ライフサイエンスコーパス: fauna

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

2 ian pests that threaten its unique flora and fauna.

3 tionally associated with the exploitation of fauna.

4 nd the consequences for dependent vertebrate fauna.

5 , both of which lack functionally-associated fauna.

6 precipitation to support rich vegetation and fauna.

7 ist taxa composing a tree species' herbivore fauna.

8 of new information on the past Asian insect fauna.

9 r the persistence of a globally endemic fish fauna.

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

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

12 hogens, threatening the archipelago's unique fauna.

13 and conservation of the cryptic subterranean fauna.

14 a substantial proportion of their vertebrate fauna.

15 e environmental drivers were influencing the fauna.

16 continues, potentially decimating its native fauna.

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

18 n the range shown to adversely impact marine fauna.

19 and centre of origin for the global deep-sea fauna.

20 a discernible effect beyond the large mammal fauna.

21 equences for other components of the benthic fauna.

22 le zonation of nutritional modes of the vent fauna.

23 ng pollutants effects in this highly exposed fauna.

24 hermal venting, and the biogeography of vent fauna.

25 l studies to investigate POP effects in this fauna.

26 tential ecotoxicological impacts on deep-sea fauna.

27 ed a role in the radiation of this black fly fauna.

28 igate the vertebrate portion of Madagascar's fauna.

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

30 s via infected prey, altering their parasite fauna.

31 lting in large mortality events in estuarine fauna.

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

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

34 d sediment risks causing toxicity to aquatic fauna.

35 t that also included aquatic and terrestrial fauna.

36 n situ origin and uniqueness of the mountain fauna.

37 , with profound consequences for the endemic fauna.

38 interacts, such as compositions of arthropod faunas.

39 d significant loss of biodiversity in marine faunas.

40 suppression of speciation within Laurentian faunas.

41 ntrast to normal survival and early recovery faunas.

42 ive under-description of tropical parasitoid faunas.

43 omponent of marine and freshwater vertebrate faunas.

44 the predominantly sessile Paleozoic crinoid faunas.

45 of the extinction, dominating all subsequent faunas.

46 species in tropical faunas than in temperate faunas.

47 ial reservoirs and mass extinction of marine faunas.

48 two of the most prominent threats to native faunas.

49 dovician exceptionally preserved open-marine faunas.

50 Between deposition of the last fossil fauna (~5 ka) and the present day, a drastic increase in

51 We retrodict also that soil fauna across the Permian-Triassic and Triassic-Jurassic

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

53 oposed for the re-establishment of the Irish fauna after the last ice age: arrival across a late-glac

54 ariate (ordination) analyses of the ostracod faunas allow demarcation of a Midcontinent Province and

55 ariable for both deep water macro- and meio- fauna along latitudinal and longitudinal gradients.

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

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

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

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

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

61 Madagascar is well known for its diverse fauna and flora, being home to many species not found an

62 er species including terrestrial and aquatic fauna and flora.

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

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

65 f endemic island faunas by imported mainland fauna and in today's anthropogenic, but threatened, Medi

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

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

68 uence from other areas, resulting in unusual faunas and floras, often unlike those found anywhere els

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

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

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

72 d new fire regime would transform the flora, fauna, and ecosystem processes in this landscape and may

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

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

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

76 Pathogen diversity is maintained by multiple faunas, and facilitated by pronounced host vagility, as

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

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

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

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

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

82 Peripheral fauna are not dominated by a single taxon, but include p

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

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

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

86 Thus, tropical amphibian faunas are threatened both by destruction of natural hab

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

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

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

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

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

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

93 Understanding the impact of noise on marine fauna at the population level requires knowledge about t

94 The ostracode fauna at this site did not fully recover until approxima

95 The origin and possible antiquity of faunas at deep-sea hydrothermal vents and seeps have bee

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

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

98 coincided with major turnover in vertebrate faunas, but previous studies have found little floral ch

99 provincial and biogeographically fragmented fauna by Middle Triassic times (Anisian, approximately 2

100 accumulation and a detritus-based arthropod fauna by the Middle Devonian period.

101 n the complete replacement of endemic island faunas by imported mainland fauna and in today's anthrop

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

103 ea anoxic/dysoxic events did not affect seep faunas, casting doubt on the suggested anoxic nature and

104 the observed extinction in the Rancholabrean fauna, changes in the Paleoindian cultures, and the onse

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

106 Smaller soil fauna co-occur with dwarf mammal taxa during the PETM; t

107 Encrusting fauna, collected from impacted and nonimpacted metres ea

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

109 The MAR fauna comprises mainly species known from continental ma

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

111 Soil fauna consistently enhanced litter decomposition at both

112 This new fauna constitutes a new biogeographic province with Nort

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

114 ographic structure of shallow-marine benthic faunas, defined by existing biogeographic schemes, can b

115 Late Ordovician Sandbian (ca 461 to 456 Ma) faunas, demonstrates strong endemicity at the species-le

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

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

118 Middle Cambrian, after which the Palaeozoic fauna dominates.

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

120 ate for the inclusion of biome-specific soil fauna effects on litter decomposition as a mean to reduc

121 quickly replaced more archaic Late Triassic faunas, either by outcompeting them or when the more arc

122 Fauna-enhanced denitrification is a potentially importan

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

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

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

126 Although independently diversified regional faunas exhibit convergent morphology, species are cluste

127 Terrestrial invertebrates dominate the fauna, exhibiting traits that allow exploitation of vari

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

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

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

131 The former represents the oldest echinoderm fauna from Gondwana, approximately equivalent in age to

132 erica, and the latter the oldest diversified fauna from Gondwana.

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

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

135 highlights the endemic, diverse dryolestoid fauna from the Cretaceous of South America.

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

137 ate Triassic, demonstrates that the theropod fauna from the Late Triassic of North America was not en

138 A 5-myr record of mammalian faunas from floodplain ecosystems of South Asia shows su

139 ( approximately 38 million years (Myr) ago) faunas from Patagonia, South America, is therefore thoug

140 e report the discovery of two new echinoderm faunas from the early part of the Cambrian of Morocco (W

141 ty of therapsids, the new finds suggest that faunas from the poorly sampled xeric belt that straddled

142 Major differences in the associated mammal faunas from the southern China sites and those from Sout

143 mprehensive assessment focuses on the oldest fauna, from the Blue Lias Formation of Street, and nearb

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

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

146 seasonality in the formation of polar marine faunas has implications for contemporary ecosystem struc

147 ea) with an otherwise depauperate freshwater fauna, has an ariid invasion gained any substantial trac

148 We predict that soil fauna have already shown reductions in size over the las

149 , but the spatial dynamics of their distinct fauna have yet to be elucidated.

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

151 an analysis of the present-day Caribbean ant fauna, I have narrowed the list of suspects to two speci

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

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

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

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

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

157 pensylvanica) on a largely endemic arthropod fauna in Hawaii.

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

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

160 , a more homogeneous and broadly distributed fauna in the Late Permian (Wuchiapingian, approximately

161 e rates of change for an entire regional bee fauna in the northeastern United States, based on >30,00

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

163 The black fly fauna in the Society Islands French Polynesia is notable

164 umptions, the presence and reseeding of this fauna in the subtropical southeast Atlantic was driven b

165 Low-diversity mammalian fauna in the western Williston Basin persisted for as li

166 ts a possible successional sequence for vent fauna in this new biogeographic province.

167 sence of preservation of similar soft-bodied faunas in later periods.

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

169 ted with this development of Paleocene polar faunas in that those in the south are more strongly diff

170 The owl roost fauna includes Rallus undescribed sp. (extinct; the firs

171 entral Florida's latest Hemphillian Palmetto Fauna includes two machairodontine felids, the lion-size

172 A diverse fauna includes two new species, here reported from two o

173 oincides with the emergence of the Ediacaran fauna, including large, motile bilaterian animals, ca. 5

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

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

176 rent echinoderm body plans in these earliest faunas indicates that considerable diversification had a

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

178 e Neotropics, the Central American butterfly fauna is best known in terms of general natural history,

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

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

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

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

183 latent risk to reveal areas where the mammal fauna is still relatively unthreatened but has high inhe

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

185 gest that greater specialization in tropical faunas is the result of differences in trophic interacti

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

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

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

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

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

191 those of deep-sea taxa, suggesting that seep faunas may be shaped by the factors that drive the evolu

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

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

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

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

196 vironments will dramatically change the fish fauna of California.

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

198 is a remnant of the highly endemic Mesozoic fauna of nontribosphenic mammals in SA and extends the k

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

200 and some aspects of the hallmark 'Gondwanan' fauna of South America and Africa may therefore reflect

201 to >60 m, complete with cold-water flora and fauna of temperate affinities.

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

203 distinctive characteristics in the mammalian fauna of the island.

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

205 The freshwater stream fauna of tropical oceanic islands is dominated by amphid

206 The Early Cretaceous fauna of Victoria, Australia, provides unique data on th

207 y dissimilar to penecontemporaneous dinosaur faunas of Africa and South America, which represent an a

208 The disappearance of faunas of Burgess Shale type curtails the stratigraphic

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

210 morphologies displayed by stem organisms in faunas of the Burgess Shale type.

211 The renowned soft-bodied faunas of the Cambrian period, which include the Burgess

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

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

214 Similarities between dinosaur faunas of Victoria and the northern continents concern t

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

216 cologically important members of the benthic fauna on coral reefs.

217 ty differently modulated the effects of soil fauna on decomposition rates between biomes, from climat

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

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

220 apes leads to striking convergence of entire faunas on four islands.

221 raditional taxonomic approaches, namely that faunas on these widely separated archipelagos stem from

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

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

224 bathypelagic species are replaced by benthic fauna otherwise unable to survive in the mid ocean.

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

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

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

228 ter downward transport and loss suggest that fauna prefer PHY, due to its lability and/or toxins asso

229 nvironments may have been hospitable for the fauna preserved in the Yangtze Gorges, which includes th

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

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

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

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

234 However, the role played by soil fauna remains largely unknown, despite its importance fo

235 versity of mammals and the mosaic pattern of fauna replacement in SA during the Cenozoic.

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

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

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

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

240 ariate statistical methods to detect how the fauna responded to environmental changes during the earl

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

242 emoved and added to an otherwise stable prey fauna, revealing specific and persistent trophic interac

243 3)C was traced into sediment organic carbon, fauna, seagrass, bacteria, and microphytobenthos and int

244 Marine reptile faunas shifted from ichthyosauromorph-dominated to sauro

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

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

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

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

249 resolution, radiocarbon-dated sequence of 22 faunas spanning the Holocene documents stasis up to the

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

251 by three intensively-sampled European fossil faunas, spanning 20 million years (Ma).

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

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

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

255 tern that is also reflected in other benthic faunas such as brachiopods.

256 t past included a range of extinct enigmatic fauna, such as elephant birds, giant lemurs and dwarfed

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

258 y outcompeting them or when the more archaic faunas suddenly became extinct.

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

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

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

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

263 diversity) between tree species in tropical faunas than in temperate faunas.

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

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

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

267 ogeny are quickly colonized with a symbiotic fauna that is provisioned in mother's milk and that clos

268 s some of the most diverse floras and insect faunas that are known, but its Cenozoic fossil record of

269 n period differed markedly from well-sampled faunas that dominated tropical-to-temperate zones to the

270 f northern Niger provide an insight into the faunas that inhabited low-latitude, xeric environments n

271 d assemblages of taxa, or major evolutionary faunas that we can then study in relation to climatic ch

272 ften deleterious effects on native flora and fauna, the consequences of biological invasions for huma

273 Evidence from the distinctive fauna, the unique community structure, and multivariate

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

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

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

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

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

279 arch of hydrothermal activity and associated fauna to assess changes since previous surveys and to ev

280 data from the natural history of the modern fauna to sketch a history of major ecological adaptation

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

282 Tropical forest insect faunas vary in space and time, and these partitions can

283 Fifty percent of California's native fish fauna was assessed as having critical or high baseline v

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

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

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

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

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

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

290 Marine and nonmarine faunas were equally affected, precluding the existence o

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

292 pecies should be broadened to include entire faunas when estimating and predicting the effects of per

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

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

295 ution; Nilo-Saharan speakers hunting aquatic fauna with barbed bone points occupied the southern Saha

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 uthern Sahara, while people hunting Savannah fauna with the bow and arrow spread southward.

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

300 stock with depth depends on the size of the fauna, with macrofaunal abundance only declining with in

301 .3 Ma) affected the distribution of tetrapod faunas within the southern hemisphere and apply quantita