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• Untangling the Stratigraphy of the Upper Paleozoic Supai and Naco Groups of the Mogollon Escarpment

  • When
    03 Dec 2024
  •  
    5:30 PM - 8:00 PM
  • Location
    Hexagon Office at 40 East Congress Street, Suite 150, Tucson, Arizona 85701
  • Registered
    3 registrants

  Register

  
  

  Arizona Geological Society
  

  2024 Speaker Series

  Tuesday,  3 December 2024 | 5:30 - 8:00 PM

  Location:  Hexagon Mining Division Office

  40 East Congress Street, Suite 150, Tucson, Arizona 85701

  
  

  Parking: On the street or parking garage (Old Pueblo Parking)

  Social Hour with Sandwiches from Beyond Bread (5:30-6:30 PM), Presentation (6:35 PM)

  For those planning to attend the event, please register by 6:00 PM on Sunday,  December 1, 2024

  For those unable to attend, here is the URL Streaming Link

  Meeting ID: 337 630 628 054

  Passcode: E6Nu3i7m

  The Arizona Geological Society thanks Hexagon

  for generously providing the venue and drinks

  
  

  Untangling the Stratigraphy of the Upper Paleozoic Supai and Naco Groups of the Mogollon Escarpment

  Stephen J. Reynolds¹, Spencer G. Lucas²

  and Julia K. Johnson¹

  ¹Arizona State University; ²New Mexico Museum of

  Natural History and Science 

  Abstract - The famous red rocks of the Mogollon Escarpment, from Sedona to White River, have traditionally been assigned the name Supai, correlating these rocks with the Supai Group of the Grand Canyon. The underlying limestone-bearing units have traditionally been called the Naco Formation in reference to the Naco Group of southeastern Arizona. Several workers, however, have proposed that the Supai nomenclature is largely not appropriate for rocks of the Mogollon Escarpment, based on proposed correlations and ages of the rocks.

  

  Sedona Section

  Due to these proposals, the stratigraphic framework of the Pennsylvanian-Permian Naco and Supai Groups of the Mogollon Escarpment have been confusing, with conflicting names, diverse proposed unit boundaries, various correlations within and between regions, and generally sparse age constraints. As a result, our team of regional geologists, biostratigraphers, and paleontologists are finishing a major program aimed at providing a data-based stratigraphic framework. We have measured dozens of stratigraphic sections, focusing on the stratigraphic unit type sections of previous workers and on strata that have the highest likelihood of providing paleontological age constraints. We have collected and identified a diverse suite of fossils, including conodonts, fossil plants, fossil pollen, and fossil trackways. In conjunction with these studies, we have obtained detrital zircon analyses from key units. Our paleontologic results, specifically identification of conodonts, are not yet complete, but we have already made major discoveries regarding the ages and correlations of units. For example, our detailed evaluation of fossil plants and pollen has demonstrated that the conglomerate-bearing interval of the lower Supai, whose importance was emphasized by Wes Peirce, is Late Pennsylvanian in age at Promontory Butte and Fossil Creek. These conglomerates are within the transition between the Supai and Naco, indicating that the Supai is in part Late Pennsylvanian. This eliminates the possibility that these rocks, including the conglomerate-bearing unit near Sedona, are correlative with the Hermit Formation, as has been proposed by some workers. Another issue is that the Naco Formation of the Mogollon Escarpment is Middle and Late Pennsylvanian in age, whereas the Naco Group of southeast Arizona ranges from Early Pennsylvanian to late Early Permian. We are considering the option that the term Naco is therefore not appropriate for rocks along the Mogollon Escarpment.

  We plan to publish a comprehensive study of the stratigraphy of the Supai and the Naco using our paleontological age constraints to discriminate between different possible correlations. We propose extending the stratigraphic name Supai Group to the Mogollon Escarpment, and elevating members proposed by prior workers, such as Jackson and Winters, to formation rank, as well as proposing some new names. In this talk we will outline stratigraphic problems, summarize key results, and discuss possible strategies for resolving the stratigraphic confusion.

  Speaker Bio:  Steven J. Reynolds earned a B.S. in Geology from the University of Texas in 1974, and a M.S. in Geosciences and Ph.D. in Geosciences from the University of Arizona in 1977 and 1982, respectively.  Initially employed as a research geologist at the Arizona Geological Survey until 1991, he returned to the University of Arizona as a Visiting Associate Professor until 1997.  Since then, Steve has held various faculty positions at the School of Earth Space Sciences at Arizona State University, where he is now an Emeritus Professor.

  Having authored or edited more than 200 geological maps, articles, and reports throughout his career, Steve's research interests currently include structure, tectonics, stratigraphy, detrital-zircon provenance studies, and mineral deposits of the southwestern United States and northern Mexico.

  
  

  
  

  Hexagon Mining Division Office - 40 East Congress Street,

  Suite 150, Tucson, Arizona 85701

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