Pg. 14, 16. Auburn chert. Intensely hard bluish limestone, with soft chert bands full of fossils, forming surface stone of Auburn, Lincoln County, central-eastern Missouri. Included in Trenton limestone. [Age is Middle Ordovician.]
Source: US geologic names lexicon (USGS Bull. 896, p. 91).
Pg. 175-194. Auburn chert. Correlated Auburn chert with Decorah shale, and stated that it "apparently lies at about same horizon as Bryant limestone." [Age is Middle Ordovician.]
Source: US geologic names lexicon (USGS Bull. 896, p. 91).
Pg. 66. Stated that Auburn chert is included in Plattin formation. [Age is Middle Ordovician.]
[Misprint (USGS Bull. 896, p. 91): cited reference, Missouri Bur. Geol. and Mines, 2nd ser., v. 2, should be Jour. Geol., v. 33, no. 1.]
Source: US geologic names lexicon (USGS Bull. 896, p. 91).
C.L. Fenton (1928) and S. Weller and S. St. Clair (1928). See under Plattin limestone.
J. Bridge, March 1937 (personal note). Auburn chert is = Decorah or possibly is slightly younger. [Age is Middle Ordovician.]
Source: US geologic names lexicon (USGS Bull. 896, p. 91).
Pg. 262-263, chart 2 (column 51). Auburn chert. Placed in lowest Trentonian to conform to placement of Spechts Ferry shale with which it is correlated. [Age is Middle Ordovician.]
Source: US geologic names lexicon (USGS Bull. 1200, p. 170).
Pg. 117. Auburn chert. Has been suggested that Auburn chert be included in Plattin group, but brachiopods are not in accord with this suggestion. Presence of RAFINESQUINA indicates a higher correlation. Here suggested that formation may be chertified Decorah of Missouri, =Barnhart formation (new), rather than Plattin and correlation should be with Guttenberg member of Decorah. [Age is Middle Ordovician (Trentonian of Twenhofel and others, 1954, GSA Bull., v. 65, p. 247-298).]
Source: Publication; US geologic names lexicon (USGS Bull. 1200, p. 170).
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