Carnivore Fauna Research Articles

Sabretooths, giant hyenas, and hominins: Shifts in the niche of Early Pleistocene scavengers in Iberia at the Epivillafranchian-Galerian transition

The Epivillafranchian and the transition to the Galerian (1.2–0.9 Ma) was a period marked by environmental fluctuations and faunal turnover. Homo arrived into Europe around 1.4 Ma. ago, and was established in Iberia during the Epivillafranchian, as evidenced by the oldest sites with hominin fossils located in the Iberian Peninsula. The Iberian ecosystems offered a variety of trophic resources to hominins, including the opportunity to scavenge carcasses of large ungulates killed by a diverse predatory guild, especially due to the presence of two sabre-toothed cats. It has been claimed that the presence of Pachycrocuta brevirostris, a strong competitor for carrion, prevented hominins from exploiting abandoned carcasses as a reliable meat and fat resource. However, computer simulation experiments suggest that the coexistence of P. brevirostris and hominins competing for carrion was ecologically viable in the Epivillafranchian. Nevertheless, the faunal turnover of the Epivillafranchian-Galerian transition drastically changed the composition of the large carnivore fauna. The changes include the extinction of the sabre-toothed felid Megantereon, frequently considered a key provider of partially consumed carcasses, and the demise of the hyperscavenger P. brevirostris. All these changes modified the ecological scenario and the opportunities for hominins and other facultative scavengers. Computer simulation experiments using the agent-based model SCAVCOMP-ABM are used here to evaluate the viability of the coexistence of hominins and giant hyenas in the Epivillafranchian-Galerian transition. Different ecological scenarios defined by the composition of the predatory guild, ecosystem productivity, and competition pressure from other scavengers are evaluated. Results suggest that hominins and giant hyenas could coexist during the Epivillafranchian with different carnivore guilds, but a disruption of the scavenging niche likely occurred in the transition to the Galerian, coinciding with the extinction of P. brevirostris. A low ecosystem productivity during the cold intervals, maintenance of a high competition for carrion with other facultative scavengers, and a hypothetical social behaviour of the sabre-toothed cat Homotherium latidens appear as key factors to explain the changes in the scavenger guild at the Epivillafranchian-Galerian transition.

Updates to the carnivore fauna from the Sima de los Huesos.

The Sima de los Huesos site in the Sierra de Atapuerca (Burgos, northern Spain) is a Middle Pleistocene locality with the most important accumulation of humans in the European record for this age. In addition to the hominin collection, the Sima has provided numerous faunal remains. Here, we update the carnivoran mammal fauna from the Sima de los Huesos. The analyzed carnivoran fauna is taxonomically diverse consisting of 11 species from 9 genera and four families. The high taxonomic diversity of carnivorans at the site is interpreted as corresponding to high overall ecosystem productivity. A synthetic description of the carnivoran remains is presented adding new information on the biochronology of the carnivoran species assemblage and its paleoecological association with European Middle Pleistocene hominins. Because of their similarity in taphonomic setting and diets-that the carnivoran fauna and humans were found in the same place and had similar protein-rich diets-clarifying the paleontological and paleoecological context of these carnivorans permits a better understanding of the humans also found at this site.

New Carnivoran (Mammalia: Carnivora) specimens from the Siwaliks of Pakistan and India and their faunal and evolutionary implications

ABSTRACT Recently collected carnivoran specimens from the Siwalik Group of Pakistan are described and discussed. These specimens add to our knowledge of the previously known taxa while also adding to our biogeographic, stratigraphic, and temporal knowledge of the carnivorans from the Siwaliks. At least eight distinct taxa are identified, and although most specimens are fragmentary, some hyaenid specimens are identified further (e.g. Lycyaena and Ictitherium). We identify and describe the first herpestid fossils from the Chinji Formation, the first hyaenid (Lycyaena cf. L. dubia) from the Tatrot Formation, and the first definitive occurrence of Ictitherium (Ictitherium cf. I. viverrinum) from the Dhok Pathan Formation. We report the first occurrences of several taxa from various sites in the Siwaliks of Pakistan, including the first reports of any carnivorans from Dhok Milan, Kohtehra, and Lawa. Individual sites show a wide range of carnivoran biodiversity, however larger scale trends are more discernible when comparing those between formations in the Siwaliks. Several taxa disappear over time from the carnivoran fauna of the Siwaliks, starting with barbourofelines, and continuing with amphicyonids (and non-carnivoran hyaenodontids). Felids and mustelids are the most diverse carnivorans in the Siwaliks, while caniforms become more prevalent through time.

Elemgasem nubilus: a new brachyrostran abelisaurid (Theropoda, Ceratosauria) from the Portezuelo Formation (Upper Cretaceous) of Patagonia, Argentina

AbstractAbelisaurids are medium–large‐sized theropod dinosaurs that were predominant in the carnivorous fauna during the Late Cretaceous of Gondwana. These predators are abundant in the Cretaceous fossil strata of Patagonia, which yield the best record for this group. In the Late Cretaceous, abelisaurids appear in almost all regions of Gondwana and in all stages, except for the Coniacian, in which they are globally unknown. Here we describe a new abelisaurid,Elemgasem nubilusgen. et sp. nov., from the Portezuelo Formation (Turonian–Coniacian), Patagonia, Argentina. The palaeohistology of the appendicular bones ofElemgasemshows that the holotype was a subadult individual, but had achieved sexual maturity. This taxon is based on several axial and appendicular elements, and is diagnosed by the presence of a marked pattern of rugosity on the lateral surface of the fibula and a dorsoventrally deep lateral wall of the calcaneum. Moreover, the posterior caudal vertebrae have a morphology slightly different from any other abelisaurid.Elemgasem nubilusis recovered as an unstable taxon within Brachyrostra, given that it was recovered as sister taxon of Furileusauria or in several positions within this clade. Despite the problematic phylogenetic relationships ofElemgasem nubilus, it is important because it is the first abelisaurid from the Turonian–Coniacian interval and it increases the diversity of this theropod family at a time of marked turnover in the tetrapod fauna of South America, global climate change, and mass extinction events recorded worldwide in the marine realm.

The exceptionally high diversity of small carnivorans from the Late Miocene hominid locality of Hammerschmiede (Bavaria, Germany).

The present study deals with new material of carnivorans (Mustelidae, Mephitidae, Ailuridae, Potamotheriinae and Viverridae) from the basal Tortonian (Late Miocene, late Astaracian) hominid-bearing locality of Hammerschmiede (Bavaria, Germany). The small carnivoran fauna includes 20 species belonging to nine different subfamilies (Guloninae, Lutrinae, Mellivorinae, Potamotheriinae, Leptarctinae, Mephitinae, Simocyoninae, Genettinae and Viverrinae). The identified forms include: "Martes" sansaniensis, "Martes" cf. munki, "Martes" sp., Circamustela hartmanni n. sp., Laphyctis mustelinus, Guloninae indet., Eomellivora moralesi, Vishnuonyx neptuni, Paralutra jaegeri, Lartetictis cf. dubia, Trocharion albanense, Palaeomeles pachecoi, Proputorius sansaniensis, Proputorius pusillus, Alopecocyon goeriachensis, Simocyoninae indet., Potamotherium sp., Semigenetta sansaniensis, Semigenetta grandis and Viverrictis modica. The new species Circamustela hartmanni n. sp. is differentiated from the other members of the genus by its small size and the morphology of its dental cusps in the upper and lower carnassials. This is one of the highest reported taxonomic diversities for fossil small carnivorans in the Miocene of Europe, including also first and last occurrences for several genera and species. Additionally, the assemblage comprises some rare taxa such as Palaeomeles pachecoi and Eomellivora moralesi. An ecomorphological comparison of the discovered taxa reveals possible cases of competition and niche partitioning.

Revising the Villafranchian carnivoran fauna from Libakos (Macedonia, Greece) with some implications for its age

ABSTRACT The mammal fauna from Libakos was collected by H. Eltgen (Technical University of Clausthal, Germany) during the end of the 1960s and studied by K. Steensma. The locality is situated within the fluviolacustrine-fluvioterrestrial deposits of the Grevena–Neapolis basin (Macedonia, Greece), which are considered as Pliocene-Pleistocene. The carnivoran collection of Libakos is poor and fragmentary with doubtful or limited determinations. The reconsideration of the carnivorans indicated the presence of the canids Caniscf. arnensis and Canis cf. etruscus, the mustelid Pannonictis nestii recognised for first time in Greece, the large-sized hyaenid Pachycrocuta brevirostris and the machairodontine Homotherium latidens. The available biochronological data, the stratigraphy and the comparison with other well-dated Villafranchian faunas of Greece, indicate a late Villafranchian age for Libakos fauna, more precisely between ~2.0 and 1.5 Ma.

A Transitional Mammalian Carnivore Community from the Paleogene–Neogene Boundary in Northern Kenya

ABSTRACT The Paleogene–Neogene boundary is an important transitional time for the evolution of African fauna. Many taxa that evolved endemically in the Paleogene begin to wane in diversity, while new taxa, many of which will become exemplars of the modern African fauna, immigrate from Eurasia via newly opened terrestrial connections. The Paleogene–Neogene boundary is documented in the fossil record at Nakwai, in northern Kenya. Here we describe the mammalian carnivore fauna, which includes the earliest carnivoran records in Africa, and an interesting mix of Paleogene and Neogene hyaenodont taxa. The carnivoran fauna includes Jinomrefu lakwanza, gen. et sp. nov., the earliest barbourofelid in Africa, which has a transitional sabertooth morphology. An analysis of ecomorphological change in African mammalian carnivores across this boundary shows that hyaenodonts become more disparate in body size and more hypercarnivorous as they are displaced by invading carnivorans. This provides another test case for possible competition between carnivorans and hyaenodonts, a group that goes extinct in Africa and globally during the Neogene. http://zoobank.org/urn:lsid:zoobank.org:pub:D803E9DB-B2F1-497D-B796-57BED91BC744

The Late Middle Miocene Mae Moh Basin of Northern Thailand: The Richest Neogene Assemblage of Carnivora from Southeast Asia and a Paleobiogeographic Analysis of Miocene Asian Carnivorans

The late middle Miocene fossil-bearing lignite zones of the Mae Moh Basin, northern Thailand, have yielded a rich vertebrate fauna, including two species of Carnivora described thus far: the bunodont otter Siamogale thailandica (known from over a 100 specimens) and the large amphicyonid Maemohcyon potisati. Here we describe additional carnivoran material from Mae Moh comprising new remains of Maemohcyon potisati as well as remains of seven new carnivorans belonging to at least four families: a new species of Siamogale (S. bounosa), a new species of another otter (Vishnuonyx maemohensis), one representative of the genus Pseudarctos (a small amphicyonid), a new genus of Asian palm civet, Siamictis, one representative of another civet (cf. Viverra sp.), a new species of mongoose (Leptoplesictis peignei) and a Feliformia indet. This carnivoran assemblage constitutes one of the richest for the middle Miocene of eastern Asia and by far the richest for the Neogene of Southeast Asia.While the presence of new species indicates a certain degree of endemism for the Mae Moh Basin, paleobiogeographic cluster analyses conducted on carnivoran faunas from the middle and late Miocene of Asia indicates that a southern Asian biogeographic province, analogous to the current Oriental Realm, has existed since at least the middle Miocene. These results strengthen the observation that the Himalayan Mountains and Tibetan Plateau constitute significant physical barriers as well as an important climatic barrier (through the strengthening of monsoon systems) preventing north-south mammal dispersals in Asia since at least the middle Miocene.

Evolution of the carnivoran (Carnivora, Mammalia) guild structure across the Middle/Upper Miocene boundary in Germany

We analyse the evolution of carnivoran guilds (body mass, locomotor pattern, and diet preference) across the Middle to Upper Miocene boundary based on a comparison of the carnivoran fauna from Steinheim (Mammal Neogene zone MN 7/8; Servallian to early Tortonian), and from the Eppelsheim Formation (Mammal Neogene zone MN 9/10; mid-Tortonian), Germany. Results reveal a massive faunal turnover between these two communties due to taxonomic differences up to the family level. Guild structures of both carnivoran faunas were similar, implying that Late Miocene taxa replaced Middle Miocene taxa in their respective niches rather than new ecological strategies being added to the guild. This is not surprising, as (1) the majority of Late Miocene taxa were derived from European Middle Miocene ancestors and mostly share their paleoecology, (2) of the few undisputed Late Miocene immigrant taxa (Eomellivora, Simocyon, Sivaonyx), only Eomellivora adds new ecological strategies to the guild, and (3) both faunas occupied the same kind of partly open woodland paleoenvironment. Our paper supports previous studies, suggesting that ecological diversity remains stable across the Middle to Upper Miocene boundary and that similar environments produce similar carnivoran guild structures irrespective of taxonomical composition.

Paleobiogeographic implications of additional Felidae (Carnivora, Mammalia) specimens from the Siwaliks

ABSTRACT Felids from G.E. Lewis’ Yale Peabody Museum collection of Siwalik fossil mammals are described, and palaeobiogeography is interpreted based on these specimens. Five felid taxa are recognised from these Miocene-Pliocene Siwalik Group collections, including three from the Chinji Zone: Sivaelurus chinjiensis, Sivaelurus sp., Pseudaelurus sp.; one from the Nagri Zone: Leptofelis cf. vallesiensis; and one from the Tatrot Zone: Metailurus cf. hengduanshanensis. Sivaelurus chinjiensis is similar to Miopanthera lorteti in morphology, and Miopanthera thus is viewed as a junior synonym of Sivaelurus. Leptofelis cf. vallesiensis from the Nagri Zone represents the first record of this genus in southern Asia, and Metailurus cf. hengduanshanensis represents one of the latest occurrences of the genus, suggesting that Metailurus survived into the late Pliocene widely in Asia. Carnivoran faunas suggest that during the Middle Miocene southern Asia shared more taxa with Europe than with eastern Asia, and a newly recognised Euroriental paleorealm is proposed based on this biogeographic pattern. Since the late Late Miocene, the similarity of southern and eastern Asian carnivoran faunas increased. This pattern coincides with that of proboscideans, and was probably controlled by geographic and environmental changes caused by the rise of the Tibetan Plateau.

The first North American Propterodon (Hyaenodonta: Hyaenodontidae), a new species from the late Uintan of Utah.

The carnivorous mammalian fauna from the Uintan (late middle Eocene) of North America remains relatively poorly documented. This is unfortunate, as this is a critical interval in the transition from “creodont” to carnivoran dominated carnivore guilds. This study reports a new species from the Uinta Formation of the Uinta Basin, Utah, the first North American species of the otherwise Asian hyaenodont genus Propterodon. The new species, Propterodon witteri, represented by a dentary with M2-3 from the late Uintan Leota Quarry, is larger than the well-known P. morrisi and P. tongi and has a larger M3 talonid, but is otherwise very similar. A phylogenetic analysis of hyaenodont interrelationships recovers P. witteri as a hyaenodontine but is generally poorly resolved. A relationship between Hyaenodontinae and Oxyaenoides, recovered by many recent analyses, is not supported. Among the Asian species of Propterodon, P. pishigouensis is reidentified as a machaeroidine oxyaenid and recombined as Apataelurus pishigouensis new combination. Isphanatherium ferganensis may also represent an Asian machaeroidine. Identification of a North American species of Propterodon and an Asian Apataelurus increases the similarity of North American Uintan and Asian Irdinmanhan faunas and suggests that there was substantial exchange of carnivorous fauna during the late middle Eocene.

Carnivora from the early Oligocene of the ‘Phosphorites du Quercy’ in southwestern France

The early Oligocene carnivorans from the Quercy phosphorites (southwestern France) studied herein come from three localities: Mas de Got, La Plante2 and Valbro, all in MP 22 of the European Paleogene Mammal stratigraphy scheme. These localities contain a rich carnivoran fauna with weasel-sized to tiger-sized species in diverse families, especially Amphicynodontidae (with four species of Pachycynodon and two of Amphicynodon) and Nimravidae. New taxa are described (Wangictis n. gen., Peignictis pseudamphictis n. gen., n. sp.). We note the absence of taxa often present in the sites of the Quercy phosphorites, such as the family Amphicyonidae and, in the Feloidea, the genera StenoplesictisFilhol, 1880 and PalaeoprionodonFilhol, 1880. The fauna of the three localities is typical of the early Oligocene prior to a faunal turnover in the middle Oligocene. Future research in the Quercy will give more precision to the timing and mode of this faunal event.

Small carnivoran fauna of the Mascall Formation, Crooked River Basin, central Oregon

ABSTRACTThe Hemingfordian North American Land Mammal Age is a poorly known time period, although recently discovered sites in central Oregon have begun to cast light on a diverse mammalian fauna. Here, we describe four small carnivorans new to this region, one of which is a new species. Cryptailurus tinaynakti, sp. nov., is a hypercarnivorous feliform. UOMNH F-70218 is the dp4 of a diminutive mustelid similar in morphology to that of extant martens, but likely of a new species based upon discussed patterns in mustelid deciduous dentition. The occurrence of two additional species, Leptocyon leidyi and Bassariscus antiquus, increases both their geographic and temporal ranges. The early to middle Miocene was a time of transition from sparse woodland to grassland ecosystems in much of North America. The Hemingfordian fauna of the Pacific Northwest inhabited a diverse wet woodland ecosystem, surprisingly rich in carnivorans. With the description of these additional small taxa, we can now get a clearer picture of what must have been a diverse assemblage of mammals with a variety of ecological roles in an undersampled period of time.

Carrying capacity, carnivoran richness and hominin survival in Europe

Carrying capacity, the maximum biomass that an ecosystem can sustain over the long term, strongly influences several ecological processes and it is also one of the main determinants of biodiversity. Here, we estimate the carrying capacity (CC) of the late Early and early Middle Pleistocene ecosystems of Europe, using equations describing the relationship between CC and climatic variables observed in the present, as well as maps of inferred paleotemperature and paleoprecipitation. Maps of paleoclimate values were interpolated from the composite benthic stable oxygen isotope ratios and a transfer function was used to estimate ungulate carrying capacity (CCU) from the interpolated mean annual temperature and annual precipitation values. Carnivoran carrying capacity was subsequently estimated from ungulate carrying capacity and the effect of CC on the carnivoran faunas was analyzed in 12 paleocommunities from Southern Europe. Our results show that carnivoran species richness is strongly related to ungulate carrying capacity in recent ecosystems, but the late Early Pleistocene paleocommunities from Southern Europe included much richer carnivore guilds than would be expected for a recent community with a similar ungulate carrying capacity. Thus, those late Early Pleistocene ecosystems supported a high number of carnivoran species, but the carnivoran biomass they could support was relatively low. Consequently, carnivorans occurred at low densities in Southern Europe compared to the recent African savanna ecosystems, but likely also compared to coeval East African ecosystems. Consequently, the first Homo populations that arrived in Europe at the end of the late Early Pleistocene found mammal communities consisting of a low number of prey species, which accounted for a moderate herbivore biomass, as well as a diverse but not very abundant carnivore guild. This relatively low carnivoran density implies that the hominin-carnivore encounter rate was lower in the European ecosystems than in the coeval East African environments, suggesting that an opportunistic omnivorous hominin would have benefited from a reduced interference from the carnivore guild.

New hyaenodonta (Mammalia) from the middle Eocene of Myanmar

The middle Eocene Pondaung Formation in Myanmar has yielded a rich mammalian fauna including several Primate taxa. Hyaenodonta are known by the genera Kyawdawia, Yarshea, Orienspterodon, and two other indeterminate taxa. We describe here new material of Kyawdawia, including some morphological details, a new species of the hypercarnivorous genus Propterodon and an indeterminate species, different from those described earlier in Myanmar, and characterized by a reduction of m3 and would belong to a third lineage with the same evolutionary trend as Galecyon and the Limnocyoninae. The hyainailourines (Orienspterodon) and hyaenodontines (Propterodon) are recorded for the first time in Southeast Asia and these subfamilies appeared in quasi the same time in Europe illustrating probably a profound change in the carnivorous fauna among Laurasia.

Large-sized theropod Spinosaurus: an important component of the carnivorous dinosaur fauna in southern continents during the Cretaceous

The Early Cretaceous of North Africa has Spinosaurinae dinosaur remains such as Spinosaurus recorded in Algeria (Guir Basin, Kem Kem beds), Egypt (Bahariya Formation), Morocco (Kem Kem beds), and Tunisia (Ain El Guettar Formation). Until now, three possible Spinosaurus species were identified: Spinosaurus aegyptiacus, Spinosaurus sp. and Spinosaurus “B”. The occurrence of this genus in the Albian-Cenomanian rocks of Africa suggests that the temporal and geographic distribution of these spinosaurines is the largest one among all genera and species of megapredators from the middle Cretaceous of Africa. The fossil record of Spinosaurus from the Albian to the Cenomanian shows a 20 million year persistence of this genus in Gondwanan ecosystems.

A new carnivoran fauna from the late Oligocene of Hungary

A new carnivoran fauna composed of rare dental and long bone remains of basal arctoid carnivores from upper Oligocene lagoon deposits of Hungary are described. Despite the small sample size, four separate taxa could be identified including the semi-aquatic basal mustelid Potamotherium valletoni, the small-sized, terrestrial basal mustelidan Amphictis sp. or Franconictis sp., another indeterminate basal mustelidan, and the medium-sized, terrestrial basal ursoid Pachycynodon boriei. These or related taxa are typically known from the Oligocene–early Miocene of Western Europe and for a much lesser extent from Eastern Asia or North America. The new Hungarian occurrence provides the first record of Oligocene carnivorans from geographically intermediate coeval localities in Eastern Europe. These remains will aid biostratigraphic correlation of the terrestrial Oligo-Miocene of Western Europe with the marine Paratethys region.

Mammalian Diversity and Matses Ethnomammalogy in Amazonian Peru Part 2: Xenarthra, Carnivora, Perissodactyla, Artiodactyla, and Sirenia

This report continues our monographic analysis of mammalian diversity and Matses ethnomammalogy in the Yavari-Ucayali interfluvial region of northeastern Peru. Based primarily on specimens collected in the region from 1926 to 2003, interviews with Matses hunters, and published sight surveys of large mammals, we document the local occurrence of 33 species of xenarthrans, carnivores, perissodactyls, artiodactyls (including cetaceans), and sirenians. All of the species in these groups, with the exception of the Amazonian manatee (Trichechus inunguis), are recognized and named by the Matses, from whom we recorded extensive accounts of mammalian natural history.The local xenarthran fauna consists of nine species (Cabassous unicinctus, Priodontes maximus, Dasypus novemcinctus, D. pastasae, Bradypus variegatus, Choloepus hoffmanni, Cyclopes didactylus, Myrmecophaga tridactyla, Tamandua tetradactyla), all of which are represented by examined specimens. Only two xenarthrans (D. pastasae and C. hoffmanni) are primary game species for the Matses, who are familiar with many aspects of their biology that were previously unrecorded in the scientific literature. However, Matses interviews also provide important new information about the behavior of D. novemcinctus (a secondary game species) and M. tridactyla, neither of which has previously been studied in rainforested environments.The local carnivore fauna consists of 16 species (Atelocynus microtis, Speothos venaticus, Leopardus pardalis, L. wiedii, Panthera onca, Puma concolor, Pu. yagouaroundi, Eira barbara, Galictis vittata, Mustela africana, Lontra longicaudis, Pteronura brasiliensis, Bassaricyon alleni, Nasua nasua, Potos flavus, Procyon cancrivorus), most of which are represented by examined specimens; six species without preserved voucher material are known from camera-trap photographs and/or unambiguous sightings by Matses hunters and field biologists. Although the coati (N. nasua) is the only carnivore occasionally hunted by the Matses for food, Matses interviews are richly informative about the natural history of other species, notably including S. venaticus, Leopardus spp., Pa. onca, Puma spp., and E. barbara.All of the local ungulates (Tapirus terrestris, Pecari tajacu, Tayassu pecari, Mazama americana, M. nemorivaga) are hunted by the Matses for food, and the hunters we interviewed are correspondingly well informed about the natural history of most of these species, with the exception of the seldom-encountered gray brocket (M. nemorivaga). Both species of local cetaceans (Inia geoffroyi, Sotalia fluviatilis) are familiar to the Matses, although neither is eaten.The xenarthrans, carnivores, ungulates, and aquatic mammals that inhabit the Yavari-Ucayali interfluve are all widespread species, so this component of the regional fauna, as currently understood, is not biogeographically distinctive, nor is it extraordinarily diverse (by western Amazonian standards). Although we discuss several noteworthy taxonomic and nomenclatural issues relevant to these taxa, the principal contribution of this report consists in the natural history information compiled from our Matses informants and the resulting overview of local community structure as defined by diurnal activity, locomotion, social behavior, and trophic relationships.

A contextual review of the Carnivora of Kanapoi

The Early Pliocene is a crucial time period in carnivoran evolution. Holarctic carnivoran faunas suffered a turnover event at the Miocene-Pliocene boundary. This event is also observed in Africa but its onset is later and the process more drawn-out. Kanapoi is one of the earliest faunas in Africa to show evidence of a fauna that is more typical Pliocene than Miocene in character. The taxa recovered from Kanapoi are: Torolutra sp., Enhydriodon (2 species), Genetta sp., Helogale sp., Homotherium sp., Dinofelis petteri, Felis sp., and Parahyaena howelli. Analysis of the broader carnivoran context of which Kanapoi is an example shows that all these taxa are characteristic of Plio-Pleistocene African faunas, rather than Miocene ones. While some are still extant and some went extinct in the Early Pleistocene, P. howelli is unique in both originating and going extinct in the Early Pliocene.

Predator-prey interactions amongst Permo-Triassic terrestrial vertebrates as a deterministic factor influencing faunal collapse and turnover.

Unlike modern mammalian communities, terrestrial Paleozoic and Mesozoic vertebrate systems were characterized by carnivore faunas that were as diverse as their herbivore faunas. The comparatively narrow food base available to carnivores in these paleosystems raises the possibility that predator-prey interactions contributed to unstable ecosystems by driving populations to extinction. Here, we develop a model of predator-prey interactions based on diversity, abundance and body size patterns observed in the Permo-Triassic vertebrate fossil record of the Karoo Basin, South Africa. Our simulations reflect empirical evidence that despite relatively high carnivore: herbivore species ratios, herbivore abundances were sufficient for carnivores to maintain required intake levels through most of the Karoo sequence. However, high mortality rates amongst herbivore populations, even accounting for birth rates of different-sized species, are predicted for assemblages immediately preceding the end-Guadalupian and end-Permian mass extinctions, as well as in the Middle Triassic when archosaurs replaced therapsids as the dominant terrestrial fauna. These results suggest that high rates of herbivore mortality could have played an important role in biodiversity declines leading up to each of these turnover events. Such declines would have made the systems especially vulnerable to subsequent stochastic events and environmental perturbations, culminating in large-scale extinctions.