4.1 Article

First occurrence of Doswellia cf. D. kaltenbachi (Archosauriformes) from the Late Triassic (middle Norian) Chinle Formation of Arizona and its implications on proposed biostratigraphic correlations across North America during the Late Triassic

Journal

JOURNAL OF VERTEBRATE PALEONTOLOGY
Volume 41, Issue 3, Pages -

Publisher

TAYLOR & FRANCIS INC
DOI: 10.1080/02724634.2021.1976196

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Funding

  1. Petrified Forest Museum Association
  2. Federal Lands Recreation Enhancement Act
  3. NSF [EAR 1943286]

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Doswellia kaltenbachi is a long-snouted non-archosaur archosauriform from the Late Triassic of the United States, with new material discovered in Arizona for the first time. The findings strengthen the presence of this taxon during the Adamanian period and establish biogeographic links to other regions like Texas and Virginia, highlighting the similarity of North American vertebrate assemblages across different time periods.
Doswellia kaltenbachi is a long-snouted non-archosaur archosauriform known from the Late Triassic of the United States (Virginia and Texas). New material from the Chinle Formation of Arizona represents the first occurrence of D. cf. D. kaltenbachi from that formation and state. This occurrence is from the type section for the Adamanian estimated holochronozone (Late Triassic: middle Norian) in Petrified Forest National Park and firmly establishes the presence of this taxon in the Adamanian. This occurrence adds to the diverse vertebrate assemblage of the upper part of the Blue Mesa Member of the Chinle Formation (Adamanian). More broadly, the new occurrence strengthens biogeographic links to the older (latest Carnian or earliest Norian) Otischalkian from Texas and the possibly older Sanfordian/Conewagian assemblages of Virginia. The spatiotemporal distribution of Doswellia underscores the similarity of North American continental vertebrate assemblages across the Carnian-Norian boundary prior to the Adamanian-Revueltian boundary.

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