I
N THEautumn of 1912, the fossil collector Richard Markgraf,
with f i nancial support and direction from Bavarian paleontol-
ogist Ernst Freiherr Stromer von Reichenbach and the Bavarian
Academy of Sciences, discovered the partial skeleton of a bizarre
predatory dinosaur in Upper Cretaceous (early Cenomanian, ϳ97
Ma, see Ismail et al., 1989; Barakat et al., 1993; El Beialy, 1994,
1995; Nabil and Hussein, 1994; Ismail and Soliman, 2001; Ibra-
him, 2002; Gradstein et al., 2005) rocks of the Bahariya Forma-
tion exposed in the Bahariya Oasis of western Egypt (Fig. 1, see
also Sereno et al., 1998; Nothdurft et al., 2002). This gigantic
theropod, Spinosaurus aegyptiacus Stromer, 1915, possessed
highly derived cranial and vertebral features suff i ciently distinct
for it to be designated as the nominal genus of the clade Spino-
sauridae (Stromer, 1915, 1936). Spinosaurids, currently def i ni-
tively known only from Europe, South America, and Africa, are
important because of the scarcity of Cretaceous Gondwanan tet-
rapod fossils (see Krause et al., 1999, 2003; Carrano et al., 2002;
Lamanna et al., 2002). Moreover, fossils of Spinosaurus Stromer,
1915 and other spinosaurids are signif i cant because ofcontroversy
surrounding the postulated paleoecology of these taxa (see dis-
cussions in Charig and Milner, 1997; Sereno et al., 1998; Sues et
al., 2002).
N THEautumn of 1912, the fossil collector Richard Markgraf,
with f i nancial support and direction from Bavarian paleontol-
ogist Ernst Freiherr Stromer von Reichenbach and the Bavarian
Academy of Sciences, discovered the partial skeleton of a bizarre
predatory dinosaur in Upper Cretaceous (early Cenomanian, ϳ97
Ma, see Ismail et al., 1989; Barakat et al., 1993; El Beialy, 1994,
1995; Nabil and Hussein, 1994; Ismail and Soliman, 2001; Ibra-
him, 2002; Gradstein et al., 2005) rocks of the Bahariya Forma-
tion exposed in the Bahariya Oasis of western Egypt (Fig. 1, see
also Sereno et al., 1998; Nothdurft et al., 2002). This gigantic
theropod, Spinosaurus aegyptiacus Stromer, 1915, possessed
highly derived cranial and vertebral features suff i ciently distinct
for it to be designated as the nominal genus of the clade Spino-
sauridae (Stromer, 1915, 1936). Spinosaurids, currently def i ni-
tively known only from Europe, South America, and Africa, are
important because of the scarcity of Cretaceous Gondwanan tet-
rapod fossils (see Krause et al., 1999, 2003; Carrano et al., 2002;
Lamanna et al., 2002). Moreover, fossils of Spinosaurus Stromer,
1915 and other spinosaurids are signif i cant because ofcontroversy
surrounding the postulated paleoecology of these taxa (see dis-
cussions in Charig and Milner, 1997; Sereno et al., 1998; Sues et
al., 2002).