ライフサイエンスコーパス: geochemistry

1 e wide range of variables that influence REE geochemistry.

2 ter floc [TE], not predicted by water column geochemistry.

3 ly important to advance the field of aqueous geochemistry.

4 ions in Sr-90 concentrations and groundwater geochemistry.

5 stals, stable isotopic data and mass balance geochemistry.

6 fe on Earth, and embeds the biosphere within geochemistry.

7 of knowledge about their involvement in lead geochemistry.

8 f chemistry, physics, materials science, and geochemistry.

9 espiring bacteria may be controlling arsenic geochemistry.

10 is one of the main recent advances in marine geochemistry.

11 icrobial biochemistry coevolved with Earth's geochemistry.

12 uspension, and phytoplankton blooms on coral geochemistry.

13 ials sciences to catalysis, nanofluidics and geochemistry.

14 ellowstone National Park that have different geochemistry.

15 at environmental pressures, temperature and geochemistry.

16 e annual precipitation, well depth, and soil geochemistry.

17 cluded average annual precipitation and soil geochemistry.

18 reconstruct a simpler life form dependent on geochemistry.

19 odynamics rely on indirect observations from geochemistry.

20 es drive sediment fluxes and influence fjord geochemistry.

21 discussed in the context of their diverging geochemistry.

22 the Southern Carpathians, Romania using peat geochemistry.

23 not explained by corresponding variation in geochemistry.

24 otential link between microbial activity and geochemistry.

25 rmaceuticals, colloidal crystallization, and geochemistry.

26 ox differences, and the influence of aquifer geochemistry.

27 ommunities undergoing substantial changes in geochemistry.

28 ve of past oceanographic conditions in their geochemistry.

29 osteohistology,(11) palaeobiogeography,(12) geochemistry,(13)(,)(14) and soft tissues(15)(,)(16)(,)(

30 sses relevant to energy(1-5), biology(6) and geochemistry(7).

31 ation of DOM and its relation to groundwater geochemistry across a petroleum hydrocarbon plume cross-

32 g the conserved FeOOH "signature" on floc TE geochemistry across sites.

33 entric energy landscape, the amalgamation of geochemistry, advanced biology, and engineering emerges

34 ipitation and dissolution and change aqueous geochemistry, all of which impacts macroscopic system be

35 Prebiotic chemistry and early Earth geochemistry allow researchers to explore possible origi

36 We find that geochemistry alone cannot positively identify source sub

37 Stone geochemistry also influenced community diversity, partic

38 e formation of soil organic matter, but soil geochemistry also plays a critical role.

39 Shell geochemistry analyses resolved six differentiated cluste

40 c prokaryotes that are influential in global geochemistry and are promising candidates for industrial

41 susceptibility, X-ray fluorescence elemental geochemistry and carbon isotope datasets obtained from t

42 Paleosol geochemistry and climate simulations indicate paleoclima

43 These seasonal changes in geochemistry and community structure are likely due to h

44 The coincidence of the observed changes in geochemistry and crustal thickness with stepwise atmosph

45 has been a major and unresolved challenge in geochemistry and Earth history.

46 en textulariids and rotaliids based on their geochemistry and establishes T. agglutinans as a geochem

47 f methods ranging from mineralogy to isotope geochemistry and find that samples from the two outcrops

48 and vegetation using measurements of bedrock geochemistry and forest productivity.

49 onal groups respond to salinity, we examined geochemistry and functional gene amplicon sequence data

50 Here, through a combination of geochemistry and geochronology(9-14), we demonstrate tha

51 and therefore plays an important role in the geochemistry and geodynamics of the Earth's interior.

52 ents, paleontological documentation, isotope geochemistry and geophysical reconstructions.

53 of Australia and the present-day distinctive geochemistry and geophysics of the Australian-Antarctic

54 g Earth's living systems, its materials, its geochemistry and geophysics, and a broad spectrum of its

55 e nucleotide polymorphism markers with shell geochemistry and in conjunction with high resolution phy

56 Detrital garnet geochemistry and inclusion suites from both modern sedim

57 Careful correlation of both the geochemistry and instrumental monitoring data improves o

58 ynamics of mantle plumes from uranium-series geochemistry and interpret their results as evidence for

59 es, whose shock conditions are keys to their geochemistry and launch mechanism.

60 ighlight the importance of sediment and soil geochemistry and ligand competition on the fate of dival

61 ted with precipitation can impact hot spring geochemistry and microbial biodiversity.

62 geothermal area, was chosen to study arsenic geochemistry and microbial community using Illumina MiSe

63 We investigated trace metal geochemistry and microbial metal utilization in methane

64 The geochemistry and microbiology show consistent trends sug

65 search represents the first study of coupled geochemistry and microbiology within the PPR and demonst

66 s and productivity) in the Tasman Sea, using geochemistry and micropalaeontology, and find evidence f

67 ) and a discrete sample analysis system (for geochemistry and microparticles), both supplied from the

68 into the long-standing "dolomite problem" in geochemistry and mineralogy and may promote a better und

69 San Diego County, California, and uses their geochemistry and mineralogy to reconstruct climate and w

70 In modern environments, pore water geochemistry and modelling simulations allow the study o

71 collapses under pressure are fundamental to geochemistry and of increasing importance to fields as d

72 itative assessment of the evolving nature of geochemistry and permeability, resulting from coupled pr

73 The geochemistry and physical structure of each vent both pl

74 reconstruction, constrained by the geology, geochemistry and present-day environmental conditions of

75 MESSENGER (MErcury Surface Space ENvironment GEochemistry and Ranging) imagery and laser altimeter to

76 played a critical role in the rise of modern geochemistry and remains extensively used in (bio-)geosc

77 Region-specific variation in geochemistry and sediment-associated 16S rRNA gene ampli

78 present results of swath mapping, heat flow, geochemistry and seismic surveys from the young eastern

79 calls for reevaluation of subduction-related geochemistry and seismicity as well as water transportat

80 geochronology, plate-motion reconstructions, geochemistry and seismology to ascertain plume melting d

81 poxia tolerance is imprinted on both otolith geochemistry and species biogeography, the model allows

82 ope mass balance approach that combines bulk geochemistry and tectonic recycling rate calculations.

83 -directed motion of cells (galvanotaxis), to geochemistry and the formation of ice phases on planets,

84 g controversies on the interpretation of SCR geochemistry and the involvement of the putative Yellows

85 ture is largely controlled by solid-phase Cu geochemistry and the relative ability of Cu acquisition

86 Geochemistry and zircon Lu-Hf isotopes reveal ancient 4.

87 Integrated with information from whole-rock geochemistry and zircon U-Pb, Hf, and O isotopes, our zi

88 etter understand the interplay of hydrology, geochemistry, and biology controlling the cycling of car

89 ng tool in fields such as nuclear forensics, geochemistry, and biology that could benefit from uncove

90 ical volcanology, radiocarbon dating, tephra geochemistry, and chronicles, we argue the source of thi

91 eath arc volcanoes is a key control on magma geochemistry, and generates a hydrous lower crust.

92 ns, consistent with the hydrologic position, geochemistry, and land use being important controls on P

93 t interpretations of marine sediments, fjord geochemistry, and marine ecosystems.The reason some of t

94 d field-scale metatranscriptomics, porewater geochemistry, and methane gas fluxes to inform microcosm

95 nship between microbial cell dispersal, soil geochemistry, and microbial structure and function; and

96 Here we investigate the age, geochemistry, and microbiology of 138 groundwater sample

97 cluding hydrological setting, native aquifer geochemistry, and operational site parameters (e.g., sou

98 s in sedimentary facies, fossil assemblages, geochemistry, and paleotemperature.

99 n by the MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) spacecraft at alti

100 008, the MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) spacecraft became

101 r on the MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) spacecraft show de

102 e by the MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) spacecraft, show t

103 nts from MErcury Surface, Space Environment, GEochemistry, and Ranging (MESSENGER) spacecraft.

104 SSENGER (MErcury Surface, Space ENvironment, GEochemistry, and Ranging) spacecraft and the NASA Godda

105 of continents also controlled the location, geochemistry, and volcanology of the hottest preserved l

106 nctioning of microbial mats using an isotope geochemistry approach.

107 e integration of laser scans, sedimentology, geochemistry, archeobotany, geometric morphometrics and

108 which suggest that these differences in gas geochemistry are a consequence of gas migration through

109 otope signatures as tracers in environmental geochemistry are discussed and future perspectives prese

110 climate change, invasive species, and local geochemistry are likely affecting the response time and

111 , electrochemistry, analytical chemistry and geochemistry are used to illustrate the widespread influ

112 ical framework with which to model noble-gas geochemistry as a function of residual mantle mineralogy

113 ite being widely inferred from trace element geochemistry as a major lower crustal phase, amphibole i

114 scussion of the status of the field of coral geochemistry as it relates to the recovery of past recor

115 The mineralogy and geochemistry associated with Rodinian assembly ( 1.3-0.9

116 When he was a postdoc in geochemistry at Caltech, Charles David Keeling found him

117 e need for more systematic studies of cerium geochemistry at the microscale in paleontological contex

118 te fate of injected CO2 at the nanoscale via geochemistry, at the pore-scale via capillary trapping,

119 e ubiquitous and relevant for, among others, geochemistry, atmospheric chemistry, and chromatography.

120 y-machine learning with global mafic igneous geochemistry big data to explore atmospheric oxygenation

121 oles in numerous fields including chemistry, geochemistry, biochemistry, and materials science.

122 ental shelves and provide insight into shelf geochemistry, biogeochemical cycles, and the deep biosph

123 stable in relation to taxonomic composition, geochemistry, biophysics, and ecophysiological functions

124 ls with applications in materials chemistry, geochemistry, biophysics, and structural biology.

125 is arousing increasing interest, not only in geochemistry, but also in biomedicine.

126 green algal diversity on marine ecology and geochemistry, but has been proven difficult given the an

127 from the Daisyworld parable to real ecology/geochemistry, but sufficiently conserved variables may b

128 lts demonstrate that deeply-sourced volatile geochemistry can be used to constrain deep dynamic proce

129 We posit that boron isotope geochemistry can be used to quantify small fractions ( a

130 bduction-related magmatic arcs, confirm that geochemistry can be used to track changes of crustal thi

131 Temporal variation in geochemistry can cause changes in microbial community st

132 This suggests that bedrock geochemistry can influence landscape evolution through a

133 recent studies including contributions from geochemistry, catalysis, chemistry, and environmental an

134 ntensively studied previously with regard to geochemistry, chemoautotrophy, microbial isolation, and

135 Cu geochemistry clearly influences MMO expression in terres

136 he past, show larger ranges of erupted magma geochemistry compared to those that have not.

137 ) of Yellowstone National Park that exhibits geochemistry consistent with mixing of a reduced volcani

138 ed in karst regions, whether and how bedrock geochemistry contributes to the low karstic vegetation p

139 Our study implies that bedrock geochemistry could exert effects on vegetation growth in

140 resent records of sediment and foraminiferal geochemistry covering the greenhouse-icehouse climate tr

141 ogram (n = 52,849 samples) providing aqueous geochemistry data but no methane concentrations.

142 The model was calibrated and tested using geochemistry data including methane concentrations from

143 typic (microsatellite) and phenotypic (shell geochemistry) data in a geospatial framework to determin

144 This first volatile-geochemistry dataset from the CIR provides direct isotop

145 Aqueous geochemistry datasets from regional groundwater monitori

146 ictions must include an understanding of the geochemistry, decay properties, and ingrowth kinetics of

147 and ecological data recorded in the bivalve geochemistry during shell deposition remain intact over

148 of fields, such as chemical forensics, (bio)geochemistry, ecology, or (astro)biology.

149 transport framework that combines a powerful geochemistry engine with advanced numerical methods for

150 netite (Fe(3)O(4)) has broad implications in geochemistry, environmental science and materials scienc

151 oach integrated the dynamic variation in ETZ geochemistry, focusing on MeHg speciation change, alongs

152 ate of CO(2) and the evolution of subsurface geochemistry following CO(2) injection.

153 highlights that the critical role of bedrock geochemistry for the karst region should not be ignored

154 is seeming paradox, zircon geochronology and geochemistry from both the frozen lava and the cogenetic

155 a shales at the active sites and matched gas geochemistry from gas wells nearby.

156 ndment water cap, integrating aqueous sulfur geochemistry, genome-resolved metagenomics and metatrans

157 With recent technological advances (e.g., geochemistry, genomic approaches), combined with an emer

158 hydrothermal systems are influenced by fluid geochemistry, geologic setting and fluid flux between ve

159 Our investigations included platinum geochemistry, granulometry, optically stimulated lumines

160 Here, we use geochemistry, gravity, topography data, and numerical mo

161 Igneous geochemistry has been used to understand how changing he

162 We coupled spatially explicit sediment geochemistry (i.e., separate oxic and suboxic) to the in

163 Geochemistry identifies the source of the bitumen as an

164 volcanic field in Southern Laos: 1) Tektite geochemistry implies the presence of young, weathered ba

165 We analyzed microcharcoal, sediments, and geochemistry in a high-resolution marine sediment core o

166 of floc exerts an important control over TE geochemistry in aquatic environments, ultimately creatin

167 the previous baseline studies of groundwater geochemistry in shale gas areas, showing that a comprehe

168 e reveal the spatial association between DOM geochemistry in the dry season vs annual ecosystem excha

169 Cable bacteria dominate the sediment geochemistry in winter, whereas, after the summer hypoxi

170 ental life history using palaeohistology and geochemistry, in a 62 million-year-old pantodont, the cl

171 biodiversity with depth that were coupled to geochemistry, including a marked community change at the

172 Relationships between Ni C(DGT) and sediment geochemistry indicated a shift in Ni partitioning from A

173 Sediment cores and porewater geochemistry indicated that aerobic respiration and sulf

174 Paleosol geochemistry indicates a shift in paleoclimate towards m

175 sal sites, and analyzed for Mo and inorganic geochemistry indicators, including boron and strontium i

176 ive elephant samples, and (2) understand how geochemistry influences mineral intake.

177 ips with underlying geology and hydrothermal geochemistry, interactions with animals via symbiosis an

178 Noble-gas geochemistry is an important tool for understanding plan

179 g the redox transitions that control rhenium geochemistry is central to paleoredox and geochronology

180 The application of Pb isotopes to marine geochemistry is currently hindered by challenges associa

181 es either that our interpretation of adakite geochemistry is incorrect, or that our understanding of

182 A long-standing paradigm of arc geochemistry is that the trace element compositions of a

183 Understanding U isotope geochemistry is then essential either to develop sustain

184 A key goal of geochemistry is to date this event, but different ages h

185 itical role of ferrihydrite in environmental geochemistry, its structure is still debated.

186 s, mineral mimicry, environmental chemistry, geochemistry, materials science, and semiconductors.

187 These findings are supported by sediment geochemistry, metabolomics, and thermodynamic modelling.

188 Here we combine experimental petrology, geochemistry, mineral physics and seismology to constrai

189 s phase may exert an important control on As geochemistry, mobility, and bioavailability.

190 Advances in geochemistry, molecular phylogeny, and cell biology have

191 tigations ever undertaken regarding spherule geochemistry, morphologies, origins, and processes of fo

192 ub-micrometer length scales, such as isotope geochemistry, nuclear safety, and materials science.

193 million years of Earth's formation, based on geochemistry of >4.0 Ga detrital zircons from Australia.

194 ng: (1) Pt and palladium (Pd) abundance, (2) geochemistry of 58 elements, (3) coprophilous spores, (4

195 transport in subduction zones come from the geochemistry of arc volcanoes, seismic images and geodyn

196 ation reconstruction based on stable isotope geochemistry of Arctica islandica shells from the Fladen

197 nic and geologic characteristics shaping the geochemistry of continental hydrothermal systems that th

198 paleo-climatic proxy based on triple oxygen geochemistry of crystalline rocks that reveals changes i

199 CMI) approach to isolate the microstructural geochemistry of each component.

200 mical cycles, have profoundly influenced the geochemistry of Earth for over 3 billion years.

201 possible significance to the geodynamics and geochemistry of Earth's interior, as well as for the rol

202 sume H(2) and play a fundamental role in the geochemistry of Earth's ocean-atmosphere system.

203 olution of which transformed the biology and geochemistry of Earth.

204 magma flux estimates and radiogenic isotope geochemistry of eruption products.

205 ese results improve our understanding of the geochemistry of Fe(II) and arsenic in reducing environme

206 Here, we report on the geochemistry of Hadean detrital zircons as old as 4.15 G

207 rates a stochastic simulation to predict the geochemistry of high salinity (>20 mg/L Cl) groundwater

208 Unraveling the surface geochemistry of hydrated clay minerals is an abiding, if

209 ur results reveal a marked transition in the geochemistry of intrusions in the Candelaria district, c

210 U-Pb geochronology with zircon trace element geochemistry of intrusive rocks associated with the Cand

211 erefore must contain light elements, and the geochemistry of mantle-derived rocks reveals extensive s

212 Our data show that a marked shift in the geochemistry of mantle-derived volcanic rocks, reflectin

213 The geochemistry of Martian meteorites provides a wealth of

214 ism/mineral interactions not only affect the geochemistry of modern environments, but may also have c

215 the oxygen-isotope and incompatible-element geochemistry of MORBs by a component of recycled crust t

216 Here we use the geochemistry of opal-forming organisms from different wa

217 s' global mass, depositional timescales, and geochemistry of parent waters.

218 Here we report the petrography and geochemistry of peridotites from the Gakkel Ridge and Ea

219 It is suggested here that the geochemistry of phosphorus on the early Earth was instea

220 ionship using palaeorecords derived from the geochemistry of planktonic foraminifera.

221 erefore, have a controlling influence on the geochemistry of plume-related magmas, although unambiguo

222 tanding of how such leakage would impact the geochemistry of potable aquifers and the vadose zone is

223 y minerals are fundamental for environmental geochemistry of redox reactions.

224 dimentology, petrography, and carbon isotope geochemistry of sedimentary rocks across the S2 impact e

225 Here, we examine the geochemistry of seeps and surface water from seven sites

226 y a unique role in the structural, bio-, and geochemistry of silicon.

227 00 y occurred in early 43 BCE, with distinct geochemistry of tephra deposited during the event identi

228 In addition, glass geochemistry of the associated pumice deposits matches t

229 The geochemistry of the brine suggests that abiotic brine-ro

230 We examine the geochemistry of the cold water coralline alga Lithothamn

231 Parallel analyses of the geochemistry of the core and paleo-climate proxies revea

232 ems controls some fundamental aspects of the geochemistry of the early Earth, such as the FeO and sid

233 works sand filters could be explained by the geochemistry of the inlet water.

234 , recent excavations have suggested that the geochemistry of the site is no longer conducive to such

235 extracellular small molecules than with the geochemistry of the thermal springs.

236 The geochemistry of these sedimentary rocks provides further

237 LREEs is an overlooked aspect of the oceanic geochemistry of this group of elements previously though

238 the main trace of the fast slipping LOFZ and geochemistry of VMG provides evidence for the slab windo

239 For some volcanic arcs, the geochemistry of volcanic rocks erupting above subducted

240 Fractures are integral to the hydrology and geochemistry of watersheds, but our understanding of fra

241 e report on the effects of climate and stone geochemistry on microbiomes of Roman stone ruins in Nort

242 results from sea-level modelling and isotope geochemistry on mollusks establish that the inhabitants

243 The effects of groundwater geochemistry on the abundance, distribution, taxonomic d

244 e gap by exploring the importance of bedrock geochemistry on vegetation productivity based on a criti

245 To understand variations in geochemistry, organic petrology, and chemical compositio

246 microbial diversity, protein expression, and geochemistry over time.

247 currence rates, models including groundwater geochemistry parameters predict arsenic occurrence rates

248 Here we show that ocean geochemistry, particularly aragonite-calcite seas, drive

249 evant for many fields of research, including geochemistry, pharmacology, and medicine.

250 n that, based on the fossil record and ocean geochemistry, probably evolved just 10-15 my earlier.

251 his alternate view of early Earth phosphorus geochemistry provides an unexplored route to the formati

252 This suggests that the prevailing geochemistry, rather than localized dispersal, is the ma

253 enozoic terrestrial sedimentation and marine geochemistry records, as well as between global CO2 and

254 ical record is challenging because bulk rock geochemistry reflects complex histories.

255 hlorination in relation to riverbed sediment geochemistry remain ill-defined.

256 nucleation, and their importance in skeletal geochemistry requires an integrated, multiscale approach

257 The geochemistry resulting from equilibration of this atmosp

258 Using recent deep-Earth geophysics and geochemistry results, we create a comprehensive map of e

259 rature data for global volcanic activity (Hg geochemistry), sea-surface temperatures (conodont oxygen

260 data set of volcanic and plutonic whole-rock geochemistry shows that differentiation trends from prim

261 s of spatial and temporal variability in the geochemistry signal.

262 vertebrate community showed surface sediment geochemistry significantly explained shifts in community

263 To better understand how geochemistry, small molecule composition, and microbial

264 entral role in all branches of chemistry, in geochemistry, solid-state physics, and biophysics.

265 Here, we use wet geochemistry, spectroscopy, and electron microscopy to i

266 s, sediment facies, geodynamic modeling, and geochemistry suggest motion of the Hawaiian plume in Ear

267 Recent advances in petroleum geochemistry suggest that inorganic sedimentary componen

268 advanced spatially correlated microscopy and geochemistry techniques.

269 missions have provided insights into Martian geochemistry that indicate oxychlorine species, particul

270 lanation for fundamental features of Earth's geochemistry that is consistent with rocky planet format

271 ution corresponds to differences in the vent geochemistry that result from deep subsurface geological

272 structural observations, phase petrology and geochemistry that these pressure differences cannot be e

273 onsiderations, most notably those related to geochemistry, that challenge the long-term safety case f

274 s >4 Gya and initiation of biochemistry from geochemistry through oxygenation of the atmosphere to cu

275 ress the relative contributions of different geochemistries to the energy demands of these ecosystems

276 es the paradigm of soluble redox shuttles in geochemistry to be adjusted to include binding and modif

277 in an early stage during the transition from geochemistry to biochemistry.

278 in fields ranging from marine chemistry and geochemistry to industry, agriculture, and pharmacology.

279 In the present study, we applied forensic geochemistry to investigate the origin and fate of spill

280 Here we use skeletal boron geochemistry to reconstruct the DIC chemistry of the flu

281 skeletons and highlight the use of skeletal geochemistry to shed light on disease pathophysiology in

282 and grain-specific major- and trace-element geochemistry, to establish a well-characterized geochemi

283 ed techniques as Level-1 analyses, including geochemistry, total concentrations of naphthenic acids (

284 Due to similar geochemistry, V and Cr co-occurred most frequently.

285 Soil geochemistry was shown to influence the transfer and ele

286 nce of dry season infiltration on speleothem geochemistry, we combine a modern, sub-seasonally resolv

287 source-to-sink approach relying on isotopic geochemistry, we discriminate the effects of climate flu

288 sing remote sensing, dendrology and sediment geochemistry, we document a significant decrease in mang

289 examinations of porewater and solid-phase V geochemistry were therefore performed on oil sands fluid

290 or DncV and beyond pathogenesis to microbial geochemistry, which is important to environmental remedi

291 sed oxygen perturbations using selenium (Se) geochemistry, which is sensitive to redox transitions ac

292 environmental magnetism, sedimentology, and geochemistry, which reveals a strengthened late Miocene

293 ed from this period, and a study of their Pu geochemistry will allow us to date ancient metamorphic e

294 er column and sediment water interface (SWI) geochemistry with hydrodynamic data to develop a holisti

295 itating tufa and travertine do vary in their geochemistry with their viruses showing distinct variabi

296 simulator, which couples aqueous and mineral geochemistry with three-phase fluid flow calculations, h

297 f the most controversial topics in petroleum geochemistry, with several differing hypotheses proposed

298 nity structure can be directly correlated to geochemistry within these sediments, thus enhancing our

299 Elemental geochemistry (X-ray fluorescence) and delta(18)O from au

300 We use a combination of field-observations, geochemistry, X-ray computed microtomography (XCT) and t