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1 how data from extant species can complement paleontological accounts of evolutionary history, openin
2 from Egyptian antiquity with direct lines of paleontological and archeological evidence to infer loca
6 ary biology is the apparent conflict between paleontological and embryological evidence regarding the
8 in primate evolution is the discord between paleontological and molecular clock estimates for the ti
10 rd origins provides a premier example of how paleontological and neontological data can interact to r
13 ng with floral, invertebrate, and vertebrate paleontological and taphonomic evidence associated with
16 rate ancestry is supported by morphological, paleontological, and paleoclimatic evidence, which colle
17 he dating and correlating of archaeological, paleontological, and paleoenvironmental data between seq
19 ontological approach complements more common paleontological approaches to discover directional trend
21 element alteration of phosphatic tissues in paleontological, archeological, and crystal-chemical con
24 uman primates and extensive osteological and paleontological collections to refine our assessment of
25 namented microfossils comprise a distinctive paleontological component of sedimentary rocks deposited
26 of cerium geochemistry at the microscale in paleontological contexts, in particular across fossil hi
28 lyse detailed phylogenies of amniote clades, paleontological data and simulations to reveal the mecha
32 allows for the integration of molecular and paleontological data in deciphering one of the most inno
33 he reliability of continuous geochemical and paleontological data in individual sections and of inter
36 nalyses of embryological, morphological, and paleontological data suggest that proboscideans and sire
38 likely to come from morphological studies of paleontological data, whether known or still to be disco
40 two phenotypes vary across neontological and paleontological datasets, we find that the major Middle
42 explain discrepancies between molecular and paleontological dates for explosive radiations in the fo
43 wever, the discrepancy between molecular and paleontological dates for three key "explosive" radiatio
48 esolve the discordance between molecular and paleontological estimates for divergence date estimates
51 teps by providing a framework; however, only paleontological evidence can determine the sequence of m
52 chemical evidence for anoxic conditions, but paleontological evidence for at least episodically oxic
53 ttus split or a more basal split, conclusive paleontological evidence for the nodal assignments has b
58 stimates of divergence times consistent with paleontological evidence over a range of perissodactyl r
59 eater bamboo lemur is critically endangered, paleontological evidence shows that it was once broadly
61 pedal terrestrial precursor, yet some recent paleontological evidence suggests that adaptations for b
64 om a theoretical standpoint and supported by paleontological evidence, we lack a practical understand
67 d production of local rare earth patterns in paleontological fossil tissues through X-ray fluorescenc
69 Less clear, however, is how to integrate the paleontological information with molecular phylogeny and
70 with previous comparative, developmental and paleontological information, our findings suggest that t
71 oorganisms, and provide good comparisons for paleontological interpretation of ancient hydrothermal s
74 process are unable to explain this uniquely paleontological observation of faunawide coordinated sta
80 phology, ecology, chemical defenses, and the paleontological record of the group's ancient history.
88 ompiled lists of direct radiocarbon dates on paleontological specimens of extinct genera from North a
91 an-chimpanzee divergence, from molecular and paleontological studies, are unlikely to be correct.
93 fossils from sub-Saharan Africa has limited paleontological testing of competing models of recent hu
94 of morphological evolution obtained from the paleontological time-series with phylogenetic rates indi
95 e persistence of DNA over archaeological and paleontological timescales in diverse environments has l
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