Chad D. McCormick

University of Colorado Denver

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David W. Pierce

Massachusetts General Hospital

Roman Sakowicz

Gilead Sciences (United States)

Zhiheng Jia

Chinese Academy of Sciences

M. Dane Picard

University of Utah

Thomas D. Pollard

Yale University

James J. Hartman

Cytokinetics (United States)

Alan Russell

Healthwise

Nenad Tomašević

Allakos (United States)

Brad J. Nolen

University of Oregon

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Cytokinetics (United States)

Gilead Sciences (United States)

GlaxoSmithKline (United States)

University of California, San Diego

Yale University

Institut thématique Génétique, génomique et bioinformatique

University of Oregon

Massachusetts General Hospital

Rensselaer Polytechnic Institute

Brandeis University

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Stratigraphy of Gartra Formation (Triassic), Uinta Mountain Area, Utah and Colorado

Chad D. McCormick M. Dane Picard

Abstract In the Uinta Mountain area, the Gartra Formation (Middle? Triassic) unconformably overlies the Moenkopi Formation on the east and the Ankareh Formation on the west, and interfingers with the overlying purple unit of the Popo Agie Formation (Late Triassic). Based on lithology, sedimentary structures, and weathering characteristics, the Gartra is informally divided into three subunits. The lower subunit is characteristically conglomeratic, poorly sorted, massive, and poorly bedded sandstone. The middle subunit is characterized by finer-grained sandstone and by dominant planar and trough cross-stratification. The upper subunit is finer grained than either of the subjacent subunits, consisting of claystone, siltstone, and very fine to medium sandstone. Horizontal and small-scale cross-stratification are characteristic of the upper subunit. The Gartra probably was deposited by a series of west-northwest flowing streams on a broad alluvial plain. Detritus was derived from plutonic, sedimentary, and gneiss-schist terranes on the east and southeast (Ancestral Rockies and Uncompahgre uplift). Gradually decreasing velocity and turbulence of stream currents were responsible for the fining-upward sequences.

Siltstone

Lithology

Conglomerate

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Characterization of two classes of small molecule inhibitors of Arp2/3 complex

Nature (2009)

Brad J. Nolen Nenad Tomašević Alan Russell David W. Pierce Zhiheng Jia

Actin remodeling

MDia1

Actin-binding protein

10.1038/nature08231

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Citations (515)