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The Origin and Evolution of Mammals - Moodle

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236 THE ORIGIN AND EVOLUTION OF MAMMALS<br />

have been generalist omnivores. In body size, they<br />

ranged up to that <strong>of</strong> a small bear, <strong>and</strong> probably had<br />

a comparably cosmopolitan diet. Chriacus (Fig. 7.6(c))<br />

was a very lightly built, agile form.<br />

Carnivorous ‘condylarths’. Arctocyonids were common<br />

in the Early Palaeocene <strong>and</strong> structurally represent<br />

the base <strong>of</strong> the ‘condylarth’ radiation, from<br />

which various more specialised groups diverged.<br />

Some became more adapted for carnivory, with a<br />

tendency to evolve molar teeth with higher, sharper<br />

cusps, <strong>and</strong> shearing edges, in place <strong>of</strong> the bunodont<br />

cusps <strong>of</strong> the arctocyonid-grade (Szalay 1969). <strong>The</strong>se<br />

constituted the very first radiation <strong>of</strong> relatively<br />

large, predaceous mammals. Three groups <strong>of</strong><br />

‘condylarths’ exhibiting an increasing expression <strong>of</strong><br />

this trend are usually combined into a taxon Cete<br />

(Archibald 1998; Prothero et al. 1988). <strong>The</strong> triisodontids<br />

are the most primitive members <strong>of</strong> this group,<br />

<strong>and</strong> include one <strong>of</strong> the very earliest ‘condylarths’.<br />

Isolated 5 mm long molars <strong>of</strong> Ragnarok occur at<br />

the base <strong>of</strong> the Palaeocene 65 Ma. Carnivorous<br />

characteristics <strong>of</strong> the dentition are only incipiently<br />

developed. <strong>The</strong> later group Hapalodectidae are<br />

more progressive in this respect, having higher,<br />

sharper cusps. Hapalodectes was a small, rat-sized<br />

animal, not found until the Eocene in North<br />

America, but already present in the Late Palaeocene<br />

<strong>of</strong> Asia. <strong>The</strong> Mesonychidae express to the greatest<br />

extent the tendency towards specialised carnivory.<br />

<strong>The</strong> molar teeth are laterally compressed, <strong>and</strong> shearing<br />

edges have developed on the front <strong>of</strong> the lower<br />

teeth, which acted against edges on the back <strong>of</strong> the<br />

uppers. This condition is described as prevallidpostvallum<br />

shearing, a system that is only analogous<br />

to the postvallid-prevallum shearing system <strong>of</strong><br />

the carnivorous teeth that evolved in the later specialist<br />

carnivore groups Creodonta <strong>and</strong> Carnivora. Some<br />

Mesonyx such as Mesonyx itself (Fig. 7.6(d) <strong>and</strong> (e))<br />

were the size <strong>of</strong> a wolf <strong>and</strong> had lightly built,<br />

digitigrade limbs. Others, such as Harpagolestes<br />

(Fig. 7.6(f)) were even larger, heavily built with powerful<br />

jaws <strong>and</strong> teeth <strong>and</strong> were probably scavengers<br />

rather than hunters. <strong>The</strong> mesonychids are also known<br />

from Asia, where they occur in the Early Palaeocene<br />

Shanghuan <strong>and</strong> the Late Palaeocene Nonshanian faunas<br />

(Wang et al. 1998; Lucas 2001). One <strong>of</strong> the last<br />

forms, Andrewsarchus (Fig. 7.6(g)), is from the Late<br />

Eocene <strong>of</strong> Mongolia, <strong>and</strong> is <strong>of</strong>ten claimed to be the<br />

largest terrestrial carnivorous mammal ever discovered.<br />

Its skull was over 80 cm in length.<br />

Herbivorous ‘condylarths’. Other lineages <strong>of</strong> ‘condylarths’<br />

evolved increasingly specialised herbivorous<br />

adaptations from an arctocyonid-like ancestry. To<br />

varying degrees the premolar teeth enlarged <strong>and</strong><br />

became more molar like, <strong>and</strong> the molars evolved<br />

broader, six-cusped occlusal surfaces. <strong>The</strong> limbs<br />

tended to become digitigrade, with well developed<br />

hooves on each <strong>of</strong> the digits. Four main families are<br />

recognised (Archibald 1998) <strong>and</strong> all <strong>of</strong> them first<br />

occur in the Early Palaeocene <strong>of</strong> China as well as<br />

North America (Wang et al. 1998; Lucas 2001).<br />

<strong>The</strong> hyopsodontids (Fig. 7.7(a)) were small,<br />

rabbit-sized animals with short limbs. <strong>The</strong> canines<br />

were very small, <strong>and</strong> the last premolar is slightly<br />

enlarged. <strong>The</strong> paraconule <strong>and</strong> metaconule cusps <strong>of</strong><br />

the upper molars had enlarged to give the sixcusped<br />

condition. Hyopsodus extended into the<br />

Eocene <strong>and</strong> is therefore one <strong>of</strong> the last surviving<br />

‘condylarths’.<br />

<strong>The</strong> family Mioclaenidae (Fig. 7.7(b)) were also<br />

relatively small, incipiently specialist herbivores. <strong>The</strong><br />

premolars were more molarised, <strong>and</strong> the occlusal<br />

surfaces <strong>of</strong> the molar teeth were simplified by having<br />

less distinct cusps, suggesting a more continuous<br />

grinding action <strong>of</strong> tougher food. Mioclaenids, or at<br />

least close relatives <strong>of</strong> this family occur in the Early<br />

Palaeocene Tiupampan fauna <strong>of</strong> the Santa Lucia<br />

Formation <strong>of</strong> Bolivia, where they have been implicated<br />

in the origin <strong>of</strong> the indigenous South American<br />

ungulate orders. Gheerbrant et al. (2001) have described<br />

‘condylarth’ teeth <strong>of</strong> Early Eocene age from<br />

Morocco in North Africa, one <strong>of</strong> which, Abdounodus<br />

(Fig. 7.7(b)), is comparable to mioclaenids.<br />

Periptychids varied from small, squirrel-sized<br />

mammals to Ectoconus (Fig. 7.7(c)), which was the<br />

size <strong>of</strong> a sheep. In this family, the premolars were<br />

more or less fully molarised, <strong>and</strong> crescentic crests<br />

had developed from the cusps <strong>of</strong> these <strong>and</strong> the<br />

molars (Fig. 7.7(d)). Archibald (1998) interpreted the<br />

tooth structure as an adaptation for dealing with<br />

tough, fibrous vegetation that was first shredded by<br />

the swollen premolars <strong>and</strong> then pulverised by the<br />

molars. <strong>The</strong> skeleton <strong>of</strong> periptychids is rather heavily<br />

built <strong>and</strong> the limbs short. <strong>The</strong> feet too are short,

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