Articles | Volume 33, issue 2
https://doi.org/10.5194/sd-33-109-2024
https://doi.org/10.5194/sd-33-109-2024
Science report
 | 
18 Jun 2024
Science report |  | 18 Jun 2024

Paleozoic Equatorial Records of Melting Ice Ages (PERMIA): calibrating the pace of paleotropical environmental and ecological change during Earth's previous icehouse

Jonathan M. G. Stine, Joshua M. Feinberg, Adam K. Huttenlocker, Randall B. Irmis, Declan Ramirez, Rashida Doctor, John McDaris, Charles M. Henderson, Michael T. Read, Kristina Brady Shannon, Anders Noren, Ryan O'Grady, Ayva Sloo, Patrick Steury, Diego P. Fernandez, Amy C. Henrici, and Neil J. Tabor

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Cited articles

Ahn, J. and Apted, M. J.: Geological repository systems for safe disposal of spent nuclear fuels and radioactive waste, Woodhead Publishing, 792 pp., First Edition, https://doi.org/10.1533/9781845699789, 2010. 
Atchley, S. C.: Influence of lowstand eolian erosional processes on stratigraphic completeness: sequence stratigraphy of the upper member of the Hermosa Formation (Upper Pennsylvanian), Paradox Basin, southeast Utah, Dissertation, University of Nebraska, Lincoln, Nebraska, 1–135 pp., ISBN 979-8-207-75988-3, 1990. 
Atchley, S. C. and Loope, D. B.: Low-stand aeolian influence on stratigraphic completeness: upper member of the Hermosa Formation (latest Carboniferous), southeast Utah, USA, Special Publications of the International Association of Sedimentologists, 16, 127–149, https://doi.org/10.1002/9781444303971.ch9, 1993. 
Baars, D. L.: Permian System of Colorado Plateau, Am. Assoc. Pet. Geol. Bull., 46, 149–218, https://doi.org/10.1306/BC74376F-16BE-11D7-8645000102C1865D, 1962. 
Baars, D. L. and Stevenson, G. M.: Tectonic evolution of the Paradox Basin, Utah & Colorado, in: Rocky Mountains Association of Geologists, edited by: Wiegand, D. L., Geology of the Paradox Basin, 23–31 pp., ISSN 01675648, 1981. 
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We present initial results from the upper 450 m of ER-1, a legacy core collected from modern-day Bears Ears National Monument, Utah, USA.  This section contains a relatively complete record of Upper Carboniferous to Early Permian sediments, providing a unique window on Earth's last icehouse–hothouse transition. Ongoing research will tie our results to important fossil sites, allowing us to better understand how this climate shift contributed to the evolution of terrestrial life.