bioRxiv Science⌕ Search

bioRxiv · 10.1101/2024.04.17.589495

Evolutionary paleoecology of European rhinocerotids across the Oligocene-Miocene transition

Abstract

The Oligocene-Miocene transition witnessed great environmental and faunal changes, but its drivers and consequences on mammals remain poorly understood. Rhinocerotoids are among the most affected taxa, reflected by great taxonomical (extinction of all non-rhinocerotids) and morphological (e.g., more mediportal forms) changes observed during this interval. However, potential associated changes in ecology have not been explored. Here, we investigated the paleoecology of 10 rhinocerotid species coming from 15 localities across Western and Central Europe and ranging from Mammal Paleogene reference level 28 to Mammal Neogene zone 3. We explored evolutionary trends for their diet, physiology, and habitat via dental wear, hypoplasia, body mass estimates, and stable isotopy. Our results (isotopy, dental wear) suggest that all rhinocerotids studied were C3 feeders, whether browsing or mixed-feeding, but niche partitioning was assumed at some localities: distinct dietary preferences and/or habitats were highlighted at Gaimersheim, Ulm-Westtangente, and Rickenbach, whereas a potential competition for the resources or different niche partitioning strategies (body mass, feeding height) are hypothesized at others localities (La Milloque, Thezels, Paulhiac). We reconstructed similar warm conditions at all localities except Gaimersheim, but found greater variations in precipitation. Indeed, a clear shift in {delta}13CCO3, enamel values was noticed at the end of the Oligocene, consistent with climatic changes (Mi-1) and vegetation modifications reported at that time. Despite these great changes, the prevalence of hypoplasia was low (< 10 %) to moderate (< 20 %) except at some localities (Pappenheim, Rickenbach, Engehalde) and for some species (Brachydiceratherium aurelianense and B. lamilloquense). Teleoceratines were particularly affected, suggesting a potential phylogenetic effect. Fourth milk molars and third molars were the most affected loci, indicating stresses around birth and environmental stresses respectively. Body mass co-variated with hypoplasia prevalence, indicating that larger species might be more susceptible to stresses and environmental changes. The tracking of rhinocerotids paleoecological preferences during the Oligocene-Miocene revealed several changes in diet and habitat (temperature, precipitation, vegetation) consistent with global changes during this period.

Explore related subjects

Keep this discovery

Explore connections, maps & timelines

BibTeXRIS

Hullot, M., Martin, C., Blondel, C., Becker, D., Roessner, G. E.. 2024-04-19. Evolutionary paleoecology of European rhinocerotids across the Oligocene-Miocene transition. https://doi.org/10.1101/2024.04.17.589495

Cite the original work for its findings. Save a collection to share your selection of sources.

KEEP EXPLORING

Related preprints

Unique pattern of injuries in Olenoides serratus from the Burgess Shale elucidate moulting process in trilobites

Ecdysozoans is one of the most abundant and diverse groups of metazoans and grow through moulting the rigid exoskeleton that provided protection. But the moulting process is often dangerous, resulting in malformations or death. Injuries have been well documented in the calcitic exoskeleton of trilobites, some of which have been attributed to moulting complications when long spines are deformed. Injuries in trilobites are often found in the trunk rather than the cephalon, and abnormal genal spines are rarely documented. Here we examine injuries in eleven specimens of Olenoides serratus from the Burgess Shale (Cambrian, Wuluian) and demonstrate an increased frequency of genal spine malformations compared to other trilobites. The unusual pattern of malformations may be attributed to moulting injuries of the long and delicate genal spines in O. serratus. To moult, trilobites curved ventrally to press the anterior margin of their cephalon into the substrate and open the facial sutures. This process exerted force on the librigenae. To exit the exuvia, the genal spines were forced to bend as the old librigenae dipped ventrally along the anterior edge, resulting in the injured genal spines in O. serratus. A similar process of moulting resulting in injuries may be seen in other early Euarthropods.

paleontology↗

Bone diagenesis in Iron Age Siberia: a histological and microtomographic study of Tunnug 1 (Russia, 2nd-4th c. CE)

The Siberian site of Tunnug 1, located in the Uyuk Valley (Tuva Republic, Russia), encompasses an Early Scythian burial mound (9th century BCE) and a peripheral cemetery attributed to the Kokel culture (2nd-4th centuries CE). Situated within a permafrost-affected environment, the site offers an opportunity to investigate bone preservation under long-term freeze-thaw cycle conditions and explore the relationship between funerary treatment and bone diagenesis. This study presents a combined histological and microtomographic analysis of 76 bone samples from 71 individuals across 36 burials. Transmitted light microscopy, scanning electron microscopy (SEM) and micro-computed tomography (micro-CT) were employed to document biological, chemical and physical degradation. Bone preservation was evaluated through three approaches: the traditional Oxford Histological Index (OHI), quantitative image analysis and assessment of (micro)cracking. The results revealed moderate bone preservation (OHI 2-4). Biological degradation in the form of Microscopical Focal Destruction (MFD) and chemical alteration were identified in six individuals. Enlarged canaliculi were observed in every bone sample. Microcracks were present in all individuals, visible exclusively under SEM. No clear diagenetic signatures linked to specific funerary practices were identified, though variations in preservation suggest a possible influence of burial depth. The distinct impact of permafrost and long-term freeze-thaw cycles on bone microstructure could not be isolated, underscoring the multifactorial nature of diagenesis. This study highlights the complementary value of combining multiple analytical methods assessing bone diagenesis and emphasises the need for continued experimental research into the effects of freezing environments on human remains.

paleontology↗

NOTE ON RHEIFORMES (AVES: PALAEOGNATHAE) FROM A QUATERNARY CAVE IN THE LAGOA SANTA KARST, EASTERN BRAZIL

Rheiformes are a South American lineage of large, flightless palaeognathous birds, currently represented by the genus Rhea and the two extant species R. americana and R. pennata. The fossil record of the group extends back to the Eocene, with its greatest diversification occurring during the Neogene. During the Quaternary, Rheiformes were widely distributed across southern and central South America. The Lagoa Santa region is particularly notable for its rich paleontological and archaeological record. Quaternary records of Rheiformes from caves in this region provide important evidence for understanding the distribution of the group in Brazil, although their chronological context remains uncertain owing to the absence of direct dating. Here, we describe and illustrate two rheiform bones recovered from a cave in the Lagoa Santa karst region. The material comprises a partially complete tibiotarsus and a fragmented tarsometatarsus, interpreted as belonging to a single individual. Comparative anatomical and morphometric analyses support their attribution to Rhea americana, based on morphological features and dimensions consistent with adult specimens of the species. This occurrence extends the Quaternary record of Rheiformes in the Lagoa Santa region and contributes to the fossil and subfossil record of Rhea in Brazil. The absence of stratigraphic and geochronological control precludes a precise age determination. Although the association with an extinct dasypodid indicates the presence of Late Pleistocene or Early Holocene faunal elements at the locality, a Holocene or even recent age for the rheiform remains cannot be excluded.

paleontology↗