T21 New Advances in Geobiology (Posters)
Sunday, 9 October 2022
9:00 AM - 1:00 PM
Exhibit Hall F
A DIVERSE MICROPALONTOLOGICAL MISS ASSEMBLAGE FROM THE LACUSTRINE MILL CANYON DINOSAUR TRACKSITE: EARLY CRETACEOUS CEDAR MOUNTAIN FORMATION, MOAB, UTAH
Paper number: T21-2
Program: Technical Sessions
Time: 9:00 AM – 1:00 PM
Authors
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Michael WizevichCentral Connecticut State University Geological Sciences, New Britain, CT
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Dakota PittingerKutztown Univ. Dept Physical Sciences, Kutztown, PA
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Brandon BilheimerKutztown Univ. Dept Physical Sciences, Kutztown, PA
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Lauren DeLongKutztown Univ. Dept Physical Sciences, Kutztown, PA
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Deidre ForneyKutztown Univ. Dept Physical Sciences, Kutztown, PA
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Noah WorkmanKutztown Univ. Dept Physical Sciences, Kutztown, PA
Abstract
The collected MCDT slabs were decontaminated using an ultra-sound cleaner. Bedding plane and vertical cuts were studied by field-emission scanning electron microscopy and energy dispersive X-ray spectroscopy. The best preserved MCDT microfossils are located on the bedding plane whereas those below the surface are more altered by diagenesis and mat degradation by heterotrophs. Fifteen morphotypes are recognized, including: single strand cyanobacteria, double strand fungal mycelium or/ bacteria, multiple strand fungal mycelium or/ bacteria, twisted strand bacteria, strands with associated amorphous masses (bacteria with EPS), polygonal (cow-web like) bacteria with EPS or fungal mycelium, capsular bacillus-type bacteria, isolated masses of EPS, isolated spheres and sphere clusters with rough textured fungal spores, isolated smooth spheric fungal spores, folded masses with irregular surfaces plant cuticles, spheres in amorphous matrix (bacteria with EPS), mini-polyhedric bacteria cysts, bacteria rods, and uniserial bacterial strands. This micropaleontological assemblage of the MCDT is one of the most diverse recognized of an ancient MISS community.
Geological Society of America Abstracts with Programs. Vol. 54, No. 6
doi: 10.1130/abs/2022AM-378711
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