ライフサイエンスコーパス: fauna

1 ean communities co-existed with the "Mammoth fauna".

2 spread taxa, leading to homogenous 'disaster faunas'.

3 needed to enable the dispersal of flora and fauna.

4 in a community of comparatively dry-adapted fauna.

5 ortation of contaminants by seabirds to soil fauna.

6 d acute harmful effects on natural flora and fauna.

7 essive extinction events reshaped the marine fauna.

8 rpation or complete extinction of anchialine fauna.

9 as yielded a particularly diverse vertebrate fauna.

10 er charismatic species of the lost Mascarene fauna.

11 standpoint, ecological traits within extinct fauna.

12 ian pests that threaten its unique flora and fauna.

13 e terrestrial, aquatic, and aerial flora and fauna.

14 to a low and patchy density of vent-endemic fauna.

15 d sediment risks causing toxicity to aquatic fauna.

16 precipitation to support rich vegetation and fauna.

17 and conservation of the cryptic subterranean fauna.

18 habitat for 832 species of native vertebrate fauna.

19 that are degraded by a species-rich benthic fauna.

20 tential ecotoxicological impacts on deep-sea fauna.

21 s via infected prey, altering their parasite fauna.

22 lting in large mortality events in estuarine fauna.

23 ng a changing balance of benthic and pelagic fauna.

24 ds for protecting the world's most imperiled fauna.

25 t that also included aquatic and terrestrial fauna.

26 n situ origin and uniqueness of the mountain fauna.

27 , with profound consequences for the endemic fauna.

28 tionally associated with the exploitation of fauna.

29 nd the consequences for dependent vertebrate fauna.

30 the conservation status of the longleaf bee fauna.

31 , both of which lack functionally-associated fauna.

32 ist taxa composing a tree species' herbivore fauna.

33 of new information on the past Asian insect fauna.

34 r the persistence of a globally endemic fish fauna.

35 ct subset of the shallow water (<30 m) coral fauna.

36 e northern deep-sea fauna to Antarctic shelf fauna.

37 hogens, threatening the archipelago's unique fauna.

38 tential long-lasting Lilliput effect in this fauna.

39 disrupting original communities of flora and fauna.

40 d trait-based community structure of benthic fauna.

41 o other novel reproductive modes of deep-sea fauna.

42 ash, avocado, and other fruits and harvested fauna.

43 les for these two Neandertals and associated fauna.

44 have impacted the evolution of its flora and fauna.

45 quency distribution of ecomorph types within faunas.

46 ntrast to normal survival and early recovery faunas.

47 two of the most prominent threats to native faunas.

48 dovician exceptionally preserved open-marine faunas.

49 interacts, such as compositions of arthropod faunas.

50 interval is largely obscure for terrestrial faunas.

51 d significant loss of biodiversity in marine faunas.

52 the marked turnover of foraminifera and reef faunas.

53 cies-level drivers of mammalian ectoparasite faunas.

54 stal foundation species and their associated fauna [1], while fishing can alter coastal food webs, re

55 Multivariate analysis of vent fauna across three oceans places Longqi in an Indian Oce

56 al or dispersed into the region as part of a fauna adapted to more open habitats.

57 ed widespread changes in the ichthyoplankton fauna along the coast of the Northeast Pacific Ocean, bu

58 ls occur alongside the remains of an insular fauna and a simple stone technology that is markedly sim

59 are regarded as alien to the European aphid fauna and among them nine are believed to be the first p

60 vidence for a synchronous turnover of flora, fauna and climate at the Eocene-Oligocene Boundary in a

61 consequences of this acidification on marine fauna and ecosystems are the subject of an increasing nu

62 on the interactions between ground-dwelling fauna and fleshy fruits.

63 International Trade in Endangered Species of Fauna and Flora (CITES), including the whale shark (Rhin

64 ecies-rich assemblages with other encrusting fauna and flora (corraline algae), and are highly abunda

65 re we present an inventory of the freshwater fauna and flora found in a sediment sample from the mumm

66 est occurrence(s) of some taxa in the modern fauna and flora giving new insights into the ecology and

67 e extremes, on the interaction between these fauna and flora has not been identified or elucidated, y

68 y focussed on encountering and photographing fauna and flora, yet the data collected in these efforts

69 l to protect domestic agriculture and native fauna and flora.

70 er species including terrestrial and aquatic fauna and flora.

71 vements, and their putative effects on local fauna and flora.

72 y on Earth's most diverse aquatic vertebrate fauna and highlights the importance of including multipl

73 develop proxies for geographic locations of fauna and humans.

74 slands has been observed both in the present fauna and in the fossil record.

75 esults indicate that nutrient transfer, soil fauna and inhibitory secondary compounds can influence m

76 eservation frames all interpretations of the fauna and its evolutionary significance.

77 owth of plant roots and the activity of soil fauna and microorganisms.

78 used to assess the organic carbon uptake by fauna and sediments, when both sources and consumers wer

79 The spatial distributions of the total fish fauna and that of the two dominant morphotypes (Coryphae

80 that biological feedbacks from plants, macro-fauna and the microbiome influence soil structure, and t

81 , suggesting modern humans integrated exotic faunas and other novel resources into their symbolic wor

82 volatile coastlines, (iii) migratory marine fauna, and (iv) plankton that are the most abundant euka

83 umented and experimentally amenable parasite fauna, and are well suited to both laboratory and field

84 ging and can negatively impact marine flora, fauna, and ecosystems.

85 background in association with a depauperate fauna, and fall to pre-extinction levels during signific

86 le stars), a dominant component of sea-floor fauna, and find patterns of biodiversity unlike known te

87 European peninsulas were refugia for flora, fauna, and human groups.

88 ties for seabirds, marine mammals and seabed fauna, and no benefit to fish stocks.

89 ies, hydrothermal biota coexisting with seep fauna, and porewater biogeochemical signatures indicativ

90 ting all evacanthine tribes and all regional faunas, and fourteen putative outgroup taxa were include

91 hological diversity in the Hispaniolan anole fauna appear to have changed little between the Miocene

92 ution patterns of macroplanktonic graptolite faunas ( approximately 447-444 Ma) leading into the Late

93 cts turn into antagonistic effects when soil fauna are absent or litter is in very late stages of dec

94 Stalked fauna are also abundant on the hard substrates of the Ha

95 In turn, many of these fauna are dependent on the flowering phenology of the pl

96 the specific biological sources of imported fauna are often difficult to identify, in particular if

97 ography and ecology of its hydrothermal vent fauna are previously unknown.

98 Post-extinction survival faunas are invariably low diversity, especially benthic

99 ) and their highly speciose and endemic fish fauna as a model system.

100 el reveals for the first time that temperate fauna as well as tropical fauna may experience substanti

101 s the diet of fossil hominins and associated fauna, as well as trophic relationships in past food web

102 nger Dryas changes in temperature, flora and fauna assemblages, and human adaptations.

103 of magnitude higher in species richness than faunas assembled by immigration alone.

104 tran Pleistocene cave with a rich rainforest fauna associated with fossil human teeth.

105 The vertebrate fauna associated with Gurbanodelta is most similar to th

106 ironmental changes will affect highly mobile fauna at a global scale.

107 of deep-sea benthic biodiversity of sessile fauna at ca. 400 m depth.

108 cord coupled with a shift to cattle and wild fauna at most sites north of the Balkan mountain range.

109 epresentatives of the deep hydrothermal vent fauna at the Mid-Atlantic Ridge.

110 d establish one of the last diverse dinosaur faunas before the end-Cretaceous extinction.

111 s generally predict that coastal and neritic fauna benefit during sea-level rise (transgression), whe

112 Marine-adapted anchialine fauna benefit from habitat expansion during transgressio

113 l production, microbial communities and soil fauna biomass.

114 ly associated with the occurrence of benthic fauna burrows and seagrass roots.

115 FOS), have been regularly detected in marine fauna but little is known about their current levels or

116 h alterations are well known for terrestrial fauna but poorly documented for marine species.

117 evidence of the ingestion of MPs by deep-sea fauna, but knowledge of MPs' fate once ingested still re

118 investigate the ecological spectrum of these faunas by classifying their major taxonomic components i

119 Wiwaxia foliosa sp. nov. from the Xiaoshiba fauna (Cambrian Stage 3, Hongjingshao Formation, Kunming

120 ical structure of eastern Africa's herbivore faunas came to resemble those of the present, here we an

121 tly drive demographic responses(3,4) and yet fauna can use local thermal refugia to avoid extremes(5-

122 ated with endemic trilobites and three major faunas can be distinguished: olenellids, redlichiids, an

123 International Trade of Endangered Flora and Fauna (CITES) treaty; (2) assess the origin and by exten

124 Encrusting fauna, collected from impacted and nonimpacted metres ea

125 extinctions are thought to produce 'disaster faunas', communities dominated by a small number of wide

126 This fauna comprises 16 native species from 11 genera and 4 t

127 The MAR fauna comprises mainly species known from continental ma

128 address ecosystem representation, threatened fauna, connectivity and climate change.

129 The continent's terrestrial fauna consists only of invertebrates, with just two nati

130 This new fauna constitutes a new biogeographic province with Nort

131 Anchialine fauna currently exhibit a disjunct biogeography that can

132 Radiocesium concentrations in some benthic fauna declined more slowly than in pelagic fish in the s

133 implications of these changes for vertebrate fauna dependent on these resources.

134 tes a low uptake of contaminants in the soil fauna, despite seabird-derived contamination of their ha

135 l dynamics of tropical reefs explains marine fauna diversification in the Tethyan Ocean during the Cr

136 morphological specialization over successive faunas during the past 66 My.

137 and cultural activities associated with this fauna (e.g., birdwatching and/or hunting).

138 ming central approaches for studying benthic fauna (e.g., quantifying species presence, behavior, and

139 Fauna-enhanced denitrification is a potentially importan

140 ie covariation between native and non-native faunas, especially in highly variable environments.

141 g term, predicting the persistence of native fauna even in the face of invasion.

142 Although the fauna evidently comprised opportunistic species adapted

143 any ecomorphotypes familiar to modern mammal fauna evolved independently early in mammalian evolution

144 malies, with active methane venting and seep fauna exist in response to magma emplacement into sedime

145 o the effects of climate change, with Arctic fauna experiencing the greatest FEN contraction.

146 t, there was no increase in carbon uptake by fauna exposed to both stressors in combination, indicati

147 recta, suggesting a characteristic microbial fauna for this insect genus.

148 frica is home to diverse avian and mammalian fauna for which almost no information exists on IAV dyna

149 the phenomena that most clearly distinguish fauna from flora: perception, cognition, and motor activ

150 on a new early Permian continental tetrapod fauna from South America in tropical Western Gondwana th

151 iscovery of an extraordinary new soft-bodied fauna from the Burgess Shale.

152 we report the discovery of a diverse primate fauna from the early Oligocene of southern China.

153 ccommodated emerging dryland-adapted amniote faunas from a western Pangaean epicentre.

154 nd the habitat suitable for fish and benthic fauna had expanded (D).

155 We show that each evolutionary fauna has a unique, nonrandom association of ecomorphs,

156 ve and mostly endemic Australian land mammal fauna has suffered an extraordinary rate of extinction (

157 Both marine and terrestrial fauna have been affected by warming(1,2) but an explicit

158 more diversity to the Liaoning dromaeosaurid fauna, helps further reveal a distinct short-armed baupl

159 ard range expansion of marine macroflora and fauna, however, the impacts on the structure and functio

160 disease outbreaks often originate from wild fauna; (ii) anthropological expansion increases the risk

161 nilifera ssp. rotundata) on native flora and fauna in a eucalypt forest in south-eastern Australia.

162 cranium and preserved DNA found with extinct fauna in a submerged cave on Mexico's Yucatan Peninsula.

163 ebrates in the world oceans and of mammalian fauna in Europe and Asia in the Cenozoic era.

164 e climate to small rodent/lagomorph-dominant fauna in forest-steppe in a dry-temperate climate across

165 hange from large-size perissodactyl-dominant fauna in forests under a warm-temperate climate to small

166 Climate-driven migrations of fauna in human-dominated landscapes will likely interact

167 redictors of the richness of tropical forest fauna in logged forest.

168 ter one year, we assessed abundances of soil fauna in lower trophic levels and indirect impacts on le

169 nges in the species composition of the aphid fauna in reference to the Eastop's studies in 1960s were

170 al data can clarify ecological attributes of fauna in sites that have subsequently been altered by an

171 e Gravettians are similar to the local macro-fauna in terms of Sr isotopic signal, the Epigravettians

172 ormation and its dinosaur-bearing vertebrate fauna in the Ischigualasto-Villa Union continental rift

173 While the fauna in the older unit is comparable to that at Hadar a

174 Distribution patterns of fragile gelatinous fauna in the open ocean remain scarcely documented.

175 Stalked-sponge fauna in the Peru Basin require the presence of manganes

176 focus on physiology and taxonomy of pelagic fauna in the study region, our study presents biodiversi

177 idae) are conspicuous members of understorey faunas in lowland Neotropical forests.

178 neages representing some of the most diverse faunas in the world today, such as lepidosauromorphs (e.

179 is a major threat to the native invertebrate fauna, in particular to the endemic wingless flies Anata

180 strates why similar basins are attractive to fauna, including our ancestors, in regions like eastern

181 E cat bones and further 34 of the associated fauna, including the European wildcat.

182 studies of previously well-researched insect faunas indicate that 1-2% of species may be truly crypti

183 Pastoral Neolithic (c 5000 to 1200 BP) faunas indicate that herders relied on cattle, sheep, an

184 assess how climate, litter quality and soil fauna interact to determine such rates.

185 sts the persistence of rhynchosaur-dominated faunas into the earliest Norian.

186 Unfortunately, due to dramatic declines this fauna is among the most threatened globally.

187 the effects of microplastics on terrestrial fauna is completely lacking.

188 Arabian Oligocene primate faunas, this Asian fauna is dominated by strepsirhines.

189 tion of resource availability for vertebrate fauna is likely to fluctuate, and the time intervals bet

190 but unfortunately, our understanding of such fauna is limited and their genetic variability and evolu

191 d assumption that the origin of polar marine faunas is linked to the onset of major global cooling in

192 previously independently evolving floras and faunas is thought to be one of the key factors that shap

193 d annually, with two-thirds of all monitored fauna killed in a single year (2009).

194 The megadiverse Neotropical fish fauna lacks a comprehensive and reliable DNA reference d

195 n and reptilian members of the Eocene Arctic fauna, likely over-wintered in the Arctic.

196 he antiquity of the specialized harpacticoid fauna living in this habitat.

197 ime that temperate fauna as well as tropical fauna may experience substantial FEN expansion with ocea

198 e change and sub-alpine rather than tropical faunas may be the most sensitive to climate change.

199 vel of FOR is consistent across the six fish faunas, meaning that, whatever the richness, over a thir

200 Responses of soil fauna, microbial biomass, and nitrogen mineralization sh

201 ndings indicate that South American ecotonal faunas might experience high rates of occupancy turnover

202 nsgressions, but fresh- and brackish-adapted fauna must emigrate, evolve to accommodate local habitat

203 rs had a greater influence on the chironomid fauna obscuring the chironomid diversity-temperature rel

204 , to the heterogeneous patterns of flora and fauna observed by urban ecologists.

205 Together with a diverse fauna of basal snakes from the Cretaceous of South Ameri

206 mmon biogeographic barrier for the flora and fauna of California.

207 point to the importance of the formerly rich fauna of large herbivores in sustaining structurally div

208 the Early Cambrian (Series 2) Sirius Passet Fauna of North Greenland, and propose that its frontal a

209 The fauna of Russia primarily includes widespread generalist

210 ndings highlight that the freshwater bivalve fauna of Southeast Asia primarily originated within thre

211 site adequately captures the entire landbird fauna of the combined focal islands.

212 hondrial genetic diversity for the butterfly fauna of the Iberian Peninsula with unprecedented resolu

213 to the most iconic species of the enigmatic fauna of the Mascarene Islands that went largely extinct

214 d more remote regions, much of the flora and fauna of the world are experiencing evolutionarily unpre

215 to explain the differences in the flora and fauna of tropical and temperate regions assume that whol

216 xpedition to survey the high-altitude rodent fauna of Volcan Llullaillaco in the Puna de Atacama of n

217 apex predator in the late Campanian dinosaur faunas of Laramidia; its absence from later units indica

218 erchange between the previously disconnected faunas of North and South America was a massive experime

219 that of small perissodactyls that dominated faunas of the Mongolian Plateau in the Eocene, and proba

220 e late Silurian-earliest Devonian vertebrate faunas of the South China Block [4].

221 geographic barrier between freshwater mussel faunas of the Western Indochina and Sundaland subregions

222 are especially diverse in tropical Asia, the faunas of which are characterized by high levels of ende

223 ght, but significantly lower than a range of fauna often found in association with anthropogenically

224 eotropics harbour the most diverse flora and fauna on Earth.

225 studies to quantify the effect sizes of soil fauna on litter decomposition rates at the global and bi

226 sments, the results indicate that anchialine fauna on low-lying islands and platforms that depend upo

227 al theory on the trophic impacts of invasive fauna on native competitors is equivocal.

228 a ninefold richness gradient in global fish faunas on tropical reefs encompassing 6,316 species dist

229 ontinue to accumulate in regional floras and faunas, or whether the pace of accumulation will decreas

230 ation increases with lake size, resulting in faunas orders of magnitude higher in species richness th

231 season investigation (3 years) of the aerial fauna over Africa, we sampled insects flying 40-290 m ab

232 Much of the loss of Australian land mammal fauna (particularly in the vast deserts and tropical sav

233 itecture which supports diverse and abundant fauna, particularly of reef fish.

234 The geology and associated vertebrate fauna place these tracks in a deltaic setting, near a la

235 Soil fauna play a fundamental role on key ecosystem functions

236 tion by bioeroding sea urchins and burrowing fauna (polychaete worms, bivalve mollusks) increased fro

237 ese tools on the butchery and consumption of fauna, probably by early Homo erectus sensu lato.

238 Forest vertebrate fauna provide critical services, such as pollination and

239 e human remains, grave goods, and associated fauna provide rare direct data on organic technology, ec

240 In the absence of human remains, fauna provide the best proxy for human movement.

241 ted for any Hirnantian fossil group, and the fauna provides a unique window into a post-extinction ec

242 n and sulphur stable isotope analysis of the fauna provides palaeoenvironmental information for this

243 However, the origin of these iconic faunas remains poorly understood because of a large, glo

244 nism samples covering the breadth of aquatic fauna requires a concerted effort to build supporting ba

245 lationships between global change and native faunas requires a quantitative toolkit that effectively

246 t cause declines in habitat availability for fauna requiring open vegetation structure (such as migra

247 niform in the challenges they present to the faunas residing in them.

248 Asian and Afro-Arabian primate faunas responded differently to EOT climatic deteriorati

249 Marine reptile faunas shifted from ichthyosauromorph-dominated to sauro

250 Although both faunas show the expected overall poleward decline in spe

251 The collective herbivore fauna shows two major change points in carbon isotope va

252 ation is its Southern equivalent, bringing a fauna similar to that of the Lufeng Formation to light.

253 a particularly dramatic effect on the Modern Fauna, so an understanding of the conditions that led to

254 ch, specifically altered precipitation, soil fauna, soil community composition, and litter decomposit

255 A spectacular Cambrian soft bodied fauna some 40 km from Walcott's original Burgess Shale l

256 that circulated among Australian metatherian fauna sometime during the late Eocene to early Oligocene

257 , a prominent biogeographic barrier dividing faunas spanning the monsoon tropics in northern Australi

258 ving in neighbourhoods with a high number of fauna species appears to be associated with a higher ris

259 m with a number of threatened and endangered fauna species susceptible to the deterioration of water

260 reducing its availability to less desirable fauna such as rats.

261 hting influences the behaviour of intertidal fauna such that the balance of interspecific interaction

262 have explicitly considered effects on tundra fauna, such as the millions of migratory songbirds that

263 over the past 3 My, but the western Atlantic fauna suffered more severe Pliocene-Pleistocene extincti

264 Ecological studies of hypoxia and marine fauna suggest multiple mechanisms through which hypoxia

265 tope data from calcite shells of the benthic fauna suggest that bottom water temperatures in the west

266 esholds of taxonomic groups of shallow-water fauna, suggesting that pressure tolerance is indeed oxyg

267 limate change forced a turnover of flora and fauna, suggesting there was a change from large-size per

268 worldwide, but comparable to Early Triassic faunas, suggesting a potential long-lasting Lilliput eff

269 ols also influence the soil micro- and macro-fauna that break down plant leaf litter.

270 ally, the new monkey is a member of a unique fauna that had dispersed from Africa and southern Asia i

271 of a diversity of depth habitats by a unique fauna that includes a group of teleost fish of the sub-o

272 pisodes of faunal associations-"evolutionary faunas"-that correspond well with previously proposed qu

273 ubregion having a largely endemic freshwater fauna, the boundaries of this subregion are still unclea

274 wed with a rich and largely endemic scorpion fauna, the origins of which have not been previously inv

275 espite intensive taxonomic work on the local fauna, the potential forces driving genetic divergences

276 s the largest land carnivoran present in the fauna, there is no evidence that it competed with these

277 , biodiversity and distributions of deep-sea fauna, thereby compromising key ecosystem services.

278 In the modern fauna, these tiny phytophages comprise insects of great

279 d contrast to Afro-Arabian Oligocene primate faunas, this Asian fauna is dominated by strepsirhines.

280 uses direct loss of habitat but also impacts fauna through collisions.

281 Precipitation may affect fauna through direct effects on physiology, behaviour or

282 he vulnerability of desert wetland flora and fauna to abrupt climate change.

283 s hypotheses relating more northern deep-sea fauna to Antarctic shelf fauna.

284 pulation 6699), which were devoid of benthic fauna up to 580 m from the effluent source in response t

285 Contrary to our hypothesis, the moth fauna was more sensitive to elevational differences with

286 Indian Ocean islands and their rich endemic fauna, we show that highly diverse UMRVs exchange betwee

287 on the ecomorphological composition of these faunas, we analyze via contingency tables and detrended

288 s on the seafloor; recognisable vent endemic fauna were not observed.

289 n increased plant biomass, direct effects on fauna were often stronger than plant-mediated effects.

290 in food availability, but its effects on the fauna were regulated by fundamental reproductive and eco

291 Endosymbiont-bearing fauna were very important in supporting the transfer of

292 tefacts and remains of other extinct endemic fauna, were dated to between about 95 and 12 thousand ca

293 , can function as marine refugia for pelagic fauna, whereas offshore locations are potentially more c

294 e soft tissue and skeletal anatomy of minute fauna, which are not typically preserved in other deposi

295 are cosmopolitan members of the mesopelagic fauna with at least ten different eye configurations acr

296 ate humid belt where a provincial vertebrate fauna with early dinosaurs may have incubated.

297 tifies coastal biogeographic provinces where fauna with high intrinsic risk are strongly affected by

298 Together, these processes produce lake fish faunas with highly variable composition, but with divers

299 on average erased 56.5% of the local source fauna, with ungulates comprising the most ubiquitous los

300 ssic was a time of major changes in tetrapod faunas worldwide, but the fossil record for this interva