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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
6                                      Using a marine algae data set, we show that quantification of fr
7 omeric pair of compounds, 4, assigned to the marine alkaloid discoipyrrole D is reported.
8  azaspirocyclization reaction, generates the marine alkaloids (-)-fasicularin 2 and a pro-forma synth
9 terrestrial life when Enterococci split from marine ancestors 400 million years ago.
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
12 ate change and causing acidification of both marine and freshwater environments.
13 sediment and ice cores from the terrestrial, marine and glacial realms.
14 on paradox' has been observed in oxygen-rich marine and lake waters, and viewed to significantly cont
15 rgence in food web structure between glacial-marine and oceanic sites.
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
20 ystem and contrast the cost-effectiveness of marine- and land-based conservation actions.
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
23 strongly affect movement behavior of tracked marine animals.
24 taceans, arguably the most abundant group of marine animals.
25  ciliated larvae of Platynereis dumerilii, a marine annelid.
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
30                  The trophic linkage between marine bacteria and phytoplankton in the surface ocean i
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
33 ic drift driving ancient genome reduction of marine bacterioplankton lineages.
34        Under oxygen-limiting conditions, the marine bacterium Dinoroseobacter shibae DFL12(T) generat
35 me analyses and phenotypic screenings of the marine bacterium Phaeobacter inhibens we found that the
36                                          The marine bacterium Vibrio fischeri is the monospecific sym
37 adation among closely related strains of the marine bacterium Vibrio splendidus One strain, V. splend
38  Chisholm tells us all about this powerhouse marine bacterium.
39 , in anoxic sediments, such as ore deposits, marine basins, and contaminated aquifers.
40 ation at urban waterways, lakes, and coastal marine beaches is responsible for costs that should be a
41 y by other extinct molluscivores such as the marine bear Kolponomos.
42 an-to maximise the extent of light-dependent marine benthic habitats across decadal timescales.
43          The Coral Triangle is a hotspot for marine biodiversity held in its coral reefs, seagrass me
44 d lineages to our expanding understanding of marine biodiversity.
45 SA produced by jet drops can be modulated by marine biological activity.
46              Here we investigate whether the marine biosphere can be identified as a source of Se and
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
49 lta(202)Hg) data for six species of Hawaiian marine bottomfish.
50 nts likely caused by nucleation in the polar marine boundary layer was quantified annually as 18%, wi
51 ciation in marine habitats, since all extant marine clades are relatively young.
52 help drive the pattern of young, depauperate marine clades.
53 ation may have far-reaching consequences for marine community and ecosystem dynamics, but its full im
54                                              Marine cone snails contain a high diversity of toxins in
55 seline sources, ambient water and tissues of marine consumers, estimates of the riverine organic matt
56                          Characterisation of marine copepod gut microbiome composition and its variab
57              The absence of correlation with marine cyclic solutes contradicts a control of atmospher
58 ntial source is the atmospheric oxidation of marine derived trimethylarsine.
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
61          Here we measured the responses of a marine diatom, Thalassiosira pseudonana, to high and low
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
64  question of how rapidly multiple drivers of marine ecosystem change develop in the future ocean.
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
69 ultiple sedimentary records and supported by marine ecosystem modeling.
70 , but also affect components of the adjacent marine ecosystem.
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
75                                 The distinct marine ecosystems found in these environments include es
76 ficant swaths of terrestrial, freshwater and marine ecosystems from a range of threats.
77 ns in herbivore function have shaped shallow marine ecosystems from kelp forests to coral reefs.
78  with the conservation and sustainability of marine ecosystems presents major challenges.
79 ation as gigantic apex predators of Mesozoic marine ecosystems suggests.
80 nthropogenic nitrogen (N) loads to nearshore marine ecosystems through sediment microbial processes s
81 stically altered the abundance of animals in marine ecosystems via exploitation.
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,
84                  Our results suggest that in marine ecosystems, pathways for bottom-up and top-down f
85 fore buffer against the impact of warming on marine ecosystems, suggesting a novel mechanism by which
86                                           In marine ecosystems, the role of bottom-up and top-down fo
87 s on how consumers affect the functioning of marine ecosystems.
88 ccessing the microbial behaviours that shape marine ecosystems.
89 porting Hg from freshwater environments into marine ecosystems.
90 ges are expected to have dramatic impacts on marine ecosystems.
91 rophic to hypereutrophic) typically found in marine ecosystems.
92 g future biogeography and the functioning of marine ecosystems.
93 a to obtain faster recovery of eutrophicated marine ecosystems.
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
96                                          The marine environment has proven to be a very rich source o
97 g and managing the risks of pollution in the marine environment requires mechanistic models for toxic
98                                       In the marine environment, fish respond quickly to warming, cau
99 plastics are widely dispersed throughout the marine environment.
100 own about their diversity, especially in the marine environment.
101  need not be confined to the photic zones of marine environments and, as such, may have been underest
102                                  Coastal and marine environments can begin up to 100 kilometers inlan
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
105           Dinoflagellates are key species in marine environments, but they remain poorly understood i
106 ning the impacts of past human activities on marine environments.
107 s it promising for practical applications in marine environments.
108 n seawater, indicating its good stability in marine environments.
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
113                        Simulations show that marine extinctions help drive the pattern of young, depa
114                   The reliable production of marine fish larvae is one of the major bottlenecks in aq
115                              Notably, 85% of marine fish species come from a single actinopterygian s
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
118               This could alter productivity, marine food webs and carbon sequestration in the Arctic
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
121 anic matter on the trophodynamics of coastal marine food webs is not well understood.
122 iability provides information on function of marine food webs, biogeochemical cycles and copepod heal
123 ostly via red meat, dairy products and fatty marine foods.
124  increase in frequency of these traits among marine genera over geological time could explain observe
125 esent a significant, and as yet unaccounted, marine geohazard.
126                          Here we show, using marine geological and geophysical data from the continen
127                                              Marine geological data show that the West Antarctic Ice
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
132 tance to ecosystem structure and function of marine habitats.
133 ated ozone (O3) deposition over seawater and marine halogen chemistry accounted for in both the later
134                            Following a 2011 'marine heatwave' in Western Australia, we observed high
135 these keystone species in the degradation of marine hydrocarbons.
136         Paleontological data show that older marine invasions have consistently ended in extinction.
137                                 Here, we use marine invertebrate communities to parameterise numerica
138 fied, including taxa previously described in marine invertebrate microbiomes with possible links to a
139                                         Many marine invertebrates including ctenophores are capable o
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
147 posited in response to sea-level rise during Marine Isotopic Stage (MIS) 13.
148 ting settlement and metamorphosis of benthic marine larvae.
149 potential for adverse health effects amongst marine life and spill responders in the northern Gulf of
150 n reef-builders, besides many other forms of marine life.
151             Such is the case for NE Atlantic marine macroalgal forests, important ecosystems whose ma
152  whales have the potential to reshape Arctic marine mammal distributions and behavior.
153 rophic levels, from zooplankton organisms to marine mammals and seabirds.
154 redator activity at-sea, with some birds and marine mammals demonstrating contrasting behavioural pat
155                                      Because marine mammals occupy upper trophic levels in Arctic foo
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
158 pleted oxygen in Earth's oceans resulting in marine mass extinction.
159 he promising bioactivity of the tetraarsenic marine metabolite arsenicin A, the dimethyl analogue 2 a
160                 Here we report on the use of marine metatranscriptomics to probe virus-host relations
161 tognaths quickly became important members of marine metazoan communities [6].
162            Nearly every important control on marine microbial physiology is currently in flux, includ
163 these viruses infect dominant members of the marine microbiome such as Prochlorococcus and Pelagibact
164             To investigate the behaviours of marine microorganisms at spatially relevant scales, we e
165                   Galloway and Lewis discuss marine microplastics and their devastating effects on oc
166 ory induction using sensory neurons from the marine mollusk Aplysia californica.
167 cation and quantification of vitellogenin in marine mussel gonads and compared the results with those
168 r cohesion exhibited by adhesion proteins of marine mussel.
169 the construction of the potent antibacterial marine natural product bromophycoic acid E scaffold.
170                               Stolonidiol, a marine natural product, has been reported to potentiate
171                                  The rise of marine nitrate could have allowed for the rapid diversif
172 ichodesmium, is an integral component of the marine nitrogen cycle and contributes significant amount
173 nce for the emergence of a pervasive aerobic marine nitrogen cycle.
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
176                      A significant amount of marine oil snow formed in the water column of the northe
177 lines of evidence indicating the presence of marine oil snow sedimentation and flocculent accumulatio
178                                         Deep marine oil spills like the Deepwater Horizon (DWH) in th
179 tocks because it is isotopically district to marine organic matter.
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
182                                     However, marine organisms have received comparatively little scie
183 ophores, a phylum of carnivorous, gelatinous marine organisms, as the sister lineage.
184 , including the adhesion proteins of several marine organisms.
185 and deoxygenation, poses a serious threat to marine organisms.
186 Brown algae are photosynthetic multicellular marine organisms.
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
189                                          The marine osmolyte dimethylsulfoniopropionate (DMSP) is one
190 itrogen loss processes using newly available marine oxidants.
191 ecific transporters has implications for the marine phosphorus redox cycle, and might aid the use of
192 on the biological communities that carry out marine photosynthesis.
193 s sense we challenge the general belief that marine phototrophs and heterotrophs compete for the same
194 2 level will lead to a variety of effects on marine phytoplankton and ecosystems.
195                                              Marine phytoplankton inhabit a dynamic environment where
196 is of a 100-day co-culture between the model marine picocyanobacterium Synechococcus sp. WH7803 and t
197                                    Using the marine planktonic diatom Pseudo-nitzschia multistriata,
198 Here we tested if mycoviruses derived from a marine plant endophyte can replicate in plant cells.
199                                              Marine plastic debris is a global environmental problem.
200                    A substantial fraction of marine plastic debris originates from land-based sources
201 uires an understanding and quantification of marine plastic sources, taking spatial and temporal vari
202 e is critical for the persistence of benthic marine populations.
203 ation dynamics of a long-lived, wide-ranging marine predator are associated with changes in the rate
204                                          Top marine predators are expected to experience a particular
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
210 mate event, only few include high-resolution marine records that span the YD.
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
214                                 We find that marine red beds are a prominent feature of the sedimenta
215 emporal record of banded iron formations and marine red beds.
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
221                      A new study of Mesozoic marine reptiles shows how minute balance organs in the i
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
225                     Yet, the extent to which marine reserves are globally interconnected and able to
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
228                                 Evidence for marine reserves' potential to manage fisheries in an eco
229 rially derived carbon (C) to atmospheric and marine reservoirs.
230                  Poly-metallic nodules are a marine resource considered for deep sea mining.
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
234 sil record, including changing quantities of marine rock or time-variable sampling effort.
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
237                                              Marine sediment records suggest that episodes of major a
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
240  conodonts, occur worldwide in many Cambrian marine sediments [6, 7].
241 hells and benthic foraminifer assemblages in marine sediments indicate that enhanced CDW upwelling, c
242 mily Teredinidae (shipworms) that burrows in marine sediments rather than wood.
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
246 bolic potential was consistent with detrital marine snow degradation.
247 olved organic matter in the ocean point to a marine source for the measured OVOCs.
248                                  For two key marine species (kelp and sea urchins), we use oceanograp
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
251 e most invasive terrestrial, freshwater, and marine species in Europe.
252 dy investigates whether 'first sightings' of marine species outside their normal ranges could provide
253                                  To test how marine species respond to climate variability, we analyz
254 s oceans threatens the ability of vocalizing marine species to communicate.
255 bal meta-dataset of observed range shifts of marine species, we show that incorporating directional a
256                            Here, we document marine sponge presenting associated with visual and acou
257 ivated bacteria that exist as symbionts in a marine sponge.
258                   Only adult males presented marine sponges, typically doing so in the presence of se
259           Here, we provide evidence that the marine streptomycete strain CNQ-525 can reduce MnO2 via
260                                              Marine sub-cluster 5.1A isolates with higher phycouribil
261 al is far shorter than the residence time of marine sulfate, any change in the sulfur isotopic record
262 ctive force for influencing diversity within marine Synechococcus populations.
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
265 management strategies on invasion success in marine systems is still unclear.
266  Mercury (Hg) bioavailability to bacteria in marine systems is the first step toward its bioamplifica
267              Despite promises that 'healthy' marine systems show increased resilience, the effects of
268 rning specific case studies of adaptation in marine systems, and discuss associated characteristics a
269                                       Within marine systems, nitrogen availability is often the limit
270 ico have the potential to drastically impact marine systems.
271  and tangible barometer of climate change in marine systems.
272             The importance of bioluminescent marine taxa is highlighted in the water column, as we sh
273                                  The EAIS is marine-terminating and grounded below sea level within t
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
276                                     However, marine tests show that vanadium (V) is preferentially ex
277 e the longest-surviving group of secondarily marine tetrapods, comparable in diversity to today's cet
278                                              Marine Thaumarchaeota are abundant ammonia-oxidizers but
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
282                                          The marine trajectory regions include climate 'source' regio
283 back is mainly associated with a decrease in marine tropical low cloud (a more positive shortwave clo
284                                              Marine tufa-columns, formed by the hydrated carbonate mi
285 ating, and fatal tumor disease of endangered marine turtles.
286 pods, being restricted mostly to parrots and marine turtles.
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
289 ted ureolytic activity and its regulation in marine vibrios.
290 kely most abundant and ecologically relevant marine viral species, such as vSAG 37-F6, which were ove
291                                              Marine viruses are key drivers of host diversity, popula
292               While the collective impact of marine viruses has become more apparent over the last de
293 the activity and biogeochemical influence of marine viruses.
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
296                    We find that incursion of marine water beyond the crest of this ridge, forming an
297 colloids from agglomeration in high salinity marine waters by electrosteric repulsion for long time p
298                            Arsenic occurs in marine waters, typically at concentrations of 1-2 mug As
299             A map of a neuronal circuit in a marine worm reveals how simple networks of neurons can c
300 m various Food and Agricultural Organisation marine zones.

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