More than two hundred subcircular to crescent-shaped depressions, often
with radiating markings, were discovered on a 120 m2 bedding plane
interpreted as base-of-slope carbonate deposits and belonging to the
Lutetian–Bartonian Peschici Formation at San Lorenzo (Vieste, Gargano
Promontory, Italy). The area was mapped using a high-resolution aerial
camera (mounted on a kite) and a terrestrial laser scanner. The survey
allowed detailed morphologic analysis and topographic mapping of the
traces, in order to analyze the very regular distribution pattern. The
ichnological study, combined with sedimentologic and stratigraphic
analyses, identifies the depressions as fish feeding traces. Although the
tracemaker cannot be definitely identified, the comparison with modern
and fossil fish excavations suggests a higher affinity with bony fishes (e.g.,
sturgeons) than with rays. The trace fossils are here attributed to the
ichnogenus Piscichnus and constitute the first discovery of this ichnotaxon
in the middle Eocene of the Apulia Carbonate Platform and of Italy
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