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1 how data from extant species can complement paleontological accounts of evolutionary history, openin
2 ary interplay between traditional taphonomic-paleontological analysis and artificial intelligence-bas
3 tons also present a rich record that enables paleontological analysis of coral origins, tracing them
6 mbined with further syntheses of Pleistocene paleontological and archaeological records and spatio-te
7 from Egyptian antiquity with direct lines of paleontological and archeological evidence to infer loca
11 group,(4)(,)(5) an idea later challenged by paleontological and developmental data.(4)(,)(6)(,)(7)(,
13 ary biology is the apparent conflict between paleontological and embryological evidence regarding the
18 in primate evolution is the discord between paleontological and molecular clock estimates for the ti
20 supplies an interesting case-study in which paleontological and neontological data can integrate and
21 rd origins provides a premier example of how paleontological and neontological data can interact to r
22 t is made difficult by discrepancies between paleontological and neontological data, mammalian tooth
28 ng with floral, invertebrate, and vertebrate paleontological and taphonomic evidence associated with
30 gruent evidence obtained from morphological, paleontological, and genetic data for the majority of ex
35 rate ancestry is supported by morphological, paleontological, and paleoclimatic evidence, which colle
36 he dating and correlating of archaeological, paleontological, and paleoenvironmental data between seq
39 ontological approach complements more common paleontological approaches to discover directional trend
41 monstrates that genetic information spanning paleontological, archaeological, and modern contexts is
42 element alteration of phosphatic tissues in paleontological, archeological, and crystal-chemical con
45 he same time, the long timescales over which paleontological changes are usually assessed are beyond
46 uman primates and extensive osteological and paleontological collections to refine our assessment of
48 namented microfossils comprise a distinctive paleontological component of sedimentary rocks deposited
49 of cerium geochemistry at the microscale in paleontological contexts, in particular across fossil hi
51 lyse detailed phylogenies of amniote clades, paleontological data and simulations to reveal the mecha
52 e new phylogenetic tree, paleoecological and paleontological data as well as data on the biology of p
54 easonable estimates of functional diversity, paleontological data could provide information on ecolog
57 allows for the integration of molecular and paleontological data in deciphering one of the most inno
58 he reliability of continuous geochemical and paleontological data in individual sections and of inter
59 n modern taxa highlights the significance of paleontological data in understanding drivers of evoluti
60 ium isotopes, Pacific volcanic ash beds, and paleontological data just above OJN basalts illustrate t
61 rhine monkeys, and the scarcity of available paleontological data precludes elucidating firmly their
66 nalyses of embryological, morphological, and paleontological data suggest that proboscideans and sire
68 0) We combine developmental information with paleontological data to evaluate the evolution of the ty
69 for three research directions: (i) leverage paleontological data to reveal long-term biodiversity re
71 likely to come from morphological studies of paleontological data, whether known or still to be disco
76 s the utility of bridging archaeological and paleontological datasets to disentangle complex biogeogr
77 two phenotypes vary across neontological and paleontological datasets, we find that the major Middle
79 explain discrepancies between molecular and paleontological dates for explosive radiations in the fo
80 wever, the discrepancy between molecular and paleontological dates for three key "explosive" radiatio
86 ined with additional ecological experiments, paleontological documentation, isotope geochemistry and
87 esolve the discordance between molecular and paleontological estimates for divergence date estimates
90 teps by providing a framework; however, only paleontological evidence can determine the sequence of m
91 chemical evidence for anoxic conditions, but paleontological evidence for at least episodically oxic
92 ttus split or a more basal split, conclusive paleontological evidence for the nodal assignments has b
98 stimates of divergence times consistent with paleontological evidence over a range of perissodactyl r
100 eater bamboo lemur is critically endangered, paleontological evidence shows that it was once broadly
102 pedal terrestrial precursor, yet some recent paleontological evidence suggests that adaptations for b
106 ne is dysmorphic, prompted us to reconstruct paleontological evidence, highlighting specific transiti
107 om a theoretical standpoint and supported by paleontological evidence, we lack a practical understand
112 d production of local rare earth patterns in paleontological fossil tissues through X-ray fluorescenc
114 Less clear, however, is how to integrate the paleontological information with molecular phylogeny and
115 with previous comparative, developmental and paleontological information, our findings suggest that t
117 oorganisms, and provide good comparisons for paleontological interpretation of ancient hydrothermal s
118 Next, we use systematic, molecular, and paleontological lines of evidence to argue that the late
120 and applying spatiotemporal phylogenetic and paleontological models of diversification for tetrapod s
121 process are unable to explain this uniquely paleontological observation of faunawide coordinated sta
133 phology, ecology, chemical defenses, and the paleontological record of the group's ancient history.
135 hip between temperature and diversity in the paleontological record over the last 145 million years.
138 d the lack of comprehensive, well-calibrated paleontological records, especially in terrestrial envir
142 zed and characterized, and open new lines of paleontological research with taxonomic, taphonomic, phy
147 ompiled lists of direct radiocarbon dates on paleontological specimens of extinct genera from North a
153 an-chimpanzee divergence, from molecular and paleontological studies, are unlikely to be correct.
158 fossils from sub-Saharan Africa has limited paleontological testing of competing models of recent hu
160 of morphological evolution obtained from the paleontological time-series with phylogenetic rates indi
161 e persistence of DNA over archaeological and paleontological timescales in diverse environments has l
162 plant) evolution, but also offers additional paleontological treasures, including animals (mostly art