ライフサイエンスコーパス: Pleistocene

1 n archaic human diaspora early in the Middle Pleistocene.

2 as mostly ice-covered during the mid-to-late Pleistocene.

3 od of climatic instability at the end of the Pleistocene.

4 ize is indicated to have occurred during the Pleistocene.

5 d this perception has been extended into the Pleistocene.

6 duction and a neopolyploidy event during the Pleistocene.

7 te for salmon processing during the terminal Pleistocene.

8 ajor glacial advances of the Middle and Late Pleistocene.

9 progenitor, probably in Beringia during the Pleistocene.

10 ital punishment on self-domestication in the Pleistocene.

11 existed across different stages of the Late Pleistocene.

12 or ambush hunting during the Lower to Middle Pleistocene.

13 lly, pursuit canids first emerged during the Pleistocene.

14 in effective population size during the late Pleistocene.

15 ajor human behavioral shifts during the Late Pleistocene.

16 s of Northern Hemisphere climate in the Late Pleistocene.

17 ns were established by at least the terminal Pleistocene.

18 the megafauna extinctions at the end of the Pleistocene.

19 floated across the Atlantic during the Late Pleistocene.

20 onset of climate changes during the terminal Pleistocene.

21 radiation first appearing in the Pliocene or Pleistocene.

22 orldwide expansion out of Africa in the Late Pleistocene.

23 curred among many hominin groups in the Late Pleistocene.

24 pulation size for all three taxa through the Pleistocene.

25 ciated with glacial terminations of the Late Pleistocene.

26 ate with human mobility through the terminal Pleistocene.

27 35 ka, placing H. naledi in the later Middle Pleistocene.

28 in effective population size throughout the Pleistocene.

29 hy and history of climate change through the Pleistocene.

30 nages caused by sea-level changes during the Pleistocene.

31 te system of MIS 19 and the following Middle Pleistocene.

32 ly geographically partitioned throughout the Pleistocene.

33 p. were widespread across Eurasia during the Pleistocene.

34 in Italy to assess human mobility in Middle Pleistocene.

35 nodes of Brachypodium and a very recent Mid-Pleistocene (0.9 Ma) time for the B. distachyon split.

36 Two early Late Pleistocene ( 105,000- to 125,000-year-old) crania from

37 g these genomes with the genomes of two Late Pleistocene, 27 domesticated, and three wild Przewalski'

38 ondrial protein-coding genes, supports a mid-Pleistocene ( 630,000 years ago) divergence between the

39 place during the late Pliocene or the early Pleistocene, a time corresponding well with the common p

40 stinguish KNM-LH 1 and other Middle and Late Pleistocene African fossils from crania of recent Africa

41 As a result the recovery of Pleistocene-age human remains is extremely rare.

42 f LMW DOC in driving the rapid metabolism of Pleistocene-age permafrost carbon upon thaw and the outg

43 n is about 1.6 times larger than the mass of Pleistocene-aged permafrost carbon released as greenhous

44 nd fluxes in lake sediments overlying thawed Pleistocene-aged permafrost.

45 ough to a lesser extent than that during the Pleistocene, along the marginal shelf in the Yellow/Boha

46 ree of congruent demographic response to the Pleistocene among codistributed taxa remains unknown.

47 During glacial periods of the Late Pleistocene, an abundance of proxy data demonstrates the

48 re and atmospheric CO2 extended into the mid-Pleistocene and demonstrates the feasibility of disconti

49 ica may have continued throughout the latest Pleistocene and early Holocene.

50 the syrinx are geologically young (from the Pleistocene and Holocene (approximately 2.5 million year

51 rient level and salinity throughout the late Pleistocene and Holocene in the Qinghai Lake region.

52 ichness of big carnivores was greater in the Pleistocene and many of them were significantly larger t

53 changes in biosphere function since the Late Pleistocene and of the functioning of contemporary ecosy

54 ths are indistinguishable from those of Late Pleistocene and recent modern humans.

55 umans who spread into Europe during the Late Pleistocene and the impact of subsequent climatic events

56 uses of extinctions during both the terminal Pleistocene and today.

57 lation bottleneck during the Middle or Early Pleistocene, and a more recent severe decline in the anc

58 er timescales from decades back to the early Pleistocene, and are critical for understanding past cli

59 son mitogenomes with ages that span the Late Pleistocene, and identified two waves of bison dispersal

60 ine in wolf numbers in Europe since the Late Pleistocene, and long-term isolation and bottlenecks in

61 KNM-LH 1 is securely dated to the Late Pleistocene, and samples a time and region important for

62 ly on dead-stranded marine mammals since the Pleistocene, and this food source is considered importan

63 e island was readily achieved throughout the Pleistocene, apparently ending at approximately 55 ka.

64 mposition and Antarctic climate from the mid-Pleistocene ( approximately 1 Ma) from ice cores drilled

65 the second of which occurred during the Late Pleistocene, approximately 45-21 thousand y ago.

66 diments (such as those comprising the deeper Pleistocene aquifer) could stimulate microbial communiti

67 sent in both the sandy Holocene and gravelly Pleistocene aquifers and is also abstracted by the pumpi

68 cross central West Bengal, India, those from Pleistocene aquifers at depths >70 m beneath paleo-inter

69 Pleistocene aquifers beneath deep paleo-channels typical

70 hallow aquifers through exploitation of deep Pleistocene aquifers would improve if guided by an under

71 In the shallowest Holocene-Pleistocene aquifers, arsenic occurrence is best describ

72 Peruvian Andes contains the highest-altitude Pleistocene archaeological sites yet identified in the w

73 The Late Pleistocene archaic humans from western Eurasia (the Nea

74 ded continuously throughout the Pliocene and Pleistocene, as did increases in the relative abundance

75 f soil invertebrates could have survived the Pleistocene at high elevation habitats protruding above

76 , we obtain a multidomain-corrected Pliocene-Pleistocene average paleointensity of 21.6 +/- 11.0 micr

77 es (the ice-albedo feedback) during the late Pleistocene, because equilibrium climate sensitivity is

78 ions, and infant/child mortality of terminal Pleistocene Beringians.

79 ates and ancient mitochondrial DNA from late Pleistocene bison fossils to determine the chronology fo

80 11 reptiles, 63 birds, 8 mammals) from late Pleistocene bone deposits in Sawmill Sink, Abaco, The Ba

81 laked bone tools, along with Middle and Late Pleistocene bone retouchers, led to a re-evaluation of t

82 f synchrotron X-ray irradiation on aDNA from Pleistocene bones.

83 ate of decline and extinction since the Late Pleistocene, both on land and more recently in the ocean

84 curs around 2.6 Ma to 2.8 Ma, near the lower Pleistocene boundary, terminates around 1.7 Ma, and peak

85 urred at least twice in the early and middle Pleistocene, but the spatial genetic distribution rarely

86 neled Scablands, which was carved during the Pleistocene by the catastrophic Missoula floods in easte

87 y mediated arsenic release from Holocene and Pleistocene Cambodian aquifer sediments was investigated

88 The Late Pleistocene Campanian Ignimbrite (CI) super-eruption (So

89 clues for understanding the ocean's role in Pleistocene carbon cycling.

90 h intervals, and consequently, we argue that Pleistocene carnivores had the capacity to, and likely d

91 he predicted prey size ranges of many of the Pleistocene carnivores.

92 Lida Ajer is a Sumatran Pleistocene cave with a rich rainforest fauna associated

93 We distinguish Late Pleistocene clades within the genus Homo based on ancien

94 likely condition their timing of response to Pleistocene climate change.

95 ctuating asymmetry) through 27,000 y of Late Pleistocene climate change.

96 n this region expanded synchronously to Late Pleistocene climate changes.

97 ize change across communities in response to Pleistocene climate cycles is likely rare in North Ameri

98 s nearly ice-free for extended periods under Pleistocene climate forcing.

99 As an evolutionary product of Pleistocene climate instability, humans possess broad ad

100 ing a clear link between ridge magmatism and Pleistocene climate transitions.

101 ting that a combination of human impacts and Pleistocene climate variability has modified the 20-mill

102 This study demonstrates that Pleistocene climatic change and mountain glaciers, rathe

103 ubsequent genetic structure is attributed to Pleistocene climatic changes, in which sky-islands acted

104 Pleistocene climatic cycles altered species distribution

105 Pleistocene climatic fluctuation, complicated topography

106 of evidence suggest that physical barriers, Pleistocene climatic oscillations and geographical heter

107 ge expansion of P. hwangshanensis during the Pleistocene climatic oscillations could have been the ca

108 ly genetic lineage that may stem from a late Pleistocene coastal migration into the Americas.

109 This relationship is highly contingent on Pleistocene connectivity, suggesting that biogeographic

110 s associated with the advance and retreat of Pleistocene continental glaciers.

111 amatic climatic oscillations following early Pleistocene cooling, so the timing and amplitude of chan

112 s of this uplift by measurements of elevated Pleistocene coral terraces.

113 eferred to Montemagrechiridae fam. nov. Nine Pleistocene corals with crescentic pits originate from F

114 Seventeen Middle Pleistocene crania from the Sima de los Huesos site (Ata

115 Recent excavations of Late Pleistocene deposits on Rusinga Island, Kenya, have unco

116 uring rapid climatic warming at the terminal Pleistocene despite dramatic turnover in the distributio

117 This trend reversed in the late Pleistocene despite low CO2, suggesting an additional re

118 west of Lake Turkana, which during the late Pleistocene/early Holocene period extended about 30 km b

119 ng the warm Pliocene as during the cold late Pleistocene epoch (0.8 to 0.01 million years ago).

120 deglaciated for extended periods during the Pleistocene epoch (from 2.6 million years ago to 11,700

121 nd global environmental perturbations as the Pleistocene epoch ended and transitioned into the Holoce

122 record from southern Asia for the early Late Pleistocene epoch is scarce.

123 most endemic species have evolved recently (Pleistocene epoch), during a period of recurrent sea-lev

124 ng human dispersals out of Africa during the Pleistocene epoch, although this has yet to be confirmed

125 During the early Pleistocene epoch, ice cover in East Greenland was dynam

126 Near the end of the Pleistocene epoch, populations of the woolly mammoth (Ma

127 , an archaeological site from the early late Pleistocene epoch, where in situ hammerstones and stone

128 e change is a ubiquitous feature of the Late Pleistocene epoch.

129 iven by either Neogene cooling or increasing Pleistocene erosion rates.

130 New evidence is presented of explosive Late Pleistocene eruptions in the Pacific Arc, currently undo

131 he emergence of different phenotypes in Late Pleistocene Europe and Africa.

132 onfirm the identification of the unique Late Pleistocene European fossil through ancient-DNA analyses

133 and identify the timing of two critical late Pleistocene events: wide-scale ecosystem change and regi

134 large-scale dispersals, was important in the Pleistocene evolutionary history of mammoths.

135 Together, these findings suggest that Plio-Pleistocene extension is not likely to have been accommo

136 rstanding of the full extent of the terminal Pleistocene extinction event.

137 de Pectinidae (scallops) during a major Plio-Pleistocene extinction in California that involved a pre

138 ison kill-off in the 1860s, and the terminal Pleistocene extinction of megafauna.

139 The late Pleistocene extinction of so many large-bodied vertebrat

140 Atlantic fauna suffered more severe Pliocene-Pleistocene extinction than did the eastern Pacific.

141 a third possibility for at least some of the Pleistocene extinctions is that they occurred through ha

142 explaining the peopling of the Americas and Pleistocene extinctions will be in error.

143 restrial megafauna to have survived the late Pleistocene extinctions.

144 the major clades was estimated to be in the Pleistocene, falling into several Pleistocene glacial st

145 ies are inferred to have been inherited from Pleistocene fluvial systems reactivated as tidal channel

146 persal into Asia as early as the late Middle Pleistocene, followed by a separate dispersal into north

147 documented diversity in the European Middle Pleistocene fossil record.

148 Two new Pleistocene fossils now provide unexpected evidence of a

149 f songbirds (Passeriformes) recorded as Late Pleistocene fossils on the Bahamian island of Abaco-the

150 ey inhabited the Arctic and Subarctic during Pleistocene full-glacial times ( approximately 18,000 (1

151 ecological state shifts that occurred as the Pleistocene gave way to the Holocene.

152 tebrates, e.g. the hypertelic antlers of the Pleistocene giant deer Megaloceros giganteus.

153 lations that present a continuously existing Pleistocene GIS.

154 Research on global ice-volume changes during Pleistocene glacial cycles is hindered by a lack of deta

155 e paradigm that global cooling during recent Pleistocene glacial cycles resulted in a burst of specie

156 ought, highlighting the role of at least one Pleistocene glacial refugium, perhaps on the Red Sea pla

157 be in the Pleistocene, falling into several Pleistocene glacial stages and postdating the formation

158 basins, attributed to past vicariance during Pleistocene glaciations and a secondary contact associat

159 Pleistocene glaciations have profoundly affected pattern

160 Pleistocene glaciations played an additional geomorpholo

161 cture shaped by vicariant events, especially Pleistocene glaciations.

162 kely location of carbon sequestration during Pleistocene glaciations.

163 t explains the re-occupation of reefs during Pleistocene glacio-eustacy.

164 ity as a potential new consideration for Mid Pleistocene global biogeochemical climate models, and im

165 The Pleistocene global dispersal of modern humans required t

166 pogenic alterations to biodiversity-the Late Pleistocene global human expansion, the Neolithic spread

167 f this closure has been correlated with Plio-Pleistocene global oceanographic, atmospheric, and bioti

168 ate swings played a key role in shaping Late Pleistocene global population distributions, whereas mil

169 elta(18)O, and delta(2)H show that the As in Pleistocene groundwater beneath deep paleo-channels is r

170 g the late Holocene (<4 ka) rather than late Pleistocene (>10 ka).

171 arkedly similar to that associated with Late Pleistocene H. floresiensis.

172 and among the latter, connection during the Pleistocene had an important impact.

173 mmalian extinction worldwide during the Late Pleistocene has been a major focus for Quaternary biochr

174 them birds) are linked to changes during the Pleistocene-Holocene Transition (PHT) ( approximately 15

175 lobal mean sedimentary delta(15)N across the Pleistocene-Holocene transition, but it is happening an

176 mate changes that took place during the late Pleistocene-Holocene transition.

177 f many cryptic biotic transitions before the Pleistocene/Holocene boundary revealed by ancient DNA co

178 Bone modifications among Ethiopian Plio-Pleistocene hominid and faunal remains at Asa Issie, Mak

179 However, such claims about Plio-Pleistocene hominids rely mostly on very small assemblag

180 possible to thoroughly characterize a Middle Pleistocene hominin paleodeme and to address hypotheses

181 sights into the genetic relationship between Pleistocene hominins and modern humans.

182 (that is, jaws and teeth) homoplasy in Plio-Pleistocene hominins, and shows that some dentognathic f

183 ht into the wide spectrum of the diet of mid-Pleistocene hominins, enhancing our understanding of the

184 anus (~3 to 2 million years ago) and several Pleistocene hominins, traditionally considered not to ha

185 y, social transmission, and communication in Pleistocene hominins.

186 The few sufficiently complete Early Pleistocene Homo clavicles seem to have relative lengths

187 attributed to a population ancestral to Late Pleistocene Homo floresiensis.

188 g into Asia met Neandertals, Denisovans, mid-Pleistocene Homo, and possibly H. floresiensis, with som

189 therium sp. samples, including the only Late Pleistocene Homotherium sample from Eurasia [4].

190 WSL, equids constitute a perplexing group of Pleistocene horses endemic to North America.

191 evolution in eastern Africa during the Plio-Pleistocene; however, this hypothesis remains inadequate

192 ree Corridor has been invoked as a route for Pleistocene human and animal dispersals between eastern

193 strong implications for our understanding of Pleistocene human evolution in Africa.

194 This morphological combination reflects Pleistocene human evolutionary patterns in general biolo

195 al-scale assessment of the opportunities for Pleistocene human occupation of Australia, the driest in

196 Although a rich record of Pleistocene human-associated archaeological assemblages

197 Modern and Middle to Late Pleistocene humans share a suite of derived features in

198 Such data suggest that, by the Late Pleistocene, humans had begun to engage in activities th

199 matrilineal genetic continuity between late Pleistocene hunter-gatherer groups and present-day popul

200 water resources were more important for late Pleistocene hunter-gatherers than previously thought and

201 nowledge of the Neandertals, a population of Pleistocene hunter-gatherers who lived in (western) Eura

202 ing suggests ice sheet stability through the Pleistocene (i.e., the past 2.7 million years).

203 rom the warm climates of the Pliocene to the Pleistocene ice ages between 3.2 and 2.6 million years a

204 rge temporal offset during the onset of Plio-Pleistocene ice ages, between a marked cooling step at 2

205 naledi, survived into the later parts of the Pleistocene in Africa, and indicate a much younger age f

206 , Kenyanthropus This continues into the late Pleistocene in Paranthropus, whereas Homo maintains a fl

207 last interglacial period (MIS 5e; early late Pleistocene), indicating that humans with manual dexteri

208 m fetus, making these the youngest-aged late Pleistocene individuals known for the Americas and the o

209 in hunter-gatherer mobility during the Late Pleistocene influenced settlement ecologies, altered hum

210 sults furnished the first evidence for major Pleistocene interglacial refugia and a latitudinal effec

211 ich Greenland was ice-free during any or all Pleistocene interglacials, may be more realistic.

212 The Middle Pleistocene is a crucial time period for studying human

213 To estimate the potential impact of Pleistocene large carnivores, we use both historic and m

214 589 years ago in Africa coincident with late Pleistocene large mammal extinctions.

215 Cave, we retrieved Denisovan DNA in a Middle Pleistocene layer near the bottom of the stratigraphy.

216 of a human deciduous incisor from the Middle Pleistocene layers of the Isernia La Pineta site (Italy)

217 n seven out of nine, radiocarbon-dated, Late Pleistocene mammoth (Mammuthus primigenius) and bison (B

218 ting global phylogeny confirms that the Late Pleistocene mammoth population comprised three distinct

219 es in eastern Africa during the Pliocene and Pleistocene may have been decoupled from aridity.

220 tions of a few large vertebrates in the late Pleistocene may have resulted in the coextinction of num

221 and accumulation of fuel related to the late Pleistocene megafauna extinction, which took place in th

222 The mechanisms of Late Pleistocene megafauna extinctions remain fiercely contes

223 s of a small population of people on extinct Pleistocene megafauna.

224 d representatives of the now largely extinct Pleistocene megafauna.

225 on hotspots, and the location of the largest Pleistocene megafaunal extinction, South America is cent

226 stereotypically characterized as hunters of Pleistocene megamammals (mostly mammoth) who entered the

227 earliest well-defined evidence of humans in Pleistocene North America.

228 atment of the youngest members of a terminal Pleistocene North American population.

229 ssociated with the waxing and waning of Late-Pleistocene Northern Hemisphere ice sheets.

230 was only a single species of middle to late Pleistocene NWSL equid, and demonstrate that it falls ou

231 ingle specimens with pits come from the late Pleistocene of Cuba and the late Pliocene of Florida, al

232 During the late Pleistocene of North America ( approximately 36,000 to 1

233 hat population structure existed in the late Pleistocene of North America with Shuka Kaa on a differe

234 tter infiltrating from riverbeds during late Pleistocene or earliest Holocene times.

235 her North American individuals from the late Pleistocene or early Holocene (i.e., Anzick-1 and Kennew

236 ic data support the hypothesis that all Late Pleistocene (or post-Villafrancian) Homotherium should b

237 mpare oysters from archaeological sites with Pleistocene oyster reefs that existed before human harve

238 American archaeological record and terminal Pleistocene paleontological record.

239 creased along the continent during the early Pleistocene period.

240 e of information for the Miocene through the Pleistocene periods, due to the abundant faunal remains

241 ately 44,800-year-old specimen from the Late Pleistocene population in northeastern Siberia.

242 ic polarities, and used as evidence for Late Pleistocene population relationships.

243 Myr) as compared with other Lower and Middle Pleistocene populations.

244 indicum expanded its range southward in the Pleistocene, possibly during the most recent or previous

245 these lineages at this location in the Late Pleistocene provides evidence for the extent of mitochon

246 ibuted to a better understanding of the Late Pleistocene record in Asia.

247 rio of extensive recombination, perhaps in a Pleistocene refugium.

248 Pleistocene residential sites with multiple contemporane

249 iment from which WB3 was isolated was brown, Pleistocene sand at a depth of 35.2 m below ground level

250 on of minimal iron oxyhydroxides in the gray Pleistocene sands by organic matter infiltrating from ri

251 Using Plio-Pleistocene sea-level variations as a forcing function,

252 reas limited As(III) release was observed in Pleistocene sediment after lactate addition, no arsenic

253 Incubation of the Pleistocene sediment with lactate favoured a 16S rRNA-ph

254 primitive hominin species discovered in Late Pleistocene sediments at Liang Bua (Flores, Indonesia),

255 ic carbon, As(III) mobilization can occur in Pleistocene sediments, having implications for future st

256 ina is a cavity infilled by at least 25 m of Pleistocene sediments.

257 drinking waters by using aquifers containing Pleistocene sediments.

258 nd D. richardsoni were recovered from a Late Pleistocene site in south-western Canada.

259 Recent excavations at the early Middle Pleistocene site of Mata Menge in the So'a Basin of cent

260 oothed cat Homotherium reveals that the late Pleistocene species from Europe and North America were t

261 odern humans, resembling middle-to-late Late Pleistocene specimens and even contemporary humans.

262 could have had bottom-up effects in the Late Pleistocene steppe-tundra ecosystem.

263 We present the oldest Middle-Late Pleistocene stratified and numerically dated faunal succ

264 assemblages of multiple and diverse types of Pleistocene "symbolic" artifacts were entirely unknown f

265 Pleistocene terrestrial ecosystems included a much great

266 of greater mtDNA diversity during the Middle Pleistocene than in later periods.

267 lation created two mtDNA lineages during the Pleistocene that are now widespread.

268 ed a pattern of population growth during the Pleistocene that could be linked to climate changes.

269 from a source population deep in the Middle Pleistocene, the hundreds of thousands of years of relat

270 logical conservatism of the Lower and Middle Pleistocene, the Middle to Upper Paleolithic transition,

271 By the end of the Pleistocene, the Sundaland corridor was submerged, and p

272 s within the northern hemisphere during Late Pleistocene time ( 46-11 ka B.P.).

273 e radiocarbon calibration curve and the Late Pleistocene time-scale at ca. 40 ka.

274 l strike-slip fault system active since Late Pleistocene time.

275 n and carving glacial landforms down to Plio-Pleistocene times.

276 e of changes in human mobility from the Late Pleistocene to the Iron Age.

277 human and faunal tooth enamel from four late Pleistocene-to-Holocene archaeological sites in Sri Lank

278 The mid-Pleistocene transition (MPT) marked a fundamental change

279 A dramatic shift is observed at the Mid-Pleistocene Transition (MPT), consistent with far-field

280 During the Mid-Pleistocene Transition (MPT; 1,200-800 kya), Earth's orb

281 f temperature and rainfall following the Mid-Pleistocene Transition around 900,000 years ago.

282 that interglacial vegetation during the Plio-Pleistocene transition mainly reflects conditions of the

283 oclimate variability associated with the Mid-Pleistocene Transition resulted in hydrologic change dom

284 disequilibrium was stronger during the Plio-Pleistocene transition than during the Mid-Pliocene Warm

285 ably stalled before the beginning of the mid-Pleistocene transition, and pre-dated the increase in th

286 lobal deep water mass properties at the Plio-Pleistocene transition, as Circumpolar Deep Water (CDW)

287 quasi-100,000-year glacial cycles at the mid-Pleistocene transition.

288 ation is the most obvious result of the Plio-Pleistocene transition.

289 y and simulate demographic events during the Pleistocene using approximate Bayesian computation (ABC)

290 , provides a unique opportunity to study mid-Pleistocene vegetal diet and is crucial for understandin

291 magma-assisted rifting associated with Plio-Pleistocene volcanism.

292 Ellsworth-Whitmore uplands may have survived Pleistocene warm periods.

293 ulation expansion during the early to middle Pleistocene was followed by decline.

294 here it is commonly thought to represent pre-Pleistocene weathering possibly associated with landscap

295 -Salween Divide and climatic oscillations in Pleistocene were the main drivers for the contemporary d

296 sibly promoted by low sea levels during Plio-Pleistocene, which further explain differences in specie

297 te in the So'a Basin during the early Middle Pleistocene, while various lines of evidence suggest the

298 n occurred in the deep oceans during the Mid Pleistocene, with a loss of over 100 species (20%) of se

299 genetic structure within Eurasia in the Late Pleistocene, with the ancient population contributing si

300 f an examination of the mummified brain of a pleistocene woolly mammoth (Mammuthus primigenius) recov