The 'Goldilocks' effect: preservation bias in vertebrate track assemblages

被引:70
作者
Falkingham, P. L. [1 ]
Bates, K. T. [2 ]
Margetts, L. [1 ]
Manning, P. L. [1 ,3 ]
机构
[1] Univ Manchester, Sch Earth Atmospher & Environm Sci, Manchester M13 9PL, Lancs, England
[2] Univ Liverpool, Dept Musculoskeletal Biol, Inst Aging & Chron Dis, Liverpool L69 3GE, Merseyside, England
[3] Univ Penn, Dept Earth & Environm Sci, Philadelphia, PA 19104 USA
基金
英国自然环境研究理事会; 英国工程与自然科学研究理事会;
关键词
footprint; finite-element analysis; trackway; computer modelling; dinosaur; FOSSIL RECORD; SAUROPOD DINOSAURS; UHANGRI FORMATION; FOOTPRINTS; MORPHOLOGY; MASS; REINTERPRETATION; COMPLETENESS; CONSISTENCY; UNDERTRACKS;
D O I
10.1098/rsif.2010.0634
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Finite-element analysis was used to investigate the extent of bias in the ichnological fossil record attributable to body mass. Virtual tracks were simulated for four dinosaur taxa of different sizes (Struthiomimus, Tyrannosaurus, Brachiosaurus and Edmontosaurus), in a range of substrate conditions. Outlines of autopodia were generated based upon osteology and published soft-tissue reconstructions. Loads were applied vertically to the feet equivalent to the weight of the animal, and distributed accordingly to fore- and hindlimbs where relevant. Ideal, semi-infinite elastic-plastic substrates displayed a 'Goldilocks' quality where only a narrow range of loads could produce tracks, given that small animals failed to indent the substrate, and larger animals would be unable to traverse the area without becoming mired. If a firm subsurface layer is assumed, a more complete assemblage is possible, though there is a strong bias towards larger, heavier animals. The depths of fossil tracks within an assemblage may indicate thicknesses of mechanically distinct substrate layers at the time of track formation, even when the lithified strata appear compositionally homogeneous. This work increases the effectiveness of using vertebrate tracks as palaeoenvironmental indicators in terms of inferring substrate conditions at the time of track formation. Additionally, simulated undertracks are examined, and it is shown that complex deformation beneath the foot may not be indicative of limb kinematics as has been previously interpreted, but instead ridges and undulations at the base of a track may be a function of sediment displacement vectors and pedal morphology.
引用
收藏
页码:1142 / 1154
页数:13
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