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1 r table gradient in peatlands-a major C sink ecosystem.
2 c control for the heavily impacted North Sea ecosystem.
3 lso affect components of the adjacent marine ecosystem.
4 ermine the mean state of the circulation and ecosystem.
5 rass meadows are an important and threatened ecosystem.
6 hic processes that link to the Gulf of Maine ecosystem.
7 vides a unique window into a post-extinction ecosystem.
8 in sea levels are expected to affect coastal ecosystems.
9 lights occurred throughout the night in both ecosystems.
10 with implications for coastal organisms and ecosystems.
11 snails, causing bottom-up effects on wetland ecosystems.
12 heds light on their metabolism in engineered ecosystems.
13 hanges in the chemistry of coastal upwelling ecosystems.
14 w be questioned for their accuracy in desert ecosystems.
15 mpact the structure and functioning of whole ecosystems.
16 nium-laden waste streams threaten freshwater ecosystems.
17 rage for bees, which is often scarce in agro-ecosystems.
18 crown fires, such as most Mediterranean-type ecosystems.
19 freshwater resources, especially lacustrine ecosystems.
20 diverse Arctic, temperate, and (sub)tropical ecosystems.
21 challenges to organisms in alpine and polar ecosystems.
22 pecies across multiple trophic levels within ecosystems.
23 erscoring the interconnected nature of these ecosystems.
24 y been examined, particularly in terrestrial ecosystems.
25 ropolitan boundaries and impact distal river ecosystems.
26 tain faster recovery of eutrophicated marine ecosystems.
27 erties and impact climate, human health, and ecosystems.
28 ry producers and nutrient cyclers in aquatic ecosystems.
29 production in both natural and agricultural ecosystems.
30 w consumers affect the functioning of marine ecosystems.
31 e production of food and the conservation of ecosystems.
32 e of water and carbon dioxide in terrestrial ecosystems.
33 f observed changes vary considerably between ecosystems.
34 y-covariance techniques in arid and semiarid ecosystems.
35 in the science of sustainable management of ecosystems.
36 ctions; this was especially evident in drier ecosystems.
37 lating carbon fluxes in boreal and temperate ecosystems.
38 ng of the functioning of tropical rainforest ecosystems.
39 per trophic level predators in North Pacific ecosystems.
40 ly influential in biological communities and ecosystems.
41 tion changes remain uncertain in terrestrial ecosystems.
42 fects and their cascading effects throughout ecosystems.
43 by which they are depolymerized in microbial ecosystems.
44 oaches to conserving historical versus novel ecosystems.
45 the most exploited fisheries and endangered ecosystems.
46 tested in the complex settings of real-world ecosystems.
47 ly alter C cycling and accumulation in these ecosystems.
48 wn about other habitats such as dry tropical ecosystems.
49 long natural stress gradients in tidal marsh ecosystems.
50 omics and virus-host interactions in natural ecosystems.
51 changes and alters the functionality of soil ecosystems.
52 ent transfer rates in soil food webs of cold ecosystems.
53 biomonitoring tool to protect local aquatic ecosystems.
54 ioning, and is widely used to study tropical ecosystems.
55 rom the drastic alterations humans impose on ecosystems.
56 te the complexity of carbon cycling in these ecosystems.
57 a anemones) are the foundation of coral-reef ecosystems.
58 roach is relatively unexplored in freshwater ecosystems.
59 in communities influences the functioning of ecosystems.
63 g the most serious global threats for marine ecosystems, affecting a wide range of top predators.
64 erving regional species pools to help buffer ecosystems against predicted increases in environmental
65 ikely to further exacerbate loss of taxa and ecosystem alteration, especially in drying climates.
66 development, and early findings of the Care Ecosystem, an adaptive, personalized, and scalable demen
68 iment runoff and a downstream coastal marine ecosystem and contrast the cost-effectiveness of marine-
69 Our results provide insight into the HNSCC ecosystem and define stromal interactions and a p-EMT pr
73 use they are keystone species in terrestrial ecosystems and are acknowledged as an unrivalled source
74 lling the interplay between the stability of ecosystems and their biodiversity is still not well unde
75 and ocean acidification are altering marine ecosystems and, from a human perspective, creating both
76 on the flux of energy and materials through ecosystems, and our methodology paves the way for rigoro
77 of the microbial ecology of mountain glacier ecosystems, and particularly those at low- to mid-latitu
78 ng of carbon and nitrogen than 'undisturbed' ecosystems, and that even if complete recovery is reache
79 timate of the water needed to maintain local ecosystems, and the resulting water volumes are compared
80 nal and functional changes of this microbial ecosystem are correlated with a variety of human patholo
81 he effects of climatic fluctuations on local ecosystems are complex in these sensitive alpine areas,
86 Recent evidence shows that warm semi-arid ecosystems are playing a disproportionate role in the in
89 ts of the sources and sinks of H2 in various ecosystems are sparse, resulting in large uncertainties
90 g in both protected and unprotected tropical ecosystems are urgently needed to avoid further defaunat
93 esponses to warming, both within and between ecosystems, better understanding the link between host p
94 ients not only spread across the terrestrial ecosystem, but also affect components of the adjacent ma
95 on of silver in Ag-NPs affects their fate in ecosystems, but its influence on interactions with aquat
96 e resilience and diversity of fire-dependent ecosystems by inhibiting seed germination or increasing
98 on community assembly and the functioning of ecosystems (CAFE), by integrating both species richness
99 s damaging effects on the human body and the ecosystem, can be released into soils, ground-, and surf
106 K N is a good predictor of instantaneous net ecosystem CO2 exchange and 3) functional diversity of le
107 ses of immune cells produce diverse cellular ecosystems composed of multiple cell types, accompanied
108 should be prioritised if the rates of marine ecosystem decline and expansion are similar and low; (2)
109 should take precedence if the rate of marine ecosystem decline is high or if the adjacent catchment i
110 m models to examine projected changes in two ecosystem-defining variables: temperature and food avail
111 Global-scale studies suggest that dryland ecosystems dominate an increasing trend in the magnitude
112 the climate change-driven trends in multiple ecosystem drivers emerge from the background of natural
113 Building upon results from two large-scale ecosystem drought experiments in the eastern Brazilian A
114 affect the carbon flux of terrestrial forest ecosystems due to the link between the growing season le
116 s study, we assessed the indirect effects of ecosystem engineering by a wood-boring beetle in a neotr
118 actions are optimal when the ratio of marine ecosystem expansion to decline is greater than 1:1.4, wi
119 f the primary productivity in coastal marine ecosystems, fix up to 27.4 Tg of carbon per year, and pr
120 of the preservation of the natural Sardinian ecosystems for endangered species and human health.
127 of anthropogenic warming on biodiversity and ecosystem function across all ecological communities.
129 lenge the trait-based approach to predicting ecosystem function by demonstrating that different combi
130 jor gap in our understanding of biodiversity-ecosystem function relationships concerns the role of in
134 cesses (LSPs) control landscape development, ecosystem functioning and climate through biogeochemical
135 eached that global biodiversity loss impairs ecosystem functioning and the sustainability of services
136 which driver exerts the largest influence on ecosystem functioning and whether their relative importa
138 al value, they are an essential component of ecosystem functioning by offering habitat for numerous w
142 , and wood traits, the role of fine roots in ecosystem functioning, and the representation of fine ro
143 rsity of all other species groups that drive ecosystem functioning, as brown and green diversity comp
144 how diverse seabirds play important roles in ecosystem functioning, global nutrient cycling and clima
148 osion, with potentially pervasive effects on ecosystem functions and future evolutionary trajectories
149 tterns are widespread and thought to mediate ecosystem functions such as productivity and robustness,
151 instability in financial systems and complex ecosystems has been pointed out: in both cases, topologi
152 results suggest that recovering and restored ecosystems have less abundance, diversity and cycling of
155 al biodiversity is necessary to assess water ecosystem health and the quality of water resources.
157 rbon played an important role in undermining ecosystem health, particularly when pH was higher than 8
161 and impact of anammox bacteria in freshwater ecosystems, however, is largely unknown, confounding ass
162 importance of considering the legacy of past ecosystem impacts and how recovery or persistence of tho
163 t source reefs', which may supply 47% of the ecosystem in a single dispersal event, emerges from the
165 diversity of STs in ILTCFs suggests that the ecosystem in such settings might be more conducive for i
166 bal hot spot for variability, with semi-arid ecosystems in that country exhibiting increased carbon u
168 he East China Sea-one of the most productive ecosystems in the world that has also had its catch repo
169 of genetic material from species in aquatic ecosystems, including environmental DNA (eDNA), have imp
175 trait values can thus help to identify when ecosystem-level effects are likely to exceed species-lev
178 e theory for population cycles, ranging from ecosystem-level to demographic modelling, grounded in ob
181 species shifts persist, the future of these ecosystems may rely on a greater concern for the composi
182 ipulation to quantify how coupling of stream ecosystem metabolism and nutrient uptake responded to a
187 lemetry data were compared with results from ecosystem niche modelling, and showed that 80% of tagged
188 mp forests (PSFs) represent a unique wetland ecosystem of distinctive hydrology which support unique
193 to mitigate climate change impacts on stream ecosystems or to proactively adapt to them will require
194 conditions are rapidly changing in temperate ecosystems, particularly for those that experience perio
196 anding of the long-term dynamics that govern ecosystem persistence and reconciliation of conflicts am
202 xotic species have little apparent impact on ecosystem processes, whereas others have dramatic conseq
206 icate that water availability as a driver of ecosystem productivity in mesic temperate forests is not
208 deciduous shrubs in arctic tundra alters key ecosystem properties including carbon balance and hydrol
209 cies subgraphs, and this has been related to ecosystem properties such as stability and robustness.
211 ve species on native community structure and ecosystem properties were evaluated as a function of dis
212 irect and indirect effects of temperature on ecosystem properties, here we evaluate replicate treelin
213 effects of sticklebacks on a broad range of ecosystem properties, including zooplankton community st
215 f South China may have aided post-extinction ecosystem recovery by stabilizing the sediment surface,
222 r challenges in ecology is to understand how ecosystems respond to changes in environmental condition
225 brown and green diversity components in our ecosystem responded differently to successional gradient
226 ikely be an important moderator of plant and ecosystem responses to adverse effects of more variable
227 ons on mercury (Hg) emissions and associated ecosystem restoration are closely linked to what Hg leve
229 These results demonstrate the persistent ecosystem retention of N deposition even as it redistrib
232 metric for the degree of isohydricity at the ecosystem scale in analogy with a recent metric introduc
233 N status is crucial for predicting plant and ecosystem-scale responses to future changes in atmospher
236 an enhance our understanding of differential ecosystem sensitivity to precipitation extremes, but the
237 mechanistic understanding of differences in ecosystem sensitivity, suggesting that new approaches ar
239 ting these management schemes can facilitate ecosystem service providers without augmenting herbivore
240 Science-Policy Platform on Biodiversity and Ecosystem Services (IPBES) recognize the importance of a
245 al testing of the effects of encroachment on ecosystem services in order to address key knowledge gap
246 restore the sequestration capacity and other ecosystem services provided by Australia tidal marshes.
252 reases the predictability and reliability of ecosystem services, and understanding the drivers of sta
253 nagement or policy to ensure the delivery of ecosystem services, integrated approaches that incorpora
258 rous consequences for water quality and lake ecosystems, so quantifying this amplified response at a
259 postfire weather could drive major shifts in ecosystem structure and function such as altered fire be
260 On the basis of current understanding of ecosystem structure and function, we theorize that mangr
261 Although context dependent, these native ecosystems subjected to prolonged invasion by exotic pla
263 ffer against the impact of warming on marine ecosystems, suggesting a novel mechanism by which divers
268 l on Yellow Sea tidal mudflats, a threatened ecosystem that has shrunk by >65% in recent decades.
269 ne sediments, fjord geochemistry, and marine ecosystems.The reason some of the Earth's tidewater glac
272 serve as one of the most productive natural ecosystems through their ecological, economic and cultur
274 otential threats to and opportunities within ecosystems to inform conservation and policy efforts whe
275 l soil C sequestration, the capacity of land ecosystems to slow the rise in atmospheric CO2 concentra
277 results highlight the importance of seagrass ecosystems to the health of humans and other organisms.
279 d experiments (CDEs) arrayed across multiple ecosystem types and focused on water can enhance our und
282 lude important considerations concerning the ecosystem value of tropical PSFs which are dependent on
283 lanation for variation in observed diversity-ecosystem variability relationships and highlights the i
285 core from Dongsha Atoll, a remote coral reef ecosystem, we observe a decline in the (15)N/(14)N of co
286 h south-shifted storm tracks, while Canadian ecosystems were greener in years when the cool-season st
288 se impacts in Arctic or Subarctic freshwater ecosystems, where the climate is changing most rapidly.
289 on AMF diversity is biased towards temperate ecosystems, whereas little is known about other habitats
290 nctional linkage of organic soils to aquatic ecosystems whereby they can help buffer the effects of h
291 tlantic marine macroalgal forests, important ecosystems whose main structuring species is the annual
292 nt of an algal knowledgebase that integrates ecosystem-wide omics data and the development of molecul
293 for cod that began with overfishing in this ecosystem will likely be exacerbated by warming, but thi
294 ervices benefit from fire, it is unknown how ecosystems will respond to increased burning and warming
295 edict that higher occurrence of FTCs in cold ecosystems will select for large body size within soil m
296 The Q10 varied significantly among different ecosystems with a global average of 2.21, ranging from t
299 cies invasion is an important disturbance to ecosystems worldwide, yet knowledge about the impacts of
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