Abstract

AbstractThe fossil record is notoriously imperfect and biased in representation, hindering our ability to place fossil specimens into an evolutionary context. For groups with fossil records mostly consisting of disarticulated parts (e.g., vertebrates, echinoderms, plants), the limited morphological information preserved sparks concerns about whether fossils retain reliable evidence of phylogenetic relationships and lends uncertainty to analyses of diversification, paleobiogeography, and biostratigraphy in Earth's history. To address whether a fragmentary past can be trusted, we need to assess whether incompleteness affects the quality of phylogenetic information contained in fossil data. Herein, we characterize skeletal incompleteness bias in a large dataset (6585 specimens; 14,417 skeletal elements) of fossil squamates (lizards, snakes, amphisbaenians, and mosasaurs). We show that jaws + palatal bones, vertebrae, and ribs appear more frequently in the fossil record than other parts of the skeleton. This incomplete anatomical representation in the fossil record is biased against regions of the skeleton that contain the majority of morphological phylogenetic characters used to assess squamate evolutionary relationships. Despite this bias, parsimony- and model-based comparative analyses indicate that the most frequently occurring parts of the skeleton in the fossil record retain similar levels of phylogenetic signal as parts of the skeleton that are rarer. These results demonstrate that the biased squamate fossil record contains reliable phylogenetic information and support our ability to place incomplete fossils in the tree of life.

Highlights

  • The fossil record is a fundamental natural historical archive for understanding evolution and Earth’s history

  • We sampled for the number of occurrences of fossil squamate skeletal elements belonging to each region

  • (2.67%, n = 82) make up almost all of the remaining occurrences. These results reveal that the majority of fossil squamate morphological data (84.28%; Supplementary Fig. S3A) in museum collections is from the axial and jaws + palatal regions of the skeleton, whereas other regions of the skeleton do not occur as frequently

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Summary

Introduction

The fossil record is a fundamental natural historical archive for understanding evolution and Earth’s history. Behind the illuminating biological information contained in the fossil record is the reality that fossil data are inherently incomplete (Darwin 1859; Foote and Sepkoski 1999; Smith 2001; Kidwell and Holland 2002), due to geological factors (Raup 1976; Smith and McGowan 2005), factors related to fossil preservation (e.g., taphonomic bias; Sansom et al 2010), and asymmetrical research interest and sampling intensity among workers (e.g., sampling bias; Smith 1994, 2001).

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