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Schröer, Laurenz, Vandenbroucke, Thijs R.A., Hints, Olle, Steeman, Thomas, Verniers, Jacques, Brett, Carlton E., Cramer, Bradley D., McLaughlin, Patrick I. (2016) A Late Ordovician age for the Whirlpool and Power Glen formations, New York. Canadian Journal of Earth Sciences, 53 (7) 739-747 doi:10.1139/cjes-2015-0226

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Reference TypeJournal (article/letter/editorial)
TitleA Late Ordovician age for the Whirlpool and Power Glen formations, New York
JournalCanadian Journal of Earth Sciences
AuthorsSchröer, LaurenzAuthor
Vandenbroucke, Thijs R.A.Author
Hints, OlleAuthor
Steeman, ThomasAuthor
Verniers, JacquesAuthor
Brett, Carlton E.Author
Cramer, Bradley D.Author
McLaughlin, Patrick I.Author
Year2016 (July)Volume53
Issue7
PublisherCanadian Science Publishing
DOIdoi:10.1139/cjes-2015-0226Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID485273Long-form Identifiermindat:1:5:485273:9
GUID0
Full ReferenceSchröer, Laurenz, Vandenbroucke, Thijs R.A., Hints, Olle, Steeman, Thomas, Verniers, Jacques, Brett, Carlton E., Cramer, Bradley D., McLaughlin, Patrick I. (2016) A Late Ordovician age for the Whirlpool and Power Glen formations, New York. Canadian Journal of Earth Sciences, 53 (7) 739-747 doi:10.1139/cjes-2015-0226
Plain TextSchröer, Laurenz, Vandenbroucke, Thijs R.A., Hints, Olle, Steeman, Thomas, Verniers, Jacques, Brett, Carlton E., Cramer, Bradley D., McLaughlin, Patrick I. (2016) A Late Ordovician age for the Whirlpool and Power Glen formations, New York. Canadian Journal of Earth Sciences, 53 (7) 739-747 doi:10.1139/cjes-2015-0226
In(2016, July) Canadian Journal of Earth Sciences Vol. 53 (7) Canadian Science Publishing
Abstract/Notes 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.


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