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Bone-Breaking Bite Force of Basilosaurus isis (转发)

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Abstract
Bite marks suggest that the late Eocence archaeocete whale Basilosaurus isis (Birket Qarun Formation, Egypt) fed upon juveniles of the contemporary basilosaurid Dorudon atrox. Finite element analysis (FEA) of a nearly complete adult cranium of B. isis enables estimates of its bite force and tests the animal’s capabilities for crushing bone. Two loadcases reflect different biting scenarios: 1) an intitial closing phase, with all adductors active and a full condylar reaction force; and 2) a shearing phase, with the posterior temporalis active and minimized condylar force. The latter is considered probable when the jaws were nearly closed because the preserved jaws do not articulate as the molariform teeth come into occulusion. Reaction forces with all muscles active indicate that B. isis maintained relatively greater bite force anteriorly than seen in large crocodilians, and exerted a maximum bite force of at least 16,400 N at its upper P3. Under the shearing scenario with minimized condylar forces, tooth reaction forces could exceed 20,000 N despite lower magnitudes of muscle force. These bite forces at the teeth are consistent with bone indentations on Dorudon crania, reatract-and-shear hypotheses of Basilosaurus bite function, and seizure of prey by anterior teeth as proposed for other archaeocetes. The whale’s bite forces match those estimated for pliosaurus when skull lengths are equalized, suggesting similar tradeoffs of bite function and hydrodynamics. Reaction forces in B. isis were lower than maxima estimated for large crocodylians and carnivorous dinosaurs. However, comparison of force estimates from FEA and regression data indicate that B. isis exerted the largest bite forces yet estimated for any mammal, and greater force than expected from its skull width. Cephalic feeding biomechanics of Basilosaurus isis are thus consistent with habitual predation.
Citation: Snively E, Fahlke JM, Welsh RC (2015) Bone-Breaking Bite Force of Basilosaurus isis (Mammalia, Cetacea) from the Late Eocene of Egypt Estimated by Finite Element Analysis. PLoS ONE 10(2): e0118380. https://doi.org/10.1371/journal.pone.0118380
Academic Editor: Andrea B. Taylor, Duke University School of Medicine, UNITED STATES
Received: July 22, 2014; Accepted: January 15, 2015; Published: February 25, 2015
Copyright: © 2015 Snively et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited
Data Availability: All relevant data can be found within the manuscript and Supporting Information files.
Funding: Funding was provided by a Feodor Lynen Fellowship of the Alexander von Humboldt Foundation (JMF), Russ College, Ohio University, Athens (ES), and the College of Science and Health, University of Wisconsin–La Crosse (ES). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.


IP属地:北京1楼2024-07-09 11:17回复
    IntroductionCetacean Evolution
    Modern cetaceans (Odontoceti and Mysticeti) emerged from archaeocete whales in the latest Eocene or earliest Oligocene, ca. 34 m.y.a. [1], [2], [3], [4]. Archaeocetes originated from terrestrial artiodactyls around the Paleocene-Eocene boundary, ca. 54 m.y.a. [3], [5], [6], with the earliest representatives of archaeocete whales appearing in the early Eocene [4].
    The transition from life on land to life in the sea took place within archaeocetes throughout the Eocene, as is documented by various semiaquatic (protocetids, ambulocetids, and remingtonocetids) and fully-aquatic forms (basilosaurids) in the middle and late Eocene, respectively (for reviews see, e.g., [3], [4]). This transition brought about morphological and functional changes that affected not only the locomotor apparatus, sensory and reproductive organs, but also feeding and diet [3], [7], [8], [9], [10], [11], [12], [13]. Isotopic and morphological studies [14], [15], [16] show that the transition to a marine environment happened relatively fast, and that semiaquatic forms were likely already marine.
    Feeding and Diet
    Primitive terrestrial artiodactyls had bunodont teeth, and were most likely herbivorous and chewed their food [13]. Modern whales, on the other hand, do not masticate. Mysticetes filter-feed, while odontocetes capture their prey and swallow it whole or in large pieces. Suction feeding is also widespread in both groups [17], [18], [19].
    Shearing facets on the cheek teeth of archaeocete whales indicate that archaeocetes chewed their food. Pakicetids and protocetids had a protocone on their molars, indicating that some grinding function was retained. The cheek teeth of basilosaurids were mediolaterally compressed and lacked grinding surfaces [13], [20]. Fahlke et al. [21] observed tooth wear and bite marks suggesting that the basilosauridBasilosaurus isisused a single, orthal-retractional occlusal movement to puncture, crush, and shear its food.
    Stomach conten


    IP属地:北京来自Android客户端2楼2024-07-09 11:18
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