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1 d samples from a 1.1-million-year-old steppe mammoth.
2 l decline and later extinction of the woolly mammoth.
3 ctic climate, similar to those of the woolly mammoth.
4 re likely to have been present in the woolly mammoth.
5 om an existing structural alignment program, MAMMOTH.
6 t in the Pleistocene evolutionary history of mammoths.
7 the small ear size in Late Quaternary woolly mammoths.
8 nal profiles from 10 Late Pleistocene woolly mammoths.
9 flesh-including the tough flesh of juvenile mammoths.
11 that H. serum preferentially hunted juvenile mammoths.(1)(,)(4) Dietary data of Homotherium are rare,
12 AMS) radiocarbon dates from Alaskan mainland mammoths, 13 new dates from Alaskan island mammoths, rec
14 Degradation of water quality by intensified mammoth activity around the lake likely exacerbated the
15 tes of a protein structure for comparison by MAMMOTH against all chains in the PDB; (ii) the AnnoLite
16 oth benchmarks, classifying structures using MAMMOTH alone does not work as well as using an SVM with
18 ed probability that orthologous elephant and mammoth amino acids differ is 0.002, corresponding to ab
24 s of the transposable elements (TEs) between mammoth and other mammals may shed light on the evolutio
25 ne of these lineages gave rise to the woolly mammoth and the other represents a previously unrecogniz
27 identified mitochondrial genomes of multiple mammoth and woolly rhinoceros individuals-both species t
29 pects of many other megafauna species (e.g., mammoths and cave bears), relatively few ancient-DNA stu
31 extracted DNA from several Pleistocene epoch mammoths and noted differences among individual specimen
33 steppe bison), Mammuthus primigenius (woolly mammoth), and Lagopus lagopus (willow ptarmigan) eDNA fr
34 xtinct American mastodon, the extinct woolly mammoth, and the modern Asian and African elephants to t
36 e to resolve the relationships of the woolly mammoth, Asian elephant, and African elephant because th
37 lant functional types consumed by the woolly mammoth at 300 m resolution on Alaska's North Slope.
39 can horse) and Mammuthus primigenius (woolly mammoth) at multiple sites persisting thousands of years
41 ing Sea--made it possible to reconstruct how mammoths became stranded in the Pribilofs and why this a
42 humans in the extinction dynamics of woolly mammoth began well before the Holocene, exerting lasting
44 ith uptake of DNA from a 43,000-y-old woolly mammoth bone, we further demonstrate that such natural t
45 of proteins and lipids within intact fossil mammoth bones of different ages and varied depositional
46 he extensive similarities between the woolly mammoth brain and the African elephant brain indicate th
47 ind evidence of steppe vegetation, bison and mammoth by approximately 12.6 cal. kyr bp, followed by o
48 a sediment sample from the mummified Woolly Mammoth carcass found in August 2010, from the Oyogos Ya
49 support a monophyletic Asian elephant-woolly mammoth clade when the American mastodon is used as an o
50 ignment methods (SAP, TM-align, Fr-TM-align, MAMMOTH, DALI, CE and FATCAT) on a diverse, non-redundan
53 resistance to antimicrobial agents has taken mammoth dimension and warrants immediate steps to minimi
55 nds (including mammuthusin-2 from the woolly mammoth, elephasin-2 from the straight-tusked elephant,
56 9.8 0.2 ka; and (6) phylogenetic analysis of mammoth environmental DNA reveals a previously unsampled
57 nce of wider spatial sampling to reconstruct mammoths' evolutionary history and demonstrate the feasi
61 large radiocarbon dating project of Alaskan mammoth fossils, I addressed this question by including
64 tly in Earth history, very large herbivores (mammoths, ground sloths, diprotodons, and many others) o
65 d that at the time of its origin, the woolly mammoth had already acquired a broad spectrum of positiv
66 ivergent in their mitochondrial genomes, the mammoths had similar nuclear genomes, a finding germane
67 on of the two genomes shows that the Wrangel mammoth has a 20% reduction in heterozygosity as well as
68 neage, whereas the Afrotherian-wide SINEs in mammoth have undergone a rather flat and stepwise expans
72 allow water channels, such as those found at Mammoth hot springs of Yellowstone National Park and the
73 The Manis site, combined with evidence of mammoth hunting at sites in Wisconsin, provides evidence
75 ography imaging data obtained for the woolly mammoth in comparison with magnetic resonance imaging da
78 eference for C(4) grazers including juvenile mammoths, in agreement with taphonomic evidence suggesti
80 ription of the preserved brain of the woolly mammoth is provided, along with a series of quantitative
82 e could support densities of 0.0-0.38 woolly mammoth km(-2) (mean 0.13) across a variety of habitats.
83 ium serum alongside an abundance of juvenile mammoths, leading some to argue that H. serum preferenti
90 gional extinctions of horse (Equus spp.) and mammoth (Mammuthus primigenius) and began during a perio
91 of nine, radiocarbon-dated, Late Pleistocene mammoth (Mammuthus primigenius) and bison (Bison priscus
93 3 billion (80%) of which are from the woolly mammoth (Mammuthus primigenius) genome and thus comprise
96 the mummified brain of a pleistocene woolly mammoth (Mammuthus primigenius) recovered from the Yakut
98 Pleistocene epoch, populations of the woolly mammoth (Mammuthus primigenius) were distributed across
100 ption and the last known occurrence of pygmy mammoths (Mammuthus exilis) on the Channel Islands, corr
103 re, we report that skin from a female woolly mammoth (*Mammuthus primigenius) that died 52,000 years
104 g of horse and camel in Canada, coupled with mammoth, mastodon, sloth, and gomphothere hunting docume
105 h greater diversity of megaherbivores (e.g., mammoths, mastodons, giant ground sloths) and thus a gre
106 tructed RTE phylogeny indicates that RTEs in mammoth may be acquired through an ancient lateral gene
107 to assemble and interpret a data set of 143 mammoth mitochondrial genomes, sampled from fossils reco
111 ns of pore-water CO2 and the minerals in the Mammoth Mountain soils can cause the release of environm
112 ntrations and visual inspection of plants at Mammoth Mountain, CA, allowed the demarcation of tree-ki
113 or a few representative cases indicates that MAMMOTH-mult delivers biologically meaningful trees and
120 resent) established the presence of Holocene mammoths on St Paul Island, a first Holocene island reco
121 ago by the discovery that the latest woolly mammoths on Wrangel Island, northeastern Siberia, were c
122 algorithms, such as DALI, CE, MultiProt and MAMMOTH, on a sample dataset of non-redundant proteins f
123 od (cooking, fermenting), the consumption of mammoths or young mammals, or additional (freshwater fis
126 of a Palaeo-Eskimo Saqqaq individual, woolly mammoths, polar bears and two equine species, we confirm
127 phylogeny confirms that the Late Pleistocene mammoth population comprised three distinct mitochondria
128 that reconciling ancient DNA data on woolly mammoth population decline with fossil evidence of locat
129 opulation, this evidence indicates that this mammoth population died out because of the synergistic e
130 to other extinction models for the St. Paul mammoth population, this evidence indicates that this ma
131 Island, which was the last surviving woolly mammoth population, was subject to reduced genetic diver
133 structured their settlements partly based on mammoth prevalence and made use of mammoths for raw mate
135 d mammoths, 13 new dates from Alaskan island mammoths, recent reconstructions of bathymetric plots an
136 d other local contemporaneous archaeological mammoth remains revealed that multiple mammoth herds con
137 , we analyzed ancient microbial DNA from 483 mammoth remains spanning over 1 million years, including
139 enic tobacco (Nicotiana tabacum cv. Maryland Mammoth) resulted in the loss of photoregulatory activit
140 We hypothesize that, shortly after this mammoth's death, the sample spontaneously freeze-dried i
141 Using well-dated samples from across the mammoth's Eurasian range, we document geographical and c
142 al genomes of Erysipelothrix from the oldest mammoth sample, representing the oldest authenticated ho
145 e active and inactive genome compartments in mammoth skin more closely resemble Asian elephant skin t
148 x, all indicate that the brain of the woolly mammoth specimen examined has many similarities with tha
150 the recovery of genome-wide data from three mammoth specimens dating to the Early and Middle Pleisto
151 sils, I addressed this question by including mammoth specimens from Bering Sea islands known to have
152 billion bases (Gb) of sequence from several mammoth specimens, 3.3 billion (80%) of which are from t
153 leistocene-Holocene transition, the dominant mammoth steppe ecosystem across northern Eurasia vanishe
154 ion dynamics of megafauna that inhabited the mammoth steppe provides insights into the causes of exti
155 uggest that a defining characteristic of the mammoth steppe was its temporal instability and imply th
156 The collapse of the steppe-tundra biome (mammoth steppe) at the end of the Pleistocene is used as
160 ion with native human populations and woolly mammoths, suggesting that only a few evolutionary strate
161 dependent indicators of extinction show that mammoths survived on St. Paul until 5,600 +/- 100 y ago.
162 econstruct the movements of an Arctic woolly mammoth that lived 17,100 years ago, during the last ice
165 lines by many millennia, and to allow woolly mammoths to persist in mainland Arctic refugia until the
167 silvestris and the short-day plant Maryland Mammoth tobacco, the quantitative long-day plant Nicotia
168 at detectable subsurface consolidation below mammoth tracks correlates with typical plantar pressure
169 e use detailed isotopic analyses of a female mammoth tusk found in a 14,000-year-old archaeological s
170 their extinction, both giant deer and woolly mammoth underwent dramatic shifts in distribution, drive
171 inct megafauna species, including the woolly mammoth until 3.9 0.2 thousand years ago (ka) and the wo
173 showed an enantiomeric ratio 75:25 while for Mammoth variety, linalool enantiomeric ratio was 95:5 (R
177 na from this region and period, we find that mammoth was the largest contributor to Clovis diet, foll
178 ucleotide differences between two particular mammoths was approximately one-eighth of that between on
179 se estimates with the forage needs of woolly mammoths, we conservatively estimate Alaska's North Slop
180 e of radiocarbon-dated evidence to show that mammoths were abundant in the open-habitat of Marine Iso
181 es associated with cold adaptation in woolly mammoths were already present one million years ago.
182 s hunters of Pleistocene megamammals (mostly mammoth) who entered the continent via Beringia and an i
183 el of mobility by megafaunal species such as mammoth would have been increasingly difficult as the ic
185 uld also be the result of the consumption of mammoths, young animals, putrid meat, cooked food, fresh