ライフサイエンスコーパス: benthic

1 re transported from afar or perhaps were not benthic.

2 on and locomotion is probably central to its benthic adaptation.

3 ival bottlenecks, in part due to competitive benthic algae interactions should be addressed, to impro

4 wn to 30 cm and observed that the planktonic/benthic amplicon ratio changed with depth.

5 Away from benthic and aeolian sources, iron reaches phytoplankton

6 Benthic and fast-flowing water adapted species with hydr

7 Eels collected this far into rivers are benthic and fully adapted to freshwater; that is, they a

8 and the variation in community structure of benthic and hyporheic communities by deploying two stand

9 odel that explains adaptation to contrasting benthic and limnetic feeding niches [5] also predicted F

10 Stickleback consume benthic and limnetic invertebrates, focusing on the form

11 g arenas in which females had access to both benthic and limnetic males, we found that F2 females mat

12 ic model of ecological speciation: sympatric benthic and limnetic threespine stickleback (Gasterosteu

13 Our ability to preserve both benthic and pelagic deep-sea ecosystems depends upon eff

14 ting light, with a strong difference between benthic and pelagic ecosystems.

15 nsiders dynamic interregional differences in benthic and pelagic energy pathways connecting phytoplan

16 The bubble-mediated link between the benthic and pelagic environment was further supported by

17 copepods), indicating a changing balance of benthic and pelagic fauna.

18 is related to the major differences between benthic and pelagic habitats in the deep ocean.

19 ifferent fixed and mobile platforms of those benthic and pelagic monitoring networks, proposing at th

20 s) are apex predators that primarily consume benthic and pelagic-feeding ice-associated seals.

21 ors of MMHg bioaccumulation near the base of benthic and planktonic food chains.

22 n the eastern equatorial Pacific (EEP) using benthic and planktonic foraminiferal (14)C.

23 ation of hydrophobic organic contaminants by benthic and sessile invertebrates.

24 among the terrestrial, floodplain, riparian, benthic and transitional ecosystems with which they conn

25 surface streambed sediment (hyporheic zone), benthic, and water column zones in controlling [Formula:

26 It is a puzzling paradox that fossils of benthic animals are often found in black shales with geo

27 his study provides a preliminary analysis of benthic Antarctic Peninsula meiofauna using high through

28 nicotinoid exposure experienced by nontarget benthic aquatic invertebrates as well as potential means

29 e describe the first ever experiment to warm benthic assemblages to ecologically relevant levels in s

30 tobenthos, and the structure of invertebrate benthic assemblages would be influenced by microplastics

31 generated organic wastes and their effect on benthic bacterial biomass.

32 tan area, and revealed a hotspot of deep-sea benthic biodiversity of sessile fauna at ca. 400 m depth

33 Benthic biofilms are vulnerable to glacial retreat induc

34 Benthic biofilms in glacier-fed streams harbor diverse m

35 To investigate microbial functions of benthic biofilms in glacier-fed streams, we predicted me

36 We studied the benthic biofilms in streams flowing through forest (upst

37 and organic carbon in both stream water and benthic biofilms, which are closely related to the diffe

38 land use are often first observed in stream benthic biofilms.

39 ree-dimensional network burrows implies that benthic biogeochemical cycling could have been maintaine

40 Here we force a size-resolved benthic biomass model, BORIS, using seafloor POC flux fr

41 MO-MEDUSA, to investigate global patterns in benthic biomass.

42 n of all sediment-associated contaminants to benthic biota are still underrepresented in water qualit

43 The benthic biota of the Clarion-Clipperton Zone (CCZ, abyss

44 nts to investigate ecotoxicological risks to benthic biota.

45 lation have suggested that turbulence in the benthic boundary layer is important for aggregate format

46 ity water column data exhibit both basal and benthic boundary layers, along with evidence of tidally

47 Rhodoliths are benthic calcium carbonate nodules accreted by crustose c

48 Stocks of immobilized benthic carbon averaged nearly 15 g m(-2) .

49 Mortality and persistence of growth, as benthic carbon immobilization, were mainly influenced by

50 Five-year recovery time doubled benthic carbon stocks.

51 Benthic chamber incubations indicated dissolution fluxes

52 ar the exposed explosive surface, as well as benthic chamber incubations.

53 Critical benthic communities (corals, seagrasses) can be partiall

54 nas are invariably low diversity, especially benthic communities [2], but ecological structure was re

55 ceiving acid mine drainage, degrading stream benthic communities by smothering of habitat, primary pr

56 lization with depth, results show that while benthic communities in shallow seas generally show highe

57 Deep-water benthic communities in the ocean are almost wholly depen

58 However, the dominant factor for modelled benthic communities is the integrated magnitude of POC r

59 fication are then applied to investigate how benthic communities may change under different future co

60 e a realistic and relevant indication of how benthic communities may change under future ocean warmin

61 een on this small spatial scale suggest that benthic communities of this area support a diverse array

62 are one of the key structure-forming taxa in benthic communities on the Antarctic continental shelf.

63 ally realistic exposure conditions to native benthic communities that have complex structural and fun

64 nking particles control the pace of deep-sea benthic communities that live a feast-or-famine existenc

65 osms were used to expose naturally colonized benthic communities to a gradient of ferric Fe (0-15 mg/

66 We exposed field colonized benthic communities to aqueous metals in a series of mes

67 ess in the general structuring of coral reef benthic communities.

68 Globally gridded satellite and benthic community area data are used to estimate communi

69 In the benthic community experiment, larval and emerging adult

70 nt with the mayfly Rhithrogena robusta and a benthic community experiment.

71 However, there was a post-bleaching shift in benthic community structure around islands with seabirds

72 of these significant specific responses, the benthic community structure, biomass and abundance at th

73 elations between pesticides and 6 metrics of benthic community structure.

74 To address this, benthic community surveys were done in kelp forests and

75 estrial nutrients were incorporated into the benthic community, we collected macroalgae over 10 days

76 ribution of species' functional diversity to benthic-community dynamics.

77 t as in the Gulf of Oman, despite comparable benthic composition and live coral cover.

78 seabed impacts and (ii) by removing overall benthic consumer biomass increasing the net availability

79 , trawling affected primarily the biomass of benthic consumers, lowering competition.

80 the marine heatwave of 2015 show a change in benthic cover mainly in the southern reefs, where there

81 Spatial and temporal patterns in benthic cover suggest growing resistance to bleaching-le

82 each 10-20 m(2) in area) and then monitored benthic cover, coral recruitment, and fish community str

83 from 11 morphologically distinct species of benthic ctenophores from the Red Sea and Sulu Sea, and t

84 Coeloplanidae, the largest family of benthic ctenophores, comprises 33 species, all described

85 erns of P. paru and S. iseri, and found that benthic cyanobacterial mats comprised 36.7% +/- 5.8% and

86 previously undocumented, top-down control on benthic cyanobacterial mats on Caribbean reefs.

87 tic Blue Tang (Acanthurus coeruleus) consume benthic cyanobacterial mats on coral reefs in Bonaire, N

88 vidence of its ability to control coral reef benthic cyanobacterial mats, which have recently prolife

89 We combined benthic data collected pre- (2014) and post-bleaching (2

90 ided with a similar transition in the marine benthic delta(18)O record for global ice volume and deep

91 ction of nitrous oxide, which is consumed by benthic denitrifying bacteria before it reaches the wate

92 ry producers through the remineralization of benthic-derived organic matter.

93 ertebrates (crabs, shrimps, benthic grazers, benthic detritivores, bivalves), and strong indirect eff

94 Benthic diatoms are the main primary producers in shallo

95 ith bacteria are strongly conserved in other benthic diatoms while many species-specific genes are st

96 the genetic diversity and gene functions in benthic diatoms.

97 Dive duration, depth, bottom time, and benthic diving increased over the first 40 days.

98 le, yet most studies use pelagic rather than benthic-dwelling organisms.

99 Our results underscore the importance for benthic ecology of reducing uncertainty in the magnitude

100 followed by a several million-year delay in benthic ecosystem recovery.

101 e encrusting communities play vital roles in benthic ecosystems and have major economic implications

102 st pristine locations on earth, the deep-sea benthic ecosystems of the archipelago are virtually unex

103 rld, creating the foundation for the complex benthic ecosystems that have sustained Metazoa from the

104 In benthic ecosystems, only a few censuses have been done,

105 pact seafloor morphology and composition and benthic ecosystems.

106 at can promote the recruitment of animals to benthic ecosystems.

107 at ecosystem-level variations in pelagic and benthic energy flows from phytoplankton to fish, trophic

108 littered the site and structured the suboxic benthic environment.

109 ents in isolated refugia, and diversified in benthic environments that became increasingly available

110 ography of coastal and deep-sea, pelagic and benthic environments, and show how land-barriers, salini

111 o which consumers feed on prey in pelagic or benthic environments.

112 vertebrates live as surface encrustations in benthic environments.

113 ystems, particularly those within in coastal benthic environments.

114 are becoming central approaches for studying benthic fauna (e.g., quantifying species presence, behav

115 eeper, and the habitat suitable for fish and benthic fauna had expanded (D).

116 ygen isotope data from calcite shells of the benthic fauna suggest that bottom water temperatures in

117 nomic and trait-based community structure of benthic fauna.

118 ea floor that are degraded by a species-rich benthic fauna.

119 Using two large UK marine benthic faunal datasets, we present a spatially gridded

120 We measured jaw kinematics during benthic feeding and cranial musculoskeletal morphologies

121 n important predicted loss mechanism for the benthic-feeding fish.

122 Sponges are benthic filter feeders that play pivotal roles in coupli

123 n early-Cambrian lineage superbly adapted to benthic filter feeding.

124 t multiple trophic levels, including shallow benthic filter-feeding communities, as the coupling betw

125 nd polyfluoroalkyl substances (PFASs) in the benthic fish white sucker (Catostomus commersonii) and s

126 able to maintain connectivity of these small benthic fishes if habitat in between them is extirpated.

127 Despite the increases in littoral-benthic food resources, trout did not utilize littoral h

128 at bottomfish relied, at least in part, on a benthic food web and identified the incorporation of dee

129 TMFs were almost consistently >1 in the benthic food web as well as when considering all data po

130 pusillus doriferus, AUFS) is a predominantly benthic forager on the shallow continental shelf of Bass

131 mical compositions of foraminifer shells and benthic foraminifer assemblages in marine sediments indi

132 ellina labradorica, a common kleptoplastidic benthic foraminifer from Arctic and North Atlantic subli

133 stronomically dated, continuous composite of benthic foraminifer isotope records developed in our lab

134 rification and O(2) respiration rates for 10 benthic foraminifer species sampled in the Peruvian oxyg

135 cycle -associated bacteria inside intertidal benthic foraminifera (Ammonia sp. (T6), Haynesina sp. (S

136 xide (SiO(2)), on a microbial eukaryote (the benthic foraminifera Ammonia parkinsoniana) using multip

137 that bacterivory is an unlikely scenario, as benthic foraminifera are known to digest bacteria only r

138 Benthic foraminifera are known to play an important role

139 ronmental impact of marine aquaculture using benthic foraminifera eDNA, a group of unicellular eukary

140 Benthic foraminifera populate a diverse range of marine

141 Here, we study growth and calcification in benthic foraminifera that inhabit a thermally polluted c

142 ikely due to the presence of DNA from living benthic foraminifera.

143 en and carbon isotope variations in deep-sea benthic foraminifera.

144 d by marine records, including delta(18)O of benthic foraminiferal calcite (delta(18)Oc).

145 correlation between delta(34)S and the bulk benthic foraminiferal delta(13)C supports this interpret

146 This study highlights the potential of the benthic foraminiferal delta(34)S as a novel tool to reco

147 Here, we show that the benthic foraminiferal delta(34)S can be used to reconstr

148 Our results show lower benthic foraminiferal delta(34)S values (~20 per mille)

149 Benthic forms with a frondose gross morphology, assigned

150 ith convergent phenotypes, where deep-bodied benthic forms with truncate caudal fins repeatedly evolv

151 slender-bodied pelagic forms and deep-bodied benthic forms.

152 patterns of colonization and succession in a benthic fouling community.

153 wn to be effective on field samples from two benthic freshwater fish species, revealing a microplasti

154 on epibenthic invertebrates (crabs, shrimps, benthic grazers, benthic detritivores, bivalves), and st

155 pe values (delta(18)O and delta(13)C) in the benthic green alga, Halimeda tuna.

156 Encrusting benthic growth was mainly determined by microalgal bloom

157 st all of the meiofaunal biodiversity in the benthic habitat has yet to be characterised, levels of b

158 onditions created a "resource-rich" littoral-benthic habitat with increases in zoobenthic production

159 nt changes in the amount of available marine benthic habitat.

160 aximise the extent of light-dependent marine benthic habitats across decadal timescales.

161 he evolution of early animals by structuring benthic habitats and providing novel niches.

162 ion resulting from the smothering of natural benthic habitats and reef complexes with sediment.

163 Strong currents are a key component of benthic habitats by supplying food and nutrients to filt

164 astal fishes, drawing larvae towards shallow benthic habitats or inducing settlement.

165 l emergence of mayfly swarms from freshwater benthic habitats, but their characterization at macrosca

166 ce on the creation and destruction of marine benthic habitats, has not been explored.

167 and megafauna) living in deep waters and in benthic habitats, whereas monitoring of ecosystem functi

168 ivotal to understand its effects on deep-sea benthic habitats.

169 h are probably central for its adaptation to benthic habitats.

170 influence the distribution and abundance of benthic harmful dinoflagellate (BHAB) species.

171 potential results from production within the benthic-hyporheic zone, and the lower [Formula: see text

172 he ostracode Krithe and sea-ice planktic and benthic indicator species, we suggest that the Mid-Brunh

173 phic position was also associated with lower benthic invertebrate availability.

174 irst systematic characterization of deep-sea benthic invertebrate communities of the Galapagos, acros

175 This characterization of Galapagos deep-sea benthic invertebrate megafauna across a range of ecosyst

176 Specimens of five benthic invertebrate species were collected at two disti

177 and fertilization of a representative marine benthic invertebrate, the red abalone Haliotis rufescens

178 g coastal systems by reducing populations of benthic invertebrates and releasing kelp forests from gr

179 lation reduction) and adverse effects on the benthic invertebrates Chironomus riparius and Lumbriculu

180 oducers, but the contribution of macrofauna (benthic invertebrates larger than 1 mm) inhabiting them

181 s a class were the most potentially toxic to benthic invertebrates, and of the 9 pyrethroids detected

182 For many benthic invertebrates, larval settlement occurs in respo

183 For many marine benthic invertebrates, migration happens during reproduc

184 and sampled communities of aquatic fungi and benthic invertebrates.

185 environment, where sponges may dominate the benthic landscape.

186 able DOM, creating organic-rich habitats for benthic life.

187 t also predicted female morphology along the benthic-limnetic trait axis.

188 s vary asymmetrically between habitats, with benthic lineages diversifying faster and colonizing midw

189 ncursions into the water column by ancestral benthic lineages in all major oceanic basins.

190 nus) and brown trout (Salmo trutta) when the benthic link was included than in the pelagic-only model

191 sorting and morphological identification of benthic macro-invertebrates, which is time-consuming and

192 study we produce a standardised dataset for benthic macrofauna and sediments through integration of

193 ers of OG extraction, and the composition of benthic macroinvertebrate and microbial communities.

194 le OG geochemical tracers, and microbial and benthic macroinvertebrate communities.

195 eake Basin-wide Index of Biotic Integrity, a benthic macroinvertebrate multimetric index, was used to

196 evelopment, shale OG geochemical tracers, or benthic macroinvertebrate or microbial community composi

197 [SigmaREE] in fish, benthic macroinvertebrates, and zooplankton declined as

198 adjustment increases dispersal potential in benthic marine animals.

199 habitats and ecosystem services developed by benthic marine calcifiers inhabiting that depth-range, s

200 Here, we examine the shallow benthic marine communities preserved in the late Cretace

201 ty, C. digermulense was a complex and likely benthic marine eukaryote exhibiting cellular differentia

202 tat (beta), and overall (gamma) diversity of benthic marine invertebrates for Phanerozoic geological

203 Settlement of many benthic marine invertebrates is stimulated by bacterial

204 vity level for survival of well-skeletonized benthic marine invertebrates over a 100-million-year-lon

205 in eliciting settlement and metamorphosis of benthic marine larvae.

206 ility of new settlers and their origins in a benthic marine organism with one of the longest pelagic

207 The growth rates and ages of many benthic marine organisms are poorly understood, complica

208 pulations leads to a better understanding of benthic marine population dynamics, especially in commer

209 ic larvae is critical for the persistence of benthic marine populations.

210 published experimental data for 41 tropical benthic marine species using methods adapted from water

211 ority of sedentary marine species are pelago-benthic, meaning the pelagic larval stages disperse usin

212 atodes, one of the most abundant taxa of the benthic meiofauna.

213 entially created a stressful environment for benthic metazoan communities.

214 ighly oxygenated niches for the evolution of benthic metazoans.

215 r results indicate that macrofauna increases benthic methane efflux by a factor of up to eight, poten

216 rbivore density and nutrient availability on benthic microalgae (diversity, abundance and biomass) an

217 y on the abundance, biomass and diversity of benthic microalgae.

218 seasonal changes in the interactions between benthic microbial assemblies and the bloom forming cyano

219 more detail as this is fundamental to marine benthic microbial communities and because recently excit

220 Perennially ice-covered lakes that host benthic microbial ecosystems are present in many regions

221 Benthic microeukaryotes are key ecosystem drivers in mar

222 omposition and geographical distributions of benthic microeukaryotes using high-throughput sequencing

223 The distributions of benthic microorganisms in the Gulf can be constrained, a

224 Benthic microorganisms transported into the water column

225 Here, benthic, midstream sediments of two undammed, open-flowi

226 pparent earlier extinction primarily affects benthic mollusks, while the boundary extinction primaril

227 e used to build robust predictive models for benthic monitoring, regardless of the taxonomic assignme

228 ding) represents a promising alternative for benthic monitoring.

229 hich have conventionally been interpreted as benthic mud-grubbers with poor swimming capabilities and

230 , we observed at least four thick (70-140 m) benthic nepheloid layers (BNLs) at water depths between

231 nia monooxygenase (amoA) gene abundances and benthic nitrification potential rates (NPR) in low-salin

232 gen (O(2))-makes them important mediators of benthic nitrogen cycling.

233 associated with leaf litter, wood, and fine benthic organic matter (FBOM) across seasonal temperatur

234 To answer these questions, we surveyed benthic organisms and fishes around islands with seabird

235 e is known about their ecological effects on benthic organisms and functions.

236 mangroves and seagrasses are in decline and benthic organisms are close to their physiological limit

237 Benthic organisms had relatively high SigmaPFASs compare

238 Benthic organisms may be exposed to polycyclic aromatic

239 t attention although their effects on marine benthic organisms such as foraminifera are still largely

240 In this study, samples of Antarctic marine benthic organisms were analyzed for legacy and emerging

241 at between 30-41% of the individual observed benthic organisms were categorized as capable of emittin

242 tential of photoinduced toxicity to occur in benthic organisms with free-swimming early life stages.

243 e parasitism, suppressed fecundity of common benthic organisms, and negative impacts on marine ecosys

244 ortant source of demographic information for benthic organisms, provided that certain assumptions abo

245 ic invertebrates, including both pelagic and benthic organisms.

246 g positive correlations to dietary intake of benthic organisms.

247 ere they may pose an environmental threat to benthic organisms.

248 ailability and, ultimately, toxic effects in benthic organisms.

249 ion can cause the loss of up to 67% of gross benthic oxygen production.

250 arisons of relative modal use of pelagic and benthic pathways revealed similar ranking of species dep

251 ess the relative contribution of pelagic and benthic pathways to fish consumer production.

252 od to define consumers' links to pelagic and benthic pathways, our results demonstrate that a substan

253 mately 70% and 30% of biomass to pelagic and benthic pathways, respectively.

254 ological and functional phenotypes along the benthic-pelagic axis are pervasive among different linea

255 feeders that play pivotal roles in coupling benthic-pelagic processes in the oceans that involve tra

256 elevated trophic transfer efficiencies with benthic-predominant systems.

257 enthivorous demersal species by (i) changing benthic prey composition through physical seabed impacts

258 r biomass increasing the net availability of benthic prey for remaining individuals.

259 a, intense trawling had a negative effect on benthic prey.

260 functions (decomposition of organic matter, benthic primary production) by acting in the opposite di

261 eferences for, and dependence on, pelagic or benthic production are governed by the availability of t

262 But they do not discriminate benthic production directly supported by phytoplankton f

263 ion directly supported by phytoplankton from benthic production recycled through detrital pathways.

264 ld have increasing ecological impacts in the benthic region over long time frames.

265 The decreased reliance on littoral-benthic resources during earlier ice break-up caused red

266 omparable picture of the adult population to benthic sampling methods and may include species richnes

267 We sampled benthic sediment from 34 stations along the Thames River

268 the spatial distribution of microplastics in benthic sediment from Lake Michigan and Lake Erie and va

269 riments involved the controlled formation of benthic sediment plumes and measurement of the plume sed

270 s highlight that the extent of dispersion of benthic sediment plumes, resulting from mining operation

271 unt when evaluating the impact and extent of benthic sediment plumes.

272 antities are among the highest recorded from benthic sediments.

273 antiquus new species and are interpreted as benthic siphonocladalean chlorophytes, suggesting that c

274 ssels (Mytilus edulis) collected at a nearby benthic site.

275 erodontus portusjacksoni, a shallow-dwelling benthic species and generalist predator endemic to the t

276 for use in species distribution modeling of benthic species and habitats.

277 Here we show that exposure of the model benthic species Chironomus riparius to lithium cobalt ox

278 ng the diversity and spatial distribution of benthic species is fundamental to properly assess the im

279 suggest they exert evolutionary pressure on benthic species, thereby selecting for elevated exploita

280 )O) in combination with a recently published benthic stable carbon isotope (delta(13)C) record from t

281 s such as collection of scientific data from benthic stations, ocean geology, and remote control of o

282 abatis gen. nov. is deeply nested within the benthic stingrays (Dasyatoidea) representing the sister

283 w hitherto unknown body plan experimented by benthic stingrays, whose evolution can be possibly linke

284 free-living, particle-associated, biofilm on benthic stones and rocks, and sediment).

285 t surveys were performed to characterize the benthic substrates present at each sampling site.

286 ropogenic stressors on carbon fluxes in soft benthic systems remain largely unknown.

287 Pelagic and benthic systems usually interact, but their dynamics and

288 During the summer, benthic temperatures show high-frequency fluctuations (2

289 exerts tangible influence on specific macro-benthic tracemaker communities in contourite deposits.

290 differential responses to the post-bleaching benthic trajectories, suggesting that projections for re

291 through the mucous nets of both pelagic and benthic tunicates.

292 eic-benthic zone in headwater streams to the benthic-water column zone in rivers.

293 potential reflects the production within the benthic-water column zone.

294 servations, TMFs determined in the estuarine benthic web were found to significantly decrease with in

295 iated breakdown) and has been limited to the benthic zone (BZ).

296 eds to understand limbless locomotion in the benthic zone found at the bottom of lakes and oceans.

297 The benthic zone in estuarine systems is the most probable l

298 and river size and shifts from the hyporheic-benthic zone in headwater streams to the benthic-water c

299 5 cm of sediment deposited over a 1.28 km(2) benthic zone.

300 a proximate measure of eDNA removal into the benthic zone.