ライフサイエンスコーパス: benthic

1 Huron) of their whole-lake production may be benthic.

2 ve as an analog for studying CO2 leakage and benthic accumulations from subsea carbon capture and sto

3 Benthic accumulations of filamentous, mat-forming bacter

4 to the reef, metamorphosing and entering the benthic adult population.

5 pecies of probable macroscopic multicellular benthic algae.

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

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

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

9 These traits diverge in parallel between benthic and limnetic species in the repeated adaptive ra

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

11 re we use highly variable male F2 hybrids of benthic and limnetic threespine sticklebacks, Gasteroste

12 m that smaller sunfish feed predominantly on benthic and on coastal pelagic species, whereas larger f

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

14 Benthic and pelagic resource availability varied between

15 Long-term declines of both benthic and pelagic species underscore the urgency of st

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

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

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

19 oxidative-weathering reactions occurring in benthic and soil environments at profound redox disequil

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

21 ds, as is seen in modern oxygen minimum zone benthic animal communities.

22 Pelagic animals were victimized more than benthic animals during previous mass extinctions but are

23 which are richly, but patchily, colonised by benthic animals.

24 ons in surface ocean O2 levels and pervasive benthic anoxia are expected in a world with much lower a

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

26 nvestigations of the biogeochemical roles of benthic Archaea in marine sediments are hampered by the

27 enomic content of four widespread uncultured benthic Archaea recovered from estuary sediments at 48%

28 ture of coral reef ecosystems is the complex benthic architecture which supports diverse and abundant

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 tion-oxidation (redox) regime in structuring benthic bacterial communities, having direct implication

33 e that graze on filamentous sulfur-oxidizing benthic bacterial mats (Alia permodesta).

34 tat, this could ultimately lead to a drop in benthic biodiversity.

35 er Viviparus viviparus significantly reduced benthic biofilm biomass and enhanced hydraulic conductiv

36 iparus (Linnaeus, 1758)) treatments to limit benthic biofilm biomass and to maintain or even increase

37 In freshwater ecosystems, benthic biofilms (i.e. thin films of algae, bacteria, fu

38 Benthic biofilms are vulnerable to glacial retreat induc

39 Benthic biofilms in glacier-fed streams harbor diverse m

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

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

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

43 community structure and functions of stream benthic biofilms.

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

45 The ABYSSLINE Project is conducting benthic biological baseline surveys for the UK Seabed Re

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

47 ease in future (2091-2100) global open ocean benthic biomass under RCP8.5 (reduction of 5.2 Mt C) com

48 pecies typically constitute approximately 3% benthic biomass) suggests an increased drawdown of appro

49 models linking water depth to POM supply or benthic biomass.

50 mpirical relationships to predict changes in benthic biomass.

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

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

53 relative expression level of the freshwater benthic Bmp6 allele at late, but not early, stages of st

54 us capture of microbial communities from the benthic boundary layer concurrent with imaging provides

55 arbon and total nitrogen, sedimentology, and benthic boundary layer turbidity, all appear to be consi

56 Rhodoliths are benthic calcium carbonate nodules accreted by crustose c

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

58 We compared benthic carbon immobilization across major regions aroun

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

60 Five-year recovery time doubled benthic carbon stocks.

61 orooctanesulfonate (PFOS) dominated in char, benthic chironomids (their main prey), and sediments, wh

62 ommon ancestor of bilaterians was probably a benthic, ciliated acoelomate worm with a single opening

63 ted CO2, provides direct evidence of shallow benthic CO2 accumulations originating from sub-seafloor

64 Crown groups of modern terrestrial and/or benthic coastal cyanobacteria appeared during the late P

65 Analysis of two decades of benthic collections showed strong increases in annual pr

66 We detected minimal impacts to benthic communities (<225 m linear distance from the eff

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

68 e major habitat-forming organisms in coastal benthic communities and have an ancient origin in evolut

69 echanisms responsible for biochar effects on benthic communities and to identify the optimal applicat

70 rgy in methane to products that sustain rich benthic communities around the gas leaks.

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

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

73 Nonetheless, benthic communities in this region remain poorly known.

74 The reason for the reduction in the benthic communities is currently unknown, and therefore,

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

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

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

78 In benthic communities of osmotrophs of sufficient density,

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

80 When benthic communities were simultaneously exposed to bioch

81 rawn some concern due to possible impacts on benthic communities.

82 altered the structure and function of stream benthic communities.

83 lumn, which results in increased exposure of benthic communities.

84 Variation in benthic community response between sampling locations wa

85 d and there were marked changes in coral and benthic community structure during the first decade of m

86 At shallower reef crest sites (3-4 m), benthic community structure recovered towards pre-distur

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

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

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

90 Benthic contributions to ecosystem PP are rarely measure

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

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

93 stics, and porewater ammonium and biomass of benthic cyanobacteria decreased.

94 viral origin) influences the functioning of benthic deep-sea ecosystems remains completely unknown.

95 In benthic deep-sea ecosystems, which represent the largest

96 viromes and viral metagenomes from different benthic deep-sea ecosystems.

97 a wider view of viral taxonomic diversity in benthic deep-sea ecosystems.

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

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

100 esulting in lower toxin concentrations among benthic detritivores.

101 ar average plastic responses to species with benthic development.

102 We show that benthic diatoms selectively perceive and behaviourally r

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

104 The estimated benthic DOC flux from the methane venting sites (8.6 x 1

105 may be physical effects of the substance on benthic dwelling organisms at environmentally relevant c

106 e-dominated, suggesting a regional change in benthic ecology during the early stages of the GOBE.

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

108 ine algae are a significant component of the benthic ecosystem.

109 gating the taxonomic diversity of viruses in benthic ecosystems in order to improve our comprehension

110 nesis that will advance our understanding of benthic ecosystems on the early Earth.

111 ms, which has clear implications for coastal benthic ecosystems suffering chronic metal pollution as

112 t new insights into micro-scale processes in benthic ecosystems that shape observed patterns at much

113 , potentially leading to sustained impact on benthic ecosystems.

114 for the evaluation of the quality of marine benthic ecosystems.

115 f CO2 at this site may preferentially impact benthic ecosystems.

116 have a significant impact on the P cycle in benthic ecosystems.

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

118 obial-mediated remineralisation processes in benthic environments - and associated levels of sediment

119 0 Mya and likely dominated microbial mats in benthic environments for most of the Proterozoic (2,500-

120 tion lutjanids that foraged in deeper water, benthic environments generally had higher Hg levels.

121 re among the larger megafauna inhabiting the benthic environments of all oceans, commonly in water de

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

123 s of large (0.1 to 2 m height) multicellular benthic eukaryotes.

124 ost likely associated with the occurrence of benthic fauna burrows and seagrass roots.

125 Radiocesium concentrations in some benthic fauna declined more slowly than in pelagic fish

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

127 luit (population 6699), which were devoid of benthic fauna up to 580 m from the effluent source in re

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

129 nction levels during significant pelagic and benthic faunal recovery.

130 on was an important source of Hg for shallow benthic feeders, while deepwater sources of mercury may

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

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

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

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

135 ry marked by a dramatic metamorphosis from a benthic filter-feeding ammocoete larvae into a parasitic

136 We tested the hypothesis that benthic fish remained more contaminated due to the bioav

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

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

139 Benthic fluxes of DOC from these sediments were 28 to 12

140 and models of biogeochemical reaction rates, benthic fluxes, and in-sediment nutrient and oxygen conc

141 ssues in the context of early diagenesis and benthic fluxes.

142 and carbon, with isotopic values suggesting benthic food sources for shallow nearshore species.

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

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

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

146 ide, as indicated by the chemical tracers of benthic foraminifer delta(13)C and foraminifer/coral (14

147 ure-corrected delta(18)O measurements on the benthic foraminifer Uvigerina spp. from deep and interme

148 A decrease in (18)O/(16)O values of benthic foraminifera accompanying the most severe deoxyg

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

150 An evolutionarily conservative group, benthic foraminifera often comprise >50% of eukaryote bi

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

152 mmonites, bivalves, and gastropods, abundant benthic foraminifera, and rare planktonic foraminifera.

153 We use benthic foraminiferal B/Ca ratios to reconstruct relativ

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

155 iatomaceous laminations and hypoxia-tolerant benthic foraminiferal species, peaks in redox-sensitive

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

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

158 Here we show that a derived benthic freshwater stickleback population has evolved an

159 e dietary uptake of Cu were evaluated in the benthic grazer Lymnaea stagnalis following 4-5 h exposur

160 trate in periphyton and thus be available to benthic grazers is less well characterized.

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

162 eriphyton and subsequent trophic transfer to benthic grazers.

163 e, resulting in proliferation of filamentous benthic green algae (Cladophora glomerata).

164 Encrusting benthic growth was mainly determined by microalgal bloom

165 Encrusting benthic growth was mainly determined by microalgal bloom

166 odular, self-similar branching and a sessile benthic habit.

167 d algal production and shrunk the oxygenated benthic habitat by 38% in our study areas, yielding fish

168 nktonic larval stages, and low dependence on benthic habitat for food or shelter during their life hi

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

170 meras to provide clear imagery of the ponds' benthic habitat.

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

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

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

174 y for microplastics from the water to marine benthic herbivores.

175 Model results also suggested that benthic Hg methylation was an important source of Hg for

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

177 s responses in growth, mortality and mass of benthic immobilized carbon.

178 Effluent quality and benthic impacts were monitored in the receiving water of

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

180 acts of ongoing DSTP and assess the state of benthic infaunal communities after its conclusion.

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

182 ems and the impact of wastewater effluent on benthic invertebrate communities in arctic receiving wat

183 ecosystem structure and functioning, halving benthic invertebrate densities and increasing decomposit

184 changes in the distribution of 65 North Sea benthic invertebrate species between 1986 and 2000 by ex

185 o assess the bioavailability and toxicity to benthic invertebrates (bivalve survival and amphipod sur

186 Benthic invertebrates Crayfish (Orcoescties spp.) had la

187 ounds in water, sediment, juvenile char, and benthic invertebrates from lakes in the high Arctic.

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

189 s increased in the whole North Sea with many benthic invertebrates showing north-westerly range shift

190 nded to feed less on zooplankton and more on benthic invertebrates than did smaller fish.

191 For many benthic invertebrates, larval settlement occurs in respo

192 via pathogen concentration and retention by benthic invertebrates.

193 ted biphenyls, chlorpyrifos, and four marine benthic invertebrates.

194 ces determine survival in the planktonic and benthic life stages, but traits established in the larva

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

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

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

198 degradable plastic carrier bags as litter on benthic macro- and meio-faunal assemblages and biogeoche

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

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

201 ndo and depth range of significant impact to benthic macrofaunal communities.

202 (elevated metal concentrations) stressors on benthic macroinvertebrate communities.

203 bility varied between seasons: peak littoral benthic macroinvertebrate density occurred in mid-winter

204 containing different animal assemblages (1-4 benthic macroinvertebrate species).

205 iments conducted with natural assemblages of benthic macroinvertebrates established concentration-res

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

207 marine planktonic cyanobacteria evolved from benthic marine and some diverged from freshwater ancesto

208 Many benthic marine animal populations are established and ma

209 opic-scale processes significantly influence benthic marine ecosystems such as coral reefs and kelp f

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

211 in eliciting settlement and metamorphosis of benthic marine larvae.

212 However, benthic marine mesoherbivores such as the common periwin

213 Pelagic dispersal of most benthic marine organisms is a fundamental driver of popu

214 Many benthic marine organisms produce calcium carbonate (CaCO

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

216 adation) was significantly different between benthic (median = -1.40 per thousand; range, -2.34 to -0

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

218 g cracks in sediments and an increase in the benthic methane flux from sediments.

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

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

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

222 tudy aimed at achieving high power output of benthic microbial fuel cells (BMFCs) with novel geometri

223 nce or environment, shaped beta-diversity of benthic microeukaryotes (including both the abundant and

224 Benthic microeukaryotes are key ecosystem drivers in mar

225 Overall, OTU richness of benthic microeukaryotes decreased with increasing water

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

227 marine macrofossils (primarily new data from benthic molluscs) from a highly expanded Cretaceous-Pale

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

229 Traditional benthic monitoring relying on morphotaxonomic inventorie

230 ding approach meets the quality standards of benthic monitoring remains to be tested.

231 We advocate that future benthic monitoring should integrate metabarcoding as a r

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

233 ding) represents a promising alternative for benthic monitoring.

234 ggesting that the Gaoyuzhuang fossils record benthic multicellular eukaryotes of unprecedentedly larg

235 tially reducing energy transfer rates though benthic multicellular food webs.

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

237 Redox dynamics are driven by benthic O2 consumption, limited air-water exchange of ox

238 Yet, small-sized benthic or soil animals such as nematodes have largely b

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

240 co-occur with well-preserved planktonic and benthic organisms at the type locality of the upper Maas

241 The burrowing and feeding activities of benthic organisms can alter metal speciation in sediment

242 Benthic organisms had relatively high SigmaPFASs compare

243 ent forms of AC (biogenic and petrogenic) on benthic organisms has been performed.

244 useful predictions of metal bioavailable to benthic organisms in dynamic sediment environments.

245 A battery of 3 different benthic organisms with different feeding and life-cycle

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

247 rrestrial plants and extinctions of deep-sea benthic organisms.

248 at inadequately capture the behavior of many benthic organisms.

249 P(+) can be assessed for neither pelagic nor benthic organisms.

250 Ga, the chemical and isotopic signatures of benthic oxidative weathering would have become more glob

251 They correlate with major positive shifts in benthic oxygen isotope records and generally coincide wi

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

253 re, a sex-inducing pheromone (SIP(+)) of the benthic pennate diatom Seminavis robusta was identified

254 te closely with tissue residue in the marine benthic polychaete Neanthes arenaceodentata exposed in t

255 thed marine population and this high-toothed benthic population reveals that increases in tooth numbe

256 n phytoplankton may have positive effects on benthic PP at the ecosystem scale.

257 to 2000s may be substantially compensated by benthic PP, which increased by up to 190%.

258 ant, but as yet unquantified, food source to benthic predators [9].

259 elevated trophic transfer efficiencies with benthic-predominant systems.

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

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

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

263 algae that often dominate pelagic as well as benthic primary production in the oceans and inland wate

264 ystems dominated by external MeHg sources or benthic production found eutrophication to decrease MeHg

265 ed the taxonomic diversity of planktonic and benthic protist communities collected in six distant Eur

266 oss the seafloor and between the pelagic and benthic realms.

267 Limited Early Triassic benthic recovery was restricted to mid-water depths and

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

269 d winter period, we expected to find general benthic reliance throughout the year, but also a seasona

270 osystems, contributing to elemental cycling, benthic remineralization, and ultimately sequestration o

271 be of particular importance for a burrowing, benthic scavenger, such as hagfish, which are likely to

272 for these populations, and, until recently, benthic sediment was thought to be the main methylmercur

273 This was in contrast to benthic sediments in Iqaluit (population 6699), which we

274 antities are among the highest recorded from benthic sediments.

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

276 etation that this species employed a form of benthic skim feeding by using its mandible to probe for

277 ns based on natural history, behavior of key benthic species and environmental context allow assessme

278 enness, and density, and some differences in benthic species composition.

279 models provide an opportunity to read across benthic species with different feeding strategies.

280 is well established in many terrestrial and benthic species, its purpose in pelagic species (squid a

281 ated biphenyl bioaccumulation by four marine benthic species.

282 ontaminant (copper ~0.1 muM) in two keystone benthic species; mussels (Mytilus edulis) and purple sea

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

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

285 early animals did not experience appreciable benthic sulfide stress.

286 However, benthic surveys performed on areas treated with AC have

287 This bottleneck is particularly severe for benthic surveys, where millions of images are obtained e

288 roduction in six study species of bryozoans (benthic suspension feeders).

289 l describes the dynamics of corals and other benthic taxa under climate-driven disturbances (hurrican

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

291 c foraminifera and of the warmer half of the benthic values.

292 that on a global scale the decomposition of benthic viruses releases approximately 37-50 megatons of

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

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

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

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

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

298 redirection of production to the near-shore benthic zone, and large lakes may exhibit shifts in auto

299 tochthonous organic matter deposition to the benthic zone, following increased loading of nutrients t

300 he potential to use freshwater crayfish as a benthic-zone indicator of nanosilver and ionic silver po