free trial issue                                  subscribe                                             back issues

Athena Review Vol. 5, no. 1


Records of Life: Fossils as Original Sources


Synapsids 2: Cynodonts to early Mammals

    

Cynodontia (class Synapsida; order Therapsida; family Cynodontia)

            Cynodontia (“dog teeth”),  grouped as a suborder of the Therapsids, are considered the direct ancestors of early mammals by the Late Triassic. For a long time, the earliest fossil evidence of mammals did not appear until the Early Jurassic at about 180 mya, in the form of Morganucodons. In the 1990s, however, earlier mammal forms began to appear, such as Adelobasilicus from the Late Triassic in west Texas (Lucas 1990, Lucas and Luo 1993).

            In the transition from early reptiles to mammals, various basic changes occurred in the skull, dentition, and post-cranial skeleton. The skull form changed substantially during the process of of accomodating stronger chewing muscles, and of repackaging an expanded brain and special sense organs. Dentition became more specialized, with changes in both teeth and jaws. Limbs and vertebrae changed, related to locomotion with legs placed under the body. Importantly, in conjuntion with changes in the jaw anatomy, the mammalian inner ear evolved with three ossicles used as amplifiers, as opposed to a single one in reptiles.

             Anatomical traits used to identify mammals, and contrast them with reptiles, are listed in  Table 1:

Table 1: Major skeletal differences between early reptiles and mammals.

trait

Early Reptiles

Mammals

1

No fenestrae in skull                  

large fenestra exposes all of braincase

 

2

Braincase attached loosely

Braincase attached firmly to skull

3

No secondary palate

Complete bony secondary palate

 

4

Undifferentiated dentition

Incisors, canines, premolars, molars

 

5

Cheek teeth are uncrowned points

Cheek teeth (PM & M) are crowned & cusped

6

Teeth replaced continuously       

Teeth replaced once at most

 

7

Teeth with single root                

Molars double-rooted

 

8

Jaw joint made up of quadrate + articular

Jaw joint made up of dentary + squamosal (*)

9

Lower jaw composed of several bones

Lower jaw composed of dentary bone only

10

Single middle ear bone or ossicle (stapes)

Three ossicles in middle ear (stapes, incus, malleus)

 

11

Joined external nares (nostrils)    

Separate external nares

 

12

Single occipital condyle

Double occipital condyle

 

13

Long cervical (neck) ribs          

Cervical ribs tiny, fused to vertebrae

 

14

Lumbar (lower back) region with ribs    

Lumbar region rib-free

 

15

No diaphragm              

Diaphragm present

 

16

Limbs sprawled out from body  

 

Limbs under body

 

17

Scapula simple

Scapula with big spine for muscles

 

18

Pelvic bones unfused    

Pelvis fused

 

19

Two sacral (hip) vertebrae

Three or more sacral vertebrae

20

Toe bone numbers 2-3-4-5-4     

Toe bone numbers 2-3-3-3-3

 

21

Body temperature variable

Body temperature constant (homeostatic)

(*) note: The presence of a dentary-squamosal jaw joint has been arbitrarily selected as the defining trait of a mammal.

 (source: Hunt 1994-1997)

            The transition from synapsid reptiles to mammals is well documented, with a long series of fossils linking vertebrate classes and families, permitting the tracing of the origin and radiation of various mammalian orders in some detail. (Szalay et al., 1993; Gingerich  1977) While the mammal-like anatomy of cynodonts has been long known, only recent finds have made it seem  demonstrable that mammals descended from a single group of cynodonts.

           One of the earlest cynodonts, Charassognathus (“notched jaw”) was a very small carnivore, dating from the Late Permian at about 260 mya. The type species, Charassognathus gracilis, was  recently found near Fraserburg, South Africa  (Botha et al., 2007). Charassognathus, whose skull was only two inches (5 cm) long, is named for a notch at the back of its lower jaw which was used to attach a chewing muscle called the adductor mandibula externus.  Charassognathus. gracilis also had a the cynodont’s typically large synapsid opening for chewing muscles. Its teeth were diversified into the four cynodont (and mammalian) classes of incisors, canines, premolars, and molars. These included both the very large canines typical of cynodonts, and tricuspid premolars.

.

Procynosuchidae

            Another early cynodont was Procynosuchus, who flourished during the Late Permian (260-253 mya)Their fossils, found in the Cistecephalus and Daptocephalus Zones of South Africa and Zambia, and Tartarian Zone IV of Russia, showed they evolved from the same basic therapsid stock as the therocephalians. Procynosuchus was named by South African paleontologist Robert Broom in 1937. Broom also named the cynodont Cyrbasiodon in 1931. A related genus, Parathrinaxodon, was named by Parrington in 1936. These genera are now regarded as synonyms of Procynosuchus.

Fig.1: Chart showing ancestral relationships or phylogeny of cynodonts (after Botha et al. 2007)

Procynosuchus delaharpae, first described by Broom, was an early cynodont with many primitive features, but also some unique skeletal features in the ribs and limbs, some possibly serving as adaptations for semi-aquatic, riverine or estuarine habits. P. delaharpae has  been found more recently in the Madumbabisa Mudstone of the Middle Luangwa Valley in Zambia (Kemp 1979, 1980).  

            Like some of the therocephalians, the cynodonts possessed a long series of small multicusped cheek teeth and a partial secondary palate. However, the cynodonts also possessed certain unique features as well, such as a closed braincase which probably served generally to strengthen the skull and to protect the brain and middle ear cavity from pressures generated by the contraction of the increased mass of jaw muscles.

            They show many advanced, mammal-like characteristics, such as a reduced number of bones in the lower jaw. Even though the jaw hinge remained reptilian, the dentary now made up about 75% of the lower jaw, with the other reptilian lower jaw bones now much reduced, near the jaw hinge. A partially formed, secondary bony palate was composed mainly of palatine bones (a mammalian trait), rather than vomers and maxilla as in reptilian forms. Procynosuchus also had a complex pattern on the crowns of their cheek teeth. The cheek teeth had a much more complex cusp pattern than that of all but a few bauriamorph therocephalians (e.g., the Bauridae). The complex cheek teeth and secondary palate show that the cynodonts were able to chew and breathe at the same time (which most reptiles cannot).  The food was broken down in the mouth rather than the stomach. Modifications in the jaw and the flared zygomatic arch reflect increased differentiation of jaw musculature. Lower incisor teeth was reduced to four per side, instead of the previous six; early mammals, by comparison, had three lower incisors per side (Kemp 1982)

            The large temporal fossae, now bounded only by the thin zygomatic arch or cheekbone served to hold a single reptilian jaw muscles, the forerunner of the mammalian masseter. Their vertebral column shows that lumbar vertebrae start to lose ribs, the first sign of functional division into thoracic and lumbar regions. Scapula beginning to change shape. Further enlargement of the ilium and reduction of the pubis in the hip. A diaphragm may have been present, which would have enhanced breathing.

.

Fig.1: Chart showing chronology of basal cynodonts (after Botha et al. 2008)

Dvinia
 

            Fossils of Dvinia, another early cynodont from the Late Permian,  have been found in Russia in the Upper Tatarian deposits of Arkhangel'sk. Dvinia (named for the Dvinia River in Russia) had cheek teeth with tiny cusps, an initial sign of teeth developing into more than simple perforators. Dvinia is also synomous with "Permocynodon" [D. prima = Permocynodon sushkini, Amalitsky 1922

            The size of the temporal fenestra increased still further in Dvinia. It had an enlarged brain, with various changes occuring in the floor of the braincase.  The dentary bone was now the major bone of the lower jaw. The other jaw bones that had been present in early reptiles were reduced to a complex of smaller bones near the jaw hinge. The stapes or columella (the reptilian middle ear ossicle) was recognized as a cartiligenous feature (Tatarinov 1968). The single occipital condyle was split into two surfaces.

         The postcranial skeleton of Dvinia remains virtually unknown. It is speculated that they had a higher metabolic rate that may have approached homeothermy.    (Battail and Surkov 2000;  Hopson 1991; Hopson and Barghusen 1986; Kemp  1982; Sidor and Hopson 1998; Tatarinov 1968). 

.

   

  . 

Galesauridae: 

Class:   Synapsida    Order: Therapsida     Suborder:   Cynodontia   (unranked): Epicynodontia      Family:  Galesauridae

            Galesaurus planiceps is a relatively advanced Cynodont from the Early Triassic of South Africa, now placed in the clade calleed Epicynodontia. When first discovered in South Africa and classified by Sir Richard Owen in 1859, Galesaurus was  incorrectly identified as a dinosaur, of which numerous examples were being found in that region.  Ten years later, in 1869, when the fossil genus Galesaurus was again mentioned in Nature (in the first issue of that journal),  it was still thought by T. H. Huxley to be a dinosaur. Eventually, it was reclassified as a  cynodont. As Owen and Huxley were two of the most accomplished  and knowledgable scientists of their day, the misidentifaction illustrates problems caused by a lack of comparative data on the therapsids (interestingly, a term coined by Huxley himself).

            In the past, the genus Galesaurus was often been used for small, immature specimens. while larger, mature specimens were grouped in the genus Glochinodontoides (van Hoepen 1916). Another synonymous taxa was Notictosaurus (Broom and Robinson 1948). All are now classed as Galesaurus

        Galesaurus had a broad snout, and an enlarged zygomatic arch. Its frontal bones had  anterior "spine" projections inserting between nasals, a trait which persisted in adults. It had a complete secondary palate. Its skeleton had distinct lumbar & thoracic regions, with ribs restricted to thoracic region. A diaphragm was probably completely established in the species.  Its  limbs were relatively upright (Hopson & Barghusen  1986; Kemp  198;  Sidor & Hopson 1998)

 Thrinaxodon: T. liorhinus Seeley 1894a.

 Range: Early Triassic Lystrosaurus Zone of South Africa; Fremouw Formation of Antarctica.

            Thrinaxodon liorhinus, dating from the early Triassic (252-247 mya), was a badger-like carnivore about 50 cm long, with short limbs and a short tail. Most examples have been discovered in South Africa,  and are museums in Cape Town, Bloemfontein, and Johannesburg.  The discovery by Edwin Colbert of Thrinaxodon in Antarctica during the 1960's provided a definite indication that Antarctica and Africa were connected during the Early Triassic.

        T. liorhinus was a relatively advanced "galesaurid" cynodont, with development of several of the cynodont features.  Its temporal fenestra was large, with large jaw muscle attachments. Its snout was about as broad as tall , with a narrow braincase and a sharp parietal crest and a robust zygomatic arch.  It had a fully ossified secondary palate. It had a near-mammalian functional division of teeth, with incisors (four uppers and three lowers), canines, and 7-9 cheek teeth with cusps for chewing.

         The brain was long and narrow, resting within a very narrow skull.   Like other cynodonts the brain filled the endocranial cavity (Rowe 1996).     In Thrinaxodon, the adductor attaches to the outside surface of the parietal, which covers the braincase. (In more basal therapsids, the jaw was closed in a reptile manner by the adductor mandibularis, which originated on the braincase.) Thus, in Thrinaxodon, the braincase no longer need be engineered to support muscle.   This configuration allowed expansion of the braincase, which in turn increased the surface area available for muscle attachment (Palaios).
        Its more reptilian or primitive features include the lower jaw attachment, with only primary evidence of a dentary- squamosal articulation. The Thrinaxodon dentary, however, was large, with the little quadrate and articular bones now loosely attached. The stapes now touched the inner side of the quadrate. The first sign of the mammalian jaw hinge appeared, in the form of a ligamentous connection between the lower jaw and the squamosal bone of the skull. The occipital condyle now consisted of two slightly separated surfaces, though not as far separated as the mammalian double condyles (Hunt 1994-7). It retained a pineal or "third eye" opening in the skull. 
            Its teeth had a "reptilian" alternate replacement pattern. Its cheek teeth had multiple cusps but were all alike (i.e., no distinction between molars and premolars), were regularly replaced, had single roots, and did not occlude. Its 
dental formula was 4/3,1/1,7-9/7-9  (Palaios).   

            Thrinaxodon’s vertebral connections more mammalian, and lumbar ribs reduced. Scapula shows development of a new mammalian shoulder muscle. Ilium increased again, and all four legs fully upright, not sprawling.  Number of toe bones is 2.3.4.4.3, intermediate between reptile number (2.3.4.5.4) and mammalian (2.3.3.3.3), and the "extra" toe bones were tiny (Hunt 1994-1997).

.  


             

            Diademodon (early Triassic, 240 Mya), found in the same strata as Cynognathus, had larger temporal fenestra, attaching to stronger jaw muscles that earlier cynodonts. It had a true bony secondary palate formed exactly as in mammals, although it did not  extend as far back. In the premaxilla area, it may have had chambered turbinate bones in the nose, suggesting a warm-blooded level of breathing and metabolism. 

        Modifications in its dentition included a decreased rate of tooth replacement. Its cheek teeth (molars) showed improved occlusion, with more defined cusps and consistent wear facets. The lower jaw of Diademodon consisted almost entirely of a single bone, the dentary, with tiny articular at the hinge. It retained a transitional or double jaw joint. In lumbar region, its ribs were much shorter than earlier cynodonts, probably improving diaphragm function and locomotion. The digits on its toes had  mammalian proportions of 2.3.3.3.3, while closely related species still showed more variable numbers in this feature (Hunt 1994-7).

            Probelesodon (230-220 Mya). This mid-Triassic cynodant from South America had very large temporal fenestra, still retaining the postorbital bar which kept the fenestra separate from the eye socket.  Its secondary palate was longer, but still not complete. Its teeth were double-rooted, as in mammals. Its nostrils (nares) were separated. Second jaw joint stronger. The lumbar ribs were totally lost; its thoracic ribs more mammalian, and its vertebral connections very mammalian. Its hip & femur were also more mammalian  (Hunt 1994-7).

.

Eucynodontia 

            Eucynodontia ("true dog teeth") is an infraorder of Therapsids that includes both mammals and most non-mammalian cynodonts. The oldest eucynodonts are known from the beginning of the Early Triassic, and possibly the end of the Late Permian. Eucynodontia includes two major subgroups, Cynognathia and Probainognathia.

Cynognathians (class Synapsida; order Therapsida; suborder Eucynodontia ).                                                                                       

           Cynognathus (“dog jaw”) was a meter-long carnivore closely related to mammals that lived during the Early and Middle Triassic (247-237 mya). It is known from a single species, Cynognathus crateronotus, which had a very wide distribution in Gondwana, the southern part of Pangaea (fig.1).  Fossils have been found in the Karoo formation of South Africa; the Fremouw Formation, in South Africa/Lesotho; in the Puesto Viejo Formation in Argentina; in Antarctica; and in China.

            Cynognathus was a heavily built animal, with a  large head about 30 cm  (1.0 ft) in length, wide jaws, and sharp teeth. The dentary (lower jaw) was equipped with differentiated teeth, and the maxilla or upper jaw included large canines, both traits typical of cynodont carnivores. The temporal fenestra was large, indicating a strong chewing muscle. The cheek teeth had cusps which met in true occlusion for more efficiently slicing up food and the rate of tooth replacement was reduced, with mammalian-style tooth roots (although still single roots). Pits and canals on the premaxilla or nasal bone represent concentrations of nerves and blood vessels. In mammals, such structures allow hairs  or whiskers  to be used as sensory organs.

Fig.1: Distribution map of Cygnognathus crateronotus

The dentary now comprised about 90% of the muscle-bearing part of the lower jaw. It contained a transitional jaw joint, combining mammalian and reptilian features. A new bony jaw joint existed between the squamosal (skull) and the surangular bone (lower jaw), while the other jaw joint bones were reduced to a compound rod lying in a trough in the dentary, close to the middle ear. 

The presence of a secondary palate in the mouth indicates that Cynognathus would have been able to breathe and swallow simultaneously. Its hind limbs were placed directly beneath the body, but the forelimbs sprawled outwards in a reptilian fashion.  Its ribcage formation was more mammalian, with ribs now lacking in the stomach region, suggesting an efficient diaphragm, an important muscle for mammalian breathing.       

            The descendents of Cynognathus gradually evolved into small carnivorous and insectivorous forms, perhaps nocturnal,  depending on their senses of hearing and smell. Due to their enlarged olfactory and auditory bulbs, Cynodont and early mammalian brains gradually grew larger than sauropsid (reptilian) brains.

            Regarding the development of the mammalian middle ear, the eardrum had developed in the lower jaw, behind the jaw hinge, supported by a wide prong (reflected lamina) of the angular bone. Airborne sound was transmitted through the eardrum to two small lower jaw bones, the articular and the quadrate, which contacted the stapes in the skull, which contacted the cochlea.

             Cynodonts, who essentially had two jaw joints, developed relatively loose quadrates and articulars that could vibrate freely for sound transmittal while still functioning as a jaw joint, strengthened by the mammalian jaw joint right next to it. All early mammals from the Lower Jurassic retained this low-frequency ear and a double jaw joint. By the middle Jurassic, mammals lost the reptilian jaw joint (though it still occurs briefly in embryos) and the articular and quadrate bones became miniaturized and migrated into the nearby middle ear as the incus and malleus, serving to amplify high-frequency sounds.

   

 . 

Probainoganathians

            Probainognathus, an advanced cynodont from the Middle Triassic (239-235 mya), was first found in Argentina, and later in South Africa, with the related genus Lumkuia. More recently Probainognathian fossils from the Middle Triassic have also been found in Madagascar. There they were part of an assemblage dated at 230-225 mya, that included early dinosaur fossils as well as several other cynodonts (Flynn et al 1999.; Caroll 1988).

            The Probainognathians, like the Cygnognathians, were mostly carnivorous, with jaws considerably shorter than those of Cygnognathus, but with similar tooth forms including large canines. They are split into four families: Probainognathidae, Chiniquodontidae, Tritheledontidae, and Mammaliaformes (the latter group comprising ancestors of mammals).  Non-mammalian probainognathians, one of the longest-lived therapsid groupings, lived from the Triassic to the Jurassic.  Probainognathians spread across the Gondwana of Triassic times, although not as widely as Cygnognathus

            Probainognathus had a relatively large brain showing various skull changes and the fusion of some skull plates. One of these involved the closing of the pineal, "third eye" formamen.  The slender cheekbone was relatively low  on the side of the eye socket, although the postorbital bar (a reptilian trait) was still present.   Like Cyngnathus, Probainognathus still had a transitional overlap of reptilian and mammalian jaw joints. Its retained attentuated versions of cervical ribs and lumbar ribus , with reptilian costal plates  on thoracic ribs mostly lost. In terms of digits, its had the same number of toe bones as mammals.

            The evolution of chewing muscles in late synapsids is well illustrated by Probainognathus, showing increasing muscular control which is related to more controlled grinding functions of specialized molars.  This control involved a split masseter or cheek muscle which had more distributed attachments (Palaios). Undoubtely this was linked to additional cusps on the molars or cheek teeth of Probainognathus.

       

   End of the therapsid carnivores

            While some cyndont groups lasted well into the Jurassic period, many therapsid carnivores became extinct during the multi-stage  Permian–Triassic extinction event. This effectively ended the dominance of the carnivores among the therapsids. In the early Triassic, all the medium-to-large land carnivore niches were taken over by archosaurs (diapsid reptiles) which, over about 35 million years, came to include the crocodylomorphs, the pterosaurs, and the dinosaurs. By the Jurassic, the dinosaurs had come to dominate the large terrestrial herbivore niches as well.

            By Early Triassic times, cynodonts had diverged into large predaceous carnivores such as Cynognathus and moderate large omnivorous and herbivorous types such as Trirachodon and Diademodon. The Middle Triassic saw a major radiation of herbivorous forms included in the family Traversodontidae. From this family evolved the highly specialized and extremely mammal-like Tritylodontidae of the Late Triassic to Middle Jurassic, the "rodents" of the early Mesozoic and culmination of the herbivorous cynodont radiation.
    By the late Triassic, the Therapsid carnivores had become small, about the size of a weasel or rabbit. The first mammals, also small in size, appeared in the Late Triassic epoch at about 220 mya, some 50 million years after the first therapsids. The majority of the mammal species that existed in the Mesozoic Era were nocturnal insectivores, the direct ancestors of multituberculates and primates. 
.          

Glossary  

.      

References:      

 
Barghusen (1968)

 Battail & Surkov  2000;

 Benton, M. J.  2000 , Vertebrate Paleontology, 2nd Ed. Blackwell Science Ltd (2004) 3rd edition

 Berman, D.S.  1977. "A New Species of Dimetrodon (Reptilia, Pelycosauria) from a Non-Deltaic Facies in the Lower Permian of North-Central New Mexico". Journal of Paleontology 51(1): 108—115;

 Carroll, R. L. 1988, Vertebrate Paleontology and Evolution, WH Freeman & Co

 Crompton & Parker (1978);

 Flynn et al. 1999, Science

 Hopson  1991

 Hopson, J.A. and Barghusen, H.R. (1986), An analysis of therapsid relationships in N Hotton, III, PD MacLean, JJ Roth and EC Roth, The Ecology and Biology of Mammal-like Reptiles, Smithsonian Institution Press, pp. 83–106  

 Hunt, Kathleen 1994-1997 Transition from amphibians to amniotes; transitional Vertebrate Fossils

 Huttenlocker, A. K.; Mazierski, D. and Reisz, R. R.  2011. "Comparative osteohistology of hyperelongate neural spines in the Edaphosauridae (Amniota: Synapsida)". Palaeontology 54: 573–590.)

 Ivakhnenko, M.F. 1999, Biarmosuches from the Ocher Faunal Assemblage of Eastern Europe, Paleontological Journal vol 33 no.3 pp. 289–296. abstract

 Kemp, T.S.  1980. "The primitive cynodont Procynosuchus: structure, function and evolution of the postcranial skeleton". Philosophical Transactions of the Royal Society B 288 (1027): 217–258.

 Kemp (1982);

 Lucas, S.G.; Spielman, J. A.; Rinehart, L.F.; Martens, T. (2009). "Dimetrodon (Amniota: Synapsida: Sphenacodontidae) from the Lower Permian Abo Formation, Socorro County, New Mexico". New Mexico Geological Society Guidebook, 60th Field Conference, Geology of the Chupadera Mesa Region: 281–284.)

Lucas, S. G. (2011). Traces of a Permian Seacoast. Prehistoric Trackways National Monument. pp. 1—48.)

Marsh, O.C. (1878). "Notice of new fossil reptiles". American Journal of Science 3(15): 409-41)

Palaios, 2013, Mammals (pdf. file including various articles from their web site at www.palaios.org)

 Romer, A.S.; and Price, L.I. (1940). "Review of the Pelycosauria". Geological Society of America Special Paper 28: 1–538.

 Rowe 1996

 Sidor & Hopson (1998);

 Tatarinov (1968)    




Athena Review Image Archive™   | Guide to Archaeology on the Internet   |   free trial issue |  subscribe  |  back issues

Main index of Athena Review   |   Subject Index   |   Research Pages   |  Galleries aand Museums  |  Ad rates |  Current issue index


Copyright  ©  1996-2014    Athena Publications, Inc.  (All Rights Reserved).