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1 n situ (surface soils) or in ultimate sinks (marine sediments).
2 ciated microorganisms directly from deep-sea marine sediment.
3 different viral genotypes in one kilogram of marine sediment.
4 rm mucosal layers, called veils, on sulfidic marine sediment.
5 on or in the seafloor occur in every type of marine sediment.
6 a Streptomyces sp. obtained from a tropical marine sediment.
7 atty acids into its membrane phospholipids - marine sediment.
8 ntify it as a partner of sulfate reducers in marine sediments.
9 e formation of calcium phosphate minerals in marine sediments.
10 le of retaining terrigenous DOM fractions in marine sediments.
11 cells have recently been quantified in deep marine sediments.
12 burial of combustion-derived black carbon in marine sediments.
13 nd cosmogenic nuclide peaks in ice cores and marine sediments.
14 t surveys of eukaryotic life in warm, anoxic marine sediments.
15 atilization occurs for all carbonate-bearing marine sediments.
16 tial to promote subarc decarbonation of most marine sediments.
17 effect on the burial of calcium carbonate in marine sediments.
18 nds receiving biosolids and in freshwater or marine sediments.
19 found to control the MeHg formation rate in marine sediments.
20 creening of ether lipid biomarkers in recent marine sediments.
21 f the role of Archaea in the carbon cycle of marine sediments.
22 surface and are especially prevalent in deep marine sediments.
23 norganic carbon and organic matter in buried marine sediments.
24 rate of POC degradation within deeply buried marine sediments.
25 a significant source of tetraether lipids to marine sediments.
26 ted for the first time from permanently cold marine sediments.
27 for rates of methanogenesis in sub-Antarctic marine sediments.
28 ridional overturning circulation recorded in marine sediments.
29 y the standing stock of microplastics within marine sediments.
30 ity and over 50% of organic carbon burial in marine sediments.
31 tific drilling has identified a biosphere in marine sediments (1) , which contain many uncultivated m
32 no divergence between the kauri and Atlantic marine sediment (14)C data sets, implying limited change
33 nge of oxygen isotope values yet measured in marine sediments (-25 per thousand to +12 per thousand)
34 ate energy-based selection typical of anoxic marine sediments, 5-15% of taxa per sample exhibit depth
37 This relation suggests that, as in modern marine sediments, adsorption of carbon compounds onto cl
38 between carbon reservoirs, such as soils and marine sediments, also modulate atmospheric carbon dioxi
39 lts showed the distribution of Ag species in marine sediments amended with AgNP-citrate, AgNP-PVP, an
40 fuel cell consisting of an anode embedded in marine sediment and a cathode in overlying seawater can
41 he surface to the >5,000-y-old subsurface of marine sediment and identify a small core set of mostly
42 C-MIP-AES method was validated using several marine sediment and tissue matrix certified reference ma
43 n of methylmercury and butyltin compounds in marine sediment and tissue using microwave-assisted acid
44 urther research into the role of high Arctic marine sediments and climate on the Arctic marine MMHg b
47 nt for over half of organic carbon burial in marine sediments and thus they play a key role in the gl
49 ortant pathway for nitrate transformation in marine sediments, and this process has been observed to
50 t component of biogeochemical cycles because marine sediments are critical for long-term carbon stora
51 itrogen (N) cycling microbial communities in marine sediments are extremely diverse, and it is unknow
52 e biogeochemical roles of benthic Archaea in marine sediments are hampered by the scarcity of culture
54 on and isotope composition have been used in marine sediments as a paleoproxy of the Earth's oxygenat
55 trafiltration LC-MS screening of extracts of marine sediment bacteria resulted in the discovery of te
56 We conclude that burial of biospheric POC in marine sediments becomes the dominant long-term atmosphe
57 glek Bay, Labrador (Canada) has contaminated marine sediments, bottom-feeding fish, seabirds, and som
58 Large amounts of methane are produced in marine sediments but are then consumed before contacting
59 ion of CH4 (AOM) is an important CH4 sink in marine sediments, but AOM has only recently been identif
61 he form of electricity can be harvested from marine sediments by placing a graphite electrode (the an
62 t al. reported that osmium isotope ratios in marine sediments can be used to determine the size of a
63 y, USA, which demonstrate that heterotrophic marine sediments can switch from being a net sink to bei
64 her with mercury anomalies in End-Cretaceous marine sediments coeval with the Deccan Traps eruptions.
67 composition of planktonic foraminifera in a marine sediment core from the Gulf of Guinea, in the eas
68 of planktonic foraminifera recovered from a marine sediment core in a region of Amazon River dischar
69 ments, and geochemistry in a high-resolution marine sediment core off Namibia to identify the process
70 face temperature (SST) proxy evidence from a marine sediment core, indicate the importance of regiona
71 stributions of DEH through depths of various marine sediment cores by quantitative PCR and pyrosequen
72 from Greenland ice cores and North Atlantic marine sediment cores document repeated extreme climate
73 ions from ice cores, continental records and marine sediment cores give conflicting results for this
74 material and geochemical parameters from six marine sediment cores in the vicinity of the Larsen ice
75 Radiocarbon-constrained chronologies from marine sediment cores indicate loss of ice contact with
76 spp. from deep and intermediate water-depth marine sediment cores to reconstruct the changes in dens
77 Here, using sea-floor geophysical data and marine sediment cores, we resolve the record of glaciati
81 ochemical data to show that early Palaeozoic marine sediments deposited approximately 540-480 Myr ago
83 Chemical analysis of an Australian coastal marine sediment-derived fungus, Phomopsis sp. (CMB-M0042
84 leolatus NRRL 18422 and from the undescribed marine sediment-derived Streptomyces sp. CNQ-525 reveale
85 ely correlated with those from ice cores and marine sediments, establishing the timing and sequence o
87 configuration may impact interpretations of marine sediments, fjord geochemistry, and marine ecosyst
88 , and genetic diversity of FIB isolated from marine sediments from a central Adriatic seaside resort.
90 nvironmental occurrence of SAmPAP diester in marine sediments from an urbanized marine harbor in Vanc
91 rations of PFOS-precursors observed in urban marine sediments from Canada, Japan, and the U.S, over a
95 lectricity from the organic matter stored in marine sediments has demonstrated the feasibility of pro
96 s and their associated metabolic activity in marine sediments have a profound impact on global biogeo
97 metabolites, but frequently inhabits coastal marine sediments heavily contaminated with anthropogenic
98 ed ketones (alkenones) preserved in lake and marine sediments hold great promise for paleoclimate stu
100 ith its ubiquity and stability in underlying marine sediments; however, the sources of IP25 have rema
101 -reducing bacteria, has been demonstrated in marine sediments in situ, and little is known of the rol
103 h deglacial warming through tar abundance in marine sediments, independent of previous geochemical pr
104 errestrial plant wax biomarkers deposited in marine sediments indicate constant C3 vegetation from ap
105 hells and benthic foraminifer assemblages in marine sediments indicate that enhanced CDW upwelling, c
108 c formation of calcium phosphate minerals in marine sediments is a major sink for the vital nutrient
109 of the organic geochemical biomarker IP25 in marine sediments is an established method for carrying o
110 uO nanoparticles (NPs) to denitrification in marine sediments is highly affected by the presence of c
111 imated that only 30% of the TerrOC buried in marine sediments is of terrestrial origin in muddy delta
114 enhouse gas and its biological conversion in marine sediments, largely controlled by anaerobic oxidat
115 such infiltration, volatiles retained within marine sediments may explain the apparent discrepancy be
116 affect the rate of biospheric POC burial in marine sediments more strongly than carbon sequestration
119 in acetate samples isolated from the anoxic marine sediment of Cape Lookout Bight, North Carolina.
120 ver the past 125 Myr, there is evidence from marine sediments of the continued role of precessional (
121 extracted from laboratory and field mesocosm marine sediment oil degradation studies indicate that th
122 restriction to regions exposing few Neogene marine sediments, or recent date of formal taxonomic des
124 cium isotope (delta(44/40)Ca) composition of marine sediments provides a tool for distinguishing amon
125 proteobacterium isolated from subzero Arctic marine sediments, provides a model for the study of life
128 n relative enrichment in reduced vs oxidized marine sediments, Re seems promising as a dead zone prox
134 s approximately 41.6 million years ago using marine sediment records of oxygen and carbon isotope val
137 n and initial delivery of these anomalies to marine sediments requires low partial pressures of atmos
138 ting organic matter mineralization in anoxic marine sediments, resulting in the temperature-driven de
141 of 2006 and January of 2008, a total of 671 marine sediment samples were collected at depths from 5
142 entire assemblages in more than 500 Cenozoic marine sediment samples, including more than 1 million t
146 Laboratory experiments with DDE-containing marine sediments showed that DDE is dechlorinated to DDM
148 ree different Certified Reference Materials (marine sediment SRM 1944, fish tissue 1947, and loamy so
149 erobic remineralization of organic matter in marine sediments, sulfate reduction coupled to fermentat
150 continuously from continents is preserved as marine sediment that can be analysed to infer the time-v
151 tion during river transport and is buried in marine sediments, then it can contribute to a longer-ter
152 ment involving direct release of CO2 through marine sediment was conducted using Ruditapes philippina
153 of SAmPAP diester and EtFOSE by bacteria in marine sediments was evaluated over 120 days at 4 and 25
154 1649a, air particulate matter; and SRM 1941, marine sediment) was based on the comparison of RI data
156 ges in the exogenic sulfur cycle recorded in marine sediments were global in scope and were linked to
158 ction-zone metamorphism of carbonate-bearing marine sediments (which are considered to be a major sou
159 action of carbon buried as organic matter in marine sediments, which can be linked to oxygen accumula
160 graphitic carbon is preserved and buried in marine sediments, while the less graphitized forms are o
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