ライフサイエンスコーパス: biota

1 ived episodes of oxia that supported diverse biota.

2 ers are prevalent in seawater, sediments and biota.

3 elps to predict its toxic effects on aquatic biota.

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

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

6 e enough to induce measurable HgT changes in biota.

7 ause function depends on prior conditions or biota.

8 tal heterogeneity relate to the evolution of biota.

9 n the elevated MeHg concentrations in Arctic biota.

10 d regenerating forests, to conserve regional biota.

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

12 duction and accumulation of methylmercury in biota.

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

14 sils of the Precambrian soft-bodied Ediacara Biota.

15 referential loss of heavily calcified marine biota.

16 investigated its consequences for the local biota.

17 onmental contaminants that can accumulate in biota.

18 on in energy budgets for the affected marine biota.

19 cumulate in the Southern Ocean and Antarctic biota.

20 n cost and its collateral toxicity to marine biota.

21 cently detected in air, water, sediment, and biota.

22 of the labile plutonium fraction in aquatic biota.

23 e impacts of microplastics (<1 mm) on marine biota.

24 te and plant fossils that comprise the Jehol Biota.

25 likely causing rapid regional replacement of biota.

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

27 FASs) have recently been described in Arctic biota.

28 ic debris within seawater samples and marine biota.

29 underlain by shared plant responses to soil biota.

30 ics may control the uptake of antibiotics by biota.

31 model for Australia's dry woodland and arid biota.

32 the diversification history of Madagascar's biota.

33 ypical Asian (Laurasia-originated) arthropod biota.

34 cialists, vernal pond inhabitants and stream biota.

35 clides predicts the toxic effects to aquatic biota.

36 ors to threaten aquatic ecosystems and their biota.

37 olds known to cause toxic effects in aquatic biota.

38 esuspension and subsequent interactions with biota.

39 in nature and therefore may not support vent biota.

40 ntal shelf sediments, porewater, and benthic biota.

41 too slowly to be readily observed in living biota.

42 his route as an important source of PBDDs in biota.

43 h simultaneous temporal measures of eDNA and biota.

44 contaminated sediments to high trophic level biota.

45 f temporal trends of PCNs in Canadian Arctic biota.

46 nd negative feedback between plants and soil biota.

47 croplastics, particularly fibers, on aquatic biota.

48 expansion but not population structure in AF biota.

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

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

51 bserved for other Western Hemispheric Arctic biota.

52 of biogeochemical cycles catalysed by extant biota.

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

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

55 e to fossils from the Cambrian Burgess Shale biota.

56 ntrations ever reported for this compound in biota.

57 ate the transfer of plastics to coprophagous biota.

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

59 roduced in a landmark study of a continental biota.

60 acts of changes to pCO2 levels on freshwater biota.

61 following the secondary contact of different biotas.

62 constant ecological challenge to their local biotas.

63 far, making it among the most diverse amber biotas.

64 e effects of temperature increases on stream biotas.

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

66 Here, we report a unique amber biota (50-53 million years ago) from the Lower Eocene of

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

68 om the analysis of HOC profiles implied that biota accumulated HOCs from sediments, porewater, and di

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

70 This is of particular importance for Polar biota adapted to extremes in ecosystem productivity.

71 t and rainfall effects on soil processes and biota affect the performance of exotics and natives in p

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

73 accumulate in the tissues of diverse aquatic biota although factors influencing exposure, such as fee

74 ments and lipid-normalized concentrations in biota and (II) that bioaccumulation does not induce leve

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

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

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

78 Relationships between soil biota and ecosystem processes have mostly been found in

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

80 common osmolyte found in a variety of marine biota and has been detected at nanomolar concentrations

81 occurring radionuclides, to both the marine biota and human fish consumers.

82 th and community structure by modifying soil biota and nutrients.

83 This was done using monitoring data of biota and organic chemicals, mainly pesticides, from fiv

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

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

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

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

88 A new study now reveals a highly diverse biota and provides a wealth of new information on the pa

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

90 ed, whereas HCB was near equilibrium between biota and sediment.

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

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

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

94 e ocean biogeochemical variables over marine biota and their broader implications for people.

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

96 The assembly of regional biotas and organismal responses to anthropogenic climate

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

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

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

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

101 Contamination of water, biota, and soils with various PFASs due to AFFF deployme

102 rosional processes, moisture availability to biota, and water flux to the atmosphere.

103 rom soil onto plant surfaces by wind, water, biota, and/or mechanical disturbances are bioavailable t

104 hreatened components of sympatric freshwater biotas, and so represents a potentially important monito

105 the equilibrium status between sediment and biota; and (iv) site-specific sediment/water distributio

106 among the most celebrated taxa from Cambrian biotas, anomalocaridids (order Radiodonta) have provoked

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

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

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

110 s and extensive exposed rocky surfaces where biota are largely restricted to microbial communities, a

111 Future changes in terrestrial biota are likely to track projected temperature increase

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

113 ors influence the biogeographic structure of biotas are essential for understanding the processes und

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

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

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

117 benefit from enhanced capacity to represent biota as a continuous distribution of traits.

118 in insolation, and self-organisation of the biota as an important separation of timescales.

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

120 s in old ice floes, and changed exposures to biota as the surface meltwater eventually reaches the oc

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

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

123 phylogenetic method that estimates rates of biota assembly for an entire community.

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

125 ed organisms lead to uneven distributions of biota at different depths in the water column.

126 ion and quantitation of SWNT in sediment and biota at environmentally relevant concentrations using N

127 -on the structure of aquatic and terrestrial biota at the community level.

128 ves, a major component of the benthic marine biota, at the 1 degrees grid-cell resolution.

129 tes are an important component of the marine biota, but a large genome with high-copy number (up to 5

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

131 ns were correlated with the lipid content in biota, but not with body size.

132 has been reported for a wide range of marine biota, but uptake into the body by other routes has rece

133 ict significant range contractions in stream biotas, but subsequent biological assessments have rarel

134 s typical of the Cambrian Burgess Shale-type biotas, but the most abundant groups were sponges, algae

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

136 eposition on Adirondack stream chemistry and biota can be mitigated by wetlands have important implic

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

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

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

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

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

142 The Ediacaran Gaojiashan biota displays soft-tissue preservational styles ranging

143 Island biotas emerge from the interplay between colonisation, s

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

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

146 Biota extracts were analyzed by Fourier transform ion cy

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

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

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

150 pid-normalized concentrations for a range of biota from a Swedish background lake.

151 rfaces to interact with corrosive waters and biota from Earth's surface, while simultaneously promoti

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

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

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

155 ctor in the bioaccumulation of Hg in aquatic biota has remained enigmatic.

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

157 but efforts to restore acidified streams and biota have had limited success.

158 graphic and temporal origins of Madagascar's biota have long been in the center of debate.

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

160 Paleogene arthropod biotas have proved important for tracing the faunal turn

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

162 For Australian biota, however, it remains paradigmatic that arid-adapte

163 ions measured in seawater HTO, as well as in biota HTO and OBT, confirm that tritium transfers from H

164 he turnover of tritium between seawater HTO, biota HTO, and OBT was investigated.

165 he functional diversity profiles of the soil biota (i.e., multiple substrate-induced respiration and

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

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

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

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

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

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

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

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

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

175 to concentrations in other low trophic level biota in the Antarctic food web (i.e., krill).

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

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

178 This suggests that Hg trends in biota in the context of a warming Arctic are likely cont

179 e most severe loss of marine and terrestrial biota in the last 542 My.

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

181 bp), a Silurian deposit preserving a marine biota in unusual three-dimensional detail.

182 The Afon Gam Biota includes many lineages typical of the Cambrian Bur

183 ly, very few studies have reported on OPs in biota including wildlife, and essentially there is no in

184 Microplastic interacts with biota, including microorganisms, in these habitats, rais

185 Ingestion of microplastics by marine biota, including mussels, worms, fish, and seabirds, has

186 d (1970-2000) contaminated some local marine biota, including the ringed seal (Pusa hispida).

187 and phyla respectively, from the Chengjiang biota indicates that specimens with eyes mostly belong t

188 We conclude that soil biota influence the abundance of close plant relatives i

189 Relative sediment and biota instrument responses were used to estimate biota-s

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

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

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

193 anations for arthropod rarity; the preserved biota is considered to be an approximation to the origin

194 cal linkages between above- and below-ground biota is critical for deepening our knowledge on the mai

195 Trace metal toxicity to aquatic biota is highly dependent on the metals chemical speciat

196 The 1.88-Ga Gunflint biota is one of the most famous Precambrian microfossil

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

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

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

200 ification of bioaccumulative contaminants in biota is time and cost-intensive and the required extens

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

202 ding toxicity and accumulation in humans and biota led to nationwide phase-outs and state bans.

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

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

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

206 ow diversity and simple morphology of Miaohe Biota macrofossils.

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

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

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

210 to 2.2-Ga "Great Oxidation Event," these two biotas may evidence an opportunistic response to the mid

211 However, concentrations in biota more downstream were higher than expected after ta

212 ems and geographic locations shows that soil biota need to be included in C and N cycling models and

213 ealistic for predicting tritium transfers to biota OBT under nonsteady-state conditions.

214 s will not have adverse effects on arthropod biota of agricultural landscapes.

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

216 aptor yangi, from the Early Cretaceous Jehol Biota of China.

217 lecebrosa from the early Cambrian Chengjiang biota of China.

218 a and tissue residue guidelines that protect biota of high trophic levels under various PCB managemen

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

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

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

222 entrations of metals in water, sediment, and biota of RAS.

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

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

225 rinated biphenyls (PCB) in surface water and biota of the Arctic Ocean.

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

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

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

229 e examined water and sediment chemistry, and biota of two neighboring water bodies with and without a

230 Exceptionally preserved fossil biotas of the Burgess Shale and a handful of other simil

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

232 To gauge the effect of biota on the fate of atmospheric P, we conducted field i

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

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

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

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

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

238 gnal, a radioisotope undetectable in Pacific biota prior to the Fukushima accident in 2011.

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

240 ther events can cause legacy effects in soil biota, promoting exotics and suppressing natives in inva

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

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

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

244 imply that the disappearance of the Ediacara biota represents an abrupt evolutionary event that corre

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

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

247 How did Earth's biota respond to the GOE?

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

249 w temperatures suppress the activity of soil biota, retarding decomposition and nitrogen release, whi

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

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

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

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

254 ethrin were measured in water, sediment, and biota samples in the vicinity of five aquaculture locati

255 presence of CWA related chemicals in marine biota samples.

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

257 Biota sediment accumulation factors (BSAFs) ranged from

258 Biota-sediment accumulation factors (BSAFs) were greater

259 tials than Dec604 and DP based on calculated biota-sediment accumulation factors (BSAFs).

260 a instrument responses were used to estimate biota-sediment accumulation factors (BSAFs).

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

262 of insolation relative to adaptation of the biota shows a sharp transition between regulating, and l

263 et-weight (ww) and organic carbon (OC)-based biota soil accumulation factors (BSAFs) for the earthwor

264 luctuations in precipitation may affect soil biota, soil processes, and the proportion of exotics in

265 The biota-soil accumulation factor (BSAF) values for unamend

266 Biota-soil accumulation factors (BSAFs) for worms expose

267 Penta-BDE biota-soil accumulation factors (BSAFs) ranged from 0.00

268 locaridid from the early Cambrian Chengjiang biota, southwest China, nearly complete specimens of whi

269 ailability of divalent metals toward aquatic biota successfully.

270 in the evolution of the Earth's contemporary biota, such as the rise of grass-dominated biomes during

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

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

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

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

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

276 quent reactions are also found in Baltic Sea biota, the results support the theory that PBDDs are for

277 rbon supply meets the demand of water-column biota; the discrepancy between known carbon sources and

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

279 diversity by the ability of the species-rich biota to display high functional redundancy: i.e., a hig

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

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

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

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

284 cted a data set on the effects of three soil biota treatments on plant growth: net whole-soil feedbac

285 eline composition and dynamics of modern-day biota under pre-Industrial conditions, where insights in

286 Freshwater and terrestrial fossils of the biota usually occur together within some horizons and ha

287 er individual contaminants will partition to biota via direct uptake or through sorption to DOC, whic

288 oxins/furans (PCDD/Fs) to resident/migratory biota was investigated in 11 finfish species and blue cr

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

290 determine uptake of vanadium species in the biota, we exposed the benthic invertebrate Hyalella azte

291 Doses to marine biota were about two orders of magnitude below the lowes

292 Biota were assigned to three trophic levels based on the

293 of the ecosystems (aqueous phase, sediments, biota) when assessing the impacts of CeO2 NPs in aquatic

294 ntrast with previous studies of the Hawaiian biota, which have suggested that most lineages colonized

295 Subsequent PFAM exposure to biota will likely lead to enzymatic hydrolysis of the am

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

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

298 ces the diversity and abundance of many soil biota, with consequences for the processes that they gov

299 he distribution and abundance of the world's biota, with significant consequences for biological dive

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