Sedimentology and ichnology of the fluvial reach to inner estuary of the Ogeechee River estuary, Georgia, USA

• Sand-dominated sedimentary fabrics of the inner Ogeechee estuary are dominated by large-scale bi-directional trough cross-bedding, current-ripple lamination, flaser and wavy bedding, and mud rip-up clasts. Ichnofossils are nearly absent
• Fluvio-tidal transition is characterized by the coarsest grain size, graded planar and trough cross-bedding, and abundant organic debris. Bioturbation is nearly absent
• Fluvial reach is represented by decreased grain size, unidirectional cross-bedding, current-ripple lamination and absence of trace fossils
• Interbedded supratidal sediments are fine-grained and contain Glossifungites ichnofacies represented by Psilonichnus- and Camborygma-like burrows
• Ichnological dataset is subordinate to physical sedimentology (physical sedimentary structures, grain size, TOC)

Through the integration of sedimentological and ichnological observations, this paper explores the character of sediments deposited across the fluvio-tidal transition zone of the upper microtidal, mixed-energy, sand-dominated Ogeechee River estuary, Georgia, USA. A transect of tidally influenced to fluvial channel-bars and their facies variability is reported. Field and laboratory methods were employed, including observation of physical and biogenic sedimentary structures on the point-bar surfaces and in trenches, collection of grab samples, suction and box coring, grain size and total organic carbon analyses, optical microscopy, core logging, and daylight photography. The data presented in the paper can help in predicting facies changes across the fluvio-tidal transition of sand-dominated fluvio-tidal deposits in the rock record.The lower inner estuary is characterized by medium-fine and fine-medium sand with planar and trough cross-bedding, small-scale ripple lamination, tidal sedimentary structures (flaser and wavy bedding, herringbone cross-stratification), abundant organic debris, and mud rip-up clasts. Bioturbation of the intertidal point bars is low, but cryptobioturbation is locally observed. Upper inner estuary deposits comprise coarse-medium- and medium-coarse-grained sand, and are characterized by faint high-angle planar and trough cross-bedding. Organic debris, mud rip-up clasts, herringbone and current-ripple lamination are rarely observed. Bioturbation is absent to sparse. The fluvio-tidal transition is represented by very-coarse- to coarse-grained sand and granules. Physical sedimentary structures constitute massive, graded planar and trough cross-bedding with abundant plant detritus. Except for rare Siphonichnus- and Lockeia-like traces, bioturbation is absent. The fluvial setting is characterized by coarse-medium sand with unidirectional cross-bedding, current-ripple lamination, and rare organic-rich mud clasts. Bioturbation is absent. Inner estuary and fluvio-tidal transition zones are bounded by supratidal marsh deposits, and may develop a substrate-controlled Glossifungites ichnofacies, comprising Psilonichnus-like burrows. The fluvial reach is surrounded by forested floodplain with crayfish domes and chimneys, forming Camborygma-like traces.