Jeheskel Shoshani

Elephant brain. Part I: gross morphology, functions, comparative anatomy, and evolution.

We report morphological data on brains of four African, Loxodonta africana, and three Asian elephants, Elephas maximus, and compare findings to literature. Brains exhibit a gyral pattern more complex and with more numerous gyri than in primates, humans included, and in carnivores, but less complex than in cetaceans. Cerebral frontal, parietal, temporal, limbic, and insular lobes are well developed, whereas the occipital lobe is relatively small. The insula is not as opercularized as in man. The temporal lobe is disproportionately large and expands laterally. Humans and elephants have three parallel temporal gyri: superior, middle, and inferior. Hippocampal sizes in elephants and humans are comparable, but proportionally smaller in elephant. A possible carotid rete was observed at the base of the brain. Brain size appears to be related to body size, ecology, sociality, and longevity. Elephant adult brain averages 4783 g, the largest among living and extinct terrestrial mammals; elephant neonate brain averages 50% of its adult brain weight (25% in humans). Cerebellar weight averages 18.6% of brain (1.8 times larger than in humans). During evolution, encephalization quotient has increased by 10-fold (0.2 for extinct Moeritherium, approximately 2.0 for extant elephants). We present 20 figures of the elephant brain, 16 of which contain new material. Similarities between human and elephant brains could be due to convergent evolution; both display mosaic characters and are highly derived mammals. Humans and elephants use and make tools and show a range of complex learning skills and behaviors. In elephants, the large amount of cerebral cortex, especially in the temporal lobe, and the well-developed olfactory system, structures associated with complex learning and behavioral functions in humans, may provide the substrate for such complex skills and behavior.

Understanding proboscidean evolution: a formidable task

A new approach to proboscidean evolution depicts taxa in three major radiations. This approach highlights general proboscidean evolutionary trends and origins more than the specific relationships among them. Data from more than 55 million years of evolution help to interpret how the integration of primitive and derived characters was essential to proboscidean success. Only two, or perhaps three, species remain of approximately 164 that lived in the past. Extinct forms were extremely cosmopolitan, occupying a variety of habitats, from deserts to mountain tops, on all continents except Australia and Antarctica. Challenges for future investigators include a better understanding of structure and function of infrasonic call production and perception, brain features, and reproductive biology in extinct proboscideans based on inferences from living forms.

A proboscidean from the late oligocene of eritrea, a "missing link" between early elephantiformes and elephantimorpha, and biogeographic implications

We report on a late Oligocene proboscidean species from Eritrea, dated to 26.8 ± 1.5 Mya. This “missing link” between early elephantiformes and Elephantimorpha is the oldest known nongomphothere proboscidean to probably display horizontal tooth displacement, typical of elephants [Elephantimorpha consists of Mammutida (mastodons) and Elephantida, and Elephantida includes gomphotheres, stegodons, and elephants]. Together with the newly discovered late Oligocene gomphotheres from Chilga, Ethiopia, the Eritrean taxon points to the importance of East Africa as a major area for the knowledge of the early evolution of Elephantimorpha before the faunal exchange between Eurasia and Africa.

FOSSIL REPTILES FROM THE PLEISTOCENE HOMO -BEARING LOCALITY OF BUIA (ERITREA, NORTHERN DANAKIL DEPRESSION)

The early to early-Middle Pleistocene fossil assemblage form the Buia area (Northern Danakil Depression, Eritrea) hosts, along with Homo and several other large mammal taxa, the following reptiles: Nile Crocodile, Crocodylus niloticus , Serrated Hinged Terrapin, Pelusios cf. P. sinuatus, Nile Monitor, Varanus niloticus and African Rock Python , Python gr. sebae . All the identified taxa belong to living species. At present, these taxa do not occur in the Northern Danakil depression since it is an arid area. P. sinuatus is not a member of the Eritrean herpetofauna. Although the marked preponderance of the crocodile remains is probably connected to the taphonomy of the sites and the collecting methods used, the ecological value of the reptile fauna corroborates that of the mammals, in indicating a lacustrine or fluvio-deltaic palaeoenvironment and a tropical/subtropical or even sub-Sahelic climate. The Buia remains represent the first reported Eritrean palaeoherpetofauna.

THE ELEPHANTS OF ZOBA GASH BARKA, ERITREA: PART 4. CHOLELITHIASIS IN A WILD AFRICAN ELEPHANT (LOXODONTA AFRICANA)

Abstract A 4.0-kg cholelith was found within the abdominal cavity of a dead wild African elephant (Loxodonta africana) in Eritrea. Analysis of this cholelith by histochemistry, electron microscopy, electrospray mass spectroscopy, and energy-dispersive x-ray spectroscopy revealed it was composed of bile alcohols but no calcium, bilirubin, or cholesterol. Bacteria were also found in the cholelith. Similar, but smaller, bile stones have been identified previously in other wild African elephants and an excavated mammoth (Mammuthus columbi). Choleliths have been reported only once in a captive Asian elephant (Elephas maximus). Elephants, along with hyraxes (Procavia capensis) and manatees (Trichechus manatus), are unique among mammals in producing only bile alcohols and no bile acids, which may predispose them to cholelithiasis, particularly in association with bacterial infection. Dietary factors may also play an important role in cholelith formation.