Late Eocene and early Oligocene teleost and associated ichthyofauna of the Jebel Qatrani Formation, Fayum, Egypt

Fishes from the late Eocene and Oligocene Jebel Qatrani Formation of the Fayum, Egypt, have been collected for many years, but have not been extensively studied. Collections from various sites in the formation, predominantly representing riverine and shallow lake deposits, include remains of several fishes not known previously. The teleost fishes from these collections [representing Characiformes, Siluriformes, Cichlidae, Latidae (= Centropomidae), and Channidae] include species that are similar to those found in the older, underlying, Qasr el Sagha Formation (catfishes), as well as species of fishes previously unrecorded from the Fayum (cichlids and latids), or even from the Tertiary of Africa (channids). It has been suggested that the Jebel Qatrani Formation represents an area of swampy rivers with overgrown banks and floating vegetation and at least one small lake. The fish remains support this reconstruction of the palaeoenvironment, and further indicate that open riverine habitat was also probably available.     

Femoral anatomy of Aegyptopithecus zeuxis,an early Oligocene anthropoid

Three partial femora from Quarries I and M of the early Oligocene Jebel Qatrani Formation in the Fayum of Egypt are attributed to Aegyptopithecus zeuxis on the basis of their appropriate size and anthropoid morphology. Compared with extant catarrhines, Aegyptopithecus is unusual in having a distinct gluteal tuberosity (third trochanter) and a relatively deep distal femoral articulation. In the estimated neck angle, Aegyptopithecus resembles arboreal quadrupeds rather than either leaping or suspensory primates. It seems likely that the femur of this species was relatively robust and short for its body mass. In aspects of its femoral anatomy, Aegyptopithecus is quite different from the parapithecid Apidium and more similar to Catopithecus from late Eocene deposits of the Fayum, and also to small hominoids from the Miocene of East Africa. Am J Phys Anthropol 106:413–424, 1998. © 1998 Wiley-Liss, Inc.     

Earliest record of a parapithecid anthropoid from the Jebel Qatrani formation, Northern Egypt

A fifth anthropoid (= anthropoidean, simian or simiiform) genus and species from the late Eocene Fayum Quarry L-41, Abuqatrania basiodontos gen. et sp. nov., further augments the already remarkable primate diversity from this locality and provides the first convincing extension of the enigmatic family Parapithecidae into the oldest productive vertebrate fossil-bearing stratum of the Jebel Qatrani Formation. A. basiodontos exhibits no clear autapomorphies nor any apomorphies that are shared exclusively with any other parapithecid species, and it is most parsimoniously interpreted as the sister taxon of a Qatrania-Parapithecus-Apidium clade. Reevaluation of two contemporaries of A. basiodontos, Serapia and Arsinoea, suggests that neither genus should be ranked as a basal parapithecid. Serapia is more derived than primitive parapithecids in the morphology of the lower fourth premolar and exhibits greater overall similarity to Proteopithecus in cusp placement and the shape and proportions of its lower teeth; accordingly, we place Serapia in the family Proteopithecidae. Arsinoea is much more problematic and does not fit well with any hitherto known Afro-Arabian anthropoid group; we place this genus in a new anthropoid family, Arsinoeidae.     

Diets of fossil primates from the Fayum Depression of Egypt: a quantitative analysis of molar shearing

Over the last 90 years, Eocene and Oligocene aged sediments in the Fayum Depression of Egypt have yielded at least 17 genera of fossil primates. However, of this diverse sample the diets of only four early Oligocene anthropoid genera have been previously studied using quantitative methods. Here we present dietary assessments for 11 additional Fayum primate genera based on the analysis of body mass and molar shearing crest development. These studies reveal that all late Eocene Fayum anthropoids were probably frugivorous despite marked subfamilial differences in dental morphology. By contrast, late Eocene Fayum prosimians demonstrated remarkable dietary diversity, including specialized insectivory (Anchomomys), generalized frugivory (Plesiopithecus), frugivory+insectivory (Wadilemur), and strict folivory (Aframonius). This evidence that sympatric prosimians and early anthropoids jointly occupied frugivorous niches during the late Eocene reinforces the hypothesis that changes in diet did not form the primary ecological impetus for the origin of the Anthropoidea. Early Oligocene Fayum localities differ from late Eocene Fayum localities in lacking large-bodied frugivorous and folivorous prosimians, and may document the first appearance of primate communities with trophic structures like those of extant primate communities in continental Africa. A similar change in primate community structure during the Eocene-Oligocene transition is not evident in the Asian fossil record. Putative large anthropoids from the Eocene of Asia, such as Amphipithecus mogaungensis, Pondaungia cotteri, and Siamopithecus eocaenus, share with early Oligocene Fayum anthropoids derived features of molar anatomy related to an emphasis on crushing and grinding during mastication. However, these dental specializations are not seen in late Eocene Fayum anthropoids that are broadly ancestral to the later-occurring anthropoids of the Fayum's upper sequence. This lack of resemblance to undisputed Eocene African anthropoids suggests that the "progressive" anthropoid-like dental features of some large-bodied Eocene Asian primates may be the result of dietary convergence rather than close phyletic affinity with the Anthropoidea.     

A highly derived anomalurid rodent (Mammalia) from the earliest Late Eocene of Egypt

Abstract: A new genus and species of diminutive anomalurid rodent, Shazurus minutus, is described on the basis of 15 isolated teeth from the earliest late Eocene (approximately 37 Ma) Birket Qarun Locality 2 in the Fayum Depression of northern Egypt. Shazurus is surprisingly specialized for its age, being most similar in dental morphology to early Miocene Paranomalurus and extant Anomalurus, and is quite different from the roughly contemporaneous anomaluroid genera Nementchamys and Pondaungimys from Algeria and Myanmar, respectively. Parsimony analysis of dental features places Shazurus within crown Anomaluridae as a sister group of two species of Paranomalurus to the exclusion of extant Anomalurus and Idiurus. The marked morphological differences between the two oldest Afro‐Arabian anomaluroids (Shazurus and Nementchamys) suggest that the taxa share a much more ancient common Afro‐Arabian ancestor, possibly derived from Zegdoumyidae. Isolated teeth of Shazurus and other Eocene anomaluroids reveal little about their palaeobiology, but the complete absence of Anomaluroidea from the younger (late Eocene to early Oligocene) Jebel Qatrani Formation is presumably a reflection of environmental change through the late Eocene in northern Africa.     

First record of a parapithecid primate from the Oligocene of Kenya

Recent excavations in northwestern Kenya have recovered a vertebrate fauna of late early or early late Oligocene age. Among the mammal remains, a fragmentary lower jaw and an isolated upper molar have been attributed to a small primate, Lokonepithecus manai gen. et sp. nov. Lokonepithecus is a primitive member of the Parapithecidae and possibly most closely related to Apidium from the Fayum. The new primate from Kenya is the youngest parapithecid known and its occurrence in the Oligocene of Kenya suggests that sub-Saharan Africa probably played a major role in the evolutionary history of several groups of mammals.     

Oldest known Varanus (Squamata: Varanidae) from the Upper Eocene and Lower Oligocene of Egypt: support for an African origin of the genus

Abstract: A large collection of lizard vertebrae from northern Africa represents the oldest unambiguous occurrence of the genus Varanus. The fossils come from late Eocene and early Oligocene freshwater deposits of the Fayum, Egypt, an area noted for many significant primate finds. The recovery and identification of this material indicate that the genus Varanus arose in Africa, before dispersing to Australia and Asia. This dispersal occurred prior to the early to mid‐Miocene, by which time fossil Varanus are known from Australia and Eurasia. Although the dispersal route remains unknown, the lizard material reported here supports the hypothesis that a corridor existed allowing freshwater and terrestrial organisms to cross from Africa to Asia.     

Puncture marks on early African anthropoids

Field studies of living primates have shown that primate predation is a rare event. This must also have been true for past primate communities. In the Fayum Oligocene of Egypt, specimens of all four species of Upper Fossil Wood Zone primates show evidence of tooth puncture marks. Of the four potential groups of primate predators--the snakes, the raptors, the crocodiles, and the primitive carnivores or creodonts--only the crocodiles and the creodonts could have made these puncture marks. When one compares the feeding habits of living crocodiles and mammalian carnivores with the evidence from the Fayum, it appears that the Fayum primates were preyed upon and/or scavenged by mammalian carnivore-like animals. The dismemberment of the Fayum primates by Oligocene predators indicates, in part, why the Fayum fossil material is rarely articulated. Bone damage by predators may well set limits on what bone associations can be discovered in the Fayum even before the bones are scattered and buried by depositional processes.     

Micropithecus clarki, a small ape from the Miocene of Uganda.

Micropithecus clarki, from Miocene sediments of Napak, Uganda, is the smallest known hominoid primate, living or fossil. In facial morphology it is very similar to extant gibbons. Dentally, it is most similar to the small apes from the Miocene of Kenya, Dendropithecus and Limnopithecus. All of the apes from the early Miocene of East Africa seem to represent a single phyletic group that could be easily derived from the Oligocene apes known from the Fayum of Egypt. Pliopithecus from the Miocene of Europe is more closely allied with the Oligocene radiation than with the later East African radiation.     

Hindlimb of a giant terrestrial bird from the upper Eocene, Fayum, Egypt

Eremopezus eocaenus Andrews, 1904 is a giant groundbird from upper Eocene deposits of the Fayum, Egypt, which has hitherto been known from non-diagnostic fragmentary material. New fossils collected from quarry L-41 of the Jebel Qatrani Formation include two well-preserved distal tarsometatarsi and an associated whole tarsometatarsus and distal tibiotarsus that allow a more precise evaluation of the phylogenetic position and tarsal function of Eremopezus. Unlike most ratites, the distal tarsometatarsus has a patent distal foramen and a slight hallucal digit. The trochlea for digits II and IV are only slightly reduced in size, are splayed to the right, and the heads lack deep grooving. These features resemble the condition seen in BalaenicepsSagittarius, suggesting active use of the toes in grasping or manipulation, rather than the condition in graviports and cursors, which have reduced medial and lateral trochleae often with distinct grooving of the heads. The limb is relatively long and gracile, another difference from graviports. There is no compelling evidence to link Eremopezus to any known ratite lineage, to the Phorusrhacoidea, or to the extinct predatory birds of the Eocene (e.g. Diatryma, Gastornis). We suggest that Eremopezus represents an endemic African group that independently attained large size and flightlessness.     

A reassessment of the Oligocene hyracoid mammals from Malembo,Cabinda, Angola

The Oligocene Malembo locality, Cabinda exclave, Angola, has yielded a rich vertebrate fauna represented by fragmentary remains. This fossiliferous locality is the only definite occurrence of Oligocene terrestrial mammals in sub-Saharan West Africa. The hyracoids from Malembo have only been very succinctly described and compared thus far, so that their systematic attribution is not consensual among specialists. A revision now allows the identification of three (or four) medium to large-sized species represented by Geniohyus dartevellei, Pachyhyrax cf. crassidentatus, and two undetermined taxa. The species G. dartevellei is revived for the holotype of Palaeochoerus dartevellei Hooijer, 1963; this species is unique to Malembo but appears close to Geniohyus mirus, a species only known from the early Oligocene of the Fayum, Egypt. Other species of Geniohyus and Pachyhyrax crassidentatus are also only known from the early Oligocene of the Fayum. The presence of Geniohyus and Pachyhyrax cf. crassidentatus at Malembo thus supports an early Oligocene age for the fauna.     

Ichnofossils and rhizoliths of the nearshore fluvial Jebel Qatrani Formation (Oligocene), Fayum Province, Egypt

The ichnofossils and rhizoliths of the Oligocene Jebel Qatrani Formation of Egypt are among the best preserved, most diverse in form, and most abundant of such structures yet recognized in fluvial rocks. Twenty-one forms are described. The ichnofauna contains traces (domichnia, fodinichnia, cubichnia) of probable annelid, insect, crustacean, and vertebrate origin. These include the first described fossil nest structures and gallery systems of subterranean termites (Isoptera), the first examples of Ophiomorpha from wholly fluvial rocks, and the first fossil vertebrate burrows from the African Tertiary. Rhizoliths associated with the ichnofauna and those occurring elsewhere document a variety of small, wetland plants, coastal mangroves, and much larger trees. The environment suggested by these traces is consistent with the coastal, tropical to subtropical, monsoonal rain forest, with adjacent more open areas, that is indicated by independent evidence of sedimentology, paleontology, and paleopedology.     

A new anthropoid from the latest middle Eocene of Pondaung, central Myanmar

A new genus and species of medium-sized fossil primate, Myanmarpithecus yarshensis, is described from the lastest middle Eocene sediments of Pondaung, central Myanmar (Burma). The specimens consist of right maxillary fragments with P(4)-M(3)and a left mandibular corpus with C-P(3)and M(2-3). To date, three purported anthropoids have been discovered from the Pondaung Formation: Pondaungia and Amphipithecus (Amphipithecidae) and Bahinia (Eosimiidae). Myanmarpithecus differs from these other Pondaung primates in having cingular hypocones on upper molars and in lacking paraconids on M(2-3). Although Myanmarpithecus resembles some utahiin omomyines in superficial aspects of the morphology of M(2-3)(i.e., mesiodistally compressed molar trigonid and enamel crenulation), the morphological analysis of upper molars and lower premolars indicates that it is neither an omomyoid nor an adapoid but is more derived than fossil prosimians (such as adapoids, omomyoids, and tarsiers) and more anthropoid-like. On the other hand, it is more primitive (prosimian-like) than early anthropoids from the late Eocene/early Oligocene of the Fayum, Egypt. Myanmarpithecus is likely to be an early, primitive anthropoid ("protoanthropoid").     

DISCOVERY OF TWO MID-TERTIARY MAMMALIAN FAUNAS FROM HAIYUAN, NINGXIA, CHINA

Inl988-199otheRegionalGeologicalSurveyTeamoftheGeologicalBureauofNingxia(RGSN)foundsomefossilmammalsinthelowerpartoftheHo11g1iugouFormationandtheupperpartoftheOligocene.Inl992ajointteamoflnstituteofVertebratePaleontologyandPaleoanthropo1ogy,AcademiaSinica(IVPP),andtheRGSNwenttoHaiyuailCountyandcollectedmorefossilmamma1sfromtheYuanjia-wowoareausi11gascreen-washingmethodThemammalfaunafromthelowerpartoftheHongliugouFormationiscomposedofAprotodonsp.,Indricotheriidaeindet.,Rhinoceroti…     

Dietary reconstruction of the Amphipithecidae (Primates, Anthropoidea) from the Paleogene of South Asia and paleoecological implications

The primate family, Amphipithecidae, lived during the early Cenozoic in South Asia. In this study, the diet of late middle Eocene amphipithecids from the Pondaung Formation (Central Myanmar) is characterized using three different approaches: body mass estimation, shearing quotient quantification and dental microwear analysis. Our results are compared with other Paleogene amphipithecids from Thailand and Pakistan, and to the other members of the primate community from the Pondaung Formation. Our results indicate a majority of frugivores within this primate community. Pondaungia and “Amphipithecus” included hard objects, such as seeds and nuts, in their diet. Folivory is secondary for these taxa. Myanmarpithecus probably had a mixed diet based on fruit and leaves. Contrasting results and a unique dental morphology distinguish Ganlea from other amphipithecids. These render interpretation difficult but nevertheless indicate a diet tending towards leaves and fruit. However, the anterior dentition of Ganlea suggests that this taxon engaged in seed predation, using its protruding canine as a tool to husk hard fruits and obtain the soft seeds inside. Bahinia and Paukkaungia, two other Pondaung primates, are small (<500 g) and therefore would have depended on insects as their source of protein. As such, they occupied a very different ecological niche from Pondaung amphipithecids. This primate community is then compared with the Eocene-Oligocene primate communities of the Fayum from North Africa. Similarities between the late middle Eocene Pondaung primate community and extant equatorial and tropical South American primate communities are noted.     

Dispersal of African mammals in Eurasia during the Cenozoic: Ways and whys

Several groups of mammals originated in Africa and then immigrated to Eurasia during some intervals of the Cenozoic, thus greatly contributing to the mammalian biodiversity in Eurasia. Nevertheless, the African components of Eurasian mammalian faunas have had variable success in their diversification and survival. The Afro-Arabian plate remained separated from Eurasia by the Tethyan seaway, which was definitely closed in the Burdigalian, some 20 myr ago. Before its closure, the marine barrier between the Afro-Arabian and Eurasian plates did not totally prevent mammalian exchanges between these landmasses, as documented by the arrival of rodents and primates in Africa in the late Paleocene-early Eocene, the dispersal of embrithopods on both sides of the Tethyan seaway during the Eocene, and the immigration of elephantoids from Africa to Asia in late Oligocene. These events seem to be restricted to some groups of mammals, which apparently had abilities to use sweepstake dispersal routes. The massive mammalian dispersal from Africa to Eurasia started sometimes in the early Miocene, involving several groups of African mammals, in particular proboscideans, hyracoids, tubulidentates, and anthropoids. This contribution discusses the timing of these events under the light of recent discoveries of Africa-originated mammals in Eurasia. The impact of the evolving paleogeography of the area situated between the Afro-Arabian and Eurasian plates on the mammalian dispersal is reconsidered. The dispersal of land mammals from Africa to Eurasia is controlled not only by the paleogeographic changes (sea level changes, dispersal routes, terrestrial bridges, etc.), but also by climatic factors that modified the environments of terrestrial mammals, favoring or not the occurrence of dispersal routes and/or the enlargement or restriction of climatic belts and biogeographic provinces to which these mammals were adapted. These questions are discussed taking into account the present knowledge of the record of the Africa-originated mammals in Eurasia during the Cenozoic times.     

Morphology and locomotor adaptations of the foot in early Oligocene anthropoids

Newly discovered foot bones of Aegyptopithecus are described and compared to those of Apidium and Dolichocebus. Locomotor adaptations are inferred for African early Oligocene propliopithecids, parapithecids, and for Argentine early Oligocene Dolichocebus. All show an anthropoid grade of development in their foot anatomy. Tarsals of Aegyptopithecus compare best with those of Miocene hominoids. Apidium shares derived calcaneal features that link it with Old World monkeys. Dolichocebus exhibits a very generalized platyrrhine talar morphology akin to that seen in Saimiri, Callicebus, Cebus, and Aotus. The morphology of early Oligocene primate foot bones suggests that at least three quite distinct groups, corresponding to three recognized superfamilies, were present in the early Oligocene of South America and Africa.     

The Fayum primate forest: Did it exist?

The primates have the reputation of being essentially arboreal, forest-adapted animals. Yet there are many genera and species that inhabit an extremely wide array of non-forest habitats. Nevertheless, palaeoprimatologists often tend to depict fossil primate habitats as being more arboreal and more forest-like than is justified by the facts. It is worthwhile, therefore, to reconsider some current interpretations. In this paper, evidence of the Fayum Oligocene primate deposits are reviewed and discussed. The following conclusions emerge:(1) The large number of primate species indicates that the Fayum ecosystem was an optimum or near-optimum habitat for primates. (2) The lithological characteristics point to a sahélien type of climate. (3) The calcified and silicified root systems, having diameters up to 4 cm, suggest a sahélien type of shrub, bushland and/or small-tree vegetation. (4) The large fossilized logs cannot have grown on the spot and apparently represent driftwood from a more humid climatic belt in the south, as is indicated by damage resulting from fluvial transportation and by palaeobotanical data. (5) There may have been some minor patches or strips of medium-height forests and/or wood-lands in the Fayum delta, but there is no evidence of these.Thus the tall forest in which the earliest known African primates are currently supposed to have lived probably never existed. Grounds for this conclusion were presented by Unger 121 years ago, by Beadnell 75 years ago and by Kräusel 41 years ago, but sank into oblivion. The classic image of the primates as arboreal specialists seems to have interfered with seeing the facts. However, more extensive verification of the evidence by means of palaeobotanical research is still required. The fossil material to do so is readily available.     

New faces of Aegyptopithecus from the Oligocene of Egypt

Three recently discovered faces of Aegyptopithecus zeuxis from the Oligocene Jebel Qatrani Formation of Egypt provide new information about the shape and variation of the facial cranium, the earliest preserved for a presumed forerunner of apes and humans. Although varying considerably in details of shape and proportion, the new finds and a skull found in 1966 all appear to be of males, a conclusion based in part on the development of temporal and sagittal crests and on the large size of upper canines or their sockets (female canines are much smaller). The snouts of the three new faces all are shorter and broader than that of the earlier found skull as reconstructed. As in most later species of Anthropoidea, variation between these specimens is high.Aegyptopithecus helps define the nature of the oldest Anthropoidea and generally most resembles later-occurring apes. Many features, both derived and shared primitive, link Aegyptopithecus, the large Miocene great apes of the Proconsul group, and modern great apes. That these shared features and proportions are not direct allometric consequences of body size is indicated by Aegyptopithecus' resemblance to the large apes and its many distinctions from similar-sized Hylobates.In Aegyptopithecus brain volume scales smaller than in later catarrhines relative to facial size, the ectotympanic tube is less developed and the premaxilla is more primitive than in later higher primates. In closure of orbits and conformation of forehead, face and dentition, Aegyptopithecus closely resembles higher primates and not prosimians. Taken together, its overall cranial and dental anatomy constitutes one of the most important connecting links in primate evolutionary history.     

内蒙古中始新世一似ameghinornithid鸟类(鸟纲:Cariamae:Ameghinornithidae?)

内蒙古二连盆地额尔登敖包剖面(相当于伊尔丁曼哈组)的中始新世早期地层中新发现的一件标本显示其属于一个与ameghinornithid相似的种,代表了Ameghinomithidae在亚洲的首个记录.新标本具有外踝半圆形,缺失骨质腱桥,伸肌沟外侧具有大而平的结节,以及其他与ameghinomithid和似ameghinomithid鸟类共有的特征.内蒙古标本与欧洲最古老的ameghinomithids记录大体属同一时代(约48 Ma).与同时期内蒙古哺乳动物群主要由亚洲类群组成兼有少量与北美有关的绝灭类群不同,这类鸟类中始新世时在北美缺失,而存在于欧洲和亚洲.加上埃及法尤姆早渐新世地层中发现的似ameghinomithid鸟类,这类已经绝灭的鸟类的地理分布似乎比过去所认为的要广泛得多.