Microwear–mesowear congruence and mortality bias in rhinoceros mass-death assemblages

Paleobiology ◽  
2017 ◽  
Vol 44 (1) ◽  
pp. 131-154 ◽  
Author(s):  
Matthew C. Mihlbachler ◽  
Daniel Campbell ◽  
Charlotte Chen ◽  
Michael Ayoub ◽  
Pawandeep Kaur

AbstractAlthough we do not know the cause of death of most fossil animals, mortality is often associated with ecological stress due to seasonality and other stochastic events (droughts, storms, volcanism) that may have caused shifts in feeding ecology preceding death. In these instances, dental microwear, which reflects feeding ecology in a narrow window of time, may provide a biased view of diet. Mesowear, another dental-wear proxy based on the morphology of worn cusps, requires macroscopic amounts of dental wear and reflects diet for a longer interval and may be less prone to bias from near-death ecological stress. We compared congruence between microwear and mesowear of North American, fossil rhinocerotid mass-death assemblages and collections of hunted modern rhinocerotids to test the hypothesis that fossil assemblages yield more incongruous microwear and mesowear data as a result of near-death ecological disturbances. In extant rhinos, both mesowear and microwear are associated with diet and height of the feeding environment. Mesowear and microwear in the modern rhinocerotid collections are statistically correlated, with strong relationships between average mesowear scores and labially distributed dental microwear. In contrast, a relationship between mesowear and microwear was not observed among the fossil rhinocerotid assemblages. Mesowear suggests that the fossil rhinos had low-abrasion diets, suggesting that they fed from clean, possibly tall vegetation. Some, but not all, mass-death assemblages produce microwear data with excessive scratches and/or pits compared with expectations based on mesowear results, suggesting that dental microwear was altered shortly before death in some but not all of the fossil assemblages. The dental-wear proxies available to paleoecologists provide a mosaic of dietary evidence reflecting diet over long (mesowear) and more abbreviated (microwear) periods of time that, together, provide a richer understanding of feeding ecology and its relationship to environment, seasonal change, and other ecological disturbances.

2021 ◽  
Vol 18 (180) ◽  
pp. 20210139
Author(s):  
Nicole L. Ackermans ◽  
Daniela E. Winkler ◽  
Ellen Schulz-Kornas ◽  
Thomas M. Kaiser ◽  
Louise F. Martin ◽  
...  

Dietary reconstruction in vertebrates often relies on dental wear-based proxies. Although these proxies are widely applied, the contributions of physical and mechanical processes leading to meso- and microwear are still unclear. We tested their correlation using sheep ( Ovis aries , n = 39) fed diets of varying abrasiveness for 17 months as a model. Volumetric crown tissue loss, mesowear change and dental microwear texture analysis (DMTA) were all applied to the same teeth. We hereby correlate: (i) 46 DMTA parameters with each other, for the maxillary molars (M1, M2, M3), and the second mandibular molar (m2); (ii) 10 mesowear variables to each other and to DMTA for M1, M2, M3 and m2; and (iii) volumetric crown tissue loss to mesowear and DMTA for M2. As expected, many DMTA parameters correlated strongly with each other, supporting the application of reduced parameter sets in future studies. Correlation results showed only few DMTA parameters correlated with volumetric tissue change and even less so with mesowear variables, with no correlation between mesowear and volumetric tissue change. These findings caution against interpreting DMTA and mesowear patterns in terms of actual tissue removal until these dental wear processes can be better understood at microscopic and macroscopic levels.


Paleobiology ◽  
2008 ◽  
Vol 34 (1) ◽  
pp. 117-127 ◽  
Author(s):  
Florent Rivals ◽  
Ellen Schulz ◽  
Thomas M. Kaiser

The Caune de l'Arago Cave (southern France) has yielded one of the best preserved and best documented sedimentary successions of the European Middle Pleistocene (Oxygen Isotopic Stages 14 to 12). Herbivorous ungulates (horse, reindeer, red deer, fallow deer, bison, musk ox, argali, and tahr) are well represented in the three major stratigraphic units CM1, CM2, and CM3. CM1 and CM3 correspond to cold and dry climate and CM2 represents temperate and humid environmental conditions. Dental microwear and mesowear analyses were performed for the ungulates from CM1–3 to test whether these methods of dental wear evaluation were suitable for detecting climate-driven changes in the dietary resources of the Arago ungulate community. We found that both dental mesowear and microwear indicate dietary traits and their relationship to climatic conditions as reflected by vegetation cover and community structure. In all units, even if some species seem to share habitats or resources, it appears that the overlap in their feeding ecology is very low. The CM1 and CM3 units, where pollen analysis indicates that the climate was cold and dry, show the lowest diversity in dietary traits. The CM2, where climate is known to be more temperate and humid, the spectrum of dietary traits is large—grazers, browsers, and mixed feeders are present.


2016 ◽  
Vol 62 (1) ◽  
pp. 111-120 ◽  
Author(s):  
Olivier Bignon-lau ◽  
Natacha Catz ◽  
Emilie Berlioz ◽  
Vebjørn Veiberg ◽  
Olav Strand ◽  
...  

2020 ◽  
Vol 142 ◽  
pp. 102736 ◽  
Author(s):  
L.M. Martínez ◽  
F. Estebaranz-Sánchez ◽  
C. Ferràndez-Cañadell ◽  
A. Romero ◽  
F. Ribot ◽  
...  

2018 ◽  
Vol 496 ◽  
pp. 103-120 ◽  
Author(s):  
Cécile Blondel ◽  
John Rowan ◽  
Gildas Merceron ◽  
Faysal Bibi ◽  
Enquye Negash ◽  
...  
Keyword(s):  

Ameghiniana ◽  
2015 ◽  
Vol 52 (5) ◽  
pp. 502-516 ◽  
Author(s):  
Victor M. Bravo-Cuevas ◽  
Jaime Priego-Vargas ◽  
Eduardo Jiménez-Hidalgo ◽  
Christian R. Barrón-Ortiz ◽  
Jessica M. Theodor ◽  
...  

PeerJ ◽  
2016 ◽  
Vol 4 ◽  
pp. e2132 ◽  
Author(s):  
Frank J. Varriale

Extensive oral processing of food through dental occlusion and orbital mandibular movement is often cited as a uniquely mammalian trait that contributed to their evolutionary success. Save for mandibular translation, these adaptations are not seen in extant archosaurs or lepidosaurs. In contrast, some ornithischian dinosaurs show evidence of precise dental occlusion, habitual intraoral trituration and complex jaw motion. To date, however, a robust understanding of the diversity of jaw mechanics within non-avian dinosaurs, and its comparison with other vertebrates, remains unrealized. Large dental batteries, well-developed dental wear facets, and robust jaws suggests that neoceratopsian (horned) dinosaurs were capable chewers. But, biomechanical analyses have assumed a relatively simple, scissor-like (orthal) jaw mechanism for these animals. New analyses of dental microwear, presented here, show curvilinear striations on the teeth ofLeptoceratops. These features indicate a rostral to caudal orbital motion of the mandible during chewing. A rostrocaudal mandibular orbit is seen in multituberculates, haramiyid allotherians, and some rodents, and its identification inLeptoceratops gracilisis the first evidence of complex, mammal-like chewing in a ceratopsian dinosaur. The term circumpalinal is here proposed to distinguish this new style of chewing from other models of ceratopsian mastication that also involve a palinal component. This previously unrecognized complexity in dinosaurian jaw mechanics indicates that some neoceratopsian dinosaurs achieved a mammalian level of masticatory efficiency through novel adaptive solutions.


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