ライフサイエンスコーパス: Pleistocene

1 isappeared from the region at the end of the Pleistocene.

2 he melting of the glaciers at the end of the Pleistocene.

3 and dry habitats that proliferated into the Pleistocene.

4 understanding of human evolution in terminal Pleistocene.

5 n Central and Northeast Asia during the Late Pleistocene.

6 n archaic human diaspora early in the Middle Pleistocene.

7 ciated with glacial terminations of the Late Pleistocene.

8 ate with human mobility through the terminal Pleistocene.

9 hy and history of climate change through the Pleistocene.

10 progenitor, probably in Beringia during the Pleistocene.

11 ital punishment on self-domestication in the Pleistocene.

12 -analogous vegetation structure in the Early Pleistocene.

13 35 ka, placing H. naledi in the later Middle Pleistocene.

14 in effective population size throughout the Pleistocene.

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

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

17 ly geographically partitioned throughout the Pleistocene.

18 p. were widespread across Eurasia during the Pleistocene.

19 in Italy to assess human mobility in Middle Pleistocene.

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

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

22 ize is indicated to have occurred during the Pleistocene.

23 d this perception has been extended into the Pleistocene.

24 duction and a neopolyploidy event during the Pleistocene.

25 ch are estimated to have diverged during the Pleistocene.

26 te for salmon processing during the terminal Pleistocene.

27 re-distribution of fault activity since the Pleistocene.

28 ead across the Holarctic throughout the Late Pleistocene.

29 iversity (including endemism) since the Late Pleistocene.

30 s from a common ancestor dated to the Middle Pleistocene.

31 ppearance of the megafauna at the end of the Pleistocene.

32 to be from dates extending well into the mid-Pleistocene.

33 and eventual ice conditions beginning in the Pleistocene.

34 d across the Eurasian steppe during the Late Pleistocene.

35 line and continued until near the end of the Pleistocene.

36 to global glaciation oscillations during the Pleistocene.

37 larly for hominins of the Pliocene and early Pleistocene.

38 d settled by modern humans at the end of the Pleistocene.

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

40 species, that went extinct at the end of the Pleistocene [1-4].

41 ue record of onshore and offshore markers of Pleistocene ~100-ka climate cycles provides an outstandi

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

43 ng to megafauna (>44 kg) extinctions in Late Pleistocene (126,000-12,000 years ago) Australia are hig

44 , most likely from East Asia during the Plio-Pleistocene (2-1Mya).

45 the best fossil records, three from the Late Pleistocene (~25 to 10 ka [1,000 y ago]) and one from th

46 vore families in the late Pliocene and early Pleistocene (3.6 to 1.05 Ma) from the Shungura Formation

47 f lineage that dwelled in Siberia during the Pleistocene.(3)(5) Previous studies have suggested that

48 nalyzed enamel of fossil teeth from the Late Pleistocene (38.4-13.5 ka) mammalian assemblage of the T

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

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

51 4 teragrams CH(4) per year at the end of the Pleistocene, about 11,600 years ago(8), but that period

52 The result suggests that later Middle Pleistocene Africa contained multiple contemporaneous ho

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

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

55 uted across northern Eurasia during the Late Pleistocene and became extinct approximately 14 thousand

56 and the Caribbean coast(7-9) during the Late Pleistocene and Early Holocene epochs.

57 ty was lost during the climate shifts of the Pleistocene and has not recovered, despite the current h

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

59 range for copal (2.58 Ma-1760 AD), including Pleistocene and Holocene copals, and the novel term "Def

60 eneck experienced by bison at the end of the Pleistocene and includes the second bottleneck which occ

61 f the Andean lineages is limited to the Late Pleistocene and intimately associated with habitat contr

62 l competition for prey throughout the latest Pleistocene and largely irrespective of changing climate

63 orthern Great Plains bison from the terminal Pleistocene and throughout the Holocene to gain insight

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

65 xisted as at least two subspecies during the Pleistocene, and that lions and cave lions were distinct

66 l transitions were similar to the end of the Pleistocene, and that the large mammal genera survived u

67 mammals likely promoted co-occurrence in the Pleistocene, and their loss contributed to the modern as

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

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

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

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

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

73 uld potentially explain the much sparser mid-Pleistocene archaeological record in the southern Kalaha

74 rn humans and more typically found in Middle Pleistocene archaic humans.

75 eistocene epoch and it is not until the Late Pleistocene (around 40,000-30,000 years ago) that this t

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

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

78 hort-lived and aborted close to the Pliocene-Pleistocene boundary.

79 ong species and emerged primarily during the Pleistocene, but divergence events were rarely concordan

80 as previously assigned broadly to the Middle Pleistocene by biostratigraphical correlation and ESR/U-

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

82 attributed to the combined influence of Plio-Pleistocene C(4) grassland expansion and pulses of aridi

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

84 and dogs, we resequenced the genomes of four Pleistocene canids from Northeast Siberia dated between

85 this question and the relationships between Pleistocene canids, present-day wolves, and dogs, we res

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

87 n and additional pre-aged (Holocene and late-Pleistocene) carbon released from thawing permafrost soi

88 onally high rates of tooth fracture in large Pleistocene carnivorans imply intensified interspecific

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

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

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

92 nctional variants associated with periods of Pleistocene climate change, and Gradient Forest analysis

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

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

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

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

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

98 Pleistocene climatic cycles altered species distribution

99 d, individualistic evolutionary responses to Pleistocene climatic fluctuations have shaped patterns i

100 ction of TRFs into and out of refugia during Pleistocene climatic fluctuations.

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

102 Si cycle may present an important control on Pleistocene CO(2) concentrations.

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

104 ehaviors of extinct cave bears living during Pleistocene cold periods at middle latitudes have been i

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

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

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

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

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

110 atmospheric CO(2) increases associated with Pleistocene deglaciations.

111 strate that sequencing the proteome of Early Pleistocene dental enamel overcomes the limitations of p

112 The survival of an Early Pleistocene dental enamel proteome in the subtropics fur

113 have been collected from the Early to Middle Pleistocene deposits of Java, Indonesia, forming the lar

114 y echoes the thermokarst-induced collapse of Pleistocene deposits.

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

116 ologies in east Asia and its links to a Late Pleistocene dispersal of modern humans.

117 Results support a Pliocene to early Pleistocene divergence between Scalesia and the closest

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

119 to analyse the 3D geometry of a sequence of Pleistocene emerged marine terraces associated with flex

120 a Levallois component during the late Middle Pleistocene epoch and it is not until the Late Pleistoce

121 s occupied the Tibetan Plateau in the Middle Pleistocene epoch and successfully adapted to high-altit

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

123 relationships between hominins of the Early Pleistocene epoch in Eurasia, such as Homo antecessor, a

124 eral extinct species of the Early and Middle Pleistocene epoch remains contentious.

125 ed environments of Southeast Asia during the Pleistocene epoch(1).

126 nships of the Eurasian Rhinocerotidae of the Pleistocene epoch(7-9), using the proteome of dental ena

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

128 ecular evolution further back into the Early Pleistocene epoch, beyond the currently known limits of

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

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

131 later in the fossil record during the Middle Pleistocene epoch, such as Homo sapiens, are highly deba

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

133 hat inhabited Eurasia in the Middle and Late Pleistocene epoch.

134 species diversified in the Pliocene to early Pleistocene era, and occurred introgressive hybridisatio

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

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

137 rismatic inhabitant of the frigid steppes of Pleistocene Eurasia.

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

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

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

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

142 the causes and consequences of the terminal Pleistocene extinction event.

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

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

145 restrial megafauna to have survived the late Pleistocene extinctions.

146 ls constituted an important component in the Pleistocene faunal communities of South America.

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

148 ing and the dead among these successful Late Pleistocene foragers.

149 Notably, distance from Pleistocene forest refugia is associated with the presen

150 ication of fossil biomineral proteins from a Pleistocene fossil invertebrate, the stony coral Orbicel

151 documented diversity in the European Middle Pleistocene fossil record.

152 day; 16 of these 27 species were recorded as Pleistocene fossils as well.

153 Two new Pleistocene fossils now provide unexpected evidence of a

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

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

156 lations that present a continuously existing Pleistocene GIS.

157 xide a delayed climate amplifier in the late Pleistocene glacial cycles.

158 an permafrost largely formed during the late Pleistocene glacial period and shrank in the Holocene Th

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

160 Pleistocene glacial-interglacial cycles are correlated w

161 al endemic species appeared to have survived Pleistocene glaciation in the eastern Palearctic, much o

162 Pleistocene glaciations have profoundly affected pattern

163 Pleistocene glaciations played an additional geomorpholo

164 kely location of carbon sequestration during Pleistocene glaciations.

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

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

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

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

169 st that the climatic oscillations during the Pleistocene have driven an insect-plant co-evolutionary

170 ommunities, and what changes occurred at the Pleistocene-Holocene boundary that might have led to tho

171 fected the local ecosystem in Texas over the Pleistocene-Holocene boundary, but climate change on its

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

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

174 east Mongolia is, to our knowledge, the only Pleistocene hominin fossil found in the country.

175 blages that have a central role in models of Pleistocene hominin morphology, dispersal and divergence

176 cent chronological studies on Chinese Middle Pleistocene hominin sites, indicate that the time span f

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

178 sister lineage to subsequent Middle and Late Pleistocene hominins, including modern humans, Neanderth

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

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

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

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

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

184 lex demographic processes that characterized Pleistocene human evolution and modern human presence in

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

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

187 cavations and analyses of more than 400 Late Pleistocene human footprints from Engare Sero, Tanzania.

188 These results suggest that two late Middle Pleistocene human groups were present at this site-an ea

189 Although Late and even Middle Pleistocene human presence has been recently documented

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

191 h degrees of morphological diversity in Late Pleistocene humans from East Asia.

192 d sexually divided foraging behavior in Late Pleistocene humans.

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

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

195 litating the occupation of this site by Late Pleistocene hunter-gatherers.

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

197 studies have suggested that during the late Pleistocene ice ages, surface-deep exchange was somehow

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

199 Neandertals by modern humans during the Late Pleistocene in Europe.

200 The end of the Pleistocene in North America saw the extinction of 38 ge

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

202 ts confirm the presence of Meganthropus as a Pleistocene Indonesian hominid distinct from Pongo, Giga

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

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

205 Late Pleistocene interglacials provide potential case example

206 data indicate that during one of the warmest Pleistocene interglacials, the ice sheet margin at the W

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

208 BG) since the late Miocene to the end of the Pleistocene is hereby newly defined, and is characterize

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

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

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

212 of morphological diversity among Late Middle Pleistocene (LMP) African hominins is largely unknown, t

213 ope Stage 11), is one of the very few Middle Pleistocene localities to have provided a fossil hominin

214 ial extinctions and declines during the Late Pleistocene (LP) due to prehistoric human impacts.

215 Frozen permafrost Pleistocene mammal carcasses with soft tissue remains ar

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

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

218 A late Middle Pleistocene mandible from Baishiya Karst Cave (BKC) on t

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 hesize that nitrogen cycling in the Pliocene-Pleistocene Mediterranean resembled modern, highly strat

222 tent with the sedimentary record of Pliocene-Pleistocene Mediterranean sapropel events.

223 ch were key characteristics for predation on Pleistocene megafauna [5].

224 ong recovery times directly preceded the end-Pleistocene megafauna extinction, resulting in regional

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

226 t beaver was once one of the most widespread Pleistocene megafauna in North America.

227 The last remnants of the European Pleistocene megafauna that survived into the Holocene we

228 ange, and contributed to extinctions of late Pleistocene megafauna.

229 d representatives of the now largely extinct Pleistocene megafauna.

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

231 tracked community structure through the end-Pleistocene megafaunal extinction in North America.

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

233 y and/or plant resources) after the terminal Pleistocene megafaunal extinction.

234 ctic large carnivores that survived the Late Pleistocene megafaunal extinctions, responding to that p

235 logical and ecological aspects of both Upper Pleistocene modern humans (UPMHs) and Neandertals provid

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

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

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

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

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

241 ia auaritae, recovered from the lower-middle Pleistocene of the La Palma island.

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

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

244 s to assess the genetic processes underlying Pleistocene palaeontological patterns.

245 hat the Earth system has operated under late Pleistocene pCO(2) levels for an extended period.

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

247 the southern latitudes of Europe during Late Pleistocene periods.

248 in permafrost systems, soil cores spanning a Pleistocene permafrost chronosequence (19,000, 27,000, a

249 Here we investigate the late Pleistocene population history of northeastern Siberia t

250 nstrates the extreme variability of terminal Pleistocene populations in China and the possibility of

251 ck and gray whale lineages and that multiple Pleistocene populations were undertaking migrations of a

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

253 lope Drift is dominated by contourite mud of Pleistocene-Recent age, substantially younger than previ

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

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

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

257 ion during the Paleolithic, as well as wider Pleistocene sequences across Eurasia.

258 Instead, each Pleistocene Siberian canid branched off the lineage that

259 .(3)(5) Previous studies have suggested that Pleistocene Siberian canids can be classified into two g

260 We detected gene flow from Pleistocene Siberian wolves, but not modern American wol

261 changes in global climate at the end of the Pleistocene significantly impacted ecosystems across Nor

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

263 The Late Pleistocene sites feature 51 resident species that have

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

265 tely adapted to the "ice-age" climate of the Pleistocene steppe [4, 5].

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

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

268 mountain streams above the elevation of the Pleistocene terminal moraine retain floodplain sediment

269 er, the lack of firm age estimates for older Pleistocene terminations confounds attempts to test the

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

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

272 esian age-depth model that brackets the late Pleistocene through early Holocene, we analyzed and quan

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

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

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

276 any studies of Olduvai Gorge during Pliocene-Pleistocene times have revealed the presence of precessi

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

278 arge effective population size over the Late Pleistocene to Holocene.

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

280 transfer and sediment storage from the late Pleistocene to the present day.

281 extreme northeast of Eurasia during the Late Pleistocene-to-Holocene warming events.

282 cally significant differences across the mid-Pleistocene Transition (ca. 1.2-0.8 Ma), suggesting that

283 The mid-Pleistocene transition (MPT) is widely recognized as a s

284 , whereas C(3) grasses decline after the mid-Pleistocene transition (MPT, c.

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

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

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

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

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

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

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 logenetic break possibly dating to the Early Pleistocene was inferred between the African and Asian L

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

296 such precipitates were abundant in the late Pleistocene, whereas present-day sedimentation is domina

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

298 ages in Argentina began during or before the Pleistocene, which is hard to reconcile with the hypothe

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

300 ns cluster with the two previously sequenced Pleistocene wolves, which are genetically more similar t