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Genesee Group
Association Between Wave- and Current-aided Hyperpycnites and Flooding Surfaces in Shelfal Mudstones: an Integrated Sedimentologic, Sequence Stratigraphic, and Geochemical Approach
Sediment transport processes and lateral facies gradients across a muddy shelf: Examples from the Geneseo Formation of central New York, United States
Muddy Prodeltaic Hyperpycnites In the Lower Genesee Group of Central New York, USA: Implications For Mud Transport In Epicontinental Seas
New perspectives on transitions between ecological-evolutionary subunits in the “type interval” for coordinated stasis
Mechanisms controlling rupture shape during subcritical growth of joints in layered rocks
The conodont genus Ancyrodella in the middle Genesee Formation (lower Upper Devonian, Frasnian), western New York
Viriatellina (Dacryoconarida) from the Middle Devonian Ludlowville Formation at Alden, New York
Reworking of Sedimentary Pyrite on Euxinic Sea Floors, Devonian, Western New York: ABSTRACT
Condensed Sedimentary Sequence and Associated Submarine Hiatus Within a Cratonic Basin Setting—Case Study of Upper Devonian Genundewa Limestone of New York: ABSTRACT
Substrate specificity of Devonian epizoa
Proximal Continental Rhythmic Sequences in the Genesee Group (Lower Upper Devonian) of Southeastern New York
Rhythmic continental sequences characterize the proximal Genesee Group (Upper Devonian) in southeastern New York, which are interpreted as the remnant elements of a sequence of coastal-plain and upland fluvial deposits. A rhythm consists of a braided pattern of coarse conglomeratic channel-fill, a composite of point-bar, channel-fill, and overbank sandstones, and overbank, mudflat, and general flood plain accumulations of siltstones and mudrocks. Widespread lateral variability, rapid vertical change, channel depths of more than 30 feet, and textural mapping suggest a significant fall-line scarp close to the east of the present outcrop limit. Various aspects of the natural rhythmic sequences of the Genesee Group have been synthesized and examined using simulation techniques.