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1 can be sustained in stable equilibrium by an ecosystem.
2 rse, yet increasingly threatened, coral reef ecosystem.
3 identity during winter in a subpolar, marine ecosystem.
4 ll profiles exposed a rich and dynamic tumor ecosystem.
5 ng from the introduction of an invader to an ecosystem.
6 tions between cells within the dynamic tumor ecosystem.
7 ture, functions and integrity of the aquatic ecosystem.
8 usly documented in any marine or terrestrial ecosystem.
9 inants potentially affecting the Great Lakes ecosystem.
10 ould be the primary producers within the mat ecosystem.
11 sing the influence of hypoxia on the coastal ecosystem.
12 n Earth and play vital roles in nearly every ecosystem.
13 , semantically interoperable phenotypic data ecosystem.
14  causing ecosystem degradation across marine ecosystems.
15 n GBH residues and their possible effects on ecosystems.
16 phyll enhancements (SICE) subsidize seamount ecosystems.
17  of implementation compared with terrestrial ecosystems.
18 using dominance shifts and the rise of novel ecosystems.
19 tant relationships in terrestrial and marine ecosystems.
20 phages from similar, geographically isolated ecosystems.
21 ypothesis for the genera that occur in these ecosystems.
22 he annual carbon balance of these vulnerable ecosystems.
23 ervation and invasion dynamics in freshwater ecosystems.
24 communicate with each other within microbial ecosystems.
25 y cascading to populations, communities, and ecosystems.
26  including creation of novel communities and ecosystems.
27 n the integrity and functionality of aquatic ecosystems.
28 how and why they vary across communities and ecosystems.
29 ion, especially when applied to hyperdiverse ecosystems.
30 tial for supporting natural and agricultural ecosystems.
31 rect effects on plants and animals in forest ecosystems.
32 aquatic invertebrate communities from stream ecosystems.
33  the flow of energy and nutrients in aquatic ecosystems.
34 g and responding to global changes in marine ecosystems.
35 standing of mineral nanoparticles in natural ecosystems.
36 easonally variable energy source to seafloor ecosystems.
37 tentially mitigate climate-change effects on ecosystems.
38  know little about how warming affects whole ecosystems.
39  the expansion of vertebrates in terrestrial ecosystems.
40 ion networks in single cells to food webs of ecosystems.
41  (CO(2) ) emissions, strongly impacts marine ecosystems.
42 ing how climate warming will impact mountain ecosystems.
43 environmental change is altering the Earth's ecosystems.
44 ound plant production in natural terrestrial ecosystems.
45 hose in the most intensively used real-world ecosystems.
46 t of shale resources to affect nearby stream ecosystems.
47  productive food webs in subtropical pelagic ecosystems.
48 t of ecological parameters in Southern Ocean ecosystems.
49 ity level, and to functional consequences in ecosystems.
50 ge as an order of magnitude over terrestrial ecosystems.
51 vity, biodiversity, and dynamics of deep-sea ecosystems.
52 obial responses to climate change in montane ecosystems.
53 ntially impacting climate, human health, and ecosystems.
54 functions like BGE and the fate of carbon in ecosystems.
55 rent best estimate of global fire effects on ecosystems.
56 ssment of greenhouse gas emission by aquatic ecosystems.
57 ter the functioning and biodiversity of many ecosystems.
58 ces and efficiency of carrion removal within ecosystems.
59 mics of the underlying networks of financial ecosystems.
60 nd an important, often adverse, influence on ecosystems.
61 ment of the concerned regions but also their ecosystems.
62 pounds, which efficiently deposit to surface ecosystems.
63 in concert with climate change in freshwater ecosystems.
64 to coral death and the degradation of marine ecosystems(2).
65 opulations in expansive, inaccessible marine ecosystems [6].
66 ere, we analyze these effects in a grassland ecosystem 9 months after an experimental fire at the Jas
67 oncentrations continue to threaten acidified ecosystems across the northern hemisphere.
68 understanding of the dynamics of the pasture ecosystem and serve as a basis for managing livestock in
69                          Cancer is a complex ecosystem and should be considered in the context of its
70       Honey bees are critical pollinators in ecosystems and agriculture, but their numbers have signi
71 tion framework developed by the Economics of Ecosystems and Biodiversity for Agriculture and Food (TE
72  highlighting the need for research in other ecosystems and habitat types.
73 arth's surface leads to adverse feedbacks on ecosystems and humans.
74 n be an important tool to understand complex ecosystems and improve risk assessment.
75 eases (EIDs) of plants continue to devastate ecosystems and livelihoods worldwide.
76 ole they must be effective at conserving the ecosystems and species that occur within their boundarie
77 ty was considerable within biomes and within ecosystems and was mediated by landscape topography, cli
78 ate potential trophic interactions across an ecosystem, and a paucity of empirical information often
79 habitat, the suboptimal colonized salt marsh ecosystem, and on docks within the marsh, an artificial
80 ents the main objective in the context of an Ecosystem Approach, with large applications for detectin
81                              Blue carbon (C) ecosystems are among the most effective C sinks of the b
82 owing human populations and stressed natural ecosystems are at significant risk to such phenomena.
83                                              Ecosystems are composed of complex networks of many spec
84                              Tropical forest ecosystems are facing unprecedented levels of degradatio
85                                   Freshwater ecosystems are heavily impacted by multiple stressors, a
86                              Tropical marine ecosystems are highly vulnerable to pollution and climat
87                       Cold seasons in Arctic ecosystems are increasingly important to the annual carb
88                               However, these ecosystems are increasingly threatened by climate change
89                            Estuarine-coastal ecosystems are rich areas of the global ocean with eleva
90                               Southern Ocean ecosystems are under pressure from resource exploitation
91 med for the amount of radiation entering the ecosystem-are greatest in the multi-group scenario when
92 chment in arctic, alpine, and arid/semi-arid ecosystems around the world, yet our understanding of th
93 hange is altering the behavior of animals in ecosystems around the world.
94 is having profound effects on coastal marine ecosystems around the world.
95 itation control primary productivity in lake ecosystems as hydrological inputs of nutrients and organ
96  in both aquatic (as larvae) and terrestrial ecosystems (as adults).
97         Experimental studies of this natural ecosystem at the microbiome-wide scale are rare, and con
98 d to systemic and abrupt changes in multiple ecosystem attributes.
99                           IOM is a holistic, ecosystem-based and knowledge-based approach that aims t
100  to a February onset of plant growth and the ecosystem became a sustained carbon sink well before win
101 ity are well understood for many terrestrial ecosystems, but remain poorly resolved for many marine e
102  between RegulonDB data and the Bioconductor ecosystem by reusing the data structures and statistical
103 his synthesis takes the lead to quantify the ecosystem C and N cycling in response to warming and adv
104     As a result, the strength of the overall ecosystem C sink did not increase over time.
105                               However, total ecosystem C storage that includes soil organic C (SOC) m
106 ctives of stakeholders across the healthcare ecosystem can influence adoption of innovations in healt
107 at drying of these typically water-saturated ecosystems can fuel a surprising burst in shrub belowgro
108 rates on infectious disease and feedbacks to ecosystem carbon and nutrient cycling.
109 to tropical forest peatlands has resulted in ecosystem carbon emissions.
110                      We quantified the total ecosystem carbon stocks (TECS) in seagrass, emergent mar
111  offshore in the Southern California coastal ecosystem (CCE).
112 ic spatial or temporal predictions of abrupt ecosystem change.
113 f a top marine predator is being affected by ecosystem change.
114 around the world endanger the functioning of ecosystems, climate stability, and conservation of biodi
115 the extents of which varied among biomes and ecosystem compartments.
116 turies to millennia) re-assembly of degraded ecosystem complexity integrating interaction network and
117  factors that can dampen or prevent ultimate ecosystem consequences.
118 urrent model for the end-Permian terrestrial ecosystem crisis holds that systematic loss exhibited by
119     Extreme heat wave events are now causing ecosystem degradation across marine ecosystems.
120                      In addition to regional ecosystem devastation, we demonstrate how 'Arctic Dimmin
121 that inhabit marine, aquatic and terrestrial ecosystems, diatoms contribute ~ 45% of global primary p
122 ime shifts' have been observed in a range of ecosystems due to various forcing factors.
123 ironmental problems in temperature-sensitive ecosystems (e.g., coral bleaching, hypoxia) and is expec
124                       Thus, both disease and ecosystem ecology stand to grow as fields by exploring q
125                  Here, we apply methods from ecosystem ecology that quantify the structure and dynami
126 re and dynamics of the trophic network using ecosystem energetics to data from a large grassland biod
127 first, that there is no loss in bioturbation ecosystem engineering behaviors after the mass extinctio
128 eviously been given to analyzing patterns in ecosystem engineering complexity as a result of the exti
129 iors include deep tier, high-impact, complex ecosystem engineering.
130     This would benefit the entire healthcare ecosystem, especially in light of the shift to value-bas
131 y of environmental stress that organisms and ecosystems experience, but effects of changing stress re
132               This is one of the first whole-ecosystem experiments to involve replicated metagenomic
133 cts from the perspectives of the animals and ecosystems exposed to the sounds.
134                                       Marine ecosystems face numerous challenges from natural and ant
135 ve severe and long-lasting impacts on marine ecosystems, fisheries and associated services.
136  significant emerging risks to biodiversity, ecosystem function and associated socioecological system
137          Aquatic insects are vital to stream ecosystem function and biodiversity but insufficiently s
138                      Controlled biodiversity-ecosystem function experiments with random biodiversity
139 als and their ambiguous role in biodiversity-ecosystem function relationships.
140 nt effects of herbicides and insecticides on ecosystem function, and slightly less consistent effects
141  and seasonal patterns of fluxes and (b) the ecosystem functional responses.
142 ient dynamics in the context of biodiversity-ecosystem functioning (BEF) research.
143 inue, preventing for accurate projections of ecosystem functioning and climate feedbacks.
144 timber and eroded soil, leading to shifts in ecosystem functioning and community composition.
145 g individuals of invasive species can affect ecosystem functioning and recovery.
146 trolling the establishment, persistence, and ecosystem functioning impacts of a regionally abundant f
147 xplore general patterns in soil biodiversity-ecosystem functioning relationships, with only 0.3% of a
148  impacts of warming and biodiversity loss on ecosystem functioning were mediated by thermal trait var
149             Bacteria are key contributors to ecosystem functioning, but relatively little is known ab
150 o occur by 2050 and can significantly affect ecosystem functioning, causing dominance shifts and the
151 individual growth, population production and ecosystem functioning, including in the assessment of su
152 communities usually provide higher levels of ecosystem functioning.
153 tes that higher species richness can enhance ecosystem functioning.
154 nderstanding of their interactive effects on ecosystem functioning.
155 rier to understanding community dynamics and ecosystem functioning.
156 henotypic traits constrain recovery of basic ecosystem functions (decomposition of organic matter, be
157 micro-food webs (microbes and nematodes) and ecosystem functions (soil C and N mineralization), using
158  across trophic levels, taxonomic groups and ecosystem functions and that decreasing plant genotypic
159  of soil biodiversity in regulating multiple ecosystem functions is poorly understood, limiting our a
160                    For soil microbes and the ecosystem functions they catalyze, whether such heteroge
161 he species richness of 16 trophic groups, 10 ecosystem functions, and 15 ecosystem services.
162 fect the relationships between biodiversity, ecosystem functions, and services, we built networks fro
163 nt leaf traits and their capacity to predict ecosystem functions.
164 s among community assembly, composition, and ecosystem functions.
165  nutrient limitation of primary consumers in ecosystems globally.
166  most genome recovery attempts in freshwater ecosystems have only targeted specific taxa.
167 rious consequences for air quality and human/ecosystem health within the region.
168 ential consequences for animal-, human-, and ecosystem-health.
169            In addition to highlighting novel ecosystem impacts of alternate bioenergy landscapes, our
170 ral microbiome, presents itself in a complex ecosystem important to health and disease.
171 n a healthy maturation of the oral microbial ecosystem in children.
172 the role of such large and biodiverse forest ecosystem in regional and global atmospheric chemistry a
173 izing ichthyoplankton dynamics across marine ecosystem in the Northeast Pacific can help elucidate th
174      Northern boreal peatlands are important ecosystems in modulating global biogeochemical cycles, y
175                Some of the densest microbial ecosystems in nature thrive within the intestines of hum
176       This framework can be applied to other ecosystems in the Anthropocene to better understand vari
177 he oral microbiome is one of the most stable ecosystems in the body and yet the reasons for this are
178                            Andean freshwater ecosystems in the Neotropical region are expected to be
179  in and near Grand Canyon supports important ecosystems in this mostly arid environment.
180 PKC family actions and interventions in this ecosystem, informed by insights into the control of stro
181                 However, New Guinea has high ecosystem intactness and both regions are rich in endemi
182                                     One such ecosystem is Florida Bay, an important nursery for the C
183  their potential toxic effects on people and ecosystems is important.
184                Restoration of coastal marine ecosystems is perceived by many to be expensive and pron
185 s critical for the maintenance of coral reef ecosystems-is increasingly threatened by environmental s
186   When a range-shifting species colonizes an ecosystem it has not previously inhabited, it may experi
187 differentiated by the average dryness of the ecosystem itself: in mesic ecosystems, sigma decreases i
188                                   We used an ecosystem-level experimental system to independently con
189        However, much research has focused on ecosystem-level responses, and we know substantially les
190 ate the potential for significant changes in ecosystem-level spatial heterogeneity of microbial funct
191 shows that a massive collapse of terrestrial ecosystems linked to volcanism-driven environmental chan
192 of the subsurface, including those microbial ecosystems located within cave systems.
193                 The complexity of coral-reef ecosystems makes it challenging to predict their dynamic
194 we analyze multiple natural and experimental ecosystems (marine plankton, intertidal mollusks, and de
195 lternatively, the maximal cost the Lightning ecosystem may impose for a given average volume of trans
196 t supply and diversity, suggesting that real ecosystems may not obey a universal nutrient-diversity r
197  in the sensitivity of different species and ecosystems means that rigorous case-by-case assessments
198 rk using the metabolic fingerprint of entire ecosystems (MeE) to facilitate the discovery of global b
199 ) loss of megabiota has a negative impact on ecosystem metabolism and functioning; and (iii) their re
200 ecosystem sensitivity to climate change, but ecosystem model projections are under-constrained by dat
201 dies must be informed by and integrated with ecosystem models that provide quantitative predictions f
202                      This feedback makes the ecosystem more prone to coral collapse under fishing pre
203     Islands are thus considered as the socio-ecosystems most vulnerable to species and habitat loss.
204  (N) deposition and resulting differences in ecosystem N and phosphorus (P) ratios are expected to im
205 valuated WUE in an Acacia-dominated woodland ecosystem of central Australia at various spatial and te
206 apy-induced adaptation of the multi-cellular ecosystem of metastatic cancer shapes clinical outcomes.
207                                  The coastal ecosystems of temperate North America provide a variety
208  and fates across wildfire-altered sagebrush ecosystems of the Great Basin ecoregion, western United
209  main evolutionary radiations in terrestrial ecosystems of the Mesozoic era (approximately 252-66 mil
210 ethane emissions has been reported for these ecosystems, offsetting mitigation potential.
211 mpounds toward safeguarding human health and ecosystems on a global scale.
212 ia, representing some of the highest biomass ecosystems on Earth.
213        Chemical spills in streams can impact ecosystem or human health.
214      A global goal of no net loss of natural ecosystems or better has recently been proposed, but suc
215 nd informative when applied across different ecosystems or over time.
216 , but remain poorly resolved for many marine ecosystems, particularly those within in coastal benthic
217                                 In a virtual ecosystem, players compete for habitats and resources, u
218                                         This ecosystem process is being jeopardized by changes in N i
219                                              Ecosystem process rates typically increase after plant i
220 terize leaf and canopy properties that drive ecosystem processes and to infer physiological processes
221 yet death from infection can alter important ecosystem processes including elemental recycling rates
222 it profiles and diversity, thereby affecting ecosystem processes of the whole tundra region.
223  predators may indirectly affect fundamental ecosystem processes, such as decomposition, by altering
224  amount and variability for most terrestrial ecosystem processes, we lack understanding of their inte
225 duce mitigation potential of terrestrial net ecosystem production by 8.3% (NEP, 22.25 Pg CO(2) /year)
226           Species contributing positively to ecosystem production in the warmed treatments were those
227 s of net ecosystem productivity (NEP), gross ecosystem productivity (GEP) and ecosystem respiration (
228 the seasonal pattern of sensitivities of net ecosystem productivity (NEP), gross ecosystem productivi
229 t how changes in winter snowfall will affect ecosystem productivity and plant community structure dur
230  influences of biogeochemical water type and ecosystem productivity on Earth's most diverse aquatic v
231 r critical resources on seasonal dynamics of ecosystem productivity remains largely unknown.
232 els to reproduce the observed sensitivity of ecosystem productivity to rainfall changes at 10 sites a
233 patial variation in population abundances to ecosystem properties.
234 articular biota, as well as on community and ecosystem properties.
235              Each additional unit area of an ecosystem provides an increasingly smaller unit of time
236         Our comprehensive picture of the HCC ecosystem provides deeper insights into immune evasion m
237                                              Ecosystem range is limited to areas with average positiv
238                        Such events may cause ecosystem reconfigurations arising from species range co
239 d by a several million-year delay in benthic ecosystem recovery.
240 hanisms driving their radiation into diverse ecosystems remain underexplored.
241 hic invertebrate megafauna across a range of ecosystems represents a first step to study future chang
242           Forecasting storm impacts on these ecosystems requires consideration of risk factors associ
243 ate the age and sources of C contributing to ecosystem respiration (R(eco) ) and CH(4) , while we con
244 NEP), gross ecosystem productivity (GEP) and ecosystem respiration (RE) in response to T(a) and EF an
245   The snow melt period coincides with rising ecosystem respiration and can offset up to 41% of the su
246 ntration from 1.6 to 2.1 mg L(-1) and stream ecosystem respiration from -3.2 to -4.5 mg L(-1).
247 eed back on one another to determine how the ecosystem responds to anthropogenic forcing.
248 ension of the importance of root exudates in ecosystem response to drought.
249                     Our results suggest that ecosystem responses are largely driven by surface peat,
250 tigate bacterial population structures at an ecosystem scale.
251                                              Ecosystem-scale calculations demonstrate that entropy fl
252 xtensive stakeholder consultation across all ecosystems, sectors and regions in Australia, involving
253 asts of future forest change are governed by ecosystem sensitivity to climate change, but ecosystem m
254                                              Ecosystem sensitivity was higher in models than observat
255  plantings to more effectively contribute to ecosystem service delivery and ecological intensificatio
256 s nitrogen, but the extent and value of this ecosystem service have not been well-characterized at th
257 nthropocene to better understand variance in ecosystem service outcomes and identify where and why br
258 ity (indicated by native vegetation) and two ecosystem services (carbon storage, sediment retention)
259                       Soils provide numerous ecosystem services (ESs) such as food production and wat
260 iodiversity Areas' and wilderness areas) and ecosystem services (productive fisheries, and carbon ser
261 e the interconnections between biodiversity, ecosystem services and sustainable development.
262 temperate North America provide a variety of ecosystem services including high rates of carbon seques
263 very of four locally important water-related ecosystem services modeled with the web-based tool AguAA
264 e review the roles of pathogens in mediating ecosystem services provided by autotrophs and outline sc
265 onsequences for the ecological functions and ecosystem services provided by reef systems.
266 s mortality events around the world threaten ecosystem services such as water filtration, nutrient cy
267 f climate change on soil microbiomes and the ecosystem services they provide present a grand challeng
268 l alter deep-sea biodiversity and associated ecosystem services, and may interact with disturbance fr
269 tructure and regeneration, biodiversity, and ecosystem services.
270 ophic groups, 10 ecosystem functions, and 15 ecosystem services.
271 portant prerequisite for the provisioning of ecosystem services.
272 ge dryness of the ecosystem itself: in mesic ecosystems, sigma decreases in drier years with a higher
273 th a higher sensitivity to dryness; in xeric ecosystems, sigma increases in drier years with a lower
274 nges in transfer efficiency compound through ecosystems, slight variations can have large effects on
275                                  Research on ecosystem stability has had a strong focus on local syst
276 idely recognised for their capacity to shape ecosystem structure and function.
277          Very large, irreversible changes to ecosystem structure are expected at levels of vegetation
278 es and in some cases irreversible changes to ecosystem structure.
279 ween squid and white sharks, in which future ecosystem studies should consider both species for manag
280 idate the role of interaction variability in ecosystem succession and to further determine if casting
281 ersity loss might affect human wellbeing and ecosystem sustainability.
282  has an impact on the carbon fluxes of these ecosystems, the direct anthropogenic disturbance may pla
283  and thus drive the responsiveness of arctic ecosystems to climate change.
284 ld measurements from 10 sites across diverse ecosystems to evaluate model performance.
285 lopment is increasing the exposure of marine ecosystems to nighttime light pollution, but is anthropo
286 pecies is to preserve natural soundscapes of ecosystems to which species have adapted to by reducing
287       CO(2) emissions were consistent across ecosystem types and climate zones, with local characteri
288 t of mercury (Hg) bioaccumulation in aquatic ecosystems, using dragonfly larvae as biosentinels, by d
289 species that co-occur in temperate grassland ecosystems, we thus investigated the effect of microplas
290 ce of biodiversity experiments to real-world ecosystems, where community assembly or disassembly may
291  tumors (gliomas) are heterogeneous cellular ecosystems, where non-neoplastic monocytic cells have em
292  the sustainability and resilience of marine ecosystems while integrating and balancing different oce
293 the performance of the community, indicating ecosystem-wide multitrophic complementarity, which is po
294 f clinical trials, and the clinical research ecosystem will need to adapt to this transformed environ
295 studies) of N fixation across three types of ecosystems with different status of disturbance (no mana
296 , to improve de-replication, and to identify ecosystems with promising characteristics as sources for
297 l temperatures across mid- and high-latitude ecosystems, with important implications for survival and
298 ms for improving our understanding of marine ecosystems, with the goal of informing policy and resour
299 present the highest risk to biodiversity and ecosystems within the APR over the next 10 years.
300 nite (CaCO(3)) skeletons support entire reef ecosystems, yet their formation mechanism is poorly unde

 
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