Continental break up and the distribution of fishes of Western Gondwana during the Early Cretaceous

By J. Maisey. 2000

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IRRITATOR CHALLENGERI, A SPINOSAURID (DINOSAURIA: THEROPODA) FROM THE LOWER CRETACEOUS OF BRAZIL (2002, background): “On balance, the age of the Romualdo Member is probably late Early Cretaceous (Albian; Maisey, 2000), but it could be as young as Cenomanian.”
A NEW NOTOSUCHIAN FROM THE EARLY CRETACEOUS OF NIGER (2003, background): “Terrestrial fossils of mid Cretaceous age (ca. 112 Ma, near the Aptian–Albian boundary) provide critical evidence (Maisey, 2000), and crocodyliforms, in this regard, have played an important role (Buffetaut and Taquet, 1979; Buffetaut, 1981; Bonaparte, 1991; Gasparini et al., 1991; Larsson…”
Late Cretaceous bioconnections between Indo‐Madagascar and Antarctica: refutation of the Gunnerus Ridge causeway hypothesis (2011, unknown): “…mid–Late Cretaceous, were already separated by a several hundred kilometre-wide marine gap (e.g. Nürnberg & Müller, 1991; Lawver et al., 1992; Müller et al., 1993; Smith et al., 1994; Scotese, 1998; Hay et al., 1999; Maisey, 2000; Néraudeau & Mathey, 2000; Pletsch et al., 2001) (Figs 1 & 5a).”
EVOLUTION OF THE SIDE-NECKED TURTLES: THE FAMILIES BOTHREMYDIDAE, EURAXEMYDIDAE, AND ARARIPEMYDIDAE (2006, background): “DEPOSITIONAL ENVIRONMENT: Near-shore marine (Maisey, 1990) with probable freshwater episodes (Maisey, 2000).”