Conus (Contraconus)  lindajoyceae (Petuch, 1991)

 

 

Edward J. Petuch actually, Contraconus lindajoyceae is from the Buckingham Member of the Tamiami Formation (not Caloosahatchee).

 

It is a much rarer species than adversarius, which is found in the younger Pinecrest Member of the Tamiami Formation. Neither lindajoyceae nor adversarius are found in the Caloosahatchee Formation, which is around 1 million years younger than the Pinecrest Member 

 

Contraconus lindajoyceae is Piacenzian Pliocene from the Buckingham Member of the Tamiami Formation. ( Petuch Unit 10). 3.4-3.6 M.Y A. The Buckingham is now put only in the end of the Piacenzian Pliocene not Zanclean anymore.

 

By Edward Petuch: The Buckingham Member of the Tamiami Formation is earliest Piacenzian Age, right after the end of the Zanclean Age, at about 4 million years

 


This species was initially called Contraconus chickee, but this name was never officially described or published; it was simply a manuscript name that Petuch later changed to Contraconus lindajoyceae (from the Buckingham Member of the Tamiami Formation): Petuch wrote "A chickee is a Seminole-Miccosukee name for a palm thatched open hut; chickees have high peaked roofs, so they reminded me of the high, protracted spire of lindajoyceae."



 

 
Contraconus lindjoyceae  (Petuch 1991)
[ 88,4 x 32,3 mm. ]
Tamiami Formation, Buckingham Member Piacenziano (Pliocene) – Sarasota
[AZFC N. 163-00 ]
 

 

 

Contraconus lindajoyceae  (Petuch 1991)
88,4 x 32,3 mm.
Piacenziano (Pliocene) – Sarasota
[AZFC N. 163-00 ]
Contraconus lindajoyceae  (Petuch 1991)
mm. 84,5
Contraconus lindajoyceae
Holotype (CM 35660)
APAC Quarry, Sarasota
County, Florida.
Tamiami Formation, Pinecrest Beds SL 79.2 mm; MD 29.1 mm.
Contraconus lindajoyceae
(Petuch 1991)
mm. 40
Arcadia, Pleistocene, Florida, USA
(Michel Brault)

 

Collected in the Buckingham Member (Petuch Unit 10) of the Tamiami Formation in the 1980’s 

 

 

 

 

 

 


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