for mammals (figure 12.4).(Readers can see the original of the specimen
for views of many mammalian brains at http://www.neurophys.wisc.edu/
brain/paleoneurology.html).The species was a small ungulate,an “ore-
odont”that lived thirty-five mya in what is now the Big Bend area of the
Rio Grande river in Texas.It is described in detail at the internet site and
is also illustrated in other publications (Jerison 1990,1991).The endo-
cast shows many major structures of the brain,such as the olfactory
bulbs,cerebral hemispheres,and cerebellum,as well as the marginal
sulcus and longitudinal sulcus of the neocortex.One can use the position
of the rhinal fissure,which is the boundary between six-layer neocortex
and paleocortex,to analyze the evolution of neocortex.In the figure I
have named a few neocortical convolutions using the same criteria as in
living ungulates as presented in standard brain atlases.
The most important conclusion from such evidence may be to show
that mammalian neocortex evolved to larger relative size during the past
sixty million years (Jerison 1990).This verified the frequently stated
hypothesis,based on comparisons among living species,that “neocorti-
calization”(an aspect of encephalization) occurred during mammalian
evolution.From expected structure-function relationships,this implies
190 Harry Jerison
Figure 12.4
Tracing from dorsal (top) and lateral (bottom) views of the fossil brain of Bathygenys
reevesi,an upper Eocene oreodont (Merycoidodontidae,Artiodactyla).A view of the orig-
inal in color is on the Internet at http://neurophys.wisc.edu/brain/paleoneurology.html.
Olfactory bulbs (OB),cerebral cortex (CX),cerebellum (CL),and medulla (M) are
labeled,as are several cortical sulci:the longitudinal sulcus (l.s.) separating the left from
the right hemisphere,marginal sulcus (mar),and rhinal fissure (r.f.).
Fig.12.4