
Shark's teeth. Outdoors in Georgia, 4(3), 5–10

Late Eocene selachians from South-central Georgia. Palaeontographica, Abt. A, 176(1–3), 52–79

Die Neoselachier der Paleokaribik (Pisces: Elasmobranchii). Courier Forschungsinstitut Senckenberg, 119, 1–102

Late Eocene selachians from Irwinton Sand Member of the Barnwell Formation (Jacksonian), WKA mines, Gordon, Wilkinson Country, Georgia. Münchner Geowissenschaftliche Abhandlungen Reihe A, Geologie und Paläontologie, 39, 5–16, 5 pl., 3 fig., 1 tabl.

A Middle Eocene Selachian Fauna from the Castle Hayne Limestone Formation of Duplin County, North Carolina. Münchner Geowissenschaftliche Abhandlungen Reihe A, Geologie und Paläontologie, 39, 17–32, 7 pl., 1 fig.

Late Eocene sharks of the Hardie Mine local fauna of Wilkinson County, Georgia. Georgia Journal of Science, 61(3), 153–179
Taxonomy and biostratigraphy of the elasmobranchs and bony fishes (Chondrichthyes and Osteichthyes) of the lower-to-middle Eocene (Ypresian to Bartonian) Claiborne Group in Alabama, USA, including an analysis of otoliths. European Journal of Taxonomy, 585, 1–274
DOI: 10.5852/ejt.2019.585
Additions to the elasmobranch assemblage from the Bandah Formation (middle Eocene, Bartonian), Jaisalmer District, Rajasthan, India, and the palaeobiogeographic implications of the fauna. Palaeovertebrata, 44(2), Article e1
DOI: 10.18563/pv.44.2.e1
Evolution, diversity, and disparity of the tiger shark lineage Galeocerdo in deep time. Paleobiology, 47(4), 574–590
DOI: 10.1017/pab.2021.6
Combining palaeontological and neontological data shows a delayed diversification burst of carcharhiniform sharks likely mediated by environmental change. Scientific Reports, 12, Article 21906
DOI: 10.1038/s41598-022-26010-7

A new Bartonian elasmobranch assemblage from the Kutch Basin, western India, and its significance in the context of paleoclimate change. Historical Biology, 36(10), 1985–2008
DOI: 10.1080/08912963.2023.2238736
Late Eocene fishes from the Tupelo Bay Formation of South Carolina, USA. Rivista Italiana di Paleontologia e Stratigrafia , 132(2), 431–512
DOI: 10.54103/2039-4942/30814








