Novel age constraints for the onset of the Steptoean Positive Isotopic Carbon Excursion (SPICE) and the late Cambrian time scale using high-precision U-Pb detrital zircon ages
Author:
Affiliation:
1. 1Department of Geosciences, Utah State University, Logan, Utah 84321, USA
2. 2Department of Geosciences, Boise State University, Boise, Idaho 83723, USA
3. 3Museum of Northern Arizona, Flagstaff, Arizona 86001, USA
Abstract
Publisher
Geological Society of America
Subject
Geology
Link
https://pubs.geoscienceworld.org/gsa/geology/article-pdf/50/12/1415/5741233/g50434.1.pdf
Reference35 articles.
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2. Breakup of a supercontinent between 625 Ma and 555 Ma: New evidence and implications for continental histories;Bond;Earth and Planetary Science Letters,1984
3. Carbon isotope stratigraphy;Cramer,2020
4. Testing the limits of Paleozoic chronostratigraphic correlation via high-resolution (<500 ky) integrated conodont, graptolite, and carbon isotope (δ13Ccarb) biochemostratigraphy across the Llandovery–Wenlock (Silurian) boundary: Is a unified Phanerozoic time scale achievable?;Cramer;Geological Society of America Bulletin,2010
5. Uranium isotopes distinguish two geochemically distinct stages during the later Cambrian SPICE event;Dahl;Earth and Planetary Science Letters,2014
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