ライフサイエンスコーパス: biota

1 of organisms and can pose a risk to aquatic biota.

2 ated feathers, first recognized in the Jehol Biota.

3 despite singular changes in its terrestrial biota.

4 itions and can interact with the surrounding biota.

5 e shaped the biodiversity patterns of island biota.

6 the bioavailable properties of a compound in biota.

7 fects of ionizing radiation exposure on soil biota.

8 sent-day population structure of Palaearctic biota.

9 t period (1891 to 1903 CE) on the Australian biota.

10 hus reducing potential impacts on non-target biota.

11 likely causing rapid regional replacement of biota.

12 expansion but not population structure in AF biota.

13 tal heterogeneity relate to the evolution of biota.

14 nd (3) activated carbon amended sediment and biota.

15 esuspension and subsequent interactions with biota.

16 h simultaneous temporal measures of eDNA and biota.

17 f temporal trends of PCNs in Canadian Arctic biota.

18 nd negative feedback between plants and soil biota.

19 croplastics, particularly fibers, on aquatic biota.

20 hina, relative to the (Tremadocian) Fezouata biota.

21 the complete halogenated fingerprint of the biota.

22 ch there are no close relatives in the local biota.

23 bserved for other Western Hemispheric Arctic biota.

24 of biogeochemical cycles catalysed by extant biota.

25 pling are assessed for water, sediments, and biota.

26 owever, they have not been widely studied in biota.

27 e to fossils from the Cambrian Burgess Shale biota.

28 ntrations ever reported for this compound in biota.

29 ate the transfer of plastics to coprophagous biota.

30 made) sound has the potential to harm marine biota.

31 nia bifurcata n. gen., n. sp., dominates the biota.

32 roduced in a landmark study of a continental biota.

33 acts of changes to pCO2 levels on freshwater biota.

34 ived episodes of oxia that supported diverse biota.

35 ers are prevalent in seawater, sediments and biota.

36 elps to predict its toxic effects on aquatic biota.

37 cury (MeHg) are accumulated in Arctic marine biota.

38 nues to be to keep inimical aluminium out of biota.

39 a is a global hazard and a threat to exposed biota.

40 e enough to induce measurable HgT changes in biota.

41 ause function depends on prior conditions or biota.

42 n the elevated MeHg concentrations in Arctic biota.

43 d regenerating forests, to conserve regional biota.

44 ter, sediment, sludge, wastewater, soil, and biota.

45 duction and accumulation of methylmercury in biota.

46 reds of measurements of water, sediment, and biota.

47 y the highest burden recorded in terrestrial biota.

48 sils of the Precambrian soft-bodied Ediacara Biota.

49 referential loss of heavily calcified marine biota.

50 organic fluorine in sediment, and 9-108% in biota.

51 ds in aqueous environmental media and within biota.

52 a factor 6 of the monitored POP residues in biota.

53 ced rates of carbon (C) mobilisation by soil biota.

54 y mediated in part by interactions with soil biota.

55 ere it has the potential to affect nontarget biota.

56 h system models to project changes in marine biota.

57 budgets or to meet the demands of subsurface biota.

58 nvestigate ecotoxicological risks to benthic biota.

59 could rival the Chengjiang and Burgess Shale biotas.

60 nd the evolutionary history of ICA's diverse biotas.

61 freezing temperatures in partitioning global biotas.

62 elanosomes from fossil vertebrates from nine biotas.

63 following the secondary contact of different biotas.

64 orld's biogeographic realms and their native biotas.

65 synthetic fragrances and UV filters in both biota (136.9-159 ng g(-1)) and the dissolved phase (3322

66 of Psittacosaurus sp. from the Chinese Jehol biota [16, 17].

67 tions on the methodologies applicable to all biota, (2) compare MP contamination levels in fish and i

68 Lagerstatte from South China, the Qingjiang biota (~518 million years old), which is dominated by so

69 SA and the three FOSAAs were detected in all biota, a total of nine diPAPs were only detected in zoop

70 Biota accelerated CO(2) mineralization over abiotic cont

71 Soil biota accounts for ~25% of global biodiversity and is vi

72 mild summer drought and whether this affects biota across 43 littoral zone sites in 11 lakes.

73 re, we characterised multiple groups of soil biota across a plant diversity gradient in a long-term e

74 to estimate depletion and recovery rates of biota after trawling.

75 at has the potential to impact the health of biota, although its modes of action remain somewhat uncl

76 ity of functional strategies present in soil biota - analogous to broad scale patterns found in plant

77 alkyl acids (PFAAs) are persistent in marine biota and are toxic to many species, including marine ma

78 ce among four variables important to Earth's biota and associated systems: annual climatic water defi

79 al for application in chemical monitoring of biota and bioaccumulation studies.

80 ble peptides that would be available to soil biota and confirming the existence of an abiotic pathway

81 ions between gastrointestinal (GI) bacterial biota and diseases.

82 eflect the complete exposure of chemicals to biota and do not provide the complete halogenated finger

83 tic understanding of how flow regimes affect biota and ecosystem processes.

84 s the daunting scope of diversity in Earth's biota and environments.

85 CAN suppresses canopy tree species and other biota and favors rhizosphere food web.

86 lant diversity affects the responses of soil biota and growth of a focal plant to these disturbances.

87 Interactions with soil biota and herbivores were the strongest drivers of exoti

88 portance of socio-cultural factors for urban biota and how these may radically differentiate the unde

89 derway to determine potential harmfulness to biota and human health.

90 be very persistent and pose a health risk to biota and humans.

91 is a key process in making iron available to biota and in the mobilization of associated trace elemen

92 asured PFBS precursor may be accumulating in biota and metabolizing to PFBS, leading to a higher than

93 temporal variability in stream chemistry and biota and not only the presence of anthropogenic activit

94 s caused the most depletion, removing 41% of biota and penetrating the seabed on average 16.1 cm.

95 perimentally that one-time additions of soil biota and plant seeds alter soil-borne nematode and plan

96 ggesting an increasing connectedness of soil biota and plants.

97 of N (UAN) largely neglect canopy-associated biota and processes and therefore may not realistically

98 ut underestimates those on canopy-associated biota and processes, ii) with low-level N addition, CAN

99 vors canopy tree species and canopy-dwelling biota and promotes the detritus food web, and iii) with

100 a powerful molecular lens to observe marine biota and provides a series of 'snapshots' across a broa

101 trations of some hydrophobic contaminants in biota and sediment, particularly when implemented after

102 maller size may have negative impact on soil biota and soil organic matter may play a key role in mod

103 c matter decomposition is partitioned across biota and streambed compartments.

104 pand the ecological dimensions of the Rhynie biota and support the hypothesis that arcellinids transi

105 ility for plastic-bound NPs to interact with biota and surrounding matter.

106 on provides an important link between extant biota and the clues from the geologic record.

107 the environment and the resultant uptake in biota and transport in food webs.

108 Depletion of biota and trawl penetration into the seabed are highly c

109 hods for studies reporting concentrations in biota and water samples, we propose a method to assess t

110 rbor sediment (MA, U.S.A.), (2) sediment and biota, and (3) activated carbon amended sediment and bio

111 icroplastics in a gut fluid mimic of aquatic biota, and also included food to provide a better repres

112 rs within the Brazilian Atlantic Forest (AF) biota, and consequently two processes of diversification

113 TIR analyses of water, wastewater, sediment, biota, and food samples.

114 n exotic plant dominance, plant traits, soil biota, and invertebrate herbivores and measured indicato

115 ex interactions among litter chemistry, soil biota, and minerals in mediating soil C storage in unman

116 er ecosystem functions performed by the soil biota, and therefore, human-induced global changes have

117 Additional mercury measurements in biota appear to contradict the previously implied connec

118 nism from the late Carboniferous Mazon Creek biota (approximately 309-307 million years ago) of Illin

119 People and biota are chronically exposed to thousands of chemicals

120 FD environmental quality standards (EQS) for biota are expressed as wet weight.

121 Marine biota are redistributing at a rapid pace in response to

122 sediment-associated contaminants to benthic biota are still underrepresented in water quality assess

123 ale and persistence of its impacts on seabed biota are unknown.

124 rophobic organic compounds (HOCs) in aquatic biota are used for compliance, as well as time and spati

125 evelop methods to assess the extent to which biotas are geographically discrete, and find that transi

126 The mechanisms shaping island biotas are not yet well understood mostly because of a l

127 tropical-associated or temperate-associated biotas are often narrow, suggesting a role for freezing

128 but the evolutionary origins of their unique biotas are poorly understood.

129 However, most studies have considered soil biota as a black box or focussed on specific groups, whe

130 eltwater system that accumulates prokaryotic biota as it travels downstream.

131 been assumed to cause this process, with the biota as passive passengers on continental blocks.

132 Steroid hormones produce adverse effects on biota as well as bioaccumulation in fish and seafood, ma

133 linear and interactive effects on particular biota, as well as on community and ecosystem properties.

134 tudy the community structure of the Ediacara biota, as well as the autecology of individual organisms

135 is is the first time such a specific mineral-biota association has been observed for incirrate octopo

136 des may presage impacts of climate change on biota at higher latitudes.

137 Analyses of biota at lower latitudes may presage impacts of climate

138 des a pathway for exposure to ice-associated biota at the base of the pelagic food web.

139 Trans R Soc Lond B 361:1023-1038], Stirling biota [Bengtson S et al. (2007) Paleobiology 33:351-381]

140 rimary production (NPP), upper trophic level biota biomass and potential fisheries catches in the fut

141 ns and peptides account for 20-75% of marine biota biomass, of which a major fraction is metabolized

142 ion significantly affects soil chemistry and biota, but its effects on the potentially growth-limitin

143 enozoic had a profound effect on terrestrial biota by creating novel ecological niches.

144 the last approximately 150 y, which affects biota by strengthening and shallowing stratification of

145 Belowground biota can deeply influence plant invasion.

146 Early Cretaceous bird fossils from the Jehol Biota (China), whose identification has previously been

147 s evident in thermal anomalies, hydrothermal biota coexisting with seep fauna, and porewater biogeoch

148 in Earth's history, with most of the visible biota coming to rely on intracellular membrane-bound org

149 ays that exotic plants interacted with novel biota compared with natives.

150 This makes it unlikely that novel island biotas composed of introduced taxa will be able to maint

151 It is the first biota CRM ever available for HCBD.

152 fossil assemblage, here named the Zuun-Arts biota, currently consists of two new species of probable

153 splits between eastern Pacific and Caribbean biota, dated on the assumption of a "universal" mitochon

154 We investigated the potential for soil biota development during the first 3 years, using outdoo

155 ttle is known of the earliest stages of soil biota development of volcanic ash, and how rapidly it ca

156 uld show a different pattern and slower soil biota development.

157 The Ediacaran Weng'an Biota (Doushantuo Formation, 609 Ma old) is a rich micro

158 erns and/or enhanced ecological pressures on biota during this interval of geologic time.

159 preserved fossil scorpion from the Waukesha Biota (early Silurian, ca. 437.5-436.5 Ma) of Wisconsin,

160 pect than previously considered, in terms of biota, ecological interactions and biogeochemical cyclin

161 However, research on this nexus of flow-biota-ecosystem processes is at an early stage.

162 k of understanding of whether and how marine biota emissions affect aerosol-cloud-climate interaction

163 Patterns of diversity within large regional biotas express the outcomes of processes, operating on b

164 the microscopic life that dominated Earth's biota for most of its history left a poor fossil record,

165 The Cambrian Burgess Shale-type biotas form a globally consistent ecosystem, usually dom

166 Understanding how alpine biotas formed in response to historical environmental ch

167 more than 30 million y range of the Ediacara Biota, fossils of these multicellular organisms demonstr

168 vel, are important determinants of [PFAS] in biota from freshwater food webs in the Canadian Arctic.

169 Manipulation studies suggest that biota from more variable marine environments have more p

170 stigating the effects of air contaminants on biota has been limited to date.

171 interpretation of the main components of the biota has been the subject of controversy [2, 3].

172 In fact, the presence of PM(1) in marine biota has never been reported.

173 and time-intensive, modeling its toxicity to biota has received little attention.

174 The Early Cretaceous Chinese Jehol Biota has yielded several such examples, with lizards, b

175 n and distributional dynamics in continental biotas has long been an interest of biogeographers, ecol

176 is now established that communities of soil biota have been substantially altered by direct human ac

177 ractions between aboveground and belowground biota have the potential to modify ecosystem responses t

178 ne flora on Earth and illustrates how modern biotas have been shaped by past geological and climatic

179 Soil biota, hitherto unaccounted for in climate models, inter

180 tive for characterizing pollutant impacts on biota in a controlled, simplified environment.

181 etermined in sediment, water, and freshwater biota in an urban creek in Canada.

182 The significance of PM(1) accumulation by biota in aquatic ecosystems and the potential risk to li

183 ided insight on Hg contamination sources for biota in coastal environment.

184 4) C-age) but dissolved inorganic carbon and biota in coastal waters were young (530 years BP (14) C-

185 ticles may be toxic to a range of organisms, biota in estuarine and coastal waters may be particularl

186 (FBSA), was identified for the first time in biota in homogenate samples of fish by liquid chromatogr

187 s of polychlorinated naphthalenes (PCNs) for biota in polar regions and even fewer reports of tempora

188 hropod from the La Voulte exceptional fossil biota in SE France.

189 ely to exert further negative effects on the biota in spite of the fact that it will likely persist f

190 ery of a deep-water sulfur-cycling microbial biota in the approximately 2.3-Ga Western Australian Tur

191 may interact with climate change impacts on biota in the coming decades.

192 release may have important consequences for biota in these environmental compartments.

193 Defining aspects of the Qingjiang biota include a high abundance of cnidarians, including

194 were dominated by fungi and associated soil biota, including increased arbuscular mycorrhizal fungi

195 iversity of algae, bacteria, fungi and total biota increased.

196 bacterial hopanes suggest that the Ediacara biota inhabited nutrient replete environments with an ab

197 Thus, organisms of the Ediacara biota inhabited nutrient-rich environments akin to those

198 Climate, physical landscapes, and biota interact to generate heterogeneous hydrologic cond

199 ent demonstrations of the role of plant-soil biota interactions have challenged the conventional view

200 ental samples including water, sediment, and biota into bioassays using total extraction or polymer-b

201 Feedback with soil biota is an important determinant of terrestrial plant d

202 The Earth's biota is changing over time in complex ways.

203 The Qingjiang biota is distinguished by pristine carbonaceous preserva

204 A major mechanism that limits MMHg uptake by biota is photodemethylation in surface waters.

205 d variability of the isotopic composition in biota is poorly understood.

206 ations since 2009-2010 suggest that Svalbard biota is still exposed to ocean-transported PFSAs.

207 While the direct physical impact on seabed biota is well understood, no studies have defined thresh

208 wide range of early life stage (ELS) aquatic biota, is a phenomenon by which ultraviolet (UV) radiati

209 as been an ongoing summertime decline of key biota-large diatoms, dinoflagellates and copepods-that t

210 Extraction of chemicals from biota leads to co-extraction of lipids.

211 All biota left comparable biosignatures in the dissolved wea

212 The chemical data are dominated by a strong biota-level signal, indicating that the primary taphonom

213 While PBDEs remain widely detected in biota, levels have declined by nearly half in sport fish

214 PCB concentrations in sediment, biota lipids (Clip) and porewater measured with passive

215 cation (OA) is expected to indirectly impact biota living in contaminated coastal environments by alt

216 mical persistence in environmental media and biota lowers the contribution of dietary ingestion.

217 ow diversity and simple morphology of Miaohe Biota macrofossils.

218 ical climate models, and imply that deep-sea biota may be sensitive to future changes in productivity

219 beyond climate forcing itself, as sensitive biota may have to migrate farther than what is prescribe

220 of global vertebrate, and particularly fish, biotas may commonly lead to widespread, long-term reduct

221 uorooctanesulfonic acid, L-PFOS) compared to biota (mean 149 mug kg(-1) L-PFOS in perch livers) resul

222 lay between physiological needs of different biota, mineral dissolution rates, and substrate nutrient

223 Biota monitoring and risk assessments of sites contamina

224 microplastic pollution poses to soil and its biota necessitates the development of methods to detect

225 r formation explains the non-essentiality in biota of both of these elements.

226 arthropod from the early Cambrian Chengjiang biota of China.

227 osauropteryx from the Early Cretaceous Jehol Biota of Liaoning, China.

228 from the Fezouata biota of Morocco (Early Ordovician epoch, around 478 Ma)

229 specimens from the Early Ordovician Fezouata Biota of Morocco, which not only show well-preserved hea

230 ov., from the Late Ordovician ( 444 Ma) Anji Biota of South China.

231 from the early Cambrian (Stage 3) Chengjiang biota of South China.

232 The benthic biota of the Clarion-Clipperton Zone (CCZ, abyssal easte

233 i is an irreplaceable link to the freshwater biota of the Mesozoic and serves as a reminder of what m

234 se-response behaviour of the drought-adapted biota of these systems, a response that is estimated to

235 ke animal from the early Cambrian Chengjiang Biota of Yunnan Province, China.

236 mism by sampling an entire tropical mountain biota on the 4,095-metre-high Mount Kinabalu in Sabah, E

237 the decrease in diversity of bacteria and of biota overall, functional gene diversity of algae, bacte

238 s caused the least depletion, removing 6% of biota per pass and penetrating the seabed on average dow

239 od webs and poses a health hazard to aquatic biota, piscivorous wildlife and humans.

240 The importance of herbivore-plant and soil biota-plant interactions in terrestrial ecosystems is am

241 (BSAF), Bioaccumulation factor (BAF) and the Biota plastic accumulation factor (BPAF).

242 The microbiota, particularly the intestinal biota, plays a central role in host physiology, and the

243 ed arable land a compositional shift in soil biota, preceded by tightening of the belowground network

244 it remote sensing, and the small size of the biota present.

245 t the effects of microplastics on the marine biota, probably because the pathway for microplastics to

246 radionuclides, seawater, and diverse marine biota provide a unique window through which to examine e

247 Myr-old Dickinsonia and Kimberella (Ediacara biota) provide the most reliable evidence for the emerge

248 105 microplastic effect studies with aquatic biota, provided a systematic overview of their character

249 he effects of aboveground herbivores on soil biota remain challenging to predict.

250 climatic warming will influence the world's biota remains largely speculative, owing to the many way

251 in of the high MeHg concentrations in Arctic biota remains uncertain.

252 The Ediacara biota represents the first complex macroscopic organisms

253 ir tracking in the environment or within the biota requires the development of appropriate labeling t

254 Furthermore, we show that biota respond differently to major El Nino events during

255 ications for our understanding of how extant biota respond to ongoing climate change and are of parti

256 These pulses impacted the marine biota resulting in episodes of anoxia and mass extinctio

257 e lethality of metal-PAH mixtures in aquatic biota revealed that more-than-additive lethality is as c

258 water, sediment, organic matter, and aquatic biota revealed that PFASs were prevalent in all food web

259 model results with monitored POP residues in biota revealed that, on average, all predictions fell wi

260 it natural waters, where it can regulate the biota's exposure to sunlight, surface solar heating, and

261 Across the 147 biota samples (18 taxa) collected, perfluorooctane sulfo

262 rial toward routinely analyzed environmental biota samples and facilitates its use as a quality assur

263 related phenylarsenic compounds from marine biota samples by a liquid chromatography-heated electros

264 tion data for mangrove water, sediments, and biota samples was further utilized to evaluate water-sed

265 presence of CWA related chemicals in marine biota samples.

266 pid-normalized bioaccumulation metrics Clip, Biota sediment accumulation factor (BSAF), Bioaccumulati

267 The biota-sediment accumulation factor of 20,181 and equival

268 Biota-sediment accumulation factors (L-PFOS BSAF(Perch l

269 Island biotas' sensitivity to extinction is well known, but isl

270 Here, biota soil accumulation factors (BSAFs) were assessed in

271 lecebrosa from the early Cambrian Chengjiang biota, Southwest China.

272 artments of the marine environment including biota such as seafood; ingestion from such sources is on

273 nds of mercury (Hg) concentrations in Arctic biota suggest that anthropogenic Hg is not the single do

274 As a palaeoaltimeter, this fossil biota suggests an elevation of ca. 1,000 m.

275 been widely detected in house dust, aquatic biota, surface water, and wastewater environments.

276 out of 48 (in seawater) and 27 out of 37 (in biota) target analytes were detected, the highest concen

277 nia cupana) is a typical product from Amazon biota that exerts antioxidant capacity due to the presen

278 Here, we report a fossil biota that sheds new light on these issues.

279 d, but should have been part of the Ediacara Biota, the earliest preserved macroscopic, complex anima

280 Invasive plants affect soil biota through litter and rhizosphere inputs, but the dir

281 component of exceptionally-preserved fossil biotas throughout the Lower Palaeozoic.

282 ce development, which will alter exposure of biota to environmental agents of disease.

283 We conclude that the strategies used by biota to respond to shifts in environmental heterogeneit

284 derived carbon inputs, contributions of soil biota to SOM storage and effect of dynamic soil structur

285 as a proxy for local adaptation by resident biota, to identify areas where current local climate con

286 derstand how global changes' impacts on soil biota translate into altered ecosystem functioning.

287 ne exceptionally preserved Hirnantian fossil biota was previously known [3, 4]; in particular, almost

288 of PFAA precursors and long chained PFAA in biota were positively correlated to the ratio of carbon

289 Disturbance effects on the soil biota were reduced when plant diversity was high, result

290 ions of earthworms and their associated soil biota were responsible for the maintenance of multifunct

291 ils resemble plant propagules from the Jehol Biota, which belong to Carpolithes multiseminalis.

292 re regulated and how these levels may impact biota, will be important for predicting future responses

293 the Yuba River food web was estimated using biota with a range of %MMHg (the percent of THg present

294 g(II) bound to DOM is a source of mercury to biota with dithiolate Hg(SR)(2) complexes as the immedia

295 opulated by different tropical and temperate biotas with links to India and Southeast Asia, or to Chi

296 ving complex mixture exposure conditions for biota, with implications for interactive effects.

297 Biota within these images were identified to density per

298 is having a major impact on wetlands and its biota worldwide.

299 If this is the case, La Voulte biota would record a combination of multiple palaeoenvir

300 material from the early Cambrian Chengjiang Biota, Yunnan Province, China, including the putative cn