A Late Ordovician age for the Whirlpool and Power Glen formations, New York

Author:

Schröer Laurenz1,Vandenbroucke Thijs R.A.1,Hints Olle2,Steeman Thomas1,Verniers Jacques1,Brett Carlton E.3,Cramer Bradley D.4,McLaughlin Patrick I.5

Affiliation:

1. Department of Geology, Ghent University, Krijgslaan 281/S8, 9000 Ghent, Belgium.

2. Institute of Geology, Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia.

3. Geology Department, University of Cincinnati, Cincinnati, Ohio 45221-0013, USA.

4. Department of Earth and Environmental Sciences, University of Iowa, Iowa City, IA 52242, USA.

5. Indiana Geological Survey, Indiana University, 611 N. Walnut Grove Avenue, Bloomington, IN 47405-2208, USA.

Abstract

A restudy of the palynology of the Whirlpool Formation and Power Glen Formation in New York (USA) yielded a diverse fossil assemblage with cryptospores, glomalean fungi, acritarchs, chitinozoans, scolecodonts, and small carbonaceous fossils. These new data, and particularly the presence of the chitinozoan index fossil Hercochitina crickmayi, combined with emerging stable carbon isotope data, suggest a Late Ordovician (Katian or Hirnantian) age for these formations, which is older than their previously suggested Silurian (Rhuddanian) age.

Publisher

Canadian Science Publishing

Subject

General Earth and Planetary Sciences

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