Inglis site is located in limestone of the Inglis Formation dating to the Eocene to Early Oligocene of ~48–33.9 Mya.[2][3] The inglis quarry itself is aberrant within this formation,being much younger than the Eocene rock its within.
Inglis site 1A was originally a sinkhole spanning 10 by 20 meters. From bottom to top, the sequence comprises a basal conglomerate, a thin clay bed, a lower sand unit, a second thin clay bed, an upper sand unit, and a cemented quartz sandstone.[4] Its mammalian fauna is regarded as a close correlate of that from Curtis Ranch in Arizona, whose age is well established by magnetostratigraphy and radioisotopic geochronology.[1]
History
Site 1A
The site was discovered in 1967 during construction of the Cross Florida Barge Canal. In January 1974, staff from the Florida Museum of Natural History excavated and screened approximately 300 cubic meters of fossil bearing sediment from the sinkhole.[5]