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1 ng and the alignment of terrestrial, ice and marine (14)C and (10)Be records, the authors show that S
2 e analyzed the genomes of 119 strains of the marine actinomycete genus Salinispora, which is currentl
3 ion intensity analysis of SSA generated by a marine aerosol reference tank were compared with observa
4 uence of polluted urban and relatively clean marine airmasses, each with distinct atmospheric chemist
5 es: the analysis of lipid production for the marine alga Thalassiosira pseudonana, and an investigati
8 azaspirocyclization reaction, generates the marine alkaloids (-)-fasicularin 2 and a pro-forma synth
10 m (1999-2015) standardized survey of pelagic marine and anadromous species off Oregon and Washington
11 additional bacterial arborinol producers in marine and freshwater environments that could expand our
14 on paradox' has been observed in oxygen-rich marine and lake waters, and viewed to significantly cont
16 We found that only a quarter of Europe's marine and terrestrial areas protected over the last 100
17 cles and fruit flies are two prominent model marine and terrestrial representatives of the Arthropoda
18 ssions (fossil methane vented naturally from marine and terrestrial seeps and mud volcanoes) are thou
19 ster randomised controlled trial among Royal Marines and Army personnel in the UK military after depl
21 However, Pi uptake in streptophyte algae and marine angiosperms requires Na(+) influx, suggesting tha
22 flects arsenobetaine's release to water from marine animals associated with the euphotic zone rather
26 egrate demographic and ecological data for a marine apex predator, the broadnose sevengill shark Noto
27 oaches to assess the environmental impact of marine aquaculture using benthic foraminifera eDNA, a gr
28 phic level, as bears and foxes consumed more marine as opposed to terrestrial food, and as the availa
29 monooxygenase (FMO), is found widespread in marine bacteria and is responsible for converting TMA to
31 relatively high salt concentration of urine, marine bacteria would be particularly well suited for bi
32 al the catalytic process of TMA oxidation by marine bacterial Tmm and first show that NADP(+) undergo
35 me analyses and phenotypic screenings of the marine bacterium Phaeobacter inhibens we found that the
37 adation among closely related strains of the marine bacterium Vibrio splendidus One strain, V. splend
40 ation at urban waterways, lakes, and coastal marine beaches is responsible for costs that should be a
47 background by at least ca. 20%, supporting a marine biosphere-climate link through sea ice melt and l
48 trend in the rate of species description for marine bivalves and find a distinct spatial bias in the
50 nts likely caused by nucleation in the polar marine boundary layer was quantified annually as 18%, wi
53 ation may have far-reaching consequences for marine community and ecosystem dynamics, but its full im
55 seline sources, ambient water and tissues of marine consumers, estimates of the riverine organic matt
59 s are tightly coupled to the cell cycle in a marine diatom, and that arresting cells in the G1 phase
60 ] leads to G1-phase cell cycle arrest in the marine diatom, Phaeodactylum tricornutum, by binding to
62 ould be the world's largest known example of marine ecosystem "engineering" and suggests that trade-o
63 ial sediment runoff and a downstream coastal marine ecosystem and contrast the cost-effectiveness of
65 ration should be prioritised if the rates of marine ecosystem decline and expansion are similar and l
66 ection should take precedence if the rate of marine ecosystem decline is high or if the adjacent catc
67 -based actions are optimal when the ratio of marine ecosystem expansion to decline is greater than 1:
68 climate-induced modifications to the Arctic marine ecosystem may increase exposure risk to certain p
71 evaluate support for this theory in lake and marine ecosystems and demonstrate that ecosystem size is
72 es may be widespread in both terrestrial and marine ecosystems and present significant conservation c
73 change and ocean acidification are altering marine ecosystems and, from a human perspective, creatin
74 biomass may be especially important in many marine ecosystems because consumers, as opposed to produ
80 nthropogenic nitrogen (N) loads to nearshore marine ecosystems through sediment microbial processes s
82 ly among the most serious global threats for marine ecosystems, affecting a wide range of top predato
83 y 15% of the primary productivity in coastal marine ecosystems, fix up to 27.4 Tg of carbon per year,
85 fore buffer against the impact of warming on marine ecosystems, suggesting a novel mechanism by which
94 of marine sediments, fjord geochemistry, and marine ecosystems.The reason some of the Earth's tidewat
95 -Hakra-Nara, probably sustained a productive marine environment as well as navigability toward old co
97 g and managing the risks of pollution in the marine environment requires mechanistic models for toxic
101 need not be confined to the photic zones of marine environments and, as such, may have been underest
103 tion and abundance of such mobile species in marine environments remain challenging, often invasive a
104 y active isoprene degraders in estuarine and marine environments using DNA-SIP and to characterise ma
109 n is not present in these cases, meaning the marine enzymes used to degrade carrageenans must possess
110 ge, that StII, a pore-forming protein from a marine eukaryotic organism, encapsulated into Lp functio
111 data on mercury (Hg) isotope composition in marine European fish, for seven distinct populations of
112 nd seamount location play a critical role in marine evolution, mainly by intermittently providing ste
116 m half of global biological CO2 uptake, fuel marine food chains, and include diverse eukaryotic algae
117 ton primary production is at the base of the marine food web; changes in primary production have dire
119 y production exerts a fundamental control on marine food webs and the flux of carbon into the deep oc
120 a large influence on the future stability of marine food webs and the functioning of global biogeoche
122 iability provides information on function of marine food webs, biogeochemical cycles and copepod heal
124 increase in frequency of these traits among marine genera over geological time could explain observe
128 nce, secondary contact, and hybridization of marine groups in the northwest Pacific marginal seas.
129 tnumber all currently known phage genomes in marine habitats and include members of previously unchar
130 riverine organic matter subsidies to glacier-marine habitats by developing a multi-trophic level Baye
131 explained by limited time for speciation in marine habitats, since all extant marine clades are rela
133 ated ozone (O3) deposition over seawater and marine halogen chemistry accounted for in both the later
138 fied, including taxa previously described in marine invertebrate microbiomes with possible links to a
140 el for survival of well-skeletonized benthic marine invertebrates over a 100-million-year-long interv
141 the acute warming response of six Antarctic marine invertebrates: a crustacean Paraceradocus miersi,
142 appreciation of geoenvironmental dynamics of marine islands has led to advances in island biogeograph
143 vironments using DNA-SIP and to characterise marine isoprene-degrading bacteria at the physiological
144 line of Virginia and North Carolina dated to Marine Isotope Stage (MIS) 3, from 50 to 35 ka, are surp
145 geometric measurements of modern and palaeo (Marine Isotope Stage (MIS) 5e) tidal notches on Bonaire
146 a during the sea level lowstand accompanying marine isotope stage 6, rejecting earlier records of bis
149 potential for adverse health effects amongst marine life and spill responders in the northern Gulf of
154 redator activity at-sea, with some birds and marine mammals demonstrating contrasting behavioural pat
156 blubber-specific markers of acute stress in marine mammals of concern for which sampling of other ti
157 cetaceans and in contrast to North American marine mammals, chlorinated MBPs and DMBPs were more abu
159 he promising bioactivity of the tetraarsenic marine metabolite arsenicin A, the dimethyl analogue 2 a
163 these viruses infect dominant members of the marine microbiome such as Prochlorococcus and Pelagibact
167 cation and quantification of vitellogenin in marine mussel gonads and compared the results with those
169 the construction of the potent antibacterial marine natural product bromophycoic acid E scaffold.
172 ichodesmium, is an integral component of the marine nitrogen cycle and contributes significant amount
174 s correlation to global transcription in the marine nitrogen-fixing cyanobacterium Trichodesmium.
175 logy and ecology of phytoplankton, influence marine nutrient cycles, and act as vectors for horizonta
177 lines of evidence indicating the presence of marine oil snow sedimentation and flocculent accumulatio
180 (TMAO) that stabilizes cellular proteins in marine organisms against the detrimental denaturing effe
181 e peptides were isolated from a multitude of marine organisms and were used for a large number of mol
187 ore retroviruses as a whole, have an ancient marine origin and originated together with, if not befor
188 of these microorganisms could be traced to a marine origin, being transported thousands of kilometres
191 ecific transporters has implications for the marine phosphorus redox cycle, and might aid the use of
193 s sense we challenge the general belief that marine phototrophs and heterotrophs compete for the same
196 is of a 100-day co-culture between the model marine picocyanobacterium Synechococcus sp. WH7803 and t
198 Here we tested if mycoviruses derived from a marine plant endophyte can replicate in plant cells.
201 uires an understanding and quantification of marine plastic sources, taking spatial and temporal vari
203 ation dynamics of a long-lived, wide-ranging marine predator are associated with changes in the rate
205 the global carbon cycle, with almost half of marine primary production transformed by heterotrophic b
206 pacts were significantly higher within large marine protected areas than outside, refuting the critiq
207 cline and expansion are similar and low; (2) marine protection should take precedence if the rate of
208 e sedimentary sulfur isotopic composition of marine pyrite by examining a 300-m drill core of Mediter
209 elds corresponding to locations across their marine range; second, for the fields that elicited signi
211 d their properties are poorly constrained by marine records, including delta(18)O of benthic foramini
212 ed precise alignment of ice, atmospheric and marine records, making it difficult to assess relationsh
213 arth's climate history is best known through marine records, the corresponding continental climatic c
216 as wide continental shelves, can function as marine refugia for pelagic fauna, whereas offshore locat
217 cade trends in species richness in nine open marine regions around North America (197 region-years) w
218 istic representation of halogen processes in marine regions can improve model prediction of O3 concen
219 he relationships between first sightings and marine regions defined by patterns of local climate velo
220 i, a species previously recovered within the marine reptile 'superclade', for which we now provide a
222 tat patches can help design better-connected marine reserve networks for the future with equivalent c
223 Here, we develop a framework for designing marine reserve networks that integrates graph theory and
224 ductions in PLD due to ocean warming, future marine reserve networks would require more and/or larger
226 h could be reversed, however, by placing new marine reserves in areas sufficiently remote to minimize
227 se goals requires well-connected networks of marine reserves that maximize larval connectivity, thus
231 ity may be useful for adaptive management of marine resources, but their suitability for this purpose
232 nteract land- and ocean-based stressors: (1) marine restoration should be prioritised if the rates of
233 ontinental fragmentation promotes increasing marine richness, but that coalescence alone has only a s
235 no divergence between the kauri and Atlantic marine sediment (14)C data sets, implying limited change
236 Here, using sea-floor geophysical data and marine sediment cores, we resolve the record of glaciati
238 Chemical analysis of an Australian coastal marine sediment-derived fungus, Phomopsis sp. (CMB-M0042
239 nt a compilation of phosphorus abundances in marine sedimentary rocks spanning the past 3.5 billion y
241 hells and benthic foraminifer assemblages in marine sediments indicate that enhanced CDW upwelling, c
243 configuration may impact interpretations of marine sediments, fjord geochemistry, and marine ecosyst
244 erobic remineralization of organic matter in marine sediments, sulfate reduction coupled to fermentat
245 logical link to mid-latitude terrestrial and marine sites, and sheds light on the long-distance trans
249 hown for other glue-producing terrestrial or marine species and thus represent a unique glue system.
250 We document 289 living Japanese coastal marine species from 16 phyla transported over 6 years on
252 dy investigates whether 'first sightings' of marine species outside their normal ranges could provide
255 bal meta-dataset of observed range shifts of marine species, we show that incorporating directional a
261 al is far shorter than the residence time of marine sulfate, any change in the sulfur isotopic record
263 genomic analyses, cobalamin biosynthesis in marine systems has been inferred in three main groups: s
264 le of Hg speciation on Hg bioavailability in marine systems has not been teased apart from that of io
266 Mercury (Hg) bioavailability to bacteria in marine systems is the first step toward its bioamplifica
268 rning specific case studies of adaptation in marine systems, and discuss associated characteristics a
274 seaward of the Aurora subglacial basin, that marine-terminating glaciers existed at the Sabrina Coast
275 results have important implications for the marine-terrestrial biodiversity gradient, and studies of
277 e the longest-surviving group of secondarily marine tetrapods, comparable in diversity to today's cet
279 ly associated with postglacial adaptation of marine threespine stickleback (Gasterosteus aculeatus) t
280 oceanographic conditions and indicates that marine top predators may be more sensitive to the rate o
281 e and cost-effective methods to detect these marine toxins and protect seafood consumers' health is b
283 back is mainly associated with a decrease in marine tropical low cloud (a more positive shortwave clo
287 udy of new environmental niches, such as the marine versus terrestrial subsurface, often expands the
288 for differential habitat use among migratory marine vertebrates, we measured the naturally occurring
290 kely most abundant and ecologically relevant marine viral species, such as vSAG 37-F6, which were ove
294 de catalyst (PCNx) has been synthesized from marine waste and its use demonstrated in a metal-free he
295 results indicate significant regions of open marine water and active biologic productivity throughout
297 colloids from agglomeration in high salinity marine waters by electrosteric repulsion for long time p
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