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Mid-Cretaceous Paleopedology and Landscape Reconstruction of the Mid-Atlantic U.S. Coastal Plain

Jesse D. Thornburg; Kenneth G. Miller; James V. Browning; James D. Wright
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Detrital-Zircon U-Pb Paleodrainage Reconstruction and Geochronology of the Campanian Blackhawk–Castlegate Succession, Wasatch Plateau and Book Cliffs, Utah, U.S.A.

Bridget S. Pettit; Mike Blum; Mark Pecha; Noah McLean; Nicolas C. Bartschi; Joel E. Saylor
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The Geochemistry of Qatar Coastal Waters and its Impact on Carbonate Sediment Chemistry and Early Marine Diagenesis

John M. Rivers; Linso Varghese; Ruqaiya Yousif; Fiona F. Whitaker; Sabrina L. Skeat; Ismail Al-Shaikh
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New Perspectives On the Geomorphic, Sedimentologic, and Stratigraphic Signatures of Former Wave-dominated Tidal Inlets: Assateague Island, Maryland, U.S.A.

Christopher T. Seminack; Randolph A. McBride
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Source-to-Sink Analysis of a Transtensional Rift Basin from Syn-Rift to Uplift Stages

Jialin Wang; Chaodong Wu; Tianqi Zhou; Wen Zhu; Yanxi Zhou; Xi Jiang; Disheng Yang
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Dense Zones of the Kharaib Formation (Lower Cretaceous), United Arab Emirates

Stephen N. Ehrenberg; Qiong Wu
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TURBULENCE!

Memes, False News, and the Death of Empiricism

V. Paul Wright
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    COVER EXPLANATION.—Microbial mats of the lower intertidal zone displaying polygonal desiccation cracks, Inland Sea, southern Qatar. Variably-structured microbial mats can be observed in low-energy intertidal settings from around the Qatar coastline, forming in evaporated marine waters ranging in salinity between 42 and 350 psu, or near-normal marine to halite-saturated concentrations. In most examples significant lithification is not observed. See Rivers et al., this issue.

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