preceded on the pillar by a thin mass of glaze which extends over the well-marked siphonal f asciole, somewhat as in some OlivcB, but with less defined boundaries.
What to read after Maryland Geological Survey 6, pt. 1?
You can find similar books in the "Read Also" column, or choose other free books by Maryland Geological Survey to read onlineMoreLess
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